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Sample records for volcano jalisco mexico

  1. Seismicity at Jalisco-Nayarit Border, Mexico

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    Rutz, M.; Nunez-Cornu, F.; Camarena, M.; Trejo, E.; Reyes-Davila, G.; Suarez-Plasencia, C.

    2003-12-01

    Since 2002 a regional seismic network from Jalisco Civil Defense and University of Guadalalajara is monitoring seismicity at the northwest border of Jalisco block. With the installation of a seismic station on Ceboruco Volcano, by Nayarit Civil Defense, coverage of the network extends to east. Ceboruco Volcano is located on the Tepic-Zacoalco graben, the east border of Jalisco block, this allow us to begin to monitoring this area. The zone of Bahia de Banderas, between the north coast of Jalisco and south coast of Nayarit, probably on a tectonic triple point, is a region of high seismic potential. Activ tectonic structures and clusters in the zone of El Tuito and the Dam Cajon de Pe¤as have been identified. The seismicity in the north area of the bay is low, meanwhile in the south, where the bay is deeper, the seismicity level is higher with an East-West tendency. At the east, the Amatlan de Ca¤as-Ameca zone presents continue activity, here have been possible to locate events with local magnitude between 2 and 4. Tectonovolcanic events registred at Ceboruco station presents waveform with scattering. The seismic distribution of the coast of Jalisco shows parallel alignments to the trench throughout al the coast. Other perpendicular alignments to the coastline show active morphologic structures within the Jalisco block related to the subduction of the Rivera plate under the Jalisco block.

  2. Sports Facilities, Zapopan, Jalisco, Mexico.

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    Amelar, Sarah

    2001-01-01

    Highlights a new K-12 school gymnasium in Mexico that changes and reacts to weather conditions, requires no air conditioning, and, on typical days, uses sunlight filtering through its ample clerestory as the sole source of illumination. Includes numerous photographs, a section drawing, and a site plan. (GR)

  3. Disparities in renal care in Jalisco, Mexico.

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    Garcia-Garcia, Guillermo; Renoirte-Lopez, Karina; Marquez-Magaña, Isela

    2010-01-01

    End-stage renal disease represents a serious public health problem in Mexico. Close to 9% of the Mexican population has chronic kidney disease (CKD) and 40,000 patients are on dialysis. However, the fragmentation of our health care system has resulted in unequal access to renal replacement therapy. In addition, poor patients in Jalisco with kidney failure have very advanced disease at the time of dialysis initiation, suggesting lack of access to predialysis care. To address these issues, a number of strategies have been implemented. Among them a renal replacement therapy program for which the cost of treatment is shared by government, patients, industry, and charitable organizations; the implementation of a state-funded hemodialysis program that provides free dialysis for the poor; the establishment of a university-sponsored residency program in nephrology and a postgraduate training in nephrology nursing; and a screening program for early detection and control of CKD. In conclusion, access to renal care is unequal. The extension of the Seguro Popular to cover end-stage renal disease treatment nationwide and the implementation of community screening programs for the detection and control of CKD offers an opportunity to correct the existing disparities in renal care in Jalisco and perhaps in other regions of Mexico.

  4. Fishprint of Coastal Fisheries in Jalisco, Mexico

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    Myrna Leticia Bravo-Olivas

    2014-12-01

    Full Text Available Coastal fisheries contribute to global food security, since fish are an important source of protein for many coastal communities in the world. However, they are constrained by problems, such as weak management of fisheries and overfishing. Local communities perceive that they are fishing less, as in other fisheries in the world. The aim of this study was to evaluate the fisheries sustainability in the Jalisco coast through the fishing footprint, or fishprint (FP, based on the primary productivity required (PPR and the appropriated surface by the activity (biocapacity. The total catch was 20,448.2 metric tons from 2002–2012, and the average footprint was calculated to be 65,458 gha/year, a figure that quadrupled in a period of 10 years; the biocapacity decreased, and the average trophic level of catches was 3.1, which implies that it has remained at average levels, resulting in a positive balance between biocapacity and ecological footprint. Therefore, under this approach, the fishing activity is sustainable along the coast of Jalisco.

  5. Hazard maps of Colima volcano, Mexico

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    Suarez-Plascencia, C.; Nunez-Cornu, F. J.; Escudero Ayala, C. R.

    2011-12-01

    Colima volcano, also known as Volcan de Fuego (19° 30.696 N, 103° 37.026 W), is located on the border between the states of Jalisco and Colima and is the most active volcano in Mexico. Began its current eruptive process in February 1991, in February 10, 1999 the biggest explosion since 1913 occurred at the summit dome. The activity during the 2001-2005 period was the most intense, but did not exceed VEI 3. The activity resulted in the formation of domes and their destruction after explosive events. The explosions originated eruptive columns, reaching attitudes between 4,500 and 9,000 m.a.s.l., further pyroclastic flows reaching distances up to 3.5 km from the crater. During the explosive events ash emissions were generated in all directions reaching distances up to 100 km, slightly affected nearby villages as Tuxpan, Tonila, Zapotlán, Cuauhtemoc, Comala, Zapotitlan de Vadillo and Toliman. During the 2005 this volcano has had an intense effusive-explosive activity, similar to the one that took place during the period of 1890 through 1900. Intense pre-plinian eruption in January 20, 1913, generated little economic losses in the lower parts of the volcano due to low population density and low socio-economic activities at the time. Shows the updating of the volcanic hazard maps published in 2001, where we identify whit SPOT satellite imagery and Google Earth, change in the land use on the slope of volcano, the expansion of the agricultural frontier on the east and southeast sides of the Colima volcano, the population inhabiting the area is approximately 517,000 people, and growing at an annual rate of 4.77%, also the region that has shown an increased in the vulnerability for the development of economic activities, supported by the construction of highways, natural gas pipelines and electrical infrastructure that connect to the Port of Manzanillo to Guadalajara city. The update the hazard maps are: a) Exclusion areas and moderate hazard for explosive events

  6. [Risk of Mycobacterium tuberculosis infection in Jalisco, Mexico].

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    Gloyd, S; López, J L; Mercado, F J; Durning, J

    1991-11-01

    Using a modified cluster sample design, skin tests with two TU PPD were performed on 4,083 first-grade children (mean age 6,7 years) in the state of Jalisco, Mexico, to estimate the annual risk of infection from Mycobacterium tuberculosis. The proportion of PPD reactions (a diameter of 10 mm or more of induration) was 7.6% in the Guadalajara metropolitan area and 5.5% in the rest of Jalisco. In the total sample, the proportion was 7.4% among children with scars attributed to BCG vaccine and 4.5% in children without BCG scars. The weighted proportion of children with PPD reactions of 10 mm or more was 6.8% statewide. The average annual risk of infection estimated from the group that had not received BCG vaccine was 0.82%. The results suggest that the incidence of smear-positive pulmonary tuberculosis is almost 10 times greater than the number of cases registered annually in Jalisco.

  7. Hydrogeochemical analyses of groundwater from Ameca, Jalisco Mexico.

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    Tostado, M.; Rosas-Elguera, J.; Gomez Hermosillo, C.

    2008-05-01

    The accelerated demographic and industrial growth of settlements in mid cities and surrounding urbane areas, requires larger water volumes for its support, including public use. Usually, these requirements are not met by superficial waters consequently underground water is required to fulfill the general necessities. TheAmeca region in Jalisco, Mexico, is located around 80km west of Guadalajara. This region has been sustained by Agriculture and mining for several decades. This last activity has been mainly developed to the north of the city, precisely on the recharge zone. The infiltrated water, eventually form the aquifers. While it travels, and due to its intrinsic dilution capacity, the water may become polluted. Eventually, if he pollutants are toxic, the water from wells used in cities like Ameca, may result in serious health problems. In this study, the Ameca aquifer is evaluated through chemical analyses of the water from wells serving the city. Thus the natural pollution caused by mineral deposit zones and mines located on the recharge zone can be evaluated.

  8. The Spanish Influence on the Mestizo Folk Dance of Yucatan, Veracruz, and Jalisco, Mexico.

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    Trujillo, Lawrence Alan

    Folk dances from three regions of Mexico (Yucatan, Veracruz, and Jalisco) are examined. Emphasis is placed on the ways in which these folk dances reflect the history and cultural attitudes of the Mexican people and, particularly, on the influence of Spanish culture and history on Mexican folk dances. For the dances of each of these areas,…

  9. The Spanish Influence on the Mestizo Folk Dance of Yucatan, Veracruz, and Jalisco, Mexico.

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    Trujillo, Lawrence Alan

    Folk dances from three regions of Mexico (Yucatan, Veracruz, and Jalisco) are examined. Emphasis is placed on the ways in which these folk dances reflect the history and cultural attitudes of the Mexican people and, particularly, on the influence of Spanish culture and history on Mexican folk dances. For the dances of each of these areas,…

  10. Salvia cacomensis (Lamiaceae, a new species from Jalisco, Mexico Salvia cacomensis (Lamiaceae, una nueva especie de Jalisco, México

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    Jesús Guadalupe González-Gallegos

    2012-06-01

    Full Text Available A new species from a botanically little known region of Jalisco, Mexico, is described and illustrated. The morphology of Salvia cacomensis J. G. González, J. Morales et J. Rodríguez is related to that of the species of sections Briquetia Epling and Tubiflorae (Epling Epling of subgenus Calosphace (Benth. Benth. The new taxon is distinguished by the combination of its essentially glabrous surface, the 2-flowered verticillasters, the pink to magenta corollas, and the particular dimensions of the floral bract, the calyx and the corolla.Se describe e ilustra una especie nueva procedente de una región botánicamente poco conocida de Jalisco, México. La morfología de Salvia cacomensis J. G. González, J. Morales et J. Rodríguez está relacionada con aquella de las especies de las secciones Briquetia Epling y Tubiflorae (Epling Epling del subgénero Calosphace (Benth. Benth. El nuevo taxón se distingue por la combinación de su superficie esencialmente glabra, sus verticilastros bifloros, el color rosa o magenta de sus corolas y las dimensiones particulares de la bráctea floral, el cáliz y la corola.

  11. Variaciones regionales de la mortalidad por homicidios en Jalisco, México Regional variations in homicide mortality in Jalisco, Mexico

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    María Guadalupe Vega-López

    2003-04-01

    Full Text Available El presente estudio busca describir las variaciones regionales de la mortalidad por homicidios en el estado de Jalisco, México, en 1989-1991, 1994-1996 y 1999-2000, analizando a su vez el comportamiento de la tasa de homicidios según género y estratos de bienestar socioeconómico. A partir de la información sobre mortalidad generada por el Instituto Nacional de Estadística, Geografía y Informática, se calcularon tasas ajustadas por edad y género e índices de sobremortalidad masculina. Además, se calcularon razones de tasa y su intervalo de confianza (95%. Los resultados reflejan que la tasa de homicidios presenta una tendencia decreciente en los años 90; que existe un patrón regional de la mortalidad por homicidios, observándose las tasas más altas en regiones periféricas del estado consideradas entre las más pobres; que los municipios ubicados en el estrato de bienestar más bajo presentan un exceso de mortalidad por homicidios estadísticamente significativo, y que hay una evidente sobremortalidad masculina por esta causa. Aspectos como los antes descritos implican tareas y desafíos para la salud pública y para los organismos encargados de preservar la ley y el orden, entre ellos la necesidad de implementar políticas intersectoriales diferenciadas, que tomen en consideración las particularidades que rodean al homicidio y al crimen violento en Jalisco.The present study describes regional variations in homicide rates in Jalisco State, Mexico, in 1989-1991, 1994-1996, and 1999-2000, analyzing the trends by gender and socioeconomic stratum. Using mortality data generated by the National Institute for Statistics, Geography, and Information Technology, homicide rates adjusted by age and gender were calculated, along with rate/female rate ratios; rate ratios by socioeconomic stratum and 95% confidence intervals were also calculated. According to the results, the homicide rate showed: a downward trend in the 1990s; a regional

  12. A Preliminary Study of Seismicity at Ceboruco, Volcano, Nayarit, Mexico

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    Sanchez, J. J.; Nunez-Cornu, F. J.; Suarez-Plascencia, C.; Trejo-Gomez, E.

    2007-12-01

    Ceboruco Volcano is located northwestern of Tepic-Zacoalco graben (Jalisco, Mexico). Its volcanic activity can be divided in four eruptive cycles differentiated by their volcano explosivity index (VEI) and chemical variations as well. As a result of andesitic effusive activity, during the first cycle the "paleo-Ceboruco" edifice was constructed. The end of this cycle is defined by a plinian eruption (VEI is estimated between 3 and 4) which occurred some 1020 years ago and formed the external caldera. During the second cycle an andesitic dome extruded in the interior of the caldera. The dome, called Dos Equis, collapsed and formed the internal caldera. The third cycle is represented by andesitic lava flows which partially cover the northern and south-southwestern part of the edifice. The last cycle is represented by historic andesitic lava flows located in the southwestern flank of the volcano. In February 2003 as part of an agreement with Nayarit Civil Defense a seismic station was installed in the SW flank of the volcano. The station is equipped with a Marslite (lennartz) digitizer with a 3DLe 1Hz. seismic sensor. Detection system is based on a STA/LTA recording algorithm. More than 2000 small earthquakes have been attributed to various local sources, and some of this earthquakes are possibly located beneath Ceboruco volcano. A preliminary classification separates high frequency and low frequency seismic events. The sources of high frequency earthquakes appear to be distributed as evidenced from waveforms variety and changing S-P arrivals separations. The low frequency seismic events also show varying signatures and some of them exhibit extended coda, including some monochromatic character.

  13. Extreme Subduction Earthquake Scenarios and their Economical Consequences for Mexico City and Guadalajara, Jalisco, Mexico

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    Chavez, M.; Cabrera, E.; Perea, N.

    2007-05-01

    The destructive effects of large magnitude, thrust subduction superficial (TSS) earthquakes on Mexico City (MC) and Guadalajara (G) has been shown in the recent centuries. For example, the 7/04/1845 a TSS earthquake with Ms 7+ and epicentral distance of about 250 km from MC occurred on the coast of the state of Guerrero, a Maximum Mercalli Modified Intensity (MMI) of IX-X was reported in MC. Furthermore, the 19/09/1985 a Ms 8.1, Mw 8.01, TSS earthquake with epicentral distance of about 340 km from MC occurred on the coast of the state of Michoacan, a maximum MMI of IX-X was reported in MC. Also, the largest, Ms 8.2, instrumentally observed TSS earthquake in Mexico, occurred in the Colima-Jalisco region the 3/06/1932, with epicentral distance of the order of 200 km from G in northwestern Mexico. The 9/10/1995 another similar event, Ms 7.4, Mw 8, with an epicentral distance of about 240 km from G, occurred in the same region and produced MMI IX in the epicentral zone and MMI up to VI in G. The frequency of occurrence of large TSS earthquakes in Mexico is poorly known, but it might vary from decades to centuries [1]. On the other hand, the first recordings of strong ground motions in MC dates from the early 1960´s and most of them were recorded after the 19/09/1985 earthquake. In G there is only one recording of the later event, and 13 for the one occurred the 9/10/1995 [2]. In order to fulfill the lack of strong ground motions records for large damaging TSS earthquakes, which could have an important economical impact on MC [3] and G, in this work we have modeled broadband synthetics (obtained with a hybrid model that has already been satisfactorily compared with observations of the 9/10/1995 Colima-Jalisco Mw 8 earthquake, [4]) expected in MC and G, associated to extreme magnitude Mw 8.5, TSS scenario earthquakes with epicenters in the so-called Guerrero gap and in the Colima-Jalisco zone, respectively. The proposed scenarios are based on the seismic history and up

  14. [Epidemiologic knowledge and current situation of Chagas disease in the state of Jalisco, Mexico].

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    Lozano-Kasten, Felipe; Magallón-Gastélum, Ezequiel; Soto-Gutiérrez, Margarita; Kasten-Monges, Marina; Bosseno, Marie-France; Brenière, Simone Frédérique

    2008-01-01

    Chagas disease in the state of Jalisco, Mexico was described for the first time in 1967; however, knowledge on the disease remains in a slow process. Between 1967 and 2006, the disease was described in its acute and chronic forms. The vector species have been identified, and the parasite Trypanosoma cruzi has been isolated and genetically characterized. Also, the magnitude of the infection in humans has been determined through serological studies of different populations as well as of blood donors. The up-to-dateness of knowledge of the disease in the state of Jalisco, unveils a necessity of increased research on the epidemiology of Chagas disease as well as on clinical studies to assess the health of individuals and the populations.

  15. Solanaceae diversity in the state of Jalisco, Mexico Diversidad de la familia Solanaceae en el estado de Jalisco, México

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    Carmen Teresa Cuevas-Arias

    2008-06-01

    Full Text Available Mexico is a center of diversity for Solanaceae. Our objective is to analyze the species diversity and geographical distribution of the Solanaceae in Jalisco. The data come from 3 405 herbarium specimens. An analysis of these specimens indicates that the Solanaceae in Jalisco are represented by 20 genera, 138 species and 140 taxa. Four genera, Solanum (55 species, Physalis (35, Cestrum (10 and Lycianthes (9 represent 79% of the total number of species. In contrast, Brachistus, Browallia, Chamaesaracha, Jaltomata, Juanulloa, Lycium, Nectouxia, Nicandra and Nierenbergia have only 1 species each. In Jalisco, the Solanaceae are widely distributed throughout the state occurring at altitudes ranging from sea level to 3 400 m. Mostly, they grow in conifer and oak forest (81 species followed by tropical subdeciduous forest (57, tropical deciduous forest (54, and cloud forest (43. Fifty-one species are commonly found in disturbed and ruderal areas. Lycianthes jalicensis, Physalis lignesens, P. longipedicellata, P. longiloba and P. tamayoi are endemic to the state. These results indicate that Jalisco ranks fourth in species diversity for Solanaceae after the states of Oaxaca, Chiapas and Veracruz.México es un centro de diversificación de la familia Solanaceae. El objetivo de este trabajo es analizar la riqueza y distribución de las especies de Solanaceae en Jalisco. Se examinaron 3 405 ejemplares de herbario y como resultado se registra la presencia de 138 especies y 140 taxones agrupadas en 20 géneros. Los géneros con el mayor número de especies son Solanum (55 especies, Physalis (35, Cestrum (10 y Lycianthes (9. Estos representan el 79% de las especies. En contraste, Brachistus, Browallia, Chamaesaracha, Jaltomata, Juanulloa, Lycium, Nectouxia, Nicandra y Nierenbergia están representados por una especie. En Jalisco, las solánaceas crecen desde el nivel del mar hasta los 3 400 m. Las especies habitan con más frecuencia en el bosque de pino y

  16. [Prevalence of iron and iodine deficiency, and parasitosis among children from Arandas, Jalisco, Mexico].

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    Vásquez-Garibay, Edgar Manuel; Romero-Velarde, Enrique; Nápoles-Rodríguez, Francisco; Nuño-Cosío, María Eugenia; Trujillo-Contreras, Francisco; Sánchez-Mercado, Oscar

    2002-01-01

    To estimate the prevalence of iron deficiency, iodine deficiency and parasitosis in children attending the Instituto Alteño para el Desarrollo de Jalisco (Highlands Institute for Development of Jalisco State, INADEJ), Arandas, Jalisco, Mexico. A cross-sectional study was conducted between 1997 and 1999, among 432 children aged 12 to 120 months attending the INADEJ. Measurements included hematological values, urine iodine concentration, and presence of parasites. Student's t test chi square tests were used for parametric and nonparametric analysis. The prevalence figures of anemia (20 vs 7.4%, p = 0.007) and iron deficiency (60.9 vs 44.4%, p = 0.02) were higher in preschool than in school children. Iodine deficiency was found in 29% (10.5% moderate or severe) and parasitosis in 47.2% of children, mainly E. histolytica (30.2%) and G. lamblia (28.9%). Low income, male gender and lack of social security policy holding were associated to parasitosis. The high prevalence rates of iron deficiency, iodine deficiency, and parasitosis, should be addressed by state health services with effective interventions to restrain these preventable diseases. The English version of this paper is available at: http://www.insp.mx/salud/index.html.

  17. New seismic images of the crust across the Rivera Plate and Jalisco Block (Mexico)

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    Cordoba, Diego; Núñez-Cornú, Francisco Javier; Bartolomé, Rafael; José Dañobeitia, Juan; Bandy, William Lee; Núñez, Diana; Prada, Manel; Escudero-Ayala, Christian; Espíndola, Juan Manuel; Zamora, Araceli; Gómez, Adán; Ortiz, Modesto; Tsujal Working Group

    2015-04-01

    During the spring and summer of 2014, we achieved an extensive offshore geophysical experiment at West Coast of México entitled "Crustal characterization of the Rivera Plate-Jalisco Block boundary and its implications for seismic and tsunami hazard assessment (TSUJAL)". The project is the result of continuous scientific collaboration between institutions in Mexico and Spain, whose main objective is to study the lithospheric structure at the collision zone between Rivera, North America Plates and the Jalisco Block, and identifying submarine structures which can potentially be tsunamigenic sources The active phase of this project carried out in February and March of 2014, we acquired around 5200 km of Multichannel Seismic Reflection (MCS) together with multibeam bathymetry and potential fields (gravity and magnetism) data. Moreover, a wide angle experiment was performed, deploying 16 OBS in 32 locations in Jalisco and Nayarit offshore regions, also recorded on a terrestrial network of 100 portable seismic stations in 240 locations across 5 seismic profiles of 200-300 km in length combined with the Seismological Network of the State of Jalisco (SisVOc). In addition, 8 land seismic stations were installed in Marías Islands and Isabel Island. These instruments registered, in continuous mode, the airgun shots generated by airgun array of 5800 ci, shooting every 120 s. The UK vessel RRS James Cook participated in this project as a part of the exchange program between Spanish and English scientific vessels, she was responsible of marine seismic experiment (MCS & WA) using a 6 km length streamer and a high capacity airgun array. Furthermore, the ARM Holzinger and RV El Puma participated in this project and were provided by the Mexican Navy and UNAM, respectively. The second phase of this project was achieved in June 2014, where 100 short period seismic stations were installed along a 200 km seismic profile from La Caldera de la Primavera (Guadalajara) to Barra de Navidad

  18. Study of Seismic Activity at Ceboruco Volcano, Mexico

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    Nunez-Cornu, F. J.; Escudero, C. R.; Rodríguez Ayala, N. A.; Suarez-Plascencia, C.

    2013-12-01

    Many societies and their economies endure the disastrous consequences of destructive volcanic eruptions. The Ceboruco stratovolcano (2,280 m.a.s.l.) is located in Nayarit, Mexico, at the west of the Mexican volcanic belt and towards the Sierra de San Pedro southeast, which is a key communication point for coast of Jalisco and Nayarit and the northwest of Mexico. It last eruptive activity was in 1875, and during the following five years it presents superficial activity such as vapor emissions, ash falls and riodacitic composition lava flows along the southeast side. Although surface activity has been restricted to fumaroles near the summit, Ceboruco exhibits regular seismic unrest characterized by both low frequency seismic events and volcano-tectonic earthquakes. From March 2003 until July 2008 a three-component short-period seismograph Marslite station with a Lennartz 3D (1Hz) was deployed in the south flank (CEBN) and within 2 km from the summit to monitoring the seismic activity at the volcano. The LF seismicity recorded was classified using waveform characteristics and digital analysis. We obtained four groups: impulsive arrivals, extended coda, bobbin form, and wave package amplitude modulation earthquakes. The extended coda is the group with more earthquakes and present durations of 50 seconds. Using the moving particle technique, we read the P and S wave arrival times and estimate azimuth arrivals. A P-wave velocity of 3.0 km/s was used to locate the earthquakes, most of the hypocenters are below the volcanic edifice within a circular perimeter of 5 km of radius and its depths are calculated relative to the CEBN elevation as follows. The impulsive arrivals earthquakes present hypocenters between 0 and 1 km while the other groups between 0 and 4 km. Results suggest fluid activity inside the volcanic building that could be related to fumes on the volcano. We conclude that the Ceboruco volcano is active. Therefore, it should be continuously monitored due to the

  19. Tsujal Project: New Geophysical Studies about Rivera PLATE and Jalisco Block (MEXICO)

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    Barba, D. C., Sr.; Nunez-Cornu, F. J.; Danobeitia, J.; Bartolome, R.; Bandy, W. L.; Escudero, C. R.; Cameselle, A. L.; Espindola de Castro, J. M., Sr.; Prada, M.; Nunez, D.; Zamora Camacho, A.; Gomez, A.; Ortiz, M.

    2014-12-01

    During spring and summer of 2014, it has been carried out the first geophysical fieldwork of the project entitled "Crustal characterization of the Rivera Plate-Jalisco Block boundary and its implications for seismic and tsunami hazard assessment (TSUJAL)". This is project is the result of a wide scientific collaboration between institutions of Mexico and Spain with the main aim of studying the lithospheric structure in Rivera and North American Plates convergence regions and Jalisco Block, and, also, identifying submarine structures that could be tsunamigenic sources. The first phase of this project was carried out in February and March of 2014. More than 5200 km of Multichannel Seismic Reflection (MCS) data were acquired, together with multibeam and parametric soundings and potential fields (gravity and magnetism) data. Wide Angle profiling were recorded deploying 16 OBS in 32 locations, offshore Jalisco and Nayarit regions Onshore, a network of 100 short period seismic portable stations were deployed in 240 locations along 5 seismic lines of 200-300 km length that worked combined with Seismological Network of Jalisco State (SisVOc). In addition, 8 land seismic stations were installed in Marías Islands and Isabel Island. These instruments registered, in continuous mode, the source energy was generated by big airgun array of 5800 ci, shooting every 120 s. The British vessel RRS James Cook, which participated in this project as a part of the exchange program between Spanish and English scientific vessels, was responsible of carrying out the MCS profiles and the deployment of OBS. For them, it was used a 6 km length digital streamer and airgun array of high capacity. Moreover, the ARM Holzinger and RV El Puma participated in this project and were provided by the Mexican Navy and UNAM, respectively. The second phase of this project was carried out in June 2014. 100 short period seismic stations were installed along one seismic profile from La Caldera de la Primavera

  20. [The social representation that adolescents from Jalisco, Mexico have of early detection of breast cancer].

    Science.gov (United States)

    Tapia Curiel, Amparo; Villaseñor Farías, Martha; Lidia Nuño Gutiérrez, Bertha; Rodríguez Carlos, Aída Araceli; Salas González, Efraín; López López, José Luis

    2014-10-01

    To describe the social representation that adolescents from Jalisco, Mexico, have of early detection of breast cancer. Qualitative cross, analytical interpretative and based on the theory of social representations. Non-probability sampling. Contact schools in basic education level of 7municipalities of the State of Jalisco, Mexico, through various government and educational institutions. A hundred thirty five schooled adolescents, men and women. Interview with 12 focus group 8-12participants and 1 with 18participants. The interviews were transcribed in Atlas Ti program version 4.1 for a semiotic analysis to identify components of social representation. The precocious detection linked itself to the decrease of deaths for cancer of breast, long treatments and mastectomy, but little coverage was perceived to the mammary health of the teenager. They refer as limiter elements of the precocious detection the aspects of kind, psychological and of access to the information and services of health; since facilitators there was mentioned the transition of the limiter elements to facilitators. A favorable panorama appears on the level of awareness of the teenagers on his mammary health, identifying as a sector highly sensitive to the information about cancer of breast and with disposition to effect actions of early detection; there are identified as important challenge the generation of campaigns, educational materials and spaces of health focused on the teenager. Copyright © 2013 Elsevier España, S.L.U. All rights reserved.

  1. Education Reform and Decentralization in Mexico and the Creation of "Educacion Civica" in the State of Jalisco

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    Contreras, Gloria; Rice, Marion J.

    2009-01-01

    In this article, the authors investigate Mexican education reform and decentralization and how the state of Jalisco focused in the early twenty-first century on developing a sequential curriculum for teaching civics in grades 1-6. The authors use the term "educacion civica" because in Mexico the curriculum emphasizes the acquisition of values and…

  2. Education Reform and Decentralization in Mexico and the Creation of "Educacion Civica" in the State of Jalisco

    Science.gov (United States)

    Contreras, Gloria; Rice, Marion J.

    2009-01-01

    In this article, the authors investigate Mexican education reform and decentralization and how the state of Jalisco focused in the early twenty-first century on developing a sequential curriculum for teaching civics in grades 1-6. The authors use the term "educacion civica" because in Mexico the curriculum emphasizes the acquisition of…

  3. Education Reform and Decentralization in Mexico and the Creation of "Educacion Civica" in the State of Jalisco

    Science.gov (United States)

    Contreras, Gloria; Rice, Marion J.

    2009-01-01

    In this article, the authors investigate Mexican education reform and decentralization and how the state of Jalisco focused in the early twenty-first century on developing a sequential curriculum for teaching civics in grades 1-6. The authors use the term "educacion civica" because in Mexico the curriculum emphasizes the acquisition of…

  4. STRUCTURAL AND GEOCHEMICAL CHARACTERISTICS OF SECONDARY DOLOMITIC BODIES OF CRETACEOUS COLIMA-JALISCO BASIN, WESTERN MEXICO

    Science.gov (United States)

    Zarate, P. F.

    2009-12-01

    The cretaceous Colima-Jalisco basin, at western Mexico, is characterized by the development of volcano sedimentary sequences belonging to the Late Jurassic-Early Cretaceous Alisitos-Teloloapan arc-island and the formation of volcanogenic massive sulphide deposits ("El Cuale", "La Minita", "Talpa de Allende"). Some bodies of dolomite have been described and have been classified into two groups in accordance with its secondary origin: sabkha (diagenetic) and hydrothermal. In both cases the primary dolomitized limestone belongs to the reef facies of the Tepalcatepec Formation (TF) of Albian-Cenomanian characterized by the next geochemical content: MgO (0.42%), CaO (53.7%), SiO2 (0.15%), Pb (140 ppm) and Zn (50 ppm). Diagenetical dolomite is characterized by an stratiform body and its contacts are consistent with the structural attitude of TF to which it belongs. In the dolomites formed by hydrothermal replacement process is limited by faults and fractures, thus its morphology is irregular and their contacts are discordant, adopting domic or columnar forms. Occasionally hydrothermal dolomite can be associated with concentrations of lead, zinc, silver and barite. The dolomitic body called "Cerro El Puro", (19° 3.7' N; 103° 36.7' W), located at 20 km SE 30° from Colima City, consists in a carbonate horizon of 300 m thick and over 5 km in length and is consistent with the structural attitude (N30°W; NE50°) of the southwestern flank of the syncline Tepames-Amarradero, in which southeast extreme an evaporitic stratiform deposits. The dolomite of this body is of ankeritic type, hence its typical light reddish brown. The geochemical content is shown on Table 1. After the structural and geochemical features of this dolomite, it is classified as sabkha with a diagenetic origin. The other dolomitic outcrop studied is called “Cerro Bola” (18°54'N; 103°47.5'W) which is located 40 km S10°W from Colima City, and consists of a single dolomitic outcrop, black in color

  5. Assessment of the levels of polybrominated diphenyl ethers in blood samples from Guadalajara, Jalisco, Mexico.

    Science.gov (United States)

    Orta-Garcia, Sandra Teresa; León-Moreno, Lilia Carolina; González-Vega, Carolina; Dominguez-Cortinas, Gabriela; Espinosa-Reyes, Guillermo; Pérez-Maldonado, Iván N

    2012-10-01

    The purpose of this study was to measure levels of polybrominated diphenyl ethers (PBDEs) in the blood of children (50 individuals) living in Guadalajara, Jalisco, Mexico. We analyzed six PBDE congeners by gas chromatography-mass spectrometry. Total PBDE levels ranged from not detectable (nd) to 15.2 μg/L on a whole-weight basis and from nd to 6,435 ng/g lipid on a lipid-weight basis. The dominant congener in our study was BDE-153, followed by BDE-154, BDE-99, BDE-100, and BDE-47. Levels of BDE-209 were below the detection limit. Our data indicate that children living in the areas studied in this work are exposed to high levels of PBDEs.

  6. Coarse-scale spatial and ecological analysis of tuberculosis in cattle: an investigation in Jalisco, Mexico

    Directory of Open Access Journals (Sweden)

    Horacio Zendejas-Martínez

    2008-11-01

    Full Text Available We have tested the hypothesis that coarse-scale environmental features are associated with spatial variation in bovine tuberculosis (BTB prevalence, based on extensive sampling and testing of cattle in the state of Jalisco, Mexico. Ecological niche models were developed to summarize relationships between BTB occurrences and aspects of climate, topography and surface. Model predictions, however, reflected the distributions of dairy cattle versus beef cattle, and the non-random nature of sampling any cattle, but did not succeed in detecting environmental correlates at spatial resolutions of 1 km. Given that the tests employed seek any predictivity better than random expectations, making the finding of no environmental associations conservative, we conclude that BTB prevalence is independent of coarsescale environmental features.

  7. Avifauna de cuatro comunidades del oeste de Jalisco, México Birds of four communities of western Jalisco, Mexico

    OpenAIRE

    Ramírez-Albores,Jorge E.

    2007-01-01

    El conocimiento de la riqueza y composición de la avifauna pueden ser de utilidad en los programas de manejo de las especies silvestres y su hábitat. Se presenta un listado avifaunístico en 4 comunidades del oeste de Jalisco. Se efectuaron monitoreos mensuales de mayo/2000 a agosto/2001, mediante registros a través de transectos. En Tomatlán se registró la mayor riqueza de especies (214), seguida por Jocotlán (190), Ley Federal (168) y Chacala (159). Las especies residentes representaron la m...

  8. Crustal Structure across Rivera Plate and Jalisco Block (MEXICO): TsuJal Project

    Science.gov (United States)

    Nuñez-Cornu, F. J.; Nunez, D.; Barba, D. C., Sr.; Trejo, E.; Escalona, F.; Danobeitia, J.; Gutierrez Pena, Q. J.

    2015-12-01

    Located on the western margin of Mexico, the collision zone between Rivera, Cocos and North American plates is a complex tectonic collage with high seismic hazards and potential tsunamigenic sources. During the spring of 2014, within the framework of TSUJAL project, Spanish and Mexican scientists investigated this region with the main objective of defining the crustal architecture of this active margin and recognizing potential structural sources that can trigger earthquakes and tsunamis at the convergence between Rivera plate-Jalisco block with the North American Plate. To achieve these goals, a wide-ranging of geophysical data was acquired in this region both offshore and onshore. In this paper, we present the preliminary results obtained from this project about bathymetric, structural geology and wide-angle seismic data of the southern coast of Bahía de Banderas. A crustal P-wave velocity model for the southern coast of Bahía de Banderas was obtained using WAS data recorded by OBS and land seismic stations for more than 150 km across Rivera Plate and Jalisco Block. The thickness of the slab in this area is about 10 km and presents a dip angle about 8º. Continental crustal thickness below Puerto Vallarta is about 20 km, no evidence of continental Moho was found in this study. This model support that due to the convergence of Rivera Plate against Jalisco Block, the region of Bahía de Banderas is under strong crustal stresses that generate structural lineaments and have the same trends offshore and inland. Most of the seismicity reported can be associated to the main structural lineaments. The Banderas Canyon apparently is in an opening process from west to east, which seems to continue through the Rio Pitillal river valley. There is no seismic or morphological evidence to consider that the Banderas Canyon is a continuation of Vallarta Graben.South of María Cleofas Island, the SC marks the limit between RP and JB, possibly being the result of the RP against JB

  9. The Geological Trace Of The 1932 Tsunamis In The Tropical Jalisco-Colima Coast, Mexico

    Science.gov (United States)

    Ramirez-Herrera, M.; Blecher, L.; Goff, J. R.; Corona, N.; Chague-Goff, C.; Lagos, M.; Hutchinson, I.; Aguilar, B.; Goguitchaichrili, A.; Machain-Castillo, M. L.; Rangel, V.; Zawadzki, A.; Jacobsen, G.

    2013-05-01

    The study and preservation of tsunami deposits have being challenging in humid tropical environments. While tsunami deposits have been widely studied at temperate latitudes, few studies assess this problem in tropical environments due to the difficulties intrinsic to these places (e.g. tsunami deposit preservation, post-burial changes in a tropical environment, mangrove vegetation, difficult access, wildlife, among others). Here we assess the problem of tsunami-deposits preservation on the Jalisco-Colima tropical coast of Mexico, which parallels the more than 1000-km long Mexican subduction, where historical accounts indicate the occurrence of two significant tsunamis on June 3 and 22, 1932 (Corona and Ramírez-Herrera, 2012a, Valdivia et al., 2012). However, up to date, no geological evidence of these events has been reported. We present geological evidence of two large tsunamis related to the June 3, M 8.2 earthquake, and the June 22, Ms 6.9 landslide-triggering event of 1932 (Corona and Ramírez-Herrera, 2012a, b). A multiproxy approach was applied to unravel the nature of anomalous sand units and sharp basal contacts in the stratigraphy of a number of sites at Palo Verde estuary, El Tecuán swales and marsh, and La Manzanilla swales, on the Jalisco-Colima coast. Lines of evidence including historical, geomorphological, stratigraphic, grain size, organic matter content, microfossils (diatoms and foraminifera), geochemical content, magnetic susceptibility and AMS analyses, together with dating (210Pb and 14C), and modeling, corroborate the presence of tsunami deposits of both the 3 June 1932 tsunami at El Tecuán and La Manzanilla, and the 22 June 1932 tsunami at Palo Verde. Further evidence of earlier tsunamis, at least four events, is also evident in the stratigraphy. Work in progress should reveal the chronology of the earliest tsunamis and their origin. Corona, N., M.T. Ramirez-Herrera. (2012a) Mapping and historical reconstruction of the great Mexican 1932

  10. Contracting private sector providers for public sector health services in Jalisco, Mexico: perspectives of system actors

    Directory of Open Access Journals (Sweden)

    González Luz

    2009-10-01

    Full Text Available Abstract Introduction Contracting out health services is a strategy that many health systems in the developing world are following, despite the lack of decisive evidence that this is the best way to improve quality, increase efficiency and expand coverage. A large body of literature has appeared in recent years focusing on the results of several contracting strategies, but very few papers have addressed aspects of the managerial process and how this can affect results. Case description This paper describes and analyses the perceptions and opinions of managers and workers about the benefits and challenges of the contracting model that has been in place for almost 10 years in the State of Jalisco, Mexico. Both qualitative and quantitative information was collected. An open-ended questionnaire was used to obtain information from a group of managers, while information provided by a self-selected group of workers was collected via a closed-ended questionnaire. The analysis contrasted the information obtained from each source. Discussion and Evaluation Findings show that perceptions of managers and workers vary for most of the items studied. For managers the model has been a success, as it has allowed for expansion of coverage based on a cost-effective strategy, while for workers the model also possesses positive elements but fails to provide fair labour relationships, which negatively affects their performance. Conclusion Perspectives of the two main groups of actors in Jalisco's contracting model are important in the design and adjustment of an adequate contracting model that includes managerial elements to give incentives to worker performance, a key element necessary to achieve the model's ultimate objectives. Lessons learnt from this study could be relevant for the experience of contracting models in other developing countries.

  11. Eruptive history, current activity and risk estimation using geospatial information in the Colima volcano, Mexico

    Science.gov (United States)

    Suarez-Plascencia, C.; Camarena-Garcia, M.; Nunez-Cornu, F. J.; Flores-Peña, S.

    2013-12-01

    Colima volcano, also known as Volcan de Fuego (19 30.696 N, 103 37.026 W), is located on the border between the states of Jalisco and Colima, and is the most active volcano in Mexico. In January 20, 1913, Colima had its biggest explosion of the twentieth century, with VEI 4, after the volcano had been dormant for almost 40 years. In 1961, a dome reached the northeastern edge of the crater and started a new lava flow, and from this date maintains constant activity. In February 10, 1999, a new explosion occurred at the summit dome. The activity during the 2001-2005 period was the most intense, but did not exceed VEI 3. The activity resulted in the formation of domes and their destruction after explosive events. The explosions originated eruptive columns, reaching altitudes between 4,500 and 9,000 masl, further pyroclastic flows reaching distances up to 3.5 km from the crater. During the explosive events, ash emissions were generated in all directions reaching distances up to 100 km, slightly affecting the nearby villages: Tuxpan, Tonila, Zapotlan, Cuauhtemoc, Comala, Zapotitlan de Vadillo and Toliman. During 2005 to July 2013, this volcano has had an intense effusive-explosive activity; similar to the one that took place during the period of 1890 through 1905. That was before the Plinian eruption of 1913, where pyroclastic flows reached a distance of 15 km from the crater. In this paper we estimate the risk of Colima volcano through the analysis of the vulnerability variables, hazard and exposure, for which we use: satellite imagery, recurring Fenix helicopter over flights of the state government of Jalisco, the use of the images of Google Earth and the population census 2010 INEGI. With this information and data identified changes in economic activities, development, and use of land. The expansion of the agricultural frontier in the lower sides of the volcano Colima, and with the advancement of traditional crops of sugar cane and corn, increased the growth of

  12. Tectonic control of the damaged areas by land subsidence: Ameca, Jalisco Mexico, a study case

    Science.gov (United States)

    Rosas-Elguera, J.; Malagon, A.; Maciel, R.; Alatorre, M. A.; Perez, G.

    2009-04-01

    The Miocene to Quaternary Trans-Mexican Volcanic Belt (TMVB), one of the largest mexican volcanic arcs built on the North America plate, covers about 1000 km along central Mexico from the Pacific ocean to the Gulf of Mexico. The structure of west-central Mexico is dominated by a complex assemblage of crustal blocks bounded by major tectonic structures of the TMVB. These are the NW-SE Tepic-Zacoalco, the N-S Colima, and the E-W Chapala grabens, which separate the Jalisco and Michoacan blocks from the stable North American plate. The three grabens join south of Guadalajara to form what has been long interpreted as an active triple junction. The Tepic-Zacoalco rift is composed of the eastern part of the Plan de Barrancas-Santa Rosa graben and by the Ameca and Zacoalco half-grabens. The Ameca city is located in the Ameca half-graben. From 80´s several houses and buildings (more than 300) have been affected by land subsidence for more than two decades. The damage area follows a specific pattern with NW trend which is similar to the regional faults. The land subsidence is associated with the water extraction. We suggest that the distribution of the damage area is controlled by the fault system in combination with the water extraction. Because of the Ameca half-graben has been affected by historical and present day earthquakes and considering the subsurface geology (sandstones, siltstone intercalated with conglomerates) sudden collapses can be expected.

  13. Avifauna de cuatro comunidades del oeste de Jalisco, México Birds of four communities of western Jalisco, Mexico

    Directory of Open Access Journals (Sweden)

    Jorge E Ramírez-Albores

    2007-12-01

    Full Text Available El conocimiento de la riqueza y composición de la avifauna pueden ser de utilidad en los programas de manejo de las especies silvestres y su hábitat. Se presenta un listado avifaunístico en 4 comunidades del oeste de Jalisco. Se efectuaron monitoreos mensuales de mayo/2000 a agosto/2001, mediante registros a través de transectos. En Tomatlán se registró la mayor riqueza de especies (214, seguida por Jocotlán (190, Ley Federal (168 y Chacala (159. Las especies residentes representaron la mayor proporción (70%. Del total de especies registradas, 86 fueron raras y 15 abundantes. Las especies insectívoras y carnívoras fueron las mejor representadas en cuanto a riqueza de especies. Las selvas baja y mediana registraron la mayor riqueza de especies (135 y 97, respectivamente, de las cuales 46 son exclusivas de estos hábitats. La riqueza y composición de la avifauna asociada a la selva baja y a la selva mediana fue diferente de aquellas asociadas a zonas abiertas y perturbadas, debido principalmente a la proporción de especies residentes y migratorias. Las actividades humanas en el uso del suelo con fines agrícolas y ganaderos han ocasionado la modificación de los ecosistemas, transformando el hábitat natural de las especies silvestres.Knowledge of richness and composition of the bird community can be of utility in management programs of wild species and their habitats. I present a list of the avifauna in four communities of the western Jalisco. Monthly monitoring (may/2000 to august/2001, by means transects. Tomatlán had the greatest species richness (214, followed by Jocotlán (190, Ley Federal (168 and Chacala (159. Resident birds representing the 70% of total bird species. Rare species were 86 and abundant 15. The guilds best represented were insectivorous species and those that feed on vertebrates. Tropical deciduous and semideciduous forest had the greatest species richness (135 and 97 species, respectively, of which 46 species

  14. [Water birds from Agua Dulce lake and El Ermitaño estuary, Jalisco, Mexico].

    Science.gov (United States)

    Hernández Vázquez, Salvador

    2005-01-01

    Waterbird abundance, and seasonal and spatial distribution, were studied in two natural water pools at Jalisco, Mexico, from December 1997 through November 1998. Maximum monthly abundance in Agua Dulce lake and El Ermitaño estuary was 86 471 birds (29 686 in Agua Dulce and 56 785 in Ermitaño), with a total cummulative abundance of 179 808 individuals (66 976 in Agua Dulce and 112 832 in Ermitaño). A total of 87 waterbirds species were recorded, 78 in Agua Dulce and 73 in Ermitaño. The higher species richness and abundance was observed during winter, when migratory species arrived. Most species prefered shallow waters, except seabirds which prefered protected areas such as dunes in Agua Dulce. Other groups, like clucks and related species. prefered low salinity areas, for example in the south-east area of Ermitaño. The higher abundance of the shorehirds was found when the water level on the estuary was low. Herons were seen often at areas with high salinity and influenced by tides (e.g. mouth of Ermitaño).

  15. Analysis of the recent (2012-2016) seismic activity in the Guadalajara, Jalisco, Mexico region.

    Science.gov (United States)

    Yamamoto, J.

    2016-12-01

    The central part of Jalisco, Mexico has experienced at different times the occurrence of low magnitude earthquakes sequences and swarms. Although the effect of these earthquakes has been limited to relatively small areas have caused general alarm within the population and even in some cases catastrophes. These groups of earthquakes that have lasted for weeks and even months have greater importance because they affect the most populous state area including the capital city of Guadalajara. An extraordinary example of these series of earthquakes occurred on 8 May 1912 that lasted until September. In the first 18 days 64 events were felt by residents of Guadalajara and about 10 thousand people fled the city for safer places. Since then, there has been a relative seismic activity calm in the region until May 2012 in which a conspicuous seismic activity reactivation has been observed. This paper analyzes the seismic activity starting with the earthquake of May 18, 2012 (03:07 UT) occurred at the west edge of Lake Chapala until the most recent earthquake on 28 July 2016. It includes seven low magnitude earthquakes with magnitudes between 3.5 and 4.8. The analysis includes hypocentral locations revision, determination of fault mechanisms based on polarity of first arrival complemented with results of waveform inversion. Possible causal correlation with known geological structures is discussed.

  16. On the Sound Environment of the City of Puerto Vallarta, Jalisco, Mexico

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    R. R. Boullosa

    2011-12-01

    Full Text Available An exploration of the sound environment in the city of Puerto Vallarta, Jalisco, Mexico, is presented. A series of interviews were held with 19 residents, of which 7 were undergraduate students, related to the perception of sound in or around places of different zones in the so-called “Viejo Vallarta” (“Old Vallarta”.The purpose was twofold, firstly, to explore the ideas people have relating to the sounds they hear in the city -and in general, the ideas they have relating to peace and tranquility and its possible relation with the sound environment-; secondly, to identify some zones or places that have a particular sound environment - positive or negative. Natural sounds emerged as an important part of the sound identity of the Vallarta region and they seem to be highlyappreciated even when the sound levels are high. Sounds related to nature emerged in all interviews: bird calls, sound of wind rustling through trees, sound of breaking sea waves, etc. The interviewees identified places or zones with a negative sonic identity due to disagreeable or high intensity sounds; traffic flow, and mostly the urban bus, is to be blamed for in the main (some mentioned radios at high volume. A series of sound levels (dBA re 20 μPa at threedifferent times of the year: February, April, and October, 2009 were measured in some locations mentioned by the interviewees. The average sound levels found on those locations considered as having a disagreeable identity were the highest.

  17. Dynamics of thermal inversions on Metropolitan Area of Guadalajara, Jalisco Mexico

    Science.gov (United States)

    Valencia, R.; Tereshchenko, I.; Perez, D. A.; Lizarraga, S. J.; Thermal Inversions, Metropolitan Area of Guadalajara

    2013-05-01

    This work attempts an analysis of the dynamics of the meteorological variables in the lower troposphere in the Metropolitan Area of Guadalajara (ZMG), Jalisco, Mexico. It was used the radiosonde database 2000-2012, and a classification of synoptic situations typical for different inversions occurring. Preliminary results indicate that surface temperature inversions dominate the climate of the study area, mainly recorded two times during the year. An investment without matching the rainy season and covers the months of June to September where investments are recorded at a frequency below 41%. And a station with investments in the type of radiation surface which covers the months of January to May and November to December, with a frequency above 86% in October as month leaving transition with a frequency of 64%. As surface temperature inversions which most affect human activity in the ZMG by not allowing the dispersion of pollutants, the results show that these investments have a thickness ranging from 50 to 250 meters high, covering this range for 85% of the investments registered with respect to the temperature difference between the base and the apex of the observed reversal of between 1°C to 12°C, where the average is 5°C and 7 °C. While this shows that during most of the year there are temperature inversions in the ZMG, this does not mean that every day you will have concentration of pollutants above the norm, this is due to the influence of synoptic scale phenomena mainly to a combination of large anticyclonic systems of the Pacific Ocean and Atlantic, affecting mostly Mexico during the months of December to February, alternating with waves of Western middle latitudes.

  18. Geology of El Chichon volcano, Chiapas, Mexico

    Science.gov (United States)

    Duffield, W.A.; Tilling, R.I.; Canul, R.

    1984-01-01

    The (pre-1982) 850-m-high andesitic stratovolcano El Chicho??n, active during Pleistocene and Holocene time, is located in rugged, densely forested terrain in northcentral Chiapas, Me??xico. The nearest neighboring Holocene volcanoes are 275 km and 200 km to the southeast and northwest, respectively. El Chicho??n is built on Tertiary siltstone and sandstone, underlain by Cretaceous dolomitic limestone; a 4-km-deep bore hole near the east base of the volcano penetrated this limestone and continued 770 m into a sequence of Jurassic or Cretaceous evaporitic anhydrite and halite. The basement rocks are folded into generally northwest-trending anticlines and synclines. El Chicho??n is built over a small dome-like structure superposed on a syncline, and this structure may reflect cumulative deformation related to growth of a crustal magma reservoir beneath the volcano. The cone of El Chicho??n consists almost entirely of pyroclastic rocks. The pre-1982 cone is marked by a 1200-m-diameter (explosion?) crater on the southwest flank and a 1600-m-diameter crater apparently of similar origin at the summit, a lava dome partly fills each crater. The timing of cone and dome growth is poorly known. Field evidence indicates that the flank dome is older than the summit dome, and K-Ar ages from samples high on the cone suggest that the flank dome is older than about 276,000 years. At least three pyroclastic eruptions have occurred during the past 1250 radiocarbon years. Nearly all of the pyroclastic and dome rocks are moderately to highly porphyritic andesite, with plagioclase, hornblende and clinopyroxene the most common phenocrysts. Geologists who mapped El Chicho??n in 1980 and 1981 warned that the volcano posed a substantial hazard to the surrounding region. This warning was proven to be prophetic by violent eruptions that occurred in March and April of 1982. These eruptions blasted away nearly all of the summit dome, blanketed the surrounding region with tephra, and sent

  19. Elements for an historical review of the 3 June, 1932 tsunami on the coast of Jalisco, Mexico

    Science.gov (United States)

    Valdivia, L.; Castillo-Aja, M. R.; Estrada-Trejo, M.

    2011-12-01

    On the morning of June 22, 1932 a series of waves between 8 and 10 meters penetrated a mile inland, destroying the town of Cuyutlán in the state of Colima (Mexico), until today it is regarded as one of the strongest tsunamis that have struck the coast of western Mexico in the last 150 years. However, two weeks earlier, on June 3, occurred the largest magnitude earthquake recorded in Mexico (8.2 ms) that cause damages in much of Jalisco, Colima and Nayarit states. The earthquake also produced a tsunami, so far underestimated, and described only as "a wave" that reached the top of the dune in Barra de Navidad (Cumming, 1932), was "observed in the coasts" of Cuyutlán and Manzanillo (Colima), and that caused some damage to Barra de Navidad (Jalisco) and San Blas (Nayarit) (Farreras et al., 1993). The seashore between these two points covers a coastline of over 300 km in length that did not receive any mention . This area, sparsely populated and inaccessible, was hit by a tsunami and its calls for help took so long to be heard that the damage was confused later with those of the Cuyutlan tsunami in June 22. Analysis of notes in the newspapers of the time allow to identify the existence of reports in local media describing that the coast of Jalisco were strongly affected by a tsunami on June 3, 1932. From these data it was possible to trace the exchange of telegrams between municipal authorities and the state government of the time. The information available nowadays let us to document the tsunami penetration up to 8 km, 300 families displaced and 4 people dead, besides the presence of sulfur water. This new evidence helps to historically rethink the tsunami magnitude, and in this way, be able to start a reconsideration of its intensity, geographical distribution and damages.

  20. Melolonthidae nocturnos recolectados en la zona agricola agavera de Jalisco, Mexico

    National Research Council Canada - National Science Library

    Lugo-Garcia, Gabriel Antonio; Ortega-Arenas, Laura Delia; Gonzalez-Hernandez, Hector; Aragon-Garcia, Agustin; Romero-Napoles, Jesus; Rubio-Cortes, Ramon; Angel Moron, Miguel

    2011-01-01

    Con la finalidad de conocer la fauna de melolontidos nocturnos en las zonas agaveras de mayor importancia en el estado de Jalisco, se realizaron capturas mensuales de mayo a agosto de 2007, utilizando...

  1. Scenarios of metal concentrations in the Arcediano Dam (State of Jalisco, Mexico).

    Science.gov (United States)

    Hansen, Anne M; Gonzalez-Marquez, Luis C

    2010-01-01

    The city of Guadalajara, Jalisco, Mexico has 4.1 million inhabitants and a serious deficit in water supply. Once constructed, the Arcediano Dam will catch waters from the Verde and Santiago rivers, and after treatment will provide water to the city. The present study was undertaken to formulate scenarios and estimate risks of polluting the water that will be collected in the dam from the release of contaminants accumulated in sediments. Desorption of metals from sediments was estimated through sampling of water and sediments, chemical analyses of the environmental samples, and numerical modeling of the water-sediment interactions. Water quality generally increased as the river flowed downstream from the El Salto sampling station to the site where the Arcediano Dam will be constructed. Aluminum exceeded the Mexican Criterion for Drinking Water Supply (MCDWS), at all sampling stations, whereas iron and manganese surpassed the criteria at some stations. Trace metals were below their respective criteria. For sediment samples in the river, chrome, copper and zinc exceeded the Canadian Interim Sediment Quality Guidelines (ISQG), whereas manganese and nickel exceeded the probable effect level (PEL). Other metals were below these limits. With exception of the El Salto sampling station, metals were mostly enriched in iron-containing sediments, followed by aluminum-containing clays and, to a lesser extent, by manganese oxides. Therefore, the interaction of metals with iron oxides was considered as the controlling adsorption mechanism. Simulations to estimate risks of water contamination by desorption of metals from sediments indicate that manganese and nickel may reach concentrations higher than the CDWS. In some cases, dissolved concentrations of lead and chrome may be higher than the respective CDWS, especially under conditions of high accumulation of sediments in the dam. Arsenic, copper and mercury concentrations did not exceed the CDWS under the simulated conditions.

  2. Fault-slip distribution of the 1995 Colima-Jalisco, Mexico, earthquake

    Science.gov (United States)

    Mendoza, C.; Hartzell, S.

    1999-01-01

    Broadband teleseismic P waves have been analyzed to recover the rupture history of the large (M(s) 7.4) Colima-Jalisco, Mexico, shallow interplate thrust earthquake of 9 October 1995. Ground-displacement records in the period range of 1-60 sec are inverted using a linear, finite-fault waveform inversion procedure that allows a variable dislocation duration on a prescribed fault. The method is applied using both a narrow fault that simulates a line source with a dislocation window of 50 sec and a wide fault with a possible rise time of up to 20 sec that additionally allows slip updip and downdip from the hypocenter. The line-source analysis provides a spatio-temporal image of the slip distribution consisting of several large sources located northwest of the hypocenter and spanning a range of rupture velocities. The two-dimensional finite-fault inversion allows slip over this rupture-velocity range and indicates that the greatest coseismic displacement (3-4 m) is located between 70 and 130 km from the hypocenter at depths shallower than about 15 km. Slip in this shallow region consists of two major sources, one of which is delayed by about 10 sec relative to a coherent propagation of rupture along the plate interface. These two slip sources account for about one-third of the total P-wave seismic moment of 8.3 X 1027 dyne-cm (M(w) 7.9) and may have been responsible for the local tsunami observed along the coast following the earthquake.

  3. The 18 May 2012 (Ms 4.5) Chapala Lake, Jalisco, Mexico Earthquake

    Science.gov (United States)

    Yamamoto, J.; Espindola, J. M.

    2015-12-01

    The central part of Jalisco, Mexico has experienced at different times the occurrence of low magnitude earthquakes series. Although the effect of these earthquakes have been limited to relatively small areas have caused general alarm within the population and even in some cases true catastrophes (e.g. San Cristobal 1875). These groups of earthquakes that have lasted for weeks and even months have greater importance because they affect the most populous state area including the capital city of Guadalajara. An extraordinary example of these series of earthquakes occurred on 8 may 1912 that lasted until September. In the first 18 days 64 events were felt by residents of Guadalajara. Since then, there has been a relative seismic activity calm in the region. This paper analyzes the earthquake of May 18, 2012 (03:07 UT) occurred at the West edge of Lake Chapala. While it's an event of low magnitude (4.5 Ms) it has the importance of having occurred just 60 km to the South of Guadalajara and for which instrumental data of first quality is available. The focus of the earthquake was located at 20.30 ° N and 103.49 ° W at a depth of 0 km using arrivals of P and S waves at 16 regional seismic stations. However, by the errors of localization inherent in the method focus could be in a range of 0 to 5 km deep. The mechanism of failure using the polarities of the first arrivals favors a clear faulting of dip slip type along a plane with strike = 227 °, Dip = 80 °, and Rake = 93 °. Waveforms analysis is being used to corroborate these results.

  4. A reconnaissance geochemical study of La Primavera geothermal area, Jalisco, Mexico

    Science.gov (United States)

    Mahood, G.A.; Truesdell, A.H.; Templos, M.L.A.

    1983-01-01

    The Sierra La Primavera, a late Pleistocene rhyolitic caldera complex in Jalisco, Me??xico, contains fumaroles and large-discharge 65??C hot springs that are associated with faults related to caldera collapse and to later magma insurgence. The nearly-neutral, sodium bicarbonate, hot springs occur at low elevations at the margins of the complex, whereas the water-rich fumaroles are high and central. The Comisio??n Federal de Electricidad de Me??xico (CFE) has recently drilled two deep holes at the center of the Sierra (PR-1 and Pr-2) and one deep hole at the western margin. Temperatures as high as 285??C were encountered at 1160 m in PR-1, which produced fluids with 820 to 865 mg/kg chloride after flashing to one atmosphere. Nearby, PR-2 encountered temperatures to 307??C at 2000 m and yielded fluids with chloride contents fluctuating between 1100 and 1560 mg/kg after flashing. Neither of the high-temperature wells produced steam in commercial quantities. The well at the western margin of the Sierra produced fluids similar to those from the hot springs. The temperature reached a maximum of 100??C near the surface and decreased to 80??C at 2000 m. Various geothermometers (quartz conductive, Na/K, Na-K-Ca, ??18O(SO4-H2O) and D/H (steam-water) all yield temperatures of 170 ?? 20??C when applied to the hot spring waters, suggesting that these spring waters flow from a large shallow reservoir at this temperature. Because the hot springs are much less saline than the fluids recovered in PR-1 and PR-2, the mixed fluid in the shallow reservoir can contain no more than 10-20% deep fluid. This requires that most of the heat is transferred by steam. There is probably a thin vapor-dominated zone in the central part of the Sierra, through which steam and gases are transferred to the overlying shallow reservoir. Fluids from this reservoir cool from ???170??C to 65??C by conduction during the 5-7 km of lateral flow to the hot springs. ?? 1983.

  5. Microbiological safety of domestic refrigerators and the dishcloths used to clean them in Guadalajara, Jalisco, Mexico.

    Science.gov (United States)

    Macías-Rodríguez, M E; Navarro-Hidalgo, V; Linares-Morales, J R; Olea-Rodríguez, M A; Villarruel-López, A; Castro-Rosas, J; Gómez-Aldapa, C A; Torres-Vitela, M R

    2013-06-01

    Household refrigerators are a potential pathogen contamination source for foods. An evaluation of the microbiological safety of 200 refrigerators in Guadalajara, Jalisco, Mexico, was made by visual inspection, ATP-bioluminescence levels, indicator microorganisms including Escherichia coli and Staphylococcus aureus, and the presence of Listeria monocytogenes and Salmonella. Additionally, interviews of the owners of the refrigerators were carried out to determine relationships between food storage practices, demographic aspects, and microbiological status. Dishcloths used to clean refrigerators were also analyzed. Operational conditions (cleanliness, fullness, organization, frequency of cleaning, and temperature) were evaluated by trained observers. Results showed deficient cleanliness in 55% of refrigerators, 22% were completely full, 43% very disorganized, 28% were usually cleaned only once in 3 to 6 months, and 53% had internal temperatures >7.1°C. ATP-bioluminescence levels were >300 relative light units on 67 and 74% of shelves and drawers, respectively, indicating that surfaces were dirty according to the luminometer manufacturer. Psychrotrophic aerobic bacteria counts on shelves, drawers, and dishcloths were 6.3, 5.2, and 6.3 log CFU/cm(2); for coliform bacteria, 5.2, 3.9, and 4.7 CFU/cm(2); for E. coli, 3.7, 3.5, and 4.8 CFU/cm(2); and for Staphylococcus aureus, 2.1, 2.5, and 2.3 CFU/cm(2), respectively. L. monocytogenes and Salmonella were isolated from 59.5, 20.5, and 17% and 32.5, 8.0 and 12.5% of shelves, drawers, and dishcloths, respectively. Four Salmonella serotypes and nine serogroups (partially serotyped isolates) were identified. The most prevalent were Salmonella Anatum (39.5%), Salmonella group E1 (19.7%), and Salmonella group E1 monophasic (12.5%). Operational conditions and microbiological status were clearly deficient in sampled refrigerators, highlighting the consequent risk of foodborne disease among users. Educational programs are needed to

  6. Especie nueva de Dolichoderus (Hymenoptera: Formicidae de Puerto Vallarta, Jalisco y nuevos registros para México A new species of Dolichoderus (Hymenoptera: Formicidae from Puerto Vallarta, Jalisco, and new records for Mexico

    Directory of Open Access Journals (Sweden)

    José Luis Ortega-De Santiago

    2012-12-01

    Full Text Available Se describe Dolichoderus tridentanodus sp. nov. recolectada en Puerto Vallaría, Jalisco, México, con base en obreras y que pertenece al complejo lugens. Esta especie se distingue de D. lugens por presentar 6 dientes en el margen interno de la mandíbula, 2 espinas dorsales en el propodeo, 2 protuberancias a los costados del pecíolo y 1 espina central; el cuerpo con abundante pubescencia de color dorado y cubierto por puntuaciones densas y marcadas;. es negro, con mandíbulas, clípeo, antenas y patas de color amarillo. Se cita para los estados de Jalisco, Nayarit y San Luis Potosí. Se proporciona una clave para las especies de Dolichoderus en México, así como la distribución de las especies con nuevos registros para algunos estados.We describe Dolichoderus tridentanodus sp. nov. collected in Puerto Vallarta, Jalisco, Mexico based on workers, which is placed in the lugens complex. This species can be distinguished from D. lugens by the presence of 6 teeth in the internal margin of the mandible, 2 spines on the dorsal face of the propodeum, 2 lateral projections on the petiole and 1 central spine; body with abundant golden pubescence, densely and uniformly covered with coarse punctures; dark color, with yellow mandibles, clipeus, antenna and legs. This species is known for the states of Jalisco, Nayarit and San Luis Potosí. We provide a key for all the species of Dolichoderus in Mexico, and data of distribution with new records for some states.

  7. Ecological Restoration of the La Primavera Forest Geothermal Zone, Jalisco, Mexico; Restauracion ecologica de lazona geotermica del bosque La Primavera, Jalisco, Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Pastrana Melchor, Eugenio J.; Manon Mercado, Alfredo; Hernandez Ayala, Cuauhtemoc [Gerencia de Proyectos Geotermoelectricos de la Comision Federal de Electricidad, Morelia, (Mexico)

    1997-05-01

    The Bosque La Primavera is an oak-pine forest covering a surface estimated in 36 000 hectares. It is located westerly from Guadalajara City, Jalisco. Over a small part of the forest, between 1980 and 1988 the Comision Federal de Electricidad (Federal Commission for Electricity, or CFE) carried out several works to drill 13 geothermal wells, which caused environmental impacts on 53 hectares of the forest; this means 0.15% of the forestry area. In March 1989 the CFE suspended its geothermal exploration and development activities in the zone, and started an exhaustive program to restore the environmental impacts. So, between 1989 and 1994 different works were done within two hydrographic micro-basins (named the Arroyo El Caracol and Arroyo El Huilustre micro-basins) where the CFE works are located. Objectives were to reduce the exposed to erosion areas at the high portions of those micro-basins, and to retain sediments at low portions of the same. Up to now the erosion index, which have been monitored by CFE each year, have reached comparable values to those from the beginning of eighties. This means those restoration works are successful. [Espanol] El bosque La Primavera se encuentra constituido principalmente por encino-pino con una superficie aproximada de 36 mil hectareas, localizado al occidente de la ciudad de Guadalajara, Jalisco. En una pequena porcion de el, la Comision Federal de Electricidad (CFE) llevo a cabo, entre 1980 y 1988, diversas obras para perforar un total de 13 pozos geotermicos que ocasionaron impactos al ambiente en 53 hectareas del bosque, correspondientes al 0.15% de la superficie boscosa. A partir de marzo de 1989 la CFE suspendio sus actividades de exploracion y desarrollo geotermico en la zona, para llevar a cabo un exhaustivo programa de restauracion ecologica de los impactos ambientales. Asi, entre 1989 y 1994 se realizaron trabajos en las dos microcuencas hidrograficas en las que se ubican las obras realizadas por la CFE, las

  8. Crustal imaging of western Michoacán and the Jalisco Block, Mexico, from Ambient Seismic Noise

    Science.gov (United States)

    Spica, Zack; Cruz-Atienza, Víctor M.; Reyes-Alfaro, Gabriel; Legrand, Denis; Iglesias-Mendoza, Arturo

    2014-12-01

    Detailed crustal imaging of western Michoacán and the Jalisco Block is obtained from ambient noise tomography. Results show a deep and well-delineated volcanic system below the Colima volcano complex, rooting up to ~ 22 km depth, with a shallow magmatic chamber constrained to the first ~ 7 km. A shallow low-velocity system to the south of the Chapala rift and west of the Michoacán-Guanajuato volcanic field merges, underneath the Colima rift, with the Colima volcano system at about 20 km depth, honoring the geometry of the Trans-Mexican Volcanic Belt. For depths greater than ~30 km, low-velocity features become parallel to the slab strike, right beneath the Mascota, Ayutla and Tapalpa volcanic fields, suggesting the presence of the mantle wedge above the Rivera plate. All mentioned low-velocity bodies are spatially correlated with the superficial volcanic activity suggesting their magmatic origin so that, the shallower these bodies, the younger are the associated volcanic deposits. Along the coast, different depths of the uppermost layer of the Rivera and the Cocos plates suggest that the latter plate subducts with an angle ~ 9° steeper than the former.

  9. [Short-term impact of changes in drinking-and-driving legislation in Guadalajara and Zapopan, Jalisco, Mexico].

    Science.gov (United States)

    Gómez-García, Lourdes; Pérez-Núñez, Ricardo; Hidalgo-Solórzano, Elisa

    2014-06-01

    The municipalities of Guadalajara and Zapopan, Jalisco State, Mexico, have participated in efforts to reduce road traffic injuries. They have participated actively in the Mexican Road Safety Initiative since 2008. As a result, in September 2010 they passed laws to reduce the legal alcohol levels for driving motor vehicles. To assess the short-term impact of these measures on rates and severity of alcohol-related collisions and injuries, we conducted a secondary analysis of official databases on mortality, morbidity, and collisions. We performed a time-series analysis to assess the trend. Significant changes were observed in the monthly proportion of alcohol-related deaths and collision rates following these interventions. The article concludes with recommendations to improve the reform's enforcement and results.

  10. Lo que Piensan los Estudiantes y Profesores Sobre la Calidad de la Educacion Superior. Estudio Comparativo en 5 Instituciones de Educacion Superior--dos publicas y tres privadas--en Guadalajara, Jalisco, Mexico (What Students and Faculties Think about the Quality of Higher Education. Comparative Study of 5 Higher Education Institutions--Two Public and Three Private--in Guadalajara, Jalisco, Mexico).

    Science.gov (United States)

    Yanez, Maria Lorena Hernandez

    This study, written in Spanish, compared attitudes of students (N=302) and faculty (N=28) at five institutions of higher education (two public and three private) in Guadalajara, Jalisco, Mexico. The study explored first, whether respondents believed there are significant quality differences between private and public universities and, second, what…

  11. Economic impact of fatal and non-fatal road traffic injuries in Guadalajara Metropolitan Area and Jalisco, Mexico.

    Science.gov (United States)

    Pérez-Núñez, Ricardo; Avila-Burgos, Leticia; Híjar-Medina, Martha; Pelcastre-Villafuerte, Blanca; Celis, Alfredo; Salinas-Rodríguez, Aarón

    2011-10-01

    To estimate the economic cost of fatal and non-fatal road traffic injuries (RTI) in Guadalajara metropolitan area (GMA) and Jalisco, Mexico during 2007. Using an incidence-based cost of illness analysis from a household perspective employing a bottom-up approach all direct medical and non-medical costs, and indirect costs were estimated for a sample of RTI people who sought care during 1 month in four different medical facilities. Individuals were surveyed just before discharge from emergency rooms (ER) and hospitalisation services. Hospitalised individuals were followed up at 8 weeks after discharge. Productivity loss was estimated with the human capital approach. Using estimated costs and administrative records of mortality and morbidity, the economic costs were dimensioned for GMA and for Jalisco. A multivariate and probabilistic sensitivity analysis was conducted to evaluate variations resulting from assumptions used. 297 injured were included in the study, 20% were hospitalised and 237 only received care at ER. A total cost of US$21190 was estimated in all injured receiving care at ER and $83309 for those hospitalised. Direct cost represents more than 30% of reported income in 8% of the ER users and 80% of hospitalised. Total economic cost was US$329,061,813 for GMA (discount rate of 3%), nearly 51% of the state total (US$650,908,924 or 1.3% of State GNP). This estimation shows the high cost (both, direct and indirect) RTI impose in households affecting their economy and leading families to lose wealth assets, get in debt or impoverished.

  12. Environmental evaluation of fluoride in drinking water at "Los Altos de Jalisco," in the central Mexico region.

    Science.gov (United States)

    Hurtado, Roberto; Gardea-Torresdey, Jorge

    Naturally occurring fluoride has been detected and quantified in drinking water in several cities of the "Los Altos de Jalisco" (LAJ) region. LAJ is located in the northeastern part of the state of Jalisco-Mexico, covering an area of 16,410 km2 with a population of 696,318 in 20 municipalities. Drinking water comes mainly from groundwater aquifers, located in the Trans-Mexican Volcanic Belt, which is a volcanic region characterized by hydrothermal activity. Results indicated that water supply from 42% of the municipalities had a fluoride concentration over the Mexican standards of 1.5 mg/L. It is important to notice that there are three cities, Lagos de Moreno (1.66-5.88 mg/L F(-)), Teocaltiche (3.82-18.58 mg/L F(-)), and Encarnación de Díaz (2.58-4.40 mg/L F(-)) where all water samples resulted in fluoride concentration over the maximum contaminant level. The total population from these three cities is over 122,000 inhabitants. Another important city with high levels of fluoride in the water supply was Tepatitlán de Morelos (2 wells with 6.54 and 13.47 mg/L F(-)). In addition to water supply, 30 samples of brand-name bottled water were tested. Surprisingly, 8 samples (27%) demonstrated fluoride level over the standards, mainly Agua de Lagos with 5.27 mg/L. Fluoridated table salt (200-300 mg/kg F(-)) is another important source of fluoride. A large number of people living in the region, mainly school children, might be under adverse health risk because they are consuming contaminated drinking water. It is well known that long-term exposure to water with high levels of fluoride produces severe health problems.

  13. Prevalencia de deficiencia de hierro y yodo, y parasitosis en niños de Arandas, Jalisco, México Prevalence of iron and iodine deficiency and parasitosis in children from Arandas, Jalisco, Mexico

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    Edgar Manuel Vásquez-Garibay

    2002-06-01

    Full Text Available Objetivo. Estimar la prevalencia de deficiencia de hierro, yodo y parasitosis en niños que asisten al Instituto Alteño para el Desarrollo de Jalisco (Inadej, Arandas, Jalisco, México. Material y métodos. Estudio transversal efectuado entre 1997 y 1999 con 432 niños de 12 a 120 meses de edad, de nuevo ingreso al Inadej. Se determinaron variables hematológicas, yodo en orina y presencia de parásitos. Se utilizaron las pruebas Ji cuadrada y t de Student en variables no paramétricas y paramétricas. Resultados. Hubo más anemia (20 vs 7.4% p=0.007 y deficiencia de hierro (60.9 vs 44.4% p=0.02 en prescolares que en escolares. El 29% presentaron deficiencia de yodo (10.5% moderada o grave y 47.2% parasitosis. Predominaron G. lamblia y E. histolytica. Bajo salario, sexo masculino y no tener seguridad social se asociaron con parasitosis. Conclusiones. La elevada prevalencia de deficiencia de hierro, yodo y parasitosis obliga al sector salud estatal a ejecutar medidas eficaces para abatir estas enfermedades prevenibles.Objective. To estimate the prevalence of iron deficiency, iodine deficiency and parasitosis in children attending the Instituto Alteño para el Desarrollo de Jalisco ((Highlands Institute for Development of Jalisco State, INADEJ, Arandas, Jalisco, Mexico. Material and Methods. A cross-sectional study was conducted between 1997 and 1999, among 432 children aged 12 to 120 months attending the INADEJ. Measurements included hematological values, urine iodine concentration, and presence of parasites. Student's t test chi square tests were used for parametric and non-parametric analysis. Results. The prevalence figures of anemia (20 vs 7.4%, p=0.007 and iron deficiency (60.9 vs 44.4%, p=0.02 were higher in preschool than in school children. Iodine deficiency was found in 29% (10.5% moderate or severe and parasitosis in 47.2% of children, mainly E. histolytica (30.2% and G. lamblia (28.9%. Low income, male gender and lack of social

  14. Land subsidence, Ground Fissures and Buried Faults: InSAR Monitoring of Ciudad Guzmán (Jalisco, Mexico

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    Carlo Alberto Brunori

    2015-07-01

    Full Text Available We study land subsidence processes and the associated ground fissuring, affecting an active graben filled by thick unconsolidated deposits by means of InSAR techniques and fieldwork. On 21 September 2012, Ciudad Guzmán (Jalisco, Mexico was struck by ground fissures of about 1.5 km of length, causing the deformation of the roads and the propagation of fissures in adjacent buildings. The field survey showed that fissures alignment is coincident with the escarpments produced on 19 September 1985, when a strong earthquake with magnitude 8.1 struck central Mexico. In order to detect and map the spatio-temporal features of the processes that led to the 2012 ground fissures, we applied InSAR multi-temporal techniques to process ENVISAT-ASAR and RADARSAT-2 satellite SAR images acquired between 2003 and 2012. We detect up to 20 mm/year of subsidence of the northwestern part of Ciudad Guzmán. These incremental movements are consistent with the ground fissures observed in 2012. Based on interferometric results, field data and 2D numerical model, we suggest that ground deformations and fissuring are due to the presence of areal subsidence correlated with variable sediment thickness and differential compaction, partly driven by the exploitation of the aquifers and controlled by the distribution and position of buried faults.

  15. Climbing in the high volcanoes of central Mexico

    Science.gov (United States)

    Secor, R. J.

    1984-01-01

    A chain of volcanoes extends across central Mexico along the 19th parallel, a line just south of Mexico City. The westernmost of these peaks is Nevado de Colima at 4,636 feet above sea level. A subsidiary summit of Nevado de Colima is Volcan de Colima, locally called Fuego (fire) it still emits sulphurous fumes and an occasional plume of smoke since its disastrous eruption in 1941. Parictuin, now dormant, was born in the fall of 1943 when a cornfield suddenly erupted. Within 18 months, the cone grew more than 1,700 feet. Nevado de Toluca is a 15,433-foot volcanic peak south of the city of Toluca. Just southeast of Mexico City are two high volcanoes that are permanently covered by snow: Iztaccihuatl (17,342 fet) and Popocatepetl (17,887 feet) Further east is the third highest mountain in North America: 18,700-foot Citlateptl, or El Pico de Orizaba. North of these high peaks are two volcanoes, 14, 436-foot La Malinche and Cofre de Perote at 14,048 feet. This range of mountains is known variously as the Cordillera de Anahuac, the Sierra Volcanica Transversal, or the Cordillera Neovolcanica. 

  16. Analysis of Vulnerability Around The Colima Volcano, MEXICO

    Science.gov (United States)

    Carlos, S. P.

    2001-12-01

    The Colima volcano located in the western of the Trasmexican Volcanic Belt, in the central portion of the Colima Rift Zone, between the Mexican States of Jalisco and Colima. The volcano since January of 1998 presents a new activity, which has been characterized by two stages: the first one was an effusive phase that begin on 20 November 1998 and finish by the middle of January 1999. On February 10of 1999 a great explosion in the summit marked the beginning of an explosive phase, these facts implies that the eruptive process changes from an effusive model to an explosive one. Suárez-Plascencia et al, 2000, present hazard maps to ballistic projectiles, ashfalls and lahars for this scenario. This work presents the evaluation of the vulnerability in the areas identified as hazardous in the maps for ballistic, ashfalls and lahars, based on the economic elements located in the middle and lower sections of the volcano building, like agriculture, forestry, agroindustries and communication lines (highways, power, telephonic, railroad, etc). The method is based in Geographic Information Systems, using digital cartography scale 1:50,000, digital orthophotos from the Instituto Nacional de Estadística, Geografía e Informática, SPOT and Landsat satellite images from 1997 and 2000 in the bands 1, 2 and 3. The land use maps obtained for 1997 and 2000, were compared with the land use map reported by Suárez in 1992, from these maps an increase of the 5 porcent of the sugar cane area and corn cultivations were observed compared of those of 1990 (1225.7 km2) and a decrease of the forest surface, moving the agricultural limits uphill, and showing also some agave cultivation in the northwest and north hillslopes of the Nevado de Colima. This increment of the agricultural surface results in bigger economic activity in the area, which makes that the vulnerability also be increased to different volcanic products emitted during this phase of activity. The degradation of the soil by the

  17. The forecasting of the 1995 Colima-Jalisco, Mexico, earthquake (Mw = 8): A case history

    OpenAIRE

    2005-01-01

    En 1995 la región de Colima-Jalisco (103.7-106°W) fue identificada como una zona con una alta probabilidad para la ocurrencia de un gran sismo (Ms #8805; 7.5) antes de finalizar el año 1996. Este pronóstico se basó en resultados obtenidos del método de reconocimiento de patrones y de estudios de brecha sísmica y la distribución Weibull para la recurrencia de grandes temblores a lo largo de la zona de subducción mexicana. El 9 de octubre de 1995, un evento de magnitud Mw = 8 ocurrió dentro de...

  18. Applicability of prediction equations for cutability in beef carcasses in Jalisco, Mexico

    Directory of Open Access Journals (Sweden)

    J.M. Zorrilla-Ríos

    2013-01-01

    Full Text Available Se evaluaron ecuaciones disponibles en la literatura de predicción de rendimiento, en cortes de canales de bovino deshuesadas tipo español- jalisciense, en condiciones comerciales en la zona Metropolitana de Guadalajara, Jalisco (México. A 30 canales de bovino se les registró peso, área del músculo Longissimus dorsae (lma, grosor de la grasa subcutánea (scfat, grasa pélvica renal y peso individual de cada corte y recorte. La suma de los cortes y recortes se expresó tanto como rendimiento total en kilogramos (trc como en porcentaje del peso de la canal (tryd. Las ecuaciones disponibles de predicción de tryd mostraron una R2 ajustada de 0.279 a 0.355. Tres de siete ecuaciones evaluadas mostraron un coeficiente del intercepto cercano a cero y uno para tasa de cambio. Al expresar los datos como trc, arrojó una R2 ajustada de 0.929 a 0.969. Estas mismas tres ecuaciones mostraron un coeficiente de intercepto y tasa de cambio cercanos a cero y uno, respectivamente. Los análisis de regresión entre las características medidas en las canales y su rendimiento sugieren que el mejor modelo para predecir el tryd incluye todas las varia bles consideradas, excepto el peso de la canal, justificando el 44.50% de la variación del porcentaje de rendimiento. Cuando se analiza el trc, el peso de la canal explicó el 95.60% de la variación existente. Se concluye que algunas ecuaciones disponibles de predicción de rendimiento de cortes para canales de bovino podrían ser aplicadas a canales procesadas en el estado de Jalisco, cuando expresen trc.

  19. Prediction of cutability of beef carcasses processed in Jalisco State, Mexico

    Directory of Open Access Journals (Sweden)

    J. M. Zorrilla-Ríos

    2013-01-01

    Full Text Available En un estudio previo se reportó la factibilidad de utilizar, en condiciones locales, ecuaciones disponibles de predicción de cortabilidad con base en kilogramos (TRC, o expresada como porcentaje de la canal (TRYD de bovino. Todas las ecuaciones consideradas incluyen variables obtenidas en el cuarteo de una media canal, lo que representa una limitante para su adopción en regiones del país (el estado de Jalisco incluido, en donde la evaluación de las canales —previa a su comercialización— se lleva a cabo sin el cuarteo de la media canal. Esta condición marca la necesidad de disponer de ecuaciones de predicción que no se sustenten en variables generadas con el cuarteo de la media canal, lo que se convirtió en el objetivo de esta investigación. Las ecuaciones de predicción propuestas se basan en los datos obtenidos de la fabricación tipo corte español, de treinta canales de toretes cruza indefinida cebú-europeo y menores a 36 meses de edad, procesadas en condiciones comerciales en una carnicería del municipio de Guadalajara, Jalisco, México. El peso de la canal fría mostró una correlación positiva (r=0.98 con el rendimiento de cortes expresados en kilogramos. Un modelo matemático de predicción del peso de los cortes comerciales mostró que la variable de peso de la canal, por sí sola, explicó el 95.60% de la varianza estimada, por lo que se propone como ecuación de predicción bajo estas condiciones.

  20. Influence of climatic conditions, topography and soil attributes on the spatial distribution of site productivity index of the species rich forests of Jalisco, Mexico

    Institute of Scientific and Technical Information of China (English)

    Adel Mohamed; Robin M. Reich; Raj Khosla; C. Aguirre-Bravo; Martin Mendoza Briseño

    2014-01-01

    This paper presents an approach based on field data to model the spatial distribution of the site productivity index (SPI) of the diverse forest types in Jalisco, Mexico and the response in SPI to site and cli-matic conditions. A linear regression model was constructed to test the hypothesis that site and climate variables can be used to predict the SPI of the major forest types in Jalisco. SPI varied significantly with topog-raphy (elevation, aspect and slope), soil attributes (pH, sand and silt), climate (temperature and precipitation zones) and forest type. The most important variable in the model was forest type, which accounted for 35% of the variability in SPI. Temperature and precipitation accounted for 8 to 9% of the variability in SPI while the soil attributes accounted for less than 4% of the variability observed in SPI. No significant differences were detected between the observed and predicted SPI for the individual forest types. The linear regression model was used to develop maps of the spatial variability in predicted SPI for the individual forest types in the state. The spatial site productivity models developed in this study provides a basis for understanding the complex relationship that exists between forest productivity and site and climatic conditions in the state. Findings of this study will assist resource managers in making cost-effective decisions about the management of individual forest types in the state of Jalisco, Mexico.

  1. Igneous Petrogenesis of Tequila Volcano, Western Mexico

    Science.gov (United States)

    Vázquez-Duarte, A.; Gómez-Tuena, A.; Díaz-Bravo, B.

    2011-12-01

    Tequila volcano belongs to a Quaternary volcanic chain that runs in parallel to the Middle American Trench, but that have been constructed within the so-called Tepic-Zacoalco rift: an extensional tectonic structure that has been active for the past 3.5 Ma. This unusual tectonic setting, and the existence of a high-resolution stratigraphy for the Tequila Volcanic Field (Lewis-Kenedi, 2005, Bull Volcanol), provide an excellent opportunity to study andesite petrogenesis. New comprehensive geochemical data allow the recognition of at least four different magmatic series around Tequila: 1) The Santa Rosa intraplate basalts (1.0 - 0.2 Ma), a volcanic plateau constructed along the Santiago River Fault north of Tequila volcano. These Na-alkaline basalts are olivine-phyric, have negligible subduction signatures (Ba/Nb= 11.75 - 49.36), and display Sr-Nd-Pb isotopic compositions that correlate with fractionation indexes, probably indicating melt-crust interactions. 2) A group of vitreous domes and flows of dacitic to rhyolitic compositions, mostly contemporaneous to the Santa Rosa basalts, that were emplaced on the periphery of Tequila volcano. These rocks can have very low Sr and Eu contents but their isotopic compositions are remarkably constant and similar to the Santa Rosa basalts, probably indicating a genetic link through low pressure fractionation in the stability field of plagioclase. 3) The main edifice of Tequila volcano (~0.2 Ma) is made of two pyroxene andesites and dacites with strong subduction signatures (Ba/Nb= 53-112), that inversely correlate with MgO contents, but that follow a diverging evolutionary trend as the rest of the sequences. The isotopic compositions of Tequila main edifice can extend to slightly more enriched values, but do not correlate with fractionation indexes, thus indicating provenance from a different source. 4) The youngest activity on Tequila volcano (~0.09 Ma) is represented by amphibole bearing andesites that erupted through the

  2. Prevalence of Dementia, Emotional State and Physical Performance among Older Adults in the Metropolitan Area of Guadalajara, Jalisco, Mexico

    Science.gov (United States)

    Velázquez-Brizuela, Irma E.; Ortiz, Genaro G.; Ventura-Castro, Lucia; Árias-Merino, Elva D.; Pacheco-Moisés, Fermín P.; Macías-Islas, Miguel A.

    2014-01-01

    Background. Dementia affects memory, thinking, language, judgment, and behavior. Depression, is common in older adults with dementia. The concomitance of dementia and depression increases disability with impaired activities of daily living (ADL), increasing the chances of institutionalization and mortality. Methods. Cross-sectional study of a population 60 years and older who live in the State of Jalisco, Mexico. A total of 1142 persons were assessed regarding their cognitive function, emotional state, and physical performance. Door-to-door interview technique was assigned in condition with multistage probability random sampling. Cognitive function, depression and functional disability were assessed by applying standardized Minimental State Examination (Folstein), Geriatric Depression Scale, and the Katz index, respectively. Diagnosis of dementia was performed according to the criteria of the Diagnostic and Statistical Manual of Mental Disorders, the Fourth Edition. Data were analyzed using SPSS software. Results. Prevalence of demency was 9.5% (63.35% women, and 36.7% men). Demency was associated with being woman, being older than 70 years, low level of education, not having the economic benefit of retirement, being single or living without a partner, low level of education, suffering from depression and have functional disability in ADL. Conclusion. Dementia is more common in women and is related to depression and disability. PMID:24795758

  3. Prevalence of Dementia, Emotional State and Physical Performance among Older Adults in the Metropolitan Area of Guadalajara, Jalisco, Mexico.

    Science.gov (United States)

    Velázquez-Brizuela, Irma E; Ortiz, Genaro G; Ventura-Castro, Lucia; Arias-Merino, Elva D; Pacheco-Moisés, Fermín P; Macías-Islas, Miguel A

    2014-01-01

    Background. Dementia affects memory, thinking, language, judgment, and behavior. Depression, is common in older adults with dementia. The concomitance of dementia and depression increases disability with impaired activities of daily living (ADL), increasing the chances of institutionalization and mortality. Methods. Cross-sectional study of a population 60 years and older who live in the State of Jalisco, Mexico. A total of 1142 persons were assessed regarding their cognitive function, emotional state, and physical performance. Door-to-door interview technique was assigned in condition with multistage probability random sampling. Cognitive function, depression and functional disability were assessed by applying standardized Minimental State Examination (Folstein), Geriatric Depression Scale, and the Katz index, respectively. Diagnosis of dementia was performed according to the criteria of the Diagnostic and Statistical Manual of Mental Disorders, the Fourth Edition. Data were analyzed using SPSS software. Results. Prevalence of demency was 9.5% (63.35% women, and 36.7% men). Demency was associated with being woman, being older than 70 years, low level of education, not having the economic benefit of retirement, being single or living without a partner, low level of education, suffering from depression and have functional disability in ADL. Conclusion. Dementia is more common in women and is related to depression and disability.

  4. Prevalence of Dementia, Emotional State and Physical Performance among Older Adults in the Metropolitan Area of Guadalajara, Jalisco, Mexico

    Directory of Open Access Journals (Sweden)

    Irma E. Velázquez-Brizuela

    2014-01-01

    Full Text Available Background. Dementia affects memory, thinking, language, judgment, and behavior. Depression, is common in older adults with dementia. The concomitance of dementia and depression increases disability with impaired activities of daily living (ADL, increasing the chances of institutionalization and mortality. Methods. Cross-sectional study of a population 60 years and older who live in the State of Jalisco, Mexico. A total of 1142 persons were assessed regarding their cognitive function, emotional state, and physical performance. Door-to-door interview technique was assigned in condition with multistage probability random sampling. Cognitive function, depression and functional disability were assessed by applying standardized Minimental State Examination (Folstein, Geriatric Depression Scale, and the Katz index, respectively. Diagnosis of dementia was performed according to the criteria of the Diagnostic and Statistical Manual of Mental Disorders, the Fourth Edition. Data were analyzed using SPSS software. Results. Prevalence of demency was 9.5% (63.35% women, and 36.7% men. Demency was associated with being woman, being older than 70 years, low level of education, not having the economic benefit of retirement, being single or living without a partner, low level of education, suffering from depression and have functional disability in ADL. Conclusion. Dementia is more common in women and is related to depression and disability.

  5. [Physical activity, sedentary behavior and quality of life in undergraduate adolescents of Ciudad Guzman, State of Jalisco, Mexico].

    Science.gov (United States)

    Hidalgo-Rasmussen, Carlos Alejandro; Ramírez-López, Guadalupe; Hidalgo-San Martín, Alfredo

    2013-07-01

    With the aim of evaluating the association between physical activity and sedentary behavior with quality of life (QoL) in undergraduate students of Ciudad Guzman, state of Jalisco, Mexico, a total of 881 adolescents aged between 17 and 19 were studied. Online questionnaires were used, namely the research version of the Youth Quality of Life Instrument and the Youth Risk Behavior Survey. Odd ratios (OR) were obtained using simple and multivariate logistic regression analysis. The number of days with physical activity was related to a higher total perceptual score, higher general QoL domain, higher self domain as well as higher environment domain. Playing in > 2 sports teams was related to a higher total perceptual score, higher general QoL domain, higher self domain as well as higher environment domain. Having 4-5 physical education classes/week was related with a higher general QoL domain. Limiting recreational screen time to < 2 hours/day was related with a higher relationship domain. In conclusion, in Mexican undergraduate adolescent students, higher QoL was associated with: physical activity at least 4 days/week; physical education classes 4 or more days/week; playing in 2 or more sports teams and limiting recreational screen time to 2 hours or less.

  6. Analysis of the 2003-2005 Eruptive Process of Colima Volcano, Mexico, using Seismic Signals

    Science.gov (United States)

    Nunez-Cornu, F. J.; Vargas-Bracamontes, D. M.; Suarez-Plascencia, C.; Sanchez, J. J.

    2006-12-01

    The current eruptive process of Colima Volcano, which began in August 1998, has presented several intermittent effusive and explosive phases. During the period this study comprises (2003-2005), a sequence of explosive events with VEI less than or equal to 3 occurred. Many of the explosive events were recorded by the digital three-component seismic stations operated by the University of Guadalajara and Jalisco Civil Defense. These signals were recorded not only by stations located on the volcanic edifice, but also by stations on the northern coast of Jalisco and Ceboruco Volcano at 184, 182 and 200 km distance, respectively. A study of these signals is presented. Each explosion was preceded by a seismic event. Nevertheless, the localized explosions did not show a common source under the volcano structure, which suggests the existence of a complex structure with more than one conduit. On the other hand, using the waveforms, spectra, time-frequency and time-scale (wavelets) representations of the seismic signals it is suggested that the source processes are non-stationary, implying that for the case of this period, a general model of the source process of the Colima volcano explosions can not be formulated. By means of seismic record sections it was determined that the sound velocities of the shock waves vary 10 per cent around the volcano. A clear relation between the magnitude of the seismic signals and the amplitude of the sonic and subsonic waves was not observed.

  7. Temperature field distribution from cooling of a magma chamber in La Primavera Caldera, Jalisco, Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Verma, S.P. [Laboratorio de Energia Solar, Temixco, UNAM (Mexico); Rodriguez-Gonzalez, U. [Facultad de Ciencias de la Tierra, Linares, UANL (Mexico)

    1997-02-01

    The temperature field distribution in La Primavera geothermal area, Jalisco, located in the western part of the Mexican Volcanic Belt (MVB), has been simulated from cooling of a shallow magma chamber (assumed as the primary heat source) during the entire volcanic history of the caldera. Similar to the other two geothermal fields of the MVB (Los Humeros and Los Azufres), it is considered that the evolution of the magma chamber is controlled by the processes of fractional crystallization as well as magma recharge. Besides these processes, heat contribution is also taken into account from decay of natural radioactive elements, U, Th, and K, present in all geological materials. In some models presented in this work, convection in the geothermal reservoir is simulated by assigning higher values of thermal conductivities (up to 20 times the rock conductivities) to respective geologic units. The heat transfer equation has been solved by a finite element implicit method. The results of temperature simulations from the magma chamber are compared with undisturbed formation temperatures in three drill wells. (author)

  8. The effects of volcanoes on health: preparedness in Mexico.

    Science.gov (United States)

    Zeballos, J L; Meli, R; Vilchis, A; Barrios, L

    1996-01-01

    The article reviews the most important aspects of volcanic eruptions and presents a summary of the harmful materials they emit. The main health effects can be classified as either physical (trauma, respiratory diseases, etc.) or psychological (depression, anxiety, nightmares, neurosis, etc.). Popocatépetl, the most famous active volcano in Mexico, lies on the borders of the States of Mexico, Puebla and Morelos. In 1993, seismic activity intensified, as did as the emission of fumaroles, followed in December 1994 by moderate tremors and strong emissions of gases and ash. In 1996, a number of seismic events led to an unexpected explosion. A daily emission of 8,000 to 15,000 tonnes of sulfur dioxide has been measured. Popocatépetl is located in a densely populated region of Mexico. A complex network to monitor the volcano using sophisticated equipment has been set up, including visual surveillance, seismic, geochemical and geodesic monitoring. An early warning system (SINAPROC/CENAPRED) has been developed to keep the population permanently informed. The warning system uses colour codes: green for normal, yellow for alert, and red for warning and evacuation. An emergency plan has been prepared, including evacuation and preparation for medical centres and hospitals in the region, as well as intense public information campaigns.

  9. Subsistence fisheries in the Sierra Manantlán Biosphere Reserve (Jalisco/Colima, Mexico

    Directory of Open Access Journals (Sweden)

    Norman Mercado-Silva

    2011-01-01

    Full Text Available Las reservas de la biósfera enfrentan el doble objetivo de proteger ecosistemas ejemplares y proveer a las comunidades locales con oportunidades de desarrollo. Las pesquerías de subsistencia están presentes en muchas áreas protegidas en México, pero son poco conocidas. Los pescadores de subsistencia tienen pocas oportunidades para expresar sus opiniones acerca de la calidad de los ecosistemas de los cuales dependen para sobrevivir. Utilizamos encuestas para describir las pesquerías de subsistencia del Río Ayuquila, (Jalisco, Colima, México y documentar las perspectivas que los pescadores tienen de la calidad ambiental del río y el manejo que se le da al mismo. La pesquería de subsistencia en el Ayuquila tiene gran importancia para las comunidades rurales de la Reserva de la Biósfera Sierra de Manantlán, pero está poco organizada, y es secundaria en importancia a actividades agropecuarias en la región. La pesquería ha sido afectada por la contaminación y la sobreexplotación, pero esfuerzos realizados por la dirección de la reserva y los gobiernos locales han resultado en mejoras a lo largo del tiempo. Estas mejoras se ven reflejadas en las opiniones que los pescadores tienen acerca de la situación ambiental actual del río, y de las instituciones que se encargan de darle manejo. Describimos cómo procesos regionales han afectado al manejo que se da al río e identificamos áreas donde es posible mejorar su situación. El empoderamiento de los pescadores de subsistencia es posible a través de su participación en encuestas como las que aquí presentamos y que pueden ser utilizadas por instituciones regionales para mejorar las condiciones de vida de los pobladores y las estrategias de conservación de recursos naturales.

  10. Empirical evaluation of confidence and prediction intervals for spatial models of forest structure in Jalisco, Mexico

    Institute of Scientific and Technical Information of China (English)

    Robin M. Reich; C. Aguirre-Bravo; Vanessa A. Bravo; Martin Mendoza Brise(n)o

    2011-01-01

    In recent years there has been an increasing interest in developing spatial statistical models for data sets that are seemingly spatially independent.This lack of spatial structure makes it difficult, if not impossible to use optimal predictors such as ordinary kriging for modeling the spatial variability in the data.In many instances, the data still contain a wealth of information that could be used to gain flexibility and precision in estimation.In this paper we propose using a combination of regression analysis to describe the large-scale spatial variability in a set of survey data and a tree-based stratification design to enhance the estimation process of the small-scale spatial variability.With this approach,sample units (i.e., pixel of a satellite image) are classified with respect to predictions of error attributes into homogeneous classes, and the classes are then used as strata in the stratified analysis.Independent variables used as a basis of stratification included terrain data and satellite imagery.A decision rule was used to identify a tree size that minimized the error in estimating the variance of the mean response and prediction uncertainties at new spatial locations.This approach was applied to a set of n=937 forested plots from a state-wide inventory conducted in 2006 in the Mexican State of Jalisco.The final models accounted for 62% to 82% of the variability observed in canopy closure (%), basal area (m2·ha-l), cubic volumes (m3·ha-1) and biomass (t·ha-1) on the sample plots.The spatial models provided unbiased estimates and when averaged over all sample units in the population, estimates of forest structure were very close to those obtained using classical estimates based on the sampling strategy used in the state-wide inventory.The spatial models also provided unbiased estimates of model variances leading to confidence and prediction coverage rates close to the 0.95 nominal rate.

  11. A reconnaissance geochemical study of La Primavera geothermal area, Jalisco, Mexico

    Science.gov (United States)

    Mahood, Gail A.; Truesdell, Alfred H.; Templos M, Luis A.

    1983-05-01

    The Sierra La Primavera, a late Pleistocene rhyolitic caldera complex in Jalisco, México, contains fumaroles and large-discharge 65°C hot springs that are associated with faults related to caldera collapse and to later magma insurgence. The nearly-neutral, sodium bicarbonate, hot springs occur at low elevations at the margins of the complex, whereas the water-rich fumaroles are high and central. The Comisión Federal de Electricidad de México (CFE) has recently drilled two deep holes at the center of the Sierra (PR-1 and Pr-2) and one deep hole at the western margin. Temperatures as high as 285°C were encountered at 1160 m in PR-1, which produced fluids with 820 to 865 mg/kg chloride after flashing to one atmosphere. Nearby, PR-2 encountered temperatures to 307°C at 2000 m and yielded fluids with chloride contents fluctuating between 1100 and 1560 mg/kg after flashing. Neither of the high-temperature wells produced steam in commercial quantities. The well at the western margin of the Sierra produced fluids similar to those from the hot springs. The temperature reached a maximum of 100°C near the surface and decreased to 80°C at 2000 m. Various geothermometers (quartz conductive, Na/K, Na-K-Ca, δ 18O(SO 4-H 2O) and D/H (steam-water) all yield temperatures of 170 ± 20° C when applied to the hot spring waters, suggesting that these spring waters flow from a large shallow reservoir at this temperature. Because the hot springs are much less saline than the fluids recovered in PR-1 and PR-2, the mixed fluid in the shallow reservoir can contain no more than 10-20% deep fluid. This requires that most of the heat is transferred by steam. There is probably a thin vapor-dominated zone in the central part of the Sierra, through which steam and gases are transferred to the overlying shallow reservoir. Fluids from this reservoir cool from ˜170°C to 65°C by conduction during the 5-7 km of lateral flow to the hot springs.

  12. Los equinodermos (Echinodermata de bahía Chamela, Jalisco, México The echinoderms (Echinodermata from bahía Chamela, Jalisco, Mexico

    Directory of Open Access Journals (Sweden)

    Eduardo Ríos-Jara

    2013-03-01

    Full Text Available Cuarenta especies de equinodermos fueron recolectadas en las zonas intermareal y submareal somero de 14 sitios de bahía Chamela. Destacan 7 nuevos registros para la costa de Jalisco. Los análisis de escalonamiento multidimensional no métrico y el índice de similitud de Jaccard permitieron identificar grupos y entidades aisladas de acuerdo a la contribución y frecuencia de las especies de 4 clases de equinodermos en los sitios de la bahía y en otras localidades del Pacífico tropical mexicano (PTM. La mayor similitud se presentó con las localidades del golfo de California. Los índices de distinción taxonómica promedio (Δ+ y su variación (Λ+ fueron utilizados para analizar la diversidad de equinodermos en los niveles de especie, género, familia, orden y clase para cada sitio de la bahía y para distintas localidades del PTM de acuerdo al número de jerarquías taxonómicas de alto orden y la variabilidad en su diversidad taxonómica. La riqueza de especies de Chamela representa el 20% de la diversidad total de equinodermos de las zonas intermareal y submareal somero del PTM, lo que indica su importancia en la contribución a la diversidad taxonómica de la región.Forty species of echinoderms were collected in the intertidal and shallow subtidal zones of 14 sites of bahía Chamela. Of particular importance are 7 new records of species for the coast of Jalisco. A nonmetric multidimensional scaling analysis and the Jaccard's similarity index identified different groups and isolated entities according to the contribution and the frequency of species of 4 classes of echinoderms in the bay and in other localities of the Mexican Tropical Pacific (MTP. The highest similarity of species was with the localities of the Gulf of California. The indices of average taxonomic distinctness (Δ+ and the variation in the taxonomic distinctness (Λ+ were estimated to analyze the diversity of echinoderms at the taxonomic levels of species, genus, family

  13. Development of the Health Atlas of Jalisco: A New Web-Based Service for the Ministry of Health and the Community in Mexico

    Science.gov (United States)

    Robles, Juan; Fonseca León, Joel

    2016-01-01

    Background Maps have been widely used to provide a visual representation of information of a geographic area. Health atlases are collections of maps related to conditions, infrastructure or services provided. Various countries have put resources towards producing health atlases that support health decision makers to enhance their services to the communities. Latin America, as well as Spain, have produced several atlases of importance such as the interactive mortality atlas of Andalucía, which is very similar to the one that is presented in this paper. In Mexico, the National Institute of Public Health produced the only health atlas found that is of relevance. It was published online in 2003 and is currently still active. Objective The objective of this work is to describe the methods used to develop the Health Atlas of Jalisco (HAJ), and show its characteristics and how it interactively works with the user as a Web-based service. Methods This work has an ecological design in which the analysis units are the 125 municipalities (counties) of the state of Jalisco, Mexico. We created and published online a geographic health atlas displaying a system based on input from official health database of the Health Ministry of Jalisco (HMJ), and some databases from the National Institute of Statistics and Geography (NISGI). The atlas displays 256 different variables as health-direct or health-related indicators. Instant Atlas software was used to generate the online application. The atlas was developed using these procedures: (1) datasheet processing and base maps generation, (2) software arrangements, and (3) website creation. Results The HAJ is a Web-based service that allows users to interact with health and general data, regions, and categories according to their information needs and generates thematic maps (eg, the total population of the state or of a single municipality grouped by age or sex). The atlas is capable of displaying more than 32,000 different maps by

  14. Petrology of Volcán Tequila, Jalisco, Mexico: disequilibrium phenocryst assemblages and evolution of the subvolcanic magma system

    Science.gov (United States)

    Wallace, Paul J.; Carmichael, Ian S. E.

    1994-09-01

    Volcán Tequila is an extinct stratovolcano in the western Mexican Volcanic Belt that has erupted lavas ranging from andesite to rhyolite during the last 0.9 Ma. Following an early period of rhyolitic volcanism, the main edifice of the volcano was constructed by central vent eruptions that produced ˜ 25 km3 of pyroxene-andesite. At about 0.2 Ma central activity ceased and numerous flows of hornblende-bearing andesite, dacite, and rhyodacite erupted from vents located around the flanks of the volcano. Bimodal plagioclase phenocryst rim compositions in lavas from both the main edifice and the flanks indicate that magma mixing commonly occurred shortly prior to or during eruption. Compositions of endmember magmas involved in mixing, as constrained by whole-rock major and trace element abundances, phenocryst compositions, and mineral-melt exchange equilibria, are similar to those of some lavas erupted from the central vent and on the flanks of the volcano. Estimated pre-eruptive temperatures for hornblende-bearing lavas (970° 830°C) are systematically lower than for lavas that lack hornblende (1045° 970°C), whereas magmatic H2O contents are systematically higher for hornblende-bearing lavas. In addition to stabilizing hornblende, high magmatic water contents promoted crystallization of calcic plagioclase (An70 82). Frequent injections of magma into the base of the subvolcanic plumbing system followed by eruption of mixed magma probably prevented formation of large volumes of silicic magma, which have caused paroxysmal, caldera-forming eruptions at other stratovolcanoes in western Mexico. The later stages of volcanic activity, represented by the flank lavas, indicate a change from a large magma storage reservoir to numerous small ones that developed along a NW-trending zone parallel to regional fault trends. Sr and Nd isotopic data for lavas from the Tequila region and other volcanoes in western Mexico demonstrate that differentiated calc-alkaline magmas are formed

  15. Registro del águila elegante (Spizaetus ornatus en la Reserva de la Biosfera sierra de Manantlán, Jalisco-Colima, México A new record for the Ornate Hawk-Eagle (Spizaetus ornatus in the Sierra Manantlán Biosphere Reserve, Jalisco-Colima, Mexico

    Directory of Open Access Journals (Sweden)

    Marcelo Aranda

    2009-04-01

    Full Text Available Se presenta un registro del águila elegante (Spizaetus ornatus en un bosque de encino-pino de la Reserva de la Biosfera Sierra de Manantlán, Jalisco-Colima, correspondiente a un individuo de 2 a 3 años de edad. Este registro es significativo ante la escasez de registros de esta especie en el occidente de México, los cuales corresponden a localidades en los estados de Nayarit (1 Colima (3, Jalisco (1 y Guerrero (1. Se considera que el águila elegante está en peligro de extinción en México (NOM-059-ECOL-2001; su presencia en esta área natural protegida da aliento para su conservación.An immature Ornate Hawk-Eagle (Spizaetus ornatus was observed and photographed while perched in pine-oak forest in the Sierra de Manantlán Biosphere Reserve, Jalisco-Colima, Mexico. From plumage characteristics we believe the eagle to be 2-3 years old. This record is significant due to the paucity of records for this species in Western Mexico: Nayarit (1 Colima (3, Jalisco (1 and Guerrero (1. The Ornate Hawk-Eagle is considered as a threatened species in Mexico, and this record from a natural protected area brings hope for its conservation.

  16. Mujeres violentadas durante el embarazo y el parto: experiencias de parteras en Jalisco, México / Women abused during pregnancy and childbirth: experiences and views of midwives from Jalisco, Mexico

    Directory of Open Access Journals (Sweden)

    Martha Villaseñor F

    2014-05-01

    Full Text Available Objetivo: explorar la experiencia y perspectiva de parteras con mujeres violentadas durante el embarazo y el parto en Jalisco, México. Metodología: se llevó a cabo un estudio cualitativo en zona rural de Jalisco, México, entre mayo y octubre de 2011 con 24 parteras, utilizando la entrevista individual, modalidad historia de vida pautada y la asamblea participativa regional como técnicas de indagación; posteriormente, los discursos fueron analizados bajo el modelo actancial semiótico. Resultados: familiaridad de las parteras con la violencia hacia la mujer durante el embarazo y el parto, atribuida principalmente a aspectos de género y ruralidad; señalan al binomio violencia-embarazo como factor de riesgo para presentar problemas obstétricos, siendo la violencia física la que más encuentran y a la pareja como principal agresor. Resalta su capacidad de diálogo y escucha activa en identificación de violencia. Refieren posibilidad de ser escuchadas en la generación de acciones frente a este problema. Discusión: necesidad de asumir una postura política estatal sobre la partería, que permita reconocer su papel en la sociedad y la posibilidad de incorporarlas en las acciones que hacen frente al problema de la violencia, y valorar los elementos propios de su ejercicio en la detección y manejo de estas mujeres. Objetive: to explore the experiences and perspectives that a group of midwives from Jalisco, Mexico had with women who were abused during pregnancy and delivery. Methodology: a qualitative study was conducted in a rural zone of Jalisco, Mexico, between May and October 2011 with 24 midwives. The techniques used to obtain the data were: individual interviews, life history, and the participatory regional assembly. After collecting the discourses, these were analyzed using the semiotic actantial model. Results: the midwives are familiar with the violence exercised against women during the pregnancy and birth process; this is mainly

  17. Subsistence fisheries in the Sierra Manantlán Biosphere Reserve (Jalisco/Colima, Mexico)

    OpenAIRE

    Norman Mercado-Silva; Eduardo Santana-Castellón; Luis Manuel Martínez Rivera; John Lyons; Timothy Moermond

    2011-01-01

    Biosphere reserves are charged with the challenging dual objectives of protecting exemplary ecosystems and providing local communities with opportunities for development. Small-scale, subsistence fisheries occur in many protected areas in Mexico, but little is known about their characteristics. Additionally, subsistence fishermen rarely have the possibility to express their opinions on the quality of the ecosystems they depend on for survival. We used surveys to describe the Ayuquila River (J...

  18. Large early afterslip following the 1995/10/09 Mw 8 Jalisco, Mexico earthquake

    Science.gov (United States)

    Hjörleifsdóttir, Vala; Sánchez Reyes, Hugo Samuel; Ruiz-Angulo, Angel; Ramirez-Herrera, Maria Teresa; Castillo-Aja, Rosío; Krishna Singh, Shri; Ji, Chen

    2017-04-01

    The behaviour of slip close to the trench during earthquakes is not well understood, with some earthquakes breaking only the near trench area, most earthquakes breaking only the deeper part of the fault interface, whereas a few break both simultaneously. Observations of multiple earthquakes breaking different down dip segments of the same subduction segment are rare. The 1995 Mw 8 Jalisco earthquake, seems to have broken the near trench area, as evidenced by anomalously small accelerations for its size, the excitation of a tsunami, a small Ms relative to Mw and a small ratio between the radiated energy and moment (Pacheco et al 1997). However, slip models obtained using GPS campaign data, indicate slip near shore (Melbourne et al 1997, Hutton et al 2001). We invert tele seismic P- and S-waves, Rayleigh and Love waves, as well as the static offsets measured by campaign GPS models, to obtain the slip distribution on the fault as a function of time, during the earthquake. We confirm that the slip models obtained using only seismic data are most consistent with slip near the trench, whereas those obtained using only GPS data are consistent with slip closer to the coast. We find remarkable similarity with models of other researchers (Hutton et al 2001, Mendoza et al 1999) using the same datasets, even though the slip distributions from each dataset are almost complementary. To resolve this inconsistency we jointly invert the datasets. However, we find that the joint inversions do not produce adequate fits to both seismic and GPS data. Furthermore, we model tsunami observations on the coast, to constrain further the plausible slip models. Assuming that the discrepancy stems from slip that occurred within the time window between the campaign GPS measurements, but not during the earthquake, we model the residual displacements by very localised slip on the interface down dip from the coseismic slip. Aftershocks (Pacheco et al 1997) align on mostly between the non

  19. New Hypocenter Relocation Results From Volcano-Tectonic Events (1995-2006) at Popocatepetl Volcano, Mexico

    Science.gov (United States)

    Berger, P.; Nava, F. A.; Valdes-Gonzalez, C.

    2008-12-01

    Popocatepetl, one of the most active strato-volcanoes in Mexico, started a fumarolic and seismic reactivation in December 1994. New hypocenter relocation results have been calculated for some 1,800 volcano-tectonic (VT) events recorded by the seismic network operating at Popocatepetl during 1995-2006, and previously located by the National Center for Disasters Prevention (CENAPRED). We used two location programs to determine hypocenter relocation. One is a recently developed genetic algorithm program, Disloca, which adjusts the differences in arrival times between the recording seismic stations. The second is HypoDD, which uses the double difference earthquake location algorithm. Disloca allowed evaluation of station corrections, plus location of non-clustered hypocenters, while HypoDD refined the locations of clustered ones. Thus, for a given velocity model, hypocenters of clustered events varied slightly depending on the location program. For both programs, four different crustal velocity models were used, two of which include a low velocity zone (LVZ) below 6 km depth. This LVZ represents the presence of magma, which has been suggested to exist at this depth. The spatial distribution of the relocated hypocenters varies from one model to another, but a carefully considered combination of features common to the four distributions, allows a new characterization of the VT activity at Popocatepetl. The distribution of the relocated hypocenters found in this study differs from that of former investigations at Popocatépetl, and gives new insights into the volcano's structures. Hypocenters occur mainly above 10 km depth, with a horizontal range of about 5 km. Features of the spatial distribution allow a tentative interpretation of several internal volcanic structures. Chief among these are branched dike complexes and different sized zones free of volcano-tectonic events, which are in turn surrounded by zones of magma-rock interaction, as indicated by the presence of

  20. Screening for kidney disease in children on World Kidney Day in Jalisco, Mexico.

    Science.gov (United States)

    Koshy, Susan M; Garcia-Garcia, Guillermo; Pamplona, Jacob Sandoval; Renoirte-Lopez, Karina; Perez-Cortes, Gustavo; Gutierrez, Ma Luisa Salazar; Hemmelgarn, Brenda; Lloyd, Anita; Tonelli, Marcello

    2009-06-01

    World Kidney Day (WKD) is intended to raise awareness and increase detection of chronic kidney disease (CKD), but most emphasis is placed on adults rather than children. We examined yield of screening for CKD and hypertension among poor children in Mexico. On WKD (2006, 2007), children (age or= 1+ protein or blood on dipstick. Hypertension was defined by gender, age, and height-specific norms. In total, 240 children were screened (mean age 8.9 +/- 4.1 years; 44.2% male). Proteinuria and hematuria were detected in 38 (16.1%) and 41 (17.5%), respectively; 15% had BMI > 95th percentile for age. Reduced GFR was detected in four (1.7%) individuals. Systolic hypertension was more prevalent in younger children (age 0-8 years, 19.6%; age 9-13 years, 7.1%; age 14-17 years, 5.3%) suggesting a possible white-coat effect. Hematuria, proteinuria, hypertension and obesity were frequently detected among children in a community based screening program in Mexico. This form of screening might be useful in identifying children with CKD and hypertension in developing nations.

  1. 墨西哥哈里斯科(Jalisco)林分结构小面积估测%Small-area estimation of forest stand structure in Jalisco, Mexico

    Institute of Scientific and Technical Information of China (English)

    Robin M.Reich; Celedonio Aguirre-Bravo

    2009-01-01

    对小的生态经济区开展自然资源统计是很困难的,政府决策人员只能依靠州水平的数据库来评价一定区域或局部的自然资源(森林、牧场、草地、农田等)状况.小面积评估技术可以用于评定这些资源.然而,哪一种小面积估测法可以给出最可靠、最准确的结果还不得而知.本研究检测了小面积评估分析常用的两种方法(即综合估计法和回归估计法)的可靠性、准确性.运用这两种方法分析墨西哥哈里斯科(Jalisco)州全州的自然资源数据,从而检测每种方法对所选择的森林林分结构特征预测结果的好坏.研究表明,回归方法在多个地理尺度上,对森林林分结构特征预测的可靠性和准确性均最好.因此,推荐州或地方资源管理者,在没有其他适当的辅助信息资料的情况下,可运用回归分析法来评估小区域内自然资源状况.

  2. Update of the volcanic risk map of Colima volcano, Mexico

    Science.gov (United States)

    Suarez-Plascencia, C.; Nuñez Cornu, F. J.; Marquez-Azua, B.

    2010-12-01

    The Colima volcano, located in western Mexico (19° 30.696 N, 103° 37.026 W) began its current eruptive process in February 10, 1999. This event was the basis for the development of two volcanic hazard maps: one for ballistics (rock fall) lahars, and another one for ash fall. During the period of 2003 to 2008 this volcano has had an intense effusive-explosive activity, similar to the one that took place during the period of 1890 through 1900. Intense pre-Plinian eruption in January 20, 1913, generated little economic losses in the lower parts of the volcano thanks to the low population density and low socio-economic activities at the time The current volcanic activity has triggered ballistic projections, pyroclastic and ash flows, and lahars, all have exceeded the maps limits established in 1999. Vulnerable elements within these areas have gradually changed due to the expansion of the agricultural frontier on the east and southeast sides of the Colima volcano. On the slopes of the northwest side, new blue agave Tequilana weber and avocado orchard crops have emerged along with important production of greenhouse tomato, alfalfa and fruit (citrus) crops that will eventually be processed and dried for exportation to the United States and Europe. Also, in addition to the above, large expanses of corn and sugar cane have been planted on the slopes of the volcano since the nineteenth century. The increased agricultural activity has had a direct impact in the reduction of the available forest land area. Coinciding with this increased activity, the 0.8% growth population during the period of 2000 - 2005, - due to the construction of the Guadalajara-Colima highway-, also increased this impact. The growth in vulnerability changed the level of risk with respect to the one identified in the year 1999 (Suarez, 2000), thus motivating us to perform an update to the risk map at 1:25,000 using vector models of the INEGI, SPOT images of different dates, and fieldwork done in order

  3. Diversidad de Agaricomycetes clavarioides en la Estación de Biología de Chamela, Jalisco, México Diversity of clavarioid Agaricomycetes at the Chamela Biological Station, Jalisco, Mexico

    Directory of Open Access Journals (Sweden)

    Itzel Ramírez-López

    2012-12-01

    Full Text Available Este estudio es una contribución al conocimiento de la diversidad y estructura de los Agaricomycetes clavarioides que se desarrollan en los bosques tropicales de la Estación de Biología de Chamela, Jalisco, México. Las recolecciones se realizaron durante la temporada de lluvias de los años 2005 a 2008; se registraron datos de hábitat y morfología de los basidiomas, tipo de vegetación y sustrato donde se desarrollan, así como del patrón de crecimiento, área de distribución, abundancia y orientación e inclinación de las laderas donde se localizaron. Los 86 ejemplares registrados corresponden a 17 especies, de las cuales Physalacria changensis, P. inflata, Pterula verticillata y Scytinopogon scaber son nuevos registros para México. Scytinopogon pallescens, Pterula sp. 2 y Thelephora sp. fueron las más abundantes y 6 especies se registraron sólo 1 vez. Los datos obtenidos indican que la frecuencia con la que se hallan los basidiomas de los clavarioides en los distintos hábitats no es aleatoria, sino que su producción se da preferentemente en las laderas sur con inclinación de 21° a 30° y en el bosque tropical subperennifolio.This study is a contribution to the biodiversity and community structure of clavarioid Agaricomycetes in the tropical forests of the Chamela Biological Station, in Jalisco, Mexico. The collections were made during the rainy seasons from 2005 to 2008 during which we recorded the morphological and ecological information, including basidiocarp morphology and patterns of growth. Likewise, records were also taken for habitat preferences, types of substrate, orientation, slope inclination, range of distribution and abundance. The 86 specimens recorded, corresponded to 17 different species, from which Physalacria changensis, P. inflata, Pterula verticillata and Scytinopogon scaber are new records for Mexico. The species S. pallescens, Pterula sp. 2 and Thelephora sp. were the most abundant, while other 6 species

  4. Interpretación de índices antropométricos en niños de Arandas, Jalisco, México Interpretation of anthropometric indices in children of Arandas, Jalisco, Mexico

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    Edgar Manuel Vásquez-Garibay

    2002-04-01

    Full Text Available Objetivo. Valorar el estado de nutrición de niños que asisten al Instituto Alteño para el Desarrollo de Jalisco en Arandas, Jalisco, y discutir los criterios de clasificación de la desnutrición en México. Material y métodos. Estudio transversal, desarrollado con 775 niños de 12 a 120 meses de edad y que asisten al Instituto Alteño para el Desarrollo de Jalisco (Inadej y 432 encuestas a niños de nuevo ingreso al Inadej. Se calcularon los índices peso/edad, talla/edad y peso/talla, y se investigaron características sociodemográficas y económicas y hábitos de alimentación; asimismo se compararon los criterios de la Organización Mundial de la Salud (OMS y de la Norma Oficial Mexicana (NOM-SSA para definir la prevalencia de desnutrición. Resultados. Hubo baja escolaridad en ambos padres (3.6 años. El ingreso familiar fue de $198 dólares mensuales y cada miembro recibió 0.56 dólar/día para las tres comidas. La prevalencia de desnutrición fue mayor en los tres índices con el uso de la NOM-SSA que con el criterio de la OMS (peso/edad 91.7 vs. 30.9%; talla/edad 66.9 vs. 17.3%; peso/talla 62.5 vs. 9.5% respectivamente. Conclusiones. El índice peso/edad y la NOM SSA sobrestiman la prevalencia de desnutrición y no discriminan entre niños genéticamente pequeños, con desnutrición aguda o desnutrición crónica o pasada. Es más útil el criterio de la OMS. Se deben incluir los índices peso/talla (desnutrición reciente y talla/edad (desnutrición crónica para comparación internacional.Objective. To assess the nutritional status of children attending the Instituto Alteño para el Desarrollo de Jalisco (Highlands Institute for Development of Jalisco State, Inadej in Arandas, Jalisco and to discuss the classification criteria of infant malnutrition in Mexico. Material and Methods. A cross-sectional study was conducted in 775 children aged between twelve and one hundred and twenty months, who attended Inadej, including 432

  5. Generation and evolution of internal waves in Banderas Bay, Jalisco-Nayarit, Mexico.

    Science.gov (United States)

    Plata, L. J.; Anatoliy, F.; Iryna, T.; Carlos, V.; Liza, K.; César, M.

    2007-05-01

    The characteristics of internal waves in Banderas Bay (Mexico) were determined by means of data from oceanographical measurements carried on spring and winter during the years 2001 and 2003. The intense fluctuations in the fields of temperature and salinity obtained from a fast oceanographical survey with an undulating CTD on April, 2001, give evidence of the presence and propagation of an internal waves' field. With the help of a bathymetric chart elaborated from a survey carried on in March and May, 2002, we found that the submarine canyon close to the southern coast of the bay, from Cabo Corrientes to Mismaloya, acts like a filter that reflects the diurnal internal tide and allows only the entrance of semidiurnal internal tide. The results of a special experiment measuring the spatiotemporal parameters of internal waves on the wide continental shelf of northwestern Banderas Bay are discussed. The oceanographical measurements consisted of: a) a fast survey with an undulating CTD along a transect perpendicular to the coast, (b) the towing of an array of temperature and depth sensors several times over the continental shelf along transects perpendicular to the coast, and (c) time series of velocity components registered by an acoustic Doppler current profiler placed on the seabed of the bay at 28 m depth. The presence of internal waves generated by semidiurnal tide and corresponding to the second normal oscillation mode (according to the linear theory of internal waves) was determined. Analysis of the data showed that, in the study area, the internal waves generated over the continental slope by the barotropic tide have the shape of an oscillatory bore, which quickly disintegrates during their propagation shoreward, producing short nonlinear waves that dissipate close to the coast, and intense vertical mixing of the whole water column. The interpretation of the results was based on the linear and nonlinear (Korteweg-de Vries equation) theories of internal waves.

  6. A summary of the geology and petrology of the Sierra La Primavera, Jalisco, Mexico

    Science.gov (United States)

    Mahood, Gail A.

    1981-11-01

    The Sierra La Primavera, near Guadalajara, Mexico, is a Late Pleistocene rhyolitic center consisting of lava flows and domes, ash flow tuff, air fall pumice, and caldera lake sediments. All eruptive units are high-silica rhyolites, but systematic compositional differences correlate with age and eruptive mode. The earliest lavas erupted approximately 145,000 years ago and were followed approximately 95,000 years ago by the eruption of about 20 km3 of magma as ash flows that form the Tala Tuff. The Tala Tuff is zoned from a mildly peralkaline first-erupted portion enriched in Na, Rb, Cs, Cl, F, Zn, Y, Zr, Nb, Sb, HREE, Hf, Ta, Pb, Th, and U to a metaluminous last-erupted part enriched in K, LREE, Sc, and Ti; Al, Ca, Mg, Mn, Fe, and Eu are constant within analytical errors. Collapse of the roof zone of the magma chamber led to the formation of a shallow 11-km-diameter caldera in which lake sediments began to collect. The earliest postcaldera lava, the south-central dome, is nearly identical to the last-erupted portion of the Tala Tuff, whereas the slightly younger north-central dome is chemically transitional from the south-central dome to later, more mafic, ring domes. This sequence of ash flow tuff and domes represents the tapping of progressively deeper levels of a zoned magma chamber 95,000 ± 5,000 years ago. Sedimentation continued and a period of volcanic quiescence was marked by the deposition of some 30 m of fine-grained ashy sediments. Approximately 75,000 years ago a new group of ring domes erupted at the southern margin of the lake. These domes are lapped by only 10-20 m of sediments as uplift resulting from renewed insurgence of magma brought an end to the lake. This uplift culminated in the eruption, beginning approximately 60,000 years ago, of aphyric lavas along a southern arc. The youngest of these lavas erupted approximately 30,000 years ago. The lavas that erupted 75,000, 60,000, and 30,000 years ago became decreasingly peralkaline and progressively

  7. Salvia carreyesii, Salvia ibugana and Salvia ramirezii (Lamiaceae, three new species from Jalisco, Mexico Salvia carreyesii, Salvia ibugana y Salvia ramirezii (Lamiaceae, tres nuevas especies de Jalisco, México

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    Jesús Guadalupe González-Gallegos

    2013-03-01

    Full Text Available Three new species from Jalisco, Mexico, are described and illustrated. These species grow in tropical or in tropical and temperate transitional forests. The 3 species belong to Salvia L. subgenus Calosphace (Benth. Benth. Salvia carreyesii J. G. González is morphologically similar with section Briquetia Epling. It is characterized by the contrasting vegetative morphology between mature and immature individuals, its relatively large and sessile or sub-sessile leaves (the uppermost amplexicaul, glandular-capitate hairs on the floral axis and calyx, and dark violet corollas. The characters of Salvia ibugana J. G. González correspond to those of the species of section Angulatae (Epling Epling, within which S. ibugana is distinguished by the digitiform papillae disperse on its stems, petioles and floral axis. Salvia ramirezii J. G. González fits well within section Sigmoideae Epling by means of the sigmoid shape of the lower branch of its style. It is morphologically similar to Salvia crucis and S. quercetorum, from which it can be distinguished by the triangular, slightly succulent, shorter, glabrous, lustrous leaves.Se describen e ilustran 3 especies nuevas de Jalisco, México. Estas especies crecen en bosques tropicales o en bosques transicionales entre tropicales y templados. Las 3 especies pertenecen a Salvia L. subgénero Calosphace (Benth. Benth. Salvia carreyesii J. G. González es morfológicamente similar a la sección Briquetia Epling. Se caracteriza por la morfología vegetativa contrastante entre individuos maduros e inmaduros, sus hojas relativamente grandes, sésiles o subsésiles (las superiores amplexicaules, tricomas capitado-glandulares sobre el eje floral y el cáliz, y corolas violeta oscuro. Las características de Salvia ibugana J. G. González corresponden a aquellas de las especies de la sección Angulatae (Epling Epling, dentro de la que S. ibugana se distingue por las papilas digitiformes que presenta en el tallo

  8. Una experiencia de educación popular en salud nutricional en dos comunidades del Estado de Jalisco, México An experience with popular nutritional health education in two communities from Jalisco, Mexico

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    Isabel Valadez Figueroa

    2000-09-01

    Full Text Available Este trabajo, da cuenta de un proceso de Educación Popular, en dos comunidades del estado de Jalisco México, con el objetivo de introducir el concentrado de Alfalfa en la dieta habitual de los habitantes, como fuente alimentaria alterna, disponible en esas regiones, dado que estudios realizados han demostrado que contiene un alto nivel de proteínas, vitaminas y aminoácidos esenciales, y puede ser utilizado para complementar y mejorar la nutrición de los niños. Recurso no aprovechado por el desconocimiento relativo de sus propiedades y del procedimiento para su obtención y por utilizarse como forraje. Se trabajo en cuatro etapas: 1 conocimiento de la comunidad, 2 abordaje comunitario, 3 formación de grupos de trabajo y 4 programa educativo, con la herramienta del autodiagnóstico, en base a dos ejes temáticos: la alimentación familiar y el concentrado de alfalfa como forma de mejorarla, desarrollados simultáneamente. Se tuvo como resultados que se aceptara el concentrado de alfalfa y se conformaran grupos comunitarios, manteniéndose actualmente un tipo de organización en cada comunidad.This study describes a popular educational process conducted in two communities in Jalisco, Mexico. The purpose was to add an alfalfa concentrate to the population's diet as an alternative, locally available food source. Previous studies had shown that alfalfa contains high protein, vitamin, and essential amino acid levels and can be useful to supplement and improve child nutrition. This resource had not been used previously due to lack of knowledge concerning its properties and harvesting and processing procedures and because it had traditionally been used as livestock feed. The current study included four steps: 1 community knowledge, 2 a community survey using interviews, home visits, and child nutrition evaluation, 3 formation of work groups in a community meeting, and 4 an educational program, working with a self-diagnostic tool taking child

  9. Serological follow-up of Trypanosoma cruzi infection from 1987 to 1994 in 32 counties of the State of Jalisco, Mexico: preliminary report

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    Trujillo-Contreras Francisco

    1995-01-01

    Full Text Available In 1987 the University of Guadalajara performed a seroepidemiological survey on the prevalence of Chagas? disease in the 124 counties of the State of Jalisco, Mexico, arriving at a rate of 21.6 per 100 inhabitants. From December 1993 to June 1994, we studied 2238 individuals from 32 rural counties in this State. Of these, we found 276 positives (12.33% and 1962 negatives (87.66%. Nevertheless, the series of serological differences found are very striking, since out of the 655 individuals that were seropositive in 1987, we noted that 276 individuals remained positive, while 50 individuals (7.63% became negative. There were no flaws in the laboratory techniques. We believe that either the immune response of Mexicans is different or that the virulence of the Mexican strains of Trypanosoma cruzi may be not as great as that in the South America countries.

  10. Serological follow-up of Trypanosoma cruzi infection from 1987 to 1994 in 32 counties of the State of Jalisco, Mexico: preliminary report

    Directory of Open Access Journals (Sweden)

    Francisco Trujillo-Contreras

    1995-09-01

    Full Text Available In 1987 the University of Guadalajara performed a seroepidemiological survey on the prevalence of Chagas’ disease in the 124 counties of the State of Jalisco, Mexico, arriving at a rate of 21.6 per 100 inhabitants. From December 1993 to June 1994, we studied 2238 individuals from 32 rural counties in this State. Of these, we found 276 positives (12.33% and 1962 negatives (87.66%. Nevertheless, the series of serological differences found are very striking, since out of the 655 individuals that were seropositive in 1987, we noted that 276 individuals remained positive, while 50 individuals (7.63% became negative. There were no flaws in the laboratory techniques. We believe that either the immune response of Mexicans is different or that the virulence of the Mexican strains of Trypanosoma cruzi may be not as great as that in the South America countries.

  11. [Description of Melolonthidae (Coleoptera) third instar larvae associated to Agave tequilana var. Azul and their population fluctuation in Jalisco, Mexico].

    Science.gov (United States)

    García, Gabriel L; Ortega-Arenas, Laura; Hernández, Héctor G; García, Agustín A; Nápoles, Jesús R; Cortés, Ramón R

    2009-01-01

    Third instars of white grubs of six species associated to agave tequilero in Jalisco, México were described from 1,145 specimens collected from soil samples from September 2006 to August 2007, in the municipalities of Ixtlahuacán del Río, Tepatitlán de Morelos and San Juan de Escobedo, Jalisco, México. Diagnostic characters were illustrated and a key was also included. Cyclocephala comata (Bates) was the most abundant species (63.2%), followed by Phyllophaga ravida (Blanchard) (21.9%), Phyllophaga polyphylla (Bates) (9.4%), Phyllophaga misteca (Bates) (4.1%), Strategus aloeus (L.) (1.1%) and Anomala hoepfneri (Bates) (0.3%). Phyllophaga ravida and A. hoepfneri are reported for the first time on the agave plant and the latter is a new record for the State of Jalisco. All Melolonthidae species showed a marked seasonality with lower number of larvae in June 2007 and high number in August 2007, which is associated with the region's rainy season and the agave plant age, respectively.

  12. Seismicity of the Jalisco Block

    Science.gov (United States)

    Nunez-Cornu, F. J.; Rutz, M.; Camarena-Garcia, M.; Trejo-Gomez, E.; Reyes-Davila, G.; Suarez-Plascencia, C.

    2002-12-01

    In April 2002 began to transmit the stations of the first phase of Jalisco Telemetric Network located at the northwest of Jalisco Block and at the area of Volcan de Fuego (Colima Volcano), in June were deployed four additional MarsLite portable stations in the Bahia de Banderas area, and by the end of August one more portable station at Ceboruco Volcano. The data of these stations jointly with the data from RESCO (Colima Telemetric Network) give us the minimum seismic stations coverage to initiate in a systematic and permanent way the study of the seismicity in this very complex tectonic region. A preliminary analysis of seismicity based on the events registered by the networks using a shutter algorithm, confirms several important features proposed by microseismicity studies carried out between 1996 and 1998. A high level of seismicity inside and below of Rivera plate is observed, this fact suggest a very complex stress pattern acting on this plate. Shallow seismicity at south and east of Bahia de Banderas also suggest a complex stress pattern in this region of the Jalisco Block, events at more than 30 km depth are located under the mouth of the bay and in face of it, a feature denominated Banderas Boundary mark the change of the seismic regime at north of this latitude (20.75°N), however some shallow events were located at the region of Nayarit.

  13. Nuevos registros del parásito Probopyrus pacificensis (Isopoda: Bopyridae en el sur de Nayarit y norte de Jalisco, México New records of the parasite Probopyrus pacificensis (Isopoda: Bopyridae in southern Nayarit and northern Jalisco, Mexico

    Directory of Open Access Journals (Sweden)

    Alberto Ocaña-Luna

    2009-04-01

    Full Text Available Se presentan nuevos registros de Probopyrus pacificensis en el arroyo San Francisco, sur de Nayarit y en el arroyo Palo María, norte de Jalisco en el Pacífico mexicano, parasitando a camarones de agua dulce de la especie Macrobrachium tenellum.New observations of Probopyrus pacificensis were recorded in Arroyo San Francisco, southern Nayarit, and Arroyo Palo María, northern Jalisco, in the Mexican Pacific, infesting the freshwater shrimp Macrobrachium tenellum.

  14. Cuidados alternativos en la atención del embarazo en Jalisco, México Alternative care options for pregnancy in Jalisco, Mexico

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    Isabel Valadez

    2003-10-01

    delivery acted as a protective factor. The culture of pregnant woman in Mexico comprises meaning and behaviors that mix concepts and prescriptive ideas concerning domestic, traditional, and academic medicine, varying according to the stage of pregnancy, and which may be used in exclusive or complementary fashion. This situation should be considered in health education programs.

  15. Salvia meera, S. rogersiana, S. santanae and S. concolor var. iltisii (Lamiaceae, three new species and a variety from Jalisco, Mexico Salvia meera, S. rogersiana, S. santanae y S. concolor var. iltisii (Lamiaceae, tres especies nuevas y una variedad de Jalisco, México

    Directory of Open Access Journals (Sweden)

    Jesús Guadalupe González-Gallegos

    2012-09-01

    Full Text Available As part of a major project on the genus Salvia in the state of Jalisco and adjacent areas, Mexico, 4 new taxa of Salvia L. are described and illustrated. Identification Keys for the related species and comparison tables of morphological characters are given. Three of them were tentatively proposed -but not formally published- as new species in the book Flora de Manantlán.Como parte de un proyecto mayor del género Salvia en el estado de Jalisco y áreas colindantes, México, se describen e ilustran 4 nuevos taxa. Se proveen claves de determinación para las especies relacionadas y tablas comparativas de caracteres morfológicos. Tres de ellos fueron tentativamente propuestos -pero no formalmente publicados- como nuevas especies en el libro de Flora de Manantlán.

  16. Radon, water chemistry and pollution check by volatile organic compounds in springs around Popocatepetl volcano, Mexico

    OpenAIRE

    Mena, M.; Cisniega, G.; Lopez, B.; M. A. Armienta; Valdés, C; Peña, P.; N. Segovia

    2005-01-01

    Popocatepetl volcano is a high-risk active volcano in Central Mexico where the highest population density in the country is settled. Radon in the soil and groundwater together with water chemistry from samples of nearby springs were analysed as a function of the 2002-2003 volcanic activity. The measurements of soil radon indicated fluctuations related to both the meteorological and sporadic explosive events. Groundwater radon showed essential differences in concentration d...

  17. Characterization and Relocation of Seismic Clusters in the Area of Bahia de Banderas, Jalisco-Nayarit, Mexico

    Science.gov (United States)

    Rutz Lopez, M.; Nunez-Cornu, F. J.; Carmona, E.

    2004-12-01

    We analysed the seismic activity that took place the year of 2003 in the area of Bahia de Banderas, between the states of Jalisco and Nayarit, registrated with a local network of 7 stations, which belongs to the Civil Defence of Jalisco and the University of Guadalajara. 400 events have been located, in these earthquakes we identified some series of a similar waveforms. For defining this similarity between seismic events and in order to classify them into clusters, we have applied the cross-correlation method of the P and S arrivals. We found a fourth part of epicentres gathered into 15 clusters of 3-25 events. For some clusters we used relocations relative to a master event. Located south of Bahia de Banderas exist clusters aligned along structures trending N-S in the area of Tuito. This trend agrees with the topographic relief of the area. Other clustes can be related with active tectonic structures at north of Cajon de Peñas dam (Tomatlan). Another cluster was identified at the East, Amatlan de Cañas-Ameca area, and one more in the center of the Bahia de Banderas.

  18. Natural gamma radioactivity and of {sup 137} Cs in soil of the Chimaltitan municipality, Jalisco, Mexico; Radiactividad gamma natural y del {sup 137} Cs en suelo del Municipio de Chimaltitan, Jalisco, Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Garay, A.; Mireles, F.; Quirino, L.L.; Davila, J.I.; Rios, C.; Lugo, J.F.; Soriano, J.M.; Angoli, A. [UAEN-Universidad Autonoma de Zacatecas, Cipres 10, Frac. La Penuela, 98000 Zacatecas (Mexico)]. e-mail: albinogaray@hotmail.com.mx

    2003-07-01

    With the purpose of determining the activity due to the natural presence of the {sup 226} Ra, {sup 232} Th, {sup 40} K and {sup 137} Cs in soil samples, of the municipality of Chimaltitan Jalisco. A set of these samples was measured in a gamma ray spectrometric system based on a High-purity Germanium detector. It is well-known that approximately 87% of the dose of the received radiation by the population is due to sources of natural radiation and 13% of the anthropogenic radiation. The gamma radiation comes mainly from the {sup 40} K and of those radionuclides of the series of radioactive decay of {sup 238} U and {sup 232} Th that its find dispersed thoroughly in the terrestrial crust. In this work its were analyzed twenty-two soil samples. It is enlarged the activity characterization for the radioisotopes of {sup 226} Ra {sup 232} Th, {sup 40} K and {sup 137} Cs. (Author)

  19. Patrones de distribución geográfica de los mamíferos de Jalisco, México Mammal geographic distribution patterns in Jalisco State, Mexico

    OpenAIRE

    Ismael Ramos-Vizcaíno; Sergio Guerrero-Vázquez; Francisco Martín Huerta-Martínez

    2007-01-01

    Se analizaron los patrones de distribución de la riqueza de mamíferos en el estado de Jalisco y sus relaciones con algunos factores ambientales. Se obtuvo información de registros de mamíferos de Jalisco de diferentes colecciones biológicas nacionales y extranjeras. Se utilizaron las localidades de recolecta para realizar una cobertura de puntos. El estado se dividió en 159 unidades de clasificación geográfica (UCG´s) de 15' por 15'. Se sobrepuso la cobertura de puntos, las UCG y algunos mapa...

  20. Mujeres violentadas durante el embarazo y el parto: experiencias de parteras en Jalisco, México / Women abused during pregnancy and childbirth: experiences and views of midwives from Jalisco, Mexico

    OpenAIRE

    Martha Villaseñor F; Jorge Laureano E; Martha L. Mejía M; Isabel Valadez F; Márquez, José M.; Jaime A. González

    2014-01-01

    Objetivo: explorar la experiencia y perspectiva de parteras con mujeres violentadas durante el embarazo y el parto en Jalisco, México. Metodología: se llevó a cabo un estudio cualitativo en zona rural de Jalisco, México, entre mayo y octubre de 2011 con 24 parteras, utilizando la entrevista individual, modalidad historia de vida pautada y la asamblea participativa regional como técnicas de indagación; posteriormente, los discursos fueron analizados bajo el modelo actancial semiótico. Resultad...

  1. Strong interseismic coupling, fault afterslip, and viscoelastic flow before and after the Oct. 9, 1995 Colima-Jalisco earthquake: continuous GPS measurements from Colima, Mexico

    Science.gov (United States)

    Azua, B.M.; DeMets, C.; Masterlark, Timothy

    2002-01-01

    Continuous GPS measurements from Colima, Mexico during 4/93-6/01, bracketing the Oct. 9, 1995 M = 8.0 Colima-Jalisco earthquake, provide new constraints on Rivera plate subduction mechanics. Modeling of margin-normal strain accumulation before the earthquake suggests the Rivera-North America subduction interface was fully locked. Transient postseismic motion from 10/ 95-6/97 is well fit by a model that includes logarithmically-decaying fault afterslip, elastic strain from shallow fault relocking, and possibly a minor viscoelastic response, but is fit poorly by models that assume a dominant Maxwell viscoelastic response of the lower crust and upper mantle, independent of the assumed viscosities. Landward, margin-normal motion since mid-1997 is parallel to but ??? 75% slower than the pre-seismic velocity. Afterslip alone fails to account for this slowdown. The viscoelastic response predicted by a FEM correctly resolves the remaining velocity difference within the uncertainties. Both processes thus offset elastic strain accumulating from the relocked subduction interface.

  2. Ecological variability and rule-making processes for forest management institutions: a social-ecological case study in the Jalisco coast, Mexico

    Directory of Open Access Journals (Sweden)

    Sofía Monroy-Sais

    2016-09-01

    Full Text Available Analysis of social-ecological systems is becoming increasingly used since the framework provides a valuable set of variables for understanding relationships between people and ecosystems. This interaction focuses on the use and management of natural resources that, in many cases, are common-pool resources. In Mexico, common-pool resources have long been explored since at least 60% of the forested lands in the country are held under the legal figure of ‘ejidos’ and indigenous communities, which aimed at driving the collective use of lands and resources. However, few studies incorporate ecological processes for an integrated understanding of social-ecological systems. In this study, we seek to understand how ecological variability influences the creation and functioning of different rules and, consequently, institutions for forests management. Our case study was conducted in an ejido with high ecological variability located in Jalisco on the Pacific coast of Mexico. The research approach was interdisciplinary and combined qualitative and quantitative methods. We conducted participant observation and 23 semi-structured interviews; botanical collections were also carried out. We found that there is strong influence between ecological variables and the emergence of rules and collective action. The most important variables influencing these processes were the economic value of resource units, ecosystem services perceived by local people and location and size of the resource system (including area and number of species. Historical processes also play a part that generates knowledge of resource systems and the current social, economic and political settings at a larger scale. The establishment of relationships with variables that produce certain outcomes for the framework of the social-ecological system is an important challenge to be met in order to move forward in both theory and practice.

  3. [Levels of oxidative stress in serum and dietary behavior in adults in a rural area of Jalisco, Mexico].

    Science.gov (United States)

    Navarro-Meza, Monica; Arroyo-Helguera, Omar; Pacheco-Moisés, Fermin; Pita-López, Maria Luisa; Santoyo-Telles, Felipe; Ortiz, Genaro G

    2014-12-01

    Introducción: El comportamiento alimentario establece la relación del ser humano con la alimentación, comprende hábitos alimentarios que podrían intervenir en el desarrollo del estrés oxidativo. Objetivos: Evaluar la relación de indicadores de estrés oxidativo (lipoperóxidos) y capacidad antioxidante (ácido ascórbico, catalasa, superóxido dismutasa) con el comportamiento alimentario en adultos que residen en Teocuitatlán de Corona, Jalisco, México. Método: Estudio observacional, descriptivo, transversal, comparativo de 44 adultos de 43 a 88 años de edad. Se aplicó un instrumento de comportamiento alimentario. Los resultados del cuestionario se relacionaron con los indicadores de estrés oxidativo. Se utilizó estadística descriptiva, distribución de frecuencias y análisis de co-varianza con ajuste de variables, se consideró una significancia de p.

  4. Biological and ecological aspects of Xantusia sanchezi, an endangered lizard in an oak forest in the state of Jalisco, Mexico Aspectos biológicos y ecológicos de Xantusia sanchezi, una lagartija en peligro en un bosque de encino en el estado de Jalisco, México

    Directory of Open Access Journals (Sweden)

    Daniel Cruz-Sáenz

    2012-03-01

    Full Text Available Xantusia sanchezi is an endangered species that is endemic to Mexico and is known only from the states of Jalisco and Zacatecas. We studied a population from a locality known as Huaxtla, in the municipality of Zapopan in the state of Jalisco. Sampling was conducted over a period of 7 months in an area of 1.5 hectares of grassland and oak forest with boulders. Collected data included: body measurements (total length, snout-vent length, tail length, head length, head width, head height, femur length, and femoral pores, sex, weight, habitat and average temperature and humidity. Habitat characterization was made using a coverage analysis. A total of 29 individuals were captured with 7 re-captures. This work provides the first data on the biology and ecology of this species, which is known in Jalisco from only a small area under tremendous threat due to urban development.Se realizó el estudio de una población de Xantusia sanchezi, una lagartija endémica de México y en peligro de extinción, que habita en los estados de Jalisco y Zacatecas. El muestreo se llevó a cabo por un periodo de 7 meses en una superficie de 1.5 hectáreas cuyo tipo de vegetación es pastizal con bosque de encino y afloramientos rocosos. El muestreo se efectuó en la localidad conocida como Huaxtla, ubicada en el municipio de Zapopan en el estado de Jalisco. Se tomaron diversos datos de los ejemplares, sexo, peso, hábitat y variables climáticas como temperatura y humedad. Además, se caracterizó el hábitat de la especie mediante el uso de análisis de las coberturas. Se registraron 29 ejemplares, algunos de estos fueron recapturados en distintas ocasiones. Este trabajo aporta datos sobre la biología y ecología de la especie, en una zona donde enfrenta fuertes presiones debido a los desarrollos habitacionales que se están construyendo y los que se tienen contemplados.

  5. Dating of a representative pottery sample from the basin of Sayula, Jalisco in Mexico using the thermoluminescence method

    Energy Technology Data Exchange (ETDEWEB)

    Mercado U, H. [CINVESTAV, Unidad Monterrey, Nuevo Leon (Mexico); Schaaf, P.; Ramirez, A. [Instituto de Geofisica, UNAM, 04510 Mexico D.F. (Mexico); Gonzalez, P.R. [ININ, 52750 Ocoyoacac, Estado de Mexico (Mexico); Brunet, J. [CUCSH, Universidad de Guadalajara, Jalisco (Mexico)

    2006-07-01

    In this work is presented a study of dating of the representative pottery sample from the west of Mexico, in a predominantly saline region. The study is carried out with the thermoluminescence method and the fine grain technique. The archaeological region was begun to study from 1990. This work also presents an historical and geographical context of the region and its relevance in the western culture of Mexico. (Author)

  6. Inventorying and Monitoring of Tropical Dry Forests Tree Diversity in Jalisco, Mexico Using a Geographical Information System

    Science.gov (United States)

    Efren Hernandez-Alvarez; Dieter R. Pelz; Carlos Rodriguez Franco

    2006-01-01

    Tropical dry forests in Mexico are an outstanding natural resource, due to the large surface area they cover. This ecosystem can be found from Baja California Norte to Chiapas on the eastern coast of the country. On the Gulf of Mexico side it grows from Tamaulipas to Yucatan. This is an ecosystem that is home to a wide diversity of plants, which include 114 tree...

  7. Integración florística de las algas marinas de la costa sur de Jalisco, México Floristic integration of the benthic marine algae from the southern coast of Jalisco, Mexico

    Directory of Open Access Journals (Sweden)

    A. Catalina Mendoza-González

    2011-03-01

    Full Text Available Se presentan los resultados obtenidos en un estudio sobre las algas marinas bentónicas en 7 localidades de la costa sur de Jalisco, México. Se determinó la presencia de 165 especies de algas marinas. Se identificaron 13 especies de Cyanophyta, 97 Rhodophyta, 28 Chlorophyta y 27 taxa de Heteroconthophyta. Cada especie se acompaña con datos sobre su distribución en el área de estudio, estado reproductivo, nivel de marea, hábitat, observaciones, epifitismo y número de herbario o de colecta. Se comparó la riqueza específica entre la estación climática de lluvias y la de secas, durante 1992,1993, 1997, 2000 y 2003. La división Rhodophyta dominó en términos de diversidad en relación con las 3 divisiones restantes. La ficoflora de la costa sur de Jalisco es de afinidad tropical y más diversa en la época de secas.We present results on the study on benthic marine algae in seven localities from the southern coast of Jalisco. We report 165 species: 13 Cyanophyta, 97 Rhodophyta, 28 Chlorophyta and 27 Heteroconthophyta. Each species includes data on its distribution, reproductive stages, tidal level, facies, epiphytism and herbarium's number. Species diversity was compared for 2 different climatic seasons during 1992, 1993, 1997, 2000 and 2003. The Rhodophyta are dominant in terms of diversity in relation to the other groups. The algal flora of the south coast of Jalisco is tropical and the greatest diversity was found during dry season.

  8. Landscape changes in a coastal system undergoing tourism development: implications for Barra de Navidad Lagoon, Jalisco, Mexico

    Directory of Open Access Journals (Sweden)

    Tara L. Holland

    2011-01-01

    Full Text Available Por medio de dos imágenes de satélite adquiridas en 1985 (Landsat TM y 2000 (Landsat ETM+, se analizan cuantitativamente los patrones de cambio de cobertura y uso del suelo ocurridos entre 1985 y 2000 en la laguna de Barra de Navidad, Jalisco, México y su cuenca de drenaje. El análisis de las imágenes se realizó mediante una clasificación supervisada y verificación en campo de seis categorías de uso/cobertura de suelo: lagunar, agricultura, selva seca tropical, manglar y sin vegetación. Los cambios espaciales en la composición del uso del suelo fueron evaluados utilizando una matriz de transición y los cambios de configuración se interpretaron utilizando la métrica del paisaje. Los resultados mostraron que las áreas urbanas y turísticas se expandieron, a costa de la selva baja y suelos sin cobertura. También el manglar mostró un gran decremento (-39% experimentando una severa fragmentación. Estos cambios parecen estar relacionados con el incremento de la sedimentación, resultado de la erosión del suelo aguas arriba y a la progradación de un abanico dentro de la laguna de Barra de Navidad. Los resultados obtenidos pueden servir como un modelo de comparación de otros sistemas que experimentan múltiples factores estresantes, especialmente cambios relacionados con el turismo y la intensificación del uso del suelo.

  9. Radon, volatile organic compounds and water chemistry in springs around Popocatepetl volcano, Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Segovia, N.; Pena, P.; Lopez, M.B.E.; Cisniega, G. [Inst. Nacional de Investigaciones Nucleares, Mexico D.F. (Mexico); Valdes, C.; Armienta, M.A.; Mena, M. [Inst. de Geofisica, UNAM, Ciudad Univ., Mexico D.F. (Mexico)

    2003-07-01

    Popocatepetl volcano is a high-risk active volcano in Central Mexico where the highest population density in the country is settled. Radon in the soil and groundwater together with water chemistry from samples of nearby springs is analysed as a function of the 2002-2003 volcanic activity. Soil radon indicated fluctuations related both to the meteorological and sporadic explosive events. Groundwater radon showed essentially differences in concentration due to the specific characteristics of the studied springs. Water chemistry showed also stability along the monitoring period indicating differences between springs. No anthropogenic pollution from volatile organic compounds was observed. (orig.)

  10. Five new species of the genera Heerz Marsh, Lissopsius Marsh and Ondigus Braet, Barbalho and van Achterberg (Braconidae, Doryctinae) from the Chamela-Cuixmala biosphere reserve in Jalisco, Mexico.

    Science.gov (United States)

    Zaldívar-Riverón, Alejandro; Martínez, Juan José; Ceccarelli, Fadia Sara; Shaw, Scott R

    2012-01-01

    Five new species belonging to the poorly known Neotropical doryctine parasitoid wasps genera Heerz Marsh (Heerz ecmahlasp. n. and Heerz macrophthalmasp. n.), Lissopsius Marsh (Lissopsius pacificussp. n. and Lissopsius jalisciensissp. n.) and Ondigus Braet, Barbalho & van Achterberg (Ondigus cuixmalensissp. n.) are described from the Chamela-Cuixmala Biosphere reserve in Jalisco, Mexico. Keys to the described species of the above three genera are provided. The phylogenetic placement of the examined taxa is investigated based on mitochondrial (COI) and nuclear (28S, 2(nd) and 3(rd) domain regions) DNA sequence data.

  11. Five new species of the genera Heerz Marsh, Lissopsius Marsh and Ondigus Braet, Barbalho and van Achterberg (Braconidae, Doryctinae from the Chamela-Cuixmala biosphere reserve in Jalisco, Mexico

    Directory of Open Access Journals (Sweden)

    Alejandro Zaldivar-Riveron

    2012-01-01

    Full Text Available Five new species belonging to the poorly known Neotropical doryctine parasitoid wasps genera Heerz Marsh (H. ecmahla sp. n. and H. macrophthalma sp. n., Lissopsius Marsh (L. pacificus sp. n. and L. jalisciensis sp. n. and Ondigus Braet, Barbalho & van Achterberg (O. cuixmalensis sp. n. are described from the Chamela-Cuixmala Biosphere reserve in Jalisco, Mexico. Keys to the described species of the above three genera are provided. The phylogenetic placement of the examined taxa is investigated based on mitochondrial (COI and nuclear (28S, 2nd and 3rd domain regions DNA sequence data.

  12. Radiologic inspection in an office built rod contaminated with radioactive material, in Tiaquepaque, Jalisco, Mexico; Inspeccion radiologica en una oficina construida con varilla contaminada con material radiactivo, en Tlaquepaque, Jalisco, Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Salas Mar, B.

    2011-07-01

    Note that in 1983 took place {sup T}he most important radiological accident occurred in Mexico in recent years occurred in Ciudad Juarez, Chihuahua, consisting ea involuntary casting a source of Cobalt-60 (originally intended for medical use in teletherapy) and manufacture of rods for the construction and steel bases for tables, in the smelter {sup S}teel de Chihuahua{sup ,} so presumably, that the rods of the office of Tlaquepaque, come from the radiological accident.

  13. Anatomy of the Colima volcano magmatic system, Mexico

    Science.gov (United States)

    Spica, Zack; Perton, Mathieu; Legrand, Denis

    2017-02-01

    Colima volcano is one of the most active volcanoes in continental north America. It is located within the Colima graben on the western part of the Colima rift zone. Although extensively studied, the internal structure and deep magmatic system remains unknown. This research gives new clues to understand how and where magmas are produced and stored at depth. Using ambient seismic noise, we jointly invert for Rayleigh and Love wave dispersion curves for both phase and group velocity, which is applied for the first time in a volcanic environment. We invert for both the shear wave velocity and radial anisotropy. The 3D high resolution shear wave velocity model shows a deep, large and well-delineated elliptic-shape magmatic reservoir below the Colima volcano complex at a depth of about 15 km. On the other hand, the radial anisotropy model shows a significant negative feature (i.e., VSV >VSH) revealed from ≥35 km depth until the top of the magma reservoir at about 12 km depth. The latter suggests the presence of numerous vertical fractures where fluids, rooting from a well-known mantle window, can easily migrate upward and then accumulate in the magma reservoir. Furthermore, the convergence of both a low velocity zone and a negative anisotropy suggests that the magma is mainly stored in conduits or inter-fingered dykes as opposed to horizontally stratified magma reservoir.

  14. Hazard map for volcanic ballistic impacts at El Chichón volcano (Mexico)

    Science.gov (United States)

    Alatorre-Ibarguengoitia, Miguel; Ramos-Hernández, Silvia; Jiménez-Aguilar, Julio

    2014-05-01

    The 1982 eruption of El Chichón Volcano in southeastern Mexico had a strong social and environmental impact. The eruption resulted in the worst volcanic disaster in the recorded history of Mexico, causing about 2,000 casualties, displacing thousands, and producing severe economic losses. Even when some villages were relocated after the 1982 eruption, many people still live and work in the vicinities of the volcano and may be affected in the case of a new eruption. The hazard map of El Chichón volcano (Macías et al., 2008) comprises pyroclastic flows, pyroclastic surges, lahars and ash fall but not ballistic projectiles, which represent an important threat to people, infrastructure and vegetation in the case of an eruption. In fact, the fatalities reported in the first stage of the 1982 eruption were caused by roof collapse induced by ashfall and lithic ballistic projectiles. In this study, a general methodology to delimit the hazard zones for volcanic ballistic projectiles during volcanic eruptions is applied to El Chichón volcano. Different scenarios are defined based on the past activity of the volcano and parameterized by considering the maximum kinetic energy associated with ballistic projectiles ejected during previous eruptions. A ballistic model is used to reconstruct the "launching" kinetic energy of the projectiles observed in the field. The maximum ranges expected for the ballistics in the different explosive scenarios defined for El Chichón volcano are presented in a ballistic hazard map which complements the published hazard map. These maps assist the responsible authorities to plan the definition and mitigation of restricted areas during volcanic crises.

  15. Late Pleistocene-Holocene cataclysmic eruptions at Nevado de Toluca and Jocotitlan volcanoes, central Mexico

    Science.gov (United States)

    Macias, J.L.; Garcia, P.A.; Arce, J.L.; Siebe, C.; Espindola, J.M.; Komorowski, J.C.; Scott, K.

    1997-01-01

    This field guide describes a five day trip to examine deposits of Late Pleistocene-Holocene cataclysmic eruptions at Nevado de Toluca and Jocotitlan volcanoes in central Mexico. We will discuss the stratigraphy, petrology, and sedimentological characteristics of these deposits which provide insights into the eruptive history, type of volcanic activity, and transport and emplacement mechanisms of pyroclastic materials. These parameters will allow us to discuss the kinds of hazards and the risk that they pose to populations around these volcanoes. The area to be visited is tectonically complex thus we will also discuss the location of the volcanoes with respect to the tectonic environment. The first four days of the field trip will be dedicated to Nevado de Toluca Volcano (19 degrees 09'N; 99 degrees 45'W) located at 23 km. southwest of the City of Toluca, and is the fourth highest peak in the country, reaching an elevation of 4,680 meters above sea level (m.a.s.l.). Nevado de Toluca is an andesitic-dacitic stratovolcano, composed of a central vent excavated upon the remains of older craters destroyed by former events. Bloomfield and Valastro, (1974, 1977) concluded that the last cycle of activity occurred nearly equal 11,600 yr. ago. For this reason Nevado de Toluca has been considered an extinct volcano. Our studies, however, indicate that Nevado de Toluca has had at least two episodes of cone destruction by sector collapse as well as several explosive episodes including plinian eruptions and dome-destruction events. These eruptions occurred during the Pleistocene but a very young eruption characterized by surge and ash flows occurred ca. 3,300 yr. BP. This new knowledge of the volcano's eruptive history makes the evaluation of its present state of activity and the geological hazards necessary. This is important because the area is densely populated and large cities such as Toluca and Mexico are located in its proximity.

  16. Diversidad de avispas parasitoides de la familia Encyrtidae (Hymenoptera: Chalcidoidea del bosque tropical caducifolio en San Buenaventura, Jalisco, México Diversity of parasitoid wasps of the family Encyrtidae (Hymenoptera: Chalcidoidea in the tropical dry forest of San Buenaventura, Jalisco, Mexico

    Directory of Open Access Journals (Sweden)

    Beatriz Rodríguez-Velez

    2011-09-01

    Full Text Available Se presentan los resultados del estudio de la fauna de avispas parasitoides de la familia Encyrtidae en el bosque tropical caducifolio de San Buenaventura, Jalisco, México. El estudio se llevó a cabo de noviembre de 1996 a octubre de 1997. La recolección se realizó con trampas Malaise durante 5 días de cada mes. Se registró un total de 61 especies, 30 géneros, 13 tribus y 2 subfamilias. El mayor número de géneros y especies fue de la subfamilia Encyrtinae, con 22 géneros y 44 especies, seguida por Tetracneminae con 8 géneros y 17 especies. El género con mayor número de especies fue Metaphycus con 11. Las especies recolectadas no fueron abundantes, y su riqueza y abundancia varió estacionalmente, registrándose los valores más altos durante la temporada de lluvias. La similitud de la fauna de San Buenaventura, Jalisco con la de Huautla, Morelos fue mayor que la encontrada en otras regiones previamente estudiadas de bosque tropical caducifolio (San Javier, Sonora y Huatulco, Oaxaca.Results of a faunistic study of the parasitoid wasps of the family Encyrtidae of the tropical dry forest of San Buenaventura, Jalisco, Mexico are presented. The study was carried out from November 1996 to October 1997. Collecting technique was Malaise trapping. Collections were carried out during 5 days of every month. A total of 61 species, 30 genera, 13 tribes and 2 subfamilies were recorded. The subfamily with the largest number of species was Encyrtinae with 22 genera and 44 species, followed by Tetracneminae with 8 genera and 17 species. The genus with the largest number of species was Metaphycus with 11. Species had low abundance. Species richness and abundance varied with time, with the highest values recorded in the rainy season. The fauna of San Buenaventura, Jalisco was most similar to that of Huautla, Morelos, than to that of San Javier, Sonora and Huatulco, Oaxaca, all of them previously studied.

  17. Geochemistry of the volcano-hydrothermal system of El Chichón Volcano, Chiapas, Mexico

    Science.gov (United States)

    Taran, Yuri; Fischer, Tobias P.; Pokrovsky, Boris; Sano, Yuji; Armienta, Maria Aurora; Macias, Jose Luis

    The 1982 eruption of El Chichón volcano ejected more than 1km3 of anhydrite-bearing trachyandesite pyroclastic material to form a new 1-km-wide and 300-m-deep crater and uncovered the upper 500m of an active volcano-hydrothermal system. Instead of the weak boiling-point temperature fumaroles of the former lava dome, a vigorously boiling crater spring now discharges / 20kg/s of Cl-rich ( 15 000mg/kg) and sulphur-poor ( / 200mg/kg of SO4), almost neutral (pHup to 6.7) water with an isotopic composition close to that of subduction-type magmatic water (δD=-15‰, δ18O=+6.5‰). This spring, as well as numerous Cl-free boiling springs discharging a mixture of meteoric water with fumarolic condensates, feed the crater lake, which, compared with values in 1983, is now much more diluted ( 3000mg/kg of Cl vs 24 030mg/kg), less acidic (pH=2.6 vs 0.56) and contains much lower amounts of S ( / 200mg/kg of SO4, vs 3550mg/kg) with δ34S=0.5-4.2‰ (+17‰ in 1983). Agua Caliente thermal waters, on the southeast slope of the volcano, have an outflow rate of approximately 100kg/s of 71 °C Na-Ca-Cl water and are five times more concentrated than before the eruption (B. R. Molina, unpublished data). Relative N2, Ar and He gas concentrations suggest extensional tectonics for the El Chichón volcanic centre. The 3He/4He and 4He/20Ne ratios in gases from the crater fumaroles (7.3Ra, 2560) and Agua Caliente hot springs (5.3Ra, 44) indicate a strong magmatic contribution. However, relative concentrations of reactive species are typical of equilibrium in a two-phase boiling aquifer. Sulphur and C isotopic data indicate highly reducing conditions within the system, probably associated with the presence of buried vegetation resulting from the 1982 eruption. All Cl-rich waters at El Chichón have a common source. This water has the appearence of a "partially matured" magmatic fluid: condensed magmatic vapour neutralized by interaction with fresh volcaniclastic deposits and depleted in S

  18. Volcanoes

    Science.gov (United States)

    ... or more from a volcano. Before a Volcanic Eruption The following are things you can do to ... in case of an emergency. During a Volcanic Eruption Follow the evacuation order issued by authorities and ...

  19. Patrones de distribución geográfica de los mamíferos de Jalisco, México Mammal geographic distribution patterns in Jalisco State, Mexico

    Directory of Open Access Journals (Sweden)

    Ismael Ramos-Vizcaíno

    2007-06-01

    Full Text Available Se analizaron los patrones de distribución de la riqueza de mamíferos en el estado de Jalisco y sus relaciones con algunos factores ambientales. Se obtuvo información de registros de mamíferos de Jalisco de diferentes colecciones biológicas nacionales y extranjeras. Se utilizaron las localidades de recolecta para realizar una cobertura de puntos. El estado se dividió en 159 unidades de clasificación geográfica (UCG´s de 15' por 15'. Se sobrepuso la cobertura de puntos, las UCG y algunos mapas de CONABIO para formar una matriz de presencia-ausencia. Se analizó la distribución de la riqueza por tipo de vegetación y altitud. Se observó un gradiente de riqueza que va desde las zonas tropicales hasta las semiáridas. Por altitud, la mayor riqueza se encontró entre los 1500 y 2000 m y la menor de los 4000 a 4500 m. Se aplicó una ordenación de Bray-Curtis y una clasificación con TWINSPAN. Ambas fueron consistentes en formar 2 grupos de mamíferos; uno con especies de la costa y el otro del noreste del estado, lo que refleja un gradiente climático. El porcentaje de variación acumulada fue del 94% y las variables del medio con mayor influencia fueron precipitación, temperatura, evaporación, altitud y vegetación.We analyzed the patterns of distribution of mammal species richness in Jalisco State and their relationships with some environmental factors. We retrieved distribution data from several national and foreign biological collections. We used the collecting localities to generate a spatial record of distribution points. The state was divided into 159 geographic units of classification (GUC's of 15' by 15'. We overlap the point cover, GUCs and some maps from CONABIO to create a presence-absence matrix. We analyzed the richness distribution by vegetation type and elevation. A richness gradient was observed from tropical to semiarid vegetation types and according to elevation; we observed higher richness between 1500 and 2000 m a. s

  20. Upgrading the seismic and geodetic network of the Popocatépetl volcano (Mexico).

    Science.gov (United States)

    Calò, Marco; Iglesias Mendoza, Arturo; Legrand, Denis; Valdés González, Carlos Miguel; Perez Campos, Xyoli

    2017-04-01

    The Popocatépetl is one of the most active volcanoes in Mexico and is located only 70 km from Mexico City, populated by more than 20 millions of people, and only 35 km from the Puebla municipality with almost 1.5 millions of people living. The recent activity of the volcano is generally marked by explosions emitting ash plumes often reaching the densely populated regions. In the framework of the Mexican Fund for Prevention of Natural Disasters (FOPREDEN) we are renovating and upgrading the existing geodetic and seismic networks monitoring the volcano. In this project we are installing 10 broadband seismic stations (120s-050Hz) in shallow boreholes (3-5m depth) and 4 GPS with real time sampling rate of 1 Hz. All instruments are equipped with continuous recording systems for real time monitoring purposes and research. The Popocatépetl exceeds 5400m, and the altitude of the stations ranges from 2200 m to 4300 m making it difficult their installation and maintenance. Because of ash emissions and the hard working condition, the real-time transmission is split into two systems in order to ensure the monitoring of the volcano also during the highest expected activity. Therefore we set up a network of "first order", consisting of four stations located about 20 km from the crater and equipped with satellite transmission. These stations, being far enough from the crater, ensure the real time monitoring of the major events also during intense periods of activity of the volcano. The remaining six stations are installed near to the crater (less than 10 km) and take part of the "second order" network equipped with a telemetered radio system transmitting the data either directly to the National Center of Disaster Prevention (CENAPRED) and National Seismological Service (SSN) or to the first order stations (for the sites that have not direct visible line with the monitoring centers). The four GPS sensors are all installed in the second order sites in order to monitor the largest

  1. Support networks of women victims of partner violence in Jalisco (Mexico [La red de apoyo en mujeres víctimas de violencia contra la pareja en el estado de Jalisco (México

    Directory of Open Access Journals (Sweden)

    Cristina Estrada Pineda

    2012-06-01

    Full Text Available The main goal of the present research is to identify the support networks of women victims of partner violence paying attention to both sources and type of support provided. Information about network support from 204 participants living in Guadalajara (Jalisco, México was obtained using the Relationship-specific Perceived Social Support (Gracia & Herrero, 2004. Cluster analysis revealed that the most frequent type of support network included friends as the main source of social support. Two other types of network support were found in this study: family of origin support (mother and sisters, mainly and partner and offspring’s support (in some cases the batterer was also included in this support network.

  2. a Reconstruction of the 1793 Eruption of San Martin Tuxtla Volcano, Veracruz, Mexico

    Science.gov (United States)

    Espindola, J.; Zamora-Camacho, A.; Godinez, L.

    2013-05-01

    San Martin Volcano is located in the State of Veracruz, Eastern Mexico (18.572N, 95.169W, 1650 masl). The last eruption of this volcano occurred in 1793. The activity, which was documented lasted for several months and produced thick ashfall deposits in its vicinity. The blasts were heard in the coast of Tampico some 500km NW from the volcano. There are also reports of noticeable ashfall at distances as far as 200 Km from the crater. No casualties from the eruption were reported but the economic and other human activities were greatly perturbed. The center of emission eruption was a cinder cone located within the 500 wide crater in the summit of the volcano. We present isopach maps of the airfall deposits from this eruption. The 5cm isopach covers an area roughly 200 Km2 with downwind axis towards the W-SW. Based on this information we reconstructed some of the characteristics of the eruption by fitting the theoretical isopachs obtained from the well known model of ash deposition by Suzuki to the observed isopachs. The estimated height of the eruptive column is of the order of 10 km for a mass erupted of 0.5 cubic km. We used wind data from the nearby meteorological station of the city of Veracruz.

  3. Influence of Tropical Cyclones Period 1970 TO 2010 IN the Region of Bahia de Banderas, Nayarit-Jalisco Mexico

    Science.gov (United States)

    Hernandez, J. M.

    2013-12-01

    This study evaluates the impacts of tropical cyclones (TC) that made landfall in populated areas along the Pacific coast of Mexico, especially in the region of Bahia de Banderas. During the period of 1970-2010 and used a database of international natural disasters to identify impacts. Were more than 13 events during the reporting period, of which 10 are examined more precipitation accumulated and 6 that caused further damage to the affected population in these cases ranged from 5000 to more than 15 000 inhabitants. Strong winds and heavy rainfall in periods of one to three days were associated with property damage and loss of life. The results of the study indicate that excessive accumulations of rain and daily intensity are important factors connected with the occurrence of disasters in densely populated areas. Six of the first 10 Tropical Cyclone associated with major disasters occurred in conditions of El Niño and four neutral conditions. With the analysis of satellite images using GOES-10 in the IDV software maps were obtained in the coastal impacts of Banderas Bay and describes the main features of each meteorological phenomena. In which concludes that no tropical cyclone entered directly to the Banderas Bay region, but its effects were very relevant, taking into account the topography, land use change and the vulnerability of the region. Tropical Cyclones that have affected the region of Bay of Banderas

  4. Tremor and its duration-amplitude distribution at Popocatépetl volcano, Mexico

    Science.gov (United States)

    Arámbula-Mendoza, R.; Valdés-González, C.; Varley, N.; Reyes-Pimentel, T. A.; Juárez-García, B.

    2016-09-01

    The duration-amplitude distribution was calculated for the tremor observed at Popocatépetl volcano during episodes of activity in 2000 and 2012-2014. An exponential function was used to obtain a good fit for the duration-amplitude distribution, and the source of volcanic tremor is probably generated by the transportation of magmatic fluids and its coupling with the host rock within the volcanic conduit. In particular, harmonic tremor has shown large amplitudes, durations, and mean values of amplitude, more than spasmodic or pulsating tremor. This is due to different generation mechanisms: in the case of harmonic tremor, it is produced during magma ascent and lava dome growth, while spasmodic and pulsating tremors are associated with fragmentation of the lava dome and gas emissions. This paper presents the duration-amplitude distribution as a method to estimate the intensity of the tremor at Popocatépetl, a volcano with the major risk in all Mexico.

  5. Crustal structure below Popocat\\'epetl Volcano (Mexico) from analysis of Rayleigh waves

    CERN Document Server

    De Barros, Louis; Métaxian, J -P; Valdés-Gonzales, C; Lesage, Philippe

    2007-01-01

    An array of ten broadband stations was installed on the Popocat\\'epetl volcano (Mexico) for five months between October 2002 and February 2003. 26 regional and teleseismic earthquakes were selected and filtered in the frequency time domain to extract the fundamental mode of the Rayleigh wave. The average dispersion curve was obtained in two steps. Firstly, phase velocities were measured in the period range [2-50] s from the phase difference between pairs of stations, using Wiener filtering. Secondly, the average dispersion curve was calculated by combining observations from all events in order to reduce diffraction effects. The inversion of the mean phase velocity yielded a crustal model for the volcano which is consistent with previous models of the Mexican Volcanic Belt. The overall crustal structure beneath Popocat\\'epetl is therefore not different from the surrounding area, and the velocities in the lower crust are confirmed to be relatively low. Lateral variations of the structure were also investigated ...

  6. Seroepidemiology of Toxoplasma gondii infection in drivers involved in road traffic accidents in the metropolitan area of Guadalajara, Jalisco, Mexico.

    Science.gov (United States)

    Galván-Ramírez, Ma de la Luz; Sánchez-Orozco, Laura Verónica; Rodríguez, Laura Rocío; Rodríguez, Saúl; Roig-Melo, Enrique; Troyo Sanromán, Rogelio; Chiquete, Erwin; Armendáriz-Borunda, Juan

    2013-10-11

    The prevalence of toxoplasmosis in the general population of Guadalajara, Mexico, is around 32%. Toxoplasmosis can cause ocular lesions and slowing of reaction reflexes. Latent toxoplasmosis has been related with traffic accidents. We aimed to assess the prevalence of anti-Toxoplasma gondii antibodies and visual impairments related with traffic accidents in drivers from the metropolitan Guadalajara. We prospectively evaluated the prevalence of IgG and IgM anti-T. gondii antibodies in 159 individuals involved in traffic accidents, and in 164 control drivers never involved in accidents. Cases of toxoplasmosis reactivation or acute infection were detected by PCR in a subset of 71 drivers studied for the presence of T. gondii DNA in blood samples. Ophthalmologic examinations were performed in drivers with IgG anti-T. gondii antibodies in search of ocular toxoplasmosis. Fifty-four (34%) traffic accident drivers and 59 (36%) controls were positive to IgG anti-T. gondii antibodies (p = 0.70). Among the 113 seropositive participants, mean anti-T. gondii IgG antibodies titers were higher in traffic accident drivers than in controls (237.9 ± 308.5 IU/ml vs. 122.9 ± 112.7 IU/ml, respectively; p = 0.01 by Student's t test, p = 0.037 by Mann-Whitney U test). In multivariate analyses, anti-T. gondii IgG antibody titers were consistently associated with an increased risk of traffic accidents, whereas age showed an inverse association. The presence of IgM-anti-T. gondii antibodies was found in three (1.9%) subjects among traffic accident drives, and in two (1.2%) controls. Three (4.2%) samples were positive for the presence of T. gondii DNA, all among seropositive individuals. No signs of ocular toxoplasmosis were found in the entire cohort. Moreover, no other ocular conditions were found to be associated with the risk of traffic accidents in a multivariate analysis. Anti-T. gondii antibody titers are associated with the risk of traffic accidents. We could not determine any

  7. The 1793 eruption of San Martín Tuxtla volcano, Veracruz, Mexico

    Science.gov (United States)

    Espíndola, J. M.; Zamora-Camacho, A.; Godinez, M. L.; Schaaf, P.; Rodríguez, S. R.

    2010-11-01

    San Martín Tuxtla (N18.562°; W95.199°, 1659 masl) is a basaltic volcano located in southern Veracruz, a Mexican State bordering the Gulf of Mexico. It rises in a volcanic field strewn with monogenetic volcanic cones, maars and three other large volcanoes mostly dormant since the late Pliocene: Santa Marta, San Martín Pajapan and Cerro El Vigía. The latest eruptive event of San Martín occurred in 1793 and was described by Don José Mariano Moziño, a naturalist under the commission of the Viceroy of the then New Spain. In this work we present results of the study of this eruption based on historical accounts and field observations. We identified an ash deposit around the volcano related to the 1793 eruption, mapped its distribution and determined its granulometric, petrographic and geochemical characteristics. These studies suggest that the volcano began its activity with explosive phreatomagmatic explosions, which were followed by Strombolian activity; this period lasting from March to October 1793. The activity continued with an effusive phase that lasted probably 2 years. The eruption covered an area of about 480 km 2 with at least 1 cm of ash; the fines reaching distances greater than 300 km from the crater. A total mass of about 2.5 × 10 14 g was ejected and the volcanic columns probably reached altitudes of the order of 10 km during the most explosive phases. The lava emitted formed a coulee that descended the northern flank of the volcano and has an approximate volume of 2.0 × 10 7 m 3.

  8. Geochemistry of summit fumarole vapors and flanking thermal/mineral waters at Popocatepetl Volcano, Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Werner, C.; Goff, F. [Los Alamos National Lab., NM (United States); Janik, C.J. [Geological Survey, Menlo Park, CA (United States)] [and others

    1997-06-01

    Popocatepetl Volcano is potentially devastating to populations living in the greater Mexico City area. Systematic monitoring of fumarole gases and flanking thermal/mineral springs began in early 1994 after increased fumarolic and seismic activity were noticed in 1991. These investigations had two major objectives: (1) to determine if changes in magmatic conditions beneath Popocatepetl might be reflected by chemical changes in fumarolic discharges and (2) to determine if thermal/mineral spring waters in the vicinity of Popocatepetl are geochemically related to or influences by the magmatic system. This report summarizes results from these two discrete studies.

  9. Fluoride in ash leachates: environmental implications at Popocatépetl volcano, central Mexico

    Directory of Open Access Journals (Sweden)

    M. A. Armienta

    2011-07-01

    Full Text Available Ash emitted by volcanic eruptions, even of moderate magnitude, may affect the environment and the health of humans and animals through different mechanisms at distances significantly larger than those indicated in the volcanic hazard maps. One such mechanism is the high capacity of ash to transport toxic volatiles like fluoride, as soluble condensates on the particles' surface. The mobilization and hazards related to volcanic fluoride are discussed based on the data obtained during the recent activity of Popocatépetl volcano in Central Mexico.

  10. Timing magma ascent at Popocatepetl Volcano, Mexico, 2000-2001

    Science.gov (United States)

    Martin-Del Pozzo, A. L.; Cifuentes, G.; Cabral-Cano, E.; Bonifaz, R.; Correa, F.; Mendiola, I. F.

    2003-07-01

    Magnetic anomalies may be used to constrain magma ascent and are useful as precursors to eruptions especially when correlated with other geophysical and geochemical data. In this paper we present multiparameter data on the magnetics, dome morphology, geochemistry and seismicity associated with the December 2000-January 2001 eruptions, the largest of the recent eruptions at Popocatepetl Volcano. A 6-month data period was studied in order to evaluate the precursors and post-eruption processes. Several cycles of dome construction and destruction occurred from September 2000 through February 2001. In December, large amplitude tremor associated with a higher effusion rate resulted in the formation of a large dome which filled the crater to within about 50 m of the lowest part of the crater rim. Seismic activity in December was marked by many volcanotectonic earthquakes and both high frequency and harmonic tremor. On December 12 and 13, an increase in the tremor amplitude was followed by ash eruptions with 1.7-5-km-high columns. Tremor amplitude increased again on December 15 and oscillated for the next four days. Activity remained high until the end of the month. On January 22, an 18-km-high plume produced ash and pumice fall to the east as well as pyroclastic flows and mudflows which reached 6 km from the crater. The eruption left three concentric explosion pits, partially destroying the December dome. Mixing of a mafic olivine-bearing melt with a more evolved magma triggered the larger eruption on January 22 as can be seen from the higher MgO concentrations in some of the ejecta and the presence of a dark andesitic scoria with lower silica content and a white andesitic pumice with higher silica content. Precursory negative magnetic anomalies up to 5 nT (-3.2 nT, -5 nT, -2.9 nT) were associated with the ascent of the larger batches of magma which preceded the increases in seismicity, before the December 2000-January 22 VEI 3-4 eruptions. No significant increases in

  11. Update of map the volcanic hazard in the Ceboruco volcano, Nayarit, Mexico

    Science.gov (United States)

    Suarez-Plascencia, C.; Camarena-Garcia, M. A.; Nunez-Cornu, F. J.

    2012-12-01

    (Hibiscus sabdariffa). Recently it has established tomato and green pepper crops in greenhouses. The regional commercial activities are concentrated in the localities of Ixtlán, Jala and Ahuacatlán. The updated hazard maps are: a) Hazard map of pyroclastic flows, b) Hazard map of lahars and debris flow, and c) Hazard map of ash-fall. The cartographic and database information obtained will be the basis for updating the Operational Plan of the Ceboruco Volcano by the State Civil & Fire Protection Unit of Nayarit, Mexico, and the urban development plans of surrounding municipalities, in order to reduce their vulnerability to the hazards of the volcanic activity.

  12. Characterization of the recent ash emissions at Popocatepetl Volcano, Mexico

    Science.gov (United States)

    Martin-Del Pozzo, A. L.; González-Morán, T.; Espinasa-Pereña, R.; Butron, M. A.; Reyes, M.

    2008-02-01

    Nine representative ash emissions from 1994-1997 were studied to characterize the recent activity and the eruptive process at Popocatepetl. A series of tephra eruptions began on December 21, 1994 and intermittent activity continues to present. The first eruptions were phreatomagmatic but in mid-March 1996 they turned magmatic. Cumulative volumes (529-1810 × 10 3 m 3), were determined for the first eruptions. However, when eruptions grew larger, more widely spaced (and magmatic), the volumes were then calculated individually (22-1107 × 10 3 m 3), both using the Simpson Rule and based on 244 sampling sites. This numerical integration method is more precise than other methods especially since sub-mm isopachs are neglected in most cases. Dominant winds carried ash mainly to the east (January through April 1995 and April 1996) except for the summer months when ash fell on Mexico City to the northwest (October 28 1996 and June 30 1997). In March 1996, changing wind direction produced ash fall to the southwest as well. During the first year, volume calculations indicated that emission rate was higher at the beginning of the eruptions and then declined and stopped. Activity resumed the following year with a similar pattern until larger amounts of magma ascended. Detailed studies of the ashfall provided constraints on the dynamics of the volcanic plumbing system. Tephra emission was related with clearing (December 1994 to March 1995), and clogging of the vent (May 1995 to February 1996), until a larger new ascending batch was able to clear its way to the surface (March 1996). After April 1996, dome formation and explosive destruction were related to individual small ascending magma batches. Tephra from December 1994 to early March 1996 was made up mostly of andesitic lithic clasts and plagioclase and pyroxene crystals with minor amounts of accidental and accessory minerals. In March 1996, prior to dome formation, glass was also detected. Afterwards, ash components were

  13. Volcanoes

    Institute of Scientific and Technical Information of China (English)

    2007-01-01

    In the past thousand years,volcanoes have claimed more than 300,000 lives. Volcanology is ayoung and dangerous science that helps us against the power of the Earth itself.We live on a fiery planet. Nearly 2000 miles beneath our feet, the Earth's inner core reachestemperatures of 12,000 degrees Fahrenheit. Molten rock or magma, rises to the earth's surface. Acold, rigid crust fractured into some twenty plates. When magma breaks through crust it becomes

  14. Analysis of the seismicity activity of the volcano Ceboruco, Nayarit, Mexico

    Science.gov (United States)

    Rodriguez-Ayala, N. A.; Nunez-Cornu, F. J.; Escudero, C. R.; Zamora-Camacho, A.; Gomez, A.

    2014-12-01

    The Ceboruco is a stratovolcano is located in the state of Nayarit,Mexico (104 ° 30'31 .25 "W, 21 ° 7'28 .35" N, 2280msnm). This is an volcano active, as part of the Trans-Mexican Volcanic Belt, Nelson (1986) reports that it has had activity during the last 1000 years has averaged eruptions every 125 years or so, having last erupted in 1870, currently has fumarolic activity. In the past 20 years there has been an increase in the population and socio-economic activities around the volcano (Suárez Plascencia, 2013); which reason the Ceboruco study has become a necessity in several ways. Recent investigations of seismicity (Rodríguez Uribe et al., 2013) have classified the earthquakes in four families Ceboruco considering the waveform and spectral features. We present analysis included 57 days of seismicity from March to October 2012, in the period we located 97 events with arrivals of P and S waves clear, registered in at least three seasons, three components of the temporal network Ceboruco volcano.

  15. Monitoring Monitoring Evolving Activity at Popocatepetl Volcano, Mexico, 2000-2001

    Science.gov (United States)

    Martin-DelPozzo, A.; Aceves, F.; Bonifaz, R.; Humberto, S.

    2001-12-01

    After 6 years of small eruptions, activity at Mexico's 5,452m high Popocatepetl Volcano in central Mexico, peaked in the December 2000-January 2001 eruptions. Precursors included an important increase in seismicity as well as in magmatic components of spring water and small scale deformation which resulted in growth of a new crater dome from January 16 on. Evacuation of the towns nearest the volcano over Christmas was decided because of the possibility of pyroclastic flows. During the previous years, crater dome growth, contraction and explosive clearing has dominated the activity. The January 22 eruption produced an eruption column approximately 17km high with associated pyroclastic flows. Ejecta was composed of both basic and evolved scoria and pumice and dome lithics. A large proportion of the juvenile material was intermediate between these 2 endmenbers (59-63percent SiO2 and 3.5 to 5.5 MgO) consistent with a small basic pulse entering a more evolved larger batch of magma. The January eruption left a large pit which has been partially infilled by another crater dome this August 2001.

  16. Analyzing changes in the beef cattle ranching communities of acatic and tepatitlan de morelos, jalisco, Mexico related to land cover and climate variability

    Science.gov (United States)

    Trevino-Pena, Melva B.

    The impacts of climate change on the environment at the global scale can be determined through the use of large-scale circulation models; however, the results from these models are difficult to interpret at the regional or local levels. Regional vulnerability analyses consider the knowledge of locals, which may provide insight into the effects of climate variability on the environment at smaller scales, and most importantly, the effects that these developments are having on society. The objective of this research was to analyze the vulnerability to climate variability of the beef cattle ranching communities of the municipalities of Acatic and of Tepatitlan de Morelos, Jalisco, Mexico. These municipalities are found in a region of the state referred to as "Los Altos". The economy of Los Altos largely relies on agricultural and farming practices; these sectors provide the largest source of employment in the area. In the two municipalities that comprise the study area, the beef cattle industry is one of the strongest economic activities. Climate variability poses great threat on these communities because the main economic activities of the region are highly dependent on natural resources. To have a better understanding of the human-environment interactions in this region, remote sensing methods were applied. Three Landsat Thematic Mapper (TM) images (years: 1985, 1993 and 2000) were employed to generate land use and land cover classification maps of the study area; these maps were then subjected to a change detections analysis. Some of the land use and land cover categories experienced more change than others; among those was the category of water, shrub land and crop land. The area covered by water nearly doubled from 1985 to 1993 and then nearly decreased by half by the year 2000. From 1985 to 1993, here was a decrease in the shrub land of about 1200 ha and concurrently an increase in the crop land of about 1400 ha. From 1993 to 2000 there was an increase in the

  17. Pleistocene cohesive debris flows at Nevado de Toluca Volcano, central Mexico

    Science.gov (United States)

    Capra, L.; Macías, J. L.

    2000-10-01

    During the Pleistocene, intense hydrothermal alteration promoted a flank failure of the southern portion of Nevado de Toluca volcano. This event produced a debris avalanche that transformed into a cohesive debris flow (Pilcaya deposit) owing to water saturation and weakness of the altered pre-avalanche rocks. The Pilcaya debris flow traveled along a narrow tectonic depression up to a distance of 40 km and then spread over a flat plain reaching up to 55 km from the volcano summit. This transition zone corresponds with a sudden break in slope from 5 to 0.5° that caused a rapid reduction in velocity and thickening of the flow that consequently reduced its competence to transport large particles. The resulting deposit thickens from 15 to 40 m, and contains boulders up to 15 m in diameter that form hummocky morphology close to the transitional zone. Sometime after the emplacement of the Pilcaya debris flow, heavy rains and superficial drainage contributed to remobilize the upper portions of the deposit causing two secondary lahars. These debris flows called El Mogote, traveled up to 75 km from the volcano. The edifice collapse generated lahars with a total volume of 2.8 km 3 that devastated an approximate area of 250 km 2. The area versus volume plot for both deposits shows that the magnitude of the event is comparable to other cohesive debris flows such as the Teteltzingo lahar (Pico de Orizaba, Mexico) and the Osceola mudflow (Mount Rainier, Wa). The Pilcaya debris flow represents additional evidence of debris flow transformed from a flank failure, a potentially devastating phenomenon that could threaten distant areas from the volcano previously considered without risk.

  18. Gravity Survey at the Ceboruco Volcano Area (Nayarit, Mexico): a 3-D Model of the Subsurface Structure

    Science.gov (United States)

    Fernandez-Cordoba, Jhonattan; Zamora-Camacho, Araceli; Espindola, Juan Manuel

    2017-07-01

    Ceboruco volcano (-104°30', 21°7', 2150 m asl) is located in the western portion of the trans-Mexican volcanic belt and NW extreme of the Tepic-Zacoalco rift zone, a structure composed of a series of NNW-trending en echelon fault-bounded basins constituting the NE boundary between the north-American plate and the Jalisco block (JB). Ceboruco experimented a Plinian eruption about 1000 years ago and several more of different styles afterward; the last one in 1870 CE. This volcano poses a significant risk because of the relatively large population in its surroundings. Ceboruco has been studied by mostly from the point of view of petrology, geochemistry, and physical volcanology; however, no geophysical studies about its internal structure have been published. In this paper, we present the results of a gravimetric survey carried out in its surroundings and a model of the internal structure obtained from inversion of the data. The Ceboruco area is characterized by a negative Bouguer anomaly spanning the volcanic structure. The probable causative body modeled with the data of the survey is located about 1 km below mean sea level and has a volume of 163 km3. We propose that this body is the magma chamber from where the products of its eruptions in the last 1000 years ensued.

  19. Geochemistry and Stable Isotopes of Tacana Volcano-Hydrothermal System, Mexico-Guatemala

    Science.gov (United States)

    Rouwet, D. /; Inguaggiato, S.; Taran, Y. /; Varley, N. /

    2003-12-01

    Tacana volcano (4100 m.s.n.m.), situated on the border between Chiapas (Mexico) and Guatemala is considered an active volcano. In May 1986, after a minor phreatic explosion, a fumarole field was formed at an altitude between 3200 and 3600 m.a.s.l. Around the volcano, at altitudes between 1500 and 2000 m.a.s.l., exist several thermal springs, with temperatures up to 63 degrees C. Incomplete chemical composition of the Agua Caliente thermal waters in the period 1986-1993 were presented by Medina (1986), De la Cruz-Reyna et al. (1989) and Armienta and De la Cruz-Reyna (1995), a chemical analysis of fumarole gases were published by Martini et al. (1986). This study presents the first series of isotope data of water and gases: hydrogen, oxygen, carbon and helium. Data on gas and water chemistry of several thermal spring waters and gases are presented in more detail than ever. Hydrogen and oxygen isotopes of Tacana thermal spring waters show that meteoric water is the main contribution for the thermal waters. Cation geothermometry of the spring waters confirm these meteoric contribution, as all waters are immature in a dynamic system of water-rock interaction with a constant infiltration of fresh meteoric waters (precipitation of 6000 mm per year). The relatively high bicarbonate (up to 1100 ppm) and sulphate (up to 1200 ppm) concentrations in the thermal waters suggest an important degassing up to 2500 m below the volcano summit, which indicates the presence of a extended and complex volcano-hydrothermal system. Helium isotopes of free and dissolved gases confirm the existence of a magmatic contribution, so as for fumarole gases (6.6 R/Ra) as for gases sampled at the thermal springs (5.7-6.2 R/Ra for free gases and between 0.50 and 5.55 R/Ra for dissolved gases). These values are typical for gases liberated at volcanoes in clasic volcanic arcs. The lower values for the dissolved He is probably due to an interaction with the granitic basement, which can be found at

  20. A Study of the Source Processes of Colima Volcano Explosions

    Science.gov (United States)

    Nunez-Cornu, F. J.; Vargas-Bracamontes, D.; Sanchez, J. J.; Suarez-Plascencia, C.

    2007-12-01

    Colima volcano, considered as Mexico's most active volcano, has presented several intermittent effusive and explosive phases in recent years. During 2005, a sequence of explosive events with VEI less than or equal to 3 occurred. This activity presented the most intense explosions since the seismic network was deployed. Many of the explosive events were recorded by the digital three-component seismic stations operated by the University of Guadalajara and Jalisco State Civil Defense. These signals were recorded not only by stations located on the volcanic edifice, but also by stations on the northern coast of Jalisco (MCUJ, BSSJ) and Ceboruco Volcano at 184, 182 and 200 km distance, respectively. A study of these signals will be presented. Each explosion was preceded by a seismic event. Nevertheless, the located earthquakes preceding the explosions did not show a common source under the volcano structure, which suggests the existence of a complex structure with possibly more than one conduit, this is also confirmed from a first motion analysis for station F03J, located 12 km at north of the volcano. From analysis of the first ten seconds of the seismic signal on F03J using different representations of the seismic signals, such as waveforms, spectra, time-frequency and time-scale analysis, it is suggested that the source processes are non-stationary, implying that for the case of this period, a general model of the source process of the Colima volcano explosions can not be formulated. The size of the events is evaluated using different criteria. A clear relation between the magnitude of the seismic signals and the amplitude of the sonic and infrasonic waves was not observed.

  1. Faults and volcanoes: Main volcanic structures in the Acambay Graben, Mexico

    Science.gov (United States)

    Aguirre-Diaz, G. J.; Pedrazzi, D.; Suñe-Puchol, I.; Lacan, P.

    2016-12-01

    The Mexican Volcanic Belt (MVB) province is best known by the major stratovolcanoes, such as Popocatepetl and Colima, but most of the province is formed by modest size stratovolcanoes and monogenetic cones. Regional fault systems were developed together with the building of the volcanic province; the most notorious one is Chapala-Tula Fault System (CTFS), which runs parallel to the central sector of the MVB, and thus it is also referred to as the Intra-Arc fault system. Acambay graben (AG) is part of this central system. It is a 20 x 70 km depression located 100 km to the NW of Mexico City, at the easternmost end of the E-W trending CTFS, and was formed as the result of NS to NE oriented extension. Seismically active normal faults, such as the Acambay-Tixmadejé fault, with a mB =7 earthquake in 1912, delimit the AG. The graben includes several volcanic structures and associated deposits ranging in age from Miocene to 3 ka. The main structures are two stratovolcanoes, Altamirano (900 m high) and Temascalcingo (800 m high). There are also several Miocene-Pliocene lava domes, and Quaternary small cinder cones and shield volcanoes. Faulting of the Acambay graben affects all these volcanic forms, but depending on their ages, the volcanoes are cut by several faults or by a few. That is the case of Altamirano and Temascalcingo volcanoes, where the former is almost unaffected whereas the latter is highly dissected by faults. Altamirano is younger than Temascalcingo; youngest pyroclastic deposits from Altamirano are dated at 12-3 ka, and those from Temascalcingo at 40-25 ka (radiocarbon ages). The relatively young ages found in volcanic deposits within the Acambay graben raise the volcanic danger level in this area, originally marked as an inactive volcanic zone, but activity could restart at any time. Supported by DGAPA-PAPIIT-UNAM grant IN-104615.

  2. Late Pleistocene flank collapse of Zempoala volcano (Central Mexico) and the role of fault reactivation

    Science.gov (United States)

    Arce, José Luis; Macías, Rodolfo; García Palomo, Armando; Capra, Lucia; Macías, José Luis; Layer, Paul; Rueda, Hernando

    2008-11-01

    Zempoala is an extinct Pleistocene (˜ 0.7-0.8 Ma) stratovolcano that together with La Corona volcano (˜ 0.9 Ma) forms the southern end of the Sierra de las Cruces volcanic range, Central Mexico. The volcano consists of andesitic and dacitic lava flows and domes, as well as pyroclastic and epiclastic sequences, and has had a complex history with several flank collapses. One of these collapses occurred during the late Pleistocene on the S-SE flank of the volcano and produced the Zempoala debris avalanche deposit. This collapse could have been triggered by the reactivation of two normal fault systems (E-W and NE-SW), although magmatic activity cannot be absolutely excluded. The debris avalanche traveled 60 km to the south, covers an area of 600 km 2 and has a total volume of 6 km 3, with a calculated Heim coefficient (H/L) of 0.03. Based on the textural characteristics of the deposit we recognized three zones: proximal, axial, and lateral distal zone. The proximal zone consists of debris avalanche blocks that develop a hummocky topography; the axial zone corresponds with the main debris avalanche deposit made of large clasts set in a sandy matrix, which transformed to a debris flow in the lateral distal portion. The deposit is heterolithologic in composition, with dacitic and andesitic fragments from the old edifice that decrease in volume as bulking of exotic clasts from the substratum increase. Several cities (Cuernavaca, Jojutla de Juárez, Alpuyeca) with associated industrial, agricultural, and tourism activities have been built on the deposit, which pose in evidence the possible impact in case of a new event with such characteristics, since the area is still tectonically active.

  3. Pleistocene to recent alkalic volcanism in the region of Sanganguey volcano, Nayarit, Mexico

    Science.gov (United States)

    Nelson, S. A.; Carmichael, I. S. E.

    1984-12-01

    Forty five cinder cones and associated lava flows have erupted within the last 300,000 years along five parallel lines through the calc-alkaline volcano, Sanganguey, in the northwestern segment of the Mexican Volcanic Belt. Lavas erupted from these cinder cones include ne- and hynormative alkali basalts, hawaiites, mugearites, and benmoreites. It is unusual that this suite has erupted in a calc-aikaline volcanic belt where volcanoes in the vicinity have been erupting calc-alkaline andesites, dacites and rhyodacites. Incompatible trace elements such Ba, Rb, Sr, and LREEs show little change with decreasing Mg, Ni, and Cr in the series alkali basalt to hawaiite, suggesting that simple crystal fractionation of observed phenocrysts has not been the dominant process in the derivation of the hawaiites from the alkali basalts. Petrographic evidence of magma mixing along with observed variation of trace element abundances suggests that the alkali basalts might represent mixtures of primitive magma with more evolved compositions. Crystal fractionation is capable of explaining major and most trace element trends in the series hawaiite — mugearite — benmoreite. However, such a process could only occur at pressure because of the requirement that clinopyroxene be a major crystallizing phase. The anomolous association of alkaline magmatism contemporaneously with calc-alkaline magmatism is probably related to the complex tectonic history associated with the rearrangement of plate boundaries in the vicinity of western Mexico.

  4. Serological follow-up of Trypanosoma cruzi infection from 1987 to 1994 in 32 counties of the State of Jalisco, Mexico: preliminary report Seguimento sorológico de infecção por Trypanosoma cruzi entre 1987 e 1994 em 32 municípios do Estado de Jalisco, México: relatório preliminar

    Directory of Open Access Journals (Sweden)

    Francisco Trujillo-Contreras

    1995-09-01

    Full Text Available In 1987 the University of Guadalajara performed a seroepidemiological survey on the prevalence of Chagas’ disease in the 124 counties of the State of Jalisco, Mexico, arriving at a rate of 21.6 per 100 inhabitants. From December 1993 to June 1994, we studied 2238 individuals from 32 rural counties in this State. Of these, we found 276 positives (12.33% and 1962 negatives (87.66%. Nevertheless, the series of serological differences found are very striking, since out of the 655 individuals that were seropositive in 1987, we noted that 276 individuals remained positive, while 50 individuals (7.63% became negative. There were no flaws in the laboratory techniques. We believe that either the immune response of Mexicans is different or that the virulence of the Mexican strains of Trypanosoma cruzi may be not as great as that in the South America countries.Em 1987, a Universidade de Guadalajara realizou um inquérito sorológico sobre a prevalência da doença de Chagas em 124 municípios do Estado de Jalisco, México, chegando a uma taxa de 21.6 por 100 habitantes. Entre dezembro de 1993 a junho de 1994, os autores estudaram 2238 indivíduos de 32 municípios da área rural desse mesmo estado. Encontraram 276 positivos (12.33% a 1962 negativos­ (87.66%. Entretanto, as séries de diferenças sorológicas foram muito marcantes, uma vez que dos 655 indivíduos que testaram positivos em 1987, 276 permaneceram positivos, enquanto 50 (7.63% tornaram-se soro­negativos. Não houve falha de técnica laboratorial. Os autores acreditam que, ou a resposta imune dos mexicanos é diferente, ou então, que a virulência das cepas mexicanas de Trypanosoma cruzi não é tão intensa quanto aquela encontrada em países sul-americanos.

  5. Observed inflation-deflation cycles at Popocatepetl volcano using tiltmeters and its possible correlation with regional seismic activity in Mexico

    Science.gov (United States)

    Contreras Ruiz Esparza, M. G., Sr.; Jimenez Velazquez, J. C., Sr.; Valdes Gonzalez, C. M., Sr.; Reyes Pimentel, T. A.; Galaviz Alonso, S. A.

    2014-12-01

    Popocatepetl, the smoking mountain, is a stratovolcano located in central Mexico with an elevation of 5450 masl. The active volcano, close to some of the largest urban centers in Mexico - 60 km and 30 km far from Mexico City and Puebla, respectively - poses a high hazard to an estimated population of 500 thousand people living in the vicinity of the edifice. Accordingly, in July 1994 the Popocatepetl Volcanological Observatory (POVO) was established. The observatory is operated and supported by the National Center for Disaster Prevention of Mexico (CENAPRED), and is equipped to fully monitor different aspects of the volcanic activity. Among the instruments deployed, we use in this investigation two tiltmometers and broad-band seismometers at two sites (Chipiquixtle and Encinos), which send the information gathered continuously to Mexico City.In this research, we study the characteristics of the tiltmeters signals minutes after the occurrence of certain earthquakes. The Popocatepetl volcano starts inflation-deflation cycles due to the ground motion generated by events located at certain regions. We present the analysis of the tiltmeters and seismic signals of all the earthquakes (Mw>5) occurred from January 2013 to June 2014, recorded at Chipiquixtle and Encinos stations. First, we measured the maximum tilt variation after each earthquake. Next, we apply a band-pass filter for different frequency ranges to the seismic signals of the two seismic stations, and estimated the total energy of the strong motion phase of the seismic record. Finally, we compared both measurements and observed that the maximum tilt variations were occurring when the maximum total energy of the seismic signals were in a specific frequency range. We also observed that the earthquake records that have the maximum total energy in that frequency range were the ones with a epicentral location south-east of the volcano. We conclude that our observations can be used set the ground for an early

  6. Field Courses for Volcanic Hazards Mapping at Parícutinand Jorullo Volcanoes (Mexico)

    Science.gov (United States)

    Victoria Morales, A.; Delgado Granados, H.; Roberge, J.; Farraz Montes, I. A.; Linares López, C.

    2007-05-01

    During the last decades, Mexico has suffered several geologic phenomena-related disasters. The eruption of El Chichón volcano in 1982 killed >2000 people and left a large number of homeless populations and severe economic damages. The best way to avoid and mitigate disasters and their effects is by making geologic hazards maps. In volcanic areas these maps should show in a simplified fashion, but based on the largest geologic background possible, the probable (or likely) distribution in time and space of the products related to a variety of volcanic processes and events, according to likely magnitude scenarios documented on actual events at a particular volcano or a different one with similar features to the volcano used for calibration and weighing geologic background. Construction of hazards maps requires compilation and acquisition of a large amount of geological data in order to obtain the physical parameters needed to calibrate and perform controlled simulation of volcanic events under different magnitude-scenarios in order to establish forecasts. These forecasts are needed by the authorities to plan human settlements, infrastructure, and economic development. The problem is that needs are overwhelmingly faster than the adjustments of university programs to include courses. At the Earth Science División of the Faculty of Engineering at the Universidad Nacional Autónoma de México, the students have a good background that permits to learn the methodologies for hazards map construction but no courses on hazards evaluations. Therefore, under the support of the university's Program to Support Innovation and Improvement of Teaching (PAPIME, Programa de Apoyo para la Innovación y Mejoramiento de la Enseñanza) a series of field-based intensive courses allow the Earth science students to learn what kind of data to acquire, how to record, and process in order to carry out hazards evaluations. This training ends with hazards maps that can be used immediately by the

  7. Age and archaeological implications of Xitle volcano, southwestern Basin of Mexico-City

    Science.gov (United States)

    Siebe, C.

    2000-12-01

    The Pedregal lavas are fresh, well-exposed basaltic flows erupted from the Xitle scoria-and-cinder cone in the southwestern part of the Basin of Mexico. These lavas cover an area of 70 km 2 and were emplaced over pyramids and other buildings (e.g. Cuicuilco and Copilco archaeological sites). Today, a part of Mexico-City (including the National University) is built on the flows. Initial strombolian activity produced an ash fallout layer, which was immediately followed by effusive emplacement of lava flows. The Xitle cone grew on the north-facing slope of Ajusco volcano, and lava flowed down to the N-NE until it reached the basin floor. More than 30 radiocarbon dates have been obtained by several workers on charcoal samples from beneath the lava, and several ages for the eruption have been proposed from these dates. Most dated samples were not directly produced by Xitle's eruption but instead are artifacts of human activity that predates the eruption. Thus, these ages (mostly about 2000 BP) are older than the eruption. A new age of 1670±35 years BP (AD 245-315) obtained on charcoal samples collected just beneath the lavas is favored for the Xitle eruption. These samples originated by ignition of vegetation during the emplacement of hot scoriaceous tephra. The new age is within the Classic period of Mesoamerican archaeology, whereas the earlier reported ages are at the end of the Preclassic. The new age carries important implications for the timing of population shifts within the Basin of Mexico.

  8. Colimaite, K3VS4 - a new potassium-vanadium sulfide mineral from the Colima volcano, State of Colima (Mexico)

    OpenAIRE

    Mikhail Ostrooumov; Yuri Taran; María Arellano-Jiménez; Alfredo Ponce; José Reyes-Gasga

    2009-01-01

    Colimaite, K3VS4, has been discovered in the active fumaroles of the Colima volcano crater, Mexico. The mineral is named colimaite after the locality, which, at the same time, is the current active volcanic crater and the name of the State of Colima (Mexico). Colimaite is the naturally occurring analog of synthetic K3VS4. The mineral formed as a sublimate from the volcanic gases and is associated with cristobalite, arcanite, thenardite, barite and native gold. Colimaite occurs in hedgehog -l...

  9. The ash-fall hazard from a Plinian eruption at Colima Volcano, Mexico

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    Rita Fonseca

    2010-06-01

    Full Text Available The historical eruptive activity at Colima Volcano has been characterized by Strombolian and Merapi type eruptions and Vulcanian explosions associated with dome growth, which have ended in a Plinian eruption about every 100 years. The situation now prevailing at Colima Volcano is similar to that which preceded these explosive eruptions, when a dome fills the crater. This study proposes seven scenarios for the ash-fall from a Plinian eruption, based on historical eruptive activity, isopach thickness from the 1913 Plinian eruption, land use, socioeconomic data, and a 15-year statistical wind study realized with daily radiosonde data grouped according to four altitudinal levels: 4,000-9,000 (I; 9,000-14,000 (II; 14,000-17,000 (III and 17,000-28,000 (IV m a.s.l., based on common wind speeds and directions. We have integrated the wind distribution at level IV and estimated the ash dispersion for a Plinian eruption. From January to March, the main impact would be towards the northeast, in April and in October, towards the east, in May, towards the north-northeast or north-northwest, from June to August, towards the northwest, in September, towards the west, and in November and December, towards the west-southwest. The fallout would damage the coniferous forests of the Colima National Park, two lagoons and three lakes. More than 30 million people living in Guadalajara, Mexico City, Leon and Colima would suffer eye, respiratory and skin problems. The proximal areas, such as Ciudad Guzman, would be subject to roof collapsing and communication problems. The agricultural and livestock sectors would suffer severe financial losses. The Queseria sugar mill, the Atenquique paper mill, and the cement plants in Zapotiltic would halt work due to chimney obstruction and machinery abrasion. Four thermoelectric plants, twenty airports and four commercial ports would be affected if the eruption occurs in summer.

  10. Geophysical characterization of hydrothermal systems and intrusive bodies, El Chichón volcano (Mexico)

    Science.gov (United States)

    Jutzeler, Martin; Varley, Nick; Roach, Michael

    2011-04-01

    The 1982 explosive eruptions of El Chichón volcano (Chiapas, Mexico) destroyed the inner dome and created a 1-km-wide and 180-m-deep crater within the somma crater. A shallow hydrothermal system was exposed to the surface of the new crater floor and is characterized by an acid crater lake, a geyser-like Cl-rich spring (soap pool), and numerous fumarole fields. Multiple geophysical surveys were performed to define the internal structure of the volcanic edifice and its hydrothermal system. We carried out a high-resolution ground-based geomagnetic survey in the 1982 crater and its surroundings and 38 very low frequency (VLF) transects around the crater lake. A 3-D inversion of the ground-based magnetic data set highlighted three high-susceptibility isosurfaces, interpreted as highly magnetized bodies beneath the 1982 crater floor. Inversion of a digitized regional aeromagnetic map highlighted four major deeply rooted cryptodomes, corresponding to major topographic highs and massive lava dome outcrops outside and on the somma rim. The intracrater magnetic bodies correspond closely to the active hydrothermal vents and their modeled maximum basal depth matches the elevation of the springs on the flanks of the volcano. Position, dip, and vertical extent of active and extinct hydrothermal vents identified by VLF-EM surveys match the magnetic data set. We interpret the shallow lake spring hydrothermal system to be mostly associated with buried remnants of the 550 BP dome, but the Cl-rich soap pool may be connected to a small intrusion emplaced at shallow depth during the 1982 eruption.

  11. Geologic Map of The Volcanoes Quadrangle, Bernalillo and Sandoval Counties, New Mexico

    Science.gov (United States)

    Thompson, Ren A.; Shroba, Ralph R.; Menges, Christopher M.; Schmidt, Dwight L.; Personius, Stephen F.; Brandt, Theodore R.

    2009-01-01

    This geologic map, in support of the U.S. Geological Survey Middle Rio Grande Basin Geologic Mapping Project, shows the spatial distribution of surficial deposits, lava flows, and related sediments of the Albuquerque volcanoes, upper Santa Fe Group sediments, faults, and fault-related structural features. These deposits are on, along, and beneath the Llano de Albuquerque (West Mesa) west of Albuquerque, New Mexico. Some of these deposits are in the western part of Petroglyph National Monument. Artificial fill deposits are mapped chiefly beneath and near the City of Albuquerque Soil Amendment Facility and the Double Eagle II Airport. Alluvial deposits were mapped in and along stream channels, beneath terrace surfaces, and on the Llano de Albuquerque and its adjacent hill slopes. Deposits composed of alluvium and colluvium are also mapped on hill slopes. Wedge-shaped deposits composed chiefly of sandy sheetwash deposits, eolian sand, and intercalated calcic soils have formed on the downthrown-sides of faults. Deposits of active and inactive eolian sand and sandy sheetwash deposits mantle the Llano de Albuquerque. Lava flows and related sediments of the Albuquerque volcanoes were mapped near the southeast corner of the map area. They include eleven young lava flow units and, where discernable, associated vent and near-vent pyroclastic deposits associated with cinder cones. Upper Santa Fe Group sediments are chiefly fluvial in origin, and are well exposed near the western boundary of the map area. From youngest to oldest they include a gravel unit, pebbly sand unit, tan sand and mud unit, tan sand unit, tan sand and clay unit, and silty sand unit. Undivided upper Santa Fe Group sediments are mapped in the eastern part of the map area. Faults were identified on the basis of surface expression determined from field mapping and interpretation of aeromagnetic data where concealed beneath surficial deposits. Fault-related structural features are exposed and were mapped near

  12. Bacterial diversity in fumarole environments of the Paricutín volcano, Michoacán (Mexico).

    Science.gov (United States)

    Medrano-Santillana, Miguel; Souza-Brito, Elcia Margaret; Duran, Robert; Gutierrez-Corona, Felix; Reyna-López, Georgina Elena

    2017-05-01

    Active volcanoes are among the most extreme environments on Earth. The extreme temperatures, presence of toxic heavy metals and low nutrient bioavailability favor the development of extremophiles. We characterized the physical-chemical parameters of and bacterial communities (T-RFLP and 16S rRNA gene libraries) inhabiting fumarole niches of the Paricutín volcano located in Michoacán (Mexico). This volcano, which surged in 1943, is one of the youngest volcanoes on Earth and the microbial diversity in this area is yet to be characterized. The sampling stations were characterized in a pH range from 5.34 to 7.89 and showed different temperatures (soil, 27-87 °C; air, 13.6-56 °C) with high concentrations of metals such as iron and arsenic. The most abundant bacterial populations, confirmed by T-RFLP and 16S rRNA gene libraries, were related to members of Firmicutes and Proteobacteria phyla including sequences associated with thermophiles and sulfate reducing bacteria. Overall, the Paricutín volcano showed low bacterial diversity and its prokaryotic diversity was characterized by the impossibility of amplifying Archaea-related sequences.

  13. Palaeomagnetic dating of two recent lava flows from Ceboruco volcano, western Mexico

    Science.gov (United States)

    Böhnel, Harald; Pavón-Carrasco, Francisco Javier; Sieron, Katrin; Mahgoub, Ahmed Nasser

    2016-11-01

    Two lava flows from the Ceboruco volcano in west-central Mexico were sampled for palaeomagnetic dating. The younger one was emitted in 1870 and used to validate the method, while the older one known as Ceboruco flow is of unknown age but probably younger than ˜1005 AD and older than 1528 AD. Each flow was sampled in at least four sites, in order to unravel between site variations. For the 1870 flow, between site differences were notable and additionally post-cooling block movements were important; therefore, two sites had to be rejected. Three sites from the vent area and one at the tip of the 1870 flow provided well-constrained directions. This is also true for Ceboruco lava flow, and overall mean directions and palaeointensities were then used for palaeomagnetic dating applying the Matlab tool archaeo_dating and the global palaeosecular variation model SHA.DIF.14k. For the 1870 lava flow, the dating resulted in an age ranging between 1755 and 1871 AD (95 per cent probability level), which includes the real emplacement age. In addition, the Ceboruco lava flow was dated between 1000 and 1134 AD, which is close to the large plinian Jala eruption producing the crater of Ceboruco volcano around 1005 AD. This age is older than previously assumed and suggests an emplacement only shortly after the Jala eruption. As this lava flow is considered to be the youngest one of seven post-Jala lava flows, the age also defines a period of inactivity of Ceboruco volcano of about 730-860 yr before the historic 1870 eruption. Future volcanic hazard analysis will have to take into account this result. Our work also shows that multiple sampling of single lava flows is important to obtain a reliable mean direction. Sampling sites have to be carefully selected so that they represent un-tilted parts of the flows. We interpret this to be the case for the Ceboruco lava flow, while three of the six sites of the 1870 lava flow may have been partly or completely affected by movements after

  14. Long term storage of explosively erupted magma at Nevado de Toluca volcano, Mexico

    Science.gov (United States)

    Arce, J. L.; Gardner, J.; Macias, J. L.

    2007-12-01

    Dacitic magmas production is common in subduction-related volcanoes, occurring in those with a long period of activity as a result of the magmatic evolution. However, in this evolution many factors (i.e. crystal fractionation, assimilation, magma mixing) can interact to produce dacites. Nevado de Toluca volcano (4,680 masl; 19°09'N; 99°45'W) Central Mexico has recorded a long period of time producing dacites explosively, at least during 42 ka of activity, involving several km3 of magma, with two important Plinian-type eruptions occurred at ~21.7 ka (Lower Toluca Pumice) and ~10.5 ka (Upper Toluca Pumice). Questions like, what was the mechanism responsible to produce voluminous dacitic magma and how the volatiles and pressure changed in the Nevado de Toluca system, remain without answers. Dacites from the Lower Toluca Pumice (LTP) contain plagioclase, amphibole, iron-titanium oxides, and minor resorbed biotite, set in a glassy-vesicular matrix and the Upper Toluca Pumice (UTP) dacites contain the same mineral phases plus orthopyroxene. Ilmenite- ulvospinel geothermometry yielded a temperature of ~860°C for the LTP dacite, a little hotter than the UTP (~ 840°C). Based on hydrothermal experiments data, amphibole is stable above 100 MPa under 900°C, while plagioclase crystallizes up to 250-100 MPa at temperatures of 850-900°C. Pyroxene occurs only at pressures of 200-100 MPa with its respective temperatures of 825-900°C. Water contents in the LTP magma (2-3.5 wt %) are similar to that calculated for the UTP magma (1.3-3.6 wt %). So, there are only small changes in temperature and pressure from ~21.7 ka to 10.5 ka. It is noteworthy that orthopyroxene is absent in the LTP, however reaction-rimmed biotite (probably xenocrystic) is commonly observed in all dacites. Hence, almost all dacitic magmas seem to be stored at relatively similar pressures, water contents, and temperatures. All of these data could suggest repetitive basic magma injections producing the

  15. Structural pattern at the northwestern sector of the Tepic-Zacoalco rift and tectonic implications for the Jalisco block, western Mexico

    Science.gov (United States)

    Urrutia-Fucugauchi, Jaime; González-Morán, Tomás

    2006-10-01

    Analysis of the aeromagnetic anomalies over the northwestern sector of the Tepic-Zacoalco rift documents a NE-SW pattern of lineaments that are perpendicular to the inferred NW-SE boundary between the Jalisco block and the Sierra Madre Occidental. The boundary lies within the central sector of the Tepic-Zacoalco rift immediately north of the Ceboruco and Tepetiltic stratovolcanoes and extends up to the San Juan stratovolcano, where it intersects the NE-SW magnetic anomaly lineament that runs toward the Pacific coast (which intersects two volcanic centers). This N35°E lineament separates the central rift zone of low amplitude mainly negative anomalies (except those positive anomalies over the stratovolcanoes) from the zone to the north and west characterized by high amplitude positive long wavelength anomalies. The NE-SW lineament is parallel to the western sector of the Ameca graben and the offshore Bahia de Banderas graben and to the structural features of the Punta Mita peninsula at the Pacific coast, and thus seems to form part of a regional NE-SW pattern oblique to the proposed westward or northwestward motion of the Jalisco block. The orientation of this regional structural pattern at the northern end of the Tepic-Zacoalco rift seems consistent with proposed dominant SW-directed extension along the rift during the Pliocene and Quaternary, rather than with NW-SE lateral strike-slip faulting. The orthogonal pattern that characterizes the northernmost boundary of the Tepic-Zacoalco rift is oblique to the pattern observed in the Grande de Santiago river (which conforms the northern limit of the rift) and for the central-eastern sectors of the Ameca graben (south of the rift). This spatial arrangement of major lineaments and structural elements points to a complex tectonic history for the region that includes the rifting of the Gulf of California and margin deformation due to plate convergence and kinematic re-organization events, and which may have resulted in

  16. The ~ 2000 yr BP Jumento volcano, one of the youngest edifices of the Chichinautzin Volcanic Field, Central Mexico

    Science.gov (United States)

    Arce, J. L.; Muñoz-Salinas, E.; Castillo, M.; Salinas, I.

    2015-12-01

    The Chichinautzin Volcanic Field is situated at the southern limit of the Basin of Mexico and the Metropolitan area of Mexico City, the third most populated city around the world. The Chichinautzin Volcanic field holds more than 220 monogenetic volcanoes. Xitle is the youngest of these with an estimated age of 1.6 ky BP. Xitle's eruptive activity took place during the Mesoamerican Mexican Pre-classic period and is related to the destruction of Cuicuilco Archaeological Site, the oldest civilization known in Central Mexico. However, there are still several regional cones that have not been dated. Based on 14C ages, stratigraphic and geomorphologic criteria, we conclude that the Jumento volcano, located to the west of Xitle, is one of the youngest cones of the Chichinautzin Volcanic Field. The Jumento volcano has a basaltic andesite composition, and its eruptive activity was initially hydromagmatic, followed by Strombolian and finally effusive events occurred recorded through: (1) a sequence of hydromagmatic pyroclastic surges and ashfall layers emplaced at a radius of > 5 km from the crater with charcoal fragments at its base; this activity built the Jumento's cone with slopes of 32°; and (2) lava flows that breached the southern part of the cone and flowed for up to 2.5 km from the vent. The resulting 14C ages for this volcano yielded a maximum age of ~ 2 ky BP. Morphometric analysis indicates that the state of degradation of Jumento cone is similar to the Xitle, suggesting that the Jumento could be in the state of degradation of a volcanic structure of similar age or younger adding credence to the probable radiocarbon age of ~ 2 ky BP for the Jumento edifice.

  17. Pre-eruptive conditions of the ~31 ka rhyolitic magma of Tlaloc volcano, Sierra Nevada Volcanic Range, Central Mexico

    Science.gov (United States)

    Macias, J.; Arce, J.; Rueda, H.; Gardner, J.

    2008-12-01

    Tlaloc volcano is located at the northern tip of the Sierra Nevada Volcanic Range in Central Mexico. This Pleistocene to Recent volcanic range consists from north to south of Tlaloc-Telapón-Teyotl-Iztaccíhuatl-and- Popocatépetl volcanoes. While andesitic to barely dacitic volcanism dominates the southern part of the range (i.e. Popocatépetl and Iztaccíhuatl); dacitic and rare rhyolithic volcanism (i.e. Telapón, Tlaloc) dominates the northern end. The known locus of rhyolitic magmatism took place at Tlaloc volcano with a Plinian-Subplinian eruption that occurred 31 ka ago. The eruption emplaced the so-called multilayered fallout and pumiceous pyroclastic flows (~2 km3 DRE). The deposit consists of 95% vol. of juvenile particles (pumice + crystals) and minor altered lithics 5% vol. The mineral association of the pumice fragments (74-76 % wt. SiO2) consists of quartz + plagioclase + sanidine + biotite and rare oxides set in a glassy groundmass with voids. Melt inclusions in quartz phenocrysts suggest that prior to the eruption the rhyolitic contain ~7% of H2O and Toluca volcano (~6 km) some 50 km to the southwest.

  18. Zircon xenocryst resorption and magmatic regrowth at El Chichón Volcano, Chiapas, Mexico

    Science.gov (United States)

    Pack, Brenda; Schmitt, Axel K.; Roberge, Julie; Tenorio, Felipe Garcia; Damiata, Brian N.

    2016-02-01

    El Chichón volcano is the only active volcano located within the Chiapanecan Volcanic Arc in southern Mexico, which lies between the Trans-Mexican Volcanic Belt and the Central American Volcanic Arc. Previous studies have shown that ~ 12 eruptions have occurred at El Chichón within the last 8000 years, forming a complex of lava domes with a central crater and surrounding pyroclastic deposits. Here, we report the discovery of zircon in Holocene El Chichón rocks, which were analyzed by high spatial resolution imaging (color cathodoluminescence CCL) and isotopic (secondary ionization mass spectrometry SIMS) methods to resolve core and rim crystallization ages. Pumice samples from five proximal pyroclastic flow and fall-out deposits were collected based on published stratigraphy. Two of the samples were further (re-)classified by new 14C dates. In addition, we sampled two lavas from the 1982 eruption and from remnants of the older Somma lava complex. Zircon crystals were dated using 230Th/238U disequilibrium (U-Th) and U-Pb geochronology. U-Th zircon ages fall between near eruption ages and ca. 84 ka, with overlapping ages in all samples. By contrast, zircon core U-Pb ages range between ca. 290 Ma and 1.9 Ga. These ages are consistent with xenocrystic origins and their heterogeneity indicates derivation from clastic country rocks. Strong age contrasts between inherited xenocrystic and young magmatic domains in individual zircon crystals are evidence for arrested assimilation of crustal rocks where initially zircon-undersaturated magmas cooled rapidly to form a crystal mush or subsolidus amalgamate as a crustally contaminated boundary layer. This layer contributed zircon crystals to eruptible magma during episodic recharge events followed by partial melt extraction, mixing and homogenization. Zircon overgrowths are significantly older than major minerals whose U-series ages and sharp zonation boundaries suggest crystallization only within a few ka before eruption

  19. La elegibilidad en Jalisco

    Directory of Open Access Journals (Sweden)

    Adrián Joaquín Miranda Camarena

    2011-01-01

    Full Text Available La elegibilidad es un calificativo que denota la posibilidad de ser elegido o electo dentro de una República representativa, democrática y federal; se entiende que existen cargos de elección popular, que cada tres o seis años se deberán elegir mediante elecciones auténticas, libres y periódicas. Tanto a nivel federal como local, la posibilidad de ser votado a cualquiera de los cargos de elección popular está supeditada a los requisitos que enmarcan tanto la Constitución Política de los Estados Unidos Mexicanos como la Constitución Política del Estado de Jalisco.

  20. Instrumental monitoring of lahars for warning purposes: new developments along the Colima Volcano, Mexico

    Science.gov (United States)

    Coviello, Velio; Capra, Lucia; Vázquez, Rosario; Márquez, Víctor H.; Cruz, Sergio

    2017-04-01

    , upstream to downstream. Here we propose a new application and development of this method to early detect and characterize rain-triggered lahars occurring along the Colima Volcano, one of the most active volcanoes in Mexico. Two monitoring stations are installed along the Southwestern flank of the volcano, in the Montegrande and the Lumbre basins. Both sites are equipped with a GVD array and a videocamera. Along the Montegrande ravine is also installed an infrasound sensor while the Lumbre monitoring station integrates a flow stage sensor. The new detection algorithm, currently under testing, is still based on the SNR but detected by two different sensors installed at the same cross-section: a geophone paired with a stage sensor or an infrasound device. Preliminary results show how this can be an effective solution to adopt along channels where is possible to monitor only one cross-section with a heavily instrumented station.

  1. Geothermal exploration results at the Ceboruco volcano, Nayarit State, Mexico; Resultados de la exploracion geotermica en el volcan Ceboruco en el estado de Nayarit, Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Venegas S, Saul [Gerencia de Proyectos Geotermoelectricos de la Comision Federal de Electricidad, Morelia (Mexico)

    1995-05-01

    Since the seventies, in Mexico, the thermal areas census and the geothermal exploration have been carried out by the Geothermal Division of Comision Federal de Electricidad (CFE), including geological, geophysical and geochemical studies and deep exploratory wells, most of them located in the Mexican Volcanic Belt (MVB). In recent years, the exploration has been intensified in the northwestern sector of this regional structure, called the Tepic-Chapala graben, also named by some authors as the Zacoalco-Tepic graben. Due to the large volumes of plio-quaternary volcanism between the tectonic limits of the Sierra Madre Occidental (SMO) and the Jalisco Block (JB), one of the greatest geothermal interest areas is located between the large volcanic apparatus of Ceboruco, Domes of San Pedro, and Tepetiltic, in the State of Nayarit, where CFE has drilled 3 deep exploratory wells. The obtained results, demonstrate that the tectonic limit between SMO and BJ physiographic provinces is much more complex than initially proposed and the hypothetical Quaternary continental rift type structure, could be of Miocene age, because in the three wells discordant lithologic contact was observed between the BJ and the MVB. Also the measured thermal gradient in the Ceboruco No. 1 well (112 degrees celsius to 2800 m), does not correspond the typical heat flow of this type of recent structures. [Espanol] La Gerencia de Proyectos Geotermoelectricos, dependiente de la Comision Federal de Electricidad (CFE), ha realizado desde 1970, el censo de focos termales en el pais. La prospeccion geotermica con base en estudios de geologia, geofisica, geoquimica y construccion tanto de pozos exploratorios profundos como de desarrollo, define a la estructura del Eje Neovolcanico Mexicano (ENM), como la provincia fisiografica con mayores posibilidades para el desarrollo de la energia geotermica. En el sector noroccidental de esta estructura regional, en los limites tectonicos de la Sierra Madre Occidental

  2. Susceptibility mapping in the Río El Estado watershed, Pico de Orizaba volcano, Mexico

    Science.gov (United States)

    Legorreta Paulin, G.; Bursik, M. I.; Lugo Hubp, J.; Paredes Mejía, L.; Aceves Quesada, F.

    2013-12-01

    In volcanic terrains, dormant stratovolcanoes are very common and can trigger landslides and debris flows continually along stream systems, thereby affecting human settlements and economic activities. It is important to assess their potential impact and damage through the use of landslide inventory maps and landslide models. This poster provides an overview of the on-going research project (Grant SEP-CONACYT no 167495) from the Institute of Geography at the National Autonomous University of Mexico (UNAM) that seeks to conduct a multi-temporal landslide inventory and produce a landslide susceptibility map by using Geographic Information Systems (GIS). The Río El Estado watershed on the southwestern flank of Pico de Orizaba volcano, the highest mountain in Mexico, is selected as a study area. The catchment covers 5.2 km2 with elevations ranging from 2676.79 to 4248.2 m a.s.l. and hillslopes between 5° and 56°. The stream system of Río El Estado catchment erodes Tertiary and Quaternary lavas, pyroclastic flows, and fall deposits. The geologic and geomorphologic factors in combination with high seasonal precipitation, high degree of weathering, and steep slopes predispose the study area to landslides. The method encompasses two main levels of analysis to assess landslide susceptibility. The first level builds a historic landslide inventory. In the study area, an inventory of more than 100 landslides was mapped from interpretation of multi-temporal aerial orthophotographs and local field surveys to assess and describe landslide distribution. All landslides were digitized into a GIS, and the spatial geo-database of landslides was constructed from standardized GIS datasets. The second level calculates the susceptibility for the watershed. Multiple Logistic Regression (MLR) was used to examine the relationship between landsliding and several independent variables (elevation, slope, terrain curvature, flow direction, saturation, contributing area, land use, and geology

  3. Magma fluxes and recurreance rate of eruptions at Nevado de Toluca volcano (Mexico)

    Science.gov (United States)

    Weber, Gregor; Probst, Line; Arce, José L.; Caricchi, Luca

    2017-04-01

    Forecasting the frequency and size of volcanic eruptions is a long-term goal for hazard mitigation. The frequency at which a given crustal magmatic system is driven towards a critical state and the magnitude of the resulting volcanic events are linked to the supply rate of fresh magma, crustal properties, and tectonic setting. Our ability to forecast the recurrence rate of eruptions is hampered by the lack of data on key variables such as the average magma flux locally and globally. The aim of this project is to identify the average magma supply rate and injection frequency for eruptions of different magnitude and eruptive style. We centred our study at Nevado de Toluca in Mexico, a subduction-related volcano with an eruptive history spanning about 1.5 million years of comparatively well documented effusive and explosive eruptions dominantly of dacitic composition. We carry out in-situ high precision zircon geochronology for a sequence of eruptions of different magnitude to obtain a distribution of crystal ages from which average crustal magma fluxes can be calculated. Eruptive fluxes will be constrained by extracting lava flow volumes from a digital elevation model. A combination of whole rock and mineral chemistry will provide quantitative insights on petrogenetic processes and on the frequency at which intensive parameters changed within the magma reservoir before the eruptions. Our results will be integrated in a global database including other volcanic systems and literature data to attempt to identify similarities and differences between magmatic reservoirs feeding volcanic eruptions of different magnitude. The final target of this project is to identify the physical factors controlling the recurrence rate of volcanic eruptions at regional and global scale.

  4. Monitoring the Dynamic of a Fluvial Channel after Lahar Disturbance: Huiloac Gorge (Popocatepetl Volcano, Mexico)

    Science.gov (United States)

    Andres, N.; Palacios, D.; Zamorano, J. J.; Tanarro, L. M.; Renschler, C.; Sanjosé, J. J.; Atkinson, A.

    2009-04-01

    Capra, L.; Poblete, M.A. and Alvarado, R. 2004. The 1997 and 2001 lahars of Popocatépetl volcano (Central Mexico): textural and sedimentological constraints on their origin and hazards. Journal of Volcanology and Geothermal Research, 131: 351-369. Gran, K. y Montgomery, D., 2005. Spatial and temporal patterns in fluvial recovery following volcanic eruptions: Channel response to basin-wide sediment loading at Mount Pinatubo, Philippines. GSA Bulletin, 117; 1-2: 195-211. Hayes, S.K., Montgomery, D.R. and Newhall, C.G., 2002, Fluvial sediment transport and deposition following the 1991 eruption of Mt. Pinatubo. Geomorphology. Vol. 45: 211-224. Major, J.J., Pierson, T.C., Dinehart, R.L. y Costa, J.E. 2000. Sediment yield following severe volcanic disturbance- A two-decade perspective from Mount St. Helens. Geology, 28, n° 9: 819-822. Major, J.J., 2003. Post-eruption hydrology and sediment transport in volcanic river systems, Water Resources IMPACT, 5(3): 10-15. Muñoz, E. 2007. Los lahares del Popocatépetl: tratamiento de la información para la prevención de catástrofes. (PhD thesis, Universidad Complutense de Madrid.) Palacios, D., 1995. Rockslide processes on the north slope of Popocatépetl Volcano, Mexico, Permafrost and Periglaciar Processes, 6: 345-356. Palacios, D., J.J. Zamorano and G. Parrilla. 1998. Proglacial debris flows in Popocatépetl North Face and their relation to 1995 eruption. Z. Geomorph. N. P., 42(3), 273-295 Palacios, D., J.J. Zamorano and A. Gómez. 2001. The impact of present lahars on the geomorphologic evolution of proglacial gorges: Popocatépetl, Mexico. Geomorphology, 37(1-2), 15-42.

  5. Geological and Geophysical Analysis of the Processes Ground Cracking and Associated Risks in Urban Basins in the Eastern and Northern of Jalisco Block, Mexico.

    Science.gov (United States)

    Suarez-Plascencia, C.

    2016-12-01

    The Jalisco Block (JB) is located in the western sector of Mexican Volcanic Belt; it is bounded on the east by the Colima graben-Zacoalco and apparently the north by the River Grande de Santiago. Three landform are regionally identified: mountain areas, piedmont and plains formed by deposits of tuffs, volcanic ash and sediment filled. These plains have been progressively urbanized since the sixteenth century; they were built in around the Guadalajara Metropolitan Area, as well as small towns like Sayula, Ciudad Guzman, Zacoalco, Jocotepec and nearby villages, in which all together are populated by about 6 million people. Since 1912 there are records of damages by the continuous formation of ground cracking, this process has increased over the past two decades, affecting natural soil, agricultural areas, urban areas and infrastructure of roads and highways. These cracks generally have a SW-NE orientation similar with the alignment of regional geological structures. They are characterized by settlements and forming steps of a few centimeters, with lengths from 300 to 1000 m and depths of a few centimeters to 15 meters and width of up to 2.5 m. Formed mainly during the rainy season from June to October each year. Recent damages have generated losses of several hundreds of thousands of dollars, especially in Ciudad Guzman, located in southern BJ, where a crack of 2.5 km was observed in 2012 and it has long affected the downtown area, the town of Nextipac-Tesistan, municipality of Zapopan in the northern sector of JB. This territory is formed by a thick deposit of pumice tuffs, which has presented cracks in the years 1912, 1975, 1987, 2004 and 2015, affecting also agricultural and urban areas. The paper will presents results which will analyze and discern through geological, geophysical and with technology of geographic information, the origin of these cracks, which can be associated with active tectonic structures, geo-hydrological processes, extraction of underground

  6. Geomorphological Characterization of Atenquique Basin in the Eastern Sector of the Volcan-Nevado-Colima, Jalisco, Mexico, As an Input to the Risk Assessment of Debris Flows.

    Science.gov (United States)

    Flores-Pena, S.; Suarez-Plascencia, C.

    2014-12-01

    The Atenquique river basin drains the eastern sector of the Volcanic Complex (VC) Volcan-Nevado de Colima, located on the border of the states of Jalisco and Colima. To use the digital geomorphological analysis 1:50000 scale mapping provided by INEGI and Landsat images, manipulating it in ArcGIS 10.2 developing the DEM that was the basis for morphometric characterization. The results show that the basin is divided into five sub-basins, with the main Atenquique (SAT) and Arroyo Seco (SAS), calculating the compactness coefficient (Kc) and the coefficient of sinuosity indicate that SAT is the most prone to floods due to straight and slightly sinuous channels. However, the density of dissection shows a more developed drainage network on the SAT, with slopes up to 84° and 600 m deep. The drainage basin has its source at an altitude of 4260 m and its mouth is in the Tuxpan River at 1040 m, which has a relative height of 2800 m; has a funnel-shaped elongated west-east, its outstanding average in the sector are Mountain 44° and 10° the piedmont. The SAT has a total area of 81.8 km2, with a dendritic river network, where the first order streams reach an 82.99%, and second order streams are the 13.4% of the total, these values show that most of the slopes of the basin have incipient development valleys and steep slopes. The basin has had 3 debris flows in recent 58 years; these are formed by large volumes of rock and mud that covered the town of Atenquique and paper mill located at the mouth of the Tuxpan River, caused deaths and significant economic damage. Its genesis is associated with the end of the summer rainy season, so he also worked in the hydrological analysis in order to determine the volume of runoff in the basin. The results of this work are used as input for the determining the risk levels in the study area, and may also be used by the municipality of Tuxpan, in order to define policies to manage risk and reduce future risks to the industrial town of

  7. Ecological variability and rule-making processes for forest management institutions: a social-ecological case study in the Jalisco coast, Mexico

    OpenAIRE

    Sofía Monroy-Sais; Alicia Castillo; Eduardo García-Frapolli; Guillermo Ibarra-Manríquez

    2016-01-01

    Analysis of social-ecological systems is becoming increasingly used since the framework provides a valuable set of variables for understanding relationships between people and ecosystems. This interaction focuses on the use and management of natural resources that, in many cases, are common-pool resources. In Mexico, common-pool resources have long been explored since at least 60% of the forested lands in the country are held under the legal figure of ‘ejidos’ and indigenous communities, whic...

  8. Characteristics of the Seismicity in the San Martin Tuxtla volcano area, Veracruz, Mexico

    Science.gov (United States)

    Espindola, J.; Zamora-Camacho, A.; Godinez, M.

    2012-12-01

    San Martin Tuxtla volcano (18.572N, 95.169W, 1650 masl) is a large volcano rising in the midst of the Tuxtla volcanic field in the State of Veracruz, eastern México. The last eruption of this volcano occurred in 1793 and produced thick ash fall deposits in its vicinity. Due to increasing population in the area, the volcano poses a significant risk. To determine the seismic characteristics of the area and evaluate their possible relationship with the volcano we installed a network of three seismic stations in its surroundings. The array has recorded the seismic activity from 2007 to 2011. We present the results of the analysis of the records of this period, which in general show that the seismicity in the area is relatively low both in frequency and magnitude: only 51 events of magnitude (Mc) less than 2.5 were observed and located. Most of the earthquakes are typical volcano tectonic events occurring at shallow depths (<< 12 km) around the volcano. This low level of seismicity is probably a characteristic of the area and not of the particular period studied, as has been observed in other areas of basaltic volcanism, and could be used to establish any unusual seismicity that could be related to impending volcanic activity.

  9. Petrologic characteristics of the 1982 and pre-1982 eruptive products of El Chichon volcano, Chiapas, Mexico.

    Science.gov (United States)

    McGee, J.J.; Tilling, R.I.; Duffield, W.A.

    1987-01-01

    Studies on a suite of rocks from this volcano indicate that the juvenile materials of the 1982 and pre-1982 eruptions of the volcano have essentially the same mineralogy and chemistry. Data suggest that chemical composition changed little over the 0.3 m.y. sample period. Modally, plagioclase is the dominant phenocryst, followed by amphibole, clinopyroxene and minor phases including anhydrite. Plagioclase phenocrysts show complex zoning: the anorthite-rich zones are probably the result of changing volatile P on the magma and may reflect the changes in the volcano's magma reservoir in response to repetitive, explosive eruptive activity.-R.E.S.

  10. Prokaryotic diversity and metabolically active microbial populations in sediments from an active mud volcano in the Gulf of Mexico.

    Science.gov (United States)

    Martinez, Robert J; Mills, Heath J; Story, Sandra; Sobecky, Patricia A

    2006-10-01

    In this study, ribosomes and genomic DNA were extracted from three sediment depths (0-2, 6-8 and 10-12 cm) to determine the vertical changes in the microbial community composition and identify metabolically active microbial populations in sediments obtained from an active seafloor mud volcano site in the northern Gulf of Mexico. Domain-specific Bacteria and Archaea 16S polymerase chain reaction primers were used to amplify 16S rDNA gene sequences from extracted DNA. Complementary 16S ribosomal DNA (crDNA) was obtained from rRNA extracted from each sediment depth that had been subjected to reverse transcription polymerase chain reaction amplification. Twelve different 16S clone libraries, representing the three sediment depths, were constructed and a total of 154 rDNA (DNA-derived) and 142 crDNA (RNA-derived) Bacteria clones and 134 rDNA and 146 crDNA Archaea clones obtained. Analyses of the 576 clones revealed distinct differences in the composition and patterns of metabolically active microbial phylotypes relative to sediment depth. For example, epsilon-Proteobacteria rDNA clones dominated the 0-2 cm clone library whereas gamma-Proteobacteria dominated the 0-2 cm crDNA library suggesting gamma to be among the most active in situ populations detected at 0-2 cm. Some microbial lineages, although detected at a frequency as high as 9% or greater in the total DNA library (i.e. Actinobacteria, alpha-Proteobacteria), were markedly absent from the RNA-derived libraries suggesting a lack of in situ activity at any depth in the mud volcano sediments. This study is one of the first to report the composition of the microbial assemblages and physiologically active members of archaeal and bacterial populations extant in a Gulf of Mexico submarine mud volcano.

  11. Short-term effects on substance use of the keepin' it real pilot prevention program: linguistically adapted for youth in Jalisco, Mexico.

    Science.gov (United States)

    Marsiglia, Flavio F; Booth, Jaime M; Ayers, Stephanie L; Nuño-Gutierrez, Bertha L; Kulis, Stephen; Hoffman, Steven

    2014-10-01

    This article presents the short-term effects of a pilot study of keepin'it REAL (Manténte REAL) conducted in central Mexico by a binational team of investigators. This middle school-based model program for preventing substance use was adapted for Mexico linguistically but not culturally. Two Guadalajara public middle schools were recruited and randomly assigned to either implement the prevention program or serve as a control site. The program was implemented in the treatment site by the students' regular teachers, who were trained by the research team. Seventh graders in ten classrooms in the treatment and control schools (N = 432) completed a pretest and posttest survey in Spanish similar to the survey utilized in the original efficacy trial of keepin'it REAL in the US. T-tests and OLS regressions were conducted to determine the effects of the intervention on substance use outcomes. Differences between treatment and control groups in frequency of use of alcohol and tobacco, the two substances of choice in this sample, were significant and in the desired direction. Differences in amount of use were also in the preferred direction but were not significant for alcohol and only marginally significant for tobacco. When the sample was split by gender, statistically significant treatment effects remained for females but were not observed among males. Effects of the linguistically adapted version of keepin'it REAL appears to be driven by the change in female use; however, the difference in male and female outcomes was not statistically significant. Implications for cultural adaptation and prevention in Mexico are discussed from a communication competency perspective. The promising results of the pilot study suggest that the linguistic adaptation was effective, but that a comprehensive cultural adaptation of keepin'it REAL in partnership with Mexican investigators and communities may be warranted.

  12. Hydrogeochemical monitoring of El Chichón Volcano crater lake, Mexico.

    Science.gov (United States)

    Ceniceros, N.; Armienta, M. A.; Ramos, S.; Cruz, O.; Aguayo, A.

    2003-04-01

    The geochemistry of the crater lake of the El Chichón volcano has been studied since 1983. Results have been used to analyze post-eruptive processes and assessing volcanic risk. Chemical analysis has included pH, temperature, principal ions, fluoride, Iron , sulfide, boron and Silica. From 1985, all determinations have been performed at the Analytical Chemistry Laboratory of the Geophysics Institute (National University of Mexico). Such analysis were made following the standard methods, as given in APHA (1989), e.g. UV-visible, emission, and atomic absorption spectroscopy, potentiometric and volumetric techniques.. The El Chichón crater lake water showed an increasing pH from 1983 to 1986 (from 0.56 to 2.33), from then pH has fluctuated around the later value (in August 2002 pH was 1.98). Conductivity showed a high fluctuations with a general decreasing trend, ranging between 83800 uS/cm (1983, Casadevall et al., 1984) and close to 2000 uS/cm (December 1998). Water-type has changed along these years: The Chichon water could be classified as acid, calcium-chloride in 1983; in 1991 changed to Sulfate-mixed and since 1992, it has been mostly of sodium chloride type, except for a few dates when it could be classified as sulfate-mixed or calcic type. Since 1985, cation concentrations produced by environmental rock dissolution decreased in the same manner. A decreasing trend with time was observed also in anions of a potential magmatic origin like sulfate, chloride and fluoride. Molar concentrations of chloride have been mostly greater than sulfate concentrations (up to two orders of magnitude) and have varied without any observed correlation. Oxidation-reduction processes may explain the large sulfate concentration changesSulfate shows large. The geochemical modeling programs (MINTEQA2, PHREEQCE) showed saturation indices close to equilibrium for gypsum and anhydrite suggesting that sulfates also can be derived from other processes such as dissolution

  13. Pleistocene glaciation of volcano Ajusco, central Mexico, and comparison with the standard Mexican glacial sequence

    Science.gov (United States)

    White, Sidney E.; Valastro, Salvatore

    1984-01-01

    Three Pleistocene glaciations and two Holocene Neoglacial advances occurred on volcano Ajusco in central Mexico. Lateral moraines of the oldest glaciation, the Marqués, above 3250 m are made of light-gray indurated till and are extensively modified by erosion. Below 3200 m the till is dark red, decomposed, and buried beneath volcanic colluvium and tephra. Very strongly to strongly developed soil profiles (Inceptisols) have formed in the Marqués till and in overlying colluvia and tephra. Large sharp-crested moraines of the second glaciation, the Santo Tomás, above 3300 m are composed of pale-brown firm till and are somewhat eroded by gullies. Below 3250 m the till is light reddish brown, cemented, and weathered. Less-strongly developed soil profiles (Inceptisols) have formed in the Santo Tomás till and in overlying colluvia and tephra. Narrow-crested moraines of yellowish-brown loose till of the third glaciation, the Albergue, are uneroded. Weakly developed soil profiles (Inceptisols) in the Albergue till have black ash in the upper horizon. Two small Neoglacial moraines of yellowish-brown bouldery till on the cirque floor of the largest valley support weakly developed soil profiles with only A and Cox horizons and no ash in the upper soil horizons. Radiocarbon dating of organic matter of the B horizons developed in tills, volcanic ash, and colluvial volcanic sand includes ages for both the soil-organic residue and the humic-acid fraction, with differences from 140 to 660 yr. The dating provides minimum ages of about 27,000 yr for the Marqués glaciation and about 25,000 yr for the Santo Tomás glaciation. Dates for the overlying tephra indicate a complex volcanic history for at least another 15,000 yr. Comparison of the Ajusco glacial sequence with that on Iztaccíhuatl to the east suggests that the Marqués and Santo Tomás glaciations may be equivalent to the Diamantes glaciation First and Second advances, the Albergue to the Alcalican glaciations, and the

  14. Geochemical and isotopic profile of Pico de Orizaba (Citlaltépetl) volcano, Mexico: Insights for magma generation processes

    Science.gov (United States)

    Schaaf, Peter; Carrasco-Núñez, Gerardo

    2010-11-01

    Pico de Orizaba or Citlaltépetl volcano is the easternmost and highest stratovolcano of the subduction-related Mexican Volcanic Belt (MVB) located > 400 km NNE of the Middle America Trench. This active volcano comprises four evolutionary stages, ranging in age from 0.65 Ma to the Holocene, and is surrounded by Quaternary monogenetic scoria cones and maar volcanoes. Magmatic products of the stratocone range from basaltic andesites to rhyolites and the cinder cones erupted basalts and basaltic andesites. All rock compositions form a continuous calc-alkaline suite. Petrogenetic processes involved in magma generation and evolution include fractional crystallization and mid-crustal assimilation. Trace element patterns with elevated Ba/Nb, positive Pb spikes, and Th enrichments indicate contributions from subducted sediment. Low Ba/Th ratios suggest melting of hydrous sediment without significant loss of fluid-mobile elements prior to melting. Sr-Nd isotopic ratios of Pico de Orizaba and cinder cones are nearly chondritic and are located on a mixing curve between Pacific MORB and Paleozoic crust of SE Mexico. However, vertical Nd distributions in an 87Sr/ 86Sr vs. ɛNd diagram cannot be explained by crustal assimilation and indicate contributions of a sedimentary component with unradiogenic Nd. In contrast to other eastern MVB volcanic centres, Pico de Orizaba magmas are derived almost exclusively from a depleted mantle source. Compared to other MVB stratocones, Pico de Orizaba shows the least radiogenic Nd isotope ratios at nearly identical 87Sr/ 86Sr. Steep trends in a 206Pb/ 204Pb vs. 207Pb/ 204Pb diagram favour the involvement of young, 207Pb-enriched oceanic sediments in magma generation processes of Pico de Orizaba volcano. The Pb isotope data do not support any assimilation of lower crustal Grenvillian basement.

  15. Study of the structural changes in the Popocatepetl volcano in Mexico related to microseismicity by applying the lineament analysis to the Aster (Terra) satellite data

    CERN Document Server

    Arellano-Baeza, A A; Trejo-Soto, M

    2007-01-01

    Mexico is one of the most volcanically active regions in North America. Volcanic activity in central Mexico is associated with the subduction of the Cocos and Rivera plates beneath the North American plate. Periods of enhanced microseismic activity, associated with the volcanic activity of the Popocatepetl volcano is compared with periods, during which the microseismic activity was low. We detected systematical changes in the number of lineaments, associated with the microseismic activity due to lineament analysis of a temporal sequence of high resolution satellite images of the Popocatepetl volcano, provided by the ASTER/VNIR instrument. The Lineament Extraction and Stripes Statistic Analysis (LESSA) software package was used for the lineament extraction. In the future it would allow develop a methodology for detection of possible elevation of pressure in volcano edifice.

  16. Geostatistics and multivariate analysis as a tool to characterize volcaniclastic deposits: Application to Nevado de Toluca volcano, Mexico

    Science.gov (United States)

    Bellotti, F.; Capra, L.; Sarocchi, D.; D'Antonio, M.

    2010-03-01

    Grain size analysis of volcaniclastic deposits is mainly used to study flow transport and depositional processes, in most cases by comparing some statistical parameters and how they change with distance from the source. In this work the geospatial and multivariate analyses are presented as a strong adaptable geostatistical tool applied to volcaniclastic deposits in order to provide an effective and relatively simple methodology for texture description, deposit discrimination and interpretation of depositional processes. We choose the case of Nevado de Toluca volcano (Mexico) due to existing knowledge of its geological evolution, stratigraphic succession and spatial distribution of volcaniclastic units. Grain size analyses and frequency distribution curves have been carried out to characterize and compare the 28-ka block-and-ash flow deposit associated to a dome destruction episode, and the El Morral debris avalanche deposit originated from the collapse of the south-eastern sector of the volcano. The geostatistical interpolation of sedimentological data allows to realize bidimensional maps draped over the volcano topography, showing the granulometric distribution, sorting and fine material concentration into the whole deposit with respect to topographic changes. In this way, it is possible to analyze a continuous surface of the grain size distribution of volcaniclastic deposits and better understand flow transport processes. The application of multivariate statistic analysis (discriminant function) indicates that this methodology could be useful in discriminating deposits with different origin or different depositional lithofacies within the same deposit. The proposed methodology could be an interesting approach to sustain more classical analysis of volcaniclastic deposits, especially where a clear field classification appears problematic because of a homogeneous texture of the deposits or their scarce and discontinuous outcrops. Our study is an example of the

  17. Some insights about the activity of the Ceboruco Volcano (Nayarit, Mexico) from recent seismic low-frequency activity

    Science.gov (United States)

    Rodríguez Uribe, María Carolina; Núñez-Cornú, Francisco Javier; Nava Pichardo, Fidencio Alejandro; Suárez-Plascencia, Carlos

    2013-10-01

    The Ceboruco stratovolcano (2,280 m.a.s.l.) is located in Nayarit, Mexico, at the western end of the Mexican volcanic belt, near several population centers and by the side of a strategic highway. During the last 1,000 years it has had, on the average, one eruption every 125 years. It last eruptive activity began in 1870, and during the following 5 years it presented superficial activity including vapor emissions, ash falls, and rhyodacitic lava flows along the southeast side. A data set consisting of 139 low-frequency volcanic-type earthquakes, recorded from March 2003 to July 2008 at the CEBN triaxial short period digital station on the southwestern side of the volcano, was classified according to waveform and spectral characteristics into four families: short duration, extended coda, bobbin, and modulated amplitude. Approximate hypocentral locations indicate that there is no particular location for events of any family, but rather that all events occur at different points within the volcano. The presence of ongoing volcanic-earthquake activity together with the ongoing vapor emissions indicate that the Ceboruco volcano continues to be active, and the higher occurrence rates of short-duration events, as compared with those for the other families, could indicate an increase in the stress in the volcanic edifice. This apparent stress increase, together with the fact that the last eruption occurred 143 years ago, tell us that the Ceboruco may be approaching a critical state, and may represent a hazard to the surrounding communities and economic activities.

  18. Eruptive dynamics of the “Citlaltépetl Pumice” at Citlaltépetl volcano, Eastern Mexico

    Science.gov (United States)

    Rossotti, Andrea; Carrasco-Núñez, Gerardo; Rosi, Mauro; Di Muro, Andrea

    2006-11-01

    Citlaltépetl (Pico de Orizaba) is Mexico's highest (5675 m a.s.l.) potentially active volcano, which is presently in a dormant state. Between 9.0 and 8.5 ky B.P., a sequence of volcanic eruptions occurred at Citlaltépetl volcano as part of the most explosive Holocene episode. This sequence is associated with the deposition of an intercalation of pumice fallout and scoria and pumice-rich pyroclastic flow deposits, named here as "Citlaltépetl Pumice" (C.P.). Detailed stratigraphic and petrographic correlation of over 100 measured sections, in conjunction with the analysis of the physical characteristics of the juvenile and lithic portions of each main layer of the sequence, provided the basis to reconstruct the eruptive episodes and to assert the eruptive dynamics of the whole sequence, which was divided into eight main eruptions separated by three brief periods of quiescence. The eruption sequence started with a phreatic phase that soon developed into a bread-crusted, bomb-bearing phase. This was followed by a sequence of vigorous Plinian explosive eruptions separated by brief periods of repose and a short dome-collapse activity. It was followed by another cycle of alternated scoria pyroclastic flows-forming and Plinian activity. This eruptive sequence shows the complexity of single eruptive events with alternated contrasting styles suggested by the compositional differences between the pyroclastic flow and fallout products.

  19. A GIS-based method to determine the volume of lahars: Popocatépetl volcano, Mexico

    Science.gov (United States)

    Muñoz-Salinas, E.; Renschler, C. S.; Palacios, D.

    2009-10-01

    Lahars are flows composed of water and volcanic sediment which are often dangerous for people living near volcanoes. Therefore, a reliable estimation of lahar volume is needed to effectively assess the risk. This paper proposes a new method to calculate the volume of lahar sediments found in channels of volcanic landscapes. The method requires surveys of several cross-sections along a gorge, a Digital Elevation Model of the study area and measurements of the thickness of the lahar deposits. With these data and a Geographical Information System (GIS), the volume is calculated for the erosive section where deposit volume is divided into oblique parallelepipeds and the sedimentary section where deposit volume is divided into polyhedrons. This new method was applied to the 1997 and 2001 lahars that occurred in the channel of a gorge at Popocatépetl volcano, Mexico. The estimated volumes are 1.85 × 10 5 and 1.6 × 10 5 m 3, respectively, which is about 40% less than those obtained by the traditional method that multiplies lahar flow-path length, sediment width and sediment depth. This observation suggests that the traditional method tends to overestimate volumes.

  20. Crust-Mantle Interactions at Pico de Orizaba (Citlaltepetl) Volcano, Mexico.

    Science.gov (United States)

    Schaaf, P.; Carrasco, G.

    2006-12-01

    Pico de Orizaba (Citlaltepetl) volcano constitutes the easternmost and highest stratovolcano of the subduction- related Plio-Quaternary Trans-Mexican Volcanic Belt (TMVB). The volcano can be divided into three main constructional stages. Its activity started during the mid-Pleistocene. The present cone was built on the remnants of the ancestral buildings by eruption of amphibole-two pyroxene dacitic lava flows, the most recent of which was erupted in the seventeenth century. The volcano is surrounded to the SW by monogenetic Quaternary cindercones and maars. All representative units were sampled in this work for geochemical and isotopic purposes, including a small quartzitic xenolith found in the basaltic monogenetic suite. Volcanic products of the stratocone are quite heterogeneous and range from calc-alkaline basaltic andesites to dome rhyolites, also displayed by a wide range of SiO2 and MgO (72.6-53.2 and 7.0-0.3 wt. %, respectively). In comparison to other TMVB stratovolcanoes (e.g., Colima, Nevado de Toluca), Pico de Orizaba shows similar 87Sr/86Sr ratios (0.7037-0.7048) but considerably more evolved Nd-Pb isotopic ratios (eNd: -1.8 to + 1.4; 206Pb/204Pb: 18.61-18.78). Elevated LILE concentrations and depleted HFSE witness the importance of slab- derived aqueous fluids and metasomatic reactions between the subducting lithosphere and overlying mantle wedge. On the other hand, Pico de Orizaba volcano shows additionally high crustal contributions of a source with depleted Sr and enriched Nd and Pb isotopic signatures, best explained by considerable assimilation of the local Grenvillian basement in magma generation processes. In contrast to Popocatépetl volcano with a high-level magma reservoir emplacement (7-8 km) and obvious interaction with the carbonate-dominated shallow basement rocks (e.g. elevated 87Sr/86Sr ratios and CO2 in gas plumes), this effect cannot be observed at Pico de Orizaba volcano, although a regional Cretaceous limestone basement is also

  1. Origin and age of the Volcanic Rocks of Tláloc Volcano, Sierra Nevada, Central Mexico

    Science.gov (United States)

    Meier, M.; Grobéty, B.; Arce, J. L.; Rueda, H.

    2007-05-01

    The Tláloc volcano (TV) is a 4125 m high stratovolcano of the Trans Mexican Volcanic Belt (TMVB) and is located in the northern end of the N-S trending Sierra Nevada, 30 km NE of Mexico City. Few data on the petrological and temporal evolution of TV have been published to date. Recently dated deposits gave ages between 32'000 and 34'500±500 years BP (Huddart and Gonzalez, 2004). Mapping and sampling of extrusive rocks in the summit region of TV revealed a dome structure with radiating lava flows consisting of dacitic rocks containing plagioclase and hornblende phenocrysts. Some flows, however, seem to be associated with a collapse structure E of the main summit. Crossing relationships indicate that this structure is older (“Paleo Tláloc”). A stratigraphy of the pyroclastic deposits was established along the northern slope of TV. From the numerous pyroclastic flows, separated by paleosoils and fluviatile deposits, only two pumice and one block and ash flow (BAF) have regional extent. Their thickness - distance relationship and their granulometry point to major explosive events. A carbonized wood sample from the BAF deposit gave ages similar to the previous ages (33'180±550 yr BP and 23'170±270 yr BP), a sample from a pyroclastic flow gave even a younger age (16'620±110 yr BP), suggesting that TV remained active also after the volcanoes Iztaccíhuatl and Popocatépetl further to the South started their activity. Based on these preliminary data it may be necessary to reconsider the accepted scenario of the temporal evolution of the central section of the TMVB, which assumes that the activity migrates from North to South with time. Huddart, D. and Gonzalez, S., 2004. Pyroclastic flows and associated sediments, Tláloc-Telapón, piedmont fringe of the eastern basin of Mexico. In: G.J. Aguirre-Diaz, Macías, J.L., and Siebe, C., (Editor), Penrose Conference. UNAM, Metepec, Puebla, Mexico, pp. 35.

  2. Lessons from Popocatepetl Volcano (Mexico): Ancient Settlement Buried by Lavas, Mudflows, and Air-Fall Deposits

    Science.gov (United States)

    Delgado, H.; Panfil, M.; Gonzalez, E. A.; Coyoacan, C. U.; Urangaela, G.; Plunket, P.; Gardner, T.; Abrams, M.

    1994-01-01

    Popocatepetl volcano is 5452 m in altitude and capped by glaciers with a long Late Pleistocene-Holocene history. Volcanic activity has been intense during the last 10 000 years. Therefore, the valleys at the NE foothills of the volcano, covered by air-fall ejecta and drained by the runoff of the glaciers, became very attractive to ancient inhabitants of the Xalizintla Valley (XV) west of Puebla City, because of fertility of soils. The XV was occupied by humans about 2000 years ago who witnessed five events related to volcanic activity related to Popo. These events, described in this paper, are being taken into account for volcanic risk evaluation since several towns with a population of more than 23 000 people reoccupied again the Xalizintla Valley.

  3. Hazard map for volcanic ballistic impacts at Popocatépetl volcano (Mexico)

    Science.gov (United States)

    Alatorre-Ibargüengoitia, Miguel A.; Delgado-Granados, Hugo; Dingwell, Donald B.

    2012-11-01

    During volcanic explosions, volcanic ballistic projectiles (VBP) are frequently ejected. These projectiles represent a threat to people, infrastructure, vegetation, and aircraft due to their high temperatures and impact velocities. In order to protect people adequately, it is necessary to delimit the projectiles' maximum range within well-defined explosion scenarios likely to occur in a particular volcano. In this study, a general methodology to delimit the hazard zones for VBP during volcanic eruptions is applied to Popocatépetl volcano. Three explosion scenarios with different intensities have been defined based on the past activity of the volcano and parameterized by considering the maximum kinetic energy associated with VBP ejected during previous eruptions. A ballistic model is used to reconstruct the "launching" kinetic energy of VBP observed in the field. In the case of Vulcanian eruptions, the most common type of activity at Popocatépetl, the ballistic model was used in concert with an eruptive model to correlate ballistic range with initial pressure and gas content, parameters that can be estimated by monitoring techniques. The results are validated with field data and video observations of different Vulcanian eruptions at Popocatépetl. For each scenario, the ballistic model is used to calculate the maximum range of VBP under optimum "launching" conditions: ballistic diameter, ejection angle, topography, and wind velocity. Our results are presented in the form of a VBP hazard map with topographic profiles that depict the likely maximum ranges of VBP under explosion scenarios defined specifically for Popocatépetl volcano. The hazard zones shown on the map allow the responsible authorities to plan the definition and mitigation of restricted areas during volcanic crises.

  4. Eruptive History of the Rhyolitic Guangoche Volcano, Los Azufres Volcanic Field, Central Mexico

    Science.gov (United States)

    Rangel Granados, E.; Arce, J. L.; Macias, J. L.; Layer, P. W.

    2014-12-01

    Guangoche is a rhyolitic and polygenetic volcano with a maximum elevation of 2,760 meters above sea level. It is situated to the southwest of the Los Azufres Volcanic Field (LAVF), in the central sector of the Trans-Mexican Volcanic Belt. Guangoche volcano is the youngest volcano described within the LAVF. It shows a horseshoe shaped crater open to the south, with a central lava dome. Its eruptive history during late Pleistocene has been intense with six explosive eruptions that consists of: 1) A southwards sector collapse of the volcano that generated a debris avalanche deposit with megablocks of heterogenous composition; 2) A plinian-type eruption that generated a pumice fall deposit and pyroclastic density currents by column collapse at 30.6 ka; 3) A plinian-type eruption "White Pumice Sequence" (29 ka) that developed a 22-km-high eruptive column, with a MDR of 7.0 x 107 kg/s (vol. = 0.53 km3); 4) A dome-destruction event, "Agua Blanca Pyroclastic Sequence" at 26.7 ka, that deposited a block-and-ash flow deposit; 5) A subplinian-plinian type eruption "Ochre Pyroclastic Sequence" (<26 ka) with an important initial phreatomagmatic phase, that generated pyroclastic density currents and pumice fallouts. The subplinian-plinian event generated a 16-km-high eruptive column, with a MDR of 1.9 x 107 kg/s, and magma volume of 0.38 km3; 6) The eruptive history ended with a subplinian eruption (<<26 ka), that generated a multilayered fall deposit, that developed a 11-km-high eruptive column, with a MDR of 2.9 x 106 kg/s and a magma volume of 0.26 km3. Volcanic activity at Guangoche volcano has been intense and future activity should not be discarded. Unfortunately, the last two events have not been dated yet. Guangoche rhyolitic magma is characterized by low-Ba contents suggesting crystal mush extraction for their genesis.

  5. Volcanic Risk Perception in Five Communities Located near the Chichón Volcano, Northern Chiapas, Mexico

    Science.gov (United States)

    Rodriguez, F.; Novelo-Casanova, D. A.

    2010-12-01

    The Chichón volcano (17° 19’ N and 93° 15’ W) is located in the state of Chiapas, Mexico. This volcano is classified by UNESCO as one of the ten most dangerous volcanos in the world. The eruptions of March and April in 1982 affected at least 51 communities located in the surroundings of the volcano and caused the death of about 2000 people. In this work we evaluate the risk perception in five communities highly populated: Juárez, Ostuacán, Pichucalco, Reforma and Sunuapa. We selected these communities because they have a high possibility to be affected by a volcanic eruption in the future. Our survey was carried out during February and March 2006. A total of 222 families were interviewed using a questionnaire to measure risk perception. These questionnaires retrieved general information as how long people had been living there and their reasons to do so; their experiences during the 1982 events, their opinion about the authorities participation and their perception of volcanic risk; the plans of the community for disaster prevention and mitigation. Some of the most important results are: (1). People perceive a very low volcanic risk and the 70% of interviewees believe that a new eruption in the future is almost improbable because it happened in 1982. This result is particularly interesting because, according to the state government, more than 100,000 inhabitants will be directly affected in case of a new similar eruption; (2). About 95% of the population do not know the current activity of the volcano and consider that the authorities do not inform properly to their communities; (3). The response of the authorities during the events of 1982 was ranked as deficient mainly because they were unable provide shelters, storage facilities, food as well as medicine and health care access; (4). Approximately 60% of the community will accept to be re-located again in case of a new eruption; (5). About 70% of the population will not accept to be re-located because

  6. Kinematics and age of Early Tertiary trench parallel volcano-tectonic lineaments in southern Mexico: Tectonic implications

    Science.gov (United States)

    Martini, M.; Ferrari, L.; Lopez Martinez, M.; Cerca Martinez, M.; Serrano Duran, L.

    2007-05-01

    We present new geological, structural, and geochronological data that constrain the timing and geometry of Early Tertiary strike slip deformation in southwestern Mexico and its relation with the concurrent magmatic activity. Geologic mapping in Guerrero and Michoacan States documented two regional WNW trending volcano-tectonic lineaments sub parallel to the present trench. The southernmost lineament runs for ~140 km from San Miguel Totolapan area (NW Guerrero) to Sanchiqueo (SE Michoacan), and passes through Ciudad Altamirano. Its southeastern part is marked by the alignment of at least eleven silicic to intermediate major domes as well as by the course of the Balsas River. The northwestern part of the lineament is characterized by ductile left lateral shear zones in Early Tertiary plutonic rocks observed in the Rio Chiquito valley. Domes near Ciudad Altamirano are unaffected by ductile shearing and yielded a ~42 Ma 40Ar/39Ar age, setting a minimum age for this deformation. The northern volcano-tectonic lineament runs for ~190 km between the areas of Huitzuco in northern Guerrero and the southern part of the Tzitzio fold in eastern Michoacan. The Huautla, Tilzapotla, Taxco, La Goleta and Nanchititla silicic centers (all in the range 37-34 Ma) are emplaced along this lineament, which continues to the WNW trough a mafic dike swarm exposed north of Tiquicheo (37-35 Ma) and the Purungueo subvolcanic body (~42 Ma). These rocks, unaffected by ductile shearing, give a minimum age of deformation similar to the southern Totolapan-Sanquicheo lineament. Post ~42 Ma deformation is essentially brittle and is characterized by several left lateral and right lateral transcurrent faults with typical Riedel patterns. Other trench-parallel left lateral shear zones active in pre-Oligocene times were recently reported in western Oaxaca. The recognizing of Early Tertiary trench-parallel and left-lateral ductile shearing in internal areas of southern Mexico suggest a field of widely

  7. Stability Evaluation Of Previous Volcanic Edifice Collapse At Pico De Orizaba Volcano, Mexico, Using Geotechnical Techniques

    Science.gov (United States)

    Concha-Dimas, A.; Watters, R. J.

    2001-12-01

    Pico de Orizaba volcano has collapsed twice during its geologic evolution (Carrasco-Nuñez, 1997). The initial stage of evolution for this volcano is known as the Torrecillas cone that collapsed 0.21 Ma b.p., and the related deposits formed the Jamapa avalanche which traveled eastward 75 km. A second, superimposed constructional stage is the Espolón de Oro cone that also ended with a collapse 20 000 years b.p., forming the Tetelzingo avalanche-lahar that traveled 85 km. Samples from the remains of old summit cores and their corresponding collapse deposits were collected and tested in order to obtain strength parameters of altered rock from old volcanic edifices. Hydrothermal alteration and variations of strength of the two avalanche deposits were correlated with the strength values and alterations from the in situ corresponding sources. Strength values: Hoek and Brown's parameters, Uniaxial Compressive Strength (50-300 kPa), cohesion (480-2000 kPa), angle of friction (6° - 35° ); and degree of alteration give insights of rock mass quality and maximum intact rock strengths of the edifice rock mass. These values provide the upper limits for numerical model input parameter values for evaluation of flank stability. Rock strength from numerical model of previous failures can be compared with those obtained for the rock mass and intact rock of the actual edifice. This would permit the assessment of future avalanche hazards.

  8. The ongoing dome emplacement and destruction cyclic process at Popocatépetl volcano, Central Mexico

    Science.gov (United States)

    Gómez-Vazquez, Angel; De la Cruz-Reyna, Servando; Mendoza-Rosas, Ana Teresa

    2016-09-01

    The ongoing eruptive activity of Popocatépetl volcano has been characterized by emplacement and subsequent destruction of a succession of lava domes. Between the onset of the current eruption in 1994 and the time of this submission, 38 episodes of lava dome formation and removal have been identified. Each dome has showed particular features related to the magma extrusion process. Among other manifestations, dome-emplacement events have been usually accompanied by relatively low-intensity, protracted explosions referred to as exhalations. After variable times of residence, emplacements have ended in partial or total destruction of the domes by strong vulcanian explosions that produced sizeable ash plumes, with most of them also ejecting incandescent debris onto the volcano flanks. Here, we present a detailed account for the observed activity related to the domes' growth and destruction, related seismic monitoring signals, and morphological features of the domes based on 19 years of visual observations and image analysis. We then discuss a model for the process of dome growth and destruction and its hazard implications.

  9. Late Pleistocene Holocene stratigraphy and radiocarbon dating of La Malinche volcano, Central Mexico

    Science.gov (United States)

    Castro-Govea, Renato; Siebe, Claus

    2007-04-01

    Previous studies of La Malinche identified and radiocarbon dated several volcanic layers, the youngest of which yielded an age of ca. 7.5 ka. An additional ash fallout layer that crops out at high altitudes was considered the most recent deposit, with an estimated age of 6 ka. In the present work 38 new radiocarbon ages are presented. From these, several date the young ash fallout layer and lie around 3.1 ka. With the aid of these dates a new and comprehensive stratigraphy documenting the Late Pleistocene-Holocene eruptive history of La Malinche is presented. The stratigraphy indicates two main stages of volcanic activity: Pre-Malinche and Malinche. The first undoubtedly comprises the major part of the eruptive history, but its deposits are largely covered by the products of the latter stage, on which this study is focused. The Malinche stage was subdivided into three eruptive periods. Period 1 started with the emplacement of the Huamantla Pumice more than 45 ka ago. This deposit consists of a thick pumice fallout overlain by pyroclastic flow deposits. Subsequently, several episodes of construction and collapse of summit domes occurred. The oldest dome was dated at ca. 45 ka. Period 2 started 21.5 ka ago with the Malinche Pumice I, a widespread pumice fallout covering the entire slopes of the volcano. Pyroclastic flows and lahars related to this eruption were channeled along deep barrancas and reached considerable distances. Deposits produced by partial sector collapse and dated at ca. 20.9 ka, and a pumice-and-ash flow deposit dated at 15.9 ka were also generated during this period. The last period started with the eruption of the Malinche Pumice II, a distinctive fallout deposit overlain by ash flow deposits on the NE slope of the volcano. The age of this pumice layer is estimated between 12 and 9 ka. Formation of block-and-ash flows, lahars and pumice-and-ash flows followed during this period, and peaked in a most intensive episode that was dated at 7.5 ka

  10. Tree-ring based reconstruction of rockfalls at Cofre de Perote volcano, Mexico

    Science.gov (United States)

    Franco-Ramos, Osvaldo; Stoffel, Markus; Vázquez-Selem, Lorenzo

    2017-08-01

    In this study, dendrogeomorphic techniques are employed to analyse the temporal frequency and spatial distribution of rockfalls on a talus slope of La Teta valley, located on the NW slopes of Cofre de Perote volcano at 4000 m above sea level. Based on the interpretation of disturbance signals in growth rings of old-growth Pinus hartwegii Lindl. trees, we identify 100 growth disturbances related with rockfall events dated between 1780 and 2011, with slightly more than half of these events being dated to the last 50 years. The sectors most susceptible to rockfall correspond with the young rock lobes located at the foot of scarps. Roughly three in ten events has been triggered by regional, M > 6 earthquakes, whereas half of the events activity coincides with periods characterized by severe, prolonged summer rainfalls such as the ones occurred in 1995, 1998, 2005 and 2011.

  11. LOS TEXTILES RECUPERADOS EN LA CULTURA BOLAÑOS, JALISCO (Textiles recovered from the Bolaños culture, Jalisco

    Directory of Open Access Journals (Sweden)

    María Teresa Cabrero G.

    2010-09-01

    Full Text Available En el México prehispánico, el hallazgo de textiles es sorprendente ya que deben reunirse determinados factores de clima y suelo para su conservación. Durante las excavaciones en El Piñón, sitio arqueológico perteneciente a la cultura Bolaños situada en el norte de Jalisco, México, se descubrieron varios fragmentos de telas elaboradas con fibras de algodón cuya antigüedad es de 1500 años. Dar a conocer este hallazgo resulta de gran importancia por ser una región inhóspita, poco conocida y alejada de las grandes urbes mexicanas. ENGLISH: It is very uncommon to find textile remains dated before the Spanish conquerors arrived in Mexico because numerous taphonomic factors, especially those pertaining to local climatic and soil chemistry conditions, must coincide to in order to preserve textiles. We found a series of cotton cloth fragments dated about 1500 years old during the archaeological recovery at the site of El Piñon, which is part of the Bolaños culture located in the North of Jalisco, Mexico. Publishing these data is very important due to the inhospitable geography and climate of the region, the fact that the site is not well known and is at a substantial distance from the closest Mexican urban centers.

  12. Gabbroic xenoliths in alkaline lavas in the region of Sanganguey Volcano, Nayarit, Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Giosa, T.A.; Nelson, S.A.

    1985-01-01

    Gabbroic xenoliths occur in alkaline cinder cones and lava flows erupted from vents along five parallel lines trending through the calc-alkaline volcano, Sanganguey in the northwestern portion of the Mexican Volcanic Belt. The xenoliths consist of varying proportions of olivine, clinopyroxene, orthopyroxene, and plagioclase. The complete lack of hydrous phases indicates that the gabbros crystallized under conditions of low PH/sub 2/O. Many xenoliths show textures indicative of a cumulate origin and others exhibit recrystallization indicative of subsolidus reactions prior to incorporation in the host liquids. Reaction between xenolithic minerals and host liquids are also observed. The range of Mg numbers calculated for liquids that would have been in equilibrium with olivines in the xenoliths suggests that these olivines crystallized from magmas such as those represented by either calc-alkaline basaltic andesites and andesites or the more evolved alkalic rocks which occur throughout the area. Crystal fractionation models show that the xenoliths may be related to such magmas. The fact that xenoliths occur most commonly in the alkaline rocks suggests that alkaline magmas rise to the surface more rapidly than the more chemically evolved calc-alkaline and alkaline magmas. Alternatively the lack of xenoliths in the more evolved magmas produced by high level crystal fractionation may indicate that the xenoliths are derived from zones below that from which the differentiated magmas begin their final ascent to the surface.

  13. The Large-Scale Debris Avalanche From The Tancitaro Volcano (Mexico): Characterization And Modeling

    Science.gov (United States)

    Morelli, S.; Gigli, G.; Falorni, G.; Garduno Monroy, V. H.; Arreygue, E.

    2008-12-01

    The Tancitaro is an andesitic-dacitic stratovolcano located in the Michoacán Guanajuato volcanic field within the west-central portion of the trans-Mexican Volcanic Belt. The volcanism in this area is characterized by two composite volcanoes, the highest of which is the Tancitaro volcanic edifice (3840 m), some low angle lava cones and more than 1,000 monogenetic cinder cones. The distribution of the cinder cones is controlled by NE-SW active faults, although there are also additional faults with NNW-SSE trends along which some cones are aligned. The Tancitaro stratovolcano is located at the intersection of the tectonical structures that originate these alignments. All this geological activity has contributed to the gravitational instability of the volcano, leading to a huge sector collapse which produced the investigated debris avalanche. The collapse structure is an east-facing horseshoe-shaped crater (4 km wide and 5.3 km long), related with a large fan that was deposited within the Tepalcatepec depression. The deposit starts only 7 km downslope from the failure scar, it is 66 km long and covers an area of approximately 1155 km2. The landslide magnitude is about 20 km3 and it was firstly determined by the reconstruction of the paleo-edifice using a GIS software and then validated by the observation of significant outcrops. The fan was primarily formed by the deposit of this huge debris avalanche and subsequently by debris flow and fluvial deposits. Field investigations on the fan area highlighted the presence of two texturally distinct parts, which are referred to the 'block facies' and the 'matrix facies'. The first sedimentary structure is responsible for the typical hummock morphologies in the proximal area, as seen in many other debris avalanche deposits. Instead in the distal zones, the deposit is made up by the 'mixed block and matrix facies'. Blocks and megablocks, some of which are characterized by a jigsaw puzzle texture, gradually decrease in size

  14. Solute fluxes and geothermal potential of Tacaná volcano-hydrothermal system, Mexico-Guatemala

    Science.gov (United States)

    Collard, Nathalie; Taran, Yuri; Peiffer, Loïc; Campion, Robin; Jácome Paz, Mariana P.

    2014-11-01

    Solute and heat fluxes from thermal springs of Tacaná volcano are estimated by the chloride-inventory method. The thermal springs, located at the northwestern slopes of the volcanic edifice, at altitudes from 1500 to 2000 m above sea level, discharge water enriched in HCO3 and SO4 (up to 1 g kg- 1 of each one) with temperatures in the 25-63 °C range. There are two distinct groups of springs with a different 'chloride-temperature' correlation but with the same 87Sr/86Sr ratio (0.7046 ± 0.0001) indicating the same wall rock composition for different aquifers. Each thermal spring feeds a thermal stream that flows into the main drainage of the area, Río Coatán. The total observed chloride discharge from the thermal springs is estimated as 14.8 g s- 1 and the total measured heat output of ~ 9.5 MW. Considering a deep fluid temperature of 250 °C (calculated using Na-K geothermometer), the corresponding advective heat transport from the deep reservoirs that feed these springs may be estimated as 26 MWt. However, the total chloride output measured in the main drainage (Coatán river) is 4 times higher (~ 59 g s- 1) than the measured Cl output of thermal springs. This means that other, undiscovered, thermal springs exist in the area and that the natural heat output through thermal springs at Tacaná is significantly higher and depends on the Cl content and temperatures of the unknown thermal water discharges. If chloride concentration in these unknown springs does not exceed 540 mg L- 1 (the highest analyzed Cl in Tacaná springs) and the discharge temperature is 50 °C, then the natural heat output can be estimated at least as 22 MWt and the corresponding advective heat transport as ~ 100 MWt.

  15. The 1982 eruptions of El Chichon volcano, Mexico (3): Physical properties of pyroclastic surges

    Science.gov (United States)

    Sigurdsson, H.; Carey, S. N.; Fisher, R. V.

    1987-04-01

    Two major pyroclastic surges generated during the 4 April 1982 eruption of El Chichon devastated an area of 153 km2 with a quasi-radial distribution around the volcano. The hot surge clouds carbonized wood throughout their extent and were too hot to allow accretionary lapilli formation by vapor condensation. Field evidence indicates voidage fraction of 0.99 in the surge cloud with extensive entrainment of air. Thermal calculations indicate that heat content of pyroclasts can heat entrained air and maintain high temperatures in the surge cloud. The dominant bed form of the surge deposits are sand waves shaped in dune forms with vertical form index of 10 20, characterized by stoss-side erosion and lee-side deposition of 1 10 cm reversely graded laminae. A systematic decrease in maximum lithic diameter with distance from source is accompanied by decrease in wavelength and amplitude. Modal analysis indicates fractionation of glass and pumice from the surge cloud relative to crystals, resulting in loss of at least 10% 25% of the cloud mass due to winnowing out of fines during surge emplacement. Greatest fractionation from the -1.0 0.0-∅ grain sizes reflects relatively lower pumice particle density in this range and segregation in the formative stages of the surge cloud. Extensive pumice rounding indicates abrasion during bed-load transport. Flow of pyroclastic debris in the turbulent surge cloud was by combination of bed-load and suspended-load transport. The surges are viewed as expanding pyroclastic gravity flows, which entrain and mix with air during transport. The balance between sedimentation at the base of the surge cloud and expansion due to entrainment of air contributed to low cloud density and internal turbulence, which persisted to the distal edge of the surge zone.

  16. Smoothed particle hydrodynamic modeling of volcanic debris flows: Application to Huiloac Gorge lahars (Popocatépetl volcano, Mexico)

    Science.gov (United States)

    Haddad, Bouchra; Palacios, David; Pastor, Manuel; Zamorano, José Juan

    2016-09-01

    Lahars are among the most catastrophic volcanic processes, and the ability to model them is central to mitigating their effects. Several lahars recently generated by the Popocatépetl volcano (Mexico) moved downstream through the Huiloac Gorge towards the village of Santiago Xalitzintla. The most dangerous was the 2001 lahar, in which the destructive power of the debris flow was maintained throughout the extent of the flow. Identifying the zone of hazard can be based either on numerical or empirical models, but a calibration and validation process is required to ensure hazard map quality. The Geoflow-SPH depth integrated numerical model used in this study to reproduce the 2001 lahar was derived from the velocity-pressure version of the Biot-Zienkiewicz model, and was discretized using the smoothed particle hydrodynamics (SPH) method. The results of the calibrated SPH model were validated by comparing the simulated deposit depth with the field depth measured at 16 cross sections distributed strategically along the gorge channel. Moreover, the dependency of the results on topographic mesh resolution, initial lahar mass shape and dimensions is also investigated. The results indicate that to accurately reproduce the 2001 lahar flow dynamics the channel topography needed to be discretized using a mesh having a minimum 5 m resolution, and an initial lahar mass shape that adopted the source area morphology. Field validation of the calibrated model showed that there was a satisfactory relationship between the simulated and field depths, the error being less than 20% for 11 of the 16 cross sections. This study demonstrates that the Geoflow-SPH model was able to accurately reproduce the lahar path and the extent of the flow, but also reproduced other parameters including flow velocity and deposit depth.

  17. Long-range hazard assessment of volcanic ash dispersal for a Plinian eruptive scenario at Popocatépetl volcano (Mexico): implications for civil aviation safety

    Science.gov (United States)

    Bonasia, Rosanna; Scaini, Chirara; Capra, Lucia; Nathenson, Manuel; Siebe, Claus; Arana-Salinas, Lilia; Folch, Arnau

    2013-01-01

    Popocatépetl is one of Mexico’s most active volcanoes threatening a densely populated area that includes Mexico City with more than 20 million inhabitants. The destructive potential of this volcano is demonstrated by its Late Pleistocene–Holocene eruptive activity, which has been characterized by recurrent Plinian eruptions of large magnitude, the last two of which destroyed human settlements in pre-Hispanic times. Popocatépetl’s reawakening in 1994 produced a crisis that culminated with the evacuation of two villages on the northeastern flank of the volcano. Shortly after, a monitoring system and a civil protection contingency plan based on a hazard zone map were implemented. The current volcanic hazards map considers the potential occurrence of different volcanic phenomena, including pyroclastic density currents and lahars. However, no quantitative assessment of the tephra hazard, especially related to atmospheric dispersal, has been performed. The presence of airborne volcanic ash at low and jet-cruise atmospheric levels compromises the safety of aircraft operations and forces re-routing of aircraft to prevent encounters with volcanic ash clouds. Given the high number of important airports in the surroundings of Popocatépetl volcano and considering the potential threat posed to civil aviation in Mexico and adjacent regions in case of a Plinian eruption, a hazard assessment for tephra dispersal is required. In this work, we present the first probabilistic tephra dispersal hazard assessment for Popocatépetl volcano. We compute probabilistic hazard maps for critical thresholds of airborne ash concentrations at different flight levels, corresponding to the situation defined in Europe during 2010, and still under discussion. Tephra dispersal mode is performed using the FALL3D numerical model. Probabilistic hazard maps are built for a Plinian eruptive scenario defined on the basis of geological field data for the “Ochre Pumice” Plinian eruption (4965 14C

  18. Glacier melting during lava dome growth at Nevado de Toluca volcano (Mexico): Evidences of a major threat before main eruptive phases at ice-caped volcanoes

    Science.gov (United States)

    Capra, L.; Roverato, M.; Groppelli, G.; Caballero, L.; Sulpizio, R.; Norini, G.

    2015-03-01

    Nevado de Toluca volcano is one of the largest stratovolcanoes in the Trans-Mexican Volcanic Belt. During Late Pleistocene its activity was characterized by large dome growth and subsequent collapse emplacing large block and ash flow deposits, intercalated by Plinian eruptions. Morphological and paleoclimate studies at Nevado de Toluca and the surrounding area evidenced that the volcano was affected by extensive glaciation during Late Pleistocene and Holocene. During the older recognized glacial period (27-60 ka, MIS 3), the glacier was disturbed by the intense magmatic and hydrothermal activity related to two dome extrusion episodes (at 37 ka and 28 ka). Glacier reconstruction indicates maximum ice thickness of 90 m along main valleys, as at the Cano ravines, the major glacial valley on the northern slope of the volcano. Along this ravine, both 37 and 28 ka block-and-ash deposits are exposed, and they directly overlay a fluviatile sequence, up to 40 m-thick, which 14C ages clearly indicate that their emplacement occurred just before the dome collapsed. These evidences point to a clear interaction between the growing dome and its hydrothermal system with the glacier. During dome growth, a large amount of melting water was released along major glacial valleys forming thick fluvioglacial sequences that were subsequently covered by the block-and-ash flow deposits generated by the collapse of the growing dome. Even though this scenario is no longer possible at the Nevado de Toluca volcano, the data presented here indicate that special attention should be paid to the possible inundation areas from fluviatile/lahar activity prior to the main magmatic eruption at ice-capped volcanoes.

  19. Late Holocene stratigraphy of the Tetimpa archaeological sites, northeast flank of Popocatepetl volcano, central Mexico

    Science.gov (United States)

    Panfil, M.S.; Gardner, T.W.; Hirth, K.G.

    1999-01-01

    Late Holocene (240 km2 on the east side of the volcano with >25 cm of tephra. Lavas from eruptive sequence I dammed drainage in the lowland area near the town of San Nicolas and caused local upstream deposition of as much as 30 m of lacustrine silts, clays, and sands. These lacustrine deposits record an eruptive hiatus for the Tetimpa area of about 750 14C yr: between ca. 2100 and ca. 1350 yr B.P., no major tephras were deposited in the Tetimpa area. In upland areas, this time period is represented by an unconformity and by Entisols formed in the top of pumice deposits and lavas from eruptive sequence I. Artifacts, agricultural furrows, and dwellings record human reoccupation of this surface. At the end of this hiatus, several lahars were deposited above the lacustrine sequence and locally above the Entisol in upland positions adjacent to streams. Between ca. 1350 and ca. 1200 yr B.P., tephras from eruptive sequence II buried these paleosols, occupation sites, lacustrine sediments, and lahars. Andesitic (~62% SiO2) pumice lapilli deposits in the Tetimpa area record three pumice-fall eruptions directed northeast and east of the crater. The first and smallest of these (maximum Tetimpa area thickness = 12 cm; >52 km2 covered by >25 cm) took place at ca. 1350 yr B.P. and was accompanied by pyroclastic surge events preserved in the Tetimpa area by charcoal, sand waves, and cross-stratified sand-sized tephra. At ca. 1200 yr B.P., the products of two Plinian-style events and additional pyroclastic surges reached the Tetimpa area. The largest of these tephra-fall events covered the Tetimpa area with 0.5-1 m of tephra and blanketed an area of >230 km2 with a thickness of >25 cm. The Tetimpa record confirms two of the four periods of explosive volcanism recognized by studies conducted around Popocatepetl in the past 30 yr. Eruptive sequence I corresponds to the explosive period between 2100 and 2500 yr B.P., and eruptive sequence II corresponds to the period between 900 and

  20. Plio-pleistocene volcano-tectonic evolution of la Reforma Caldera, Baja California, Mexico

    Science.gov (United States)

    Demant, Alain; Ortlieb, Luc

    1981-01-01

    La Reforma volcanic complex, in east-central Baja California, shows a characteristic caldera structure, 10 km in diameter. The first eruptive stage, during the Pliocene, was manifested by ash and pumice falls and by subaqueous pumitic flows. In a second stage basic flows were deposited in a near-shore environment (subaerial and pillow lavas). During the early Pleistocene a large ignimbritic eruption, producing mainly pantelleritic tuffs, immediately predated the formation of the caldera itself. Afterwards, along marginal fractures of the caldera, some rhyolitic domes and flows partially covered the thick ignimbritic sheet. A block of Miocene substratum, in the center of the caldera, has been uplifted, nearly 1 km, by "resurgent doming". Small outcrops of diorite might constitute the top of coarse-grained crystallized magmatic bodies, and thus support the "resurgent doming" interpretation. A few basaltic cones were finally built on the flanks of the caldera complex; the latter are not related to the caldera history but to the extension tectonics of the Gulf of California which are also responsible for the Tortuga Island and the Holocene Tres Virgenes tholeiitic cones. South of la Reforma are found the highest (+300 m) Pleistocene marine deposits of the Gulf coast of Baja California. The uplift of this area is due in part to the positive epeirogenic movements of the whole peninsular crustal block, and also to the late doming of the caldera. On the coastal (eastern) flank of La Reforma complex up to seven stepped wave-cut terraces have been preserved, the highest reaching more than +150 m and the lowest ones +25 m. Lateral correlations of the marine terraces along the whole Gulf of California suggest that this volcano-tectonic uplift, that is still active, is of the order of 240 mm/10 3 y. The set of terraces is interpreted to be Middle (700-125 × 10 3y) to Upper (125-80 × 10 3y) Pleistocene, and is tentatively correlated with the paleoclimatic chronology of deep

  1. Isotopic, chemical and dissolved gas constraints on spring water from Popocatepetl volcano (Mexico): evidence of gas water interaction between magmatic component and shallow fluids

    Science.gov (United States)

    Inguaggiato, S.; Martin-Del Pozzo, A. L.; Aguayo, A.; Capasso, G.; Favara, R.

    2005-03-01

    Geochemical research was carried out on cold and hot springs at Popocatepetl (Popo) volcano (Mexico) in 1999 to identify a possible relationship with magmatic activity. The chemical and isotopic composition of the fluids is compatible with strong gas-water interaction between deep and shallow fluids. In fact, the isotopic composition of He and dissolved carbon species is consistent with a magmatic origin. The presence of a geothermal system having a temperature of 80-100° C was estimated on the basis of liquid geothermometers. A large amount of dissolved CO 2 in the springs was also detected and associated with high CO 2 degassing.

  2. Comments on cladocerans of crater lakes of the Nevado de Toluca Volcano (Central Mexico), with the description of a new species, Alona manueli sp. nov.

    Science.gov (United States)

    Sinev, Artem Y; Zawisza, Edyta

    2013-01-01

    Cladoceran communities of two lakes of Nevado de Toluca Volcano, Central Mexico, were studied. A new species of Aloninae, Alona manueli sp. nov., is described. It was previously confused with Palearctic Alona intermedia Sars, 1862, but clearly differs from it in the morphology of postabdomen, head shield and head pores, and thoracic limbs. Position of Alona manueli sp. nov. within the genus is unclear, it did not belong to any species-group within Alona s. lato. Other species recorded in the studied lakes are Alona ossiani Sinev, 1998, Alonella pulchella Herrick, 1884, Chydorus belonging to sphaericus-group, Eurycercus longirostris Hann, 1982 and Pleuroxus cf. denticulatus Birge, 1879.

  3. Crater lake and post-eruption hydrothermal activity, El Chichón Volcano, Mexico

    Science.gov (United States)

    Casadevall, Thomas J.; de la Cruz-Reyna, Servando; Rose, William I.; Bagley, Susan; Finnegan, David L.; Zoller, William H.

    1984-01-01

    Explosive eruptions of Volcán El Chichón in Chiapas, Mexico on March 28 and April 3–4, 1982 removed 0.2 km3 of rock to form a 1-km-wide 300-m-deep summit crater. By late April 1982 a lake had begun to form on the crater floor, and by November 1982 it attained a maximum surface area of 1.4 × 105 m2 and a volume of 5 × 106 m3. Accumulation of 4–5 m of rainfall between July and October 1982 largely formed the lake. In January 1983, temperatures of fumaroles on the crater floor and lower crater walls ranged from 98 to 115°C; by October 1983 the maximum temperature of fumarole emissions was 99°C. In January 1983 fumarole gas emissions were greater than 99 vol. % H2O with traces of CO2, SO2, and H2S. The water of the lake was a hot (T = 52–58°C), acidic (pH = 0.5), dilute solution (34,046 mg L−1 dissolved solids; Cl/S = 20.5). Sediment from the lake contains the same silicate minerals as the rocks of the 1982 pyroclastic deposits, together with less than 1% of elemental sulfur. The composition and temperature of the lake water is attributed to: (1) solution of fumarole emissions; (2) reaction of lake water with hot rocks beneath the lake level; (3) sediments washed into the lake from the crater walls; (4) hydrothermal fluids leaching sediments and formational waters in sedimentary rocks of the basement; (5) evaporation; and (6) precipitation.

  4. Renewed Volcano-Stratigraphc Studies of Calderas with Geothermal Potential in Mexico

    Science.gov (United States)

    Macias, J. L.; Arce, J. L.; García-Tenorio, F.; Layer, P. W.; Saucedo, R.; Castro, R.; Garduño, V. H.; Jimenez, A.; Pérez, H.; Valdez, G.; Meriggi, L.

    2014-12-01

    During the past six years we have carried out volcanologic fieldwork either in active geothermal fields in Mexico (Los Azufres, Tres Vírgenes, and Cerro Prieto) or in potential sites in which some geothermal exploration studied had been done by the National Power Company (CFE). These studies have been very successful in reassessing the location of the geothermal reservoirs within the volcanic successions through detailed mapping of the volcanic units using high resolution topography and satellite imagery to produce 3-D imagery in conjunction with field work to produce preliminary geologic maps. Detailed stratigraphy of volcanic units, assisted with 40Ar/39Ar and radiocarbon geochronology have redefined the evolution of some of these complexes. For example, our studies at Los Azufres geothermal field located in the State of Michoacán indicate that the volcanic complex of the same name sits upon a structural high transected by E-W faults related to the youngest structures of the Trans-Mexican Volcanic Belt. The volcanic complex has been emplaced during the past ~1.5 Ma. During this time, magmas evolved from basaltic to rhyolitic in composition with the emplacement of circa 100 vents. Several landforms have undergone intense hydrothermal alteration and, in some cases, generated debris avalanches. The revised stratigraphy based on drill holes and new dates of cores suggested that the geothermal reservoir is hosted in Miocene rocks bracketed between the Miocene Sierra de Mil Cumbres volcanics (17-22 Ma) and the products of the volcanic field itself. Similar studies will be carried out at four other Pleistocene calderas (Acoculco, La Primavera, Aguajito and Reforma) attempting to refine their volcanic stratigraphy, evolution, and the location of the geothermal system, and those results will help in the design of exploration strategies for geothermal sources.

  5. Morphological analysis of Nevado de Toluca volcano (Mexico): new insights into the structure and evolution of an andesitic to dacitic stratovolcano

    Science.gov (United States)

    Norini, Gianluca; Groppelli, Gianluca; Capra, Lucia; De Beni, Emanuela

    2004-09-01

    We present a morphological analysis of Nevado de Toluca volcano located 80 km WSW of Mexico City based on digital elevation model study, where slope and aspect maps have been generated and analysed. Aerial photograph and satellite image observations improve the morphological analysis. The synoptic view which is offered by this analysis allowed for recognition and localization of the main volcanic and tectonic features of the area. On the basis of digital elevation model value distribution and surface textures, five morphological domains were defined. The most interesting domain, south of the crater, reflects the occurrence of an ancient complex volcano distinct from the adjacent areas. Interaction between the volcanic and volcano-tectonic evolution and the basement produced the other domains. Single volcanic edifices, like lava domes and scoria cones, and eruptive fractures were recognized. Finally, flank collapse scarps opened to the east and to the north were identified and four relevant morphostructural lineaments and their possible role in the Nevado de Toluca geological and structural evolution are discussed.

  6. Assessing landslide susceptibility, hazards and sediment yield in the Río El Estado watershed, Pico de Orizaba volcano, Mexico

    Science.gov (United States)

    Legorreta Paulin, G.; Bursik, M. I.; Lugo Hubp, J.; Aceves Quesada, J. F.

    2014-12-01

    This work provides an overview of the on-going research project (Grant SEP-CONACYT # 167495) from the Institute of Geography at the National Autonomous University of Mexico (UNAM) that seeks to conduct a multi-temporal landslide inventory, analyze the distribution of landslides, and characterize landforms that are prone to slope instability by using Geographic Information Systems (GIS). The study area is the Río El Estado watershed that covers 5.2 km2 and lies on the southwestern flank of Pico de Orizaba volcano.The watershed was studied by using aerial photographs, fieldwork, and adaptation of the Landslide Hazard Zonation Protocol of the Washington State Department of Natural Resources, USA. 107 gravitational slope failures of six types were recognized: shallow landslides, debris-avalanches, deep-seated landslides, debris flows, earthflows, and rock falls. This analysis divided the watershed into 12 mass-wasting landforms on which gravitational processes occur: inner gorges, headwalls, active scarps of deep-seated landslides, meanders, plains, rockfalls, non-rule-identified inner gorges, non-rule-identified headwalls, non-rule-identified converging hillslopes and three types of hillslopes classified by their gradient: low, moderate, and high. For each landform the landslide area rate and the landslide frequency rate were calculated as well as the overall hazard rating. The slope-stability hazard rating has a range that goes from low to very high. The overall hazard rating for this watershed was very high. The shallow slide type landslide was selected and area and volume of individual landslides were retrieved from the watershed landslide inventory geo-database, to establish an empirical relationship between area and volume that takes the form of a power law. The relationship was used to estimate the total volume of landslides in the study area. The findings are important to understand the long-term evolution of the southwestern flank stream system of Pico de

  7. Petrogenesis and metal budget of Pelagatos volcano in the Chichinautzin monogenetic field, Mexico: A Melt Inclusion Study

    Science.gov (United States)

    Roberge, J.; Mercer, C. N.; Kent, A. J.; Guilbaud, M.

    2013-12-01

    Melt inclusions are now widely used to quantify pre-eruptive volatile contents and to track the compositional evolution of magma. In recent years, the use of melt inclusions has also increased markedly for research in economic geology. Melt inclusions are becoming a powerful tool to track metal contents in ore-forming magmatic reservoirs and metals like Ag, Cu, Li, Mo, Sn, Pb, W, Zn are now commonly included in trace element analyses. Investigating metal reservoirs in currently active volcanic systems provides insight into the conditions that favor mineralization in ore-forming deposits compared to barren systems. In this work, we present volatiles (H2O, CO2, S, Cl) and major and trace element contents of olivine-hosted melt inclusion from 4 samples spanning the entire eruption of Pelagatos scoria cone. Pelagatos is a small and young (less than 14 000 years B.P.) monogenetic volcano within the Sierra Chichinautzin volcanic field located in the central portion of the Trans Mexican Volcanic Belt (south-east of Mexico City). The melt inclusions are basaltic andesite to andesite in composition, with 1.84 - 6.02 wt% MgO, 51.95 - 59.21 wt% SiO2 and 0.64 - 1.55 wt% K2O. The H2O varies from 0.5 to 4.3 wt% whereas CO2 varies from below detection up to 976 ppm. Sulfur contents vary from 35 to 1451 ppm, showing a decrease with increasing MgO content suggesting that S is being lost with progressive differentiation, but since S concentrations do not correlate with any other gas phase (H2O, CO2, Cl) we hypothesize that it partitioned into an immiscible fluid or mineral phase. On the other hand, Cl contents are broadly constant (900 to 1267 ppm), and shows no correlation with MgO or K2O. All analyzed metals (Ag, Cu, Li, Mo, Sn, Pb, W, Zn ) behave incompatibly showing a positive correlation with La. Cu (18 to 82 ppm), Pb (2 to 8 ppm) Zn (30 to 107 ppm) and Mo correlate positively together indicating that fractional crystallization concentrates these elements. These results provide

  8. Scientific and public responses to the ongoing volcanic crisis at Popocatépetl Volcano, Mexico: Importance of an effective hazards-warning system

    Science.gov (United States)

    de la Cruz-Reyna, Servando; Tilling, Robert I.

    2008-01-01

    Volcanic eruptions and other potentially hazardous natural phenomena occur independently of any human actions. However, such phenomena can cause disasters when a society fails to foresee the hazardous manifestations and adopt adequate measures to reduce its vulnerability. One of the causes of such a failure is the lack of a consistent perception of the changing hazards posed by an ongoing eruption, i.e., with members of the scientific community, the Civil Protection authorities and the general public having diverging notions about what is occurring and what may happen. The problem of attaining a perception of risk as uniform as possible in a population measured in millions during an evolving eruption requires searching for communication tools that can describe—as simply as possible—the relations between the level of threat posed by the volcano, and the level of response of the authorities and the public. The hazards-warning system adopted at Popocatépetl Volcano, called the Volcanic Traffic Light Alert System(VTLAS), is a basic communications protocol that translates volcano threat into seven levels of preparedness for the emergency-management authorities, but only three levels of alert for the public (color coded green–yellow–red). The changing status of the volcano threat is represented as the most likely scenarios according to the opinions of an official scientific committee analyzing all available data. The implementation of the VTLAS was intended to reduce the possibility of ambiguous interpretations of intermediate levels by the endangered population. Although the VTLAS is imperfect and has not solved all problems involved in mass communication and decision-making during a volcanic crisis, it marks a significant advance in the management of volcanic crises in Mexico.

  9. Scientific and public responses to the ongoing volcanic crisis at Popocatépetl Volcano, Mexico: Importance of an effective hazards-warning system

    Science.gov (United States)

    De la Cruz-Reyna, Servando; Tilling, Robert I.

    2008-02-01

    Volcanic eruptions and other potentially hazardous natural phenomena occur independently of any human actions. However, such phenomena can cause disasters when a society fails to foresee the hazardous manifestations and adopt adequate measures to reduce its vulnerability. One of the causes of such a failure is the lack of a consistent perception of the changing hazards posed by an ongoing eruption, i.e., with members of the scientific community, the Civil Protection authorities and the general public having diverging notions about what is occurring and what may happen. The problem of attaining a perception of risk as uniform as possible in a population measured in millions during an evolving eruption requires searching for communication tools that can describe—as simply as possible—the relations between the level of threat posed by the volcano, and the level of response of the authorities and the public. The hazards-warning system adopted at Popocatépetl Volcano, called the Volcanic Traffic Light Alert System (VTLAS), is a basic communications protocol that translates volcano threat into seven levels of preparedness for the emergency-management authorities, but only three levels of alert for the public (color coded green-yellow-red). The changing status of the volcano threat is represented as the most likely scenarios according to the opinions of an official scientific committee analyzing all available data. The implementation of the VTLAS was intended to reduce the possibility of ambiguous interpretations of intermediate levels by the endangered population. Although the VTLAS is imperfect and has not solved all problems involved in mass communication and decision-making during a volcanic crisis, it marks a significant advance in the management of volcanic crises in Mexico.

  10. Mexico.

    Science.gov (United States)

    Semaan, Leslie

    The text explores Mexico's history, geography, art, religion, and lifestyles in the context of its complex economy. The text focuses on Mexico's economy and reasons for its current situation. Part I of this teaching unit includes: Teacher Overview, Why Study Mexico, Mexico Fact Sheet, Map of Mexico, the Land and Climate, History, Government,…

  11. The age and composition of the pre-Cenozoic basement of the Jalisco Block: implications for and relation to the Guerrero composite terrane

    Science.gov (United States)

    Valencia, Victor A.; Righter, Kevin; Rosas-Elguera, Jose; López-Martínez, Margarita; Grove, Marty

    2013-09-01

    The Jalisco Block is thought to be part of the Guerrero terrane, but the nature and age of the underlying crystalline basement are largely unknown. We have collected a suite of schists, granitoids, and weakly metamorphosed marine sediments from various parts of the Jalisco Block including Atenguillo and Ameca, Mascota and San Sebastián, Cuale, Puerto Vallarta, Punta Mita, Yelapa, and Tomatlán. The schists range in age from 135 to 161 Ma, with many exhibiting Proterozoic and Phanerozoic zircon ages. The granitoids range in age from 65 to 90 Ma, and are calc-alkaline compositionally—similar to granitoids from the Puerto Vallarta and Los Cabos batholiths. The Jalisco granitoids also experienced similar uplift rates to granitoids from the regions to the north and south of the Jalisco Block. The marine sediments yield a maximum depositional age of 131 Ma, and also contain a significant zircon population with ages extending back to the Archean. Granitoids from this study define two age groups, even after the effects of thermal resetting and different closure temperatures are considered. The 66.8-Ma silicic ash flow tuff near Union de Tula significantly expands the extent of this Cretaceous-Paleocene age ash flow tuff unit within the Jalisco Block, and we propose calling the unit "Carmichael silicic ash flow tuff volcanic succession" in honor of Ian Carmichael. The ages of the basement schists in the Jalisco Block fully overlap with the ages of terranes of continental Mexico, and other parts of the Guerrero terrane in the south, confirming the autochthonous origin of the Jalisco Block rather than exotic arc or allochthonous origin. Geologic data, in combination with geochronologic and oxygen isotopic data, suggest the evolution of SW Mexico with an early 200-1,200-Ma passive margin, followed by steep subduction in a continental arc setting at 160-165 Ma, then shallower subduction by 135 Ma, and finally, emplacement of granitoids at 65-90 Ma.

  12. The anatomy of a cinder cone: preliminary paleomagnetic, rock magnetic, structural, and petrologic data from the La Cienega volcano, Cerros del Rio volcanic field, northern New Mexico

    Science.gov (United States)

    Petronis, M. S.; Foucher, M.; Lineline, J.; Van Wyk de Vries, B.

    2011-12-01

    The Cerros del Rio volcanic field is one of several middle Pliocene to Pleistocene basaltic volcanic fields of the axial Rio Grande Rift in central and northern New Mexico. It is a monogenetic volcanic field that comprises about 60 cinder-spatter cones, occupies ~ 700 km2, and ranges in age from 2.7 Ma to 1.1 Ma. Eruptive centers are typically central vent volcanoes, ranging from low-relief shields to steep-sided, breached cinder and spatter cone remnants. They represent short eruptive events that likely were derived from rapidly evolving reservoir-conduit systems. Mining activity has exposed the volcanic plumbing system of the Cienega Mine cinder cone, just west of Santa Fe, NM. Here, geologists from France and USA have been investigating the exposed roots of this eviscerated Pliocene volcano to investigate magma conduit geometry, magma flow structures, and eruption patterns. We are testing models for magma transport and volcano construction using a variety of field and laboratory tools. Common models of volcanic construction envision the magma feeder as a dike or pipe-like conduit transporting molten rock from a deep reservoir to the eruptive vent. We posit that small volcanic pluming systems are inherently more complex and actually involve numerous feeder geometries throughout the volcano lifespan. Our preliminary work suggests that the simple exteriors of some cinder cones hide a long life and complex history, both of which would change the appreciation of the related volcanic hazards in active systems. The Cienega Mine cinder cone consists of several meter- to decimeter-wide intrusions that connect to eruptive centers. These intrusions show a continuity of brittle to ductile structures from their margins to interiors. We have collected samples across each intrusion as well as along strike for anisotropy of magnetic susceptibility (AMS) and petrographic analysis in order to establish magma flow patterns. AMS results yield a remarkably consistent dataset that

  13. Metal enrichment of soils following the April 2012-2013 eruptive activity of the Popocatépetl volcano, Puebla, Mexico.

    Science.gov (United States)

    Rodriguez-Espinosa, P F; Jonathan, M P; Morales-García, S S; Villegas, Lorena Elizabeth Campos; Martínez-Tavera, E; Muñoz-Sevilla, N P; Cardona, Miguel Alvarado

    2015-11-01

    We analyzed the total (Zn, Pb, Ni, Hg, Cr, Cd, Cu, As) and partially leachable metals (PLMs) in 25 ash and soil samples from recent (2012-2013) eruptions of the Popocatépetl Volcano in Central Mexico. More recent ash and soil samples from volcanic activity in 2012-2013 had higher metal concentrations than older samples from eruptions in 1997 suggesting that the naturally highly volatile and mobile metals leach into nearby fresh water sources. The higher proportions of As (74.72%), Zn (44.64%), Cu (42.50%), and Hg (32.86%) reflect not only their considerable mobility but also the fact that they are dissolved and accumulated quickly following an eruption. Comparison of our concentration patterns with sediment quality guidelines indicates that the Cu, Cd, Cr, Hg, Ni, and Pb concentrations are higher than permissible limits; this situation must be monitored closely as these concentrations may reach lethal levels in the future.

  14. A voluminous avalanche-induced lahar from Citlaltépetl volcano, Mexico: Implications for hazard assessment

    Science.gov (United States)

    Carrasco-Núñez, Gerardo; Vallance, James W.; Rose, William I.

    1993-12-01

    During the late Pleistocene the ancestral edifice of Citlaltépetl volcano (also known as Pico de Orizaba) collapsed to form a clay-rich deposit that extends 85 km from its source, has a volume of 1.8 km 3, and covers an area of 143 km 2 east of the volcano. The deposit has clay content ranging from 10 to 16% and contains secondary alteration minerals such as smectite and kaolinite. The deposit's features suggest that it had an origin as a sector collapse of hydrothermally altered rock that transformed from a debris avalanche to a cohesive lahar very close to its source. The presence of glacier ice and a hydrothermal system during late Pleistocene times apparently provided a source of pore water which enhanced the hydrothermal alteration of the summit of Citlaltépetl and was the origin of most of the water for the lahar. This deposit and several others suggest that glaciated volcanoes are sites where hydrothermal alteration and resulting cohesive lahars are most likely. Although cohesive lahars and debris avalanches both have origins as sector collapses, cohesive lahars are more mobile than similar-sized debris avalanches. Thus potential hazard of edifice collapse at glaciated volcanoes, especially those with large volumes of hydrothermally altered rock, includes the possibility of large-volume cohesive lahars.

  15. Archeomagnetic dating of the eruption of Xitle volcano (Mexico) from a reappraisal of the paleointensity with the MSP-DSC protocol.

    Science.gov (United States)

    Bravo-Ayala, Manuel; Camps, Pierre; Alva-Valdivia, Luis; Poidras, Thierry; Nicol, Patrick

    2014-05-01

    The Xitle volcano, located south of Mexico City, is a monogenic volcano that has provided seven lava flows in a time interval of a few years. The age of these eruptions, estimated by means of radiocarbon dates on charcoal from beneath the flows, is still very poorly known, ranging from 4765±90 BC to 520±200 AD (see Siebe, JVGR, 2000 for a review). This lava field was emplaced over the archaeological city of Cuicuilco whose occupation is estimated between 700 BC and 150 AD. Thus a question is still pending: Is the downfall of Cuicuilco directly attributable to the eruption of Xitle? It seems that the answer is negative if we consider the latest radiocarbon dating by Siebe (2000), which sets the age of the eruption to 280±35 AD, that is significantly younger to the abandon of the city. Because this new age has direct implications on the history of the movements of ancient populations in the Central Valley of Mexico, we propose in the present study to check this estimate by archaeomagnetic dating. Xitle lava have been investigated several times for paleomagnetism, including directional analyses and absolute paleointensity determinations (see Alva, EPS, 57, 839-853, 2005 for a review). The characteristic Remanence direction is precisely determined. It is much more difficult to estimate precisely the paleointensity with the Thellier method: values scatter between 40 and 90 μT in a single flow (Alva, 2005). We propose here to estimate the paleointensity by means of the MSP-DSC protocol (Fabian and Leonhardt, 2010) with the new ultra-fast heating furnace FUReMAG developed in Montpellier (France). The sampling was performed along four profiles, one vertical through the entire thickness of the flow and three horizontal (at the top, middle and the bottom of the flow). Our preliminary results show that there is no difference between the values found in the different profiles, all providing a value around 62 μT. The comparison of our results (Dec = 359.0°, Inc = 35.2

  16. Gender differences and regionalization of the cultural significance of wild mushrooms around La Malinche volcano, Tlaxcala, Mexico.

    Science.gov (United States)

    Montoya, A; Torres-García, E A; Kong, A; Estrada-Torres, A; Caballero, J

    2012-01-01

    The purpose of this study was to determine the cultural significance of wild mushrooms in 10 communities on the slopes of La Malinche volcano, Tlaxcala. The frequency and order of mention of each mushroom species in interviews of 200 individuals were used as indicators of the relative cultural significance of each species. A X(2) analysis was used to compare the frequency of mention of each species between males and females, and a Mann-Whitney U test was used to compare the difference in the total number of fungi mentioned by either gender. Traditional names for mushroom species were documented and frequency of mention assessed through multivariate statistics. The fungi with highest frequency of mention were Amanita basii, Lyophyllum decastes, Boletus pinophilus, Gomphus floccosus and Cantharellus cibarius complex. We found significant differences in the frequency of mention of different fungi by males and females but no significant difference was found for the total number of fungi mentioned by either gender. Principal component analysis suggested a cultural regionalization of La Malinche volcano communities based on preferences for consumption and use of traditional names. We observed two groups: one formed by communities on the eastern part of the volcano (with mixed cultures) and the other including communities on the western slope (ethnic Nahua towns). San Isidro Buensuceso is the most distinct community, according to the criteria in this study.

  17. Hydrochemical dynamics of the “lake spring” system in the crater of El Chichón volcano (Chiapas, Mexico)

    Science.gov (United States)

    Rouwet, D.; Taran, Y.; Inguaggiato, S.; Varley, N.; Santiago Santiago, J. A.

    2008-12-01

    El Chichón volcano (Chiapas, Mexico) erupted violently in March-April 1982, breaching through the former volcano-hydrothermal system. Since then, the 1982 crater has hosted a shallow (1-3.3 m, acidic (pH ˜ 2.2) and warm (˜ 30 °C) crater lake with a strongly varying chemistry (Cl/SO 4 = 0-79 molar ratio). The changes in crater lake chemistry and volume are not systematically related to the seasonal variation of rainfall, but rather to the activity of near-neutral geyser-like springs in the crater (Soap Pool). These Soap Pool springs are the only sources of Cl for the lake. Their geyser-like behaviour with a long-term (months to years) periodicity is due to a specific geometry of the shallow boiling aquifer beneath the lake, which is the remnant of the 1983 Cl-rich (24,000 mg/l) crater lake water. The Soap Pool springs decreased in Cl content over time. The zero-time extrapolation (1982, year of the eruption) approaches the Cl content in the initial crater lake, meanwhile the extrapolation towards the future indicates a zero-Cl content by 2009 ± 1. This particular situation offers the opportunity to calculate mass balance and Cl budget to quantify the lake-spring system in the El Chichón crater. These calculations show that the water balance without the input of SP springs is negative, implying that the lake should disappear during the dry season. The isotopic composition of lake waters (δD and δ 18O) coincide with this crater lake-SP dynamics, reflecting evaporation processes and mixing with SP geyser and meteoric water. Future dome growth, not observed yet in the post-1982 El Chichón crater, may be anticipated by changes in lake chemistry and dynamics.

  18. Pre-eruptive conditions of dacitic magma erupted during the 21.7 ka Plinian event at Nevado de Toluca volcano, Central Mexico

    Science.gov (United States)

    Arce, J. L.; Gardner, J. E.; Macías, J. L.

    2013-01-01

    The Nevado de Toluca volcano in Central Mexico has been active over the last ca. 42 ka, during which tens of km3 of pyroclastic material were erupted and two important Plinian-type eruptions occurred at ca. 21.7 ka (Lower Toluca Pumice: LTP) and ca. 10.5 ka (Upper Toluca Pumice: UTP). Samples from both the LTP and UTP contain plagioclase, amphibole, iron-titanium oxides, and minor anhedral biotite, set in a vesicular, rhyolitic, glassy matrix. In addition, UTP dacites contain orthopyroxene. Analysis of melt inclusions in plagioclase phenocrysts yields H2O contents of 2-3.5 wt.% for LTP and 1.3-3.6 wt.% for UTP samples. Ilmenite-ulvospinel geothermometry yields an average temperature of ~ 868 °C for the LTP magma (hotter than the UTP magma, ~ 842 °C; Arce et al., 2006), whereas amphibole-plagioclase geothermometry yields a temperature of 825-859 °C for the LTP magma. Water-saturated experiments using LTP dacite suggest that: (i) amphibole is stable above 100 MPa and below 900 °C; (ii) plagioclase crystallizes below 250-100 MPa at temperatures of 850-900 °C; and (iii) pyroxene is stable only below pressures of 200-100 MPa and temperatures of 825-900 °C. Comparison of natural and experimental data suggests that the LTP dacitic magma was stored at 150-200 MPa (5.8-7.7 km below the volcano summit). No differences in pressure found between 21.7 ka and 10.5 ka suggest that these two magmas were stored at similar depths. Orthopyroxene produced in lower temperature LTP experiments is compositionally different to those found in UTP natural samples, suggesting that they originated in two different magma batches. Whole-rock chemistry, petrographic features, and mineral compositions suggest that magma mixing was responsible for the generation of the dacitic Plinian LTP eruption.

  19. Seismic Swarms at Paricutin Volcano Area. Magmatic Intrusion or Tectonic Seismicity?

    Science.gov (United States)

    Pinzon, J. I.; Nunez-Cornu, F. J.; Escudero, C. R.; Rowe, C. A.

    2014-12-01

    We relocate a seismic swarm with more than 700 earthquakes that took place between May and June 2006 in the Paricutin volcano area, Mexico inside of the Michoacan monogenetic volcanic field. This seismic swarm was recorded by the project "Mapping the Riviera Subduction Zone" (MARS), a temporary seismic network that was installed in the states of Jalisco, Colima and Michoacán between January 2006 and June 2007. Previously seismic swarms in the area were reported in the years of 1997, 1999 and 2000. For one that took place in the year of 1997 the Servicio Sismologico Nacional deployed a local network in the area, they conclude that the source of the seismicity was tectonic with depths between 18 and 12 km. The episodes of 1999 and 2000 were reported as similar to the 1997 swarm. A previous analysis of the 2006 swarm concludes that the depth of seismicity migrates from 9 to 5 km and was originated by a magmatic intrusion. We did a relocation of this swarm reading all the events and using Hypo71 and the P-wave velocity model used by the Jalisco Seismic and Acelerometric Network; a waveform analysis using cross-correlation method was also carried out. We obtained 15 earthquakes families with a correlation factor equal or greater than 0.79 and composed focal mechanism for each family. These families present a migration in depth beginning at 16 km and ended at 9 km. Our results agrees with a magmatic intrusion, but not so shallow as the previous study of the 2006 swarm.

  20. Stratigraphic reconstruction of two debris avalanche deposits at Colima Volcano (Mexico): Insights into pre-failure conditions and climate influence

    Science.gov (United States)

    Roverato, M.; Capra, L.; Sulpizio, R.; Norini, G.

    2011-10-01

    Throughout its history, Colima Volcano has experienced numerous partial edifice collapses with associated emplacement of debris avalanche deposits of contrasting volume, morphology and texture. A detailed stratigraphic study in the south-eastern sector of the volcano allowed the recognition of two debris avalanche deposits, named San Marcos (> 28,000 cal yr BP, V = ~ 1.3 km 3) and Tonila (15,000-16,000 cal yr BP, V = ~ 1 km 3 ). This work sheds light on the pre-failure conditions of the volcano based primarily on a detailed textural study of debris avalanche deposits and their associated pyroclastic and volcaniclastic successions. Furthermore, we show how the climate at the time of the Tonila collapse influenced the failure mechanisms. The > 28,000 cal yr BP San Marcos collapse was promoted by edifice steep flanks and ongoing tectonic and volcanotectonic deformation, and was followed by a magmatic eruption that emplaced pyroclastic flow deposits. In contrast, the Tonila failure occurred just after the Last Glacial Maximum (22,000-18,000 cal BP) and, in addition to the typical debris avalanche textural characteristics (angular to sub-angular clasts, coarse matrix, jigsaw fit) it shows a hybrid facies characterized by debris avalanche blocks embedded in a finer, homogenous and partially cemented matrix, a texture more characteristic of debris flow deposits. The Tonila debris avalanche is directly overlain by a 7-m thick hydromagmatic pyroclastic succession. Massive debris flow deposits, often more than 10 m thick and containing large amounts of tree trunk logs, represent the top unit in the succession. Fluvial deposits also occur throughout all successions; these represent periods of highly localized stream reworking. All these lines of evidence point to the presence of water in the edifice prior to the Tonila failure, suggesting it may have been a weakening factor. The Tonila failure appears to represent an anomalous event related to the particular climatic

  1. Estrategias metodológicas para operacionalizar la práctica educativa transdisciplinaria, en conjunto con los actores universitarios, en las licenciaturas del Centro de Estudios Universitarios Arkos (CEUArkos de Puerto Vallarta, Jalisco, México / Methodological Strategies to put into operation a Transdisciplinary Educational Practice in collaboration with the University Members, in the Baccalaureates of Centro de Estudios Universitarios Arkos (CEUArkos, Puerto Vallarta, Jalisco, Mexico

    Directory of Open Access Journals (Sweden)

    Ana Cecilia Espinosa Martínez

    2011-06-01

    Full Text Available

    Recibido 29 de noviembre de 2010 • Aceptado 09 de marzo de 2011 • Corregido 12 de abril de 2011

     

    Resumen. El artículo resume los procesos vividos y los resultados obtenidos a través de una investigación-acción con actores (profesores, estudiantes y directivos de las distintas áreas del CEUArkos de Puerto Vallarta, Jalisco, México. Su propósito es construir y llevar a la práctica estrategias metodológicas para operacionalizar la transdisciplinariedad y la complejidad en el aprendizaje, la enseñanza y la investigación –como parte de la docencia– en las licenciaturas de la institución, a fin de sentar las bases para el paso de una formación universitaria que transite de la disciplinariedad hacia la transdisciplinariedad en todas las carreras que la Universidad oferta. Aborda, asimismo, el tema del currículo universitario.

     

    Abstract. This paper summarizes the processes experienced and results obtained throughout a research-action carried out with professors, students and directors of the different areas of CEUArkos, a university center located in Puerto Vallarta, Jalisco, México. Its purpose is building and taking into practice methodological strategies to put into operation transdisciplinarity and complexity in learning, teaching and research –as part of teaching– in all its baccalaureates, to set the wheels in motion for university education to move from disciplinarity to transdisciplinarity in all the study programs. The university curriculum is also analyzed in this paper.

  2. Conductas delictivas en Tepatitlán de Morelos, Jalisco/Offences in Tepatitlan Morelos, Jalisco

    Directory of Open Access Journals (Sweden)

    Martha Fabiola García Álvarez

    2012-01-01

    Full Text Available The multifactoriality of the crime is a constant in the various analyses that are made about the crime, a case study of these theoretical approaches is the analysis of crime in Tepatitlan de Jalisco. A description about how crimes such as robbery and murder, have behaved likewise a brief description of several of the causes that motivated the crime.

  3. [Ichthyofauna of the Navidad Bay, Jalisco, México].

    Science.gov (United States)

    Aguilar-Palomino, B; Pérez Reyes, C; Galván-Magaña, F; Abitía-Cardenas, L A

    2001-03-01

    A check-list and the relative abundance of the ichthyofauna from Bahia de Navidad, Jalisco, Mexico is presented. This poorly known area of the eastern Tropical Pacific ocean is characterized by its great fish diversity. A total of 245 fish species (163 genera, 72 families) were collected during the 1994-1995 annual cycle. Vouchers were deposited in Centro de Ecologia Costera, Universidad de Guadalajara. The most important families in number of species were Carangidae (20 species), Haemulidae (20), Serranidae (17), Sciaenidae (13) and Lutjanidae (8); 20 species represented 85% and 80% of relative abundance and biomass respectively. Microlepidotus brevipinnis, Caranx caninus, Caranx caballus, Kiphosus analogus and Caranx sexfasciatus, were the dominant species. Most fish species collected in Bahia de Navidad have zoogeographical affinity with the Panamic Province (65%), and in lesser proportion with the Eastern Pacific Ocean (19%), Circumtropical (7%), Mexican Province (5%), Indo-Pacific Ocean (3%) and Gulf of California (0.4%). The great ichthyological affinity between the study area and the southern Gulf of California suggests an extension of the of Gulf southern limit.

  4. [Development of children in socially depressed areas of the state of Jalisco].

    Science.gov (United States)

    Pando Moreno, M; Aranda Beltrán, C; Amezcua Sandoval, M T; Salazar Estrada, J G; Aldrete Rodríguez, M G

    2004-09-30

    To determine the overall development level in children ages 0 to 4 who live in very depressed socioeconomic and cultural conditions. This study is observational, cross-sectional, and prospective. The study was carried out in four types of communities in the state of Jalisco, Mexico: migrant, indigenous, rural, and irregular urban communities on the outskirts of cities. 1277 children under the age of 4 years, who live in the communities selected for the study. Evaluation of the overall development level was based on the Jalisco Scale for Evaluation of Overall Development, which is designed especially for socioeconomically and culturally depressed groups in Mexico. The average development score found in the children was 71.7, which is considered moderately low according to the 3 classification levels of adequate, moderately low, and low. Only 30.4% of the children achieved scores in the adequate category. All the children are considered to live in a high-risk psychosocial environment, which explains the low scores in overall development as evaluated. Differences were observed in some variables within the uniformly low social level of the subjects studied. These differences could be considered as an indication of greater risk within a group that is already high-risk. In cases of overall development that is very low, mothers do not perceive that children have any problems at the time the study is being conducted. This could imply that these mothers do not respond proactively to community education and/or health programs that focus on early intervention.

  5. Holocene block-and-ash flows from summit dome activity of Citlaltépetl volcano, Eastern Mexico

    Science.gov (United States)

    Carrasco-Núñez, Gerardo

    1999-01-01

    A major eruption produced several block-and-ash flows about 4,100 years B.P. at Citlaltépetl volcano (Pico de Orizaba), an ice-capped, 5670-m-high, andesitic, active stratovolcano located at the eastern end of the Mexican Volcanic Belt. Repetitive gravitational collapse of a dacitic dome at the summit crater produced a series of block-and-ash flows, lahars, and floods, which were channeled through two main river-valleys on the west and south flanks of the volcano. The total erupted volume is estimated to be at least 0.27 km 3. The deposits in both areas are similar in composition, and size, but they differ in the area covered, distribution, and structure. The western deposits form a large fan, cover a larger area, and include numerous laharic and fluviatile deposits. In contrast, the southern deposits form prominent terraces where confined in narrow channels, and have associated laharic units in distal areas, where the flows reach a maximum distance of 30 km from the vent. Directed disruptions of a central summit dome occurred, possibly first to the west and then to the southeast, perhaps due to minor modifications of the summit dome morphology, producing the voluminous block-and-ash flow deposits documented here. The flows were strongly controlled by topography, influencing the deposition of the moving particles. Grain-size variations along the flow paths are hardly detectable suggesting no evident lateral downstream transformations. Because sudden changes in dome morphology may cause significant variations in the direction of future dome collapse, specific areas of potential affectation cannot be predicted. Therefore, about 350,000 inhabitants living within a radius of 35-km from the vent could be potentially impacted if catastrophic block-and-ash flows were to recur in the future from similar summit dome activity. Recognition of these deposits is therefore important for hazard assessment because some seemingly safe areas may be at high risk.

  6. Observation of cosmic ray hadrons at the top of the Sierra Negra volcano in Mexico with the SciCRT prototype

    Energy Technology Data Exchange (ETDEWEB)

    Ortiz, E.; Valdés-Galicia, J. F.; Matsubara, Y.; Nagai, Y.; Hurtado, A.; Musalem, O.; García, R.; Anzorena, M. A.; González, L. X.; Itow, Y.; Sako, T.; Lopez, D.; Sasai, Y.; Munakata, K.; Kato, C.; Kozai, M.; Shibata, S.; Takamaru, H.; Kojima, H.; Watanabe, K.; Tsuchiya, H.; Koi, T.

    2016-11-01

    In this work we report the flux of protons and neutral emission measured at the top of the Sierra Negra volcano at 4600 m.a.s.l. (575 g/cm2), in Eastern Mexico. As an example of the capability of the mini-SciCR as a cosmic ray detector we present the Forbush decrease recorded on March 7, 2012. These data were obtained with a cosmic ray detector prototype called mini-SciCR that was operating from October 2010 to July 2012. Our main aims were to measure the hadronic component flux of the secondary cosmic ray and to show the appropriate performance of all system of the detector. To separate the signals of protons from other charged particles we obtained the energy deposition pattern when they cross the detector using a Monte Carlo simulation, and to separate the signals of neutral emission we used an anticoincidence system between the edge bars and the internal bars of the detector. The mini-SciCR is a prototype of a new cosmic ray detector called SciBar Cosmic Ray Telescope (SciCRT) installed in the same place, which is in the process of calibration. The SciCRT will work mainly as a Solar Neutron and Muon Telescope, it is designed to achieve: (1) larger effective area than the current Solar Neutron Telescope, (2) higher energy resolution to determine the energy spectrum of solar neutrons, (3) lower energy threshold, and (4) higher particle identification ability.

  7. Observation of cosmic ray hadrons at the top of the Sierra Negra volcano in Mexico with the SciCRT prototype

    Science.gov (United States)

    Ortiz, E.; Valdés-Galicia, J. F.; Matsubara, Y.; Nagai, Y.; Hurtado, A.; Musalem, O.; García, R.; Anzorena, M. A.; González, L. X.; Itow, Y.; Sako, T.; Lopez, D.; Sasai, Y.; Munakata, K.; Kato, C.; Kozai, M.; Shibata, S.; Takamaru, H.; Kojima, H.; Watanabe, K.; Tsuchiya, H.; Koi, T.

    2016-11-01

    In this work we report the flux of protons and neutral emission measured at the top of the Sierra Negra volcano at 4600 m.a.s.l. (575 g/cm2), in Eastern Mexico. As an example of the capability of the mini-SciCR as a cosmic ray detector we present the Forbush decrease recorded on March 7, 2012. These data were obtained with a cosmic ray detector prototype called mini-SciCR that was operating from October 2010 to July 2012. Our main aims were to measure the hadronic component flux of the secondary cosmic ray and to show the appropriate performance of all system of the detector. To separate the signals of protons from other charged particles we obtained the energy deposition pattern when they cross the detector using a Monte Carlo simulation, and to separate the signals of neutral emission we used an anticoincidence system between the edge bars and the internal bars of the detector. The mini-SciCR is a prototype of a new cosmic ray detector called SciBar Cosmic Ray Telescope (SciCRT) installed in the same place, which is in the process of calibration. The SciCRT will work mainly as a Solar Neutron and Muon Telescope, it is designed to achieve: (1) larger effective area than the current Solar Neutron Telescope, (2) higher energy resolution to determine the energy spectrum of solar neutrons, (3) lower energy threshold, and (4) higher particle identification ability.

  8. Chemical and isotopic compositions of thermal springs, fumaroles and bubbling gases at Tacaná Volcano (Mexico-Guatemala): implications for volcanic surveillance

    Science.gov (United States)

    Rouwet, Dmitri; Inguaggiato, Salvatore; Taran, Yuri; Varley, Nicholas; Santiago S., José A.

    2009-04-01

    This study presents baseline data for future geochemical monitoring of the active Tacaná volcano-hydrothermal system (Mexico-Guatemala). Seven groups of thermal springs, related to a NW/SE-oriented fault scarp cutting the summit area (4,100m a.s.l.), discharge at the northwest foot of the volcano (1,500-2,000m a.s.l.); another one on the southern ends of Tacaná (La Calera). The near-neutral (pH from 5.8 to 6.9) thermal ( T from 25.7°C to 63.0°C) HCO3-SO4 waters are thought to have formed by the absorption of a H2S/SO2-CO2-enriched steam into a Cl-rich geothermal aquifer, afterwards mixed by Na/HCO3-enriched meteoric waters originating from the higher elevations of the volcano as stated by the isotopic composition (δD and δ18O) of meteoric and spring waters. Boiling temperature fumaroles (89°C at ~3,600m a.s.l. NW of the summit), formed after the May 1986 phreatic explosion, emit isotopically light vapour (δD and δ18O as low as -128 and -19.9‰, respectively) resulting from steam separation from the summit aquifer. Fumarolic as well as bubbling gases at five springs are CO2-dominated. The δ13CCO2 for all gases show typical magmatic values of -3.6 ± 1.3‰ vs V-PDB. The large range in 3He/4He ratios for bubbling, dissolved and fumarolic gases [from 1.3 to 6.9 atmospheric 3He/4He ratio ( R A)] is ascribed to a different degree of near-surface boiling processes inside a heterogeneous aquifer at the contact between the volcanic edifice and the crystalline basement (4He source). Tacaná volcano offers a unique opportunity to give insight into shallow hydrothermal and deep magmatic processes affecting the CO2/3He ratio of gases: bubbling springs with lower gas/water ratios show higher 3He/4He ratios and consequently lower CO2/3He ratios (e.g. Zarco spring). Typical Central American CO2/3He and 3He/4He ratios are found for the fumarolic Agua Caliente and Zarco gases (3.1 ± 1.6 × 1010 and 6.0 ± 0.9 R A, respectively). The L/ S (5.9 ± 0.5) and ( L + S)/ M

  9. Paleomagnetic, Anisotropy of Magnetic Susceptibility, and 40AR/39AR Data from the Cienega Volcano, Cerros del Rio Volcanic Field, New Mexico

    Science.gov (United States)

    Foucher, M. S.; Petronis, M. S.; Lindline, J.; Van Wyk de Vries, B.

    2012-12-01

    Cinder cone eruptions are typically interpreted to have formed by the ascension of magma through a simple conduit. Recent field work and laboratory studies on different excavated volcanoes around the world suggest that magma transport within cinder cones can involve a complex system of feeder geometries. We studied the Cienega volcano, a cinder cone in the Cerros del Rio volcanic field, northern New Mexico, in order to better understand the complexity and the evolution of volcanic plumbing systems in the development of cinder cone volcanoes. We hypothesized that cinder cone plumbing systems are inherently complex and involve numerous feeder geometries (e.g. dikes, sills) and flow patterns both towards and away from the central vent complex. The Cienega volcano comprises tephra fall deposits as well as several vents, multiple intrusions, and numerous lava flow sequences. We inspected the magmatic plumbing system using different laboratory methods including paleomagnetic, anisotropy of magnetic susceptibility (AMS), rock magnetic and thin section studies. We collected samples across each outcrop of the feeder system. The dikes are olivine porphyritic basalts with major clinopyroxene, calcic plagioclase feldspar, magnetite, and xenocrystic quartz. Most samples display a trachytic texture with plagioclase crystals showing a preferred orientation parallel to the dike margins. The magnetic information is held predominantly by a cubic phase magnetite with a low- to moderate-Ti composition of Single or Pseudo-Single Domain grains. The AMS results show various flow directions. Three of six dikes yielded magma flow directions away from the vent. The other dikes showed both a subvertical flow, which corresponds to the typical movement of magma in a dike originating from a deeper crustal level, and a downward flow direction. We concluded that magma initially flowed upward from the magma chamber until it encountered flow resistance. At this structural level (the current

  10. Volcano Preparedness

    Science.gov (United States)

    ... You might feel better to learn that an ‘active’ volcano is one that has erupted in the past ... miles away. If you live near a known volcano, active or dormant, following these tips will help you ...

  11. Geomorphological evolution of a fluvial channel after primary lahar deposition: Huiloac Gorge, Popocatépetl volcano (Mexico)

    Science.gov (United States)

    Tanarro, L. M.; Andrés, N.; Zamorano, J. J.; Palacios, D.; Renschler, C. S.

    2010-10-01

    Popocatépetl volcano (19°02' N, 98°62' W, 5424 m) began its most recent period of volcanic activity in December 1994. The interaction of volcanic and glacier activity triggered the formation of lahars through the Huiloac Gorge, located on the northern flank of the volcano, causing significant morphological changes in the channel. The most powerful lahars occurred in April 1995, July 1997 and January 2001, and were followed by secondary lahars that formed during the post-eruptive period. This study interprets the geomorphological evolution of the Huiloac Gorge after the January 2001 lahar. Variations in channel morphology at a 520 m-long research site located mid-way down the gorge were recorded over a 4 year period from February 2002 to March 2005, and depicted in five geomorphological maps (scale 1:200) for 14 February and 15 October 2002, 27 September 2003, 9 February 2004, and 16 March 2006. A GIS was used to calculate the surface area for the landforms identified for each map and detected changes and erosion-deposition processes of the landforms using the overlay function for different dates. Findings reveal that secondary lahars and others types of flows, like sediment-laden or muddy streamflows caused by precipitation, rapidly modified the gorge channel following the January 2001 non-eruptive lahar, a period associated with volcanic inactivity and the disappearance of the glacier once located at the headwall of the gorge. Field observations also confirmed that secondary flows altered the dynamics and geomorphological development of the channel. These flows incised and destroyed the formations generated by the primary lahars (1997 and 2001), causing a widening of the channel that continues today. After February 2004, a rain-triggered lahar and other flows infilled the channel with materials transported by these flows. The deposits on the lateral edges of the channel form terraces. A recent lull in lahar activity contrasts with the increasing instability of

  12. Mexico

    Science.gov (United States)

    2002-01-01

    This true-color image of Mexico was acquired by the Moderate-resolution Imaging Spectroradiometer (MODIS), flying aboard NASA's Terra spacecraft. In areal extent, Mexico is the third largest country on the continent of North America (not counting Greenland, which is a province of Denmark), comprised of almost 2 million square kilometers (756,000 square miles) of land. Home to roughly 100 million people, Mexico is second only to the United States in population, making it the world's largest Spanish-speaking nation. To the north, Mexico shares its border with the United States-a line that runs some 3,100 kilometers (1,900 miles) east to west. About half of this border is defined by the Rio Grande River, which runs southeast to the Gulf of Mexico (partially obscured by clouds in this image) and marks the dividing line between Texas and Mexico. Toward the upper left (northwest) corner of this image is the Baja California peninsula, which provides the western land boundary for the Gulf of California. Toward the northwestern side of the Mexican mainland, you can see the Sierra Madre Occidental Mountains (brownish pixels) running southeast toward Lake Chapala and the city of Guadalajara. About 400 km (250 miles) east and slightly south of Lake Chapala is the capital, Mexico City. Extending northward from Mexico City is the Sierra Madre Oriental Mountains, the irregular line of brownish pixels that seem to frame the western edges of the bright white cumulus clouds in this image. Between these two large mountain ranges is a large, relatively dry highland region. To the south, Mexico shares borders with Guatemala and Belize, both of which are located south of Mexico's Yucatan Peninsula. Image courtesy Reto Stockli, Brian Montgomery, and Robert Simmon, based on data from the MODIS Science Team

  13. Vertical AMS variation within basalt flow profiles from the Xitle volcano (Mexico) as indicator of heterogeneous strain in lava flows

    Science.gov (United States)

    Caballero-Miranda, C. I.; Alva-Valdivia, L. M.; González-Rangel, J. A.; Gogitchaishvili, A.; Urrutia-Fucugauchi, J.; Kontny, A.

    2016-02-01

    The within-flow vertical variation of anisotropy of the magnetic susceptibility (AMS) of three basaltic flow profiles from the Xitle volcano were investigated in relation to the lava flow-induced shear strain. Rock magnetic properties and opaque microscopy studies have shown that the magnetic mineralogy is dominated by Ti-poor magnetite with subtle vertical variations in grain size distribution: PSD grains dominate in a thin bottommost zone, and from base to top from PSD-MD to PSD-SD grains are found. The vertical variation of AMS principal direction patterns permitted identification of two to three main lava zones, some subdivided into subzones. The lower zone is very similar in all profiles with the magnetic foliation dipping toward the flow source, whereas the upper zone has magnetic foliation dipping toward the flow direction or alternates between dipping against and toward the flow direction. The K1 (maximum AMS axis) directions tend to be mostly parallel to the flow direction in both zones. The middle zone shows AMS axes diverging among profiles. We present heterogeneous strain ellipse distribution models for different flow velocities assuming similar viscosity to explain the AMS directions and related parameters of each zone. Irregular vertical foliations and transverse to flow lineation of a few samples at the bottommost and topmost part of profiles suggest SD inverse fabric, levels of intense friction, or degassing effects in AMS orientations.

  14. Evaluation of ASTER and SRTM DEM data for lahar modeling: A case study on lahars from Popocatépetl Volcano, Mexico

    Science.gov (United States)

    Huggel, C.; Schneider, D.; Miranda, P. Julio; Delgado Granados, H.; Kääb, A.

    2008-02-01

    Lahars are among the most serious and far-reaching volcanic hazards. In regions with potential interactions of lahars with populated areas and human structures the assessment of the related hazards is crucial for undertaking appropriate mitigating actions and reduce the associated risks. Modeling of lahars has become an important tool in such assessments, in particular where the geologic record of past events is insufficient. Mass-flow modeling strongly relies on digital terrain data. Availability of digital elevation models (DEMs), however, is often limited and thus an obstacle to lahar modeling. Remote-sensing technology has now opened new perspectives in generating DEMs. In this study, we evaluate the feasibility of DEMs derived from the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) and the Shuttle Radar Topography Mission (SRTM) for lahar modeling on Popocatépetl Volcano, Mexico. Two GIS-based models are used for lahar modeling, LAHARZ and a flow-routing-based debris-flow model (modified single-flow direction model, MSF), both predicting areas potentially affected by lahars. Results of the lahar modeling show that both the ASTER and SRTM DEMs are basically suitable for use with LAHARZ and MSF. Flow-path prediction is found to be more reliable with SRTM data, though with a coarser spatial resolution. Errors of the ASTER DEM affecting the prediction of flow paths due to the sensor geometry are associated with deeply incised gorges with north-facing slopes. LAHARZ is more sensitive to errors of the ASTER DEM than the MSF model. Lahar modeling with the ASTER DEM results in a more finely spaced predicted inundation area but does not add any significant information in comparison with the SRTM DEM. Lahars at Popocatépetl are modeled with volumes of 1 × 10 5 to 8 × 10 6 m 3 based on ice-melt scenarios of the glaciers on top of the volcano and data on recent and historical lahar events. As regards recently observed lahars, the travel

  15. Tectonic and magmatic controls on the location of post-subduction monogenetic volcanoes in Baja California, Mexico, revealed through spatial analysis of eruptive vents

    Science.gov (United States)

    Germa, Aurélie; Connor, Laura J.; Cañon-Tapia, Edgardo; Le Corvec, Nicolas

    2013-12-01

    Post-subduction (12.5 Ma to less than 1 Ma) monogenetic volcanism on the Baja California peninsula, Mexico, formed one of the densest intra-continental areas of eruptive vents on Earth. It includes about 900 vents within an area ˜700 km long (N-S) and 70 to 150 km wide (W-E). This study shows that post-subduction volcanic activity was distributed along this arc and that modes exist in the volcano distribution, indicating that productivity of the magma source region was not uniform along the length of the arc. Vent clustering, vent alignments, and cone elongations were measured within eight monogenetic volcanic fields located along the peninsula. Results indicate that on a regional scale, vent clustering varies from north to south with denser spatial clustering in the north on the order of 1.9 × 10-1 vents/km2 to less dense clustering in the south on the order of 7.8 × 10-2 vents/km2. San Quintin, San Carlos, Jaraguay, and Santa Clara are spatially distinct volcanic fields with higher eruptive vent densities suggesting the existence of individual melt columns that may have persisted over time. In contrast, the San Borja, Vizcaino, San Ignacio, and La Purisima vent fields show lower degrees of vent clustering and no obvious spatial gaps between fields, thus indicating an area of more distributed volcanism. Insight into the lithospheric stress field can be gained from vent alignments and vent elongation measurements. Within the fields located along the extinct, subduction-related volcanic arc, elongation patterns of cinder cones and fissure-fed spatter cones, vent clusters, and vent alignments trend NW-SE and N-S. Within the Santa Clara field, located more to the west within the forearc, elongation patterns of the same volcanic features trend NE-SW. These patterns suggest that magmatism was more focused in the forearc and in the northern part of Baja California than in its southern region. Within the extinct arc, magma ascent created volcano alignments and elongate

  16. Mexico.

    Science.gov (United States)

    1988-02-01

    Focus in this discussion of Mexico is on the following: geography; the people; history; political conditions; the economy; foreign relations; and relations between the US and Mexico. As of July 1987, the population of Mexico numbered 81.9 million with an estimated annual growth rate of 2.09%. 60% of the population is Indian-Spanish (mestizo), 30% American Indian, 9% white, and 1% other. Mexico is the most populous Spanish-speaking country in the world and the 2nd most populous country in Latin America. Education is decentralized and expanded. Mexico's topography ranges from low desert plains and jungle-like coastal strips to high plateaus and rugged mountains. Hernan Cortes conquered Mexico in 1919-21 and founded a Spanish colony that lasted for almost 300 years. Independence from Spain was proclaimed by Father Miguel Hidalgo on September 16, 1810; the republic was established on December 6, 1822. Mexico's constitution of 1917 provides for a federal republic with a separation of powers into independent executive, legislative, and judicial branches of government. Significant political themes of the administration of President Miguel de la Madrid Hurtado, who began his 6-year term in 1982, have been restructuring the economy, liberalizing trade practices, decentralizing government services, and eliminating corruption among public servants. In 1987, estimates put the real growth of the Mexican economy at 1.5%; the gross domestic product (GDP) had shrunk by 3.5% in 1986. Yet, on the positive side, Mexico's international reserves increased to record levels in 1987 (to about $15 billion), and its current account surplus reached more than $3 billion. Mexico has made considerable progress in moving to restructure its economy. It has substantially reduced impediments to international trade and has moved to reduce the number of parastatal firms. 1987 was the 2nd consecutive year in which Mexico recorded triple-digit inflation; inflation reached 158.8%. Other problems include

  17. Sulfur and oxygen isotopic systematics of the 1982 eruptions of El Chichón Volcano, Chiapas, Mexico

    Science.gov (United States)

    Rye, R.O.; Luhr, J.F.; Wasserman, M.D.

    1984-01-01

    Thermometers based on sulfur and oxygen isotopic compositions of anhydrite, pyrrhotite, titanomagnetite, and plagioclase crystals from fresh pumices of the 1982 eruptions of El Chichón Volcano indicate a pre-eruption temperature of 810 ± 40°C, confirming textural evidence that the anhydrite precipitated directly from the melt. The isotopic composition of sulfate leached from fresh ashfall samples shows it to be a mixture of anhydrite microphenocrysts and adsorbed sulfate derived from oxidized sulfur (SO2) in the eruption plume. The leachate data show no evidence for rapid oxidation of significant amounts of H2S in the eruption cloud even though the fugacity ratio of H2S/SO2 in the gas phase of the magma was >400. This may indicate kinetic inhibition of H2S to SO2 conversion in the eruption cloud. Prior to eruption, the magma contained an estimated 2.6 wt. % sulfur (as SO3). The estimated δ 34S of the bulk magma is 5.8‰. Such a high value may reflect assimilation of 34S-enriched evaporites or the prior loss of 34S-depleted H2S to a fluid or gas phase during formation of a small prophyry-type hydrothermal system or ore deposit. In either case, the original magma must have been very sulfur rich. It is likely that the initial high sulfur content of the magma and at least some of its 34S enrichment reflects involvement of subducted volcanogenic massive sulfides deposits during Benioff-zone partial melting. Isotopic data on mineralized, accidental lithic fragments support the possible development of a porphyry-type system at El Chichón.

  18. Sulfur and oxygen isotopic systematics of the 1982 eruptions of El Chichón Volcano, Chiapas, Mexico

    Science.gov (United States)

    Rye, R. O.; Luhr, J. F.; Wasserman, M. D.

    1984-12-01

    Thermometers based on sulfur and oxygen isotopic compositions of anhydrite, pyrrhotite, titanomagnetite, and plagioclase crystals from fresh pumices of the 1982 eruptions of El Chichón Volcano indicate a pre-eruption temperature of 810 ± 40°C, confirming textural evidence that the anhydrite precipitated directly from the melt. The isotopic composition of sulfate leached from fresh ashfall samples shows it to be a mixture of anhydrite microphenocrysts and adsorbed sulfate derived from oxidized sulfur (SO 2) in the eruption plume. The leachate data show no evidence for rapid oxidation of significant amounts of H 2S in the eruption cloud even though the fugacity ratio of H 2S/SO 2 in the gas phase of the magma was >400. This may indicate kinetic inhibition of H 2S to SO 2 conversion in the eruption cloud. Prior to eruption, the magma contained an estimated 2.6 wt. % sulfur (as SO 3). The estimated δ 34S of the bulk magma is 5.8‰. Such a high value may reflect assimilation of 34S-enriched evaporites or the prior loss of 34S-depleted H 2S to a fluid or gas phase during formation of a small prophyry-type hydrothermal system or ore deposit. In either case, the original magma must have been very sulfur rich. It is likely that the initial high sulfur content of the magma and at least some of its 34S enrichment reflects involvement of subducted volcanogenic massive sulfides deposits during Benioff-zone partial melting. Isotopic data on mineralized, accidental lithic fragments support the possible development of a porphyry-type system at El Chichón.

  19. Broadband seismic measurements of degassing activity associated with lava effusion at Popocatépetl Volcano, Mexico

    Science.gov (United States)

    Arciniega-Ceballos, Alejandra; Chouet, Bernard; Dawson, Phillip; Asch, Guenter

    2008-02-01

    From November 1999 through July 2000, a broadband seismic experiment was carried out at Popocatépetl Volcano to record seismic activity over a wide period range (0.04-100 s). We present an overview of the seismicity recorded during this experiment and discuss results of analyses of long-period (LP) and very-long-period (VLP) seismic signals recorded at stations nearest to the crater over a four-month interval December 1999-March 2000. Three families of LP signals (Types-I, II, and III) are identified based on distinctive waveform features observed periods shorter than 1 s, periods longer than 15 s, and within the period range 0.5-2.5 s. Type-I LP events have impulsive first arrivals and exhibit a characteristic harmonic wave train with dominant periods in the 1.4-1.9 s range during the first 10 s of signal. These events are also associated with a remarkable VLP wavelet with period near 30 s. Type-II LP events represent pairs of events occurring in rapid succession and whose signatures are superimposed. These are typically marked by slowly emergent first arrivals and by a characteristic VLP wave train with dominant period near 30 s, made of two successive wavelets whose shapes are quasi-identical to those of the VLP wavelets associated with Type-I events. Type-III LP events represent the most energetic signals observed during our experiment. These have an emergent first arrival and display a harmonic signature with dominant period near 1.1 s. They are dominated by periods in the 0.25-0.35 s band and contain no significant energy at periods longer than 15 s. Hypocentral locations of the three types of LP events obtained from phase picks point to shallow seismic sources clustered at depths shallower than 2 km below the crater floor. Observed variations in volcanic eruptive activity correlate with defined LP families. Most of the observed seismicity consists of Type-I events that occur in association with 1-3-min-long degassing bursts ("exhalations"). Eruptive

  20. Ataques de cocodrilo de río (Crocodylus acutus en Puerto Vallarta, Jalisco, México: presentación de cinco casos American crocodile (Crocodylus acutus attacks in Puerto Vallarta, Jalisco, México: Presentation of five cases

    Directory of Open Access Journals (Sweden)

    F.G. Cupul-Magaña

    2010-09-01

    Full Text Available Se presentan cinco casos de ataques por cocodrilos a personas, sin consecuencias fatales, en la región de Puerto Vallarta, Jalisco, México (2007-2010. En cuatro de los casos, la víctima sufrió amputación del miembro superior o inferior, y en un caso sólo resultó con mordeduras avulsivas en el brazo. Con la documentación de estos cinco casos, el número de ataques por cocodrilo americano (Crocodylus acutus en la costa del estado mexicano de Jalisco durante los últimos 52 años es de entre 30 y 31. Los resultados muestran un incremento en los ataques entre 0,57 y 0,59 por año. Se describen los casos y se proponen explicaciones sobre los posibles motivos de los ataques por parte de los cocodrilos.Five cases of non-fatal crocodile attacks on people in the region of Puerto Vallarta, Jalisco, Mexico (2007-2010 are presented. In four cases the victim suffered amputation of upper or lower extremity, but only in one case the victim resulted in bitten on the arm. With the documentation of these five cases, the number of attacks by American crocodile (Crocodylus acutus in the coast of the Mexican state of Jalisco for the past 52 years is between 30 and 31. The results show an increase in crocodile attacks from 0,57 to 0,59 per year. We describe the cases and suggest possible explanations for the crocodile's attacks.

  1. Entrepreneurship and social capital: Sources of local development, the jewelery industry in Jalisco

    Directory of Open Access Journals (Sweden)

    María Mercedes León Sánchez

    2013-01-01

    Full Text Available In the last forty years in various regions of Mexico, Jalisco, has given impetus to the development of industries known as "modern" as electronics and software, this is intended to increase growth and foster development, all this has been detrimental to those industries considered "traditional" (footwear, textile, jewelery, industries that have long been the basis for productive development of these regions. Policies that have followed in industrial countries has been to promote the first under the assumption that they are incorporating the technology, while the latter incorporates little technology intheir production processes and generally do not innovate. However industrial behavior has demonstrated that the above is a fallacy.Government policies that were implemented in industrial resulted in the increase in the share of industrial production called "modern", such as electronics and software, but those traditional activities such as jewelry, not only maintained but that increased production and commercial dynamism. This dynamic is observed in the absorption of employment and productive participation nationwide. The jewelry industry is a case in point, because from generation entrepreneurshipcapacity, social capital and working together with the government, among others, has managed to influence local development in the region. Therefore in this paper analyzes trying to emphasize that industry, from interviews with key actors and quantitative analysis for this industry, basic factors that impacted on the local development of Jalisco.

  2. Crustal Architecture at the Collision Zone Between Rivera and North American Plates at the Jalisco Block: Tsujal Project

    Science.gov (United States)

    Dañobeitia, Juanjo; Bartolomé, Rafael; Prada, Manel; Nuñez-Cornú, Francisco; Córdoba, Diego; Bandy, William L.; Estrada, F.; Cameselle, Alejandra L.; Nuñez, Diana; Castellón, Arturo; Alonso, José Luis; Mortera, Carlos; Ortiz, Modesto

    2016-09-01

    Processing and analysis of new multichannel seismic records, coincident with wide-angle seismic profiles, acquired in the framework of the TsuJal project allow us to investigate in detail the complex structure of the oceanic domain in the collision zone between Rivera Plate and Block Jalisco at its northern termination. The subducting Rivera Plate, which is overridden by the North American Plate-Jalisco Block, is clearly identified up to 21.5°N (just south of Maria Magdalena Island) as a two clear reflections that we interpret as the interplate and Moho discontinuities. North of the Tres Marias Islands the seismic images display a different tectonic scenario with structures that are consistent with large faulting and rifted margin. A two-dimensional velocity approach for the crustal geometry is achieved using joint refraction/reflection travel time tomography, the uncertainty of the results is assessed by means of Monte Carlo analysis. Our results show an average oceanic crustal thickness of 6-7 km with a moderate increase towards the Jalisco Block, an anomalous thick layers (~3.0 km) displaying a relatively low velocity (~5.5 km/s) underneath Maria Magdalena Rise, and an estimated Moho depth deeper than 15 km in the collision zone between Rivera Plate and Jalisco Block. We have also determined an anomalous crust on the western flank of the Tres Marias Islands, which may be related to the initial phases of continental breakup of the Baja California Peninsula and Mexico mainland. High-resolution bathymetry provides remarkable images of intensive slope instabilities marked by relatively large slides scars of more than 40 km2 extent, and mass-wasting deposits probably triggered by the intense seismicity in the area.

  3. Crustal Architecture at the Collision Zone Between Rivera and North American Plates at the Jalisco Block: Tsujal Project

    Science.gov (United States)

    Dañobeitia, Juanjo; Bartolomé, Rafael; Prada, Manel; Nuñez-Cornú, Francisco; Córdoba, Diego; Bandy, William L.; Estrada, F.; Cameselle, Alejandra L.; Nuñez, Diana; Castellón, Arturo; Alonso, José Luis; Mortera, Carlos; Ortiz, Modesto

    2016-10-01

    Processing and analysis of new multichannel seismic records, coincident with wide-angle seismic profiles, acquired in the framework of the TsuJal project allow us to investigate in detail the complex structure of the oceanic domain in the collision zone between Rivera Plate and Block Jalisco at its northern termination. The subducting Rivera Plate, which is overridden by the North American Plate-Jalisco Block, is clearly identified up to 21.5°N (just south of Maria Magdalena Island) as a two clear reflections that we interpret as the interplate and Moho discontinuities. North of the Tres Marias Islands the seismic images display a different tectonic scenario with structures that are consistent with large faulting and rifted margin. A two-dimensional velocity approach for the crustal geometry is achieved using joint refraction/reflection travel time tomography, the uncertainty of the results is assessed by means of Monte Carlo analysis. Our results show an average oceanic crustal thickness of 6-7 km with a moderate increase towards the Jalisco Block, an anomalous thick layers (~3.0 km) displaying a relatively low velocity (~5.5 km/s) underneath Maria Magdalena Rise, and an estimated Moho depth deeper than 15 km in the collision zone between Rivera Plate and Jalisco Block. We have also determined an anomalous crust on the western flank of the Tres Marias Islands, which may be related to the initial phases of continental breakup of the Baja California Peninsula and Mexico mainland. High-resolution bathymetry provides remarkable images of intensive slope instabilities marked by relatively large slides scars of more than 40 km2 extent, and mass-wasting deposits probably triggered by the intense seismicity in the area.

  4. Broadband seismic measurements of degassing activity associated with lava effusion at Popocatépetl Volcano, Mexico

    Science.gov (United States)

    Arciniega-Ceballos, Alejandra; Chouet, Bernard A.; Dawson, Phillip; Asch, Guenter

    2008-01-01

    From November 1999 through July 2000, a broadband seismic experiment was carried out at Popocatépetl Volcano to record seismic activity over a wide period range (0.04–100 s). We present an overview of the seismicity recorded during this experiment and discuss results of analyses of long-period (LP) and very-long-period (VLP) seismic signals recorded at stations nearest to the crater over a four-month interval December 1999–March 2000. Three families of LP signals (Types-I, II, and III) are identified based on distinctive waveform features observed periods shorter than 1 s, periods longer than 15 s, and within the period range 0.5–2.5 s. Type-I LP events have impulsive first arrivals and exhibit a characteristic harmonic wave train with dominant periods in the 1.4–1.9 s range during the first 10 s of signal. These events are also associated with a remarkable VLP wavelet with period near 30 s. Type-II LP events represent pairs of events occurring in rapid succession and whose signatures are superimposed. These are typically marked by slowly emergent first arrivals and by a characteristic VLP wave train with dominant period near 30 s, made of two successive wavelets whose shapes are quasi-identical to those of the VLP wavelets associated with Type-I events. Type-III LP events represent the most energetic signals observed during our experiment. These have an emergent first arrival and display a harmonic signature with dominant period near 1.1 s. They are dominated by periods in the 0.25–0.35 s band and contain no significant energy at periods longer than 15 s. Hypocentral locations of the three types of LP events obtained from phase picks point to shallow seismic sources clustered at depths shallower than 2 km below the crater floor. Observed variations in volcanic eruptive activity correlate with defined LP families. Most of the observed seismicity consists of Type-I events that occur in association with 1–3-min-long degassing bursts (

  5. Vanishing Volcano

    Institute of Scientific and Technical Information of China (English)

    杨树仁

    1995-01-01

    Mauna Loa, the world’s largest active volcano,is sinking into the Pacific Ocean——and it’s taking the main island of Hawaii with it! The problem:The mighty volcano has gained too much weight, says Peter Lipman of the U. S. Geological Survey.

  6. Assessing lahars from ice-capped volcanoes using ASTER satellite data, the SRTM DTM and two different flow models: case study on Iztaccíhuatl (Central Mexico)

    OpenAIRE

    2008-01-01

    Lahars frequently affect the slopes of ice-capped volcanoes. They can be triggered by volcano-ice interactions during eruptions but also by processes such as intense precipitation or by outbursts of glacial water bodies not directly related to eruptive activity. We use remote sensing, GIS and lahar models in combination with ground observations for an initial lahar hazard assessment on Iztaccíhuatl volcano (5230 m a.s.l.), considering also possible future developments of the glaciers on the v...

  7. Mexico.

    Science.gov (United States)

    1993-01-01

    The background notes on Mexico provide text and recent statistical information on the geography, population, government, economy, and foreign relations, specifically the North American Free Trade Agreement with US. The 1992 population is estimated at 89 million of which 60% are mestizo (Indian-Spanish), 30% are American Indian, 9% are Caucasian, and 1% are other. 90% are Roman Catholic. There are 8 years of compulsory education. Infant mortality is 30/1000 live births. Life expectancy for males is 68 years and 76 years for females. The labor force is comprised of 30% in services, 24% in agriculture and fishing, 19% in manufacturing, 13% in commerce, 7% in construction, 4% in transportation and communication, and .4% in mining. There are 31 states and a federal district. Gross domestic product (GDP) per capita was $3200 in 1991. Military expenditures were .5% of GDP in 1991. The average inflation rate is 19%. Mexico City with 20 million is the largest urban center in the world. In recent years, the economy has been restructured with market oriented reforms; the result has been a growth of GDP of 3.6% in 1991 from 2% in 1987. Dependence on oil exports has decreased. There has been privatization and deregulation of state-owned companies. Subsidies to inefficient companies have been stopped. Tariff rates were reduced. The financial debt has been reduced and turned into a surplus of .8% in 1992. Mexico's foreign debt has been reduced from its high in 1987 of $107 billion. Agricultural reforms have been ongoing for 50 years. Land was redistributed, but standards of living and productivity have improved only slightly. Rural land tenure regulations have been changed, and other economic reforms are expected. Mexico engages in ad hoc international groups and is selective about membership in international organizations.

  8. Update of Bioclimatic Atlas of Jalisco State

    Directory of Open Access Journals (Sweden)

    Hermes Ulises Ramirez Sanchez

    2013-02-01

    Full Text Available In this new version of the bioclimatic Atlas of Jalisco State, we present a more detailed description of bioclimate conditions for municipalities in the state, obtained using the most current methodology and larger meteorological database, than used in the previous version, by Amador SEMADES (2009. Processed data were used from 1971-2000 from the Climatological Normal data of the National weather Service belonging to the National Water Commission. The maps were developed using the ArcGIS Geographic Information System 9.3, with monthly and annual seasonality. It is observed that in the months of January to May the predominant bioclimate in most of the state is dry extremes, with lesser occurrence of warm and cold, but from June, the bioclimate changes to warm, with occurrence temperate days. In July temperate bioclimate predominates with lesser occurrence of warm and August is characterized by warm; then from September to October temperate dominates again, followed by warm bioclimate. Finally in November and December extremely dry is dominant again and followed by temperate and cold. As for the annual distribution, since the average bioclimate is a balance of extremes, most of the state has temperate bioclimate.

  9. Dante's volcano

    Science.gov (United States)

    1994-09-01

    This video contains two segments: one a 0:01:50 spot and the other a 0:08:21 feature. Dante 2, an eight-legged walking machine, is shown during field trials as it explores the inner depths of an active volcano at Mount Spurr, Alaska. A NASA sponsored team at Carnegie Mellon University built Dante to withstand earth's harshest conditions, to deliver a science payload to the interior of a volcano, and to report on its journey to the floor of a volcano. Remotely controlled from 80-miles away, the robot explored the inner depths of the volcano and information from onboard video cameras and sensors was relayed via satellite to scientists in Anchorage. There, using a computer generated image, controllers tracked the robot's movement. Ultimately the robot team hopes to apply the technology to future planetary missions.

  10. What Are Volcano Hazards?

    Science.gov (United States)

    ... Sheet 002-97 Revised March 2008 What Are Volcano Hazards? Volcanoes give rise to numerous geologic and ... as far as 15 miles from the volcano. Volcano Landslides A landslide or debris avalanche is a ...

  11. Earthquake cycle implications of the Jalisco/Colima GPS project, 1995-2007

    Science.gov (United States)

    Demets, C.; Marquez-Azua, B.; Sanchez, O.; Stock, J.

    2007-05-01

    This talk will summarize results from modeling of campaign and continuous GPS measurements in a 30+ station network that extends 350 km along the Pacific coast and 300 km inland in the states of Jalisco, Colima, and Michoacan. Measurements since March of 1995 have recorded in detail the Oct 9, 1995 M=8.0 Colima/Jalisco and Jan 22, 2003 M=7.4 Tecoman earthquakes, constituting the only earthquakes with magnitudes above 6.5 that have ruptured the northwestern end of the Middle America trench since 1932. Modeling of coseismic offsets for both earthquakes indicate that coseismic slip extended no farther downdip than the Pacific coastline, defining a shallower seismogenic zone than is typical for subduction zone. Near-term postseismic measurements demonstrate that both earthquakes were followed within hours to days by aseismic propagation of slip along the subduction interface to deeper areas beneath the continent, decaying logarithmically with time after the earthquakes. These are diagnostic of fault-centered afterslip, representing a transient frictional response to the earthquake. Measurements months to years after each earthquake clearly show protracted, decaying transient deformation, consistent with viscoelastic flow of the upper mantle and possibly lower crust to relax the seismically-elevated stresses at depth. The afterslip and viscoelastic transients are further superimposed on linear landward motions of the GPS sites, which are an elastic response to relocking of shallow seismogenic areas of the subduction interface. The site motions are poorly fit by models that exclude steady interseismic strain accumulation, afterslip, or viscoelastic transients, strongly suggesting that all three contribute to surface deformation. Interestingly, no episodic transient slip has been recorded in Jalisco or Colima since continuous GPS recording was initiated by INEGI in early 1993. Unlike the rest of western and southern Mexico, where ETS is pervasive and presumably caused by

  12. Historic and ancient tsunamis uncovered on the Jalisco-Colima Pacific coast, the Mexican subduction zone

    Science.gov (United States)

    Ramírez-Herrera, María Teresa; Bógalo, María Felicidad; Černý, Jan; Goguitchaichvili, Avto; Corona, Néstor; Machain, María Luisa; Edwards, Arturo Carranza; Sosa, Susana

    2016-04-01

    Research on extreme wave events such as tsunamis using the geological record in areas of infrequent and or small magnitude earthquakes can aid in extending the long-term history and recurrence intervals of large events. This information is valuable for risk management and community preparedness in coastal areas. Here we investigate tsunami deposits on the Jalisco coast of Mexico that overlies the subducting Rivera Plate under the North American plate, an area due for a large thrust earthquake and potential tsunami. Here, we apply a full battery of rock-magnetic analyses that also include a detailed AMS study and other typically applied proxies in tsunami deposits research. We present evidence to demonstrate that anomalous sand units with sharp basal contacts at La Manzanilla, Tenacatita Bay, and El Tecuán shore sites on the Jalisco coast may be the products of tsunamis generated by known historical (Ms 8.2 earthquake of 3 June 1932) and other earlier tsunamigenic earthquakes. A sandy unit with a sharp basal contact, flame structures at the base, rip-up clasts at La Manzanilla, and four sand units with sharp basal contact overlying buried soils at El Tecuán, together with other proxies, such as magnetic properties and others, suggest tsunami deposits. 210Pb dating of sediments slightly above the upper sand layer indicate an age A.D. 1935 ± 11 at El Tecuán. Historical accounts of tsunami inundation at both sites provide further evidence that this is most probably the result of the 3 June 1932 tsunami. Hence this study may provide the first evidence of a tsunami triggered by this earthquake and also of three probable predecessors. Further evidence of at least three earlier tsunamis that occurred since the fifteenth century is also evident in the stratigraphy. These events may correspond to events listed in historical archives, namely the 1563, 1816, and/or the 1818 events.

  13. Zea diploperennis (Gramineae): A New Teosinte from Mexico.

    Science.gov (United States)

    Iltis, H H; Doebley, J F; M, R G; Pazy, B

    1979-01-12

    A perennial teosinte or "wild maize" endemic to the Cerro de San Miguel, Sierra de Manantlan, Jalisco, Mexico differs from Zea perennis by dimorphic rhizomes, robust habit, and a larger number of longer, laxer tassel branches. The fact that it is a diploid (2n = 20) has taxonomic and agronomic significance. The seeds are used locally for food.

  14. Jalisco y Colima, México

    Directory of Open Access Journals (Sweden)

    A. Talavera-Villarreal

    2006-01-01

    Full Text Available Esta investigación se realizó en dos parcelas de limón (Citrus aurantifolia, ubicadas —una de ellas— en el municipio de Autlán de Navarro (AN, Jalisco; y la otra, en Colima, Colima (COL México, durante el periodo de 1998 a 2000. El objetivo fue determinar la dinámica poblacional de la fase larvaria de Phyllocnistis citrella Stainton (minador de la hoja de los cítricos, MHC y la contribución de varios gremios de artrópodos nativos en el control natural del insecto. En AN, las poblaciones de larvas y pupas mostraron dos periodos de abundancia, asociados a los meses de agosto y noviembre, respectivamente; durante los meses de diciembre a mayo de 1999, la incidencia del insecto fue inapreciable. En COL, los periodos de abundancia de la fase larval fueron distintos a los de AN; en primer lugar, de noviembre a junio, las poblaciones se incrementaron paulatinamente; y de julio a septiembre, el MHC fue inapreciable debido a la presencia de un fitopatógeno que eliminó los brotes de los árboles en el sitio experimental. En ambas localidades, los patrones de mortalidad observados muestran que los depredadores tuvieron una incidencia importante en el tercer estadio y la pupa de P. citrella. Por otro lado, en COL fue posible observar que la mortalidad de las larvas del MHC se debió, principalmente, a depredadores que raptan la larva de la mina (82%; otra fracción de la población es depredada por insectos o artrópodos que punzan al insecto y lo consumen en la mina (9.5 % y por ectoparásitos (6.7%; una proporción reducida de la mortalidad (2% no fue posible asignarla a un gremio de depredador. La mortalidad de las pupas se debió, primordialmente, a ectoparásitos (91%, y el resto (9%, no fue posible asignarla a una fuente de mortalidad específica. En adición, se observó que hay una relación denso-dependiente positiva entre la abundancia de P. citrella y la mortalidad causada por los depredadores.

  15. Diversidad y datos reproductivos de mamíferos medianos y grandes en el bosque mesófilo de montaña de la Reserva de la Biosfera Sierra de Manantlán, Jalisco-Colima, México Medium and large mammal diversity and reproductive data in the cloud forest, Biosphere Reserve of Sierra Manantlán, Jalisco-Colima, Mexico

    Directory of Open Access Journals (Sweden)

    Marcelo Aranda

    2012-09-01

    Full Text Available El bosque mesófilo de montaña (BMM es uno de los ecosistemas con menor extensión territorial y de los más amenazados en México. Este trabajo presenta datos sobre la riqueza, abundancia relativa, actividad y datos reproductivos de especies de mamíferos medianos y grandes en el BMM ubicado en la Reserva de la Biosfera Sierra de Manantlán. Entre febrero de 2008 y agosto de 2009, mediante la utilización de fototrampas, se obtuvieron 372 registros independientes que corresponden a 17 especies. Esta información respalda la elección adecuada de método y sitios de monitoreo. Los resultados indican que el ecosistema se encuentra en buen estado de conservación, lo que coincide con lo que en fecha reciente registró la Comisión Nacional para el Conocimiento y Uso de la Biodiversidad. Es recomendable establecer acciones de monitoreo a mediano y largo plazo en múltiples sitios, para complementar la evaluación que se ha realizado de este ecosistema en el país.The cloud forest (CF is one of the ecosystems with less surface and the most threatened in Mexico. This paper presents information on the richness, relative abundance, activity and reproductive data of medium and large mammals in the CF located in the Sierra de Manantlán Biosphere Reserve. Between February 2008 and August 2009, we used camera-traps with which we obtained 372 independent records, corresponding to 17 species. We believe this data supports an appropriate choice of method and monitoring sites; but also data on richness, abundance and reproduction of the species indicate that the ecosystem is properly preserved in the area, which is consistent with recently reported Conabio. Therefore we recommend establishing monitoring activities in the medium and long term in multiple sites, which could complement the assessment that has been undertaken at national level in this ecosystem.

  16. Sr, Nd and Pb isotope and geochemical data from the Quaternary Nevado de Toluca volcano, a source of recent adakitic magmatism, and the Tenango Volcanic Field, Mexico

    Science.gov (United States)

    Martínez-Serrano, Raymundo G.; Schaaf, Peter; Solís-Pichardo, Gabriela; Hernández-Bernal, Ma. del Sol; Hernández-Treviño, Teodoro; Julio Morales-Contreras, Juan; Macías, José Luis

    2004-11-01

    Volcanic activity at Nevado de Toluca (NT) volcano began 2.6 Ma ago with the emission of andesitic lavas, but over the past 40 ka, eruptions have produced mainly lava flows and pyroclastic deposits of predominantly orthopyroxene-hornblende dacitic composition. In the nearby Tenango Volcanic Field (TVF) pyroclastic products and lava flows ranging in composition from basaltic andesite to andesite were erupted at most of 40 monogenetic volcanic centers and were coeval with the last stages of NT. All volcanic rocks in the study area are characterized by a calc-alkaline affinity that is consistent with a subduction setting. Relatively high concentrations of Sr (>460 ppm) coupled with low Y (45 km) that underlies the volcanoes of the study area, the geochemical and isotopic patterns of these rocks indicate low interaction with this crust. NT volcano was constructed at the intersection of three fault systems, and it seems that the Plio-Quaternary E-W system played an important role in the ascent and storage of magmas during the recent volcanic activity in the two regions. Chemical and textural features of orthopyroxene, amphibole and Fe-Ti oxides from NT suggest that crystallization of magmas occurred at polybaric conditions, confirming the rapid upwelling of magmas.

  17. Assessing lahars from ice-capped volcanoes using ASTER satellite data, the SRTM DTM and two different flow models: case study on Iztaccíhuatl (Central Mexico)

    Science.gov (United States)

    Schneider, D.; Delgado Granados, H.; Huggel, C.; Kääb, A.

    2008-06-01

    Lahars frequently affect the slopes of ice-capped volcanoes. They can be triggered by volcano-ice interactions during eruptions but also by processes such as intense precipitation or by outbursts of glacial water bodies not directly related to eruptive activity. We use remote sensing, GIS and lahar models in combination with ground observations for an initial lahar hazard assessment on Iztaccíhuatl volcano (5230 m a.s.l.), considering also possible future developments of the glaciers on the volcano. Observations of the glacial extent are important for estimations of future hazard scenarios, especially in a rapidly changing tropical glacial environment. In this study, analysis of the glaciers on Iztaccíhuatl shows a dramatic retreat during the last 150 years: the glaciated area in 2007 corresponds to only 4% of the one in 1850 AD and the glaciers are expected to survive no later than the year 2020. Most of the glacial retreat is considered to be related to climate change but in-situ observations suggest also that geo- and hydrothermal heat flow at the summit-crater area can not be ruled out, as emphasized by fumarolic activity documented in a former study. However, development of crater lakes and englacial water reservoirs are supposed to be a more realistic scenario for lahar generation than sudden ice melting by rigorous volcano-ice interaction. Model calculations show that possible outburst floods have to be larger than ~5×105 m3 or to achieve an H/L ratio (Height/runout Length) of 0.2 and lower in order to reach the populated lower flanks. This threshold volume equals 2.4% melted ice of Iztaccíhuatl's total ice volume in 2007, assuming 40% water and 60% volumetric debris content of a potential lahar. The model sensitivity analysis reveals important effects of the generic type of the Digital Terrain Model (DTM) used on the results. As a consequence, the predicted affected areas can vary significantly. For such hazard zonation, we therefore suggest the use of

  18. Assessing lahars from ice-capped volcanoes using ASTER satellite data, the SRTM DTM and two different flow models: case study on Iztaccíhuatl (Central Mexico

    Directory of Open Access Journals (Sweden)

    D. Schneider

    2008-06-01

    Full Text Available Lahars frequently affect the slopes of ice-capped volcanoes. They can be triggered by volcano-ice interactions during eruptions but also by processes such as intense precipitation or by outbursts of glacial water bodies not directly related to eruptive activity. We use remote sensing, GIS and lahar models in combination with ground observations for an initial lahar hazard assessment on Iztaccíhuatl volcano (5230 m a.s.l., considering also possible future developments of the glaciers on the volcano. Observations of the glacial extent are important for estimations of future hazard scenarios, especially in a rapidly changing tropical glacial environment. In this study, analysis of the glaciers on Iztaccíhuatl shows a dramatic retreat during the last 150 years: the glaciated area in 2007 corresponds to only 4% of the one in 1850 AD and the glaciers are expected to survive no later than the year 2020. Most of the glacial retreat is considered to be related to climate change but in-situ observations suggest also that geo- and hydrothermal heat flow at the summit-crater area can not be ruled out, as emphasized by fumarolic activity documented in a former study. However, development of crater lakes and englacial water reservoirs are supposed to be a more realistic scenario for lahar generation than sudden ice melting by rigorous volcano-ice interaction. Model calculations show that possible outburst floods have to be larger than ~5×105 m3 or to achieve an H/L ratio (Height/runout Length of 0.2 and lower in order to reach the populated lower flanks. This threshold volume equals 2.4% melted ice of Iztaccíhuatl's total ice volume in 2007, assuming 40% water and 60% volumetric debris content of a potential lahar. The model sensitivity analysis reveals important effects of the generic type of the Digital Terrain Model (DTM used on the results. As a consequence, the predicted affected areas can vary significantly. For such

  19. Entre el patrimonio natural y el cultural habita el mito: Isla del río Cuale (Puerto Vallarta, Jalisco, México

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    Andrade Romo, Edmundo

    2007-01-01

    Full Text Available International tourist places experience continuous changes, faster than non tourist cities or towns. This urban -tourist evolution is an excellent investigation subject to study local cultural heritage and its partner-anthropological implications, Puerto Vallarta, Jalisco, one of the three most important tourist centers in Mexico has not been the exception. This work notice how natural elements are transformed into cultural ones; by diachronic analysis diverse moments that conform and explain local identity are distinguished as well as the mythological construction about the local origin. Finally the former condition and social perception about the island, is exposed as the most significant natural-cultural element for people in Puerto Vallarta.

  20. La transformación urbana de Puerto Vallarta, Jalisco

    OpenAIRE

    Ericka Patricia Cárdenas Gómez; Juan Jorge Rodríguez Bautista

    2012-01-01

    Este artículo hace un recuento de la transformación urbana de Puerto Vallarta, Jalisco, durante un siglo (xx); se analiza la traza urbana y los cambios que ha vivido este municipio jalisciense a partir de relacionar el crecimiento urbano con los flujos migratorios y varios procesos de cambio social. El texto tiene como soporte empírico diversos planos y mapas, así como información estadística y documental.

  1. ARCHAEOMAGNETIC DATING OF THE ERUPTION OF XITLE VOLCANO, BASIN OF MEXICO: IMPLICATIONS FOR THE MESOAMERICAN CENTERS OF CUICUILCO AND TEOTIHUACAN (Datación arqueomagnética de la erupción del volcán Xitle, cuenca de México: implicaciones para los centros mesoamericanos de Cuicuilco y Teotihuacan)

    OpenAIRE

    Jaime Urrutia-Fucugauchi; Avto Goguitchaichvili; Ligia Pérez-Cruz; Juan Morales

    2016-01-01

    The Cuicuilco archaeological site in southern Basin of Mexico is covered by lava flows from the Xitle volcano. Dating the Xitle eruption and Cuicuilco abandonment has long been attempted. Contrasting results with radiocarbon dates around 2000 and 1670 yr BP have been reported, with implications for the development of the Mesoamerican centers of Cuicuilco and Teotihuacan. Here, we analyze radiocarbon dates and paleomagnetic data for the Xitle lava flows. New age estimates for the eruption are ...

  2. Santorini Volcano

    Science.gov (United States)

    Druitt, T.H.; Edwards, L.; Mellors, R.M.; Pyle, D.M.; Sparks, R.S.J.; Lanphere, M.; Davies, M.; Barreirio, B.

    1999-01-01

    Santorini is one of the most spectacular caldera volcanoes in the world. It has been the focus of significant scientific and scholastic interest because of the great Bronze Age explosive eruption that buried the Minoan town of Akrotiri. Santorini is still active. It has been dormant since 1950, but there have been several substantial historic eruptions. Because of this potential risk to life, both for the indigenous population and for the large number of tourists who visit it, Santorini has been designated one of five European Laboratory Volcanoes by the European Commission. Santorini has long fascinated geologists, with some important early work on volcanoes being conducted there. Since 1980, research groups at Cambridge University, and later at the University of Bristol and Blaise Pascal University in Clermont-Ferrand, have collected a large amount of data on the stratigraphy, geochemistry, geochronology and petrology of the volcanics. The volcanic field has been remapped at a scale of 1:10 000. A remarkable picture of cyclic volcanic activity and magmatic evolution has emerged from this work. Much of this work has remained unpublished until now. This Memoir synthesizes for the first time all the data from the Cambridge/Bristol/Clermont groups, and integrates published data from other research groups. It provides the latest interpretation of the tectonic and magmatic evolution of Santorini. It is accompanied by the new 1:10 000 full-colour geological map of the island.

  3. Solute fluxes from Tacaná volcano-hydrothermal system, Mexico-Guatemala. Implications for estimation of geothermal potential of the deep aquifer.

    Science.gov (United States)

    Collard, N.; Taran, Y.; Jácome Paz, M. P.; Campion, R.

    2014-12-01

    Tacaná (4100 m asl) is the northernmost volcano of the Central America Volcanic Arc. The volcano hosts a volcano-hydrothermal system that is manifested as a low-temperature fumarolic field at 3600 m asl and several groups of thermal springs principally located at the northwestern slopes of the volcanic edifice, at altitudes 1500 - 2000 m asl. These thermal springs discharge SO4-HCO3-enriched water (up to 1 g/kg of each one) with temperatures in the 25-63°C range. There are two distinct groups of springs with a different chloride-temperature and chloride-sulfate correlations but with the same 87Sr/86Sr ratio (~0.7046±0.0002) indicating the same wall rock composition for different aquifers. On April 2014, we found a cold spring (Manantial Nuevo), located at an elevation ~500 m lower than the others and with a different chemical composition, that discharges Na-Cl-type water with Cl concentration of 1.4 g/l and Na+K concentration up to 1.5 g/l. This new spring forms a fourth group, representing a stratified geothermal aquifer. Each thermal spring feeds a thermal stream that flows into the main drainage of the area, Río Coatán. Solute and heat fluxes from thermal springs of Tacaná volcano are estimated by the chloride-inventory method. The total observed chloride discharge from the thermal springs is estimated as 14.8 g/s and the total measured heat output of ~9.5 MW. Considering a deep fluid temperature of 250°C, the corresponding advective heat transport from the deep reservoirs that feed these springs may be estimate as 26 MW. However, the total chloride output measured in the main drainage (Coatán river) is 4 times higher (~59 g/s) than the measured Cl output of all known thermal springs. This means that other, undiscovered, thermal discharges exist in the area and that the natural heat output through thermal springs at Tacaná is significantly higher and depends on the Cl content and temperatures of the unknown thermal water discharges. If chloride

  4. Water quality of springs and water wells which are used in human consumption, in the Jocotitlan volcano region at State of Mexico; Calidad del agua de manantiales y pozos que se utilizan para consumo humano, en la region del volcan Jocotitlan, Estado de Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Baca G, A.; Segovia, N.; Iturbe, J.L. [Instituto Nacional de Investigaciones Nucleares, A.P. 18-1027, 11801 Mexico D.F. (Mexico); Martinez, V. [CIRA, UAEM, Unidad San Cayetabo, Toluca-Ixtlahuaca (Mexico); Armienta, M.A. [IGFUNAM, C. Universitaria, Mexico D.F. (Mexico); Seidel, J.L. [CNRS, Univ. Montpellier (France)

    1998-07-01

    In this work are presented the results of water quality of seven springs (San Antonio Enchisi, Las Fuentes, El Cerro, Pasteje, Los Reyes, Santa Cruz and Tiacaque) and two water wells (Jocotitlan No. 2 and La Providencia No. 35) which are used for human consumption and that are located surrounding area to Jocotitlan volcano, state of Mexico. It was determined the {sup 222} Rn concentration through liquid scintillation, the {sup 226} Ra by Gamma spectroscopy, the physical-chemical parameters (major elements) and bacteriological, using standardized methods. The minor elements and trace in solution were determined by Icp-Ms mass spectroscopy. The water quality was established in function of the standing standards. Therefore Las Fuentes, El Cerro, Santa Cruz, Tiacaque springs and the Jocotitlan No. 2 well, are drinkable water. So, Pasteje, Los Reyes, San Antonio Enchisi springs and the La Providencia No. 35 well are chemically drinkable but presenting bacteriological pollution. (Author)

  5. Mud Volcanoes Formation And Occurrence

    Science.gov (United States)

    Guliyev, I. S.

    2007-12-01

    Mud volcanoes are natural phenomena, which occur throughout the globe. They are found at a greater or lesser scale in Azerbaijan, Turkmenistan, Georgia, on the Kerch and Taman peninsulas, on Sakhalin Island, in West Kuban, Italy, Romania, Iran, Pakistan, India, Burma, China, Japan, Indonesia, Malaysia, New Zealand, Mexico, Colombia, Trinidad and Tobago, Venezuela and Ecuador. Mud volcanoes are most well-developed in Eastern Azerbaijan, where more than 30% of all the volcanoes in the world are concentrated. More than 300 mud volcanoes have already been recognized here onshore or offshore, 220 of which lie within an area of 16,000 km2. Many of these mud volcanoes are particularly large (up to 400 m high). The volcanoes of the South Caspian form permanent or temporary islands, and numerous submarine banks. Many hypotheses have been developed regarding the origin of mud volcanoes. Some of those hypotheses will be examined in the present paper. Model of spontaneous excitation-decompaction (proposed by Ivanov and Guliev, 1988, 2002). It is supposed that one of major factors of the movement of sedimentary masses and formation of hydrocarbon deposits are phase transitions in sedimentary basin. At phase transitions there are abnormal changes of physical and chemical parameters of rocks. Abnormal (high and negative) pressure takes place. This process is called as excitation of the underground environment with periodicity from several tens to several hundreds, or thousand years. The relationship between mud volcanism and the generation of hydrocarbons, particularly methane, is considered to be a critical factor in mud volcano formation. At high flow rates the gas and sediment develops into a pseudo-liquid state and as flow increases the mass reaches the "so-called hover velocity" where mass transport begins. The mass of fluid moves as a quasi-uniform viscous mass through the sediment pile in a piston like manner until expelled from the surface as a "catastrophic eruption

  6. The 21,700 yr b.p. Lower Toluca Pumice Plinian Eruption of Nevado de Toluca Volcano (Mexico): Evidences of Magma Mixing Process as Triggering Mechanism.

    Science.gov (United States)

    Capra, L.; Arce, J.; Macias, J.

    2006-05-01

    Approximately 21,700 yr B.P., after a period of quiescence of 4800 yr, Nevado de Toluca volcano erupted, producing the Lower Toluca Pumice deposit. The activity generated a 24-km-high Plinian column that lasted ~11 h and dispersed 2.3 km3 (0.8 km3 dense rock equivalent) of tephra toward the NE, blanketing the Lerma basin, an area occupied today by the city of Toluca, with up to 5 cm of ash. Subsequent eruptive pulses were sub-Plinian in style, accompanied by phreatomagmatic explosions that emplaced surge deposits. Finally, the column collapsed toward the NE with the emplacement of a pumice flow deposit. The high vesicularity of the pumice from the basal Plinian layer, up to 83% by volume, indicates that exsolution was dominantly magmatic, and that pressurization of the magma chamber was probably due to a magma mixing process. Evidence for this includes the compositional range of juvenile products (from 55 to 65 wt% SiO2), as well as the presence of two types of plagioclase, one in equilibrium and the other one with disequilibrium textures and reverse zoning. This suggests input of an andesitic liquid into the dacitic magma chamber. Based on the eruptive record, the most likely future eruptive activity at Nevado de Toluca volcano will be Plinian. Although quiet for more than 3250 yr, Plinian activity could occur after a long period of quiescence, and it could represent a hazard for the entire Toluca basin, where more than one million people live today.

  7. La transformación urbana de Puerto Vallarta, Jalisco

    Directory of Open Access Journals (Sweden)

    Ericka Patricia Cárdenas Gómez

    2012-01-01

    Full Text Available Este artículo hace un recuento de la transformación urbana de Puerto Vallarta, Jalisco, durante un siglo (xx; se analiza la traza urbana y los cambios que ha vivido este municipio jalisciense a partir de relacionar el crecimiento urbano con los flujos migratorios y varios procesos de cambio social. El texto tiene como soporte empírico diversos planos y mapas, así como información estadística y documental.

  8. Magmatic controls on eruption dynamics of the 1950 yr B.P. eruption of San Antonio Volcano, Tacaná Volcanic Complex, Mexico-Guatemala

    Science.gov (United States)

    Mora, Juan Carlos; Gardner, James Edward; Macías, José Luis; Meriggi, Lorenzo; Santo, Alba Patrizia

    2013-07-01

    San Antonio Volcano, in the Tacaná Volcanic Complex, erupted ~ 1950 yr. B.P., with a Pelean type eruption that produced andesitic pyroclastic surges and block-and-ash flows destroying part of the volcano summit and producing a horse-shoe shaped crater open to the SW. Between 1950 and 800 yr B.P. the eruption continued with effusive andesites followed by a dacite lava flow and a summit dome, all from a single magma batch. All products consist of phenocrysts and microphenocrysts of zoned plagioclase, amphibole, pyroxene, magnetite ± ilmenite, set in partially crystallized groundmass of glass and microlites of the same mineral phases, except for the lack of amphibole. Included in the andesitic blocks of the block-and-ash flow deposit are basaltic andesite enclaves with elongated and ellipsoidal forms and chilled margins. The enclaves have intersertal textures with brown glass between microphenocrysts of plagioclase, hornblende, pyroxene, and olivine, and minor proportions of phenocrysts of plagioclase, hornblende, and pyroxene. A compositional range obtained of blocks and enclaves resulted from mixing between andesite (866 °C ± 22) and basaltic andesite (enclaves, 932 °C ± 22), which may have triggered the explosive Pelean eruption. Vestiges of that mixing are preserved as complex compositional zones in plagioclase and clinopyroxene-rich reaction rims in amphibole in the andesite. Whole-rock chemistry, geothermometry, experimental petrology and modeling results suggest that after the mixing event the eruption tapped hybrid andesitic magma (≤ 900 °C) and ended with effusive dacitic magma (~ 825 °C), all of which were stored at ~ 200 MPa water pressure. A complex open-system evolution that involved crustal end-members best explains the generation of effusive dacite from the hybrid andesite. Amphibole in the dacite is rimmed by reaction products of plagioclase, orthopyroxene, and Fe-Ti oxides produced by decompression during ascent. Amphibole in the andesite

  9. Tectonic evolution of the central-eastern sector of Trans Mexican Volcanic Belt and its influence on the eruptive history of the Nevado de Toluca volcano (Mexico)

    Science.gov (United States)

    Bellotti, F.; Capra, L.; Groppelli, G.; Norini, G.

    2006-11-01

    The Nevado de Toluca is an andesitic to dacitic stratovolcano of Late Pliocene-Holocene age located within the central and eastern sectors of the Trans Mexican Volcanic Belt. Morphostructural analysis, aerial photograph and satellite image interpretation, structural analysis and geological fieldwork were methods used to investigate the relationship between the evolution of the volcano and the tectonic framework of its basement. The study revealed that the area of Nevado de Toluca is affected by three main fault systems that intersect close to the volcanic edifice. These are from oldest to youngest, the Taxco-Querétaro, San Antonio and Tenango fault systems. The NNW-SSE Taxco-Querétaro fault system was active in the area since Early Miocene, and is characterized by right-lateral transtensive movement. Its reactivation during Early to Middle Pleistocene was responsible for the emplacement of andesitic to dacitic lava flows and domes of La Cieneguilla Supersynthem. The NE-SW San Antonio fault system was active during Late Pliocene, before the reactivation of the Taxco-Querétaro fault system, and is characterized by extensional left-lateral oblique-slip kinematics. The youngest is the E-W Tenango fault system that has been active since Late Pleistocene. This fault system is characterized by transtensive left-lateral strike-slip movement, and partly coeval with the youngest eruptive phase, the Nevado Supersynthem, which formed the present summit cone of the Nevado de Toluca volcano. The stress re-orientation from the Taxco-Querétaro to the Tenango fault system during Late Pleistocene is responsible for the ˜ 1 Ma hiatus in the magmatic activity between 1.15 Ma and 42 ka. After this period of repose, the eruptive style drastically changed from effusive to explosive with the emission of dacitic products. The methodology presented here furnish new data that can be used to better assess the complex structural evolution of this sector of the Trans Mexican Volcanic Belt

  10. Four new species of Cymatodera Gray from central and southern Mexico (Coleoptera, Cleridae, Tillinae

    Directory of Open Access Journals (Sweden)

    Alan F. Burke

    2015-07-01

    Full Text Available Four new species of Cymatodera are described from Mexico: C. tortuosa Burke & Rifkind, sp. n. from Hidalgo and Tamaulipas; C. ortegae Burke, sp. n. from Colima, Jalisco and Michoacan; C. gerstmeieri Burke & Rifkind, sp. n. from Chiapas; and C. mixteca Burke & Rifkind, sp. n. from Puebla and Guerrero. Male genitalia and other characters of taxonomic value are illustrated.

  11. Four new species of Cymatodera Gray from central and southern Mexico (Coleoptera, Cleridae, Tillinae)

    Science.gov (United States)

    Burke, Alan F.; Rifkind, Jacques; Zolnerowich, Gregory

    2015-01-01

    Abstract Four new species of Cymatodera are described from Mexico: Cymatodera tortuosa Burke & Rifkind, sp. n. from Hidalgo and Tamaulipas; Cymatodera ortegae Burke, sp. n. from Colima, Jalisco and Michoacan; Cymatodera gerstmeieri Burke & Rifkind, sp. n. from Chiapas; and Cymatodera mixteca Burke & Rifkind, sp. n. from Puebla and Guerrero. Male genitalia and other characters of taxonomic value are illustrated. PMID:26257571

  12. Payments for ecosystem services and rural development: Landowners' preferences and potential participation in western Mexico

    NARCIS (Netherlands)

    Balderas Torres, A.; MacMillan, D.C.; Skutsch, M.; Lovett, J.C.

    2013-01-01

    Incentive-based mechanisms can contribute to rural development and deliver environmental services, but need to be attractive to landowners and communities to ensure their participation. Here we study the views of landowners and agrarian communities (ejidos) from central Jalisco in Mexico to identify

  13. Genetic data of 15 autosomal STRs (Identifiler kit) of three Mexican Mestizo population samples from the States of Jalisco (West), Puebla (Center), and Yucatan (Southeast).

    Science.gov (United States)

    Rubi-Castellanos, R; Anaya-Palafox, M; Mena-Rojas, E; Bautista-España, D; Muñoz-Valle, J F; Rangel-Villalobos, H

    2009-06-01

    We report autosomal STR data (Identifiler PCR amplification kit) of a total sample of 884 unrelated Mestizos from three different regions of Mexico. The population sample included 309, 313 and 262 individuals from the states of Jalisco (West), Puebla (Center) and Yucatan (Southeast), respectively. Allele distribution and forensic statistical parameters are described. Genotype distribution by locus and two-loci combination was in agreement with Hardy-Weinberg expectations for all 15 STRs. Pairwise comparisons including Mexican populations reported in the literature demonstrated a significant differentiation, principally between North/West with regard to Center/Southeast Mexico. These results increase STR data from previously unreported regions of this country, and constitute a valuable guide in forensic casework for choosing an auxiliary STR database in states where it is not available.

  14. Sem Analysis of particles from the 28, 000 B.P El Zaguan debris avalanche deposit, Nevado de Toluca volcano, Central Mexico: evidences of flow behavior during emplacement

    Science.gov (United States)

    Caballero, L.; Capra, L.

    2008-12-01

    The Zaguan deposit originated at 28, 000 yr. B.P from the flank collapse of the Nevado de Toluca volcano, a dacitic stratovolcano of the Transmexican Volcanic Belt. A Scanning Electron Microprobe analysis (SEM) was made to some clasts of this deposit to observe microtextures produced during transport and emplacement of the debris avalanche flow. Particles from 2, 0 and -2 Φ granulometric classes were randomly selected and their surface textures were described. The textures observed were divided in two groups, collision and shear structures indicating different clast interaction. Shear textures were observed predominantly on the basal part of the deposit and consisted of parallel ridges, parallel grooves, scratches and lips. Collision textures were mainly present in the upper part of the deposit and consisted of fractures, percussion marks, and broken or grinded crystals. These characteristics, coupled with field observation, like the presence of clast dikes and deformed lacustrine megaclasts, indicate that the basal part of the debris avalanche was moving in a partially liquefied state, were particles were not able to move freely because of the confinement exerted by the upper part of the flow, so shear stresses dominated. On the contrary, the particles in the upper part were able to move freely so the principal mechanism of interaction between particles was collision. These microscopic textures are in agreement with previously described behavior of emplacement of debris avalanches of volcanic origin, that suggest a stratified flow dominated by different transport and depositional mechanism depending on flow depth and possible fluid content at their base.

  15. Del sacrificio al ocio en Jalisco, México

    Directory of Open Access Journals (Sweden)

    Jose Luis Cornejo\\u2011Ortega

    2016-01-01

    Full Text Available El turismo religioso, turismo en espacios religiosos o las peregrinaciones, han crecido considerablemente, más de 30 millones de personas se desplazan anualmente en México sólo por motivación religiosa y se estima una derrama económica de 680 millones de dólares. Este trabajo pretende establecer la motivación de la visita de santuarios en seis localidades del estado de Jalisco y analizar si se relaciona con la idea de sacrificio y fe del peregrino o con el ocio y placer del turista dedicado a la experiencia y vivencia del fenómeno religiosos, así como el grado de transición entre recinto religioso y atractivo turístico., desde una perspectiva del turismo cultural, lo que enfrenta la idea de un turismo alternativo. Se puede afirmar que en Jalisco, con relación al turismo religioso, predomina la condición de peregrino (sacrificio en los visitantes y los espacios sacros y sus contenidos culturales aún cumplen la función de generar entornos propicios para la veneración, la contemplación y la adoración.

  16. Watershed Management and Mercury Biogeochemical Cycling in Lake Zapotlan, Mexico

    Science.gov (United States)

    Malczyk, E. A.; Branfireun, B. A.

    2009-05-01

    Lake Zapotlan is an endorheic subtropical eutrophic lake located in Jalisco State, Mexico. The lake supports a small but important local fishery for carp (Cyprinus sp.) and tilapia (Oreochromis sp.) and is an internationally recognized RAMSAR site. Very little research exists in these regions regarding mercury biogeochemical cycling. The lake receives considerable untreated municipal wastewater discharge that is elevated in inorganic total mercury (250-800 ng Hg/L) and organic methylmercury (3-10 ng CH3Hg+/L). The lake is also located on an active fault zone near an active volcano which may cause natural mercury enrichment. To assess a mercury risk to the commercial fishery we investigated the distribution of total inorganic mercury and organic methylmercury in waters, sediments, and fish tissues of the lake, surrounding wetlands, and incoming waters. Although there were high concentrations of inorganic mercury entering the lake in wastewater and seasonal tributary stream flow inputs, average concentrations in lake surface waters (3 ng Hg/L) and sediments (50 ng Hg/gdw) were relatively low. Average concentrations of total inorganic mercury were an order of magnitude higher in water (70 ng Hg/L) and sediment (245 ng Hg/gdw) in wetlands receiving the wastewater discharges. Mercury loading to the main body of the lake is likely reduced by these wetland buffer zones which allow mercury bound to particulate matter to settle out. A similar pattern was seen with respect to methylmercury concentrations. Average concentrations of methylmercury in lake surface water (below detect) and sediment (0.1 ng/gdw) were lower than in impounded wetlands (1 ng CH3Hg+/L, 0.7 ng CH3Hg+/gdw). Mercury concentrations in tilapia (3.5 ng/g) and carp (8 ng/g) from the commercial catch were found to be low in mercury; likely due to a combination of physiological, biogeochemical, and ecological factors.

  17. Geomorphological evolution of volcanic fluvial channels: Eighteen years of morphological monitoring of the upper strect of the Tenenepanco Gorge, Popocatépetl volcano, Mexico

    Science.gov (United States)

    Tanarro, Luis Miguel; Juan Zamorano, Jose; Andres, Nuria; Palacios, David

    2015-04-01

    During volcanic eruptions a significant volume of material accumulates on the slopes and pre-existing gorges of the stratovolcanoes. This abundance of loose and unconsolidated material is very likely to be mobilized by rapid flows or lahars generated by sudden heavy rain or melting snow and ice. Thus, volcanic gorges are affected by complex cycles of incision, filling and widening, altering the equilibrium of river systems due to the major changes that lahars cause in channel morphology. These geomorphological dynamics characterize the gorges located on the north flank of the Popocatépetl volcano (19°02' N, 98°62' W, 5424 m). This volcano, located in the centre of the Trans-Mexican Volcanic Belt, began its most recent eruptive period in December 1994, when a glacier partially covered the northern slope. Since then, the interaction of volcanic and glacier activity triggered the formation of lahars in the gorges, causing significant morphological changes in the channel (especially in April 1995, July 1997 and January 2001). The most recent major eruption at Popocatépetl took place on 19 July 2003, and since then a series of smaller eruptions has reduced the glacier to near extinction. The aim of this study is to assess the morphological response of the Tenenepanco channel over an 18-year period, from 1995-2013, where two main scenarios can be observed: a) the period from 1995 to 2001 of volcanic activity and glacier retreat with the formation of flows and b) the period from 2002 to 2013 of relative volcanic calm, the almost complete extinction of the glacier, and the formation of secondary lahars associated with heavy rainfall. Monitoring of the gorge has consisted in the elaboration of 14 geomorphological maps during field studies (November 14, 1995, December 5, 1997, February 7, 1998, October 6, 2001, November 14, 1995, December 5, 1997, February 7, 1998, October 6, 2001, Julio 16, 2002, February 11, 2004, September 8, 2004, February 5, 2006, November 2, 2008

  18. Maternal fetal transmission of Trypanosoma cruzi: a problem of public health little studied in Mexico.

    Science.gov (United States)

    Cardoso, Enedina Jiménez; Valdéz, Guillermina Campos; Campos, Adrián Cortes; de la Luz Sanchez, Rene; Mendoza, Carlos Rivera; Hernández, Arturo Plascencia; Ramírez, María Hernández; Habana, Joel Ruiz; González, Edmundo Bonilla; Matzumura, Pablo Damian; Carlier, Yves

    2012-08-01

    The first case of neonatal Chagas was reported in Mexico in 1998, but there have been no studies since then. Therefore, we investigated the rates of congenital infection of Trypanosoma cruzi by examining the seroprevalence among 1448 pregnant women in Oaxaca, Jalisco and Mexico City. We performed ELISAs to screen for recombinant and total antigens in mothers, and examined the frequency of congenital T. cruzi transmission by PCR with cord blood and antibody testing in children when they reached two years old. Our results showed that the prevalence of infection in pregnant women was 7.32% (106/1448) overall, and 4.4% (35/794) in Oaxaca, 12.02% (67/557) in Jalisco and 4.12% (4/97) in the Mexico City. In Oaxaca, T. cruzi infection was detected by PCR in 20% (7/35) of infants born to seroreactive mothers and 11.9% (8/67) in Jalisco. No infections were identified in infants from the Mexico City. From these only eleven serological follow up their children are agree to take blood. Therefore, the maternal-fetal overall transmission rate was 4.08% (4/98) in Oaxaca and 9.1% (3/33) in Jalisco 1.5% (1/65) children with positive serology were given specific treatment Chagas. In conclusion, these are the first reports of the rates of congenital Chagas disease in Mexico. The seroprevalence was higher in mothers from Jalisco, and could be related to that there is not the periodic fumigation of the transmitting vector performed in that state. The high rates of maternal-fetal transmission found in Oaxaca could be related to the differences of pathogenicity of trypanosome. No association between both the rate of congenital transmission and the gynecologic anthropometric data was observed.

  19. An overview of a GIS method for mapping landslides and assessing landslide susceptibility in the Río La Carbonera watershed, on the SE flank of Pico de Orizaba Volcano, Mexico.

    Science.gov (United States)

    Legorreta Paulin, G.; Bursik, M. I.; Contreras, T.

    2015-12-01

    This poster provides an overview of the on-going research project (Grant PAPIIT # IN102115) from the Institute of Geography at the National Autonomous University of Mexico (UNAM) that seeks to conduct a multi-temporal landslide inventory, produce a landslide susceptibility map, and estimate sediment production by using Geographic Information Systems (GIS). The Río La Carbonera watershed on the southeastern flank of Pico de Orizaba volcano, the highest mountain in Mexico, is selected as a study area. The catchment covers 71.9 km2 with elevations ranging from 1224 to 3643 m a.s.l. and hillslopes between <5° and 68°. The stream system of Río La Carbonera catchment erodes Tertiary and Quaternary lavas, pyroclastic flows, and fall deposits. The geologic and geomorphologic factors in combination with high seasonal precipitation, high degree of weathering, and steep slopes predispose the study area to landslides. The methodology encompasses three main stages of analysis to assess landslide hazards: Stage 1 builds a historic landslide inventory. In the study area, an inventory of more than 200 landslides is created from multi-temporal aerial-photo-interpretation and local field surveys to assess landslide distribution. All landslides were digitized into a geographic information system (GIS), and a spatial geo-database of landslides was constructed from standardized GIS datasets. Stage 2 calculates the susceptibility for the watershed. During this stage, (SINMAP using default values) is evaluated. Stage 3 Estimate the potential total material delivered to the main stream drainage channel by all landslides in the catchment. Detailed geometric measurements of individual landslides visited during the field work will be carried out to obtain the landslide area and volume. These measurements revealed an empirical relationship between area and volume that took the form of a power law. This relationship will be used to estimate the potential volume of material delivered to the

  20. An overview of a GIS method for mapping landslides and assessing landslide hazards at Río El Estado watershed, on the SW flank of Pico de Orizaba Volcano, Mexico

    Science.gov (United States)

    Legorreta Paulin, G.; Bursik, M. I.; Contreras, T.; Polenz, M.; Ramírez Herrera, M.; Paredes Mejía, L.; Arana Salinas, L.

    2012-12-01

    This poster provides an overview of the on-going research project (Grant SEP-CONACYT no 167495) from the Institute of Geography at the National Autonomous University of Mexico (UNAM) that seeks to conduct a multi-temporal landslide inventory, produce a landslide susceptibility map, and estimate sediment production by using Geographic Information Systems (GIS). The Río El Estado watershed on the southwestern flank of Pico de Orizaba volcano, the highest mountain in Mexico, is selected as a study area. The catchment covers 5.2 km2 with elevations ranging from 2676.79 to 4248.2 m a.s.l. and hillslopes between 0° and 56°. The stream system of Río El Estado catchment erodes Tertiary and Quaternary lavas, pyroclastic flows, and fall deposits. The geologic and geomorphologic factors in combination with high seasonal precipitation, high degree of weathering, and steep slopes predispose the study area to landslides. The methodology encompasses three main stages of analysis to assess landslide hazards: Stage 1 builds a historic landslide inventory. In the study area, an inventory of more than 170 landslides is created from multi-temporal aerial-photo-interpretation and local field surveys to assess landslide distribution. All landslides were digitized into a geographic information system (GIS), and a spatial geo-database of landslides was constructed from standardized GIS datasets. Stage 2 Calculates the susceptibility for the watershed. During this stage, Multiple Logistic Regression and SINMAP) will be evaluated to select the one that provides scientific accuracy, technical accessibility, and applicability. Stage 3 Estimate the potential total material delivered to the main stream drainage channel by all landslides in the catchment. Detailed geometric measurements of individual landslides visited during the field work will be carried out to obtain the landslide area and volume. These measurements revealed an empirical relationship between area and volume that took the

  1. Application of HydroGeoSphere to model the response to anthropogenic climate change of three-dimensional hydrological processes in the geologically, geothermally, and topographically complex Valles Caldera super volcano, New Mexico: Preliminary results

    Science.gov (United States)

    Wine, M.; Cadol, D. D.

    2014-12-01

    Anthropogenic climate change is expected to reduce streamflow in the southwestern USA due to reduction in precipitation and increases in evaporative demand. Understanding the effects of climate change in this region is particularly important for mountainous areas since these are primary sources of recharge in arid and semi-arid environments. Therefore we undertook to model effects of climate change on the hydrological processes in Valles Caldera (448 km2), located in the Jemez Mountains of northern New Mexico. In Valles Caldera modeling the surficial, hydrogeological, and geothermal processes that influence hydrologic fluxes each present challenges. The surficial dynamics of evaporative demand and snowmelt both serve to control recharge dynamics, but are complicated by the complex topography and spatiotemporal vegetation dynamics. Complex factors affecting evaporative demand include leaf area index, temperature, albedo, and radiation affected by topographic shading; all of these factors vary in space and time. Snowmelt processes interact with evaporative demand and geology to serve as an important control on streamflow generation, but modeling the effects of spatiotemporal snow distributions on streamflow generation remains a challenge. The complexity of Valles Caldera's geology—and its associated hydraulic properties—rivals that of its surficial hydrologic forcings. Hydrologically important geologic features that have formed in the Valles Caldera are three-dimensionally intricate and include a dense system of faults, alluvium, landslides, lake deposits, and features associated with the eruption and collapse of this super volcano. Coupling geothermally-driven convection to the hydrologic cycle in this still-active geothermal system presents yet an additional challenge in modeling Valles Caldera. Preliminary results from applying the three-dimensional distributed hydrologic finite element model HydroGeoSphere to a sub-catchment of Valles Caldera will be

  2. Regional Development and Sustainability: Cultural Tourism in the Southern Region of Jalisco

    Directory of Open Access Journals (Sweden)

    José G. Vargas-Hernández

    2012-11-01

    Full Text Available This study aims to determine the potential of cultural tourism in the municipalities that comprise region 6 of the State of Jalisco, territorially delimited in the South of Jalisco. (Subject is missing Are tested first to identify the demand for cultural tourism to determine the profile of the cultural tourist under the assumptions that tourists especially motivated by culture tend to travel longer distances than most tourists. It discusses the motivations and satisfactions of cultural tourists in order to establish the potential market in accordance with the characteristics of the target market in the southern region of Jalisco. Any operation of cultural tourism companies should make the strategic diagnosis, which explains the use of SWOT analysis as a tool for strategic planning of cultural tourism enterprises. Finally, we propose some development strategies of cultural tourism in this region of Southern Jalisco.

  3. Source mechanism of Vulcanian degassing at Popocatépetl Volcano, Mexico, determined from waveform inversions of very long period signals

    Science.gov (United States)

    Chouet, Bernard A.; Dawson, Phillip B.; Arciniega-Ceballos, Alejandra

    2005-01-01

    The source mechanism of very long period (VLP) signals accompanying volcanic degassing bursts at Popocatépetl is analyzed in the 15–70 s band by minimizing the residual error between data and synthetics calculated for a point source embedded in a homogeneous medium. The waveforms of two eruptions (23 April and 23 May 2000) representative of mild Vulcanian activity are well reproduced by our inversion, which takes into account volcano topography. The source centroid is positioned 1500 m below the western perimeter of the summit crater, and the modeled source is composed of a shallow dipping crack (sill with easterly dip of 10°) intersecting a steeply dipping crack (northeast striking dike dipping 83° northwest), whose surface extension bisects the vent. Both cracks undergo a similar sequence of inflation, deflation, and reinflation, reflecting a cycle of pressurization, depressurization, and repressurization within a time interval of 3–5 min. The largest moment release occurs in the sill, showing a maximum volume change of 500–1000 m3, pressure drop of 3–5 MPa, and amplitude of recovered pressure equal to 1.2 times the amplitude of the pressure drop. In contrast, the maximum volume change in the dike is less (200–300 m3), with a corresponding pressure drop of 1–2 MPa and pressure recovery equal to the pressure drop. Accompanying these volumetric sources are single-force components with magnitudes of 108 N, consistent with melt advection in response to pressure transients. The source time histories of the volumetric components of the source indicate that significant mass movement starts within the sill and triggers a mass movement response in the dike within a few seconds. Such source behavior is consistent with the opening of a pathway for escape of pent-up gases from slow pressurization of the sill driven by magma crystallization. The opening of this pathway and associated rapid evacuation of volcanic gases induces the pressure drop. Pressure

  4. Global Volcano Locations Database

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — NGDC maintains a database of over 1,500 volcano locations obtained from the Smithsonian Institution Global Volcanism Program, Volcanoes of the World publication. The...

  5. Seven new species of Allorhogas (Hymenoptera: Braconidae: Doryctinae) from Mexico

    OpenAIRE

    Juan José Martínez; Alejandro Zaldívar-Riverón

    2013-01-01

    Seven new Mexican species of the gall associated doryctine genus Allorhogas are described, illustrated and molecularly characterized: A. amuzgo sp. nov., A. coccolobae sp. nov., A. crassifemur sp. nov., A. jaliscoensis sp. nov., A. marshi sp. nov., A. parvus sp. nov., and A. scotti sp. nov. These new species were collected in tropical dry forests situated along the Pacific coast of Mexico in the states of Jalisco, Oaxaca and Guerrero. Allorhogas coccolobae was reared from leaf galls probably ...

  6. A Scientific Excursion: Volcanoes.

    Science.gov (United States)

    Olds, Henry, Jr.

    1983-01-01

    Reviews an educationally valuable and reasonably well-designed simulation of volcanic activity in an imaginary land. VOLCANOES creates an excellent context for learning information about volcanoes and for developing skills and practicing methods needed to study behavior of volcanoes. (Author/JN)

  7. UN ACERCAMIENTO AL TURISMO RELIGIOSO EN LOS ALTOS DE JALISCO

    Directory of Open Access Journals (Sweden)

    Rogelio Martínez Cárdena

    2009-07-01

    Full Text Available El turismo religioso en la región de Los Altos de Jalisco ha encontrado un campo fértil desde el siglo XVII con el surgimiento de la devoción a la Virgen de San Juan de los Lagos, y que a partir del año 2000 ha visto incrementada la afluencia de visitantes debido a la canonización de los mártires cristeros, esto ha dado como resultado un programa oficial de promoción turística denominado “ruta cristera” y el surgimiento de nuevos centros de devoción religiosa que tan sólo en el caso de Santa Ana de Guadalupe recibe aproximadamente un millón de visitantes al año.

  8. [Risk factors for osteoporosis in postmenopausal women from Guadalajara, Jalisco].

    Science.gov (United States)

    González-Mercado, Anahí; Sánchez-López, J Yoaly; Ibarra, Bertha

    2013-12-01

    To know risk factors and the frequency of osteoporosis (OP) in postmenopausal women. Bone mineral density was measured in lumbar spine of 513 postmenopausal women from a hospital of Guadalajara, Jalisco during 2007-2008. The cutoff points of the associated variables were obtained by ROC curves and odds ratio (OR) by logistic regression. The 25.2% (95%CI 21.44-28.96) of the women was OP. The variables associated with OP and cutoff points were age >60 years, weight <71 kg, height <1.54 m and BMI <29.2 kg/m(2), with OR greater than 3.19 (p<0.0001). It is recommended setting cutoff points to estimate risk factors for OP more accurately in each population.

  9. Sindicalismo en Jalisco: nuevo proceso de fin de siglo

    Directory of Open Access Journals (Sweden)

    Ignacio Medina Núñez

    1999-01-01

    Full Text Available En este artículo se aborda la situación del sindicalismo en el estado de Jalisco, tratando de caracterizar la pluralidad organizativa que se ha generado hasta la década de los noventa. Con algunas consideraciones teóricas sobre el modelo del corporativismo sindical y ofreciendo luego algunos antecedentes históricos, se intenta profundizar en el reacomodo de las dirigencias sindicales después de la muerte de los principales líderes y en la pluralidad de diversas organizaciones sindicales que han surgido, situación en donde concurre la permanencia del sindicalismo oficial y el surgimiento de otras opciones como los independientes, la Unión Nacional de Trabajadores, etc.

  10. Volcano seismology

    Science.gov (United States)

    Chouet, B.

    2003-01-01

    A fundamental goal of volcano seismology is to understand active magmatic systems, to characterize the configuration of such systems, and to determine the extent and evolution of source regions of magmatic energy. Such understanding is critical to our assessment of eruptive behavior and its hazardous impacts. With the emergence of portable broadband seismic instrumentation, availability of digital networks with wide dynamic range, and development of new powerful analysis techniques, rapid progress is being made toward a synthesis of high-quality seismic data to develop a coherent model of eruption mechanics. Examples of recent advances are: (1) high-resolution tomography to image subsurface volcanic structures at scales of a few hundred meters; (2) use of small-aperture seismic antennas to map the spatio-temporal properties of long-period (LP) seismicity; (3) moment tensor inversions of very-long-period (VLP) data to derive the source geometry and mass-transport budget of magmatic fluids; (4) spectral analyses of LP events to determine the acoustic properties of magmatic and associated hydrothermal fluids; and (5) experimental modeling of the source dynamics of volcanic tremor. These promising advances provide new insights into the mechanical properties of volcanic fluids and subvolcanic mass-transport dynamics. As new seismic methods refine our understanding of seismic sources, and geochemical methods better constrain mass balance and magma behavior, we face new challenges in elucidating the physico-chemical processes that cause volcanic unrest and its seismic and gas-discharge manifestations. Much work remains to be done toward a synthesis of seismological, geochemical, and petrological observations into an integrated model of volcanic behavior. Future important goals must include: (1) interpreting the key types of magma movement, degassing and boiling events that produce characteristic seismic phenomena; (2) characterizing multiphase fluids in subvolcanic

  11. PRESENCIA DE LA CERÁMICA SEUDO-CLOISONNÉ EN LA CULTURA BOLAÑOS, JALISCO Y ZACATECAS (Presence of the Pseudo-cloisonné Pottery in the Bolaños Culture, Jalisco and Zacatecas

    Directory of Open Access Journals (Sweden)

    María Teresa Cabrero G.

    2012-12-01

    Full Text Available La cerámica seudo-cloisonné tuvo una amplia distribución en el mundo prehispánico mexicano a partir de 200 d. C. Se denominó así por la semejanza en la técnica decorativa con el verdadero cloisonné elaborado sobre metal. La presencia de esta técnica poscocción en la cultura Bolaños, ubicada en parte de los estados de Jalisco y Zacatecas, constituyó una prueba más del contacto comercial que existió con la cultura Chalchihuites (noroeste de Zacatecas; a la cual le llegó a través de la ruta de intercambio comercial que partía desde Teotihuacan hacia el norte, en búsqueda de la preciada turquesa cuyos yacimientos se encuentran en Nuevo México. La decoración de las vasijas empleando esta técnica demostró la presencia de artesanos especialistas dentro de una sociedad con un avanzado desarrollo; los motivos señalan la ideología de sus creadores al plasmar representaciones de la fauna, la flora y personajes distinguidos dentro de la sociedad. ENGLISH: The pseudo-cloisonné pottery was widely distributed among the prehispanic world in Mexico from 200 AD. These objects are described as pseudo-cloisonné because of similarities to the decorative technique employed by the true cloisonné made of metal. The presence of this technique post-firing in the Bolaños culture, which is located among the states of Jalisco and Zacatecas, is further evidence of the commercial contact that took place with the Chalchihuites culture (Northeast Zacatecas. These objects arrived to Chalchihuites through the commercial exchange that began in Teotihuacan and traveled northward in search of the valuable turquoise mines located in New Mexico. The decoration on these objects using this technique shows evidence of the existence of highly skilled people specialized in this technique among this society. The decoration in general represents the ideology of the craftsmen when they embedded the features of nature as well as distinctive people among their

  12. Volcanoes: Nature's Caldrons Challenge Geochemists.

    Science.gov (United States)

    Zurer, Pamela S.

    1984-01-01

    Reviews various topics and research studies on the geology of volcanoes. Areas examined include volcanoes and weather, plate margins, origins of magma, magma evolution, United States Geological Survey (USGS) volcano hazards program, USGS volcano observatories, volcanic gases, potassium-argon dating activities, and volcano monitoring strategies.…

  13. Constraints on Jalisco Block Motion and Tectonics of the Guadalajara Triple Junction from 1998-2001 Campaign GPS Data

    Science.gov (United States)

    Selvans, Michelle M.; Stock, Joann M.; Demets, Charles; Sanchez, Osvaldo; Marquez-Azua, Bertha

    2011-08-01

    A GPS campaign network in the state of Jalisco was occupied for ~36 h per station most years between 1995 and 2005; we use data from 1998-2001 to investigate tectonic motion and interseismic deformation in the Jalisco area with respect to the North America plate. The twelve stations used in this analysis provide coverage of the Jalisco Block and adjacent North America plate, and show a pattern of motion that implies some contribution to Jalisco Block boundary deformation from both tectonic motion and interseismic deformation due to the offshore 1995 earthquake. The consistent direction and magnitude of station motion on the Jalisco Block with respect to the North America reference frame, ~2 mm/year to the southwest (95% confidence level), perhaps can be attributed to tectonic motion. However, some station velocities within and across the boundaries of the Jalisco Block are also non-zero (95% confidence level), and the overall pattern of station velocities indicates both viscoelastic response to the 1995 earthquake and partial coupling of the subduction interface (together termed "interseismic deformation"). Our results show motion across the northern Colima rift, the eastern boundary of the Jalisco Block, which is likely to be sinistral oblique extension rather than pure extension. We constrain extension across both the Colima rift and the northeastern boundary of the Jalisco Block, the Tepic-Zacoalco rift, to ≤8 mm/year (95% confidence level), slow compared to relative rates of motion at nearby plate boundaries.

  14. Reproducción de la morena, Gymnothorax equatorialis (Pisces: Muraenidae en Jalisco y Colima, México

    Directory of Open Access Journals (Sweden)

    G Lucano-Ramírez

    2008-03-01

    Full Text Available Con el fin de analizar los aspectos reproductivos de Gymnothorax equatorialis se recolectaron mensualmente 707 organismos en las costas de Jalisco y Colima, México, de diciembre de 1995 a diciembre de 1998 y de agosto a diciembre de 1999. Las hembras fueron más numerosas y presentaron una longitud (54.7 cm mayor a la de los machos (52.1 cm. La fecundidad total mínima fue de 9 660 huevos, la máxima de 99 992 y la media fue 32 029 huevos. La talla en la que el 50 % de los individuos presentan gónadas maduras (L50 fue de 43.7 cm de longitud total en hembras y de 42.7 cm en machos. Los ovarios presentaron dos tipos de ovocitos, los pequeños inmaduros en fase cromatina nucleolo (85.1 µm y los grandes maduros en fase de vitelogénesis secundaria (701.6 µm. En el testículo maduro se observó una gran cantidad de espermatozoides en el tubo seminal y el desarrollo del testículo es de tipo lobular. Con base en las características de las gónadas y la evolución temporal del índice gonadosomático, se concluye que G. equatorialis se reproduce dos veces al año (a mediados y finales del año.Reproduction of the fish Gymnothorax equatorialis (Pisces: Muraenidae in Jalisco and Colima, Mexico. A total of 707 Gymnothorax equatorialis were collected monthly in the Jalisco and Colima coast, Mexico, from December 1995 to December 1998 and from August to November 1999, in order to determine their reproduction patterns. Females outnumbered and had longer bodies (mean length 54.7 cm than males (52.1 cm. The minimum, maximum and mean values of total fecundity were respectively 9 660, 99 992 and 32 029 eggs. The total body length at which 50 percent of individuals have ripe gonads (L50 was 43.7 cm for females and 42.7 cm TL for males. Ovaries had two main types of oocytes: small inmature in cromatin nucleolus phase (85.1 µm and large mature in secundary vitellogenesis phase (701.6 µm. High numbers of spermatozoa were observed in the seminal tubes of ripe

  15. Radiocarbon Dates from a Tomb in Mexico.

    Science.gov (United States)

    Furst, P T

    1965-02-01

    The first series of radiocarbon dates to be obtained from a deep shaft-and-chamber tomb of the type restricted in Mesoamerica to parts of Nayarit, Jalisco, and Colima in western Mexico ranges from 2230 +/- 100 years to 1710 +/- 80 years. Examination of the evidence indicates that for the present a date equivalent to A.D. 250 should be accepted for at least one phase, possibly a late phase, of the shaft tomb culture and for the hollow, polychrome figurines associated with the tombs.

  16. Aproximación al análisis de la vulnerabilidad del volcán de fuego de Colima (Jalisco, México

    Directory of Open Access Journals (Sweden)

    Luis Hernández Calvento

    2013-11-01

    Full Text Available Se aborda en este artículo una aproximación al estudio de la vulnerabilidad de la población ante las manifestaciones del Volcán de Fuego de Colima (Estado de Jalisco, México, desde un punto de vista geográfico. Para su desarrollo se plantea el uso de dos escalas: en primer lugar se estudia el entorno del Volcán, haciendo uso de Tecnologías de la Información Geográfica (T.I.G. para el análisis de sus coberturas del suelo; en segundo lugar, se toma como área piloto el núcleo de Juan Barragán, en las inmediaciones del Volcán, y se analizan las motivaciones de la población, sus disponibilidades y medios de evacuación, así como su actitud ante una hipotética manifestación volcánica.An approach to the study of vulnerability in volcanic manifestations of Volcán de Fuego de Colima (State of Jalisco, México, from a geographic point of view, is the aim of this paper. Two scales are used to broach the problem: first and foremost was necessary to analyse the land-cover arround the Volcán de Fuego de Colima, using Geographic Information Technologies (G.I.T.; at the same time, the village of Juan Barragán, neighbouring the volcano, was consider like a pilot area, and so, its population was analized with the purpose of understand their reasons of stay at the area, and their possibilities and chances faced with a hypothetic volcanic manifestation.

  17. Geomorphometric comparative analysis of Latin-American volcanoes

    Science.gov (United States)

    Camiz, Sergio; Poscolieri, Maurizio; Roverato, Matteo

    2017-07-01

    The geomorphometric classifications of three groups of volcanoes situated in the Andes Cordillera, Central America, and Mexico are performed and compared. Input data are eight local topographic gradients (i.e. elevation differences) obtained by processing each volcano raster ASTER-GDEM data. The pixels of each volcano DEM have been classified into 17 classes through a K-means clustering procedure following principal component analysis of the gradients. The spatial distribution of the classes, representing homogeneous terrain units, is shown on thematic colour maps, where colours are assigned according to mean slope and aspect class values. The interpretation of the geomorphometric classification of the volcanoes is based on the statistics of both gradients and morphometric parameters (slope, aspect and elevation). The latter were used for a comparison of the volcanoes, performed through classes' slope/aspect scatterplots and multidimensional methods. In this paper, we apply the mentioned methodology on 21 volcanoes, randomly chosen from Mexico to Patagonia, to show how it may contribute to detect geomorphological similarities and differences among them. As such, both its descriptive and graphical abilities may be a useful complement to future volcanological studies.

  18. Foci of Volcanoes

    Energy Technology Data Exchange (ETDEWEB)

    Yokoyama, I.

    1974-01-01

    One may assume a center of volcanic activities beneath the edifice of an active volcano, which is here called the focus of the volcano. Sometimes it may be a ''magma reservoir''. Its depth may differ with types of magma and change with time. In this paper, foci of volcanoes are discussed from the viewpoints of four items: (1) Geomagnetic changes related with volcanic activities; (2) Crustal deformations related with volcanic activities; (3) Magma transfer through volcanoes; and (4) Subsurface structure of calderas.

  19. Cultura política y partidos en Jalisco

    Directory of Open Access Journals (Sweden)

    Carlos Silva Moreno

    2000-01-01

    Full Text Available El presente trabajo es un intento de análisis y reflexión sobre la cultura política de uno de los componentes de todo sistema político que se precie de ser democrático (al menos formalmente: los partidos políticos. Se estudia la cultura política de los partidos políticos en Jalisco a partir del análisis de las representaciones y valores que los partidos políticos tienen sobre la democracia interna, para después contrastarlas con algunas prácticas referentes al liderazgo, dirección y formas de competencia. Debido a que las dimensiones de la democracia son muy amplias y variadas, nos centramos en dos indicadores: la forma en que se da la competencia por los cargos de dirección interna y el carácter de la dirección y el liderazgo.

  20. de La Ciénega, costa sur de Jalisco

    Directory of Open Access Journals (Sweden)

    Peter R. W. Gerritsen

    2008-01-01

    Full Text Available Hoy día la producción agroindustrial de alimentos es una actividad que está causando gran impacto tanto en los recursos naturales como en las culturas y los tejidos sociales; mientras que el modo campesino, opuesto al agroindustrial, propone una agricultura justa con base en las prácticas y experiencias campesinas generando así alternativas sustentables de producción.En este artículo se analizan cuatro estudios de caso de agricultores en el ejido de La Ciénega en la costa sur de Jalisco, los cuales se ubican en estos dos sistemas de producción. Los resultados exponen las técnicas de producción y estrategias campesinas que se desarrollan, así como la relación de los sistemas de producción ante las políticas agropecuarias. Terminamos resaltando la importancia de las prácticas y experiencias endógenas para el fortalecimiento de un desarrollo rural sustentable

  1. El nacimiento de la ingeniería en Jalisco (1827-1869)

    OpenAIRE

    DelaTorre, Federico

    1995-01-01

    La presencia de la ingeniería en la educación superior, tanto en Europa como en América, comenzó hasta finales del siglo XVIII. En México, la profesionalización de la ingeniería se remonta a la creación del Colegio de Minería en 1792; sin embargo, en el resto del país, específicamente en Jalisco, su profesionalización se dio de manera más lenta. El autor relata la evolución de la enseñanza de las ciencias en el estado de Jalisco desde la formación del Instituto de Ciencias de Jalisco en 1826....

  2. Multichannel Seismic Imaging of the Rivera Plate Subduction at the Seismogenic Jalisco Block Area (Western Mexican Margin)

    Science.gov (United States)

    Bartolome, Rafael; Górriz, Estefanía; Dañobeitia, Juanjo; Cordoba, Diego; Martí, David; Cameselle, Alejandra L.; Núñez-Cornú, Francisco; Bandy, William L.; Mortera-Gutiérrez, Carlos A.; Nuñez, Diana; Castellón, Arturo; Alonso, Jose Luis

    2016-10-01

    During the TSUJAL marine geophysical survey, conducted in February and March 2014, Spanish, Mexican and British scientists and technicians explored the western margin of Mexico, considered one of the most active seismic zones in America. This work aims to characterize the internal structure of the subduction zone of the Rivera plate beneath the North American plate in the offshore part of the Jalisco Block, to link the geodynamic and the recent tectonic deformation occurring there with the possible generation of tsunamis and earthquakes. For this purpose, it has been carried out acquisition, processing and geological interpretation of a multichannel seismic reflection profile running perpendicular to the margin. Crustal images show an oceanic domain, dominated by subduction-accretion along the lower slope of the margin with a subparallel sediment thickness of up to 1.6 s two-way travel time (approx. 2 km) in the Middle American Trench. Further, from these data the region appears to be prone to giant earthquake production. The top of the oceanic crust (intraplate reflector) is very well imaged. It is almost continuous along the profile with a gentle dip (continental crust presents a well-developed accretionary prism consisting of highly deformed sediments with prominent slumping towards the trench that may be the result of past tsunamis. Also, a bottom simulating reflector (BSR) is identified in the first half a second (twtt) of the section. High amplitude reflections at around 7-8 s twtt clearly image a discontinuous Moho, defining a very gentle dipping subduction plane.

  3. Wilsonia citrina, nuevo registro para el Estado de Jalisco, México

    OpenAIRE

    Sarahy Contreras-Martínez; Nohemi Villalpando-Navarrete; José Cruz Gómez Llamas; Brenda Yanet Cruz Rivera; L. I. Iñiguez Dávalos

    2006-01-01

    Reportamos a Wilsonia citrina (chipe encapuchado) como un nuevo registro para el Estado de Jalisco, México, capturado en la zona ribereña del Río Ayuquila, en el límite de la Reserva de la Biosfera Sierra de Manantlán, Jalisco. Este registro, único hasta el momento para la zona, es considerado como inusual, ya que la el individuo está fuera del rango de distribución invernal habitual de la especie

  4. Desarrollo regional y sustentabilidad: turismo cultural en la región sur de Jalisco

    OpenAIRE

    2013-01-01

    Este estudio tiene como objetivo determinar el potencial del turismo cultural en los municipios que conforman la región 6 del Estado de Jalisco, territorialmente delimitado en el Sur de Jalisco. Primeramente se identifica la demanda de turismo cultural para conocer el perfil del turista cultural bajo los supuestos de que los turistas especialmente motivados por la cultura tienden a viajar distancias más largas que la mayoría de los turistas. Se analizan las motivaciones y satisfacciones de lo...

  5. Los notarios de Jalisco: estructura y coyuntura en un campo profesional Jalisco's notaries: structure and junctures in a professional field

    Directory of Open Access Journals (Sweden)

    Alberto Arellano Ríos

    2011-09-01

    Full Text Available Este artículo analiza la actividad notarial mexicana a partir del caso jalisciense. El enfoque con el que se trabaja es la hibridación de la noción de campo de Pierre Bourdieu y Otto Maduro, además de explicitar algunas características del derecho mexicano. Estos planteamientos sirven para hacer sociología jurídica, al trazar los elementos que ordenan y dan lógica a la actividad notarial. Asimismo, se muestran algunos conflictos suscitados en este espacio social.This article analyzes Mexican notaries' activity focusing on the case of Jalisco. The approach used combines Pierre Bourdieus and Otto Maduro's notions of social field in addition to explaining certain characteristics of the Mexican law. This analysis serves to advance the sociology of law by tracing the features that arrange and provide a logical framework for notarial activity. It also shows some of the conflicts that have arisen in this social space.

  6. [Perceptions of adolescents Jalisco campaign on breast cancer].

    Science.gov (United States)

    Tapia-Curiel, Amparo; Nuño-Gutiérrez, Bertha Lidia; Flores-Padilla, Luis; Villaseñor-Farías, Martha; López-López, José Luis; Covarrubias-Bermúdez, María de los Ángeles

    2015-01-01

    Introducción: las campañas sobre cáncer de mama (CaMa) y las estrategias de sensibilización tienen limitada evidencia sobre su efectividad en jóvenes. La percepción referente conductual que da cuenta cómo individuos seleccionan, organizan e interpretan información. Este estudio muestra la percepción de adolescentes jaliscienses sobre campañas de CaMa. Métodos: estudio cualitativo, exploratorio, transversal, basado en las teorías construccionista y asociacionista de la percepción. Entrevista con consentimiento informado a 13 grupos focales, 129 hombres y mujeres de 12 a 19 años, escolarizados, residentes de 6 regiones de Jalisco, muestreo: técnica bola de nieve. Entrevistas transcritas y procesadas en Atlas Ti 4.1, análisis por codificación abierta. Resultados: se identificaron 10 campañas, la percepción de ellas mostró 3 procesos: 1) Selección: permeada por elementos del diseño de las campañas; 2) Organización: influenciada por significados pre estructurados sobre el color rosa, alcances y limitaciones de las campañas, y 3) Interpretación: mostró juicios referentes a visibilización del CaMa, accesibilidad al conocimiento y recursos, permeabilización de pautas y códigos culturales positivos y no cobertura a expectativas. Conclusiones: se evidenció alta sensibilización de adolescentes ante el CaMa y amplia necesidad de información y servicios. Recomendamos generar estrategias en educación formal en la adolescencia sobre salud mamaria.

  7. Ecological effects of water hyacinth (Eichhornia crassipes) on Lake Chapala, Mexico

    OpenAIRE

    Villamagna, Amy Marie

    2009-01-01

    Water hyacinth (Eichhornia crassipes) is a floating non-native plant that has been reoccurring in Lake Chapala, Jalisco, Mexico for more than 100 years. In this research, I explore the effects of water hyacinth on freshwater ecosystems worldwide and specifically on Lake Chapala. In chapter 1, I reviewed studies conducted on water hyacinth worldwide and found that the effects of water hyacinth on water quality are similar but the magnitude of effects is dependent on the percent cover and p...

  8. Socioeconomic Incentives for Migration from Mexico to the United States: Magnitude, Recent Changes, and Policy Implications.

    Science.gov (United States)

    1980-07-01

    AD- AIRS 125 DEPARTMENT OF STATE WASHINGTON OC OFFICE OF EXTERNAL--ETC FIG 5/l1 JUL AOSOCIOECONOMIC INCENTIVES FOR MIGRATION FROM MEXICO TO THE UNITE...Nogales 35. San Luis Potosi Norte 65. Puebla Sier!:a 6. Chihuahua Cd. Juarez 36. San Luis Potosi Sur 66. Puebla Area Metro. 7. Chihuahua Sierra 37...Veracruz Poza Rica 67. Puebla Centro-Sur 8. Chihuahua Noreste 38. Nayarit 68. Veracruz Centro 9. Chihuahua Guerrero 39. Jalisco Bolafios 69. Veracruz

  9. Volcanoes - Direct Download

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — This map layer includes Holocene volcanoes, which are those thought to be active in the last 10,000 years, that are within an extended area of the northern...

  10. Italian active volcanoes

    Institute of Scientific and Technical Information of China (English)

    RobertoSantacroce; RenawCristofolini; LuigiLaVolpe; GiovanniOrsi; MauroRosi

    2003-01-01

    The eruptive histories, styles of activity and general modes of operation of the main active Italian volcanoes,Etna, Vulcano, Stromboli, Vesuvio, Campi Flegrei and Ischia, are described in a short summary.

  11. Primer registro del ratón de los volcanes (Neotomodon alstoni para el estado de Hidalgo, México First record of the volcano mouse (Neotomodon alstoni from the State of Hidalgo, Mexico

    Directory of Open Access Journals (Sweden)

    Alejandro García-Becerra

    2012-06-01

    Full Text Available El ratón de los volcanes (Neotomodon alstoni se registra por primera vez en el estado de Hidalgo, México. Los ejemplares se recolectaron en diciembre de 2010, en el municipio de Almoloya, aproximadamente a 32.8 km al norte de la localidad documentada más cercana al estado de Tlaxcala, por lo que este nuevo registro se convierte en el más norteño para la distribución conocida del ratón de los volcanes.The volcano mouse (Neotomodon alstoni is firstly recorded in the State of Hidalgo. Specimens were collected in December 2010, at the municipality of Almoloya, approximately 32.8 km to the north from the nearest locality in the state of Tlaxcala. Therefore, this is the northernmost record for the range of the Mexican volcano mouse.

  12. Genesis and Characteristics of Debris Flow Ocurred in 2013 in the Atenquique Ravine, Located on the Eastern Slope of the Colima Volcanic Complex, Mexico.

    Science.gov (United States)

    Suarez-Plascencia, C.; Flores-Pena, S.; Nunez-Cornu, F. J.; Arreola-Ochoa, L. C.; Suarez-Gonzalez, B. V.

    2014-12-01

    Hurricane Manuel affected the Pacific coast of Mexico on September 15 and 16, 2013 causing heavy rainfall of about 240 mm in a 24 hour period in the area of the Volcanic Complex (VC). Heavy rainfall led to the beginning of a significant flow of mud and rocks draining from the Atenquique Creek, located on the eastern slope of the VC in a west east direction. The result of this flow was the heavy damage sustained by the local paper plant located next to the town of Atenquique in the distal part of the basin where the stream is gathered by the Tuxpan River. Damages totaling over 15 million dollars affected a large part in their recycled fibers factory, resulting in an 18-month full stoppage of the factory. This in turn caused a heavy setback of the economy located within a large region of the southern state of Jalisco. Once again on November 25, debris flow occurred only at a lower volume than the September rains, without causing any damage. Both flows contained a viscous and solid liquid flow that left deposits of silt-sandy clasts and other abundant materials of reverse gradation. The first flow reached a thickness of 4.5 m in the Tuxpan riverbed over a length of about 15 km, while the November flow left behind 1.3 m of fine materials and few clasts. The Atenquique ravine historically has had debris flow caused by heavy rainfall from hurricanes. On October 1955 debris flow claimed many deaths and heavy damage to the town and local paper mill. These flows are generated in the summer and they are associated to several factors such as weather, steep slopes, unstable volcanic strata, these elements add an important environmental history in the area, as is the use of continuous deforestation. The current land use has resulted in a positive change from forest to intensive agriculture; but having constant wildfires on the high slopes of the VC and the combination of many other factors such as changes on the soil of the slopes and movement of geological material "scarps and

  13. Spatial modeling of fires: a predictive tool for La Primavera Forest, Jalisco Mexico

    Directory of Open Access Journals (Sweden)

    Jose Luis Ibarra-Montoya

    2016-03-01

    Full Text Available The interaction of various elements of socioeconomic, political and cultural nature, influenced by landscape and climatic factors, are important aspects of fire regimes. Space models that integrate these elements and factors help to more accurately predict potential fire areas. The Protected Area Wildlife La Primavera (APFFLP is the main regulator of the climate of the Guadalajara metropolitan area, and forest fires frequently occur there. These represent a challenge for science and technology to develop methodologies that help predict forest fires. This study involves the construction of a spatial model that helps identify potential areas of fire in that area. The model integrates meteorological variables, landscape, fuels, anthropogenic and / or causality, and historical occurrences of fires during the period 1998-2012. According to the model, the variables that determine the areas of greatest fire potential are: slope (landscape, relative humidity (weather, vegetation type (causality and land use (anthropogenic. The model predicts a large area with high potential for fire, located in the central and northwest APFFLP polygon; also, there are small, isolated potential zones in the eastern part of the polygon. The information developed by this study could support the generation of local risk maps, thereby optimizing the actions of fire management and restoration of the La Primavera forest.

  14. The pronunciamiento in nineteenth-century Mexico : the case of Jalisco (1821-1852)

    OpenAIRE

    Doyle, Rosie

    2012-01-01

    The pronunciamiento was a political practice with its origins in early nineteenth-century Spain. It was a form of political petitioning usually undertaken by coalitions of military and civilian actors to make demands against regional and national governments and negotiate political change. The petitions were generally accompanied with the threat of the use of military force should the demands not be met. As such, pronunciamientos have been defined by Will Fowler as “forceful negotiations.” Th...

  15. Structure of La Primavera caldera, Jalisco, Mexico, deduced from gravity anomalies and drilling results

    Science.gov (United States)

    Yokoyama, I.; Mena, M.

    1991-07-01

    Previous studies of La Primavera caldera have mostly been based on surface geology and topography. Since 1980, many wells, exploring for geothermal energy, have reached depths of about 2 to 3 km at the center of the caldera. The results of the drillings, together with those of the gravity surveys, provide information about the subsurface structure of the caldera, and shed light on its formation. The drilling results and gravity anomalies at La Primavera caldera and San Marcos, located at about 40 km distance from the caldera, suggest that regional gravity anomalies can be interpreted in terms of depths of the granitic basements: the basement beneath La Primavera caldera is about 3 km deep and consists of roughly the same horizon as that beneath San Marcos. The drilling results within the caldera reveal that the depth of the caldera fills ranges from 0.3 to 1 km at the drilling sites. The andesite basement, about 1 km deep, remains approximately horizontal, and the granitic basement has a depth of about 3 km. The surface topographies, such as the postcaldera domes, scarcely disturb the subsurface strata. The local gravity anomalies show two lows within the caldera reflecting the configuration of caldera bottom, two funnel-shaped depressions, one of which corresponds to a vent of the Tala tuff deduced from geological observations. The mass deficiency within the caldera estimated from the gravity anomaly, satisfies the general relationship that the mass deficiency is proportional to the caldera diameter cubed. This means that caldera structure is three-dimensional: the larger the diameter, the deeper the funnel-shape. At present this argument may be limited to funnel-shaped calderas.

  16. Noise levels at critical points in the municipality of Guadalajara, Jalisco, Mexico

    Science.gov (United States)

    Figueroa, Arturo; Garcia, Jesus; Macias, Jorge; Orozco, Martha; Garcia, Javier; Delgadillo, Alan

    2002-11-01

    Studies of acoustic conditions are planning tools on which we can diagnose the problem of noise pollution in the cities. The first study on noise pollution made in the city was made by the University of Guadalajara in 1995 and updated in 1998 covering with measuring points the city center. This paper discusses the problem of noise pollution by motor vehicles at critical points and covers a total of 105 points. The study also analyzes the problem of noise pollution base on the community annoyance from which a regulation policy should derive. Results of the study show that the most critical points are located within zone 1 (center) where Leq levels within the range of 70-85 dB were found. Such levels exceed by far the international standard of 65 dB as recommended for ambient noise by the World Health Organization.

  17. Cook Inlet and Kenai Peninsula, Alaska ESI: VOLCANOS (Volcano Points)

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — This data set contains the locations of volcanos in Cook Inlet and Kenai Peninsula, Alaska. Vector points in the data set represent the location of the volcanos....

  18. Multichannel Seismic Imaging of the Rivera Plate Subduction at the Seismogenic Jalisco Block Area (Western Mexican Margin)

    Science.gov (United States)

    Bartolome, R.; Gorriz, E.; Danobeitia, J.; Barba, D. C., Sr.; Martí, D.; L Cameselle, A.; Nuñez-Cornu, F. J.; Bandy, W. L.; Mortera, C.; Nunez, D.; Alonso, J. L.; Castellon, A.; Prada, M.

    2016-12-01

    During the TSUJAL marine geophysical survey, conducted in February and March 2014 Spanish, Mexican and British scientists and technicians explored the western margin of Mexico, considered one of the most active seismic zones in America. This work aims to characterize the internal structure of the subduction zone of the Rivera plate beneath the North American plate in the offshore part of the Jalisco Block, to link the geodynamic and the recent tectonic deformation occurring there with the possible generation of tsunamis and earthquakes. For this purpose, it has been carried out acquisition, processing and geological interpretation of a multichannel seismic reflection profile running perpendicular to the margin. Crustal images show an oceanic domain, dominated by subduction-accretion along the lower slope of the margin with a subparallel sediment thickness of up to 1.6 s two way travel time (approx. 2 km) in the Middle American Trench. Further, from these data the region appears to be prone to giant earthquake production. The top of the oceanic crust (intraplate reflector) is very well imaged. It is almost continuous along the profile with a gentle dip (<10°); however, it is disrupted by normal faulting resulting from the bending of the plate during subduction. The continental crust presents a well-developed accretionary prism consisting of highly deformed sediments with prominent slumping towards the trench that may be the result of past tsunamis. Also, a Bottom Simulating Reflector (BSR) is identified in the first half a second (twtt) of the section. High amplitude reflections at around 7-8 s twtt clearly image a discontinuous Moho, defining a very gentle dipping subduction plane.

  19. Multichannel Seismic Imaging of the Rivera Plate Subduction at the Seismogenic Jalisco Block Area (Western Mexican Margin)

    Science.gov (United States)

    Bartolome, Rafael; Górriz, Estefanía; Dañobeitia, Juanjo; Cordoba, Diego; Martí, David; Cameselle, Alejandra L.; Núñez-Cornú, Francisco; Bandy, William L.; Mortera-Gutiérrez, Carlos A.; Nuñez, Diana; Castellón, Arturo; Alonso, Jose Luis

    2016-06-01

    During the TSUJAL marine geophysical survey, conducted in February and March 2014, Spanish, Mexican and British scientists and technicians explored the western margin of Mexico, considered one of the most active seismic zones in America. This work aims to characterize the internal structure of the subduction zone of the Rivera plate beneath the North American plate in the offshore part of the Jalisco Block, to link the geodynamic and the recent tectonic deformation occurring there with the possible generation of tsunamis and earthquakes. For this purpose, it has been carried out acquisition, processing and geological interpretation of a multichannel seismic reflection profile running perpendicular to the margin. Crustal images show an oceanic domain, dominated by subduction-accretion along the lower slope of the margin with a subparallel sediment thickness of up to 1.6 s two-way travel time (approx. 2 km) in the Middle American Trench. Further, from these data the region appears to be prone to giant earthquake production. The top of the oceanic crust (intraplate reflector) is very well imaged. It is almost continuous along the profile with a gentle dip (<10°); however, it is disrupted by normal faulting resulting from the bending of the plate during subduction. The continental crust presents a well-developed accretionary prism consisting of highly deformed sediments with prominent slumping towards the trench that may be the result of past tsunamis. Also, a bottom simulating reflector (BSR) is identified in the first half a second (twtt) of the section. High amplitude reflections at around 7-8 s twtt clearly image a discontinuous Moho, defining a very gentle dipping subduction plane.

  20. Volcanoes: Coming Up from Under.

    Science.gov (United States)

    Science and Children, 1980

    1980-01-01

    Provides specific information about the eruption of Mt. St. Helens in March 1980. Also discusses how volcanoes are formed and how they are monitored. Words associated with volcanoes are listed and defined. (CS)

  1. ARQUEOFAUNA DEL SITIO ARQUEOLÓGICO EL PIÑÓN, CULTURA BOLAÑOS, JALISCO, MÉXICO/Archaeofauna of the archaeological site “El Piñón”, Cultura Bolaños, Jalisco, México.

    Directory of Open Access Journals (Sweden)

    Bernardo Rodríguez Galicia

    2012-11-01

    Full Text Available La cultura Bolaños comprende diversas comunidades humanas que se asentaron en uno de los cañones que forman la Sierra Madre Occidental y se ubica, cronológicamente, entre el año 100 a.C. y llega al 1260 de nuestra era, extendiéndose desde el sur de Zacatecas hasta llegar a la desembocadura del río Grande de Santiago, en el centro de Jalisco, México. La base de su desarrollo fue el intercambio de artefactos por productos y materias primas que no existían en la región del occidente mexicano. Aquí el estudio arqueozoológico realizado con las colecciones de restos óseos obtenidos de las excavaciones efectuadas en el sitio arqueológico “El Piñón”, y su correspondiente interpretación, permitió reconstruir tanto el ambiente natural como el cultural suscitado en el pasado. La fauna identificada consistió, en un primer análisis preliminar, en poco más de 3333 especímenes óseos, entre huesos y dientes no modificados, y alterados por cocción, cremación o trabajados, los cuales correspondieron a más de 250 individuos, entre los que se pueden mencionar: conejos, liebres, ardillas, tuzas (topos, perros, pumas, linces, pecaríes, venados, guajolotes (pavos, patos, codornices y guacamayas verdes, entre otros vertebrados que son comunes al ambiente semiseco-templado que prevalece en la región de Zacatecas-Jalisco.   Abstract   The Bolaños culture is made up of many human communities that established in one of the western Sierra Madre canyons, Mexico. Their occupations are chronologically dated between 100 years BC and 1260 years AD, and extended from southern Zacatecas to the mouth of the Rio Grande of Santiago, in the center of Jalisco, Mexico. The basis of their development was the exchange of artifacts for products and raw material that didn’t exist in the western Mexican region. Here, the archaeozoological study performed with the bone remains recovered in excavations from the “El Piñon” archaeological site is

  2. Seismic Signals of the 2005 Explosive Events at Volcan de Fuego, Mexico.

    Science.gov (United States)

    Nunez-Cornu, F. J.; Vargas-Bracamontes, D. M.; Suarez-Plascencia, C.

    2005-12-01

    The current eruptive process of Volcan de Fuego (also known as Colima Volcano), started in the second semester of 1998, has presented several intermittent effusive and explosive phases. Since early 2005, a sequence of explosive events with VEI less or equal than 3 occured, the behavior of such explosive activity has been similar to that presented by the volcano in 1903. Most of the explosive events has been recorded by the seismic digital three components stations operated by the University of Guadalajara and Jalisco Civil Defense. These signals have been recorded not only by stations located on the volcanic edifice, but also by the stations BSSJ (San Sebastian del Oeste) and MCUJ (Minas del Cuale) located at 184 and 182 km in the northern coast of Jalisco, respectively. These stations recorded the seismic signal and the sonic wave. The origin times of the explosions were calculated using the sonic wave, also the sound velocity at the explosion time. Velocities of the seismic waves between the volcano and the seismic stations were also evaluated. Finally, the magnitude of the seismic signals and the energy of the sonic waves were calculated and compared with the size of the explosions reported by other authors.

  3. La colonización de la costa de Jalisco: 1953-1959

    OpenAIRE

    Carlos Tello Díaz

    2014-01-01

    El trabajo describe el periodo de 1953-1959, en el que se consolidó la coloni - zación de la costa de Jalisco, impulsada por el gobernador Agustín Yáñez con el apoyo de la entidad que creó para ese fin, la Comisión de Planeación de la Costa de Jalisco, coordinada por una persona cercana a él, José Rogelio Álva - rez. La colonización se consolidó sobre todo por medio de obras de infraestruc - tura como caminos y puertos, entre las que destaca la planeación de la ciudad de Barra de Navidad, con...

  4. Jalisco: pueblos indígenas y regiones de alto valor biológico

    Directory of Open Access Journals (Sweden)

    Darcy Víctor Tetreault

    2011-01-01

    Full Text Available En México y en otras partes de América Latina se ha observado un gran traslape entre los territorios indígenas y las regiones de alto valor biológico. En este trabajo preguntamos si se puede observar el mismo traslape en el estado de Jalisco, en el occidente de México. Para contestar esta pregunta, empezamos con un estudio sucinto de las dos principales regiones indígenas del Jalisco rural: la Sierra Huichola en el norte del estado y la Sierra de Manantlán, en el sur. Luego, se extiende el análisis al estado en su totalidad, con una investigación que pretende medir el traslape entre los territorios indígenas "desindianizados" y las regiones de alto valor biológico.

  5. Measurements of radon and chemical elements: Popocatepetl volcano; Mediciones de radon y elementos quimicos: Volcan Popocatepetl

    Energy Technology Data Exchange (ETDEWEB)

    Pena, P.; Segovia, N.; Lopez, B.; Reyes, A.V. [Instituto Nacional de Investigaciones Nucleares, A.P. 18-1027, 11801 Mexico D.F. (Mexico); Armienta, M.A.; Valdes, C.; Mena, M. [IGFUNAM, Ciudad Universitaria, 04510 Mexico D.F. (Mexico); Seidel, J.L.; Monnin, M. [UMR 5569 CNRS Hydrosciences, Montpellier (France)

    2002-07-01

    The Popocatepetl volcano is a higher risk volcano located at 60 Km from Mexico City. Radon measurements on soil in two fixed seasons located in the north slope of volcano were carried out. Moreover the radon content, major chemical elements and tracks in water samples of three springs was studied. The radon of soil was determined with solid detectors of nuclear tracks (DSTN). The radon in subterranean water was evaluated through the liquid scintillation method and it was corroborated with an Alpha Guard equipment. The major chemical elements were determined with conventional chemical methods and the track elements were measured using an Icp-Ms equipment. The radon on soil levels were lower, indicating a moderate diffusion of the gas across the slope of the volcano. The radon in subterranean water shown few changes in relation with the active scene of the volcano. The major chemical elements and tracks showed a stable behavior during the sampling period. (Author)

  6. Organizational changes at Earthquakes & Volcanoes

    Science.gov (United States)

    Gordon, David W.

    1992-01-01

    Primary responsibility for the preparation of Earthquakes & Volcanoes within the Geological Survey has shifted from the Office of Scientific Publications to the Office of Earthquakes, Volcanoes, and Engineering (OEVE). As a consequence of this reorganization, Henry Spall has stepepd down as Science Editor for Earthquakes & Volcanoes(E&V).

  7. On the morphometry of terrestrial shield volcanoes

    Science.gov (United States)

    Grosse, Pablo; Kervyn, Matthieu

    2016-04-01

    Shield volcanoes are described as low angle edifices that have convex up topographic profiles and are built primarily by the accumulation of lava flows. This generic view of shields' morphology is based on a limited number of monogenetic shields from Iceland and Mexico, and a small set of large oceanic islands (Hawaii, Galapagos). Here, the morphometry of over 150 monogenetic and polygenetic shield volcanoes, identified inthe Global Volcanism Network database, are analysed quantitatively from 90-meter resolution DEMs using the MORVOLC algorithm. An additional set of 20 volcanoes identified as stratovolcanoes but having low slopes and being dominantly built up by accumulation of lava flows are documented for comparison. Results show that there is a large variation in shield size (volumes range from 0.1 to >1000 km3), profile shape (height/basal width ratios range from 0.01 to 0.1), flank slope gradients, elongation and summit truncation. Correlation and principal component analysis of the obtained quantitative database enables to identify 4 key morphometric descriptors: size, steepness, plan shape and truncation. Using these descriptors through clustering analysis, a new classification scheme is proposed. It highlights the control of the magma feeding system - either central, along a linear structure, or spatially diffuse - on the resulting shield volcano morphology. Genetic relationships and evolutionary trends between contrasted morphological end-members can be highlighted within this new scheme. Additional findings are that the Galapagos-type morphology with a central deep caldera and steep upper flanks are characteristic of other shields. A series of large oceanic shields have slopes systematically much steeper than the low gradients (<4-8°) generally attributed to large Hawaiian-type shields. Finally, the continuum of morphologies from flat shields to steeper complex volcanic constructs considered as stratovolcanoes calls for a revision of this oversimplified

  8. Hawaii's volcanoes revealed

    Science.gov (United States)

    Eakins, Barry W.; Robinson, Joel E.; Kanamatsu, Toshiya; Naka, Jiro; Smith, John R.; Takahashi, Eiichi; Clague, David A.

    2003-01-01

    Hawaiian volcanoes typically evolve in four stages as volcanism waxes and wanes: (1) early alkalic, when volcanism originates on the deep sea floor; (2) shield, when roughly 95 percent of a volcano's volume is emplaced; (3) post-shield alkalic, when small-volume eruptions build scattered cones that thinly cap the shield-stage lavas; and (4) rejuvenated, when lavas of distinct chemistry erupt following a lengthy period of erosion and volcanic quiescence. During the early alkalic and shield stages, two or more elongate rift zones may develop as flanks of the volcano separate. Mantle-derived magma rises through a vertical conduit and is temporarily stored in a shallow summit reservoir from which magma may erupt within the summit region or be injected laterally into the rift zones. The ongoing activity at Kilauea's Pu?u ?O?o cone that began in January 1983 is one such rift-zone eruption. The rift zones commonly extend deep underwater, producing submarine eruptions of bulbous pillow lava. Once a volcano has grown above sea level, subaerial eruptions produce lava flows of jagged, clinkery ?a?a or smooth, ropy pahoehoe. If the flows reach the ocean they are rapidly quenched by seawater and shatter, producing a steep blanket of unstable volcanic sediment that mantles the upper submarine slopes. Above sea level then, the volcanoes develop the classic shield profile of gentle lava-flow slopes, whereas below sea level slopes are substantially steeper. While the volcanoes grow rapidly during the shield stage, they may also collapse catastrophically, generating giant landslides and tsunami, or fail more gradually, forming slumps. Deformation and seismicity along Kilauea's south flank indicate that slumping is occurring there today. Loading of the underlying Pacific Plate by the growing volcanic edifices causes subsidence, forming deep basins at the base of the volcanoes. Once volcanism wanes and lava flows no longer reach the ocean, the volcano continues to submerge, while

  9. Nuevos movimientos sociales en Jalisco: un estudio desde el capital social

    Directory of Open Access Journals (Sweden)

    Andrés Valdez Zepeda

    2010-01-01

    Full Text Available En el presente trabajo, se hace un análisis, a la luz de la teoría sobre capital social, del movimiento de protesta por la defensa de los recursos públicos y el Estado Laico que se realizó en el estado de Jalisco, durante los primeros meses del 2008, a raíz de la donación por parte del gobierno del estado de Jalisco de 30 millones de pesos (de 90 prometidos de recursos públicos para la construcción del Santuario de los Mártires Cristeros en el Cerro del Tesoro en Tlaquepaque, Jalisco. Se concluye, que el éxito de las movilizaciones ciudadanas, al logrársela devolución del donativo el 23 de junio del 2008, ayudó a crear una mayor confianza colectiva sobre las protestas y movilizaciones sociales, empoderando a la sociedad y, en consecuencia, coadyuvan a la creación de un mayor capital social y fortalecen el proceso de democratización de la entidad.

  10. Santa Maria Volcano, Guatemala

    Science.gov (United States)

    2002-01-01

    The eruption of Santa Maria volcano in 1902 was one of the largest eruptions of the 20th century, forming a large crater on the mountain's southwest flank. Since 1922, a lava-dome complex, Santiaguito, has been forming in the 1902 crater. Growth of the dome has produced pyroclastic flows as recently as the 2001-they can be identified in this image. The city of Quezaltenango (approximately 90,000 people in 1989) sits below the 3772 m summit. The volcano is considered dangerous because of the possibility of a dome collapse such as one that occurred in 1929, which killed about 5000 people. A second hazard results from the flow of volcanic debris into rivers south of Santiaguito, which can lead to catastrophic flooding and mud flows. More information on this volcano can be found at web sites maintained by the Smithsonian Institution, Volcano World, and Michigan Tech University. ISS004-ESC-7999 was taken 17 February 2002 from the International Space Station using a digital camera. The image is provided by the Earth Sciences and Image Analysis Laboratory at Johnson Space Center. Searching and viewing of additional images taken by astronauts and cosmonauts is available at the NASA-JSC Gateway to

  11. Anatomy of a volcano

    NARCIS (Netherlands)

    Wassink, J.

    2011-01-01

    The Icelandic volcano Eyjafjallajökull caused major disruption in European airspace last year. According to his co-author, Freysteinn Sigmundsson, the reconstruction published in Nature six months later by aerospace engineering researcher, Dr Andy Hooper, opens up a new direction in volcanology. “W

  12. Catalogue of Icelandic Volcanoes

    Science.gov (United States)

    Ilyinskaya, Evgenia; Larsen, Gudrun; Gudmundsson, Magnus T.; Vogfjord, Kristin; Pagneux, Emmanuel; Oddsson, Bjorn; Barsotti, Sara; Karlsdottir, Sigrun

    2016-04-01

    The Catalogue of Icelandic Volcanoes is a newly developed open-access web resource in English intended to serve as an official source of information about active volcanoes in Iceland and their characteristics. The Catalogue forms a part of an integrated volcanic risk assessment project in Iceland GOSVÁ (commenced in 2012), as well as being part of the effort of FUTUREVOLC (2012-2016) on establishing an Icelandic volcano supersite. Volcanic activity in Iceland occurs on volcanic systems that usually comprise a central volcano and fissure swarm. Over 30 systems have been active during the Holocene (the time since the end of the last glaciation - approximately the last 11,500 years). In the last 50 years, over 20 eruptions have occurred in Iceland displaying very varied activity in terms of eruption styles, eruptive environments, eruptive products and the distribution lava and tephra. Although basaltic eruptions are most common, the majority of eruptions are explosive, not the least due to magma-water interaction in ice-covered volcanoes. Extensive research has taken place on Icelandic volcanism, and the results reported in numerous scientific papers and other publications. In 2010, the International Civil Aviation Organisation (ICAO) funded a 3 year project to collate the current state of knowledge and create a comprehensive catalogue readily available to decision makers, stakeholders and the general public. The work on the Catalogue began in 2011, and was then further supported by the Icelandic government and the EU through the FP7 project FUTUREVOLC. The Catalogue of Icelandic Volcanoes is a collaboration of the Icelandic Meteorological Office (the state volcano observatory), the Institute of Earth Sciences at the University of Iceland, and the Civil Protection Department of the National Commissioner of the Iceland Police, with contributions from a large number of specialists in Iceland and elsewhere. The Catalogue is built up of chapters with texts and various

  13. Spatial epidemiology of bovine tuberculosis in Mexico.

    Science.gov (United States)

    Martínez, Horacio Zendejas; Suazo, Feliciano Milián; Cuador Gil, José Quintín; Bello, Gustavo Cruz; Anaya Escalera, Ana María; Márquez, Gabriel Huitrón; Casanova, Leticia García

    2007-01-01

    The purpose of this study was to use geographic information systems (GIS) and geo-statistical methods of ordinary kriging to predict the prevalence and distribution of bovine tuberculosis (TB) in Jalisco, Mexico. A random sample of 2 287 herds selected from a set of 48 766 was used for the analysis. Spatial location of herds was obtained by either a personal global positioning system (GPS), a database from the Instituto Nacional de Estadìstica Geografìa e Informàtica (INEGI) or Google Earth. Information on TB prevalence was provided by the Jalisco Commission for the Control and Eradication of Tuberculosis (COEETB). Prediction of TB was obtained using ordinary kriging in the geostatistical analyst module in ArcView8. A predicted high prevalence area of TB matching the distribution of dairy cattle was observed. This prediction was in agreement with the prevalence calculated on the total 48 766 herds. Validation was performed taking estimated values of TB prevalence at each municipality, extracted from the kriging surface and then compared with the real prevalence values using a correlation test, giving a value of 0.78, indicating that GIS and kriging are reliable tools for the estimation of TB distribution based on a random sample. This resulted in a significant savings of resources.

  14. Catalogue of Icelandic volcanoes

    Science.gov (United States)

    Ilyinskaya, Evgenia; Larsen, Gudrun; Vogfjörd, Kristin; Tumi Gudmundsson, Magnus; Jonsson, Trausti; Oddsson, Björn; Reynisson, Vidir; Barsotti, Sara; Karlsdottir, Sigrun

    2015-04-01

    Volcanic activity in Iceland occurs on volcanic systems that usually comprise a central volcano and fissure swarm. Over 30 systems have been active during the Holocene. In the last 100 years, over 30 eruptions have occurred displaying very varied activity in terms of eruption styles, eruptive environments, eruptive products and their distribution. Although basaltic eruptions are most common, the majority of eruptions are explosive, not the least due to magma-water interaction in ice-covered volcanoes. Extensive research has taken place on Icelandic volcanism, and the results reported in scientific papers and other publications. In 2010, the International Civil Aviation Organisation funded a 3 year project to collate the current state of knowledge and create a comprehensive catalogue readily available to decision makers, stakeholders and the general public. The work on the Catalogue began in 2011, and was then further supported by the Icelandic government and the EU. The Catalogue forms a part of an integrated volcanic risk assessment project in Iceland (commenced in 2012), and the EU FP7 project FUTUREVOLC (2012-2016), establishing an Icelandic volcano Supersite. The Catalogue is a collaborative effort between the Icelandic Meteorological Office (the state volcano observatory), the Institute of Earth Sciences at the University of Iceland, and the Icelandic Civil Protection, with contributions from a large number of specialists in Iceland and elsewhere. The catalogue is scheduled for opening in the first half of 2015 and once completed, it will be an official publication intended to serve as an accurate and up to date source of information about active volcanoes in Iceland and their characteristics. The Catalogue is an open web resource in English and is composed of individual chapters on each of the volcanic systems. The chapters include information on the geology and structure of the volcano; the eruption history, pattern and products; the known precursory signals

  15. The diversity of mud volcanoes in the landscape of Azerbaijan

    Science.gov (United States)

    Rashidov, Tofig

    2014-05-01

    As the natural phenomenon the mud volcanism (mud volcanoes) of Azerbaijan are known from the ancient times. The historical records describing them are since V century. More detail study of this natural phenomenon had started in the second half of XIX century. The term "mud volcano" (or "mud hill") had been given by academician H.W. Abich (1863), more exactly defining this natural phenomenon. All the previous definitions did not give such clear and capacious explanation of it. In comparison with magmatic volcanoes, globally the mud ones are restricted in distribution; they mainly locate within the Alpine-Himalayan, Pacific and Central Asian mobile belts, in more than 30 countries (Columbia, Trinidad Island, Italy, Romania, Ukraine, Georgia, Azerbaijan, Turkmenistan, Iran, Pakistan, Indonesia, Burma, Malaysia, etc.). Besides it, the zones of mud volcanoes development are corresponded to zones of marine accretionary prisms' development. For example, the South-Caspian depression, Barbados Island, Cascadia (N.America), Costa-Rica, Panama, Japan trench. Onshore it is Indonesia, Japan, and Trinidad, Taiwan. The mud volcanism with non-accretionary conditions includes the areas of Black Sea, Alboran Sea, the Gulf of Mexico (Louisiana coast), Salton Sea. But new investigations reveal more new mud volcanoes and in places which were not considered earlier as the traditional places of mud volcanoes development (e.g. West Nile Rive delta). Azerbaijan is the classic region of mud volcanoes development. From over 800 world mud volcanoes there are about 400 onshore and within the South-Caspian basin, which includes the territory of East Azerbaijan (the regions of Shemakha-Gobustan and Low-Kura River, Absheron peninsula), adjacent water area of South Caspian (Baku and Absheron archipelagoes) and SW Turkmenistan and represents an area of great downwarping with thick (over 25 km) sedimentary series. Generally, in the modern relief the mud volcanoes represent more or less large uplifts

  16. Volcano-hazard zonation for San Vicente volcano, El Salvador

    Science.gov (United States)

    Major, J.J.; Schilling, S.P.; Pullinger, C.R.; Escobar, C.D.; Howell, M.M.

    2001-01-01

    San Vicente volcano, also known as Chichontepec, is one of many volcanoes along the volcanic arc in El Salvador. This composite volcano, located about 50 kilometers east of the capital city San Salvador, has a volume of about 130 cubic kilometers, rises to an altitude of about 2180 meters, and towers above major communities such as San Vicente, Tepetitan, Guadalupe, Zacatecoluca, and Tecoluca. In addition to the larger communities that surround the volcano, several smaller communities and coffee plantations are located on or around the flanks of the volcano, and major transportation routes are located near the lowermost southern and eastern flanks of the volcano. The population density and proximity around San Vicente volcano, as well as the proximity of major transportation routes, increase the risk that even small landslides or eruptions, likely to occur again, can have serious societal consequences. The eruptive history of San Vicente volcano is not well known, and there is no definitive record of historical eruptive activity. The last significant eruption occurred more than 1700 years ago, and perhaps long before permanent human habitation of the area. Nevertheless, this volcano has a very long history of repeated, and sometimes violent, eruptions, and at least once a large section of the volcano collapsed in a massive landslide. The oldest rocks associated with a volcanic center at San Vicente are more than 2 million years old. The volcano is composed of remnants of multiple eruptive centers that have migrated roughly eastward with time. Future eruptions of this volcano will pose substantial risk to surrounding communities.

  17. Study of Seismic Clusters at Bahía de Banderas Region, Mexico

    Science.gov (United States)

    Nunez-Cornu, F. J.; Rutz-Lopez, M.; Suarez-Plascencia, C.; Trejo-Gomez, E.

    2010-12-01

    Given that the coast in the states of Jalisco and south of the state of Nayarit is located within a region of high seismic potential and also because population is increasing, perhaps motivated by the development of tourism, the Civil Defense authorities of Jalisco and the Centro de Sismología y Volcanología de Occidente-SisVOc of Universidad de Guadalajara started in the year 2000 a joint project to study the seismic risk of the region, including the seismic monitoring of Colima volcano (located between the states of Jalisco and Colima). This work focuses on the study of seismicity in the area of Bahía de Banderas and northern coast of Jalisco. To this end, we perform an analysis of available seismograms to characterize active structures, their relationship to surface morphology, and possible reach of these structures into the shallow parts of the bay. The data used in this work are waveforms recorded during the year 2003 during which the seismograph network spanned the region of study. Our method is based on the identification of seismic clusters or families using cross-correlation of waveforms, earthquake relocation and modeling of fault planes. From an initial data set of 404 earthquakes located during 2003, 96 earthquakes could be related to 17 potentially active continental structures. A modeling of fault planes was possible for 11 of these structures. Subgroups of 7 structures are aligned parallel to the Middle America Trench, a possible consequence of oblique subduction. The magnitudes of earthquakes grouped into families is less than 3.6 (Ml), corresponding to fault dimensions of hundreds of meters.

  18. Notes on the Quality of Life of Artisanal Small-Scale Fishermen along the Pacific Coast of Jalisco, México

    Directory of Open Access Journals (Sweden)

    Myrna Leticia Bravo-Olivas

    2015-05-01

    Full Text Available Sustainable fishing includes the socioeconomic status of fishers. We combined empirical quality of life (QOL and subjective lived experiences methods to explore the social sustainability of artisanal fishers in five fishery collectives along the coast of Jalisco, Mexico, where the average daily income is slightly above the poverty level. The QOL scores were also related to annual catch and incomes within each collective. A QOL index is used in this study that combines importance and achievement ratings scores; the results are indicative of an acceptable QOL for fishermen. The concept of lived experiences, incorporating aspects of life relating to Mind, Body, Work and People was explored through interviews with 12 fishers. The QOL data revealed that family and friends are important indicators related to positive QOL reported by the sample, while economic indicators were not important. Although four of the five collectives perceived that the future looks worse than the present and past, there was limited correlation between catch or income and QOL. However, while the lived experiences exercise in part supported the QOL findings, in that People was the most important dimension for almost all of the fishers interviewed, negative economic gaps related to poor catches and incomes were prevalent in the Mind and Work dimensions. The findings suggest that to understand the socioeconomic component of sustainable fisheries, both of these approaches should be considered, as they can illuminate different aspects of fishers’ lives that need to be considered during the development of fisheries’ management policies.

  19. Geology of Kilauea volcano

    Energy Technology Data Exchange (ETDEWEB)

    Moore, R.B. (Geological Survey, Denver, CO (United States). Federal Center); Trusdell, F.A. (Geological Survey, Hawaii National Park, HI (United States). Hawaiian Volcano Observatory)

    1993-08-01

    This paper summarizes studies of the structure, stratigraphy, petrology, drill holes, eruption frequency, and volcanic and seismic hazards of Kilauea volcano. All the volcano is discussed, but the focus is on its lower east rift zone (LERZ) because active exploration for geothermal energy is concentrated in that area. Kilauea probably has several separate hydrothermal-convection systems that develop in response to the dynamic behavior of the volcano and the influx of abundant meteoric water. Important features of some of these hydrothermal-convection systems are known through studies of surface geology and drill holes. Observations of eruptions during the past two centuries, detailed geologic mapping, radiocarbon dating, and paleomagnetic secular-variation studies indicate that Kilauea has erupted frequently from its summit and two radial rift zones during Quaternary time. Petrologic studies have established that Kilauea erupts only tholeiitic basalt. Extensive ash deposits at Kilauea's summit and on its LERZ record locally violent, but temporary, disruptions of local hydrothermal-convection systems during the interaction of water or steam with magma. Recent drill holes on the LERZ provide data on the temperatures of the hydrothermal-convection systems, intensity of dike intrusion, porosity and permeability, and an increasing amount of hydrothermal alteration with depth. The prehistoric and historic record of volcanic and seismic activity indicates that magma will continue to be supplied to deep and shallow reservoirs beneath Kilauea's summit and rift zones and that the volcano will be affected by eruptions and earthquakes for many thousands of years. 71 refs., 2 figs.

  20. 4D volcano gravimetry

    Science.gov (United States)

    Battaglia, Maurizio; Gottsmann, J.; Carbone, D.; Fernandez, J.

    2008-01-01

    Time-dependent gravimetric measurements can detect subsurface processes long before magma flow leads to earthquakes or other eruption precursors. The ability of gravity measurements to detect subsurface mass flow is greatly enhanced if gravity measurements are analyzed and modeled with ground-deformation data. Obtaining the maximum information from microgravity studies requires careful evaluation of the layout of network benchmarks, the gravity environmental signal, and the coupling between gravity changes and crustal deformation. When changes in the system under study are fast (hours to weeks), as in hydrothermal systems and restless volcanoes, continuous gravity observations at selected sites can help to capture many details of the dynamics of the intrusive sources. Despite the instrumental effects, mainly caused by atmospheric temperature, results from monitoring at Mt. Etna volcano show that continuous measurements are a powerful tool for monitoring and studying volcanoes.Several analytical and numerical mathematical models can beused to fit gravity and deformation data. Analytical models offer a closed-form description of the volcanic source. In principle, this allows one to readily infer the relative importance of the source parameters. In active volcanic sites such as Long Valley caldera (California, U.S.A.) and Campi Flegrei (Italy), careful use of analytical models and high-quality data sets has produced good results. However, the simplifications that make analytical models tractable might result in misleading volcanological inter-pretations, particularly when the real crust surrounding the source is far from the homogeneous/ isotropic assumption. Using numerical models allows consideration of more realistic descriptions of the sources and of the crust where they are located (e.g., vertical and lateral mechanical discontinuities, complex source geometries, and topography). Applications at Teide volcano (Tenerife) and Campi Flegrei demonstrate the

  1. Pairing the Volcano

    CERN Document Server

    Ionica, Sorina

    2011-01-01

    Isogeny volcanoes are graphs whose vertices are elliptic curves and whose edges are $\\ell$-isogenies. Algorithms allowing to travel on these graphs were developed by Kohel in his thesis (1996) and later on, by Fouquet and Morain (2001). However, up to now, no method was known, to predict, before taking a step on the volcano, the direction of this step. Hence, in Kohel's and Fouquet-Morain algorithms, many steps are taken before choosing the right direction. In particular, ascending or horizontal isogenies are usually found using a trial-and-error approach. In this paper, we propose an alternative method that efficiently finds all points $P$ of order $\\ell$ such that the subgroup generated by $P$ is the kernel of an horizontal or an ascending isogeny. In many cases, our method is faster than previous methods. This is an extended version of a paper published in the proceedings of ANTS 2010. In addition, we treat the case of 2-isogeny volcanoes and we derive from the group structure of the curve and the pairing ...

  2. Recursos naturales en la región de los valles, Jalisco.

    Directory of Open Access Journals (Sweden)

    Lilia Francisca Sánchez Moreno

    2014-12-01

    Full Text Available La Región Valles se encuentra en los límites de las provincias fisiográficas IV Sierra Madre occidental y X Eje Neovolcánico correspondiendo los sistemas de topoformas predominantes a sierras, lomeríos y mesetas según la Comisión Estatal de Agua, Jalisco (CEA, Jal. Esta Región Valles se encuentra en el centro occidente del Estado y colinda con las regiones 01 Norte, 10 Sierra Occidental, 12 Centro, 06 Sur y 07 Sierra de Amula, así como con el Estado de Nayarit. Tiene una superficie de 5,851 km2 , lo cual representa 7.3 por ciento del total Estatal, lo cual ubica a Valles como una área geográfica media, con relación al resto de las regiones del Estado de Jalisco. Esta región tiene una gran riqueza en cuanto a Recursos Naturales se refiere, ya que cuenta con la recién declarada Área Estatal de Protección Hidrológica, “Sierra del Águila” el 18 de febrero del 2010, Presa de la Vega declarada sitio Ramsar en el mismo año y tiene uno de los recursos hídricos más importantes de Jalisco, Cuenca del Río Ameca. De acuerdo con la Comisión Nacional del Agua (CONAGUA, la región Valles es una superficie donde la capacidad de los mantos acuíferos permite la extracción para cualquier tipo de uso, encontrando dos zonas geohidrológicas donde se realizan extracciones, que son la de Tequila (RH12 y la de Ameca (RH14.

  3. PAISAJES Y LUCHAS AGRARIAS EN AUTLAN Y EL GRULLO, JALISCO, MÉXICO

    Directory of Open Access Journals (Sweden)

    Hirineo Martinez Barangan

    2005-12-01

    Full Text Available Autlán y El Grullo son dos municipios ubicados en la parte suroeste de Jalisco, juntos suman un territorio de 877 Km2, con una población aproximada de 69,000 habitantes, distribuidos en 160 asentamientos humanos; aquí la mayor parte de la PEA (Población Económicamente Activa se dedica a las actividades agropecuarias, principalmente al cultivo de maíz en las tierras de temporal, hortalizas y caña de azúcar en las tierras de riego; su principal agroindustria es un ingenio azucarero.

  4. Vulnerabilidad, trabajo y salud en mujeres de la tercera edad en Ameca, Jalisco

    OpenAIRE

    Angélica Navarro Ochoa

    2017-01-01

    En esta investigación se analizan las condiciones de vida de los adultos mayores, en especial de las mujeres en Ameca, Jalisco, México. Examinar su situación, desde un enfoque de género, permite mostrar la complejidad de las relaciones que construyen para enfrentar la desigualdad, el empobrecimiento y una mayor vulnerabilidad, en comparación con los hombres. El estudio es cualitativo, aunque no se descartó el análisis cuantitativo. A partir de entrevistas a profundidad, se reconstruyen experi...

  5. Untersuchungen zur Eutergesundheit in Milchviehbeständen des Bundesstaates Jalisco, Mexiko

    OpenAIRE

    Jäger, Sybille Petra

    2006-01-01

    Die vorliegende Arbeit hatte zum Ziel, das Vorkommen subklinischer und klinischer Eutergesundheitsstörungen in 33 Milchviehherden in Jalisco, Mexiko, aufzuzeigen. Von 2937 mittels CMT untersuchten Eutervierteln zeigten 1996 (66,9%) eine positive und hiervon 1087 (37%) eine deutlich bis stark positive Reaktion. Im Abgleich mit den bakteriologischen Untersuchungen ergab sich eine Prävalenz an subklinischen Mastitiden in Höhe von 43,7%. Klinische Mastitiden ließen sich zu 2,5% nachweisen. 53,8% ...

  6. Vulnerabilidad, trabajo y salud en mujeres de la tercera edad en Ameca, Jalisco

    OpenAIRE

    Angélica Navarro Ochoa

    2017-01-01

    En esta investigación se analizan las condiciones de vida de los adultos mayores, en especial de las mujeres en Ameca, Jalisco, México. Examinar su situación, desde un enfoque de género, permite mostrar la complejidad de las relaciones que construyen para enfrentar la desigualdad, el empobrecimiento y una mayor vulnerabilidad, en comparación con los hombres. El estudio es cualitativo, aunque no se descartó el análisis cuantitativo. A partir de entrevistas a profundidad, se reconstruyen experi...

  7. Estructura organizacional de las empresas de la confección de Zapotlanejo, Jalisco

    Directory of Open Access Journals (Sweden)

    María del Rosario Cota Yáñez

    2004-01-01

    Full Text Available Sin lugar a dudas, Zapotlanejo, Jalisco representa un ejemplo ilustrativo del surgimiento y desarrollo de las iniciativas locales para llevar a cabo el desarrollo económico a partir del surgimiento y desarrollo de una actividad económica, en este caso la confección de prendas de vestir para dama. La fabricación de prendas de vestir en la localidad generó la configuración de diversas zonas de influencia expresadas principalmente en el asentamiento de microempresas, la comercialización y se ha constituido un mercado laboral.

  8. New state records and updated checklist of Aphodiini and Eupariini (Coleoptera: Scarabaeidae: Aphodiinae) from Mexico.

    Science.gov (United States)

    Minor, Pablo

    2017-03-22

    Thirty one new state records of species of Aphodiinae (Coleoptera: Scarabaeidae) from Mexico are presented, 24 species belong to Aphodiini and seven species to Eupariini into the genera Agrilinellus, Alloblackburneus, Aphotaenius, Ataenius, Blackburneus, Cephalocyclus, Coelotrachelus, Euparia, Euparixia, Geomyphilus, Gonaphodiellus, Gonaphodiopsis, Haroldiellus, Liothorax, Nialaphodius, Odontolytes, Oscarinus, Pharaphodius, and Planolinellus. New records are from the states of Aguascalientes, Baja California, Baja California Sur, Campeche, Colima, Chiapas, Estado de México, Guerrero, Hidalgo, Jalisco, Michoacán, Morelos, Nayarit, Puebla, Sonora, Tabasco, Tamaulipas, Tlaxcala, Veracruz, Zacatecas, and Distrito Federal. A checklist with updated nomenclature is included for the recorded species of Aphodiini and Eupariini from Mexico.

  9. Radon in soil concentration levels in Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Segovia, N.; Tamez, E.; Mena, M

    1991-09-15

    Radon in soil surveys in Mexico have been carried out since 1974 both for uranium prospectus and to correlate mean values of the gas emanation with local telluric behaviour. The mapping includes the northern uranium mining region, the Mexican Neo volcanic Belt, the coastal areas adjacent to the zone of subduction of the Cocos Plate under the North American Plate, some of the active volcanoes of Southern Mexico and several sedimentary valleys in Central Mexico. Recording of {sup 222} Rn alpha decay is systematically performed with LR115 track detectors. Using mean values averaged over different observation periods at fixed monitoring stations, a radon in soil map covering one third of the Mexican territory is presented. The lowest mean values have been found in areas associated with active volcanoes. The highest levels are found in uranium ore zones. Intermediate values are obtained in regions with enhanced hydrothermal activity and stations associated with intrusive rocks. (Author)

  10. CASCABELES DE COBRE EN LA CULTURA BOLAÑOS, JALISCO (Copper Bells in the Bolaños Culture, Jalisco

    Directory of Open Access Journals (Sweden)

    María Teresa Cabrero G.

    2013-10-01

    Full Text Available En el sitio de El Piñón, perteneciente a la cultura Bolaños, se recuperaron siete cascabeles pequeños de forma globular elaborados en cobre nativo y elementos traza de arsénico y plata. Como en otros sitios del occidente de México, se encontraron asociados a entierros, lo cual sugiere una relación religiosa enfocada a la muerte. Las circunstancias sociales y económicas de este hallazgo, en especial dentro de la cultura Bolaños y en el centro rector de la región como lo fue El Piñón, es probable que representaran objetos de muy alto valor que llegaron al sitio como un regalo destinado al grupo de poder, como lo atestiguan los entierros donde fueron encontrados. ENGLISH: At the site of El Piñon, belonging to the Bolaños Culture, seven small globular bells made in native copper were recovered. The bells have trace elements of arsenic and silver. Like other sites in western Mexico, these objects were associated with burials, suggesting a religious relationship focused on death. The social and economic circumstances of this find, particularly within the Bolaños Culture and given El Piñon’s location near the governing center of the region, likely represent very high value items that reached the site intended as a gift for the group in power, as evidenced by the burials where the bells were found.

  11. Italian Volcano Supersites

    Science.gov (United States)

    Puglisi, G.

    2011-12-01

    Volcanic eruptions are among the geohazards that may have a substantial economic and social impact, even at worldwide scale. Large populated regions are prone to volcanic hazards worldwide. Even local phenomena may affect largely populated areas and in some cases even megacities, producing severe economic losses. On a regional or global perspective, large volcanic eruptions may affect the climate for years with potentially huge economic impacts, but even relatively small eruptions may inject large amounts of volcanic ash in the atmosphere and severely affect air traffic over entire continents. One of main challenges of the volcanological community is to continuously monitor and understand the internal processes leading to an eruption, in order to give substantial contributions to the risk reduction. Italian active volcanoes constitute natural laboratories and ideal sites where to apply the cutting-edge volcano observation systems, implement new monitoring systems and to test and improve the most advanced models and methods for investigate the volcanic processes. That's because of the long tradition of volcanological studies resulting into long-term data sets, both in-situ and from satellite systems, among the most complete and accurate worldwide, and the large spectrum of the threatening volcanic phenomena producing high local/regional/continental risks. This contribution aims at presenting the compound monitoring systems operating on the Italian active volcanoes, the main improvements achieved during the recent studies direct toward volcanic hazard forecast and risk reductions and the guidelines for a wide coordinated project aimed at applying the ideas of the GEO Supersites Initiative at Mt. Etna and Campi Flegrei / Vesuvius areas.

  12. Ruiz Volcano: Preliminary report

    Science.gov (United States)

    Ruiz Volcano, Colombia (4.88°N, 75.32°W). All times are local (= GMT -5 hours).An explosive eruption on November 13, 1985, melted ice and snow in the summit area, generating lahars that flowed tens of kilometers down flank river valleys, killing more than 20,000 people. This is history's fourth largest single-eruption death toll, behind only Tambora in 1815 (92,000), Krakatau in 1883 (36,000), and Mount Pelée in May 1902 (28,000). The following briefly summarizes the very preliminary and inevitably conflicting information that had been received by press time.

  13. Entre aromas de incienso y pólvora : Los Altos de Jalisco, México, 1917-1940

    NARCIS (Netherlands)

    López Ulloa, José Luis

    2008-01-01

    This thesis focuses on the Mexican Revolution and on the opposition strategies followed by the opponents of the revolutionary regime who lived in the region known as Los Altos de Jalisco. In this particular region, the Catholic population, supported by the Clergy, was in constant conflict with the r

  14. Asentamientos y pueblos indios desaparecidos en Los Altos de Jalisco durante el virreinato

    Directory of Open Access Journals (Sweden)

    RAMÓN GOYAS MEJÍA

    2013-01-01

    Full Text Available En este trabajo se analiza la desaparición de pueblos indígenas duran- te el periodo colonial en la región de Los Altos de Jalisco. Diversos autores han analizado la catastrófica disminución de la población indí- gena a raíz de la llegada de los europeos al continente americano; sin embargo, al menos para el occidente de México no hay estudios deta- llados que describan la redistribución del espacio luego de dicha pér- dida de habitantes. Tal situación es aún más evidente para el caso de Los Altos de Jalisco, donde, a pesar de que se han llevado a cabo gran cantidad de estudios para entender la propiedad ranchera como forma típica de asentamiento local, los antiguos pueblos indios del área han pasado casi inadvertidos, de ahí la relevancia del presente análisis.

  15. Preliminary volcano-hazard assessment for Iliamna Volcano, Alaska

    Science.gov (United States)

    Waythomas, Christopher F.; Miller, Thomas P.

    1999-01-01

    Iliamna Volcano is a 3,053-meter-high, ice- and snow-covered stratovolcano in the southwestern Cook Inlet region about 225 kilometers southwest of Anchorage and about 100 kilometers northwest of Homer. Historical eruptions of Iliamna Volcano have not been positively documented; however, the volcano regularly emits steam and gas, and small, shallow earthquakes are often detected beneath the summit area. The most recent eruptions of the volcano occurred about 300 years ago, and possibly as recently as 90-140 years ago. Prehistoric eruptions have generated plumes of volcanic ash, pyroclastic flows, and lahars that extended to the volcano flanks and beyond. Rock avalanches from the summit area have occurred numerous times in the past. These avalanches flowed several kilometers down the flanks and at least two large avalanches transformed to cohesive lahars. The number and distribution of known volcanic ash deposits from Iliamna Volcano indicate that volcanic ash clouds from prehistoric eruptions were significantly less voluminous and probably less common relative to ash clouds generated by eruptions of other Cook Inlet volcanoes. Plumes of volcanic ash from Iliamna Volcano would be a major hazard to jet aircraft using Anchorage International Airport and other local airports, and depending on wind direction, could drift at least as far as the Kenai Peninsula and beyond. Ashfall from future eruptions could disrupt oil and gas operations and shipping activities in Cook Inlet. Because Iliamna Volcano has not erupted for several hundred years, a future eruption could involve significant amounts of ice and snow that could lead to the formation of large lahars and downstream flooding. The greatest hazards in order of importance are described below and shown on plate 1.

  16. Potential Flooding area for local Tsunami in Nayarit Region (Western Coast of Mexico).

    Science.gov (United States)

    Trejo-Gomez, E.; Ortiz, M.; Nuñez-Cornu, F. J.

    2016-12-01

    The western coast of Mexico in the region of Jalisco and Nayarit states has a complex tectonics and a high seismic activity. In the last century, four big tsunamis occurred in this area, (three of them in 1932 and one in 1995, that hit the coast of Colima, Jalisco and Nayarit. Three of these tsunamis were generated by earthquakes and one more (22 June 1932) by an underwater landslide. Currently, there is a seismic Gap on the north coast of Jalisco and southern Nayarit. Recent published papers (Urías-Espinosa et al, 2016) and the first results of TsuJal Project (Núñez- Cornú et al, 2016) suggest that subduction regime to the north of Cabo Corrientes changes and the Rivera plate subducts with a very low angle and this structure remains until Maria Madre Island at north of the Marias Islands. The hypothesis of this work is the estimation of the tsunami run up and the flooding zone after a great magnitude earthquake generated by the rupture of the hypothetical subduction structure north of Cabo Corrientes. The possible effects on the coasts of Nayarit, Islas Marias and Banderas Bay (Puerto Vallarta) are proposed in this study.

  17. Elementary analysis of data from Tianchi Volcano

    Institute of Scientific and Technical Information of China (English)

    LIU Guo-ming; ZHANG Heng-rong; KONG Qing-jun; WU Cheng-zhi; GUO Feng; ZHANG Chao-fan

    2004-01-01

    Tianchi Volcano is the largest potential erupticve volcano in China. Analyzing these data on seismic monitoring, deformation observation and water chemistry investigation gained from the Tianchi Volcano Observatory (TVO), the authors consider that the Tianchi Volcano is in going into a new flourishing time.

  18. Lava dome emplacement and destruction cyclic process at Popocatépetl volcano, Mexico: The distribution of dome volumes and its consequences on the hazard associated to the current activity

    Science.gov (United States)

    De la Cruz-Reyna, Servando; Gomez-Vazquez, Angel; Mendoza-Rosas, Ana

    2017-04-01

    Popocatépetl is a large stratovolcano surrounded by one of the most densely populated areas of the world. Its eruptive history includes a wide range of eruption types, from moderate effusive episodes to Plinian phases and even massive debris avalanches. The historical record of the last 500 years describes several episodes similar to the current one that began in 1994. The current activity is characterized by the cyclic emplacement and destruction of lava domes, with a count of at least 38 between 1996 and 2015. The previous historical episode (1919-1927) probably emplaced around 10 domes. However, 1200 yBP a major Plinian phase affected human settlements, and at least six other major explosive eruptions have been reported in the Holocene. Such eruptive history leads to question the significance of the ongoing activity in the context of a volcano capable to produce extreme eruptions. The analysis of dome parameters characterizing the current activity offers some insight into the underlying physical process sustaining the eruption, and the conditions that may signal an evolution into higher-intensity phases. Although the process is irregular and non-stationary in the time domain, the maximum volumes and thicknesses of the domes estimated from aerial images are well described by an exponential survival distribution N=No*exp(-V/Va), where No is the number of emplaced domes, Va their average volume, and N the number of domes with volumes equal or exceeding V. A variable buoyancy force caused by the variable density contrast between volatile-rich magma and country rock may offer a possible interpretation of the process. The cyclic character of magma ascent may be a consequence of a self-regulating process caused by intense outgassing of magma controlling buoyancy. The proposed scaling law may then be a consequence of the gravitational energy release of the buoyancy force governing the height and volume of the domes. A significant departure from that scaling law in

  19. Mount Rainier active cascade volcano

    Science.gov (United States)

    1994-01-01

    Mount Rainier is one of about two dozen active or recently active volcanoes in the Cascade Range, an arc of volcanoes in the northwestern United States and Canada. The volcano is located about 35 kilometers southeast of the Seattle-Tacoma metropolitan area, which has a population of more than 2.5 million. This metropolitan area is the high technology industrial center of the Pacific Northwest and one of the commercial aircraft manufacturing centers of the United States. The rivers draining the volcano empty into Puget Sound, which has two major shipping ports, and into the Columbia River, a major shipping lane and home to approximately a million people in southwestern Washington and northwestern Oregon. Mount Rainier is an active volcano. It last erupted approximately 150 years ago, and numerous large floods and debris flows have been generated on its slopes during this century. More than 100,000 people live on the extensive mudflow deposits that have filled the rivers and valleys draining the volcano during the past 10,000 years. A major volcanic eruption or debris flow could kill thousands of residents and cripple the economy of the Pacific Northwest. Despite the potential for such danger, Mount Rainier has received little study. Most of the geologic work on Mount Rainier was done more than two decades ago. Fundamental topics such as the development, history, and stability of the volcano are poorly understood.

  20. Mount Rainier active cascade volcano

    Science.gov (United States)

    Mount Rainier is one of about two dozen active or recently active volcanoes in the Cascade Range, an arc of volcanoes in the northwestern United States and Canada. The volcano is located about 35 kilometers southeast of the Seattle-Tacoma metropolitan area, which has a population of more than 2.5 million. This metropolitan area is the high technology industrial center of the Pacific Northwest and one of the commercial aircraft manufacturing centers of the United States. The rivers draining the volcano empty into Puget Sound, which has two major shipping ports, and into the Columbia River, a major shipping lane and home to approximately a million people in southwestern Washington and northwestern Oregon. Mount Rainier is an active volcano. It last erupted approximately 150 years ago, and numerous large floods and debris flows have been generated on its slopes during this century. More than 100,000 people live on the extensive mudflow deposits that have filled the rivers and valleys draining the volcano during the past 10,000 years. A major volcanic eruption or debris flow could kill thousands of residents and cripple the economy of the Pacific Northwest. Despite the potential for such danger, Mount Rainier has received little study. Most of the geologic work on Mount Rainier was done more than two decades ago. Fundamental topics such as the development, history, and stability of the volcano are poorly understood.

  1. Soufriere Hills Volcano

    Science.gov (United States)

    2002-01-01

    In this ASTER image of Soufriere Hills Volcano on Montserrat in the Caribbean, continued eruptive activity is evident by the extensive smoke and ash plume streaming towards the west-southwest. Significant eruptive activity began in 1995, forcing the authorities to evacuate more than 7,000 of the island's original population of 11,000. The primary risk now is to the northern part of the island and to the airport. Small rockfalls and pyroclastic flows (ash, rock and hot gases) are common at this time due to continued growth of the dome at the volcano's summit.This image was acquired on October 29, 2002 by the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) on NASA's Terra satellite. With its 14 spectral bands from the visible to the thermal infrared wavelength region, and its high spatial resolution of 15 to 90 meters (about 50 to 300 feet), ASTER images Earth to map and monitor the changing surface of our planet.ASTER is one of five Earth-observing instruments launched December 18, 1999, on NASA's Terra satellite. The instrument was built by Japan's Ministry of Economy, Trade and Industry. A joint U.S./Japan science team is responsible for validation and calibration of the instrument and the data products.The broad spectral coverage and high spectral resolution of ASTER will provide scientists in numerous disciplines with critical information for surface mapping, and monitoring of dynamic conditions and temporal change. Example applications are: monitoring glacial advances and retreats; monitoring potentially active volcanoes; identifying crop stress; determining cloud morphology and physical properties; wetlands evaluation; thermal pollution monitoring; coral reef degradation; surface temperature mapping of soils and geology; and measuring surface heat balance.Dr. Anne Kahle at NASA's Jet Propulsion Laboratory, Pasadena, California, is the U.S. Science team leader; Bjorn Eng of JPL is the project manager. The Terra mission is part of NASA

  2. Crust and subduction zone structure of Southwestern Mexico

    Science.gov (United States)

    Suhardja, Sandy Kurniawan; Grand, Stephen P.; Wilson, David; Guzman-Speziale, Marco; Gomez-Gonzalez, Juan Martin; Dominguez-Reyes, Tonatiuh; Ni, James

    2015-02-01

    Southwestern Mexico is a region of complex active tectonics with subduction of the young Rivera and Cocos plates to the south and widespread magmatism and rifting in the continental interior. Here we use receiver function analysis on data recorded by a 50 station temporary deployment of seismometers known as the MARS (MApping the Rivera Subduction zone) array to investigate crustal structure as well as the nature of the subduction interface near the coast. The array was deployed in the Mexican states of Jalisco, Colima, and Michoacan. Crustal thickness varies from 20 km near the coast to 42 km in the continental interior. The Rivera plate has steeper dip than the Cocos plate and is also deeper along the coast than previous estimates have shown. Inland, there is not a correlation between the thickness of the crust and topography indicating that the high topography in northern Jalisco and Michoacan is likely supported by buoyant mantle. High crustal Vp/Vs ratios (greater than 1.82) are found beneath the trenchward edge of magmatism including below the Central Jalisco Volcanic Lineament and the Michoacan-Guanajuato Volcanic Field implying a new arc is forming closer to the trench than the Trans Mexican Volcanic Belt. Elsewhere in the region, crustal Vp/Vs ratios are normal. The subducting Rivera and Cocos plates are marked by a dipping shear wave low-velocity layer. We estimate the thickness of the low-velocity layer to be 3 to 4 km with an unusually high Vp/Vs ratio of 2.0 to 2.1 and a drop in S velocity of 25%. We postulate that the low-velocity zone is the upper oceanic crust with high pore pressures. The low-velocity zone ends from 45 to 50 km depth and likely marks the basalt to eclogite transition.

  3. Characteristics of Hawaiian volcanoes

    Science.gov (United States)

    Poland, Michael P.; Takahashi, T. Jane; Landowski, Claire M.

    2014-01-01

    Founded in 1912 at the edge of the caldera of Kīlauea Volcano, HVO was the vision of Thomas A. Jaggar, Jr., a geologist from the Massachusetts Institute of Technology, whose studies of natural disasters around the world had convinced him that systematic, continuous observations of seismic and volcanic activity were needed to better understand—and potentially predict—earthquakes and volcanic eruptions. Jaggar summarized the aim of HVO by stating that “the work should be humanitarian” and have the goals of developing “prediction and methods of protecting life and property on the basis of sound scientific achievement.” These goals align well with those of the USGS, whose mission is to serve the Nation by providing reliable scientific information to describe and understand the Earth; minimize loss of life and property from natural disasters; manage natural resources; and enhance and protect our quality of life.

  4. Do Glazed Ceramic Pots in a Mexico-US Border City Still Contain Lead?

    OpenAIRE

    Valles-Medina, Ana M.; Osuna-Leal, Angel I.; Martinez-Cervantes, Maria Elena; Castillo-Fregoso, Maria Carmen; Vazquez-Erlbeck, Martha; Rodriguez-Lainz, Alfonso

    2014-01-01

    In order to identify the presence of lead in glazed ceramic pots in a Mexico-US border city, 41 clay pots were sampled. The pots were purchased in several establishments located in different geographical areas of the city. The presence of lead was determined using LeadCheck Swabs. Most (58.5%) of the pots were from the State of Jalisco and 24.4% were of unknown origin. Only 4 pots did not contain varnish and were lead-negative. Thirty-seven (81.1%) of the glazed pots were lead positive. Among...

  5. The effects of social networks on tobacco use among high-school adolescents in Mexico Efectos de redes sociales sobre el uso de tabaco en adolescentes de preparatoria en México

    OpenAIRE

    Guadalupe Ramírez-Ortiz; Ramiro Caballero-Hoyos; Guadalupe Ramírez-López; Thomas W. Valente

    2012-01-01

    OBJECTIVE: To identify the effect of centrality in social network positions on tobacco-use among high-school adolescents in Tonala, Jalisco, Mexico. MATERIALS AND METHODS: Longitudinal sociometric social network data were collected among 486 high-school adolescents in 2003 and 399 in 2004. The survey included: social network components, smoking and sociodemographic characteristics. Social network measures of centrality were calculated and multivariate logistic regression was used. RESULTS: Ev...

  6. Volcanoes in Eruption - Set 1

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — The word volcano is used to refer to the opening from which molten rock and gas issue from Earth's interior onto the surface, and also to the cone, hill, or mountain...

  7. Volcanoes in Eruption - Set 2

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — The word volcano is used to refer to the opening from which molten rock and gas issue from Earth's interior onto the surface, and also to the cone, hill, or mountain...

  8. USGS Volcano Notification Service (VNS)

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — Website provides a subscription service to receive an email when changes occur in the activity levels for monitored U.S. volcanoes and/or when information releases...

  9. Acceso y usos de internet en el occidente de México: el caso de Jalisco

    OpenAIRE

    Pablo Arredondo Ramírez

    2007-01-01

    Este trabajo representa una aproximación inicial a la presencia de la internet en una región de México. El estudio muestra la penetración de la red y los usos más recurrentes entre los internautas del estado de Jalisco. El fenómeno se analiza en el contexto de las tendencias más amplias de "consumo mediático" que imperan en la entidad. El análisis se deriva de los resultados de una encuesta, elaborada en 2006, que evalúa el peso de los medios de comunicación, los usos y las pre...

  10. Seguridad Pública, Justicia Penal y Derechos Humanos en el Estado de Jalisco (1995-2002)

    OpenAIRE

    Moloeznik, Marcos Pablo

    2003-01-01

    Este trabajo pretende llevar a cabo un análisis crítico sobre la seguridad pública, la justicia penal y los derechos humanos como política pública en el Estado de Jalisco, durante la gestión de los dos gobiernos de alternancia encabezados por el Partido Acción Nacional (PAN). En particular, se centra en los asuntos críticos que ponen en entredicho la vigencia del Estado de Derecho, así como en la identificación de tendencias que condicionan el diseño y la ejecución de la denominada política c...

  11. Reformas sin mejora: las leyes de fiscalización superior en Jalisco

    Directory of Open Access Journals (Sweden)

    Aimée Figueroa Neri

    2013-01-01

    Full Text Available En este trabajo se analiza la evolución del ordenamiento jurídico de la fiscalización superior de Jalisco, México, del año 2000 al 2009 en materia de rendición de cuentas, con el referente de la legislación federal de ese mismo periodo y el contexto nacional. El objetivo es valorar si las reformas a las normas jurídicas jaliscienses apuntaron hacia la mejora de la estructura y sistema de rendición de cuentas. También se incluyen los principales avances detectados, los retrocesos y las áreas de riesgo para el control de los recursos públicos.

  12. GLACIERS OF THE KORYAK VOLCANO

    Directory of Open Access Journals (Sweden)

    T. M. Manevich

    2012-01-01

    Full Text Available The paper presents main glaciological characteristics of present-day glaciers located on the Koryaksky volcano. The results of fieldwork (2008–2009 and high-resolution satellite image analysis let us to specify and complete information on modern glacial complex of Koryaksky volcano. Now there are seven glaciers with total area 8.36 km2. Three of them advance, two are in stationary state and one degrades. Moreover, the paper describes the new crater glacier.

  13. Alteration, slope-classified alteration, and potential lahar inundation maps of volcanoes for the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) Volcano Archive

    Science.gov (United States)

    Mars, John C.; Hubbard, Bernard E.; Pieri, David; Linick, Justin

    2015-01-01

    This study identifies areas prone to lahars from hydrothermally altered volcanic edifices on a global scale, using visible and near infrared (VNIR) and short wavelength infrared (SWIR) reflectance data from the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) and digital elevation data from the ASTER Global Digital Elevation Model (GDEM) dataset. This is the first study to create a global database of hydrothermally altered volcanoes showing quantitatively compiled alteration maps and potentially affected drainages, as well as drainage-specific maps illustrating modeled lahars and their potential inundation zones. We (1) identified and prioritized 720 volcanoes based on population density surrounding the volcanoes using the Smithsonian Institution Global Volcanism Program database (GVP) and LandScan™ digital population dataset; (2) validated ASTER hydrothermal alteration mapping techniques using Airborne Visible and Infrared Imaging Spectrometer (AVIRIS) and ASTER data for Mount Shasta, California, and Pico de Orizaba (Citlaltépetl), Mexico; (3) mapped and slope-classified hydrothermal alteration using ASTER VNIR-SWIR reflectance data on 100 of the most densely populated volcanoes; (4) delineated drainages using ASTER GDEM data that show potential flow paths of possible lahars for the 100 mapped volcanoes; (5) produced potential alteration-related lahar inundation maps using the LAHARZ GIS code for Iztaccíhuatl, Mexico, and Mount Hood and Mount Shasta in the United States that illustrate areas likely to be affected based on DEM-derived volume estimates of hydrothermally altered rocks and the ~2x uncertainty factor inherent within a statistically-based lahar model; and (6) saved all image and vector data for 3D and 2D display in Google Earth™, ArcGIS® and other graphics display programs. In addition, these data are available from the ASTER Volcano Archive (AVA) for distribution (available at http://ava.jpl.nasa.gov/recent_alteration_zones.php).

  14. [Frequency of cervical epithelial lesions reported in the Regional Laboratory of Exfoliative Cytology in Jalisco].

    Science.gov (United States)

    González-López, Sergio; Martínez-Silva, María G; Hernández-Hernández, Dulce M; Aguilar-Lemarroy, Adriana; Jave-Suárez, Luis Felipe

    2015-01-01

    Introducción: La Norma Oficial Mexicana para la prevención, tratamiento y control del Cáncer Cérvico Uterino (CaCU) indica que el Papanicolaou (Pap) es el procedimiento de elección para la detección oportuna de esta neoplasia, por lo que es de interés conocer la prevalencia de casos tamizados mediante esta técnica en la población mexicana. En la presente investigación se muestran los casos que se identificaron como sospecha para CaCU por tamizaje en el estado de Jalisco, México. Métodos: se realizó un estudio retrospectivo de las muestras que llegaron para su análisis al Laboratorio Regional de Citología Exfoliativa (LARCE) del Instituto Mexicano del Seguro Social (IMSS) en Guadalajara, Jalisco. Se consideraron todos los casos de enero de 2010 a diciembre de 2012. Resultados: se analizaron 188 095 casos, de los cuales el 5.3 % se reportaron con sospecha de displasia leve, el 0.18 % de displasia moderada y el 0.05 % de displasia grave. En cáncer microinvasor e invasor se observó una baja frecuencia (0.03 %). Conclusiones: la frecuencia de hallazgos anormales identificados por citología cervicovaginal es relativamente baja. El número de muestras inadecuadas más limitadas para valoración citológica es alto; existe una elevada proporción de mujeres que asisten por primera vez en la vida a estudio citológico en grupos de edad avanzados.

  15. Variaciones regionales de la mortalidad por homicidios en Jalisco, México

    Directory of Open Access Journals (Sweden)

    Vega-López María Guadalupe

    2003-01-01

    Full Text Available El presente estudio busca describir las variaciones regionales de la mortalidad por homicidios en el estado de Jalisco, México, en 1989-1991, 1994-1996 y 1999-2000, analizando a su vez el comportamiento de la tasa de homicidios según género y estratos de bienestar socioeconómico. A partir de la información sobre mortalidad generada por el Instituto Nacional de Estadística, Geografía y Informática, se calcularon tasas ajustadas por edad y género e índices de sobremortalidad masculina. Además, se calcularon razones de tasa y su intervalo de confianza (95%. Los resultados reflejan que la tasa de homicidios presenta una tendencia decreciente en los años 90; que existe un patrón regional de la mortalidad por homicidios, observándose las tasas más altas en regiones periféricas del estado consideradas entre las más pobres; que los municipios ubicados en el estrato de bienestar más bajo presentan un exceso de mortalidad por homicidios estadísticamente significativo, y que hay una evidente sobremortalidad masculina por esta causa. Aspectos como los antes descritos implican tareas y desafíos para la salud pública y para los organismos encargados de preservar la ley y el orden, entre ellos la necesidad de implementar políticas intersectoriales diferenciadas, que tomen en consideración las particularidades que rodean al homicidio y al crimen violento en Jalisco.

  16. Variaciones regionales de la mortalidad por homicidios en Jalisco, México

    Directory of Open Access Journals (Sweden)

    María Guadalupe Vega-López

    Full Text Available El presente estudio busca describir las variaciones regionales de la mortalidad por homicidios en el estado de Jalisco, México, en 1989-1991, 1994-1996 y 1999-2000, analizando a su vez el comportamiento de la tasa de homicidios según género y estratos de bienestar socioeconómico. A partir de la información sobre mortalidad generada por el Instituto Nacional de Estadística, Geografía y Informática, se calcularon tasas ajustadas por edad y género e índices de sobremortalidad masculina. Además, se calcularon razones de tasa y su intervalo de confianza (95%. Los resultados reflejan que la tasa de homicidios presenta una tendencia decreciente en los años 90; que existe un patrón regional de la mortalidad por homicidios, observándose las tasas más altas en regiones periféricas del estado consideradas entre las más pobres; que los municipios ubicados en el estrato de bienestar más bajo presentan un exceso de mortalidad por homicidios estadísticamente significativo, y que hay una evidente sobremortalidad masculina por esta causa. Aspectos como los antes descritos implican tareas y desafíos para la salud pública y para los organismos encargados de preservar la ley y el orden, entre ellos la necesidad de implementar políticas intersectoriales diferenciadas, que tomen en consideración las particularidades que rodean al homicidio y al crimen violento en Jalisco.

  17. 76 FR 6843 - Additional Designations, Foreign Narcotics Kingpin Designation Act

    Science.gov (United States)

    2011-02-08

    ..., Jalisco, Mexico; Ciudad Victoria, Allende Hwy, Allende, Guanajuato, Mexico; Ocampo 49, Tecalitlan, Jalisco...; Fraccionamiento Santa Isabel, Paseo San Eliseo 1695, Zapopan, Jalisco, Mexico; DOB 11 Aug 1976; alt. DOB 2...

  18. Mahukona: The missing Hawaiian volcano

    Energy Technology Data Exchange (ETDEWEB)

    Garcia, M.O.; Muenow, D.W. (Univ. of Hawaii, Honolulu (USA)); Kurz, M.D. (Woods Hole Oceanographic Institution, MA (USA))

    1990-11-01

    New bathymetric and geochemical data indicate that a seamount west of the island of Hawaii, Mahukona, is a Hawaiian shield volcano. Mahukona has weakly alkalic lavas that are geochemically distinct. They have high {sup 3}He/{sup 4}He ratios (12-21 times atmosphere), and high H{sub 2}O and Cl contents, which are indicative of the early state of development of Hawaiian volcanoes. The He and Sr isotopic values for Mahukona lavas are intermediate between those for lavas from Loihi and Manuna Loa volcanoes and may be indicative of a temporal evolution of Hawaiian magmas. Mahukona volcano became extinct at about 500 ka, perhaps before reaching sea level. It fills the previously assumed gap in the parallel chains of volcanoes forming the southern segment of the Hawaiian hotspot chain. The paired sequence of volcanoes was probably caused by the bifurcation of the Hawaiian mantle plume during its ascent, creating two primary areas of melting 30 to 40 km apart that have persisted for at least the past 4 m.y.

  19. Qualitative evidence on abortion stigma from Mexico City and five states in Mexico.

    Science.gov (United States)

    Sorhaindo, Annik M; Juárez-Ramírez, Clara; Díaz Olavarrieta, Claudia; Aldaz, Evelyn; Mejía Piñeros, María Consuelo; Garcia, Sandra

    2014-01-01

    Social manifestations of abortion stigma depend upon cultural, legal, and religious context. Abortion stigma in Mexico is under-researched. This study explored the sources, experiences, and consequences of stigma from the perspectives of women who had had an abortion, male partners, and members of the general population in different regional and legal contexts. We explored abortion stigma in Mexico City where abortion is legal in the first trimester and five states-Chihuahua, Chiapas, Jalisco, Oaxaca, and Yucatán-where abortion remains restricted. In each state, we conducted three focus groups-men ages 24-40 years (n = 36), women 25-40 years (n = 37), and young women ages 18-24 years (n = 27)-and four in-depth face-to-face interviews in total; two with women (n = 12) and two with the male partners of women who had had an abortion (n = 12). For 4 of the 12 women, this was their second abortion. This exploratory study suggests that abortion stigma was influenced by norms that placed a high value on motherhood and a conservative Catholic discourse. Some participants in this study described abortion as an "indelible mark" on a woman's identity and "divine punishment" as a consequence. Perspectives encountered in Mexico City often differed from the conservative postures in the states.

  20. Mexico Geoid Heights (MEXICO97)

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — This 2' geoid height grid for Mexico, and North-Central America, is the MEXICO97 geoid model. The computation used about one million terrestrial and marine gravity...

  1. 1985 Mexico City, Mexico Images

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — The magnitude 8.1 earthquake occurred off the Pacific coast of Mexico. The damage was concentrated in a 25 square km area of Mexico City, 350 km from the epicenter....

  2. "Mediterranean volcanoes vs. chain volcanoes in the Carpathians"

    Science.gov (United States)

    Chivarean, Radu

    2017-04-01

    Volcanoes have always represent an attractive subject for students. Europe has a small number of volcanoes and Romania has none active ones. The curricula is poor in the study of volcanoes. We want to make a parallel between the Mediterranean active volcanoes and the old extinct ones in the Oriental Carpathians. We made an comparison of the two regions in what concerns their genesis, space and time distribution, the specific relief and the impact in the landscape, consequences of their activities, etc… The most of the Mediterranean volcanoes are in Italy, in the peninsula in Napoli's area - Vezuviu, Campi Flegrei, Puzzoli, volcanic islands in Tirenian Sea - Ischia, Aeolian Islands, Sicily - Etna and Pantelleria Island. Santorini is located in Aegean Sea - Greece. Between Sicily and Tunisia there are 13 underwater volcanoes. The island called Vulcano, it has an active volcano, and it is the origin of the word. Every volcano in the world is named after this island, just north of Sicily. Vulcano is the southernmost of the 7 main Aeolian Islands, all volcanic in origin, which together form a small island arc. The cause of the volcanoes appears to be a combination of an old subduction event and tectonic fault lines. They can be considered as the origin of the science of volcanology. The volcanism of the Carpathian region is part of the extensive volcanic activity in the Mediterranean and surrounding regions. The Carpathian Neogene/Quaternary volcanic arc is naturally subdivided into six geographically distinct segments: Oas, Gutai, Tibles, Calimani, Gurghiu and Harghita. It is located roughly between the Carpathian thrust-and-fold arc to the east and the Transylvanian Basin to the west. It formed as a result of the convergence between two plate fragments, the Transylvanian micro-plate and the Eurasian plate. Volcanic edifices are typical medium-sized andesitic composite volcanoes, some of them attaining the caldera stage, complicated by submittal or peripheral domes

  3. CENTROS URBANOS, ZONAS RURALES Y ESPACIOS FLEXIBLES DE TRANSICIÓN: EL ESPACIO PRODUCIDO EN LOS ALTOS DE JALISCO

    Directory of Open Access Journals (Sweden)

    Margarita Camarena Luhrs

    2003-01-01

    Full Text Available Con el objetivo de determinar las centros urbanos y las zonas rurales que organizan el conjunto de microrregiones de Los Altos de Jalisco, en términos de subsistemas funcionales, se aplican criterios que hacen posible valorar las capacidades disponibles para el desarrollo de la población, incluyendo entre éstas, fundamentalmente, el espacio producido por las interacciones de grupos sociales entre distintos lugares. De esta manera, se busca establecer si el conjunto de localidades urbanas y rurales de Los Altos en Jalisco puede funcionar para satisfacer una serie de requisitos económicos como: inserción vía producción y empleo, e incorporación a los circuitos amplios de circulación global, y como partes de ésta la producción y distribución de productos y servicios, para garantizar su desarrollo futuro.

  4. Active Extensional Faulting at the Southern Half-Graben Belt of the Tepic-Zacoalco Rift, Western Mexico

    Science.gov (United States)

    Rosas-Elguera, J.; Ferrari, L.; Delgado, M.; Uribe, A.; Valdivia, L.; Castillo, R.

    2003-12-01

    In the past decade much debate has centered upon the kinematics and the mechanism of continental deformation in western Mexico and the motion of the Jalisco block relative to North America. Two distinct models have been proposed. The first one suggest a NW-motion of the Jalisco block that would implies a right-lateral faulting along the Tepic-Zacoalco rift (TZR). More recently others authors have documented a N-NE extensional tectonics active since late Miocene and suggested that the continental boundaries of the Jalisco block, are older structures reactivated by plate boundary forces. Studies on the crustal seismicity and the kinematics of Quaternary faults provide another constraint on the direction of motion between the Jalisco block and North America. On November 4, 5, 6, and 7, 1995, one month after the October 09, 1995, Manzanillo earthquake (Mw = 8.0), a swarm of small events was felt in the Amatlan de Ca¤as half-graben and recorded by the regional seismic network of Comision Federal de Electricidad. The coda magnitude of the largest event was Mc = 2.5-3.6 and the events were located depth ranging from 6 to 10 km. This seismic activity provoked that people from Pie de la Cuesta and Yerbabuena villages were evacuated. After that a seismic station equipped with an analogic seismograph MEQ-800 at Pie de la Cuesta was installed for three months. During the same time, October, 1995, some houses distributed along a WNW trend in Ameca city underwent severe damages, they are. The digital elevations model of the Ameca city suggest that several structures tectonics are shorter than 2 km are present in the area. The present direction of motion of the Rivera plate relative to North America plate along Middle America Trench has been estimated between N19° E to N48° E (e.g. Bandy et al., 1996). During the October 09, 1995, subduction-related earthquake (Mw = 8.0) a GPS network recorded a SW motion of the Jalisco block which could be associated to an elastic deformation

  5. ARCHAEOMAGNETIC DATING OF THE ERUPTION OF XITLE VOLCANO, BASIN OF MEXICO: IMPLICATIONS FOR THE MESOAMERICAN CENTERS OF CUICUILCO AND TEOTIHUACAN (Datación arqueomagnética de la erupción del volcán Xitle, cuenca de México: implicaciones para los centros mesoamericanos de Cuicuilco y Teotihuacan

    Directory of Open Access Journals (Sweden)

    Jaime Urrutia-Fucugauchi

    2016-06-01

    Full Text Available The Cuicuilco archaeological site in southern Basin of Mexico is covered by lava flows from the Xitle volcano. Dating the Xitle eruption and Cuicuilco abandonment has long been attempted. Contrasting results with radiocarbon dates around 2000 and 1670 yr BP have been reported, with implications for the development of the Mesoamerican centers of Cuicuilco and Teotihuacan. Here, we analyze radiocarbon dates and paleomagnetic data for the Xitle lava flows. New age estimates for the eruption are determined from correlating full vector data with the geomagnetic secular variation reference model. The revised archaeomagnetic data give ages correlating with the radiocarbon chronology, with a mean of 2086 cal yr BP and 95% confidence interval from 1995 to 2177 cal yr BP. Bootstrap analysis of the calibrated radiocarbon and archaeomagnetic dates gives mean dates and confidence intervals of 2041 and 1968–2041 cal yr BP and 2035 and 1968–2073 cal yr BP, respectively. The interval estimated of ~90 BC to ~AD 20 supports a possible link between the abandonment of Cuicuilco and the early development of Teotihuacan. ESPAÑOL: La zona arqueológica de Cuicuilco, en el sur de la cuenca de México, está cubierta por flujos de lava del volcán Xitle. Se ha intentado la datación de la erupción y el abandono del centro de Cuicuilco aplicando diferentes métodos. Se han propuesto fechas contrastantes alrededor de 2000 y 1670 años AP, con implicaciones para el desarrollo de los centros urbanos mesoamericanos Cuicuilco y Teotihuacan. A continuación, analizamos las fechas de radiocarbono y los datos paleomagnéticos para los flujos de Xitle. Se presentan nuevas estimaciones de la edad de la erupción usando datos del vector completo con el modelo geomagnético de referencia. Los datos paleomagnéticos revisados dan edades con una media de 2086 años AP e intervalo de confianza del 95 % entre 1995–2177 años AP. El análisis bootstrap de las edades radiocarb

  6. Earthquake families in the seismicity of Popocatepetl volcano

    Energy Technology Data Exchange (ETDEWEB)

    Espindola, J. M [Instituto de Geofisica, Universidad Nacional Autonoma de Mexico (Mexico); Zamora-Camacho, A [Posgrado en Ciencias de la Tierra, Universidad Nacional Autonoma de Mexico (Mexico); Jimenez, Z [Instituto de Geofisica, Universidad Nacional Autonoma de Mexico (Mexico)

    2005-04-15

    Analysis of the seismicity of Popocatepetl volcano (Central Mexico) over the period September 1 to December 31, 1995, shows the existence of three earthquake families, with correlation coefficients better than 0.5 in all components of three stations. For two families the events have similar magnitudes and occur over a relatively long period of time. This suggests that they are of the asperity type. They occur up to a depth of 4 km below sea level underneath the volcano, and may be generated by the passage of magma through the upper volcanic conduits. [Spanish] El analisis de la sismicidad asociada al volcan Popocatepetl (Meseta Central, Mexico) en el periodo 1 de septiembre a 31 de diciembre de 1995 permitio la identificacion de 3 familias de temblores. El coeficiente de correlacion encontrado para todos los miembros de las familias es mayor de 0.5 en todas las componentes de 3 estaciones cercanas a los epicentros. Los eventos de dos de las familias son de similar magnitud y ocurren dentro de un periodo relativamente largo. Esto sugiere que sean generados por la accion de una misma aspereza. Los hipocentros de los eventos se localizan bajo el edificio volcanico a profundidades de hasta 4 km bajo el nivel del mar y fueron generados probablemente por el paso de magma a traves de los conductos volcanicos superiores.

  7. Tectonic tremor and slow slip along the northwestern section of the Mexico subduction zone

    Science.gov (United States)

    Brudzinski, Michael R.; Schlanser, Kristen M.; Kelly, Nicholas J.; DeMets, Charles; Grand, Stephen P.; Márquez-Azúa, Bertha; Cabral-Cano, Enrique

    2016-11-01

    The southwestern coast of Mexico is marked by active subduction of the Rivera and Cocos plates, producing megathrust earthquakes that tend to recur every 50-100 yr. Herein, we use seismic and GPS data from this region to investigate the potential relationship between earthquakes, tectonic (non-volcanic) tremor, and transient slip along the westernmost 200 km of the Mexico subduction zone. Visual examination of seismograms and spectrograms throughout the 18-month-long MARS seismic experiment reveals clear evidence for frequent small episodes of tremor along the Rivera and Cocos subduction zones beneath the states of Jalisco, Colima, and Michoacán. Using a semi-automated process that identifies prominent energy bursts in envelope waveforms of this new data, analyst-refined relative arrival times are inverted for source locations using a 1-D velocity model. The resulting northwest-southeast trending linear band of tremor is located downdip from the rupture zones of the 1995 Mw 8.0 Colima-Jalisco and 2003 Mw 7.2 Tecoman subduction-thrust earthquakes and just below the regions of afterslip triggered by these earthquakes. Despite the close proximity between tremor and megathrust events, there is no evidence that the time since the last great earthquake influences the spatial or temporal pattern of tremor. A well-defined gap in the tremor beneath the western Colima Graben appears to mark a separation along the subducted Rivera-Cocos plate boundary. From the position time series of 19 continuous GPS sites in western Mexico, we present the first evidence that slow slip events occur on the Rivera plate subduction interface. Unlike the widely-recorded, large-amplitude, slow slip events on the nearly horizontal Cocos plate subduction interface below southern Mexico, slow slip events below western Mexico have small amplitudes and are recorded at relatively few, mostly coastal stations. The smaller slow slip beneath western Mexico may be due to the steeper dip, causing a

  8. Áreas prioritarias para colectar germoplasma de Amaranthus en México con base en la diversidad y riqueza de especies Priority areas to collect Amaranthus germplasm in Mexico based on diversity and species richness

    Directory of Open Access Journals (Sweden)

    Eduardo Espitia Rangel

    Full Text Available Esta investigación tuvo como objetivo utilizar el Sistema de Información Geográfico, para crear mapas de índices de diversidad y riqueza de especies del género Amaranthus en México, para proyectar las mejores áreas de colecta de germoplasma. La máxima riqueza de especies se encontró en el centro occidente del Estado de México incluyendo el Distrito Federal y la costa del Pacífico, entre Jalisco y Colima, así como en Sinaloa. El índice de biodiversidad de Brillouin mostró alta diversidad en la costa del Pacífico, Sinaloa, entre los estados de Jalisco y Colima, además el centro occidente de Nuevo León, la región de la Huasteca del sureste de Tamaulipas y noreste de Veracruz, así como la zona noroeste de la Península de Yucatán. Las áreas prioritarias que se proponen son: la costa central de Sinaloa, sur de la región biogeográfica de Sonora, parte centro occidente del Estado de México incluyendo el Distrito Federal, región biogeográfica del Eje Volcánico Transmexicano y la costa del pacífico centro entre los estados de Jalisco y Colima, finalmente en la región biogeográfica de la costa pacífica mexicana.This investigation had as objective to use the Geographical Information System, to create maps of indexes of diversity and wealth of species of genus Amaranthus in Mexico, to plan the best areas of germplasm collection. The maximum wealth of species was in west center of State of Mexico including Distrito Federal and the Pacific coast, between Jalisco and Colima, as well as in Sinaloa. The Brillouin index of biodiversity showed high diversity in the Pacific coast, Sinaloa, between the states of Jalisco and Colima, also the west center of Nuevo León, the region of Huasteca of southeast of Tamaulipas and northeast of Veracruz, as well as the northwest area of Yucatán Peninsula. The priority areas proposed are: the central coast of Sinaloa, south of biogeographic region of Sonora, west center section of State of Mexico

  9. Global Volcano Model

    Science.gov (United States)

    Sparks, R. S. J.; Loughlin, S. C.; Cottrell, E.; Valentine, G.; Newhall, C.; Jolly, G.; Papale, P.; Takarada, S.; Crosweller, S.; Nayembil, M.; Arora, B.; Lowndes, J.; Connor, C.; Eichelberger, J.; Nadim, F.; Smolka, A.; Michel, G.; Muir-Wood, R.; Horwell, C.

    2012-04-01

    Over 600 million people live close enough to active volcanoes to be affected when they erupt. Volcanic eruptions cause loss of life, significant economic losses and severe disruption to people's lives, as highlighted by the recent eruption of Mount Merapi in Indonesia. The eruption of Eyjafjallajökull, Iceland in 2010 illustrated the potential of even small eruptions to have major impact on the modern world through disruption of complex critical infrastructure and business. The effects in the developing world on economic growth and development can be severe. There is evidence that large eruptions can cause a change in the earth's climate for several years afterwards. Aside from meteor impact and possibly an extreme solar event, very large magnitude explosive volcanic eruptions may be the only natural hazard that could cause a global catastrophe. GVM is a growing international collaboration that aims to create a sustainable, accessible information platform on volcanic hazard and risk. We are designing and developing an integrated database system of volcanic hazards, vulnerability and exposure with internationally agreed metadata standards. GVM will establish methodologies for analysis of the data (eg vulnerability indices) to inform risk assessment, develop complementary hazards models and create relevant hazards and risk assessment tools. GVM will develop the capability to anticipate future volcanism and its consequences. NERC is funding the start-up of this initiative for three years from November 2011. GVM builds directly on the VOGRIPA project started as part of the GRIP (Global Risk Identification Programme) in 2004 under the auspices of the World Bank and UN. Major international initiatives and partners such as the Smithsonian Institution - Global Volcanism Program, State University of New York at Buffalo - VHub, Earth Observatory of Singapore - WOVOdat and many others underpin GVM.

  10. Remote Sensing of Active Volcanoes

    Science.gov (United States)

    Francis, Peter; Rothery, David

    The synoptic coverage offered by satellites provides unparalleled opportunities for monitoring active volcanoes, and opens new avenues of scientific inquiry. Thermal infrared radiation can be used to monitor levels of activity, which is useful for automated eruption detection and for studying the emplacement of lava flows. Satellite radars can observe volcanoes through clouds or at night, and provide high-resolution topographic data. In favorable conditions, radar inteferometery can be used to measure ground deformation associated with eruptive activity on a centimetric scale. Clouds from explosive eruptions present a pressing hazard to aviation; therefore, techniques are being developed to assess eruption cloud height and to discriminate between ash and meterological clouds. The multitude of sensors to be launched on future generations of space platforms promises to greatly enhance volcanological studies, but a satellite dedicated to volcanology is needed to meet requirements of aviation safety and volcano monitoring.

  11. Mount Rainier: A decade volcano

    Science.gov (United States)

    Swanson, Donald A.; Malone, Stephen D.; Samora, Barbara A.

    Mount Rainier, the highest (4392 m) volcano in the Cascade Range, towers over a population of more than 2.5 million in the Seattle-Tacoma metropolitan area, and its drainage system via the Columbia River potentially affects another 500,000 residents of southwestern Washington and northwestern Oregon (Figure 1). Mount Rainier is the most hazardous volcano in the Cascades in terms of its potential for magma-water interaction and sector collapse. Major eruptions, or debris flows even without eruption, pose significant dangers and economic threats to the region. Despite such hazard and risk, Mount Rainier has received little study; such important topics as its petrologic and geochemical character, its proximal eruptive history, its susceptibility to major edifice failure, and its development over time have been barely investigated. This situation may soon change because of Mount Rainier's recent designation as a “Decade Volcano.”

  12. Systematic radon survey over active volcanoes

    Energy Technology Data Exchange (ETDEWEB)

    Seidel, J.L.; Monnin, M.; Garcia Vindas, J.R. [Centre National de la Recherche Cientifique, Montpellier (France). Lab. GBE; Ricard, L.P.; Staudacher, T. [Observatoire Volcanologique Du Pitou de la Fournaise, La Plaine des Cafres (France)

    1999-08-01

    Data obtained since 1993 on Costa Rica volcanos are presented and radon anomalies recorded before the eruption of the Irazu volcano (December 8, 1994) are discussed. The Piton de la Fournaise volcano is inactive since mid 1992. The influence of the external parameters on the radon behaviour is studied and the type of perturbations induced on short-term measurements are individuate.

  13. GlobVolcano pre-operational services for global monitoring active volcanoes

    Science.gov (United States)

    Tampellini, Lucia; Ratti, Raffaella; Borgström, Sven; Seifert, Frank Martin; Peltier, Aline; Kaminski, Edouard; Bianchi, Marco; Branson, Wendy; Ferrucci, Fabrizio; Hirn, Barbara; van der Voet, Paul; van Geffen, J.

    2010-05-01

    The GlobVolcano project (2007-2010) is part of the Data User Element programme of the European Space Agency (ESA). The project aims at demonstrating Earth Observation (EO) based integrated services to support the Volcano Observatories and other mandate users (e.g. Civil Protection) in their monitoring activities. The information services are assessed in close cooperation with the user organizations for different types of volcano, from various geographical areas in various climatic zones. In a first phase, a complete information system has been designed, implemented and validated, involving a limited number of test areas and respective user organizations. In the currently on-going second phase, GlobVolcano is delivering pre-operational services over 15 volcanic sites located in three continents and as many user organizations are involved and cooperating with the project team. The set of GlobVolcano offered EO based information products is composed as follows: Deformation Mapping DInSAR (Differential Synthetic Aperture Radar Interferometry) has been used to study a wide range of surface displacements related to different phenomena (e.g. seismic faults, volcanoes, landslides) at a spatial resolution of less than 100 m and cm-level precision. Permanent Scatterers SAR Interferometry method (PSInSARTM) has been introduced by Politecnico of Milano as an advanced InSAR technique capable of measuring millimetre scale displacements of individual radar targets on the ground by using multi-temporal data-sets, estimating and removing the atmospheric components. Other techniques (e.g. CTM) have followed similar strategies and have shown promising results in different scenarios. Different processing approaches have been adopted, according to data availability, characteristic of the area and dynamic characteristics of the volcano. Conventional DInSAR: Colima (Mexico), Nyiragongo (Congo), Pico (Azores), Areanal (Costa Rica) PSInSARTM: Piton de la Fournaise (La Reunion Island

  14. Alaska volcanoes guidebook for teachers

    Science.gov (United States)

    Adleman, Jennifer N.

    2011-01-01

    Alaska’s volcanoes, like its abundant glaciers, charismatic wildlife, and wild expanses inspire and ignite scientific curiosity and generate an ever-growing source of questions for students in Alaska and throughout the world. Alaska is home to more than 140 volcanoes, which have been active over the last 2 million years. About 90 of these volcanoes have been active within the last 10,000 years and more than 50 of these have been active since about 1700. The volcanoes in Alaska make up well over three-quarters of volcanoes in the United States that have erupted in the last 200 years. In fact, Alaska’s volcanoes erupt so frequently that it is almost guaranteed that an Alaskan will experience a volcanic eruption in his or her lifetime, and it is likely they will experience more than one. It is hard to imagine a better place for students to explore active volcanism and to understand volcanic hazards, phenomena, and global impacts. Previously developed teachers’ guidebooks with an emphasis on the volcanoes in Hawaii Volcanoes National Park (Mattox, 1994) and Mount Rainier National Park in the Cascade Range (Driedger and others, 2005) provide place-based resources and activities for use in other volcanic regions in the United States. Along the lines of this tradition, this guidebook serves to provide locally relevant and useful resources and activities for the exploration of numerous and truly unique volcanic landscapes in Alaska. This guidebook provides supplemental teaching materials to be used by Alaskan students who will be inspired to become educated and prepared for inevitable future volcanic activity in Alaska. The lessons and activities in this guidebook are meant to supplement and enhance existing science content already being taught in grade levels 6–12. Correlations with Alaska State Science Standards and Grade Level Expectations adopted by the Alaska State Department of Education and Early Development (2006) for grades six through eleven are listed at

  15. Identity narratives by American and Canadian retirees in Mexico.

    Science.gov (United States)

    Banks, Stephen P

    2004-12-01

    Ethnographic materials, including depth interviews and a video, are analyzed to better understand how expatriate retirees living in the Lake Chapala Riviera region of Jalisco, Mexico manage personal identities in retirement. Using concepts from narrative gerontology, this study demonstrates how expatriates' stories and descriptions of Mexicans and Mexican ways of life reflexively construct storytellers' identities and provide a logic for intercultural relationships. While the host population is characterized as happy, friendly, helpful, enterprising and polite, concurrent stories by the same narrators portray them also as untrustworthy, inaccessible, lazy and incompetent. A discourse analysis that extends Cavarero's narrative identity theory argues that these contrasting conceptions of the host culture and population are deployed so as to reflexively position expatriate retirees as interpersonally attractive, culturally tolerant and pragmatically adaptable. Implications for the subjective experience of international migrant retirees are drawn from the descriptive analysis.

  16. Preliminary volcano-hazard assessment for Augustine Volcano, Alaska

    Science.gov (United States)

    Waythomas, Christopher F.; Waitt, Richard B.

    1998-01-01

    Augustine Volcano is a 1250-meter high stratovolcano in southwestern Cook Inlet about 280 kilometers southwest of Anchorage and within about 300 kilometers of more than half of the population of Alaska. Explosive eruptions have occurred six times since the early 1800s (1812, 1883, 1935, 1964-65, 1976, and 1986). The 1976 and 1986 eruptions began with an initial series of vent-clearing explosions and high vertical plumes of volcanic ash followed by pyroclastic flows, surges, and lahars on the volcano flanks. Unlike some prehistoric eruptions, a summit edifice collapse and debris avalanche did not occur in 1812, 1935, 1964-65, 1976, or 1986. However, early in the 1883 eruption, a portion of the volcano summit broke loose forming a debris avalanche that flowed to the sea. The avalanche initiated a small tsunami reported on the Kenai Peninsula at English Bay, 90 kilometers east of the volcano. Plumes of volcanic ash are a major hazard to jet aircraft using Anchorage International and other local airports. Ashfall from future eruptions could disrupt oil and gas operations and shipping activities in Cook Inlet. Eruptions similar to the historical and prehistoric eruptions are likely in Augustine's future.

  17. Establishment and development of Tabebuia rosea (Bignoniaceae) seedlings in a semideciduous tropical forest under management, Pacific coast of Mexico

    OpenAIRE

    Mora Santacruz, Antonio; Valdez Hernández, Juan Ignacio; Ángeles Pérez, Gregorio; Musálem Santiago, Miguel Ángel; Vaquera Huerta, Humberto

    2014-01-01

    We evaluated the effect of soil “scarification” and vegetation clearing treatments on the natural regeneration and initial development of Tabebuia rosea (Bertold) DC. seedlings in a moderate sized semideciduous tropical forest subjected to wood harvesting on the coast of Jalisco, Mexico. The treatments were applied under “seed” trees, and the number of germinated seedlings and their development were evaluated for nine months. Soil “scarification” promoted seed germination and initial seedling...

  18. Family physicians clinical aptitude for the nutritional management of type 2 diabetes mellitus in Guadalajara, Mexico.

    Science.gov (United States)

    Cabrera Pivaral, C E; Gutiérrez Roman, E A; Gonzalez Pérez, G; Gonzalez Reyes, F; Valadez Toscano, F; Gutiérrez Ruvalcaba, C; Rios Riebeling, C D

    2008-02-01

    There are 180,000 new Diabetes Mellitus cases in Mexico each year (1). This chronic, complex and multifactor disease requires an adequate nutritional management plan to be prescribed by family physicians. They should be trained to identify the potential difficulties in the patient's dietary schedule and orientate their management from an integrative point of view. The purpose of this study was to detect and measure family physician's clinical aptitudes for the nutritional management of Type 2 diabetes, in a representative family physician's sample from five Family Medicine Units of the Mexican Institute of Social Security in Guadalajara, Jalisco, Mexico. A structured and validated instrument was applied to 117 physicians from a total of 450 in Guadalajara, Jalisco. The main study variable was clinical aptitude for nutritional management of Type 2 diabetes. Aptitude levels were defined by an ordinal scale and related to the other variables using the median, Mann-Whitney's U test and Kruskal Wallis (KW) test. Global results showed a median of 30 points that relates to a low and a very low aptitude level for the 72% of physicians without statistical significance (KW: p>0.05) with the rest of variables. These results reflect family physician's difficulties to orientate the nutritional management of Type 2 diabetes, as well as the lack of work environments that facilitate case reflection and formative educational strategies.

  19. Age Determination of Microlepidotus brevipinnis (Steindachner, 1869 (Pisces: Haemulidae in the Coast of Jalisco, Mexico, by Reading Otoliths and Scales

    Directory of Open Access Journals (Sweden)

    E.G. Cabral-Solis

    2010-01-01

    Full Text Available This study deals with age determination of the brassy grunt Microlepidotus brevipinnis by reading otoliths (sagittae and scales which allowed the identification of 13 age groups. Growth of otoliths and scales is proportional to the growth of the fish. The time of formation of fast and slow growth bands in sagittae, as well as the time of ring formation in the scales is one year. The highest growth in length of this species takes place during the first year of life, in which the organism reaches 125.0 mm, this reduces natural mortality of the individuals by decreasing depredation. Growth in weight of this species is isometric. Sexual differentiation of the organisms is apparent after the age of two years and there were differences in the average length for each age in scales and otoliths for males and females. The age of other members of the Haemulidae family were compared with those obtained in the present study and M. brevipinnis reaches its oldest age in 13 years. It occupies a middle point (442.4 mm in relation to the total lengths of other haemulids in the Mexican Pacific coast.

  20. Regional application of a cropping systems simulation model: crop residue retention in maize production systems of Jalisco, Mexico

    NARCIS (Netherlands)

    Hartkamp, A.D.; White, J.W.; Rossing, W.A.H.; Ittersum, van M.K.; Bakker, E.J.; Rabbinge, R.

    2004-01-01

    To ensure the productivity of smallholder maize production systems in Central America, increased attention must be paid to conserving soil and water resources. Various stakeholders from national agricultural research services (NARS), networks, non-governmental organizations (NGO's) and research

  1. Regional application of a cropping systems simulation model: crop residue retention in maize production systems of Jalisco, Mexico

    NARCIS (Netherlands)

    Hartkamp, A.D.; White, J.W.; Rossing, W.A.H.; Ittersum, van M.K.; Bakker, E.J.; Rabbinge, R.

    2004-01-01

    To ensure the productivity of smallholder maize production systems in Central America, increased attention must be paid to conserving soil and water resources. Various stakeholders from national agricultural research services (NARS), networks, non-governmental organizations (NGO's) and research inst

  2. International Workshop on Educational Infrastructure: Conclusions (Summary of Proceedings, Guadalajara, Jalisco, Mexico, February 24-27, 2002).

    Science.gov (United States)

    Organisation for Economic Cooperation and Development, Paris (France). Programme on Educational Building.

    This document summarizes themes developed and conclusions from the International Workshop on Educational Infrastructure. The opening topic was "Delivering Education and Training in the Knowledge Society." It was clear to participants that educational infrastructure must go hand-in-hand with reengineering processes to adjust to the needs…

  3. Rol del apoyo social en la reincorporacion de penados: un estudio del Sistema de Postpenitenciario de Jalisco, Mexico

    National Research Council Canada - National Science Library

    Rodriguez Diaz, Francisco Javier; Herrero Olaizola, Juan; Estrada Pineda, Cristina

    2014-01-01

    Este articulo es resultado de un estudio cuantitativo que tiene como objetivo el definir el perfil de las redes de apoyo formales e informales en relacion con la reincorporacion social de los usuarios...

  4. La red de apoyo en mujeres victimas de violencia contra la pareja en el estado de Jalisco (Mexico)

    National Research Council Canada - National Science Library

    Rodriguez Diaz, Francisco Javier; Herrero Olaizola, Juan; Estrada Pineda, Cristina

    2012-01-01

    El objetivo de este trabajo es identificar las caracteristicas del apoyo social informal otorgado a la mujer maltratada por su pareja intima, quienes lo aportan, asi como el tipo de apoyo percibido por las entrevistadas...

  5. Dietary fat and antioxidant vitamin intake in patients of neurodegenerative disease in a rural region of Jalisco, Mexico

    Science.gov (United States)

    Navarro-Meza, Mónica; Gabriel-Ortiz, Genaro; Pacheco-Moisés, Fermín P.; Cruz-Ramos, José A.; López-Espinoza, Antonio

    2014-01-01

    Objective To evaluate and compare the intake of lipids and (A, E, and C) vitamins in patients with and without possible neurodegenerative diseases. Methods Twenty adults with possible Alzheimer's disease or Parkinson's disease and 41 control subjects (50–89 years old) from a rural region were studied. Dietary intake was evaluated with the analysis of macronutrients and micronutrients conducted by a food frequency questionnaire and 24 hours dietary record. Analyses were adjusted for age, sex, body mass index, and energy intake. Through interrogation and use of medical record form of health secretary we obtained information about the sociodemographic characteristics. Multivariate analysis of variance to allow for covariated adjustment was used. Results Patients had a lower energy intake, vitamin C (P = 0.016), fruits (P < 0.001), vegetables (P = 0.037), and oils and fat (P = 0.002), than the controls. Interestingly, the C vitamin intake in patients was still higher than the recommended. Patients had a higher consumption of cereals (P = 0.017), high-animal fat diet (P = 0.024), and whole milk (P < 0.001); 2.4% of the controls smoke and 5% are alcohol consumers. Eighty-five percent of patients and 78% of the controls do not have physical activity. Family history of subjects in this study indicated chronic diseases. Conclusion The subjects included in this study had a high intake of C vitamin, this is due to the consumption of fruits and vegetables. However, patients with possible Alzheimer's or Parkinson's disease had a lower intake of fruits and vegetables, which could be due to type of food to which they have access. PMID:24257159

  6. Mount Rainier, a decade volcano

    Energy Technology Data Exchange (ETDEWEB)

    Kuehn, S.C.; Hooper, P.R. (Washington State Univ., Pullman, WA (United States). Dept. of Geology); Eggers, A.E. (Univ. of Puget Sound, Tacoma, WA (United States). Dept. of Geology)

    1993-04-01

    Mount Rainier, recently designated as a decade volcano, is a 14,410 foot landmark which towers over the heavily populated southern Puget Sound Lowland of Washington State. It last erupted in the mid-1800's and is an obvious threat to this area, yet Rainier has received little detailed study. Previous work has divided Rainier into two distinct pre-glacial eruptive episodes and one post-glacial eruptive episode. In a pilot project, the authors analyzed 253 well-located samples from the volcano for 27 major and trace elements. Their objective is to test the value of chemical compositions as a tool in mapping the stratigraphy and understanding the eruptive history of the volcano which they regard as prerequisite to determining the petrogenesis and potential hazard of the volcano. The preliminary data demonstrates that variation between flows is significantly greater than intra-flow variation -- a necessary condition for stratigraphic use. Numerous flows or groups of flows can be distinguished chemically. It is also apparent from the small variation in Zr abundances and considerable variation in such ratios as Ba/Nb that fractional crystallization plays a subordinate role to some form of mixing process in the origin of the Mount Rainier lavas.

  7. Vulnerabilidad, trabajo y salud en mujeres de la tercera edad en Ameca, Jalisco

    Directory of Open Access Journals (Sweden)

    Angélica Navarro Ochoa

    2017-01-01

    Full Text Available En esta investigación se analizan las condiciones de vida de los adultos mayores, en especial de las mujeres en Ameca, Jalisco, México. Examinar su situación, desde un enfoque de género, permite mostrar la complejidad de las relaciones que construyen para enfrentar la desigualdad, el empobrecimiento y una mayor vulnerabilidad, en comparación con los hombres. El estudio es cualitativo, aunque no se descartó el análisis cuantitativo. A partir de entrevistas a profundidad, se reconstruyen experiencias de algunas adultas mayores que enfrentan desamparo, incapacidad o maltrato, y que tienen que trabajar para sobrevivir. Este trabajo contribuye a visibilizar la situación riesgosa y vulnerable de esta población, y los resultados muestran que existe una relación entre sus padecimientos y el exceso de trabajo físico que realiza. Por tanto, la condición de vida de los ancianos es vulnerable, debido a circunstancias familiares, culturales y económicas, que se reflejan en pobreza, abandono y marginalidad.

  8. RIESGO DE TRABAJO OCURRIDOS CON PERSONAL DE UN HOSPITAL EN EL ESTADO DE JALISCO 2009

    Directory of Open Access Journals (Sweden)

    Sergio A. Franco C.

    2012-01-01

    Full Text Available Se presenta un análisis sobre accidentes de trabajo y de trayecto, del año 2009 en un hospital de seguridad social en el estado de Jalisco con el objetivo de evaluar accidentabilidad, se revisaron los formatos existentes en lo referente accidentes de trabajo y de trayecto, dándose una accidentabilidad de 106 riesgos de trabajo de los cuales 66 fueron accidentes de trabajo y 49 accidentes de trayecto, en dicho periodo. En la categoría de enfermera general, los accidentados de trabajo como de trayecto, fue la de mayor accidentabilidad con un 25.50% . En lo referente al área de trabajo y vía publica se tuvo el 37.74% en la vía publica. En las actividades que se realizaban, el de conducir vehículo obtuvo el 15.09% . En el turno matutino se dio la mayor accidentabilidad con el 54.72%. El mes de octubre fue el de mayor accidentabilidad con el 15.09%. en la región anatómica el cuello como los tobillos se dio el 20.75% respectivamente. El tipo de accidente, el movimiento brusco obtuvo el 48.11%. las causas de los accidentes por falta de atención se dio el 34.91% y el agente de la lesión fue reacción corporal con el 46.23%.

  9. Isla del río Cuale (Puerto Vallarta, Jalisco, México

    Directory of Open Access Journals (Sweden)

    Edmundo Andrade Romo

    2007-01-01

    Full Text Available Los destinos turísticos internacionales experimentan cambios continuos y a velocidades generalmente mayores que en ciudades o poblados no turísticos. Esta evolución urbano-turística resulta un excelente tema de investigación para el estudio del patrimonio cultural local y sus implicaciones socioantropológicas, Puerto Vallarta, Jalisco, uno de los tres destinos turísticos internacionales más importantes de México, no ha sido la excepción. En el presente artículo se advierte como los elementos naturales se transforman en culturales y a través del análisis diacrónico se distinguen los distintos momentos que conforman y explican la identidad local, así como de la elaboración mitológica sobre el origen local. Finalmente se expone la situación actual impactada por el turismo y la percepción social sobre la Isla del río Cuale como el elemento natural-cultural más significativo en la población vallartense.

  10. Escenario sobre el Autismo en Jalisco desde la Legislación actual.

    Directory of Open Access Journals (Sweden)

    Roberto Govela Espinosa

    2014-10-01

    Full Text Available El día 30 de abril del 2015 se publicó en el Diario Oficial de la Federación, la Ley General para la Atención y Protección a Personas con el Espectro Autista. Un día antes la Cámara de Diputados declaró el 2 de abril como el Día Nacional de la Integración de las Personas con Autismo. Ambos acontecimientos son importantes avances en el apoyo al desarrollo social de las personas con autismo, pero ¿Cuáles son las condiciones socioculturales, y educativas en que viven los menores de edad que tienen la condición autista en el estado de Jalisco? Para analizar esto se realizará una investigación documental de tipo exploratorio – porque desafortunadamente no hay mucha información al respecto - en base a los datos oficiales existente

  11. Another Mexico

    Science.gov (United States)

    Romano, Carlin

    2009-01-01

    A Mexican saying holds that "Como Mexico no hay dos"--There is only one Mexico. American media these days interpret that notion with a vengeance. Story after story depicts a country overrun by out-of-control drug wars and murder, where corrupt police officers trip over beheaded victims more often than they nab perpetrators. South of the…

  12. Another Mexico

    Science.gov (United States)

    Romano, Carlin

    2009-01-01

    A Mexican saying holds that "Como Mexico no hay dos"--There is only one Mexico. American media these days interpret that notion with a vengeance. Story after story depicts a country overrun by out-of-control drug wars and murder, where corrupt police officers trip over beheaded victims more often than they nab perpetrators. South of the…

  13. Phenotypic variation of the Mexican duck (Anas platyrhynchos diazi) in Mexico

    Science.gov (United States)

    Scott, N.J.; Reynolds, R.P.

    1984-01-01

    A collection of 98 breeding Mexican Ducks (Anas platyrhynchos diazi) was made in Mexico from six areas between the United States border with Chihuahua and Lake Chapala, Jalisco, in order to study geographic variation. Plumage indices showed a relatively smooth clinal change from north to south; northern populations were most influenced by the Northern Mallard (A. platyrhynchos) phenotype. Measurements of total, wing, and culmen lengths and bill width were usually significantly larger in males at any one site, but showed no regular geographic trends. Hybridization between platyrhynchos and diazi phenotypes may or may not be increasing in the middle Rio Grande and Rio Conchos valleys; available data are insufficient to decide. A spring 1978 aerial census yielded an estimate of 55,500 diazi -like birds in Mexico. Populations of diazi appear to be as large as the available habitat allows; management should be directed towards increasing and stabilizing the nesting habitat; and the stability of the zone of intergradation should be investigated.

  14. Present-day kinematics of the Rivera plate and implications for tectonics in southwestern Mexico

    Science.gov (United States)

    Demets, Charles; Stein, Seth

    1990-01-01

    A model for the present-day motion of the Rivera plate relative to the North America, Cocos, and Pacific plates is derived using new data from the Pacific-Rivera rise and Rivera transform fault, together with new estimates of Pacific-Rivera motions. The results are combined with the closure-consistent NUVEL-1 global plate motion model of DeMets et al. (1990) to examine present-day deformation in southwestern Mexico. The analysis addresses several questions raised in previous studies of the Rivera plate. Namely, do plate motion data from the northern East Pacific rise require a distinct Rivera plate? Do plate kinematic data require the subduction of the Rivera plate along the seismically quiescent Acapulco trench? If so, what does the predicted subduction rate imply about the earthquake recurrence interval in the Jalisco region of southwestern Mexico?

  15. González Torreros, Lucia. El modelo sustentable para la actividad turística del municipio de Tequila, Jalisco

    OpenAIRE

    Marmolejo Duarte, Carlos Ramiro

    2011-01-01

    Comentaris respecte la tesi doctoral de Lucia González, dirigida pel Dr. Horacio Roldán López i codirigida pel Dr. Luis Felipe Cabrales Barajas, titulada "El model sostenible per l’activitat turística del municipi de Tequila, Jalisco". Comments regarding the doctoral thesis of Lucia Gonzalez, directed by Dr. Horacio Roldan Lopez and co-directed by Dr. Luis Felipe Cabrales Barajas, entitled "Sustainable model for tourism activity in the municipality of Tequila, Jalisco". Comentarios resp...

  16. Migration, development and remittances in rural Mexico.

    Science.gov (United States)

    Rubenstein, H

    1992-06-01

    The argument is that remittances to Mexico from migrants in the US contribute to household prosperity and lessen the balance of payments problem. The purpose of this article is to provide an overview of the incentives and constraints to development and individual economic well-being in rural Mexico. Examination is made of the financial amount of remittances, the use of remittances, the impact on development of remittances, models of migration, and migration historically. The viewpoint is that migration satisfies labor needs in developed countries to the detriment of underdeveloped countries. $2 billion a year are sent by illegal migrants from the US to Mexico. This sum is 4 times the net earning of Mexico's tourist trade. 21.1% of the Mexican population depend in part on money sent from the US. 79% of illegal migrants remitted money to relatives in Jalisco state. 70% of migrant families receive $170/month. In Guadalupe, 73% of families depended on migrant income. In Villa Guerrero, 50% of households depended on migrant income. Migrant income supported 1 out of 5 households in Mexico. Money is usually spent of household subsistence items. Sometimes money is also spent on community religious festivals, marriage ceremonies, and education of children or improved living conditions. Examples are given of money being used for investment in land and livestock. Migration affects community solidarity, and comparative ethic, and the influence on others to migrate. Employment opportunities are not expanded and cottage and community industries are threatened. Land purchases did not result in land improvements. Migration models are deficient. There is a macro/micro dichotomy. The push-and-pull system is not controllable by individual migrants. The migration remittance model is a product of unequal development and a mechanism feeding migration. Mexican migration has occurred since the 1880's; seasonal migration was encouraged. There was coercion to return to Mexico after the

  17. Organizaciones lecheras en los Altos Sur de Jalisco: un análisis de las interacciones productivas

    Directory of Open Access Journals (Sweden)

    Roberto A. Vázquez-Valencia

    2010-01-01

    Full Text Available Con una perspectiva de redes y el concepto de confianza como elementos fundamentales, este trabajo explica las interacciones entre productores lecheros de diez organizaciones en la región Altos de Jalisco. Se muestra la importancia de las relaciones de confianza en la construcción y constancia de dichas interacciones, que influyen en la consolidación de agrupaciones. Y, con base en el análisis de una encuesta a productores y entrevistas a informantes clave, se presentan las interacciones de las organizaciones con instituciones e industria regionales.

  18. Mallas de valor global en la agricultura de hortalizas en México. El caso de Sayula, Jalisco

    OpenAIRE

    Alejandro Macías Macías

    2009-01-01

    Desde mediados de la década de 1980, el cultivo de jitomate, brócoli y otras hortalizas ha cobrado importancia en Sayula, Jalisco. Este tipo de actividad se enmarca en mallas de valor en las que existen dinámicas extraterritoriales evidentes, como la provisión de insumos, factores de producción (incluida la mano de obra), comercialización y consumo, cuya labor central se ubica en otros territorios. Ahora bien, dentro de estas mallas de valor existen formas de organización diversas de la relac...

  19. CONTROL SOCIAL E INSTITUCIONES DE RECLUSIÓN. EL CASO DE LA PENITENCIARÍA DE JALISCO EN EL PORFIRIATO

    OpenAIRE

    Antonio Padilla Arroyo

    2001-01-01

    En este texto se describe y examina una de las instituciones de control social, la penitenciaría de Jalisco. Es una contribución al estudio de los regímenes penitenciarios en el siglo XIX, especialmente en el último tercio, en México. El estudio de esos sistemas se sitúa en el marco del pensamiento criminológico y del pensamiento penitenciario, así como de las prácticas institucionales, lo cual permite dilucidar los dispositivos de control que se diseñaron para ejercer la vigilancia, la obser...

  20. DISTRIBUCIÓN ESPACIAL DEL pH DE LOS SUELOS AGRÍCOLAS DE ZAPOPAN, JALISCO, MÉXICO

    OpenAIRE

    Daniel Ibarra Castillo; José Ariel Ruiz Corral; Diego Raymundo González Eguiarte; José Germán Flores Garnica

    2009-01-01

    El objetivo del presente estudio fue determinar la distribución espacial del pH del suelo en la región agrícola del municipio Zapopan, Jalisco, México. En 2004 se colectaron 105 muestras de suelo georeferenciadas del estrato 0-60 cm y se les determinó el pH. Los valores de pH se capturaron en hoja de cálculo electrónico para integrar una base de datos georeferenciada, a partir de la cual se probaron dos métodos de interpolación espacial: Kriging ordinario y Distancia Inversa Ponderada. Se det...

  1. Reproducción de la morena, Gymnothorax equatorialis (Pisces: Muraenidae) en Jalisco y Colima, México

    OpenAIRE

    G. Lucano-Ramírez; S. Ruiz-Ramírez; J.A. Rojo-Vázquez; G. González-Sansón

    2006-01-01

    Con el fin de analizar los aspectos reproductivos de Gymnothorax equatorialis se recolectaron mensualmente 707 organismos en las costas de Jalisco y Colima, México, de diciembre de 1995 a diciembre de 1998 y de agosto a diciembre de 1999. Las hembras fueron más numerosas y presentaron una longitud (54.7 cm) mayor a la de los machos (52.1 cm). La fecundidad total mínima fue de 9 660 huevos, la máxima de 99 992 y la media fue 32 029 huevos. La talla en la que el 50 % de los individuos presentan...

  2. Glucemia de ayuno en un grupo de pacientes diabéticos de Jalisco, México

    OpenAIRE

    R. Bustos-Saldaña; G. López-Hernández; A. Bustos-Mora; R. Bustos-Mora; F. Pérez-Larios; M. Salgado-Rodríguez

    2005-01-01

    Objetivo: Identificar los cambios diarios que tienen los resultados de glucemias de ayuno de los pacientes diabéticos. Diseño: Estudio descriptivo y transversal. Material y Métodos: 4,515 resultados de glucemia de pacientes diabéticos detectados durante el año 2003 que fueron atendidos en el Servicio de Medicina Familiar del Hospital General de Zona con Medicina Familiar No. 9 del Instituto Mexicano del Seguro Social en Ciudad Guzmán, Jalisco. Resultados: 2,796 pacientes (66%) fueron mujeres ...

  3. Aleutian Islands Coastal Resources Inventory and Environmental Sensitivity Maps: VOLCANOS (Volcano Points)

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — This data set contains point locations of active volcanoes as compiled by Motyka et al., 1993. Eighty-nine volcanoes with eruptive phases in the Quaternary are...

  4. Tsujal Marine Survey: Crustal Characterization of the Rivera Plate-Jalisco Block Boundary and its Implications for Seismic and Tsunami Hazard Assessment

    Science.gov (United States)

    Bartolome, R.; Danobeitia, J.; Barba, D. C., Sr.; Nunez-Cornu, F. J.; Cameselle, A. L.; Estrada, F.; Prada, M.; Bandy, W. L.

    2014-12-01

    During the spring of 2014, a team of Spanish and Mexican scientists explored the western margin of Mexico in the frame of the TSUJAL project. The two main objectives were to characterize the nature and structure of the lithosphere and to identify potential sources triggering earthquakes and tsunamis at the contact between Rivera plate-Jalisco block with the North American Plate. With these purposes a set of marine geophysical data were acquired aboard the RRS James Cook. This work is focus in the southern part of the TSUJAL survey, where we obtain seismic images from the oceanic domain up to the continental shelf. Thus, more than 800 km of MCS data, divided in 7 profiles, have been acquired with a 6km long streamer and using an air-gun sources ranging from 5800 c.i. to 3540 c.i. Furthermore, a wide-angle seismic profile of 190 km length was recorded in 16 OBS deployed perpendicular to the coast of Manzanillo. Gravity and magnetic, multibeam bathymetry and sub-bottom profiler data were recorded simultaneously with seismic data in the offshore area. Preliminary stacked MCS seismic sections reveal the crustal structure in the different domains of the Mexican margin. The contact between the Rivera and NA Plates is observed as a strong reflection at 6 s two way travel time (TWTT), in a parallel offshore profile (TS01), south of Manzanillo. This contact is also identified in a perpendicular profile, TS02, along a section of more than 100 km in length crossing the Rivera transform zone, and the plate boundary between Cocos and Rivera Plates. Northwards, offshore Pto. Vallarta, the MCS data reveals high amplitude reflections at around 7-8.5 s TWTT, roughly 2.5-3.5 s TWTT below the seafloor, that conspicuously define the subduction plane (TS06b). These strong reflections which we interpret as the Moho discontinuity define the starting bending of subduction of Rivera Plate. Another clear pattern observed within the first second of the MCS data shows evidences of a bottom

  5. Volcano Monitoring Using Google Earth

    Science.gov (United States)

    Bailey, J. E.; Dehn, J.; Webley, P.; Skoog, R.

    2006-12-01

    At the Alaska Volcano Observatory (AVO), Google Earth is being used as a visualization tool for operational satellite monitoring of the region's volcanoes. Through the abilities of the Keyhole Markup Language (KML) utilized by Google Earth, different datasets have been integrated into this virtual globe browser. Examples include the ability to browse thermal satellite image overlays with dynamic control, to look for signs of volcanic activity. Webcams can also be viewed interactively through the Google Earth interface to confirm current activity. Other applications include monitoring the location and status of instrumentation; near real-time plotting of earthquake hypocenters; mapping of new volcanic deposits; and animated models of ash plumes within Google Earth, created by a combination of ash dispersion modeling and 3D visualization packages. The globe also provides an ideal interface for displaying near real-time information on detected thermal anomalies or "hotspot"; pixels in satellite images with elevated brightness temperatures relative to the background temperature. The Geophysical Institute at the University of Alaska collects AVHRR (Advanced Very High Resolution Radiometer) and MODIS (Moderate Resolution Imaging Spectroradiometer) through its own receiving station. The automated processing that follows includes application of algorithms that search for hotspots close to volcano location, flagging those that meet certain criteria. Further automated routines generate folders of KML placemarkers, which are linked to Google Earth through the network link function. Downloadable KML files have been created to provide links to various data products for different volcanoes and past eruptions, and to demonstrate examples of the monitoring tools developed. These KML files will be made accessible through a new website that will become publicly available in December 2006.

  6. Modeling eruptions of Karymsky volcano

    OpenAIRE

    Ozerov, A.; Ispolatov, I.; Lees, J.

    2001-01-01

    A model is proposed to explain temporal patterns of activity in a class of periodically exploding Strombolian-type volcanos. These patterns include major events (explosions) which follow each other every 10-30 minutes and subsequent tremor with a typical period of 1 second. This two-periodic activity is thought to be caused by two distinct mechanisms of accumulation of the elastic energy in the moving magma column: compressibility of the magma in the lower conduit and viscoelastic response of...

  7. The Seismic Alert System of Mexico (SASMEX): Performance and Evolution

    Science.gov (United States)

    Espinosa Aranda, J.

    2013-05-01

    Originally the Seismic Alert System of Mexico (SASMEX) was proposed to integrate the Seismic Alert System of Mexico City (SAS), operating since 1991, with the Seismic Alert System of Oaxaca City (SASO), in services since 2003. And today, after the intense big earthquake activity observed in our world during 2010 and 2011, local governments of Mexico City, Oaxaca Estate, and the Mexican Ministry of the Interior have been promoting the expansion of this technological EEW development. Until 2012 SASMEX better coverage includes 48 new field seismic sensors (FS) deployed over the seismic region of Jalisco, Colima, Michoacan and Puebla, with someone enhancements over Guerrero and Oaxaca, to reach 97 FS. During 2013, 35 new FS has been proposed to SASMEX enhancements covering the Chiapas and Veracruz seismic regions. The SASMEX, with the support of the Mexico Valley Broadcasters Association (ARVM) since 1993, automatically issue Public and Preventive earthquake early warning signals in the Cities of Mexico, Toluca, Acapulco, Chilpancingo, and Oaxaca. The seismic warning range in each case is seated in accordance with local Civil Protection Authorities: Public Alert, if they expect strong earthquake effects, and Preventive Alert one, the effect could be moderated. Now the SASMEX warning time opportunity could be different to the 60 sec. average typically generated when SAS warned earthquake effects coming from Guerrero to Mexico City valley. Mexican EEW issued today reach: 16 Public and 62 Preventive Alert in Mexico City; 25 Public and 19 Preventive Alerts in Oaxaca City; also 14 Public and 4 Preventive Alerts in Acapulco; 14 Public and 5 Preventive Alerts in Chilpancingo. The earthquakes events registered by SASMEX FS until now reach 3448. With the support of private and Federal telecommunications infrastructure like, TELMEX, Federal Electric Commission, and the Mexican Security Ministry, it was developed a redundant communication system with pads to link the different

  8. Acuacultura rural en la Costa Sur de Jalisco: caso de estudio

    Directory of Open Access Journals (Sweden)

    M. García-Ulloa

    2010-01-01

    Full Text Available La acuicultura ha contribuido desde siempre a la mitigación de la pobreza en áreas rurales cuya subsistencia depende parcial o totalmente de actividades acuícolas, ya sea de extracción o producción. En base a dicho fundamento, se realizó un ciclo de cultivo de tilapia en jaulas en el embalse concesionado a la comunidad de Las Guásimas, Jalisco, para evaluar su potencial de producción y para establecer una alternativa laboral afín a la pesca tradicional que ahí se practica, bajo la supervisión in situ, del personal de un centro de investigación. Bajo condiciones de baja salinidad en el agua, se observó un adecuado crecimiento promedio de los animales (1.2 g/d sin presentar enfermedades. Los peces alcanzaron la talla mínima de venta (> 150 g en 81 días de cultivo, logrando un 90% de supervivencia final. Despuésde la cosecha y venta de todos los peces cultivados, se discuten aspectos de producción (densidad, costos, uso de organismos monosexo, etcétera, sociales (generación de empleos, inclusión de adolescentes y mujeres en el proceso de producción, entre otros y se identifican problemáticas operativas de diversa índole (limitantes del lugar, formalización en la participación de los miembros de la cooperativa, etcétera, ubicando el cultivo de tilapia en jaulas como una alternativa real y patente con necesidad de apoyo inmediato por parte de programas privados o gubernamentales integrales para mejorar la calidad de vida de comunidades rurales.

  9. Earthquakes - Volcanoes (Causes and Forecast)

    Science.gov (United States)

    Tsiapas, E.

    2009-04-01

    EARTHQUAKES - VOLCANOES (CAUSES AND FORECAST) ELIAS TSIAPAS RESEARCHER NEA STYRA, EVIA,GREECE TEL.0302224041057 tsiapas@hol.gr The earthquakes are caused by large quantities of liquids (e.g. H2O, H2S, SO2, ect.) moving through lithosphere and pyrosphere (MOHO discontinuity) till they meet projections (mountains negative projections or projections coming from sinking lithosphere). The liquids are moved from West Eastward carried away by the pyrosphere because of differential speed of rotation of the pyrosphere by the lithosphere. With starting point an earthquake which was noticed at an area and from statistical studies, we know when, where and what rate an earthquake may be, which earthquake is caused by the same quantity of liquids, at the next east region. The forecast of an earthquake ceases to be valid if these components meet a crack in the lithosphere (e.g. limits of lithosphere plates) or a volcano crater. In this case the liquids come out into the atmosphere by the form of gasses carrying small quantities of lava with them (volcano explosion).

  10. Active Deformation of Etna Volcano Combing IFSAR and GPS data

    Science.gov (United States)

    Lundgren, Paul

    1997-01-01

    The surface deformation of an active volcano is an important indicator of its eruptive state and its hazard potential. Mount Etna volcano in Sicily is a very active volcano with well documented eruption episodes.

  11. Abundancia estacional, fenología reproductiva y fidelidad al sitio del mulato (Melanotis caerulescens en ambientes ribereños del suroeste de Jalisco Seasonal abundance, reproductive phenology and site fidelity in riparian environments of the Blue Mockingbird (Melanotis caerulescens in southwestern Jalisco

    Directory of Open Access Journals (Sweden)

    Luz de los Milagros Rodríguez-Parga

    2012-06-01

    Full Text Available Este estudio describe la abundancia estacional, fenología reproductiva y fidelidad al sitio de Melanotis caerulescens, especie de ave endémica de México, localmente conocida como mulato y valorada por su canto. Se realizó un muestreo con el método de captura con redes de niebla durante 2 años en 3 sitios de la vegetación ribereña del río Ayuquila, Jalisco. Se caracterizó el hábitat mediante muestreos de los estratos arbóreo, arbustivo y herbáceo. Mediante modelos lineales generalizados se analizaron las diferencias de cobertura de los estratos entre los sitios y se identificó el efecto del sitio y el mes sobre la abundancia de la especie. La presencia de parche de incubación y protuberancia cloacal describe un periodo reproductor de abril a agosto. La abundancia del mulato se relacionó positivamente con sitios de mayor cobertura arbustiva y el análisis de fidelidad (por presencia-ausencia de 16 individuos mostró que 3 parejas reproductoras mantuvieron sus territorios. Estos resultados sugieren que mantener una adecuada densidad de sotobosque arbustivo en zonas ribereñas es importante para proveer alimento y áreas para la nidificación que requiere el mulato. El presente estudio es relevante por tratarse de los primeros datos al respecto que se publican sobre esta especie endémica.This study describes the seasonal abundance, reproductive phenology and site fidelity of the Blue Mockingbird (Melanotis caerulescens, an endemic species of Mexico noted for its singing capabilities. This species was sampled using mist-nets for 2 consecutive years at 3 sites of riparian vegetation in the Ayuquila River, Jalisco. Habitat characterization was carried out through sampling strata of trees, shrubs, and herbaceous ground cover. We used Generalized Linear Models to analyze the differences in coverage strata between the sites, and to identify the effect of site and month on the abundance of the species. The presence of a brood patch and

  12. Estimación de la exposición a fluoruros en Los Altos de Jalisco, México Estimation of exposure to fluoride in "Los Altos de Jalisco", México

    Directory of Open Access Journals (Sweden)

    Roberto Hurtado-Jiménez

    2005-02-01

    Full Text Available OBJETIVO: Estimar la exposición a fluoruros y riesgos potenciales a la salud humana en Los Altos de Jalisco, México. MATERIAL Y MÉTODOS: Se midió electroquímicamente la concentración de fluoruros en 105 pozos y seis tomas de agua potable, en los Altos de Jalisco, de mayo a julio de 2002. Se estimó la dosis de exposición y la ingestión total de fluoruros para: bebés de 10 kg, niños de 20 kg y adultos de 70 kg. RESULTADOS: La concentración de fluoruros en las muestras de agua varió entre 0.1 y 17.7 mg/l. El 45% de las muestras excede el límite permitido por la normatividad (1.5 mg/l. La ingestión total y dosis de exposición a fluoruros estimados están en los rangos de 0.5-18.4 mg/d y 0.04-1.8 mg/kg/d, respectivamente. CONCLUSIONES: Una parte importante de la población está expuesta a fluorosis dental, fluorosis esquelética y fracturas óseas. Para reducir los riesgos se debe evitar el consumo de sal fluorada, pastas dentales con flúor y agua potable cuya concentración de fluoruros sea mayor de 0.7 mg/l.OBJECTIVE: To estimate the level of fluoride exposure and human health risks in Los Altos de Jalisco (Jalisco State Heights region. MATERIAL AND METHODS: This study was conducted between May and July 2002. The fluoride concentrations of 105 water wells and six tap water samples were electrochemically measured. Exposure doses to fluoride and total intake of fluoride were estimated for babies (10 kg, children (20 kg, and adults (70 kg. RESULTS: The fluoride concentration of the water samples ranged from 0.1 to 17.7 mg/l. More than 45% of the water samples exceeded the national guideline value for fluoride of 1.5 mg/l. The estimated values of the exposure doses to fluoride and total intake of fluoride were in the range of 0.04-1.8 mg/kg/d and 0.5-18.4 mg/d, respectively. CONCLUSIONS: Dental fluorosis, skeletal fluorosis, and bone fractures are some of the potential health risks due to the intake of high doses of fluoride for the

  13. Campgrounds in Hawaii Volcanoes National Park

    Data.gov (United States)

    National Park Service, Department of the Interior — This dataset provides campground locations in Hawaii Volcanoes National Park. Information about facilities, water availability, permit requirements and type of...

  14. Ambient seismic noise tomography of the Colima Volcano Complex

    Science.gov (United States)

    Escudero, Christian R.; Bandy, William L.

    2017-02-01

    The Colima Volcanic Complex (CVC) located in the western sector of the Trans-Mexican Volcanic Belt contains the most active Mexican volcano, Volcan Colima. The CVC is located within the Colima Rift, a regional north south striking extensional structure. We used ambient seismic noise recorded by stations deployed in western Mexico during the Mapping the Rivera Subduction Zone (MARS) and the Colima Volcano Deep Seismic Experiment (CODEX). We computed the cross-correlations of the vertical component of continuous records of ambient noise data to extract empirical Greens functions. These functions provide detailed images of Rayleigh wave group velocity for different periods. Using the arrival travel time of these waves for a given period, estimates can be obtained of the lateral variations in velocity for a given period using 2D tomography. The study aims to better understand the geometry and the seismic surface wave velocity structure of the CVC and relate it to the volcanoes' structure and the geologic setting of the region. Source of low velocity anomaly over CVC is distributed fairly continuously with depth in the subsurface, which indicates magma rising along fractures. The progressive increasing toward the south in the size of low velocity anomalies indicates migration towards the south of the melting that correlates with the trend of the stratovolcanoes that form the CVC. The zone of magma generation presently fully developed under Volcan de Fuego might be starting to shift towards south to the area NW of Armería where a new void in the tear zone may be starting to form.

  15. Dos nuevos registros de alimentación de Quiscalus mexicanus y Cyanocorax sanblasianus en la costa de Chamela, Jalisco, México

    OpenAIRE

    Marco A. GURROLA HIDALGO; Cornelio SÁNCHEZ-HERNÁNDEZ; María de Lourdes ROMERO ALMARAZ

    2009-01-01

    Information over the feeding habits of neotropical birds have been relatively few documented, this is the first report in México over the depredation of the mole crabs (Emerita spp.) by the Great-tailed Grackle (Quiscalus mexicanus) and for Ruddy-ground Dove (Columbina talpacoti) by San Blas Jay (Cyanocorax sanblasianus), in the coast of Chamela, Jalisco, México.

  16. Prevalencia de deficiencia de hierro y yodo, y parasitosis en niños de Arandas, Jalisco, México

    Directory of Open Access Journals (Sweden)

    Vásquez-Garibay Edgar Manuel

    2002-01-01

    Full Text Available Objetivo. Estimar la prevalencia de deficiencia de hierro, yodo y parasitosis en niños que asisten al Instituto Alteño para el Desarrollo de Jalisco (Inadej, Arandas, Jalisco, México. Material y métodos. Estudio transversal efectuado entre 1997 y 1999 con 432 niños de 12 a 120 meses de edad, de nuevo ingreso al Inadej. Se determinaron variables hematológicas, yodo en orina y presencia de parásitos. Se utilizaron las pruebas Ji cuadrada y t de Student en variables no paramétricas y paramétricas. Resultados. Hubo más anemia (20 vs 7.4% p=0.007 y deficiencia de hierro (60.9 vs 44.4% p=0.02 en prescolares que en escolares. El 29% presentaron deficiencia de yodo (10.5% moderada o grave y 47.2% parasitosis. Predominaron G. lamblia y E. histolytica. Bajo salario, sexo masculino y no tener seguridad social se asociaron con parasitosis. Conclusiones. La elevada prevalencia de deficiencia de hierro, yodo y parasitosis obliga al sector salud estatal a ejecutar medidas eficaces para abatir estas enfermedades prevenibles.

  17. Quaternary glacial stratigraphy and chronology of Mexico

    Science.gov (United States)

    White, Sidney E.

    The volcano Iztaccihuatl in central Mexico was glaciated twice during the middle Pleistocene, once probably in pre-Illinoian (or pre-Bull Lake) time, and once in late Illinoian (or Bull Lake) time. Glaciation during the late Pleistocene was restricted to the late Wisconsin (or Pinedale). A maximum advance and one readvance are recorded in the early part, and one readvance in the latter part. Three or four small neoglacial advances occurred during the Holocene. Two other volcanoes nearby, Ajusco and Malinche, have a partial record of late Pleistocene and Holocene glaciations. Three others, Popocatépetl, Pico de Orizaba, and Nevado de Toluca, have a full Holocene record of three to five glacial advances during Neoglaciation.

  18. Results from the Autonomous Triggering of in situ Sensors on Kilauea Volcano, HI, from Eruption Detection by Spacecraft

    Science.gov (United States)

    Doubleday, J.; Behar, A.; Davies, A.; Mora-Vargas, A.; Tran, D.; Abtahi, A.; Pieri, D. C.; Boudreau, K.; Cecava, J.

    2008-12-01

    Response time in acquiring sensor data in volcanic emergencies can be greatly improved through use of autonomous systems. For instance, ground-based observations and data processing applications of the JPL Volcano Sensor Web have promptly triggered spacecraft observations [e.g., 1]. The reverse command and information flow path can also be useful, using autonomous analysis of spacecraft data to trigger in situ sensors. In this demonstration project, SO2 sensors were incorporated into expendable "Volcano Monitor" capsules and placed downwind of the Pu'u 'O'o vent of Kilauea volcano, Hawai'i. In nominal (low) power conservation mode, data from these sensors were collected and transmitted every hour to the Volcano Sensor Web through the Iridium Satellite Network. When SO2 readings exceeded a predetermined threshold, the modem within the Volcano Monitor sent an alert to the Sensor Web, and triggered a request for prompt Earth Observing-1 (EO-1) spacecraft data acquisition. The Volcano Monitors were also triggered by the Sensor Web in response to an eruption detection by the MODIS instrument on Terra. During these pre- defined "critical events" the Sensor Web ordered the SO2 sensors within the Volcano Monitor to increase their sampling frequency to every 5 minutes (high power "burst mode"). Autonomous control of the sensors' sampling frequency enabled the Sensor Web to monitor and respond to rapidly evolving conditions, and allowed rapid compilation and dissemination of these data to the scientific community. Reference: [1] Davies et al., (2006) Eos, 87, (1), 1 and 5. This work was performed at the Jet Propulsion Laboratory-California Institute of Technology, under contract to NASA. Support was provided by the NASA AIST program, the Idaho Space Grant Consortium, and the New Mexico Space Grant Program. We also especially thank the personnel of the USGS Hawaiian Volcano Observatory for their invaluable scientific guidance and logistical assistance.

  19. Research on Methods for Building Volcano Disaster Information System--taking Changbai Mountain as an example

    Institute of Scientific and Technical Information of China (English)

    ZHANG Xuexia; BO Liqun; LU Xingchang

    2001-01-01

    Volcano eruption is one of the most serious geological disasters in the world. There are volcanoes in every territory on the earth, about a thousand in China, among which Changbai Mountain Volcano, Wudalianchi Volcano and Tengchong Volcano are the most latent catastrophic eruptive active volcanoes. The paper, following an instance of Changbai Mountain Volcano, expounds that monitoring, forecasting and estimating volcano disaster by building Volcano Disaster Information System (VDIS) is feasible to alleviate volcano disaster.

  20. Volcanic hazards at Atitlan volcano, Guatemala

    Science.gov (United States)

    Haapala, J.M.; Escobar Wolf, R.; Vallance, James W.; Rose, William I.; Griswold, J.P.; Schilling, S.P.; Ewert, J.W.; Mota, M.

    2006-01-01

    Atitlan Volcano is in the Guatemalan Highlands, along a west-northwest trending chain of volcanoes parallel to the mid-American trench. The volcano perches on the southern rim of the Atitlan caldera, which contains Lake Atitlan. Since the major caldera-forming eruption 85 thousand years ago (ka), three stratovolcanoes--San Pedro, Toliman, and Atitlan--have formed in and around the caldera. Atitlan is the youngest and most active of the three volcanoes. Atitlan Volcano is a composite volcano, with a steep-sided, symmetrical cone comprising alternating layers of lava flows, volcanic ash, cinders, blocks, and bombs. Eruptions of Atitlan began more than 10 ka [1] and, since the arrival of the Spanish in the mid-1400's, eruptions have occurred in six eruptive clusters (1469, 1505, 1579, 1663, 1717, 1826-1856). Owing to its distance from population centers and the limited written record from 200 to 500 years ago, only an incomplete sample of the volcano's behavior is documented prior to the 1800's. The geologic record provides a more complete sample of the volcano's behavior since the 19th century. Geologic and historical data suggest that the intensity and pattern of activity at Atitlan Volcano is similar to that of Fuego Volcano, 44 km to the east, where active eruptions have been observed throughout the historical period. Because of Atitlan's moderately explosive nature and frequency of eruptions, there is a need for local and regional hazard planning and mitigation efforts. Tourism has flourished in the area; economic pressure has pushed agricultural activity higher up the slopes of Atitlan and closer to the source of possible future volcanic activity. This report summarizes the hazards posed by Atitlan Volcano in the event of renewed activity but does not imply that an eruption is imminent. However, the recognition of potential activity will facilitate hazard and emergency preparedness.

  1. Allele and haplotype distribution for 16 Y-STRs (AmpFlSTR Y-filer kit) in the state of Chihuahua at North Center of Mexico.

    Science.gov (United States)

    Gutiérrez-Alarcón, A B; Moguel-Torres, M; León-Jiménez, A K; Cuéllar-Nevárez, G E; Rangel-Villalobos, H

    2007-05-01

    The AmpFlSTR Y-filer kit, including 16 Y-STRs was analyzed in 326 males from Chihuahua, at North Central, Mexico. Allele frequencies and gene diversity for each locus were estimated. Four allele duplications, namely DYS389II, DYS390, DYS391 and DYS439; and one allele null at DYS448 were observed in the sample. The haplotype diversity was 99.97+/-0.3%. The AMOVA results, including a previous report from West of Mexico (Jalisco), showed that most of the genetic variability between these Mexican populations is attributable to intrapopulational differences (99.87%). This result supports a low-genetic differentiation between males from North and West regions of Mexico.

  2. Micro-earthquake signal analysis and hypocenter determination around Lokon volcano complex

    Energy Technology Data Exchange (ETDEWEB)

    Firmansyah, Rizky, E-mail: rizkyfirmansyah@hotmail.com [Geophysical Engineering, Faculty of Mining and Petroleum Engineering, Institut Teknologi Bandung, Bandung, 40132 (Indonesia); Nugraha, Andri Dian, E-mail: nugraha@gf.itb.ac.id [Global Geophysical Group, Faculty of Mining and Petroleum Engineering, Institut Teknologi Bandung, Bandung, 40132 (Indonesia); Kristianto, E-mail: kris@vsi.esdm.go.id [Center for Volcanology and Geological Hazard Mitigation (CVGHM), Geological Agency, Bandung, 40122 (Indonesia)

    2015-04-24

    Mount Lokon is one of five active volcanoes which is located in the North Sulawesi region. Since June 26{sup th}, 2011, standby alert set by the Center for Volcanology and Geological Hazard Mitigation (CVGHM) for this mountain. The Mount Lokon volcano erupted on July 4{sup th}, 2011 and still continuously erupted until August 28{sup th}, 2011. Due to its high seismic activity, this study is focused to analysis of micro-earthquake signal and determine the micro-earthquake hypocenter location around the complex area of Lokon-Empung Volcano before eruption phase in 2011 (time periods of January, 2009 up to March, 2010). Determination of the hypocenter location was conducted with Geiger Adaptive Damping (GAD) method. We used initial model from previous study in Volcan de Colima, Mexico. The reason behind the model selection was based on the same characteristics that shared between Mount Lokon and Colima including andesitic stratovolcano and small-plinian explosions volcanian types. In this study, a picking events was limited to the volcano-tectonics of A and B types, hybrid, long-period that has a clear signal onset, and local tectonic with different maximum S – P time are not more than three seconds. As a result, we observed the micro-earthquakes occurred in the area north-west of Mount Lokon region.

  3. Micro-earthquake signal analysis and hypocenter determination around Lokon volcano complex

    Science.gov (United States)

    Firmansyah, Rizky; Nugraha, Andri Dian; Kristianto

    2015-04-01

    Mount Lokon is one of five active volcanoes which is located in the North Sulawesi region. Since June 26th, 2011, standby alert set by the Center for Volcanology and Geological Hazard Mitigation (CVGHM) for this mountain. The Mount Lokon volcano erupted on July 4th, 2011 and still continuously erupted until August 28th, 2011. Due to its high seismic activity, this study is focused to analysis of micro-earthquake signal and determine the micro-earthquake hypocenter location around the complex area of Lokon-Empung Volcano before eruption phase in 2011 (time periods of January, 2009 up to March, 2010). Determination of the hypocenter location was conducted with Geiger Adaptive Damping (GAD) method. We used initial model from previous study in Volcan de Colima, Mexico. The reason behind the model selection was based on the same characteristics that shared between Mount Lokon and Colima including andesitic stratovolcano and small-plinian explosions volcanian types. In this study, a picking events was limited to the volcano-tectonics of A and B types, hybrid, long-period that has a clear signal onset, and local tectonic with different maximum S - P time are not more than three seconds. As a result, we observed the micro-earthquakes occurred in the area north-west of Mount Lokon region.

  4. Evaluación de la exposición a selenio en Los Altos de Jalisco, México Evaluation of the exposure to selenium in Los Altos de Jalisco, México

    Directory of Open Access Journals (Sweden)

    Roberto Hurtado-Jiménez

    2007-08-01

    Full Text Available OBJETIVO: Evaluar la exposición a selenio (Se vía agua potable en los habitantes de Los Altos de Jalisco. MATERIAL Y MÉTODOS: Se determinó la concentración de Se en 125 pozos y se estimaron los niveles de exposición a Se en bebés, niños y adultos. RESULTADOS: La dosis de exposición y la ingestión de Se vía agua potable variaron en los siguientes rangos: a bebés: 1.3-6.7 µg/kg/d y 12.6-67.2 µg/d; b niños: 0.8-4.5 µg/kg/d y 16.8-89.6 µg/d; c adultos: 0.6-3.0 µg/kg/d y 33.6-179.2 µg/d. CONCLUSIONES: En este caso, la exposición a Se representa un riesgo potencial para la salud de la población, ya que en la mayoría de los casos es mayor que la recomendada por organismos internacionales de salud. Sin embargo, no es tan alta como para esperar la ocurrencia de selenosis.OBJECTIVE: To evaluate the exposure to selenium in drinking water in Los Altos de Jalisco (Jalisco State Heights. MATERIALS AND METHODS: The concentration of selenium was determined in 125 water wells, and the exposure doses to selenium were estimated for babies, children and adults. RESULTS: The estimated values of the exposure doses to selenium and total intake of selenium were in the following ranges, respectively: (a babies: 1.3-6.7 µg/kg/d and 12.6-67.2 µg/d; (b children: 0.8-4.5 µg/kg/d and 16.8-89.6 µg/d, (c adults: 0.6-3.0 µg/kg/d and 33.6-179.2 µg/d. CONCLUSIONS: The estimated exposure levels to selenium were higher than those recommended as optimum by international health organizations, representing a potential health risk. Nevertheless, estimated values are not high enough to produce selenosis.

  5. Validación de un instrumento para vigilar la inseguridad alimentaria en la Sierra de Manantlán, Jalisco Validation of an instrument to monitor food insecurity in Sierra de Manantlán, Jalisco

    Directory of Open Access Journals (Sweden)

    Hugo Melgar-Quiñonez

    2005-12-01

    Full Text Available OBJETIVO: Validar una versión de la Escala de Seguridad Alimentaria (FSS en comunidades de la Sierra de Manatlán, Jalisco. MATERIAL Y MÉTODOS: Usando grupos focales se modificó la FSS. Posteriormente se aplicó una encuesta a mujeres con niños preescolares. La FSS se validó correlacionándola con el inventario de alimentos del hogar y con la variedad de dieta de la entrevistada. La encuesta incluyó un cuestionario socio-económico. RESULTADOS: El 44% de los hogares indicaron inseguridad alimentaria leve, 33% hambre moderada y 19.7% hambre severa. La inseguridad alimentaria estuvo inversamente correlacionada con el inventario de alimentos (r=-0.36**, alimentos de origen animal (r=-0.28**, lácteos (r=-0.25**, alimentos procesados (r=-0.37**, frutas (r=-0.21* y verduras (r=-0.28**; *pOBJECTIVE: To validate a version of the Food Security Scale (FSS in communities located in Sierra de Manantlán, Jalisco. MATERIAL AND METHODS: Using focus groups, the FSS was modified to fit the Mexican context. Subsequently, a survey was applied to women with pre-school aged children. The FSS was validated in correlation with a household food inventory and the dietary variety of the individual being interviewed. The interview also included a socioeconomic questionnaire. RESULTS: Forty-four percent of the households reported mild food insecurity, 33% reported moderate hunger and 19.7% reported severe hunger. Food insecurity was significantly and inversely correlated with the number of food items in the household (r=-0.36**, animal source foods (r=-0.28**, dairy products (r=-0.25*, processed foods (r=-0.37**, fruits (r=-0.21*, and vegetables (r=-0.28**; *p<0.05, **p< 0.01. Food insecurity was also associated with low dietary variety (r=-0.23, p=0.02. These associations were maintained in multivariate models. CONCLUSIONS: The FSS is a useful tool for monitoring food insecurity in rural regions of Jalisco.

  6. Predictability of Volcano Eruption: lessons from a basaltic effusive volcano

    CERN Document Server

    Grasso, J R

    2003-01-01

    Volcano eruption forecast remains a challenging and controversial problem despite the fact that data from volcano monitoring significantly increased in quantity and quality during the last decades.This study uses pattern recognition techniques to quantify the predictability of the 15 Piton de la Fournaise (PdlF) eruptions in the 1988-2001 period using increase of the daily seismicity rate as a precursor. Lead time of this prediction is a few days to weeks. Using the daily seismicity rate, we formulate a simple prediction rule, use it for retrospective prediction of the 15 eruptions,and test the prediction quality with error diagrams. The best prediction performance corresponds to averaging the daily seismicity rate over 5 days and issuing a prediction alarm for 5 days. 65% of the eruptions are predicted for an alarm duration less than 20% of the time considered. Even though this result is concomitant of a large number of false alarms, it is obtained with a crude counting of daily events that are available fro...

  7. Caesarean sections in Mexico: are there too many?

    Science.gov (United States)

    Gonzalez-Perez, G J; Vega-Lopez, M G; Cabrera-Pivaral, C; Muñoz, A; Valle, A

    2001-03-01

    This paper seeks to quantify the magnitude of caesarean sections in Mexican public health-care institutions in recent years, to characterize the evolution of caesarean section rates (CSR) during the last decade, and to estimate the possible economic cost caused by the excess of caesareans performed in these institutions. The study is based on data obtained from the health sector, both for Mexico in the 5-year period 1993-97 and for the Mexican State of Jalisco between 1983 and 1998. Linear regression analysis was used to evaluate time series, and "excess of caesareans" was considered the number of caesarean deliveries performed above the admissible 15% CSR. The results reflect that on the national level, more than one-quarter of the deliveries handled by public institutions ended in caesarean section for each analyzed year, and if the deliveries performed in private institutions are included, the national rate is around 30%. A marked increase in CSR can be observed in Jalisco between 1983 and 1998 (almost 50%); and the cost for the nation of this CSR excess in financial terms is highly significant: several millions of dollars--obtained from public funds--are spent annually and unnecessarily by health services. The findings suggest that the increase in CSR is a public health problem that has not been satisfactorily faced by the health sector authorities. Many unnecessary caesareans would undoubtedly be avoided if the policies of these public health-care institutions were to consider, as a priority, both the known higher risk implicit in a caesarean for the health of the mother and child, and the economic impact on the country and its health institutions of the excessive number of caesareans performed yearly.

  8. Newberry Volcano's youngest lava flows

    Science.gov (United States)

    Robinson, Joel E.; Donnelly-Nolan, Julie M.; Jensen, Robert A.

    2015-01-01

    Most of Newberry Volcano's youngest lava flows are found within the Newberry National Volcanic Monument in central Oregon. Established November 5, 1990, the monument is managed by the U.S. Forest Service as part of the Deschutes National Forest. Since 2011, a series of aerial surveys over the monument collected elevation data using lidar (light detection and ranging) technology, which uses lasers to directly measure the ground surface. These data record previously unseen detail in the volcano’s numerous lava flows and vents. On average, a laser return was collected from the ground’s surface every 2.17 feet (ft) with ±1.3 inches vertical precision.

  9. Geochemistry of fluids from submarine hot springs at Punta de Mita, Nayarit, Mexico

    Science.gov (United States)

    Taran, Y. A.; Inguaggiato, S.; Marin, M.; Yurova, L. M.

    2002-06-01

    Thermal springs with a maximum measured temperature of 89°C discharge hot water and gas from a depth of 11 m, 400 m offshore of Punta Pantoque, located in the northern part of Bahı´a de Banderas, near Puerto Vallarta, Mexico. The composition of all water samples collected from the sea bottom is close to that of sea water. Nevertheless, it was possible to estimate the thermal endmember composition by extrapolating the sulfate concentration to zero. This endmember is similar in chemical composition both to waters of the Rio Purificacion and La Tuna thermal springs, located to the South along the Pacific coast of the Jalisco Block, and to pore waters from the deep-sea drilling cores from some accretionary complexes. Gas composition as well as isotopic composition of He and carbon from CO 2, CH 4 and C 2H 6 suggests an essentially thermo-biogenic origin for the gas and the presence of a high proportion of radiogenic, crustal helium. Isotopic composition of He in the Punta de Mita gas (0.4 Ra) is the lowest ever measured in Mexican hydrothermal gases. These findings do not support the idea that there exists a direct connection between the Punta de Mita springs and the last volcanic events which occurred in this area at ˜3 Ma. Rather, this hydrothermal activity is related to deep active faulting and the existence of a deep regional aquifer or local aquifers of connate waters underlying the granites of the Jalisco Block.

  10. Seamount subduction and related deformation and seismicity of the continental slope off Manzanillo, Mexico, as evidenced by multibeam data

    Science.gov (United States)

    Bandy, W. L.; Castillo Maldonado, M.; Mortera-Gutierrez, C. A.

    2014-12-01

    The west coast of Mexico presents a complex pattern of deformation related to the convergence and subduction of the Rivera plate beneath the Jalisco Block/North American plate. Previous single beam bathymetric data have evidenced a large bathymetric high at 104.6218oW, 18.7123oN, in the continental slope region off Manzanillo, Mexico. One school of thought held that this high was the offshore extension of the onshore Manzanillo horst, although the two features are offset in a right-lateral sense. Alternatively, given the presence of a large positive magnetic anomaly near the bathymetric high, the high could also be caused by the collision and subsequent subduction of a large seamount. Given that the offset between the two structures was the main evidence for proposing the existence of a forearc sliver in the offshore area of the Jalisco margin, resolving the nature of this bathymetric high is quite important in our attempts to understand the plate kinematics and tectonics of this region. Thus, to better define the deformation pattern associated with the bathymetric high, multibeam bathymetric data (obtained using the Kongsberg EM300 multibeam system), subbottom profiles (obtained using the Kongsberg TOPAS18 system), and total field magnetic data (obtained using the Geometrics G877 marine proton precession magnetometer) were collected in the continental slope region between Manzanillo, Colima, and Chamela, Jalisco, during several cruises of UNAM´s research vessel the B.O. EL PUMA. The morphology and structural deformation patterns obtained in this study indicate very clearly that a large seamount is in the process of subducting beneath the continental slope off Manzanillo. The results also indicate that not only has the seamount uplifted the slope but has resulted in slumping of the area of the slope landward of the seamount. Given these results the proposal of the existence of an independent forearc sliver in the offshore area of the southern Jalisco block needs

  11. Los peces de las aguas continentales del estado de Jalisco, México. Análisis preliminar

    Directory of Open Access Journals (Sweden)

    Manuel Guzmán A.

    2003-01-01

    Full Text Available Análisis bibliográfico y documental y revisión de las colecciones de peces de los museos de zoología de las Universidades de Michigan, Wisconsin, y del Instituto de Limnología, de la Universidad de Guadalajara. De las 20 cuencas hidrológicas de la región estudiada se analizaron 15, que cubren el 72.9 % del territorio de Jalisco. El artículo presenta un listado sistemático de las 137 especies encontradas, repartidas en 32 familias y 69 géneros. Sin embargo, dichos datos son preliminares dado que algunas cuencas están todavía en proceso de estudio y, por tanto, no se cuenta con la información suficiente. El artículo propone también un sistema de análisis de las características de las especies, dividido en ocho grupos de información distribuidos por afinidad biogeográfica, categoría ecológica, límite geográfico, hábitat, situación actual, estatus legal, y uso y distribución de la especie. De acuerdo con la Norma Oficial Mexicana, 11 especies se encuentran en Jalisco y se conocen dos especies extintas: la Notropis amecae y la Allotoca maculata. Como resultado de un análisis de riqueza de especies y de endemismo en la zona de estudio, se propuso un índice de pureza (proporción de especies nativas respecto al total de las mismas. La riqueza varió de 14 a 50. El endemismo por cuenca tuvo un rango de 3.4% a un 8.5%, con un promedio de 5.8%. De acuerdo con las relaciones ictiofaunísticas entre cuencas, destacan dos grupos: el primero corresponde a cuencas de aguas limnéticas y el segundo a cuencas en contacto con aguas estuarinas y marinas. Finalmente se da una serie de recomendaciones para la conservación de la ictiofauna en el estado de Jalisco

  12. The effect of Saccharomyces cerevisiae on digestion and mortality in the volcano rabbit (Romerolagus diazi)

    Institute of Scientific and Technical Information of China (English)

    Rogelio Campos-Morales; Germn D Mendoza; Javier Ojeda; Fernando X Plata; Jos A Martnez

    2015-01-01

    An experiment was conducted to evaluate whether supplementation with a probiotic could enhance digestion and reduce mortality in the volcano rabbit in captivity. Two enclosures at Chapultepec Zoo, Mexico (114 individuals) were used in a cross-over design (two periods of 60 days) with the fol owing treatments:control group and supplementation with Saccharomyces cerevisiae (2×108 CFU/exhibit/day). Supplementation with the probiotic negatively affected (P<0.01) the digestibility of dry matter, organic matter, neutral detergent ifber (NDF) and energy. Mortality increased (P<0.04) fol owing supplementation with the probiotic (4.26%vs. 8.89%), primarily in the juvenile rabbits. The results indicate that yeast supplementation in the volcano rabbit negatively affects digestion and mortality in captivity.

  13. PRESENCIA DE LA CERÁMICA SEUDO-CLOISONNÉ EN LA CULTURA BOLAÑOS, JALISCO Y ZACATECAS (Presence of the Pseudo-cloisonné Pottery in the Bolaños Culture, Jalisco and Zacatecas)

    OpenAIRE

    María Teresa Cabrero G.

    2012-01-01

    La cerámica seudo-cloisonné tuvo una amplia distribución en el mundo prehispánico mexicano a partir de 200 d. C. Se denominó así por la semejanza en la técnica decorativa con el verdadero cloisonné elaborado sobre metal. La presencia de esta técnica poscocción en la cultura Bolaños, ubicada en parte de los estados de Jalisco y Zacatecas, constituyó una prueba más del contacto comercial que existió con la cultura Chalchihuites (noroeste de Zacatecas); a la cual le llegó a través de la ruta de ...

  14. Volcanic hazard zonation of the Nevado de Toluca volcano, México

    Science.gov (United States)

    Capra, L.; Norini, G.; Groppelli, G.; Macías, J. L.; Arce, J. L.

    2008-10-01

    The Nevado de Toluca is a quiescent volcano located 20 km southwest of the City of Toluca and 70 km west of Mexico City. It has been quiescent since its last eruptive activity, dated at ˜ 3.3 ka BP. During the Pleistocene and Holocene, it experienced several eruptive phases, including five dome collapses with the emplacement of block-and-ash flows and four Plinian eruptions, including the 10.5 ka BP Plinian eruption that deposited more than 10 cm of sand-sized pumice in the area occupied today by Mexico City. A detailed geological map coupled with computer simulations (FLOW3D, TITAN2D, LAHARZ and HAZMAP softwares) were used to produce the volcanic hazard assessment. Based on the final hazard zonation the northern and eastern sectors of Nevado de Toluca would be affected by a greater number of phenomena in case of reappraisal activity. Block-and-ash flows will affect deep ravines up to a distance of 15 km and associated ash clouds could blanket the Toluca basin, whereas ash falls from Plinian events will have catastrophic effects for populated areas within a radius of 70 km, including the Mexico City Metropolitan area, inhabited by more than 20 million people. Independently of the activity of the volcano, lahars occur every year, affecting small villages settled down flow from main ravines.

  15. La prematurez y sus repercusiones en el crecimiento y desarrollo del niño, en la Zona Metropolitana de Guadalajara, Jalisco, México Premature birth and its repercussions on growth and development in Guadalajara, Jalisco, México

    Directory of Open Access Journals (Sweden)

    Alfredo Ramos Ramos

    1998-04-01

    Full Text Available El presente estudio tiene por objetivo conocer las repercusiones de la prematurez en el crecimiento y desarrollo del niño, para lo cual se hace un seguimiento de niños nacidos en hospitales de la Zona Metropolitana de Guadalajara, Jalisco, México, de los más representativos del Sistema de Atención Médica en México. Estos niños fueron seguidos con evaluaciones semestrales, tanto en lo que se refiere al estado nutricional (crecimiento, como al desarrollo (Prueba Selectiva de Denver. El análisis de los resultados se realiza con la consideración de las clases sociales como categorías determinantes, para ubicar posteriormente a la prematurez como variable dependiente. Los resultados sugieren que tanto la prematurez como las clases sociales son aspectos que, en Salud Pública, deben ser considerados en el momento de planificar las acciones de atención a la salud.This study focuses on the repercussions of prematurity for the growth and development of newborns from hospitals in Guadalajara, Jalisco, México, typical of the health care system in México. Infants were assessed every six months as to nutritional status and the Denver Selective Test. In analyzing the results, social groups were considered determinant categories for studying prematurity as the dependent variable. The results shows that both prematurity and social group are risk factors to be considered by the public health field when designing health care programs.

  16. Carbon and Aerosol Emissions from Biomass Fires in Mexico

    Science.gov (United States)

    Hao, W. M.; Flores Garnica, G.; Baker, S. P.; Urbanski, S. P.

    2009-12-01

    Biomass burning is an important source of many atmospheric greenhouse gases and photochemically reactive trace gases. There are limited data available on the spatial and temporal extent of biomass fires and associated trace gas and aerosol emissions in Mexico. Biomass burning is a unique source of these gases and aerosols, in comparison to industrial and biogenic sources, because the locations of fires vary considerably both daily and seasonally and depend on human activities and meteorological conditions. In Mexico, the fire season starts in January and about two-thirds of the fires occur in April and May. The amount of trace gases and aerosols emitted by fires spatially and temporally is a major uncertainty in quantifying the impact of fire emissions on regional atmospheric chemical composition. To quantify emissions, it is necessary to know the type of vegetation, the burned area, the amount of biomass burned, and the emission factor of each compound for each ecosystem. In this study biomass burning experiments were conducted in Mexico to measure trace gas emissions from 24 experimental fires and wildfires in semiarid, temperate, and tropical ecosystems from 2005 to 2007. A range of representative vegetation types were selected for ground-based experimental burns to characterize fire emissions from representative Mexico fuels. A third of the country was surveyed each year, beginning in the north. The fire experiments in the first year were conducted in Chihuahua, Nuevo Leon, and Tamaulipas states in pine forest, oak forest, grass, and chaparral. The second-year fire experiments were conducted on pine forest, oak forest, shrub, agricultural, grass, and herbaceous fuels in Jalisco, Puebla, and Oaxaca states in central Mexico. The third-year experiments were conducted in pine-oak forests of Chiapas, coastal grass, and low subtropical forest on the Yucatan peninsula. FASS (Fire Atmosphere Sampling System) towers were deployed for the experimental fires. Each FASS

  17. 77 FR 2609 - Unblocking of Specially Designated Nationals and Blocked Persons Pursuant to the Foreign...

    Science.gov (United States)

    2012-01-18

    ...., Guadalajara, Jalisco, Mexico; DOB 05 Aug 1959; POB Guadalajara, Mexico; citizen Mexico; nationality Mexico; C... EXPRESS, S.A. DE C.V.; a.k.a. GRUPO LOMEDIC), Av. del Parque 489, Col. San Andres, Guadalajara, Jalisco...

  18. 76 FR 58562 - Additional Designations, Foreign Narcotics Kingpin Designation Act

    Science.gov (United States)

    2011-09-21

    .... VASQUES HERNANDEZ, Alfredo; a.k.a. ``Alfredo Compadre''; a.k.a. BAZAN OROZCO, Alberto; a.k.a. ``Don..., Guadalajara, Jalisco, Mexico; DOB 19 Jan 1973; POB Jalisco, Mexico; Citizen Mexico; Nationality Mexico; C.U.R...

  19. Instrumentation Recommendations for Volcano Monitoring at U.S. Volcanoes Under the National Volcano Early Warning System

    Science.gov (United States)

    Moran, Seth C.; Freymueller, Jeff T.; LaHusen, Richard G.; McGee, Kenneth A.; Poland, Michael P.; Power, John A.; Schmidt, David A.; Schneider, David J.; Stephens, George; Werner, Cynthia A.; White, Randall A.

    2008-01-01

    As magma moves toward the surface, it interacts with anything in its path: hydrothermal systems, cooling magma bodies from previous eruptions, and (or) the surrounding 'country rock'. Magma also undergoes significant changes in its physical properties as pressure and temperature conditions change along its path. These interactions and changes lead to a range of geophysical and geochemical phenomena. The goal of volcano monitoring is to detect and correctly interpret such phenomena in order to provide early and accurate warnings of impending eruptions. Given the well-documented hazards posed by volcanoes to both ground-based populations (for example, Blong, 1984; Scott, 1989) and aviation (for example, Neal and others, 1997; Miller and Casadevall, 2000), volcano monitoring is critical for public safety and hazard mitigation. Only with adequate monitoring systems in place can volcano observatories provide accurate and timely forecasts and alerts of possible eruptive activity. At most U.S. volcanoes, observatories traditionally have employed a two-component approach to volcano monitoring: (1) install instrumentation sufficient to detect unrest at volcanic systems likely to erupt in the not-too-distant future; and (2) once unrest is detected, install any instrumentation needed for eruption prediction and monitoring. This reactive approach is problematic, however, for two reasons. 1. At many volcanoes, rapid installation of new ground-1. based instruments is difficult or impossible. Factors that complicate rapid response include (a) eruptions that are preceded by short (hours to days) precursory sequences of geophysical and (or) geochemical activity, as occurred at Mount Redoubt (Alaska) in 1989 (24 hours), Anatahan (Mariana Islands) in 2003 (6 hours), and Mount St. Helens (Washington) in 1980 and 2004 (7 and 8 days, respectively); (b) inclement weather conditions, which may prohibit installation of new equipment for days, weeks, or even months, particularly at

  20. [Scorpion stings: a public health problem in Morelos (Mexico)].

    Science.gov (United States)

    Bourée, Patrice; Frinot Joseph, P; Fernot Joseph, P; Gil, R E Morell; Fils-Aimé, F; Barrera, R Rosales; Goyffon, M

    2005-01-01

    Scorpion stings represent a major public health problem in Mexico. Their annual incidence is estimated at 150,000 cases; 800-1,000 people die from them each year, 72.5% of whom are children younger than 5 years old. The states most affected are Aguascalientes, Colima, Durango, Guanajuato, Guerrero, Jalisco, Michoacán, Morelos, Oaxaca, Puebla, Sinaloa, and Zacatecas. Morelos is an endemic zone, and scorpion stings are relatively frequent, but the indigenous population underestimates the risks. In this locality, scorpion stings lead to high morbidity, with an average of 10,219 cases each year, and a prevalence varying from 584.86 per 100,000 inhabitants in 1994 to 2043.3 per 100,000 inhabitants in 2003. Because of this upsurge, systematic medical supervision and serum therapy are necessary if scorpion poisoning is suspected in a child. The indigenous community as well as tourists visiting Mexico must be informed about the substantial risk of scorpion poisoning.

  1. Prevalence of Successful Aging in the Elderly in Western Mexico

    Directory of Open Access Journals (Sweden)

    Elva Dolores Arias-Merino

    2012-01-01

    Full Text Available Objectives. The aim of this paper is to estimate the prevalence of successful aging in the elderly in Western Mexico and to analyze its variability by age, sex, education, marital status, and pension. Methods. This study employs data from the Health, Wellbeing, and Aging Study (SABE in Jalisco and Colima, Mexico. Successful aging was operationalized in accordance with no important disease, no disability, physical functioning, cognitive functioning, and being actively. There were a total of 3116 elderly. Results. 12.6% of older adults were “successful” aging. The old-old is a lower proportion of successful aging people; it ranges from 18.9% among people aged 60–69 years to 3.9% in the 80–89 years and up to 1% in people 90 and older. There were also differences according to sex (P=.000, with a higher proportion of successful aging men (18.4% compared with 9.2% of women. There were differences in educational level (P=.000; those higher with education were found to be more successful aging, and also there were differences in marital status for married people (P=.000. Discussion. A small number of older adults meet the criteria definition of successful aging, suggesting the need to analyze in depth the concept and the indicators.

  2. Prevalence of successful aging in the elderly in Western Mexico.

    Science.gov (United States)

    Arias-Merino, Elva Dolores; Mendoza-Ruvalcaba, Neyda Ma; Arias-Merino, Martha Judith; Cueva-Contreras, Jazmín; Vazquez Arias, Carlos

    2012-01-01

    Objectives. The aim of this paper is to estimate the prevalence of successful aging in the elderly in Western Mexico and to analyze its variability by age, sex, education, marital status, and pension. Methods. This study employs data from the Health, Wellbeing, and Aging Study (SABE) in Jalisco and Colima, Mexico. Successful aging was operationalized in accordance with no important disease, no disability, physical functioning, cognitive functioning, and being actively. There were a total of 3116 elderly. Results. 12.6% of older adults were "successful" aging. The old-old is a lower proportion of successful aging people; it ranges from 18.9% among people aged 60-69 years to 3.9% in the 80-89 years and up to 1% in people 90 and older. There were also differences according to sex (P = .000), with a higher proportion of successful aging men (18.4% compared with 9.2% of women). There were differences in educational level (P = .000); those higher with education were found to be more successful aging, and also there were differences in marital status for married people (P = .000). Discussion. A small number of older adults meet the criteria definition of successful aging, suggesting the need to analyze in depth the concept and the indicators.

  3. Mallas de valor global en la agricultura de hortalizas en México. El caso de Sayula, Jalisco

    Directory of Open Access Journals (Sweden)

    Alejandro Macías Macías

    2009-01-01

    Full Text Available Desde mediados de la década de 1980, el cultivo de jitomate, brócoli y otras hortalizas ha cobrado importancia en Sayula, Jalisco. Este tipo de actividad se enmarca en mallas de valor en las que existen dinámicas extraterritoriales evidentes, como la provisión de insumos, factores de producción (incluida la mano de obra, comercialización y consumo, cuya labor central se ubica en otros territorios. Ahora bien, dentro de estas mallas de valor existen formas de organización diversas de la relación entre agricultores y compradores, de acuerdo con las características del producto, de los mercados y actores involucrados. Esto genera una diversidad de estructuras de gobierno, estudiadas en este trabajo, para así entender tanto los beneficios que le generan al agricultor, como las limitaciones que éste enfrenta ante tales relaciones.

  4. Risk factors associated with iron depletion and parasites in preschool and school children of Arandas, Jalisco, México.

    Science.gov (United States)

    Vásquez-Garibay, Edgar M; Campos Barrera, Liliana Romina; Romero Velarde, Enrique; Miranda Ríos, Lizette; Nuño Cosío, María Eugenia; Nápoles Rodríguez, Francisco

    2014-01-01

    Objetivo: Explorar factores asociados con depleción de hierro y parasitosis en preescolares y escolares que asisten al Instituto Alteño para el Desarrollo de Jalisco (INADEJ) y los niños que asisten a escuelas en Arandas, Jalisco. Métodos: Este estudio transversal evaluó dos grupos de niños. En el grupo INADEJ, fueron incluidos 102 niños de 60 a 144 meses de edad; en el grupo Escuelas fueron seleccionados 206 niños al azar de las escuelas del mismo municipio. Se obtuvieron las variables: ferritina (g/mL), parasitosis, variables demográficas, socioeconómicas, educativas y datos dietéticos. Se realizaron pruebas t de Student, U de Mann-Whitney, ji cuadrada; odds ratio y regresiones logísticas. Resultados: El ingreso familiar en el grupo escuelas era $ 5,707 pesos mexicanos (pm), más alto que el grupo INADEJ ($ 4,311 pm), p=0,031. La proporción de padres con educación primaria incompleta fue mayor en el grupo INADEJ (41,3%) que en el grupo escuelas (35,4%) [OR = 1,88 (1,0-3,55)]. Trabajo inestable del padre fue más frecuente en el grupo INADEJ [OR = 5,6 (3,26-9,62)]. La concentración de ferritina fue menor en el grupo INADEJ que en el grupo Escuelas (25 μg/L vs. 60 μg/ml, respectivamente), p.

  5. Volcanoes

    Science.gov (United States)

    ... Part 3 of 3) Hot Weather Tips Heat Stress in Older Adults FAQs Extreme Heat PSAs Related Links MMWR Bibliography CDC's Program Floods Flood Readiness Personal Hygiene After a Disaster Cleanup of Flood Water After a Flood Worker Safety Educational Materials Floods ...

  6. Redoubt Volcano: 2009 Eruption Overview

    Science.gov (United States)

    Bull, K. F.

    2009-12-01

    Redoubt Volcano is a 3110-m glaciated stratovolcano located 170 km SW of Anchorage, Alaska, on the W side of Cook Inlet. The edifice comprises a oil production in Cook Inlet was halted for nearly five months. Unrest began in August, 2008 with reports of H2S odor. In late September, the Alaska Volcano Observatory (AVO)’s seismic network recorded periods of volcanic tremor. Throughout the fall, AVO noted increased fumarolic emissions and accompanying ice- and snow-melt on and around the 1990 dome, and gas measurements showed elevated H2S and CO2 emissions. On January 23, seismometers recorded 48 hrs of intermittent tremor and discrete, low-frequency to hybrid events. Over the next 6 weeks, seismicity waxed and waned, an estimated 5-6 million m3 of ice were lost due to melting, volcanic gas emissions increased, and debris flows emerged repeatedly from recently formed ice holes near the 1990 dome, located on the crater’s N (“Drift”) side. On March 15, a phreatic explosion deposited non-juvenile ash from a new vent in the summit ice cap just S of the 1990 dome. Ash from the explosion rose to ~4500 m above sea level (asl). The plume was accompanied by weak seismicity. The first magmatic explosion occurred on March 22. Over the next two weeks, more than 19 explosions destroyed at least two lava domes and produced ash plumes that reached 6-18 km asl. Tephra was deposited along variable azimuths including trace to minor amounts on Anchorage and Kenai Peninsula communities, and reached Fairbanks, ~800 km to the N. Several lahars were produced by explosive disruption and melting of the “Drift” glacier. The largest lahars followed explosions on March 23 and April 4 and inundated the Drift River valley to the coast, causing temporary evacuation of the Drift River Oil Terminal, ~40 km from the vent. Time-lapse images captured pyroclastic flows and lahars in the “Drift” glacier valley during several of the explosions. Ballistics and pyroclastic flow deposits were

  7. Linking space observations to volcano observatories in Latin America: Results from the CEOS DRM Volcano Pilot

    Science.gov (United States)

    Delgado, F.; Pritchard, M. E.; Biggs, J.; Arnold, D. W. D.; Poland, M. P.; Ebmeier, S. K.; Wauthier, C.; Wnuk, K.; Parker, A. L.; Amelug, F.; Sansosti, E.; Mothes, P. A.; Macedo, O.; Lara, L.; Zoffoli, S.; Aguilar, V.

    2015-12-01

    Within Latin American, about 315 volcanoes that have been active in the Holocene, but according to the United Nations Global Assessment of Risk 2015 report (GAR15) 202 of these volcanoes have no seismic, deformation or gas monitoring. Following the 2012 Santorini Report on satellite Earth Observation and Geohazards, the Committee on Earth Observation Satellites (CEOS) has developed a 3-year pilot project to demonstrate how satellite observations can be used to monitor large numbers of volcanoes cost-effectively, particularly in areas with scarce instrumentation and/or difficult access. The pilot aims to improve disaster risk management (DRM) by working directly with the volcano observatories that are governmentally responsible for volcano monitoring, and the project is possible thanks to data provided at no cost by international space agencies (ESA, CSA, ASI, DLR, JAXA, NASA, CNES). Here we highlight several examples of how satellite observations have been used by volcano observatories during the last 18 months to monitor volcanoes and respond to crises -- for example the 2013-2014 unrest episode at Cerro Negro/Chiles (Ecuador-Colombia border); the 2015 eruptions of Villarrica and Calbuco volcanoes, Chile; the 2013-present unrest and eruptions at Sabancaya and Ubinas volcanoes, Peru; the 2015 unrest at Guallatiri volcano, Chile; and the 2012-present rapid uplift at Cordon Caulle, Chile. Our primary tool is measurements of ground deformation made by Interferometric Synthetic Aperture Radar (InSAR) but thermal and outgassing data have been used in a few cases. InSAR data have helped to determine the alert level at these volcanoes, served as an independent check on ground sensors, guided the deployment of ground instruments, and aided situational awareness. We will describe several lessons learned about the type of data products and information that are most needed by the volcano observatories in different countries.

  8. Xenoliths From Isla Isabel, Nayarit, Mexico: The Nature of the Upper Mantle Underneath the Western Part of the Mexican Volcanic Belt

    Science.gov (United States)

    Housh, T. B.; Aranda-Gomez, J. J.; Luhr, J. F.

    2007-12-01

    Isla Isabel is located ~65 km NW of San Blas (Nayarit), off the Pacific coast of central Mexico. The island is a Quaternary (Ar/Ar < 0.7 Ma) volcanic complex built atop attenuated continental crust. Isabel lies on the east side of the mouth of the Gulf of California, near the area previously occupied (early Pliocene) by Los Cabos Block. Southeast of Isabel, on the mainland, is the NW-trending Tepic-Zacoalco rift, a major volcano-tectonic structure in the western part of the Mexican Volcanic Belt. On land, the rift is the boundary between the Jalisco and Sierra Madre Occidental blocks, and Isabel lies along its projection. Immediately S of Isabel is the San Blas Trough, a swale that trends NW-SE, co-linear with a gravity lineation parallel to the Tamayo and San Blas fault zones, which are the transform boundaries between the northern Rivera and North American plates. Plio-Quaternary alkaline and calc-alkaline lavas have erupted contemporaneously in the Tepic-Zacoalco rift, but so far no mantle xenoliths have been reported in them. Isabel's rocks are intra-plate type alkaline basalts to trachybasalts, with 5-6%\\ normative Ne. Primary paragenesis in the lavas is: Ol + Pl + Cpx + TMt. Small (< 5 cm) peridotite xenoliths, and xenocrysts derived from them, are ubiquitous in the rocks. Eleven xenoliths were studied comprising 3 dunites, 7 harzburgites (one Pl-bearing), and 1 gabbro. Compared to other Mexican xenolith localities N of the MVB, they are refractory as they are depleted in, or lack, Cpx. Ol crystals in xenoliths are homogenous and their Mg#\\ s range as follows: peridotites (92-88), gabbro (84), and Pl-harzburgite (80). Cores of primary Ol phenocrysts (90.5-86.5) in Isabel's volcanic rocks are significantly higher in Mg#\\ s than in Ol from other Mexican xenolith localities (max. 86) and overlap with the associated peridotite xenoliths. Such overlap has not been reported for other Mexican xenolith localities. Xenolith equilibration temperatures for 5

  9. Chemical evolution of a pleistocene rhyolitic center: Sierra La Primavera, Jalisco, México

    Science.gov (United States)

    Mahood, Gail A.

    1981-06-01

    The late Pleistocene caldera complex of the Sierra La Primavera, Jalisco, México, contains well-exposed lava flows and domes, ash-flow tuff, air-fall pumice, and caldera-lake sediments. All eruptive units are high-silica rhyolites, but systematic chemical differences correlate with age and eruptive mode. The caldera-producing unit, the 45-km3 Tala Tuff, is zoned from a mildly peralkaline first-erupted portion enriched in Na, Rb, Cs, Cl, F, Zn, Y, Zr, Hf, Ta, Nb, Sb, HREE, Pb, Th, and U to a metaluminous last-erupted part enriched in K, LREE, Sc, and Ti; Al, Ca, Mg, Mn, Fe, and Eu are constant within analytical errors. The earliest post-caldera lava, the south-central dome, is nearly identical to the last-erupted portion of the Tala Tuff, whereas the slightly younger north-central dome is chemically transitional from the south-central dome to later, moremafic, ring domes. This sequence of ash-flow tuff and domes represents the tapping of progressively deeper levels of a zoned magma chamber 95,000 ± 5,000 years ago. Since that time, the lavas that erupted 75,000, 60,000, and 30,000 years ago have become decreasingly peralkaline and progressively enriched only in Si, Rb, Cs, and possibly U. They represent successive eruption of the uppermost magma in the post-95,000-year magma chamber. Eruptive units of La Primavera are either aphyric or contain up to 15% phenocrysts of sodic sanidine ≧quartz >ferrohedenbergite >fayalite>ilmenite±titanomagnetite. Whereas major-element compositions of sanidine, clinopyroxene, and fayalite phenocrysts changed only slightly between eruptive groups, concentrations of many trace elements changed by factors of 5 to 10, resulting in crystal/glass partition coefficients that differ by factors of up to 20 between successively erupted units. The extreme variations in partitioning behavior are attributed to small changes in bulk composition of the melt because major-element compositions of the phenocrysts and temperature, pressure, and

  10. Volcano Monitoring Using Google Earth

    Science.gov (United States)

    Cameron, W.; Dehn, J.; Bailey, J. E.; Webley, P.

    2009-12-01

    At the Alaska Volcano Observatory (AVO), remote sensing is an important component of its daily monitoring of volcanoes. AVO’s remote sensing group (AVORS) primarily utilizes three satellite datasets; Advanced Very High Resolution Radiometer (AVHRR) data, from the National Oceanic and Atmospheric Administration’s (NOAA) Polar Orbiting Satellites (POES), Moderate Resolution Imaging Spectroradiometer (MODIS) data from the National Aeronautics and Space Administration’s (NASA) Terra and Aqua satellites, and NOAA’s Geostationary Operational Environmental Satellites (GOES) data. AVHRR and MODIS data are collected by receiving stations operated by the Geographic Information Network of Alaska (GINA) at the University of Alaska’s Geophysical Institute. An additional AVHRR data feed is supplied by NOAA’s Gilmore Creek satellite tracking station. GOES data are provided by the Naval Research Laboratory (NRL), Monterey Bay. The ability to visualize these images and their derived products is critical for the timely analysis of the data. To this end, AVORS has developed javascript web interfaces that allow the user to view images and metadata. These work well for internal analysts to quickly access a given dataset, but they do not provide an integrated view of all the data. To do this AVORS has integrated its datasets with Keyhole Markup Language (KML) allowing them to be viewed by a number of virtual globes or other geobrowsers that support this code. Examples of AVORS’ use of KML include the ability to browse thermal satellite image overlays to look for signs of volcanic activity. Webcams can also be viewed interactively through KML to confirm current activity. Other applications include monitoring the location and status of instrumentation; near real-time plotting of earthquake hypocenters; mapping of new volcanic deposits using polygons; and animated models of ash plumes, created by a combination of ash dispersion modeling and 3D visualization packages.

  11. Scutellaria cuevasiana and Scutellaria sublitoralis (Lamiaceae, two new species from Jalisco and Nayarit, Mexico Scutellaria cuevasiana y Scutellaria sublitoralis (Lamiaceae, dos especies nuevas de Jalisco y Nayarit, México

    Directory of Open Access Journals (Sweden)

    Jesús Guadalupe González-Gallegos

    2013-03-01

    Full Text Available Scutellaria cuevasiana J. G. González et A. Vázquez and Scutellaria sublitoralis J. G. González are described and illustrated. Scutellaria cuevasiana fits best within section Uliginosae (Epling Epling. It is morphologically close to S. blepharophylla Epling, S. rosei Fernald and S. seleriana Loes. It differs from them by its magenta corollas, small and sessile floral bracts, longer petioles and bigger leaves. Scutellaria sublitoralis does not manifest any clear morphological affinity with species of the sections enumerated by Epling. It could be related to species in sections Pallidiflorae Epling or Uliginosae, particularly with the "Scutellaria ovata" or "Scutellaria caerulea" species groups defined by Paton. It is morphologically similar to S. pallidiflora Epling; however, it can be recognized by wider leaves with usually cordate to subcordate bases, persistent floral bracts, floral axis and calyces without glandular-capitate hairs, longer corollas, and narrower toward the throat.Se describen e ilustran Scutellaria cuevasiana J. G. González et A. Vázquez y Scutellaria sublitoralis J. G. González. Scutellaria cuevasiana se ajusta mejor a la sección Uliginosae (Epling Epling; es cercana en su morfología a S. blepharophylla Epling, S. rosei Fernald y S. seleriana Loes. Difiere de las mismas debido a sus corolas magenta, brácteas florales más pequeñas y sésiles, peciolos más largos y hojas más grandes. Scutellaria sublitoralis no muestra una clara afinidad con las especies de las secciones establecidas por Epling; podría estar relacionada con las especies de las secciones Pallidiflorae Epling o Uliginosae, particularmente con los grupos de especies de "Scutellaria ovata" y "Scutellaria caerulea" definidos por Paton. Es morfológicamente similar a S. pallidiflora Epling; sin embargo, puede reconocerse por sus hojas más anchas con bases por lo usual cordadas a subcordadas, brácteas florales persistentes, eje floral y cálices sin tricomas capitado-glandulares, corolas más largas, y estrechas hacia el ápice.

  12. Prevalence and risk factors for brucellosis in goats in areas of Mexico with and without brucellosis control campaign.

    Science.gov (United States)

    Oseguera Montiel, David; Frankena, Klaas; Udo, Henk; Keilbach Baer, Nícola Maria; van der Zijpp, Akke

    2013-08-01

    Brucellosis is a major constraint for small-scale goat farming systems in Mexico. This study estimated the prevalence of testing positive to brucellosis and identified and quantified risk factors in goats from small-scale farms of Michoacán that had participated in a brucellosis campaign (i.e. vaccination, serological testing, culling and awareness) and of Jalisco that had negligible brucellosis campaign participation. A cross-sectional serological survey was conducted among 1,713 goats of 83 flocks. The prevalence of testing positive to brucellosis was higher (38%) in Jalisco than in Michoacán (11%). Logistic regression analysis indicated that goats from Michoacán had lower odds to test positive for brucellosis (odds ratio (OR) = 0.32, 95% confidence interval (CI) 0.21-0.48) compared to goats from Jalisco. Goats in zero-grazing systems had lower odds than goats in grazing systems (OR = 0.22, 95% CI 0.09-0.57). When goats were kept in pens with low density (0.002 to 0.22 goat/m(2)), odds was lower (OR = 0.44, 95% CI 0.28-0.67) compared to goats kept in pens with higher density (0.23 to 1 goat/m(2)). Odds was higher for testing positive when farmers bought goats from goat traders (OR = 1.82, 95% CI 1.15-2.87) compared to farmers who did not. If scavenger poultry had access to goat pens, the odds was half (OR = 0.52, 95% CI 0.33-0.83) of those where poultry had no access. Regular disinfection of the pen reduced the odds (OR = 0.66, 95% CI 0.44-0.99) compared to where disinfection was not regular. The brucellosis control campaign was effective in reducing brucellosis seropositivity.

  13. Lahar hazards at Agua volcano, Guatemala

    Science.gov (United States)

    Schilling, S.P.; Vallance, J.W.; Matías, O.; Howell, M.M.

    2001-01-01

    At 3760 m, Agua volcano towers more than 3500 m above the Pacific coastal plain to the south and 2000 m above the Guatemalan highlands to the north. The volcano is within 5 to 10 kilometers (km) of Antigua, Guatemala and several other large towns situated on its northern apron. These towns have a combined population of nearly 100,000. It is within about 20 km of Escuintla (population, ca. 100,000) to the south. Though the volcano has not been active in historical time, or about the last 500 years, it has the potential to produce debris flows (watery flows of mud, rock, and debris—also known as lahars when they occur on a volcano) that could inundate these nearby populated areas.

  14. Volcanoes muon imaging using Cherenkov telescopes

    CERN Document Server

    Catalano, Osvaldo; Mineo, Teresa; Cusumano, Giancarlo; Maccarone, Maria Concetta; Pareschi, Giovanni

    2015-01-01

    A detailed understanding of a volcano inner structure is one of the key-points for the volcanic hazards evaluation. To this aim, in the last decade, geophysical radiography techniques using cosmic muon particles have been proposed. By measuring the differential attenuation of the muon flux as a function of the amount of rock crossed along different directions, it is possible to determine the density distribution of the interior of a volcano. Up to now, a number of experiments have been based on the detection of the muon tracks crossing hodoscopes, made up of scintillators or nuclear emulsion planes. Using telescopes based on the atmospheric Cherenkov imaging technique, we propose a new approach to study the interior of volcanoes detecting the Cherenkov light produced by relativistic cosmic-ray muons that survive after crossing the volcano. The Cherenkov light produced along the muon path is imaged as a typical annular pattern containing all the essential information to reconstruct particle direction and energ...

  15. Radial anisotropy ambient noise tomography of volcanoes

    Science.gov (United States)

    Mordret, Aurélien; Rivet, Diane; Shapiro, Nikolai; Jaxybulatov, Kairly; Landès, Matthieu; Koulakov, Ivan; Sens-Schönfelder, Christoph

    2016-04-01

    The use of ambient seismic noise allows us to perform surface-wave tomography of targets which could hardly be imaged by other means. The frequencies involved (~ 0.5 - 20 s), somewhere in between active seismic and regular teleseismic frequency band, make possible the high resolution imaging of intermediate-size targets like volcanic edifices. Moreover, the joint inversion of Rayleigh and Love waves dispersion curves extracted from noise correlations allows us to invert for crustal radial anisotropy. We present here the two first studies of radial anisotropy on volcanoes by showing results from Lake Toba Caldera, a super-volcano in Indonesia, and from Piton de la Fournaise volcano, a hot-spot effusive volcano on the Réunion Island (Indian Ocean). We will see how radial anisotropy can be used to infer the main fabric within a magmatic system and, consequently, its dominant type of intrusion.

  16. A field guide to Newberry Volcano, Oregon

    Science.gov (United States)

    Jenson, Robert A.; Donnelly-Nolan, Julie M.; McKay, Daniele

    2009-01-01

    Newberry Volcano is located in central Oregon at the intersection of the Cas