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Sample records for andes mendoza province

  1. Payenia volcanic province, southern Mendoza, Argentina

    DEFF Research Database (Denmark)

    Søager, Nina; Holm, Paul Martin; Llambias, Eduardo Jorge

    2013-01-01

    The Pleistocene to Holocene Payenia volcanic province is a backarc region of 60,000 km2 in Mendoza, Argentina, which is dominated by transitional to alkaline basalts and trachybasalts. We present major and trace element compositions of 139 rocks from this area of which the majority are basaltic...

  2. Quaternary Glaciations in the Rio Mendoza Valley, Argentine Andes

    Science.gov (United States)

    Espizua, Lydia E.

    1993-09-01

    In the Rio Mendoza valley, five Pleistocene drifts and one Holocene drift are distinguished by multiple relative-age criteria, including surface-rock weathering, development of rock varnish, moraine morphology, soil-profile development, and stratigraphic relationships. Several absolute ages suggest a preliminary chronology. During the oldest (Uspallata) glaciation, a system of valley glaciers flowed 110 km from the Andean drainage divide and 80 km from Cerro Aconcagua to terminate at 1850 m. Drift of this ice advance is older than a widespread tephra dated by fission-track at 360,000 ± 36,000 yr. During the Punta de Vacas advance, ice terminated at 2350 m, while during the subsequent Penitentes advance, the glacier system ended at 2500 m. A travertine layer overlying Penitentes Drift has U-series age of 24,200 ± 2000 yr B.P. The distribution of Horcones Drift, which is inferred to represent the last glacial maximum, delimits an independent ice stream that flowed 22 km down Horcones valley to 2750 m. A later readvance (Almacenes) reached 3250 m. Confluencia Drift is considered to be Neoglacial in age and extends downvalley to 3300 m. The moraine sequence is compared with those studied by Caviedes (1972) along Rio Aconcagua on the Chilean flank of the Andes.

  3. 75 FR 36347 - Determination of Pest-Free Areas in Mendoza Province, Argentina; Request for Comments

    Science.gov (United States)

    2010-06-25

    ... Animal and Plant Health Inspection Service Determination of Pest-Free Areas in Mendoza Province... Argentina asked that we recognize the Southern and Central Oases in the southern half of Mendoza Province as... southern half of Mendoza Province meet the criteria of Sec. 319.56-5(a) and (b) with respect to freedom...

  4. 76 FR 51934 - Determination of Pest-Free Areas in Mendoza Province, Argentina; Request for Comments

    Science.gov (United States)

    2011-08-19

    ... Animal and Plant Health Inspection Service Determination of Pest-Free Areas in Mendoza Province... half of Mendoza Province as an area that is free of Medfly. In accordance with our process, we... in the area. The second commenter provided information to support a finding that the Mendoza Province...

  5. 76 FR 80870 - Notice of Determination of Pest-Free Areas in Mendoza Province, Argentina

    Science.gov (United States)

    2011-12-27

    ... Animal and Plant Health Inspection Service Notice of Determination of Pest-Free Areas in Mendoza Province... the public that we are recognizing the Southern and Central Oases in the southern half of Mendoza... information to support a finding that the Mendoza Province is free of the South American ] fruit fly...

  6. Les variations glaciaires dans les Andes de Mendoza (Argentine entre 1975 et 2007

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    Étienne Cossart

    2010-05-01

    Full Text Available Le suivi des glaciers constitue un enjeu essentiel pour l’organisation des sociétés et le fonctionnement des milieux montagnards. Dans la mesure où les glaciers influencent fortement le régime des cours d’eau, et donc les stratégies d’irrigation, leur disparition peut remettre en cause de nombreux usages liés à l’eau. Or, si nombre de glaciers sont étudiés individuellement, des méthodes permettant d’effectuer des suivis de l’englacement à l’échelle régionale manquent. Nous proposons donc ici une méthode, fondée sur la reconstitution de champs d’altitudes de la Ligne d’Équilibre Glaciaire, aboutissant à la réalisation de cartes diachroniques régionales. Nous synthétisons ainsi les variations glaciaires depuis 30 ans sur l’ensemble d’un secteur de plusieurs milliers de kilomètres carr��s : les Andes de Mendoza (Argentine.

  7. Chaco ansilta new species from Mendoza province, Western Argentina (Araneae: Nemesiidae

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    NELSON FERRETTI

    2014-12-01

    Full Text Available A new species of Chaco Tullgren, 1905 is described and illustrated from the Andean foothills of Mendoza province, western Argentina. This is the tenth species of the genus and the first record of Chaco in Mendoza. An updated key is presented for all Chaco species. The cladistic analysis based on a previously published morphological character matrix resulted in the consensus tree: (C. obscura, C. tucumana, C. castanea, (C. socos + C. tigre (C. tecka (C. sanjuanina (C. Patagonia + C. ansilta sp. nov..

  8. Darwin's observation in South America: what did he find at agua de la zorra, Mendoza province?

    OpenAIRE

    Stella Poma; Vanesa D Litvak; Magdalena Koukharsky; E. Beatriz Maisonnave; Sonia Quenardelle

    2009-01-01

    Scarcely 23 km from Uspallata, along the track of the old national highway 7, lies the district of Agua de la Zorra, in Mendoza province in western Argentina. Charles Darwin visited the area during his South American journeys in the 19th century and discovered a geological sequence that contained a paleoflora never described before. The flora includes an important number of species, particularly what is considered a small conifer forest with many silicified trunks still in life position. Darw...

  9. Primer registro de Tityus trivittatus (Scorpiones: Buthidae en la provincia de Mendoza (Argentina First record of Tityus trivittatus (Scorpiones: Buthidae in Mendoza province (Argentina

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    Florencia Fernández Campón

    2009-06-01

    Full Text Available En la siguiente nota se informa sobre el primer registro del escorpión Tityus trivittatus Kraepelin en la provincia de Mendoza en el Barrio Campo Papa, departamento de Godoy Cruz. T trivittatus es dentro de nuestro país una de las especies de escorpiones con importancia médica, debido a que su veneno neurotóxico puede causar lesiones en el sistema nervioso y en algunos casos la muerte, particularmente en niños.This note reports the first record on the scorpion Tityus trivittatus Kraepelin in Mendoza province in the locality of Campo Papa, Godoy Cruz. T. trivittatus is one of the species of scorpion of medical importance in Argentina, due to the fact that its neurotoxic venom can damage the nervous system and may even be fatal in some cases, especially among children.

  10. A new species of Liolaemus (Reptilia: Squamata: Tropiduridae from Mendoza province, Argentina

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    Etheridge, Richard

    2001-05-01

    Full Text Available Una nueva especie del complejo Liolaemus darwinii es descrita para el centro de la provincia de Mendoza, Argentina. Se parece más a L. olongasta y L. laurenti en que los machos adultos tienen pigmento negro en el pliegue antehumeral y manchas escapulares que no son agrandadas. Difiere de estas especies en tener un cuerpo adulto menor, un número mayor de escamas en la mitad del cuerpo, una cola más corta y un mayor número de poros precloacales en machos, y un patrón ventral distinto en machos adultos. En el norte de su distribución se encuentra L. darwinii en el norte de la provincia de Mendoza y en la provincia de San Luis, y en el sur en el oeste de la provincia de La Pampa, en el noroeste de la provincia de Neuquén y en la provincia de Río Negro, pero se desconoce si estas poblaciones del norte y del sur de L. darwtnii están separadas por la distribución de la nueva especie. Análisis cladísticos basados en comportamiento, morfología y secuencias de DNA muestran filogenias conflictivas, pero concuerdan en que la nueva especie es un miembro del grupo boulengeri, con afinidades más cercanas a L. darwinii, L. olongasta y L. laurenti. A new species,of the Liolaemus darwinii complex is described from central Mendoza Province, Argentina. It most closely resembles L. olongasta and L. laurenti in that adult males have black pigment in the antehumeral fold and scapular spots that are not enlarged. It differs from these species in having a smaller adult body size, a higher number of midbody scales, a shorter tail, more precloacal pores in males, and a different adult male ventral body pattern. Its range is bordered by L. darwinii on the north in northern Mendoza and San Luis provinces, and on the south in western La Pampa and northwestern Neuquén and Río Negro provinces, but it is unknown whether these northern and southern populations of L. darwinii are separated by the range of the new species. Cladistic analyses based on behaviour

  11. Detection of Slope Instabilities Along the National Road 7, Mendoza Province, Argentina, Using Multi-Temporal InSAR

    Science.gov (United States)

    Michoud, Clément; Derron, Marc-Henri; Baumann, Valérie; Jaboyedoff, Michel; Rune Lauknes, Tom

    2013-04-01

    About 2'230 vehicles per day pass through the National Road 7 that link Buenos Aires to Santiago de Chile, crossing Andes Cordillera. This extremely important corridor, being the most important land pass between Argentina and Chile, is exposed to numerous natural hazards, such as snow avalanches, rockfalls and debris flows and remains closed by natural hazards several days per year. This goal of this study is to perform a regional mapping of geohazard susceptibilities along the Road 7 corridor, as started by Baumann et al. (2005), using modern remote sensing and numerical approaches with field checking. The area of interest is located in the Mendoza Province, between the villages Potrerillos and Las Cuevas near the Chilean border. The diversity of soil and rock conditions, the active geomorphological processes associated to post-glacial decompression, seasonal freeze and thaw and severe storms along the road corridor, increase the risk to natural hazard. With the support of the European Space Agency (ESA Category-1 Project 7154), we have in this study processed a large number of ERS and Envisat ASAR scenes, covering the period from 1995 to 2000. We applied both the small-baseline (SB) and the persistent scatterer (PSI) multi-temporal interferometric SAR (InSAR) techniques. The study area contains sparse vegetation, and the SB InSAR method is therefore well suited to map the area containing mainly distributed scatterers. Furthermore, PSI algorithms are also used for comparison for selected landslides in the inventory. Both approaches show a relatively good coherence within mountain areas, which is a good point for the landslide detections along the road. Indeed, the authors identified several large slope instabilities even active scree deposits. This inventory is finally compared with field observations and with existing susceptibility maps regarding snow avalanches, debris-flows and rockfalls. The final objective of this project is to develop a risk strategy that

  12. Radial patterns of bitumen dykes around Quaternary volcanoes, provinces of northern Neuquén and southernmost Mendoza, Argentina

    Science.gov (United States)

    Cobbold, Peter R.; Ruffet, Gilles; Leith, Leslie; Loseth, Helge; Rodrigues, Nuno; Leanza, Hector A.; Zanella, Alain

    2014-12-01

    Where the Neuquén Basin of Argentina abuts the Andes, hundreds of veins of solid hydrocarbon (bitumen) are visible at the surface. Many of these veins became mines, especially in the last century. By consensus, the bitumen has resulted from maturation of organic-rich shales, especially the Vaca Muerta Fm of Late Jurassic age, but also the Agrio Fm of Early Cretaceous age. To account for their maturation, recent authors have invoked regional subsidence, whereas early geologists invoked magmatic activity. During 12 field seasons (since 1998), we have tracked down the bitumen localities, mapped the veins and host rocks, sampled them, studied their compositions, and dated some of them. In the provinces of northern Neuquén and southernmost Mendoza, the bitumen veins are mostly sub-vertical dykes. They tend to be straight and continuous, crosscutting regional structures and strata of all ages, from Jurassic to Palaeocene. Most of the localities lie within 70 km of Tromen volcano, although four are along the Rio Colorado fault zone and another two are at the base of Auca Mahuida volcano. On both volcanic edifices, lavas are of late Pliocene to Pleistocene age. Although regionally many of the bitumen dykes tend to track the current direction of maximum horizontal tectonic stress (ENE), others do not. However, most of the dykes radiate outward from the volcanoes, especially Tromen. Thicknesses of dykes tend to be greatest close to Tromen and where the host rocks are the most resistant to fracturing. Many of the dykes occur in the exhumed hanging walls of deep thrusts, especially at the foot of Tromen. Here the bitumen is in places of high grade (impsonite), whereas further out it tends to be of medium grade (grahamite). A few bitumen dykes contain fragments of Vaca Muerta shale, so that we infer forceful expulsion of source rock. At Curacó Mine, some shale fragments contain bedding-parallel veins of fibrous calcite (beef) and these contain some bitumen, which is

  13. Petrology and mineralogy of the La Peña igneous complex, Mendoza, Argentina: An alkaline occurrence in the Miocene magmatism of the Southern Central Andes

    Science.gov (United States)

    Pagano, Diego Sebastián; Galliski, Miguel Ángel; Márquez-Zavalía, María Florencia; Colombo, Fernando

    2016-04-01

    The La Peña alkaline igneous complex (LPC) is located in the Precordillera (32°41‧34″ S - 68°59‧48″ W) of Mendoza province, Argentina, above the southern boundary of the present-day flat-slab segment. It is a 19 km2 and 5 km diameter subcircular massif emplaced during the Miocene (19 Ma) in the Silurian-Devonian Villavicencio Fm. The LPC is composed of several plutonic and subvolcanic intrusions represented by: a cumulate of clinopyroxenite intruded by mafic dikes and pegmatitic gabbroic dikes, isolated bodies of malignite, a central intrusive syenite that develops a wide magmatic breccia in the contact with clinopyroxenite, syenitic and trachytic porphyries, a system of radial and ring dikes of different compositions (trachyte, syenite, phonolite, alkaline lamprophyre, tephrite), and late mafic breccias. The main minerals that form the LPC, ordered according to their abundance, are: pyroxene (diopside, hedenbergite), calcium amphibole (pargasite, ferro-pargasite, potassic-ferro-pargasite, potassic-hastingsite, magnesio-hastingsite, hastingsite, potassic-ferro-ferri-sadanagaite), trioctahedral micas (annite-phlogopite series), plagioclase (bytownite to oligoclase), K-feldspar (sanidine and orthoclase), nepheline, sodalite, apatite group minerals (fluorapatite, hydroxylapatite), andradite, titanite, magnetite, spinel, ilmenite, and several Cu-Fe sulfides. Late hydrothermal minerals are represented by zeolites (scolecite, thomsonite-Ca), epidote, calcite and chlorite. The trace element patterns, coupled with published data on Sr-Nd-Pb isotopes, suggest that the primary magma of the LPC was generated in an initially depleted but later enriched lithospheric mantle formed mainly by a metasomatized spinel lherzolite, and that this magmatism has a subduction-related signature. The trace elements pattern of these alkaline rocks is similar to other Miocene calc-alkaline occurrences from the magmatic arc of the Southern Central Andes. Mineral and whole

  14. Historical Glacier Variations in Southern South America since the Little Ice Age: Examples from Lago Viedma (Southern Patagonia) and Mendoza (Central Andes), Argentina

    Science.gov (United States)

    Nussbaumer, S. U.; Masiokas, M.; Pitte, P.; Berthier, E.; Guerrido, C.; Luckman, B. H.; Villalba, R.

    2013-12-01

    The evaluation of historical information can give valuable insight into past glacier dynamics, especially before the onset of modern measurements. Early photographs and maps depict changes for selected glaciers in southern South America. Within this study, written documents and pictorial historical records (drawings, sketches, engravings, photographs, chronicles, topographic maps) are analysed critically, with a particular focus on two regions: Lago Viedma (El Chaltén, southern Patagonia, 49.5°S, 73.0°W) and the Río Mendoza basin (Mendoza, central Andes, 33.1°S, 69.9°W). For the Lago Viedma area, early historical data for the end of the 19th century stem from the expedition of the Chilean-Argentinean border commission. In addition, the expedition by the German Scientific Society, conducted between 1910 and 1916, and the later photographs by Alberto M. de Agostini give an excellent depiction of the glaciers. Glaciar Viedma is a calving glacier which shows distinct retreat from 1896 until the present (though with a stationary or possibly advancing glacier front between 1930/31 and 1951/52), similar to the neighbouring glaciers. On the contrary, nearby Glaciar Perito Moreno shows an exceptional behaviour: the glacier front has been advancing during the first half of the 20th century, staying in an advanced position until the present. At the beginning of the 20th century, Robert Helbling explored the Argentinean-Chilean Andes together with his friend Friedrich Reichert. In the summer of 1909/10, they started a detailed survey of the highly glacierized Juncal-Tupungato mountains (Río Mendoza basin), leading to the first accurate topographic map of the area published in 1914. Its outstanding quality allows a comparison with contemporary satellite imagery. The area received attention in 1934, when the sudden drainage of a glacier-dammed lake in the upper Río del Plomo valley caused fatalities and considerable damage to constructions and the Transandine Railway. A

  15. Darwin's observation in South America: what did he find at agua de la zorra, Mendoza province?

    Directory of Open Access Journals (Sweden)

    Stella Poma

    2009-04-01

    Full Text Available Scarcely 23 km from Uspallata, along the track of the old national highway 7, lies the district of Agua de la Zorra, in Mendoza province in western Argentina. Charles Darwin visited the area during his South American journeys in the 19th century and discovered a geological sequence that contained a paleoflora never described before. The flora includes an important number of species, particularly what is considered a small conifer forest with many silicified trunks still in life position. Darwin described and interpreted the sequence as sedimentary; his records show a very detailed level of observation. He also wondered about the processes that would cause the burial of the paleoflora, which he considered had happened in a marine sedimentary environment. In the modern geological framework and after a detailed study of the rocks containing the trunks, it is now interpreted that the conifer forest was buried by pyroclastic flows. Darwin accurately described the fine volcanic materials as an essential part of the deposit, but the key of the enigma about the origin of the deposits and the burial of the forest is the identification of the pyroclastic flow features; these were unknown process at the time of Darwin´s observations and interpretation.

  16. Paleomagnetism of Upper Triassic rocks in the Los Colorados hill section, Mendoza province, Argentina

    Science.gov (United States)

    Vizán, Haroldo; Ixer, Robert; Turner, Peter; Cortés, José María; Cladera, Gerardo

    2004-12-01

    Different authors have highlighted a systematic disagreement between Late Carboniferous-Triassic paleomagnetic poles (PPs) for Gondwanaland and Laurasia when they are repositioned in a classical reconstruction prior to the breakup of Pangea A. This disagreement has been interpreted in geodynamic terms or as an evidence of non-dipole components of the geomagnetic field. Such analyses have been made using data on South American PPs published approximately 25 years ago and obtained using outdated methodologies. In this article, the authors present new Late Triassic paleomagnetic data from rocks that crop out in the Pre-Andean ranges (Precordillera) of Mendoza province (Argentina). Samples of different lithologies were taken from two limbs of a doubly plunging syncline, and several field tests of paleomagnetic stability were applied. The results indicate primary site mean directions that yield a PP with geographic coordinates and statistical parameters as follows: Lat.=76°S, Lon.=280°E, N=12, R=11.63, α95=8°, K=30.2. This PP agrees with mean PPs of Laurasia of similar ages in different models of Pangea A, indicating that the hypothesis of a dipolar paleomagnetic field could be valid for the Late Triassic.

  17. Molecular characterization of cryptic and sympatric lymnaeid species from the Galba/Fossaria group in Mendoza Province, Northern Patagonia, Argentina

    Science.gov (United States)

    2013-01-01

    Background Freshwater lymnaeid snails can act as the intermediate hosts for trematode parasites such as the liver fluke Fasciola hepatica, that cause significant economic and biomedical burden worldwide, particularly through bovine fascioliasis. Transmission potential is tightly coupled to local compatibility with snail hosts, so accurate identification of lymnaeid species is crucial for understanding disease risk, especially when invasive species are encountered. Mendoza Province, in Argentina, is a center of livestock production and also an area of endemic fascioliasis transmission. However, the distribution of lymnaeid species in the region is not well known. Methods This study examined lymnaeid snails from seven localities in the Department of Malarguë, Mendoza Province, using morphological and molecular analyses and also describing ecological variables associated with snail presence. Results While morphological characters identified two species of lymnaeid, Galba truncatula and G. viatrix, molecular data revealed a third, cryptic species, G. neotropica, which was sympatric with G. viatrix. G. truncatula was exclusively found in high altitude (>1900 meters above sea level [masl]) sites, whereas mixed G. neotropica/G. viatrix localities were at middle elevations (1300–1900 masl), and G. viatrix was found alone at the lowest altitude sites (variables while avoiding nomenclature redundancy. As the three species observed here, including one alien invasive species, are considered hosts of varying susceptibility to Fasciola parasites, and given the economic importance of fascioliasis for livestock production, this research has critical importance for the ultimate aim of controlling disease transmission. PMID:24499569

  18. Darwin's observation in South America: what did he find at agua de la zorra, Mendoza province? Las observaciones de Darwin en Sudamérica: ¿Qué encontró en Agua de la Zorra, provincia de Mendoza?

    OpenAIRE

    Stella Poma; Vanesa D Litvak; Magdalena Koukharsky; E. Beatriz Maisonnave; Sonia Quenardelle

    2009-01-01

    Scarcely 23 km from Uspallata, along the track of the old national highway 7, lies the district of Agua de la Zorra, in Mendoza province in western Argentina. Charles Darwin visited the area during his South American journeys in the 19th century and discovered a geological sequence that contained a paleoflora never described before. The flora includes an important number of species, particularly what is considered a small conifer forest with many silicified trunks still in life position. Darw...

  19. The Northern and Central Oases of the Province of Mendoza (Argentina): water resources and sustainability challenges

    OpenAIRE

    Salatino, Santa E.; Morabito, José; Lavie, Emilie

    2013-01-01

    International audience; Pendant les dernières décennies du 20ème siècle, les oasis de Mendoza, au coeur de la diagonale aride sudaméricaine, ont connu de profondes mutations de leur modèle socio-économique, fondé sur l'agriculture et les industries agro-alimentaires. La mondialisation, Mendoza l'a connue assez brutalement : la crise économique du Mercosur des années 2000 - suivant de près celle des marchés asiatiques (1997-98) - a entrainé un afflux massif d'investissements internationaux, ma...

  20. Oxfordian reef architecture of the La Manga Formation, Neuquén Basin, Mendoza Province, Argentina

    Science.gov (United States)

    Palma, Ricardo M.; Kietzmann, Diego A.; Adamonis, Susana; Gómez, José López

    2009-11-01

    The Neuquén back-arc basin is located on the west margin of the South American platform between latitudes 36° and 40° S. The basin is famous for its continuous sedimentary record from the Late Triassic to Cenozoic comprising continental and marine clastic, carbonate, and evaporitic deposits up to 2.600 m in thickness. The stratigraphical and paleontological studies of the outcrops of the La Manga Formation, Argentina, located near the Bardas Blancas region, Mendoza province (35° S and 69° O) allow the reconstruction of the sedimentary environments of an Oxfordian carbonate ramp, where outer ramp, middle ramp, inner ramp (oolitic shoal), inner ramp margin (patch reef) lagoon and paleokarst were differentiated. The reefs consist of back reef facies and insitu framework of coral boundstones that was formed at the top of shallowing-upward succession. Coral reefs were analyzed by defining coral colonies shapes, paleontological content, coral diversity and taphonomy studies. In some studied sections abundant fragments of gryphaeids, encrusting bryozoans, and isolated sponges provided a suitable substrate for coral colonization; however, other sections show an increase in the proportions of ooids, peloidal and coral intraclasts. The core reef facies is composed of white-grey unstratified and low diversity scleractinian coral limestone dominated by robust and thinly branching corals with cerioid-phocoid growths and massive coral colonies with meandroid-thamnasteroid growth forms. The assemblage is characterized by Actinastraea sp., Australoseris sp., Thamnasteria sp. and Garateastrea sp. Internal facies organization and different types of coral colonies allow to recognize the development of varying framework as well as intercolony areas. A superstratal growth fabric characterizes the coral assemblage. On the basis of coral growth fabric (branche and domal types), the reef of La Manga Formation is considered a typical mixstones. The intercolony areas consist of

  1. Deciphering the geochemical and mineralogical changes of a Miocene sedimentary basin infill, Mendoza Province, Argentina

    Science.gov (United States)

    Hunger, Gabriel; Moscariello, Andrea; Ventra, Dario

    2017-04-01

    low to moderate weathering values (CIA = 45-65) and shows the evolution of the composition towards the illite pole, in agreement with the QEMSCAN results. The evolution of the source rock composition shows a trend towards more mafic sources. La Pilona Fm. is characterized by more scarce composition certainly due to the advance of the thrust front coupled with inputs from the uplifting Frontal Cordillera, a tectonic province feeding the basin with different igneous sources. The integration of heavy mineral and isotopic data to constrain the source area changes will also allow us to have a better understanding of the evolution of the uplifting Andes.

  2. Evidencias de la zona de contacto entre los terrenos de Precordillera y Pie de Palo, Provincias de San Juan y Mendoza Evidence of the contact area between Precordillera and Pie de Palo terranes, Provinces of San Juan and Mendoza.

    Directory of Open Access Journals (Sweden)

    Maximiliano García Torrejón

    2011-12-01

    Full Text Available Se realizó un estudio gravimétrico en la región norte de la cuenca Cuyana, entre las provincias de San Juan y Mendoza. Mediante relaciones de gradientes gravimétricos tales como señal analítica, Tilt y fase del Tilt, se observó un marcado gradiente, que fue interpretado como un cambio lateral de litologías, que coincidiría con el área de una probable paleosutura del margen proto-andino, que separa en el terreno compuesto de Cuyania, al terreno de Precordillera con el terreno de Pie de Palo.We made the study in the northern Cuyo basin, between the provinces of San Juan and Mendoza. in the present work we show the results of gravimetric processing data from this basin and surrounding region. We applied anomaly-enhancement techniques such as analytic signal, tilt and phase of tilt. This allowed the observation of a marked gradient, which was interpreted as a lateral variation in lithology, which would coincides with the area of paleosuture of the proto-Andean margin, which separates in the Cuyania composite terrane the Precordillera from the Pie de Palo terranes.

  3. Analysis of the potential production and the development of bioenergy in the province of Mendoza - Bio-fuels and biomass - Using geographic information systems

    Energy Technology Data Exchange (ETDEWEB)

    Flores Marco, Noelia; Hilbert, Jorge Antonio [Instituto de Ingenieria Rural, INTA Las Cabanas y Los Reseros s/n, CP: 1712 Castelar, Buenos Aires (Argentina); Silva Colomer, Jorge [INTA EEA Junin Mendoza, Carril Isidoro Busquets s/n CP: 5572 (Argentina); Anschau, Renee Alicia; Carballo, Stella [Instituto de Clima y Agua, INTA. Las Cabanas y Los Reseros s/n, CP:1712 Castelar, Buenos Aires (Argentina)

    2010-06-15

    In this work, the partial results of the potential production of energy, starting from the biomass and the development of the crops, directed to the production of bio-fuels (Colza and Topinamur) in the North irrigation oasis of Mendoza, Argentina within the National Program of Bio-energy developed by INTA is presented. For the evaluation of the bio-energetic potential, derived from the biomass, the WISDOM methodology developed by FAO and implemented by INTA in Argentina was applied with the collaboration of national and provincial governmental entities that contribute local information The study of the potential production and the development of the bio-energetic crops have been carried out with the advising and participation of the experts of INTA of the studied crops. The province of Mendoza has semi-deserted agro-climatic characteristics. The type of soil and type of weather allows the production of great quality fruits and vegetables in the irrigated areas. The four great currents of water conform three oasis; Northeast, Center and South, which occupy the 3.67% of the surface of Mendoza. Today, Mendoza has 267,889 irrigated hectares, but the surface that was farmed by irrigation was near to the 400,000 ha. The climate contingencies, froze and hailstorm precipitations, plus the price instability cause great losses in the productive sector, taking it to the forlornness of the exploitations. The crop setting of these forlornness lands with crops directed to the production of bio-fuels and the utilization of the biomass coming from the agriculture activities and the agro industry (pruning of fruit trees, refuses of olive and vine, remnants of the peach industry, etc.) could assist the access to the energy in the rural areas, stimulating the economical improvement and the development in these communities. (author)

  4. First Late Triassic Record of a Paleoentomofauna from South America(Malargüe Basin,Mendoza Province,Argentina)

    Institute of Scientific and Technical Information of China (English)

    Carsten BRAUCKMANN; Oscar F.GALLEGO; Norbert HAUSCHKE; Rafael G.MARTINS-NETO; Elke GROENING; Jan-M.ILGER; María B.LARA

    2010-01-01

    Late Middle Triassic to early Late Triassic insects from Argentina have been previously described from the Bermejo and Cuyana Basins where they have been recovered from the Ischichuca-Los Rastros and Potrerillos-Cacheuta Formations,respectively.The insect fauna discussed herein was collected during field studies in 1986/1987 from the Llantenes section(Norian to Rhaetian? Late Triassic),which is situated in the Malargtie Basin in southern Mendoza province.The insect remains were found in the upper part of the Llantenes section(Llantenes Formation),which is built up of two coarsening-upwards cycles reflecting a deltaic progradation of a fluvial into a lacustrine environment(lower part),succeeded by repeated progradations into a floodplaindominated environment(upper part; with finds of insects,conchostracans,fish remains,plant fragments,and drifted logs).The new finds represent the youngest Triassic insect records described from Argentina and even from South America in its entirety.There is only one contemporaneous fossil assemblage in Gondwana:in the Clarence/Moreton Basin(Aberdare Conglomerate; Late Norian)in Australia.The new Triassic insects include an impression of an isolated Mecopterida-like wing(Mendozachorista volkheimeri gen.et sp.nov.;Mendozachoristidae fam.nov.),coleopteran elytra of the Permosynidae(Ademosyne rosenfeldi sp.nov.and Ademosyne llantenesensis sp.nov.)and other isolated body fragments.This new Late Triassic entomofauna from Argentina is of considerable importance in the reconstruction of the biotic recovery of continental environments in Gondwana after the catastrophic mass extinction at the P/T boundary.

  5. Mendoza, Argentina. El terremoto de 1861 como disparador del cambio de representación social de la identidad de una ciudad al pie de los Andes

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    Jorge Ricardo Ponte

    2007-12-01

    Full Text Available The definition of a town´s identity is a contemporary problematic. The process of economic globalization, far from devastating with the regional or national particularities seems to have exacerbated them. For that reason, to look for the bases of the national or regional identity in the present forces to be dig in our own history to try to find out the real or mythical origins of the same one. But the identity is not an easy or univocal concept or of an immediate apprehension. It was neither in the past nor in the present. For that reason, this article aims to introduce the problematic of the identity form the theory of the social representations and as a case applied to the City of Mendoza, Argentina.//La definición de la identidad de los pueblos es una problemática de absoluta vigencia contemporánea. El proceso de globalización económica vigente, lejos de arrasar con las particularidades regionales o nacionales parece que, en cambio, las ha exacerbado.Por ello, buscar las bases de la identidad nacional o regional en el presente, obliga a remitirse a la propia historia para tratar de escudriñar los orígenes reales o míticos de la misma. Pero la identidad no es un concepto unívoco o de fácil e inmediata aprehensión, ni el presente, ni el pasado. Por ello, este artículo apunta a presentar la problemática de la identidad vista desde la teoría de las representaciones sociales y como caso aplicado a la Ciudad de Mendoza, Argentina.

  6. Los cuerpos ígneos neógenos del cerro de Las Minas (35,3°S - 69,9°O, Cordillera Principal de los Andes, SO de Mendoza: geología, petrografía y geoquímica The Neogene igneous bodies of the Cerro de las Minas (35.3°S-69.9°W, Main Cordillera of the Andes, SW of Mendoza: geology, petrography and geochemistry

    Directory of Open Access Journals (Sweden)

    M.J. Pons

    2007-06-01

    Full Text Available El cerro de Las Minas (35,3°S - 69,9°O consiste en cuatro unidades ígneas epizonales: plutón diorítico-tonalítico, plutón granodiorítico, plutón granítico y diques -filones capa andesíticos. Estas unidades forman parte del arco magmático neógeno del SO de Mendoza correspondiente a la Andesita Huincán. Intruyen a rocas sedimentarias jurásicas de las Formaciones Puchenque y Auquilco y las que en las cercanías del contacto con los plutones diorítico y granítico, están modificadas a hornfels, calizas recristalizadas y skarns bandeados con mineralización de Fe. Geoquímicamente, constituyen un conjunto de plutones cogenéticos de amplio rango composicional, metaluminosos, subalcalinos con afinidad calcoalcalina y del tipo I, características que son semejantes a las de otros plutones de márgenes convergentes vinculados a skarns de Fe. Han evolucionado por cristalización fraccionada de sus componentes minerales principales (plagioclasa-piroxeno-anfíbol-magnetita-titanita y mezcla localizada entre los magmas diorítico y granodiorítico. Sus patrones de elementos trazas incompatibles y tierras raras son similares a los observados en las rocas ígneas: a del arco volcánico neógeno (Andesita Huincán, b vinculadas a otros skarns de Fe del SO de Mendoza (Hierro Indio y El Kaiser, c del cerro Nevazón (37,5°S perteneciente al arco volcánico paleógeno del NO de Neuquén y, finalmente, d del arco volcánico cuaternario de un sector de la zona volcánica sur (TSVZ (34,5°-37°S de los Andes, emplazados en una corteza continental relativamente delgada (35-50 km. Esto sugiere que las rocas ígneas del cerro de las Minas se formaron a partir de magmas parentales calcoalcalinos y metaluminosos, derivados de una fuente mantélica similar, con escasez o ausencia de granate residual en la fuente.The cerro de las Minas (35.3°S-69.9°W consists of four epizonal igneous units: diorite-tonalite, granodiorite and granite plutons and andesite

  7. Darwin's observation in South America: what did he find at agua de la zorra, Mendoza province? Las observaciones de Darwin en Sudamérica: ¿Qué encontró en Agua de la Zorra, provincia de Mendoza?

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    Stella Poma

    2009-04-01

    Full Text Available Scarcely 23 km from Uspallata, along the track of the old national highway 7, lies the district of Agua de la Zorra, in Mendoza province in western Argentina. Charles Darwin visited the area during his South American journeys in the 19th century and discovered a geological sequence that contained a paleoflora never described before. The flora includes an important number of species, particularly what is considered a small conifer forest with many silicified trunks still in life position. Darwin described and interpreted the sequence as sedimentary; his records show a very detailed level of observation. He also wondered about the processes that would cause the burial of the paleoflora, which he considered had happened in a marine sedimentary environment. In the modern geological framework and after a detailed study of the rocks containing the trunks, it is now interpreted that the conifer forest was buried by pyroclastic flows. Darwin accurately described the fine volcanic materials as an essential part of the deposit, but the key of the enigma about the origin of the deposits and the burial of the forest is the identification of the pyroclastic flow features; these were unknown process at the time of Darwin´s observations and interpretation.A escasos 23 km de Uspallata, a lo largo de la antigua ruta nacional 7, se encuentra la localidad de Agua de la Zorra en la provincia de Mendoza al oeste de Argentina. La región fue explorada por Charles Darwin durante su viaje por Sudamérica en el siglo XIX. Allí descubrió una secuencia geológica conteniendo una paleoflora que no había sido descripta hasta entonces. La flora incluye un importante número de especies y particularmente, un pequeño bosque de coníferas, los que se encuentran silicificados, y en posición de vida. Darwin describió e interpretó la secuencia como sedimentaria; sus notas y descripciones muestran un alto nivel de detalle en las observaciones. Darwin además se cuestion

  8. State modernization and economic regulation in the provinces winemakers. Mendoza, 1936-1946 Modernización estatal y regulación económica en provincias vitivinicultoras. Mendoza, 1936-1946

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    María Silvia Ospital

    2009-01-01

    Full Text Available The policies implemented in the country to overcome the consequences of the crisis of 1930 were measures to regulate production and trade, in the case of agricultural activities and industries. The entity created to handle the winemaking was Junta Reguladora de Vinos, which began operations after 1935. At the same time that they put into execution the provisions adopted by this national institution, the provincial authorities in the producing region arbitrated various practices designed to offset the sharper edges of the crisis and to reposition the agricultural industry at local and national market. In the province of Mendoza provincial authorities prescribed, starting in 1936, some regulations aimed at modernizing the state apparatus in an attempt to achieve greater efficiency in the implementation of regulatory policies and making the machinery of government to the demands of the new stage. The creation of a office specifically dedicated to the production of statistics and economic research under the provincial Ministry of Finance was the most important measure in this regard, while other provisions were trying to find in contemporary tourism development of a complementary alternative traditional winesLas políticas implementadas en el país para superar las consecuencias de la crisis de 1930 se manifestaron, en el caso de las actividades agrarias y agroindustriales, en medidas de regulación de la producción y el comercio. La entidad creada para ocuparse de la vitivinicultura fue la Junta Reguladora de Vinos que comenzó a operar a partir de 1935. Al mismo tiempo que se ponían en ejecución las disposiciones emanadas de ese organismo nacional, las autoridades provinciales de la región productora arbitraban diversas prácticas destinadas a paliar las aristas más agudas de la crisis y a reposicionar a la agroindustria en el ámbito local y el mercado nacional. En la provincia de Mendoza las autoridades provinciales instrumentaron, a partir

  9. Evidencias de la zona de contacto entre los terrenos de Precordillera y Pie de Palo, Provincias de San Juan y Mendoza Evidence of the contact area between Precordillera and Pie de Palo terranes, Provinces of San Juan and Mendoza.

    OpenAIRE

    Maximiliano García Torrejón; Orlando Alvarez Pontoriero; Silvina Nacif; Iván Novara; Marcos Sánchez; Silvana Spagnoto; Patricia Martinez; Mario Gimenez

    2011-01-01

    Se realizó un estudio gravimétrico en la región norte de la cuenca Cuyana, entre las provincias de San Juan y Mendoza. Mediante relaciones de gradientes gravimétricos tales como señal analítica, Tilt y fase del Tilt, se observó un marcado gradiente, que fue interpretado como un cambio lateral de litologías, que coincidiría con el área de una probable paleosutura del margen proto-andino, que separa en el terreno compuesto de Cuyania, al terreno de Precordillera con el terreno de Pie de Palo.We...

  10. Emplacement of the La Peña alkaline igneous complex, Mendoza, Argentina (33° S): Implications for the early Miocene tectonic regime in the retroarc of the Andes

    Science.gov (United States)

    Pagano, D. S.; Galliski, M. A.; Márquez-Zavalía, M. F.

    2014-03-01

    The La Peña alkaline complex (LPC) of Miocene age (18-19 Ma) lies on the eastern front of the Precordillera (32°41ʹ34ʺS, 68°59ʹ48″W, 1400-2900 m a.s.l.), 30 km northwest of Mendoza city, Argentina. It is a subcircular massif of 19 km2 and 5 km in diameter, intruded in the metasedimentary sequence of the Villavicencio Formation of Silurian-Devonian age. It is the result of integration of multiple pulses derived from one or more deep magma chambers, which form a suite of silicate rocks grouped into: a clinopyroxenite body, a central syenite facies with a large breccia zone at the contact with the clinopyroxenite, bodies of malignite, trachyte and syenite porphyry necks, and a system of radial and annular dikes of different compositions. Its subcircular geometry and dike system distribution are frequent features of intraplate plutons or plutons emplaced in post-orogenic settings. These morphostructural features characterize numerous alkaline complexes worldwide and denote the importance of magmatic pressures that cause doming with radial and annular fracturing, in a brittle country rock. However, in the LPC, the attitude of the internal fabric of plutonic and subvolcanic units and the preferential layout of dikes match the NW-SE extensional fractures widely distributed in the host rock. This feature indicates a strong tectonic control linked to the structure that facilitate space for emplacement, corresponding to the brittle shear zone parallel to the N-S stratigraphy of the country rock. Shearing produced a system of discontinuities, with a K fractal fracture pattern, given by the combination of Riedel (R), anti-Riedel (R‧), (P) and extensional (T) fracture systems, responsible for the control of melt migration by the opening of various fracture branches, but particularly through the NW-SE (T) fractures. Five different pulses would have ascent, (1) an initial one from which cumulate clinopyroxenite was formed, (2) a phase of mafic composition represented by

  11. Ecosistemas presentes y pasados en la Quebrada Benjamín Matienzo (32º 35' - 32º 50' L. S. y 70º 06' L. O., Cordillera de Los Andes, Mendoza, Argentina Present and past ecosystems in the quebrada Benjamín Matienzo (32º 35' - 32º 50'S and 70º 06'W, cordillera de Los Andes, Mendoza, Argentina

    Directory of Open Access Journals (Sweden)

    Mónica C Wingenroth

    2012-09-01

    Full Text Available Los sedimentos de un perfil en la quebrada Benjamín Matienzo, cordillera de Los Andes (32º 35' - 32º 50' L. S. y 70º 06' L. O., aproximadamente a 3400 m de altura, fueron datados en 6400 años AP a los 572 cm de profundidad. El polen identificado en 174 eventos (capas hallados en dicho perfil se relacionó con el polen presente (1980-1981 / 1981-1982. Un total de siete ambientes se definieron en la quebrada, en base a las diferencias registradas entre la cantidad y calidad del polen local, sugiriendo cambios de la vegetación y/o producción de polen, en respuesta a las variaciones en la disponibilidad del agua y la temperatura. A partir de las diferencias detectadas entre la cantidad y calidad del polen alóctono, se infirieron las direcciones predominantes de los vientos que llegaron a Matienzo en cada evento pasado. A su vez para los eventos incluidos en los mencionados ambientes se sugirieron balances acumulativos de la masa de hielo positivos y negativos, derretimiento de las áreas periglaciales congeladas y los correspondientes ciclos solares y su actividad.Sediments from a profile in the quebrada Benjamín Matienzo, cordillera de Los Andes (32º35'-32º50'S and 70º06'W, 3400 m asl, were dated at the bottom of a 572 cm-depth core to 6400 years B.P. The pollen identified in 174 events (layers of the profile was related to the present pollen assemblage (1980-1981 / 1981-1982. Differences between the quantity and quality of the local pollen defined a total of seven environments in the quebrada Benjamín Matienzo and suggested changes in vegetation and/or pollen production due to water availability and temperature variations. In turn, differences between the quantity and quality of the allochthonous pollen were used to infer the predominant wind directions reaching the quebrada Benjamín Matienzo during each past event. In addition, positive and negative cumulative ice mass balance, melting of frozen periglacial areas and correspondence

  12. Very long pahoehoe inflated basaltic lava flows in the Payenia volcanic province (Mendoza and la Pampa, Argentina

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    Giorgio Pasquarè

    2008-03-01

    Full Text Available Extremely long basaltic lava flows are here presented and described. The flows originated from the great, polygenetic, fissural Payen Volcanic Complex, in the Andean back-arc volcanic province of Payenia in Argentina. The lava flows outpoured during the Late Quaternary from the summit rift of a shield volcano representing the first volcanic centre of this complex. One of these flows presents an individual tongue-like shape with a length of 181 km and therefore is the longest known individual Quaternary lava flow on Earth. Leaving the flanks of the volcano this flow reached the Salado river valley at La Pampa and, in its distal portion, maintained its narrow and straight shape without any topographic control over a flat alluvial plain. It has a hawaiite composition with low phenocryst content of prevailing olivine and minor plagioclase. Rare Earth element patterns are typical of Na-alkaline basalts, but incompatible trace element patterns and Sr -Nd isotope ratios, suggest a geodynamic setting transitional to the orogenic one. The flow advanced following the thermally efficient "inflation" mechanism, as demonstrated by a peculiar association of well developed morphological, structural and textural features. The temperature of 1130-1160°C and the viscosity of 3-73 Pa*s, calculated by petrochemical data, may be considered, together with a very low cooling rate and a sustained and long lasting effusion rate, the main causes of the extremely long transport system of this flow. Both the extreme length of the flow and the partial lack of topographic control may provide new constraints on the physics of large inflated flows, which constitute the largest volcanic provinces on Earth and probably also on the terrestrial planets.

  13. Holocene compression in the Acequión valley (Andes Precordillera, San Juan province, Argentina): Geomorphic, tectonic, and paleoseismic evidence

    Science.gov (United States)

    Audemard, M.; Franck, A.; Perucca, L.; Laura, P.; Pantano, Ana; Avila, Carlos R.; Onorato, M. Romina; Vargas, Horacio N.; Alvarado, Patricia; Viete, Hewart

    2016-04-01

    The Matagusanos-Maradona-Acequión Valley sits within the Andes Precordillera fold-thrust belt of western Argentina. It is an elongated topographic depression bounded by the roughly N-S trending Precordillera Central and Oriental in the San Juan Province. Moreover, it is not a piggy-back basin as we could have expected between two ranges belonging to a fold-thrust belt, but a very active tectonic corridor coinciding with a thick-skinned triangular zone, squeezed between two different tectonic domains. The two domains converge, where the Precordillera Oriental has been incorporated to the Sierras Pampeanas province, becoming the western leading edge of the west-verging broken foreland Sierras Pampeanas domain. This latter province has been in turn incorporated into the active deformation framework of the Andes back-arc at these latitudes as a result of enhanced coupling between the converging plates due to the subduction of the Juan Fernández ridge that flattens the Nazca slab under the South American continent. This study focuses on the neotectonics of the southern tip of this N-S elongated depression, known as Acequión (from the homonym river that crosses the area), between the Del Agua and Los Pozos rivers. This depression dies out against the transversely oriented Precordillera Sur, which exhibits a similar tectonic style as Precordillera Occidental and Central (east-verging fold-thrust belt). This contribution brings supporting evidence of the ongoing deformation during the Late Pleistocene and Holocene of the triangular zone bounded between the two leading and converging edges of Precordillera Central and Oriental thrust fronts, recorded in a multi-episodic lake sequence of the Acequión and Nikes rivers. The herein gathered evidence comprise Late Pleistocene-Holocene landforms of active thrusting, fault kinematics (micro-tectonic) data and outcrop-scale (meso-tectonic) faulting and folding of recent lake and alluvial sequences. In addition, seismically

  14. Geological evidence for fluid overpressure, hydraulic fracturing and strong heating during maturation and migration of hydrocarbons in Mesozoic rocks of the northern Neuquén Basin, Mendoza Province, Argentina

    Science.gov (United States)

    Zanella, Alain; Cobbold, Peter R.; Ruffet, Gilles; Leanza, Hector A.

    2015-10-01

    In the northern Neuquén Basin of Argentina (especially in Mendoza Province), there is strong geological evidence for fluid overpressure in the past. The evidence takes the form of bitumen veins and bedding-parallel veins of fibrous calcite ('beef'). Such veins are widespread in the fold-and-thrust belt of the Malargűe area, where bitumen mining has been active for a century or so. So as to collect information on the development of fluid overpressure in this part of the Neuquén Basin, several old mines were visited and studied in the Malargűe area. Here the bitumen veins have intruded mainly the Late Jurassic to Early Cretaceous Mendoza Group, but also the Late Cretaceous Neuquén Group. The veins have the forms of bedding-parallel sills or dykes and they are especially thick within anticlines, forming saddle-reefs in several places. Beef veins are also numerous in the Malargűe area. They contain bitumen and therefore seem to have formed at the same time as the bitumen veins. Near many outcrops of bitumen and beef, we have found fine-grained volcanic intrusive bodies. The best examples are from the La Valenciana syncline. According to 39Ar-40Ar dating, these bodies are mainly of Mid-Miocene age. More generally, volcanism, deformation and maturation of source rocks seem to have reached a climax in Miocene times, when the subducting Pacific slab became relatively flat.

  15. PRELIMINARY GEOID MODEL IN SAN JUAN PROVINCE: A CASE STUDY IN THE ANDES

    DEFF Research Database (Denmark)

    Tocho, Claudia; Miranda, Silvia; Pacino, Maria Cristina

    2008-01-01

    A high-resolution and high-precision detailed gravimetric geoid has been computed for San Juan province in Argentina, ranging from 27 degrees S to 34 degrees S in latitude and 72 degrees W to 65 degrees W in longitude. The gravimetric geoid was calculated using the RTM method, a multiband spherical...... Stokes Fast Fourier Transformation, and the removerestore technique for the spherical harmonic reference field and the terrain. As an external evaluation, the gravimetric quasigeoid/geoid was compared to the geoid heights obtained from 90 GPS/levelling points available for the province. Finally, a GPS......-tailored local geoid, which fits the GPS observations, was computed....

  16. Xenolitos ultramáficos en el cerro De la Laguna, volcanismo basáltico de retroarco en el sureste de la provincia de Mendoza, Argentina Ultramafic xenoliths in De la Laguna hill, retro-arc basaltic volcanism in the southeast of Mendoza Province, Argentina

    Directory of Open Access Journals (Sweden)

    G. W. Bertotto

    2002-12-01

    Full Text Available Se describen por primera vez xenolitos ultramáficos incluidos en basaltos de retroarco cenozoicos, en el sector extraandino de la provincia de Mendoza. El basalto portador tiene estructura masiva y textura porfírica con asociaciones de fenocristales de olivino-clinopiroxeno y olivino-plagioclasa. Todos los xenolitos ultramáficos son peridotitas en facies de espinela, se reconocieron lherzolitas, wehrlitas y dunitas, en orden de abundancia. Presentan una asociación mineral compuesta por olivino, ortopiroxeno, clinopiroxeno y espinela. Las texturas identificadas son porfiroclástica de Tipo I y porfiroclástica a equigranular de Tipo I. Estos xenolitos tienen zonas de reacción microscópicas mayormente desarrolladas en los ortopiroxenos y clinopiroxenos en el contacto con el basalto. La presencia de reacción indica al menos un evento de desequilibrio. Estas peridotitas representan fragmentos del manto superior situado debajo de la zona estudiada.Ultramafic xenoliths in Cenozoic retro-arc basalts of the extra-Andean sector of Mendoza province are described here for the first time. The host basalt has a massive structure and porphyritic texture with phenocryst assemblages of olivine-clinopyroxene and olivine-plagioclase. All the ultramafic xenoliths are spinel-bearing peridotites; lherzolite, wehrlite and dunite, in order of abundance, have been recognized. The mineral assemblage is olivine-orthopyroxene-clinopyroxene-spinel. Textures are porphyroclastic Type I and porphyroclastic to equigranular Type I. The xenoliths contain microscopic reaction areas, mainly developed in orthopyroxene and clinopyroxene in the contact with basalt. The reaction indicates at least one disequilibrium event. The peridotites are fragments of the upper mantle situated beneath the study area.

  17. Los cuerpos ígneos neógenos del cerro de Las Minas (35,3°S - 69,9°O, Cordillera Principal de los Andes, SO de Mendoza: geología, petrografía y geoquímica

    Directory of Open Access Journals (Sweden)

    M.J. Pons

    2007-06-01

    Full Text Available El cerro de Las Minas (35,3°S - 69,9°O consiste en cuatro unidades ígneas epizonales: plutón diorítico-tonalítico, plutón granodiorítico, plutón granítico y diques -filones capa andesíticos. Estas unidades forman parte del arco magmático neógeno del SO de Mendoza correspondiente a la Andesita Huincán. Intruyen a rocas sedimentarias jurásicas de las Formaciones Puchenque y Auquilco y las que en las cercanías del contacto con los plutones diorítico y granítico, están modificadas a hornfels, calizas recristalizadas y skarns bandeados con mineralización de Fe. Geoquímicamente, constituyen un conjunto de plutones cogenéticos de amplio rango composicional, metaluminosos, subalcalinos con afinidad calcoalcalina y del tipo I, características que son semejantes a las de otros plutones de márgenes convergentes vinculados a skarns de Fe. Han evolucionado por cristalización fraccionada de sus componentes minerales principales (plagioclasa-piroxeno-anfíbol-magnetita-titanita y mezcla localizada entre los magmas diorítico y granodiorítico. Sus patrones de elementos trazas incompatibles y tierras raras son similares a los observados en las rocas ígneas: a del arco volcánico neógeno (Andesita Huincán, b vinculadas a otros skarns de Fe del SO de Mendoza (Hierro Indio y El Kaiser, c del cerro Nevazón (37,5°S perteneciente al arco volcánico paleógeno del NO de Neuquén y, finalmente, d del arco volcánico cuaternario de un sector de la zona volcánica sur (TSVZ (34,5°-37°S de los Andes, emplazados en una corteza continental relativamente delgada (35-50 km. Esto sugiere que las rocas ígneas del cerro de las Minas se formaron a partir de magmas parentales calcoalcalinos y metaluminosos, derivados de una fuente mantélica similar, con escasez o ausencia de granate residual en la fuente.

  18. Patrones fenologico de la provincia de Mendoza, Argentina: Mediante serie temporal de imágenes NOAA - AVHRR NDI GAC

    NARCIS (Netherlands)

    González Loyarte, M.M.; Menenti, M.; Roig, F.A.

    2010-01-01

    Phenological patterns of the province of Mendoza, Argentina, through a temporal series of NOAA-AVHRR NDVI GAC images. The temporal dynamics of vegetation in Mendoza is described through analysis of regional foliar phenology using a series of 108 monthly NOAA-AVHRR NDVI GAC images. A Fast Fourier

  19. Patrones fenologico de la provincia de Mendoza, Argentina: Mediante serie temporal de imágenes NOAA - AVHRR NDI GAC

    NARCIS (Netherlands)

    González Loyarte, M.M.; Menenti, M.; Roig, F.A.

    2010-01-01

    Phenological patterns of the province of Mendoza, Argentina, through a temporal series of NOAA-AVHRR NDVI GAC images. The temporal dynamics of vegetation in Mendoza is described through analysis of regional foliar phenology using a series of 108 monthly NOAA-AVHRR NDVI GAC images. A Fast Fourier Tra

  20. Perichaena megaspora, a new nivicolous species of myxomycete from the Andes.

    Science.gov (United States)

    Ronikier, Anna; Lado, Carlos; de Basanta, Diana Wrigley

    2013-01-01

    A new nivicolous species of Perichaena is described from the Andes in Argentina. The most conspicuous characteristics of Perichaena megaspora are the large spores and their ornamentation in the form of flattened warts. The 16-21 μm diam spores make the new species unique in the genus in which all other species have spores rarely reaching 15 μm diam. Twenty-two collections were found in the field during two consecutive years at 10 localities in Mendoza province Argentina, including one collection isolated from a moist chamber culture of ground litter. The new species was examined under stereomicroscope, light microscope and scanning electron microscope and micrographs of relevant details are included.

  1. Very long pahoehoe inflated basaltic lava flows in the Payenia volcanic province (Mendoza and la Pampa, Argentina Flujos de lava basáltica pahoehoe muy extendidos en la provincia volcánica Payenia (Mendoza y La Pampa, Argentina

    Directory of Open Access Journals (Sweden)

    Giorgio Pasquarè

    2008-03-01

    Full Text Available Extremely long basaltic lava flows are here presented and described. The flows originated from the great, polygenetic, fissural Payen Volcanic Complex, in the Andean back-arc volcanic province of Payenia in Argentina. The lava flows outpoured during the Late Quaternary from the summit rift of a shield volcano representing the first volcanic centre of this complex. One of these flows presents an individual tongue-like shape with a length of 181 km and therefore is the longest known individual Quaternary lava flow on Earth. Leaving the flanks of the volcano this flow reached the Salado river valley at La Pampa and, in its distal portion, maintained its narrow and straight shape without any topographic control over a flat alluvial plain. It has a hawaiite composition with low phenocryst content of prevailing olivine and minor plagioclase. Rare Earth element patterns are typical of Na-alkaline basalts, but incompatible trace element patterns and Sr -Nd isotope ratios, suggest a geodynamic setting transitional to the orogenic one. The flow advanced following the thermally efficient "inflation" mechanism, as demonstrated by a peculiar association of well developed morphological, structural and textural features. The temperature of 1130-1160°C and the viscosity of 3-73 Pa*s, calculated by petrochemical data, may be considered, together with a very low cooling rate and a sustained and long lasting effusion rate, the main causes of the extremely long transport system of this flow. Both the extreme length of the flow and the partial lack of topographic control may provide new constraints on the physics of large inflated flows, which constitute the largest volcanic provinces on Earth and probably also on the terrestrial planets.En este trabajo se presentan y describen flujos de lava extremadamente largos. Estos flujos se originaron en el complejo volcánico fisural Payen, dentro de la provincia volcánica Payenia en el retroarco andino. Los flujos de lava

  2. Composition and provenance of Late Pleistocene-Holocene alluvial sediments of the eastern Andean piedmont between 33 and 34° S (Mendoza Province, Argentina)

    Science.gov (United States)

    Mehl, A.; Blasi, A.; Zárate, M.

    2012-12-01

    The Andean cordillera, and its piedmont in the central western Argentina, has been long considered as one of the main source areas of detritus for the Chaco-Pampean plain sand dune fields and loess/loess-like deposits of central Argentina. The main goal of this study is to evaluate the composition of the late Pleistocene-Holocene alluvial deposits of the Andes cordillera piedmont, from 33° to 34° S. The results are interpreted in the context of the regional geology, tectonic setting of the study area and its implications in the continent-wide perspective of modern alluvial sands proposed by Potter (1994). Sampling was conducted at the alluvial stratigraphic sequences of four study sites along three Andean piedmont arroyos; modal mineralogy in the very fine sand fraction (3 phi to 4 phi) was determined using standard petrographic microscope methods. Q:F:LF average compositions indicate that the Late Pleistocene-Holocene very fine-grained alluvial sands of the Cordillera Frontal piedmont reflects the modern lithic arenites of the Argentine Association reported by Potter (1994). The results show two geologically distinct sources in the catchment areas, volcaniclastic and metamorphic rocks. High concentrations of mica and volcanic glass are likely related to particle morphologies and to the deposition sedimentary environment recorded in the alluvial sequences—floodplains. The overabundance of micas over the volcanic glass in the mid-late Holocene alluvial sequence indicates the drainage of a metamorphic area at the expense of other lithological sources. Source areas are located mainly in the Frontal cordillera, and to a lesser extent, in the piedmont Tertiary deposits, another likely source for the analyzed Quaternary alluvial sediments. The mineralogical signature of the late Pleistocene and Holocene alluvial sequences is in agreement with the composition of the southern Pampean sand mantles, loess and loess-like deposits mainly formed by a volcanic mineral

  3. The Choiyoi volcanic province at 34°S-36°S (San Rafael, Mendoza, Argentina): Implications for the Late Palaeozoic evolution of the southwestern margin of Gondwana

    Science.gov (United States)

    Kleiman, Laura E.; Japas, María S.

    2009-08-01

    The Choiyoi rhyolitic province of Chile and Argentina (23°S-42°S) was emplaced at the SW margin of Gondwana during the Permian. The San Rafael Massif (Mendoza, Argentina, 34°-36°S), is a key area to analyse the relative timing of Choyoi magmatism and related deformation as it bears one of the most complete and well exposed succession. Stratigraphic, structural and magmatic studies indicate that major changes of geodynamic conditions occurred during the Permian since arc-related sequences syntectonic with transpression (lower Choiyoi) were followed by transitional to intraplate, postorogenic suites coeval with transtension (upper Choiyoi). During the Early Permian, a major event of N-NNW dextral transpressional motions deformed the Carboniferous foreland basin in the San Rafael Massif. This event is attributed to the first episode of the San Rafael orogeny and can be related to oblique subduction (Az. 30°) of the Palaeo-Pacific plate. Ca. 280 Ma the inception of voluminous calc-alkaline volcanism (lower Choiyoi) syntectonic with WNW sinistral transpression of the second episode of the San Rafael orogeny, is associated with an eastward migration of the magmatic arc at this latitude. To the southeast of San Rafael, magmatism and transpression continued to migrate inland suggesting that a progressively younger, WNW, sinistral, thick skinned deformation belt broadens into the foreland and can be traced from San Rafael to Sierra de la Ventana, linking the San Rafael orogeny with the Gondwanide orogeny of the Cape Fold Belt in South Africa. This distribution of magmatism and deformation is interpreted as being the consequence of a progressive shallowing of the Palaeo-Pacific plate starting to the north of San Rafael, and culminating with a flat-slab region south of 36°S. Ca. 265 Ma the onset of predominantly felsic volcanism (upper Choiyoi) in San Rafael occurred in a Post-San Rafael extensional setting. Kinematic indicators and strain fabric analyses of San Rafael

  4. SIMGRO, a GIS-Supported Regional Hydrologic Model in Irrigated Areas : Case study in Mendoza, Argentina

    NARCIS (Netherlands)

    Querner, E.P.; Morabito, J.A.; Tozzi, D.A.

    2008-01-01

    The SIMGRO hydrologic simulation model was extended to include irrigation practice. It could then be used to evaluate the effect of hydrologic changes in an irrigated area in the province of Mendoza, Argentina where, given an average annual rainfall of approximately 200mm , irrigation is crucial for

  5. Patrones fenológicos de la Provincia de Mendoza, Argentina, mediante serie temporal de imágenes NOAA-AVHRR NDVI GAC Phenological patterns of the province of Mendoza, Argentina, through a temporal series of NOAA-AVHRR NDVI GAC images

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    M. M González Loyarte

    2010-12-01

    Full Text Available Se describe la dinámica temporal de la vegetación de Mendoza mediante análisis de la fenología foliar regional con una serie de 108 imágenes mensuales de índice de vegetación NOAA-AVHRR NDVI GAC. La serie se descompone aplicando la Transformada Rápida de Fourier en parámetros dinámicos: NDVI medio, amplitudes (máxima variabilidad del NDVI y fases (tiempo entre inicio del ciclo y máximo NDVI para diferentes períodos. Con los parámetros con mayor información (variablilidad inter e intraanual se hace una clasificación y se obtiene un mapa de 18 áreas de comportamiento fenológico. Éste se vincula con los ecosistemas y con las unidades de vegetación. Se modela el patrón fenológico (curva NDVI mensual para 17 unidades de vegetación. El mapa aporta elementos dinámicos al estudio regional de la vegetación generando una zonificación nueva explicada por variables que determinan la actividad vegetativa. El patrón fenológico describe el funcionamiento de la vegetación y permite comprender sus variaciones geográficas. El conjunto de la vegetación de Mendoza responde a un ciclo anual con matices localizados de ligera bimodalidad. Los patrones de bajo contraste invierno-verano corresponden a condiciones climáticas xéricas expresando su máximo vegetativo al final del verano; la disponibilidad hídrica incrementa este contraste acortando el tiempo de máxima expresión vegetativa.The temporal dynamics of vegetation in Mendoza is described through analysis of regional foliar phenology using a series of 108 monthly NOAA-AVHRR NDVI GAC images. A Fast Fourier Transform was used to decompose the series into dynamic parameters: mean NDVI, amplitudes (maximum NDVI variability and phases (time from start of cycle to maximum NDVI for different time periods. A classification is made based on those parameters with larger information content (inter- and intra-annual variability, achieving a map of 18 areas of phenological behaviour. This

  6. Ciclos tectónicos, volcánicos y sedimentarios del Cenozoico del sur de Mendoza-Argentina (35°-37°S y 69°30'W Cenozoic tectonic, volcanic and sedimentary cycles in southern Mendoza Province, Argentina (35°-37°S y 69°30'W

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    Ana María Combina

    2011-01-01

    Full Text Available En este trabajo se describe la estratigrafía sedimentaria y volcánica asociada a los procesos de deformación de las unidades con edades del Cretácico Tardío al Plioceno Tardío aflorantes en el sur de Mendoza, Argentina, entre los ríos Atuel y Barrancas en el ámbito de la Cordillera Principal. Se proponen tres ciclos tectovolcano-sedimentarios, limitados por discordancias regionales generadas por la acción de las Fases Incaica, Quechua, Pehuenche y Diaguita. El primer ciclo comprende las unidades volcánicas y sedimentarias del Cretácico Superior hasta el Oligoceno Superior (Formaciones Roca y Pircala-Coihueco y el Ciclo Eruptivo Molle. El segundo abarca desde el Oligoceno Tardío al Mioceno Tardío (Formación Agua de la Piedra y las Andesitas Huincán. Por último, el tercer ciclo comprende desde el Mioceno Tardío al Plioceno (Formaciones Butaló, Pincheiras, Loma Fiera, Río Diamante y las Andesitas La Brea.This article describes the volcanic and sedimentary stratigraphy and their associated proces-ses with the Andean deformation during the Late Cretaceous to Late Pliocene. The studied área is located between the Atuel and Barrancas rivers and the Main Cordillera, in southern Mendoza, Argentina. Three tectovolcano-sedimentary cycles limited by regional discordances (Inca, Quechua, Pehuenche and Diaguita are proposed. The first comprises Upper Oligocene to Upper Miocene volcanic and sedimentary units (Roca and Pircala-Coihueco formations and the Volcanic Cycle Molle. The second extends from the Late Oligocene to Late Miocene (Agua de la Piedra Formation and the Huincán Andesites volcanic cycle. Finally, the third cycle ranges from the Late Miocene to Pliocene (Butaló, Pincheiras, Loma Fiera and Rio Diamante formations and La Brea Andesites.

  7. La estructura de la faja corrida y plegada de Malargüeen la zona del río Diamante (34º30'-34º50' l.s. y su relación con laCordillera Frontal, provincia de Mendoza Thestructure of the Malargüe fold-and-thrust belt at the Rio Diamante area (34º30'-34º50' S.L. and itsrelationship with the Cordillera Frontal, Mendoza province

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    Martín M. Turienzo

    2009-10-01

    Full Text Available La faja corrida y plegada deMalargüe es un cinturón orogénico de piel gruesa desarrollado principalmente enel Mioceno- Plioceno durante la orogenia andina, en la provincia de Mendoza. Enbase a un detallado mapeo de campo, información sísmica y de perforaciones, serealizaron tres secciones estructurales balanceadas resultando un acortamientopromedio de 14, 2 km (24% para las rocas del basamento y de la cubierta.Regionalmente, la estructura está conformada por dos importantes ascensos delbasamento entre los cuales queda configurada una zona donde predomina ladeformación en la cubierta sedimentaria. En la zona occidental se desarrollantres grandes cuñas de basamento asociadas a corrimientos producidos por lacompresión andina las cuales se insertan en la cubierta sedimentaria (a lolargo del yeso de las Formaciones Tábanos y Auquilco, lo cual muestra laestrecha relación espacial y temporal entre la deformación del basamento y lacubierta. En la región con deformación de piel fina, la abundancia de lutitas yevaporitas en el sector occidental favorece el plegamiento mientras que lasunidades más competentes presentes hacia el este forman imbricaciones yestructuras duplex (corrimientos Mesón y Sosneado. En el sectororiental, la falta de niveles de despegue dentro de la cubierta dificulta eldesarrollo de cuñas de basamento y en cambio tiene lugar una importante deformaciónmediante retrocorrimientos. Con la continuidad de la compresión, la fallaCarrizalito alcanzó la superficie colocando las rocas pre-jurásicas sobre lossedimentos sinorogénicos terciarios en la zona norte y central, mientras quehacia el sur las estructuras de basamento permanecen en el subsuelo.The Malargüe fold-and-thrust belt is a thick-skinnedone developed mainly in Miocene-Pliocene times during the Andean orogeny, in Mendoza province. Based on detailed field mapping, seismicand well information, three balanced structural cross-sections were maderesulting an

  8. Estudio de la contaminación con huevos de Toxocara sp. en suelos de espacios públicos de San Martín de los Andes, Provincia del Neuquén. Argentina. (Soil contamination with Toxocara sp. eggs in public parks from San Martín de los Andes, Province of Neuquen, Argentina

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    Brusoni, Claudio: Medico Veterinario,

    2005-10-01

    Full Text Available Con el objetivo de determinar la presencia de huevos de Toxocara sp. en suelos de espacios públicos de San Martín de los Andes, Provincia del Neuquén, Argentina, se estudiaron suelos de 12 parques de la localidad entre Abril y Julio de 2005. Se comprobó la presencia de huevos de Toxocara sp. en el 92% de los sitios de muestreados. Se recomienda la implementación de acciones para minimizar los riesgos a la salud pública. The objective being to determine if our soil in parks and publics areas were contaminated with Toxocara sp. eggs, we surveyed 12 different places in the area of San Martín de los Andes, Province of Neuquén from April to July, 2005. The presence of Toxocara sp. Eggs was confirmed in 92% of the places studied. In order to minimize the risk for our public health, we recommended the implementation of safety measures.

  9. Evolución de la natación de competencia en la provincia de Mendoza, Argentina, desde 1950 hasta el año 2000 = Evolution of the swimming competition in the province of Mendoza (Argentina, from 1950 to the year 2000

    Directory of Open Access Journals (Sweden)

    Adrián Javier Sáez

    2013-03-01

    Full Text Available La investigación llevada a cabo se sustenta en un estudio exploratorio y descriptivo. El tipo de diseño de la investigación es no experimental retrospectiva porque no se manipulan las variables y se buscan datos del pasado. Fue evaluada una población de N=40 conformada por 28 nadadores, 8 entrenadores y 4 dirigentes de distintas épocas, con una encuesta para recolectar datos de los orígenes y evolución de la natación de competencia en Mendoza. Asimismo se evaluó la evolución de los records de las pruebas de 100 metros en los cuatro estilos, los 400, 800 y 1500 metros libres ambos sexos en pileta de 25 y 50 metros. Se consideró la cantidad de clubes participantes, los nadadores con licencia nacional en los distintos años y las nominaciones para Seleccionados Nacionales en las distintas décadas. No se obtuvo diferencias estadísticamente significativas entre la evolución de los records realizados en pileta de 25 con la de 50 metros. Se comprobó que disminuyó tanto la cantidad de clubes participantes en los torneos desde 1950 hasta el año 2000 como la de nadadores federados. El estudio nos revela que el nivel competitivo de los nadadores se ha elevado por el aumento en las nominaciones a Seleccionados Nacionales. Como conclusión obtuvimos que posiblemente estos valores obtenidos se deban a la evolución en las técnicas de nado y en los métodos de entrenamiento, interrogante que puede servir para próximos estudios y que, en este caso, la cantidad de deportistas no es directamente proporcional a los logros deportivos.------------------------------------------------------------------------------The investigation that we carried out sustains in an exploratory and descriptive study. The type of design of the investigation is non experimental retrospective because the variables are not manipulated and data of the past look for. A population of N=40 conformed by 28 swimmers, 8 trainers and 4 leaders of different times was evaluated

  10. Mendoza various production scenarios: in search of a commercial fruit growing (1900-1930

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    Florencia Rodriguez Vázquez

    2016-04-01

    Full Text Available The formation of a diversified regional economy in Mendoza finds antecedents in the early twentieth century. Indeed, the leading sectors, entrepreneurs and technicians looked for alternatives in order to clarify the effects of cyclical crises affecting the wine industry, agribusiness main activity of the province. Mode in this period is to attend a transitional period, in which a panorama complexity of agricultural production as a result of the combination of several factors that are detected and analyzed in this paper.

  11. Seven-year follow-up of the immune response after one or two doses of inactivated hepatitis A vaccine given at 1 year of age in the Mendoza Province of Argentina.

    Science.gov (United States)

    Espul, Carlos; Benedetti, Laura; Linares, Mariela; Cuello, Hector; Castro, Ivana Lo; Thollot, Yaël; Rasuli, Anvar

    2017-09-21

    This monocentre, descriptive, prospective, non-interventional study evaluated the long-term immune responses following routine vaccination with one or two doses of a licensed inactivated hepatitis A (HA) vaccine (Avaxim® 80U Pediatric) at age 11-23 months in a cohort of children from Mendoza, Argentina. Antibodies to hepatitis A virus (anti-HAV) were quantified annually up to Y5, and at Y7. Children whose titer decreased to below the seroprotection threshold (defined as an anti-HAV antibody concentration of ≥10 mIU/inmL in a microparticle enzyme immunoassay up to Y5, or ≥3 mIU/mL in an electrochemiluminescence immunoassay at Y7) received a routine booster dose of the same HA vaccine. This report summarizes the data at 7 years after the first vaccination. Of 546 participants initially included, 266 participants remained at Year 7. Of these, 206 having received one HA primary dose as a toddler were still seroprotected at Y7; titers for a further 7 also having received one HA dose as a toddler fell to below the seroprotection threshold and they therefore received a booster; all 53 having received two HA doses as a toddler and still present at Y7 remained seroprotected at Y7. One or two primary doses of this HA vaccine in toddlers result in very good persistence of anti-HAV up to 7 years post-first vaccination.

  12. El volcanismo del Terciario superior del sur de Mendoza Upper Terciary volcanism from southern Mendoza

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    F. E. Nullo

    2002-06-01

    Full Text Available Se describe por primera vez la petrografía y geoquímica de unidades volcánicas terciarias del sur de la provincia de Mendoza. Se analizan la nomenclatura estratigráfica y sus edades, estableciéndose una secuencia de eventos magmáticos ocurridos durante el Neógeno, comenzando con la evolución de un retro-arco, seguido por un arco magmático más joven. Se intenta respetar la nomenclatura estratigráfica existente, sin embargo, la definición de unidades se ha realizado sobre la base de las edades radimétricas y sus edades de cristalización, más sobre sus características petrográficas. La actividad magmática se extiende desde el Oligoceno superior al Mioceno superior, correspondiendo a el Ciclo Eruptivo Molle y el Ciclo Eruptivo Huincán, y comenzó con un episodio magmático basáltico inicial (CEM. Esta actividad se generó en la corteza inferior dominada por la concentración de gabros, dioritas y rocas híbridas (granulitas máficas. Debido a un engrosamiento de la corteza como consecuencia de la actividad tectónica durante Mioceno superior o por el estancamiento de magmas o por la combinación de ambos procesos, la formación de granulitas granatíferas resultó un producto distintivo de la corteza inferior. Con el desarrollo del arco magmático (CEH en el Mioceno superior, los magmas ascendieron desde la fuente mantélica, encontrándose con una corteza inferior granatífera, perdiendo capacidad de ascenso por falta de contraste de densidades, produciéndose una fusión extendida, la homogeinización y el ascenso, en equilibrio con la corteza baja, proceso que caracteriza el volcanismo de un arco magmático.The petrology and geochemistry of the exposed Tertiary volcanic units in southern Mendoza Province are described for the first time. The formal stratigraphic nomenclature and ages are analyzed and a stratigraphic basis is established for successive magmatic events occurring during the Neogene, starting with the evolution of

  13. Evolución estructural de la zona de transición entre las fajas plegadas y corridas de Aconcagua y Malargüe Provincia de Mendoza Structural evolution of the transition zone between the Aconcagua and Malargûe fold and thrust belts, province of Mendoza

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    S. Broens

    2005-12-01

    Full Text Available En el presente trabajo se describe brevemente la estratigrafía y la estructura de los Andes en la zona de transición entre las fajas plegadas y corridas del Aconcagua y Malargüe. Las rocas aflorantes corresponden a un basamento volcánico acido permotriásico, sedimentitas mesozoicas de la cuenca neuquina y efusiones volcánicas y depósitos continentales neógenos. Estructuralmente se reconocen de oeste a este, cuatro segmentos denominados: zona de inversión tectónica, zona de pliegues apretados, zona central o de imbricación y anticlinal del Carrizalito. Se construyeron dos secciones estructurales que se ajustan a los datos de campo recogidos en las zonas de imbricación, de pliegues apretados y del flanco dorsal del anticlinal del Carrizalito, que permitieron describir las estructuras presentes en el área. Lineamientos regionales de orientación noroeste-sureste podrían estar actuando como zonas de transferencia de rechazos. Pueden reconocerse dos o tres pulsos deformacionales según se considere la edad relativa de las estructuras respecto al levantamiento de la Cordillera Frontal. Para el caso en que el cordón del Carrizalito haya actuado como un alto de basamento se proponen dos pulsos, uno de piel fina y otro posterior que levanta a la Cordillera Frontal basculando la secuencia previamente deformada. Si en cambio la estructuración del anticlinal del Carrizalito hizo que este se comporte como punto de fijación (sticking point podria sumarse un tercer episodio deformacional con corrimientos fuera de secuencia.In this work we describe briefly the stratigraphy and the structure of the Andes in the transition zone between the Aconcagua and Malargüe fold and thrust belts. The outcrops are a Permotriasic volcanic acid basement, Mesozoic sediments of the Cuenca Neuquina and Neogene volcanic rocks and continental deposits. Structuraly we distinguish from west to east four segments: a tectonic inversion zone, a tight folds zone, a

  14. VITICULTURA Y POLÍTICA INTERNACIONAL: EL INTENTO DE REINCORPORAR A MENDOZA Y SAN JUAN A CHILE (1820-1835

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    PABLO LACOSTE

    2006-06-01

    Full Text Available Entre 1830 y 1835 algunos dirigentes de Mendoza y San Juan, provincias vitivinícolas, trataron de separarse de la República Argentina y regresar a Chile, tal como en la época colonial. Durante más de dos siglos, Mendoza y San Juan fueron parte del Corregimiento de Cuyo del Reino de Chile. Esta situación cambió desde 1776 con la creación del Virreinato del Río de la Plata. Después de la Revolución de 1810, Mendoza y San Juan formaron parte de la República Argentina. Pero algunos años después de la independencia, un grupo descontento con la acción y decisiones del gobierno de Buenos Aires, inició acciones orientadas a la secesión. Este artículo investiga las razones y motivaciones socioeconómicas de este grupoBetween 1830 and 1835 some leaders of Mendoza and San Juan, wine industry oriented provinces, attempted to withdrawal from Argentina Republic, and come back to Chile such as in colonial times. During more than two centuries, Mendoza and San Juan were members of Cuyo Province in Chile's Kingdom. This situation changed since 1776 because the creation of the River Plate Viceroyalty. After Revolution of 1810, Mendoza and San Juan took part of Argentina Republic. But some years after the independence, a group discontented with de action and decision of Buenos Aires government begun the action oriented to secession. This paper explores the socioeconomic reasons and motivation of this group

  15. ARTESANOS, TRABAJADORES METALÚRGICOS Y VITIVINICULTURA MODERNA EN MENDOZA ARGENTINA (1885-1930

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    Eduardo Pérez Romagnoli

    2005-12-01

    Full Text Available A fines del siglo XIX, la reconversión económica hacia la vitivinicultura moderna, liderada por un sector del grupo social dominante, generaba cambios profundos en Mendoza –al pie de los Andes y a 1000 km de Buenos Aires- en los que los inmigrantes europeos mediterráneos desempeñaron un papel central. Se produjo un rápido aumento de la superficie con viñedo -acompañada por un aumento de la red que distribuía el escaso recurso hídrico- y la difusión de la producción industrial de vino en el oasis norte, irrigado por los ríos Mendoza y Tunuyán. A principios del siglo XX, el proceso era también notable en el oasis sur, conformado por los ríos Diamante y Atuel. Según el Segundo Censo Nacional, en 1914, la superficie con viñedo alcanzaba las 70 mil hectáreas y había registradas más de 1300 bodegas; pero su capacidad de producción era muy contrastada

  16. Subduction controls on Miocene back-arc lavas from Sierra de Huantraico and La Matancilla and new 40Ar/39Ar dating from the Mendoza Region, Argentina

    Science.gov (United States)

    Dyhr, Charlotte T.; Holm, Paul M.; Llambías, Eduardo J.; Scherstén, Anders

    2013-10-01

    Back-arc volcanism in the western Argentinian provinces of Mendoza and Neuquén has been widespread from the Miocene to historic times. We present a detailed investigation of profiles through two of the major Miocene volcanic areas of the region, the neighboring Huantraico and La Matancilla plateaus, including new 40Ar/39Ar age results of major and trace elements as well as Nd, Sr and Pb isotopic data. Four million years of eruptions from 24.4 ± 0.3 Ma (2σ) of alkali olivine basalts with OIB-type incompatible trace element enrichments at La Matancilla (~ 36.50°S) provide evidence for the presence of back-arc mantle devoid of subduction-related components. In contrast, the lower Huantraico lavas (~ 37.30°S) require an atypical back-arc mantle, almost devoid of arc-like components (e.g. low La/Ta = 15-18 and Ba/La = 12-18), but with a more depleted isotopic signature (e.g. 87Sr/86Sr, 0.7033-0.7037) than observed elsewhere in the Andean back-arc. The Lower to Upper Series development in the Huantraico sequence represents a gradual change from basaltic to trachyandesitic back-arc lavas with a weak but temporally increasing arc geochemical signature (e.g. La/Ta = 15-21; Ba/La = 12-45), which is accompanied by Sr, Nd and Pb isotopic compositions approaching present day values of the Andes arc. The compositional change is accompanied by a gradually decreasing role for garnet in the mantle source, a decreasing degree of melting, but also simultaneously increasing influence from subducted fluids, probably as the slab geometry changes through time. The volcanism at Huantraico ceased when a flat slab was established around 15 Ma.

  17. The Andean orogenic front at Sierra de Las Peñas-Las Higueras, Mendoza, Argentina

    Science.gov (United States)

    Costa, Carlos H.; Gardini, Carlos E.; Diederix, Hans; Cortés, José M.

    2000-07-01

    The Sierra de Las Peñas-Las Higueras (Mendoza Province, Argentina, 32°15'S-32°45'S) presents one of the clearest and most continuous exposures of the Quaternary thrust front of the Precordilleran fold-and-thrust belt. It is characterized by an east-verging thrust that breaks the surface and causes Neogene sedimentary rocks to override Quaternary alluvial conglomerates. Monoclinal folds and progressive unconformities are characteristic of deformation in the upper part of the alluvial cover, indicating synchronous development of sedimentation and thrusting during the Quaternary. South of this range, ongoing deformation is by gentle warping of the piedmont alluvial plain, hiding blind thrusts at depth.

  18. Palaeoclimate reconstructions from lacustrine terraces and lake-balance modeling in the southern central Andes: New insights from Salar de Pocitos (Salta Province, Argentina)

    Science.gov (United States)

    Bekeschus, Benjamin; Bookhagen, Bodo; Strecker, Manfred R.; Freymark, Jessica; Eckelmann, Felix; Alonso, Ricardo

    2013-04-01

    The arid Puna Plateau in the southern central Andes of NW-Argentina constitutes the southern part of Earth's second largest orogenic plateau. Numerous internally drained basins are restricted by ranges that peak 5-6 km above sea level, creating a compressional basin and range morphology. The conspiring effects of this structurally controlled topography and the high degree of aridity have resulted in low stream power of the fluvial network and internally drained basins. A steep rainfall gradient exists across this area ranging from a humid Andean foreland (>1m/yr annual rainfall) to progressively drier areas westwards. At the present-day, the interior of the plateau is widely characterized by annual rainfall and high evaporation rates. Thus continuous lacustrine archives are limited and sediments are dominated by evaporites. Several closed basins contain vestiges of moister conditions from past pluvial periods. For example, the staircase morphology of lacustrine shorelines and abrasion platforms in the distal sectors of alluvial fans and pediments at Salar de Pocitos (24.5°S, 67°W, 3650 m asl) records repeated former lake highstands. This intermontane basin has existed since the late Tertiary, constituting a 435 km² salt flat in the region of Salta, NW Argentina. Comparison with palaeoclimate records from the neighboring Salar de Atacama suggests that the terrace systems at Salar de Pocitos were formed during the Late Pleistocene and early Holocene. Here we report on our preliminary results of the extent of several terrace generations in this region. We mapped terraces in the field and on satellite images and determined their elevations during a high-resolution DGPS field survey. Our analysis reveals 3-4 distinct terrace levels associated with individual lake-level highstands. However, basin-wide correlation is difficult due to ongoing tectonism and differential tilting of the basin. The highest lake terrace, ca. 25 m above modern base level, locally comprises a

  19. Andes 1997 Gravity Data

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — The Central Andes gravity data (6,151 records) were compiled by Professor Gotze and the MIGRA Group. This data base was received in April, 1997. Principal gravity...

  20. History of Lake Andes

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — Information about the history and management of Lake Andes is compiled in this report. It is intended to help future refuge managers become acquainted with the...

  1. El arriero y el transporte terrestre en el Cono Sur (Mendoza, 1780-1800

    Directory of Open Access Journals (Sweden)

    Lacoste, Pablo

    2008-12-01

    Full Text Available This paper explores the muleteer as an economic actor in terrestrial transportation in South Cone, specially in the route across the Andes in order to connect Atlantic and Pacific markets. Since Mendoza’s customs records, this study has processed 120.000 freight-carrying mules to know the origin and destiny places, main routes, volume and kind of charge. The muleteer promoted an intensive activity in terms of transportation, trade and wine industry. As a result, he leaded the rise of a regional proto-bourgeoisie.

    El artículo examina al arriero como actor económico en el transporte terrestre del Cono Sur, sobre todo en la ruta a través de la Cordillera de los Andes, para enlazar los mercados del Atlántico y el Pacífico. A partir de los manuales de Cargo y Data de la Aduana de Mendoza, se han procesado 120.000 mulas de carga para determinar los lugares de origen y destino, principales rutas, volumen y tipo de carga transportada. El arriero impulsó una intensa actividad en el transporte, el comercio y en la industria vitivinícola; como resultado, este actor promovió el surgimiento de una protoburguesía regional.

  2. Mendoza : Rahvuslike huvide eiramine toob Euroliidule kollapsi / Alan Mendoza ; interv. Indrek Veiserik

    Index Scriptorium Estoniae

    Mendoza, Alan

    2008-01-01

    Intervjuu Henry Jacksoni Ühingu presidendiga, kes vastab küsimustele, mis puudutavad NATO laienemist, Lissaboni lepet, Euroopa Liidu kaitse- ja välispoliitikat, Eesti välispoliitikat ja suhteid Venemaaga. Vt. samas: Alan Mendoza ja Henry Jacksoni ühing

  3. Mendoza : Rahvuslike huvide eiramine toob Euroliidule kollapsi / Alan Mendoza ; interv. Indrek Veiserik

    Index Scriptorium Estoniae

    Mendoza, Alan

    2008-01-01

    Intervjuu Henry Jacksoni Ühingu presidendiga, kes vastab küsimustele, mis puudutavad NATO laienemist, Lissaboni lepet, Euroopa Liidu kaitse- ja välispoliitikat, Eesti välispoliitikat ja suhteid Venemaaga. Vt. samas: Alan Mendoza ja Henry Jacksoni ühing

  4. A Late Quaternary shortening rate for the frontal thrust of the Andean Precordillera north of Mendoza

    Science.gov (United States)

    Schmidt, S.; Kuhlmann, J.; Hetzel, R.; Mingorance, F.; Ramos, V. A.

    2009-12-01

    Although large historical earthquakes occurred in the Andean back-arc region between 28° and 34°S - for instance Mendoza was destroyed by an earthquake of magnitude MS = 7.0 in 1861 - the slip rates of active faults remain unknown. We report a slip rate for the 50-km-long Las Penas thrust, which constitutes the frontal thrust of the Precordillera. In its southern part, a well preserved fluvial terrace along La Escondida Creek (Costa et al., 2000) is displaced vertically by 10.6 ± 0.7 m as documented by several fault scarp profiles. Apart from radiocarbon dating of plant remnants, three different approaches for 10Be exposure dating have been applied to constrain the age of the terrace. Amalgamated sandstone pebbles (corrected for an inherited 10Be component using similar pebbles from the active creek) and a depth profile obtained from four sand samples yield 10Be exposure ages of 12.2 ± 1.5 and 11.3 ± 2.0 kyr, respectively. Both ages are in excellent agreement with the 14C age of 12.61 ± 0.20 cal kyr BP. In contrast, 10Be ages of five sandstone boulders vary significantly and exceed the age of the terrace by 10 to 70 kyr, which demonstrates that the widely used assumption of a negligible inherited component is not valid here. The age of the river terrace combined with the vertical fault offset yields an uplift rate of ~0.8 mm/yr for the Las Penas thrust. Combined with the fault dip of 25°, we determine a Late Quaternary horizontal shortening rate of ~1.8 mm/yr, which is about 40% of the GPS derived shortening rate of 4.5 ± 1.7 mm/yr in the back-arc region of the Andes (Brooks et al., 2003). References Brooks, B.A., Bevis, M., Smalley, R., Kendrick, E., Manceda, R., Lauria, E., Maturana, R. & Araujo, M. (2003): Crustal motion in the Southern Andes (26° - 36°S): Do the Andes behave like a microplate? Geochem. Geophys. Geosyst., 4 (10), pp. 14, 1085, doi 10.1029/2003GC000505. Costa, C.H., Gardini, C.E., Diederix, H., Cortés, J.M. (2000): The Andean orogenic

  5. Quaternary continetal back-arc evolution from southern Mendoza, Argentina

    Science.gov (United States)

    Espanon, Venera; Chivas, Allan; Dosseto, Anthony; Honda, Masahiko; Phillips, David; Matchan, Erin; Price, David

    2016-04-01

    The Quaternary evolution of the Payenia Basaltic Province (PBP) in southern Mendoza, Argentina has been investigated using a multi-dating approach in combination with pre-exiting geochemical data. This basaltic province covers an area of approximately 40000 km2 and is mainly characterised by backarc volcanism. In the current investigation nine new radiometric ages obtained using surface exposure, 40Ar/39Ar and thermoluminescence dating are presented. Six ages correspond to the late Pleistocene and three to the Holocene. The surface exposure ages obtained using cosmogenic 3He and 21Ne are in good agreement with previous publications and confidently suggest that part of this basaltic province was active at least 4000 years ago (taking a conservative approach). In addition, we combined the available geochronological and geochemical data to reconstruct the Quaternary evolution of this basaltic province. This approach was used to create maps of geospatial distribution of trace-element ratios to determine geochemical changes during the Pleistocene. Employing this method it is evident that two geochemical distinct types of magma were erupting at the same time interval within the PBP. In the north eastern part (Nevado volcanic field) of the PBP an arc-like signature is evident, while in the southern part (Río Colorado volcanic field) of the same basaltic province an Ocean Island Basalt (OIB) signature is evident. The arc-like signature in the north eastern part of the PBP, decreased during the Pleistocene in a north-west direction indicated by a reduction in Ba/La and La/Ta in the Nevado and Llancanelo volcanic field. The Holocene volcanism is restricted to the western side of the Payún Matrú volcanic field and is dominated by OIB-like signatures such as high Ta/Hf and low Ba/La and La/Ta. This contribution presents new geochronology for the PBP and confirms that two different types of volcanism occurred simultaneously during the Pleistocene, while the Holocene

  6. Minerales de mena del depósito epitermal de baja sulfuración Don Sixto, Mendoza Ore minerals from Don Sixto, a low sulfidation epithermal deposit from Mendoza

    Directory of Open Access Journals (Sweden)

    Ana Cecilia Mugas Lobos

    2012-03-01

    Full Text Available El proyecto minero Don Sixto es un depósito epitermal de baja sulfuración de Au-Ag, ubicado en el bloque de San Rafael, en el SE de la provincia de Mendoza. En este depósito, cuyo recurso aurífero es próximo a las 900.000 onzas, se ha identificado una asociación de minerales de metales preciosos que incluye: uytenbogaardtita, stromeyerita, naumannita, acantita, polibasita, stützita y cervelleita. Estos minerales son escasos y se encuentran frecuentemente asociados a oro y plata de variable fineza, diseminados en vetas de cuarzo hidrotermal y en unidades volcánicas-piroclásticas de los Grupos Choiyoi y El Portillo. En este depósito se encuentra abundante pirita, con cantidades menores de arsenopirita, calcopirita, esfalerita, magnetita, hematita y, en forma subordinada, pirrotina, galena, marcasita, bornita y boulangerita, junto con calcosina, digenita y covellina. La presencia de uytenbogaardtita, stützita, cervelleita y polibasita constituye la primera mención de estos minerales para la provincia de Mendoza.The Don Sixto mining project is a low sulfidation Au-Ag deposit, with a gold resource close to 900,000 ounces, located in the San Rafael Massif, in the SE of Mendoza province. Recently, it was found a precious-metal mineral association including uy-tenbogaardtite, stromeyerite, naumannite, acanthite, polybasite, stützite and cervelleite. These minerals are scarce and are commonly related to gold and silver of variable fineness, disseminated in hydrothermal quartz veins and volcanic-pyroclastic rock units from the Choiyoi and El Portillo Group. The most common mineral is pyrite associated with subordinated arsenopyrite, chalcopyrite, sphalerite, magnetite and hematite; lesser amounts of pyrrhotite, galena, marcasite, bornite, boulangerite, chalcocite, digenite and covellite were also recognized. This is the first mention in Mendoza province for uytenbogaardtite, stützite, cervelleite and polybasite.

  7. Alkaline lavas from southern Mendoza, Argentina, extend the Patagonian DUPAL mantle field to the north

    Science.gov (United States)

    Soager, N.; Holm, P. M.; Llambias, E.

    2010-12-01

    The lavas sampled around Río Colorado ~37°S at the border of Mendoza and Neuquén provinces, Argentina, define an OIB-like end-member composition for the Pleistocene and Holocene activity in the Payún Matrú volcanic field. Although positioned in the far back-arc of the Andes, only a few lavas show signs of involvement of slab fluids or crustal contamination such as relatively high LILEs relative to Nb. The very low La/Nb (~0.66) and Zr/Nb (~5) and high U/Pb (0.3-0.4) of the end-member composition clearly distinguish the source from normal MORB mantle, while high Ba/Nb (~10) and K/Nb (370-400) compared to FOZO and HIMU type OIBs suggest an EM type of mantle. Overall, the trace element patterns of the Río Colorado lavas are similar to the central and north Patagonian intraplate basalts and to South Atlantic E-MORB affected by the Discovery plume and the LOMU component (le Roux et al., 2002, EPSL 203). The isotopic composition of the Río Colorado component has a 206Pb/204Pb = 18.4, 207Pb/204Pb = 15.58, 208Pb/204Pb = 38.3, 87Sr/86Sr = 0.70353 and 143Nd/144Nd = 0.51285. This composition overlaps the central and north Patagonian intraplate basalts in Pb-isotopic space but is slightly less enriched in Sr and Nd-isotopes. It is distinctly different from the FOZO like composition of the south Patagonian intraplate basalts and the nearby Juan Fernandéz plume but similar to the South Atlantic N-MORB and MORB from the southern Chile Ridge segment 4 (Sturm et al., 1999, JGR 104) described as DUPAL type. The DUPAL-MORB type isotopic composition and the plume-like trace element patterns of the Río Colorado lavas suggest the presence of a weak plume beneath the area. The eruption of the large Payún Matrú volcano and the gigantic Pleistocene flood basalts also calls for a thermal anomaly to produce these melts during a weakly compressive tectonic regime with no significant addition of slab fluids. This was supported by Burd et al. (2008, Abstr., 7th Int. Sym. And. Geo

  8. Sauropod and theropod dinosaur tracks from the Upper Cretaceous of Mendoza (Argentina): Trackmakers and anatomical evidences

    Science.gov (United States)

    González Riga, Bernardo Javier; Ortiz David, Leonardo Daniel; Tomaselli, María Belén; dos Anjos Candeiro, Carlos Roberto; Coria, Juan Pedro; Prámparo, Mercedes

    2015-08-01

    New findings of dinosaur ichnites from Agua del Choique section (Mendoza Province, Argentina) provides ichnological and anatomical information about the Cretaceous sauropods and theropods. Around 330 tracks distributed in six footprint levels were identified in this area, one of most important of South America. Two ichnocenoses are located in different paleoenvironmental contexts. In the Anacleto Formation (early Campanian) around 20 titanosaurian tracks were found in floodplain and ephemeral channel deposits. Herein, one pes track shows three claw impressions and this is congruent to two new titanosaur specimens recently discovered in Mendoza Province that have articulated and complete pedes. In this context, for the first time to titanosaurs, ichnological evidences are supported by skeletal elements. In the Loncoche Formation (late Campanian-early Maastrichtian) titanosaurian tracks of Titanopodus mendozensis are abundant (around 310 tracks) and were produced by titanosaurs that walked in a very wet substrate of tidally dominated deltas related with the first Atlantic transgression for northern Patagonia. In this facies association, three different trydactl tracks indicate the presence of small theropods (1-2 m long), expanding the knowledge about the faunistic components that lived in these marine marginal environments.

  9. Domestic wastewater treatment in waste stabilization ponds for irrigation in Mendoza, Argentina: policies and challenges.

    Science.gov (United States)

    Vélez, O R; Fasciolo, G E; Bertrano, A V

    2002-01-01

    Arid areas call for imaginative water management solutions to avoid the dangers of water shortages. Growing demands of water for domestic and industrial uses decrease the availability of water for agriculture. It therefore becomes necessary to set up a policy for the use of domestic effluents. For the province of Mendoza, Argentina, with 1,500,000 inhabitants, a master plan was designed as of 1991 for the treatment of domestic effluents and subsequent disposal for irrigation. The guidelines set up by WHO for the use of wastewater in agricultural applications were taken into consideration. At present, the Province of Mendoza has available projects which are either complete, in execution or in the bidding process, entailing secondary treatment capacity with reuse of 320,000 cubic metres/day and an estimated possible irrigation area of 10,000 hectares. With this infrastructure, some strategic lines of action are recommended to establish a policy for the agricultural use of wastewater: (a) to program the use of treated wastewater to avoid discharges to irrigation flows; (b) to develop an institutional scheme for the efficient and safe use of these waters; and (c) develop scientific and technologic know-how to accompany the updated policies.

  10. GasAndes will flow by mid year

    Energy Technology Data Exchange (ETDEWEB)

    True, W.R.

    1997-04-21

    An important gas pipeline in the Southern Cone of South America will start up later this year in time for the region`s Southern Hemisphere winter. Gasoducto GasAndes S.A., Santiago, Chile, has completed pipelay on the $350 million, 287 mile, 24-in. line from La Mora, state of Mendoza, Argentina, to Santiago. The line`s significance lies in part in how it draws the historically antagonistic countries into closer interdependence. And it is also the first gas-import project to one of the region`s largest and most important cities. The line will bring gas to fuel several power plants supplying electricity to Santiago. In addition, Metrogas S.A., Santiago`s gas distribution company and a partner in GasAndes, will also be receiving gas for the city`s first natural-gas distribution system, which is currently being installed. The paper discusses the market, the pipeline, scada and metering, and environmental measures.

  11. Paleozoogeography of the Wine Mouse (Akodon oenos & Late Holocene Paleoenvironments in South-Central Mendoza, Argentina

    Directory of Open Access Journals (Sweden)

    Fernando Julián Fernández

    2011-02-01

    Full Text Available Cranial remains of the wine mouse (Akodon oenos are documented from an archaeological site in south-central Mendoza, Argentina (Agua de La Mula, 35º22' S, 68º15' W, which dates to the end of the late Holocene (1610 ± 60; 1260 ± 60; 1000 ± 50 C14 yr B.P.. The taxonomic status of this small rodent is currently being assessed, but these remains represent the first fossil record for the morphotaxon A. oenos. The species’ present distribution is restricted to a few records from Mendoza province. Analysis of the remains supports paleoenvironmental reconstruction using the small mammal assemblage recovered from this site. From the late Holocene into modernity temperature decreased and winter precipitation increased, resulting in advance of Patagonian steppe grading with altitude into Monte desert. Holocene climatic conditions may explain the relatively late human occupation of ecologically marginal environments in this region, which probably favored effective human occupation of the Payunia region at sites such as Agua de La Mula between 1600 and 1000 years B.P.

  12. Trees in the Andes:

    OpenAIRE

    Jost, François Paul

    2017-01-01

    High mountain regions including the Andean region are very sensitive to climate change. Farmers in the central Andes of Peru are increasingly being exposed to the impacts of climate variability. This transdisciplinary research uses field laboratories, combining the farming system and the sustainable livelihood approaches, to carry out social, ecological, and financial assessments so as to identify sustainable and resilient livelihood strategies for small-scale Andean farmers. The first r...

  13. Payenia Quaternary flood basalts (southern Mendoza, Argentina: Geophysical constraints on their volume

    Directory of Open Access Journals (Sweden)

    Mauro G. Spagnuolo

    2016-09-01

    Full Text Available The Quaternary volcanic province of Payenia is located in southern Mendoza and northern Neuquén provinces of Argentina and is characterized by a dominant basaltic composition. The volcanic province covers an area larger than 40,000 km2 and its origin and evolution has been the center of several studies. In this study we analyzed gravity data together with more accurate volcanic volumes calculations in order to investigate the subsurface structure of the Payenia volcanic province. The volume of material was calculated using digital elevation models and geographic information system (GIS techniques to estimate the volume of material erupted and then, with those values, make an estimation of the intrusive material that could be located within the crust. The results of the calculations were compared with different 2D-sections constructed to model the gravity data and compare with the observed satellite gravity. After evaluating different models which have been generated to match both: the observed gravity data and the subsurface material calculated, we discuss those that best fit with observation. The results clearly indicate that the lithosphere is attenuated below the region.

  14. Payenia Quaternary flood basalts (southern Mendoza, Argentina):Geophysical constraints on their volume

    Institute of Scientific and Technical Information of China (English)

    Mauro G. Spagnuolo; Darío L. Orts; Mario Gimenez; Andres Folguera; Victor A. Ramos

    2016-01-01

    The Quaternary volcanic province of Payenia is located in southern Mendoza and northern Neuquén provinces of Argentina and is characterized by a dominant basaltic composition. The volcanic province covers an area larger than 40,000 km2 and its origin and evolution has been the center of several studies. In this study we analyzed gravity data together with more accurate volcanic volumes calculations in order to investigate the subsurface structure of the Payenia volcanic province. The volume of material was calculated using digital elevation models and geographic information system (GIS) techniques to estimate the volume of material erupted and then, with those values, make an estimation of the intrusive material that could be located within the crust. The results of the calculations were compared with different 2D-sections constructed to model the gravity data and compare with the observed satellite gravity. After evaluating different models which have been generated to match both: the observed gravity data and the subsurface material calculated, we discuss those that best fit with observation. The results clearly indicate that the lithosphere is attenuated below the region.

  15. Geomorphological and geophysical investigation of a complex rock glacier system - Morenas Coloradas valley (Cordon del Plata, Mendoza, Argentina)

    Science.gov (United States)

    Otto, Jan-Christoph; Götz, Joachim; Keuschnig, Markus; Hartmeyer, Ingo; Trombotto, Dario; Schrott, Lothar

    2010-05-01

    In the semi-arid high Andes of Argentina and Chile, rock glaciers are more frequent and often larger than glaciers. Aridity and high solar radiation hamper the development of large glaciers, favour permafrost conditions and the generation of rock glaciers. One of the few rock glaciers that have been studied in more detail since more than 20 years is located in the Cordon del Plata range about 60 km west of Mendoza, Argentina. The Morenas Coloradas rock glacier in the Rio Vallecitos catchment can be described as a multilobe, multiunit, multiroot and multipart rock glacier. It is a complex, transitional landform composed of a high altitude glaciated zone, which transforms into a debris covered glacier with thermokarst phenomena followed by various active rock glacier lobes and subsequently, inactive and relict lobes in the lower sections. Its total length is about 5 km. Complex transitional landforms between debris covered glaciers and rock glaciers are frequently observed in semi-arid mountain environments with high sediment production in periglacial areas like the Andes of Argentina but can be found also in other similar mountain ranges like for example Pamir, or Karakorum. However, the evolution and internal characteristics of such landforms are often unknown. Glacial and periglacial landforms of this size represent important water stores that play an essential role in water management and agriculture in the foreland of the Andes of Mendoza. In February 2008 subsurface conditions were investigated at three different altitudes using geophysical methods (ground penetrating radar, electric resistivity tomography). Complemented by digital geomorphological mapping we analyse the complex rock glacier ensemble, to gain insight into landform evolution, sediment flow structures and internal characteristics (permafrost occurrence, active layer depths, ice content, possible ice origin). Geophysical surveying at Morenas Coloradas clearly indicates the existence of frozen

  16. The severe zonda wind event of 11 July 2006 east of the Andes Cordillera (Argentine): a case study using the BRAMS model

    Science.gov (United States)

    Norte, Federico Augusto; Ulke, Ana Graciela; Simonelli, Silvia Carmen; Viale, Maximiliano

    2008-11-01

    The zonda is a wind that exhibits the so-called foehn effect: a warm, dry, strong wind related to adiabatic compression upon descending in the lee of the Andes. This phenomenon occurs mostly in winter and spring over the entire length of the extratropical Andes. It is frequently detected near the cities of Mendoza and San Juan, the most important urban regions of western Argentina. The aim of this work is to understand why a zonda wind event, occurring on 11 July 2006, reached and maintained the higher category Z4 during several hours. A secondary aim is to evaluate the ability of a Brazilian regional atmospheric modeling system (BRAMS) model to represent the features of this extreme episode and to explore if it can be used to predict a zonda event. The difference found with respect to other severe zonda wind episodes analyzed was that the wind registered the highest category (Z4) with extreme gusts during a long period. This condition was registered in particular on southern plain areas of San Juan province. The phenomenon had a great impact on the community, with residences and buildings being affected or destroyed, trees being felled, power supply and communications being shutdown, and several rural and urban fires being reported. The event was characterized through surface and upper-level information and model results. The synoptic surface and upper-air conditions were those typically associated with a severe zonda wind occurrence: a surface cold front approaching the region, driven by a 500 hPa trough, a strong upper-air jet stream, and a deep low-pressure surface system at higher latitudes over the Atlantic Ocean. The North West Argentine Low in central west Argentina during the following hours could be observed centered approximately at 31°S 66°W. in a few lower latitude than the location observed by National Center of Environmental Prediction (NCEP) reanalysis. On the other hand, it is the authors’ impression that the BRAMS model achieved an acceptable

  17. A NEGATIVE ANSWER TO A PROBLEM OF FREMLIN AND MENDOZA

    Institute of Scientific and Technical Information of China (English)

    Ye Guoju; Stefan Schwabik

    2007-01-01

    This article studies some convergence results for the McShane integral of functions mapping the interval [0, 1] into a Banach space X from the point of view of an open problem proposed by D.H.Fremlin and J. Mendoza in [2], also the anthors give a negative answer to this open problem.

  18. Chronology of Late Pleistocene glacier advances in the Rı´o Mendoza Valley, Argentina

    Science.gov (United States)

    Espizua, Lydia E.

    1999-10-01

    correlate with marine oxygen isotope stage 4. The Penitentes-Horcones nonglacial sediments may have been deposited during interglacial isotope stage 3. The Horcones advance and the nonglacial sediments deposited between Horcones and Almacens tills may likely equate with stage 2. The moraine sequence is compared with those studied by Espizua (1998) along the Rio Grande valley in the southwestern Mendoza Province.

  19. Phenolic Compounds Profiling of Virgin Olive Oils from Different Varieties Cultivated in Mendoza, Argentina, by Using Liquid Chromatography-Mass Spectrometry.

    Science.gov (United States)

    Monasterio, R P; Olmo-García, L; Bajoub, A; Fernández-Gutiérrez, A; Carrasco-Pancorbo, A

    2017-09-20

    The aim of this work was to achieve a preliminary characterization of the profile of the phenolic fraction of virgin olive oils (VOOs) from Maipú (Mendoza, Argentina). Thus, 25 commercial VOO samples from Arauco, Arbequina, Picual, Frantoio, Changlot, Empeltre, Nevadillo, Manzanilla, and Coratina (both monovarietals and blends) were analyzed using LC-ESI-QTOF MS and LC-ESI-IT MS for identification and quantification purposes, respectively. A rapid LC method (15 min) accomplished quantitative information about a total of 40 phenolic compounds, including secoiridoid derivatives, which have not been evaluated before in samples coming from the subregion so-called Maipú (Mendoza province, Argentina). The results make evident that olive oils coming from Mendoza can be considered as important sources of phenolic bioactive compounds, exhibiting similar phenolic compound levels to those shown by oils from other typical world production regions. Moreover, some distinctive features of the Arauco variety (Argentinean autochthonous variety) were pointed out; indeed, a correlation between flavonoids content and botanical variety was established herewith.

  20. El represamiento y aluvión del río Santa Cruz, Andes Principales (31°40'S, provincia de San Juan Landslide dam and outburst of the Río Santa Cruz, Main Andes, (31°40'S, province of San Juan

    Directory of Open Access Journals (Sweden)

    Patricio E. D'odorico

    2009-12-01

    Full Text Available En la región de los Andes Principales sanjuaninos, existe una alta concentración de deslizamientos, cuyos depósitos han originado represamientos naturales. El colapso de estos diques generados por movimientos de ladera es el proceso evolutivo más probable de estas geoformas. El análisis de imágenes satelitales y fotos aéreas permite reconstruir las características y el origen de los deslizamientos que formaron esos diques naturales. En esta región de los Andes Principales, el rápido levantamiento y erosión de las cadenas montañosas ha creado pendientes muy abruptas y una estructuración interna en los materiales, que determinaron un aumento de la susceptibilidad al colapso de las pendientes, independientemente de disparadores como la actividad sísmica o las precipitaciones. El presente trabajo tiene como objetivo analizar las causas que llevaron a la formación del dique natural que produjo el represamiento y desarrollo de la laguna Los Erizos en el curso medio del río Santa Cruz, el colapso del dique y su consecuente aluvión y las características morfológicas de la región de estudio. La comparación temporal entre fotos aéreas e imágenes satelitales, indica que la causa del dique natural, fue el deslizamiento de detritos de la ladera occidental de la cordillera de Santa Cruz, localizado debajo del Cerro Estrella. El constante flujo de agua produjo un aumento del nivel del cuerpo de agua hasta alcanzar la cota máxima del dique. Con el aporte adicional del río Santa Cruz, el lago empezó a drenar mediante un delgado curso de agua establecido sobre el dique que tuvo un fuerte efecto erosivo. El debilitamiento progresivo desencadenó progresivo la rotura de la represa y consecuente aluvión el día 12 de noviembre de 2005. En base a un análisis temporal de imágenes satelitales sobre el sector de la laguna y la región en general, se pudo monitorear toda la cuenca del río San Juan, y detectar posibles diques naturales

  1. Vida y muerte de doña Melchora Lemos, empresaria vitivinícola y terciaria de la Orden de Predicadores (Mendoza, Reino de Chile, 1691-1741

    Directory of Open Access Journals (Sweden)

    Lacoste, Pablo

    2006-08-01

    Full Text Available This paper studies the life and death of doña Melchora Lemos, «pulpera», miller and wine maker in Mendoza, in Chile’s Kingdom. She was the only woman who owned a «pulperia» in the province; she built the only mill of the city; and she leaded one of better winery of Mendoza. Her life and death developed under catholic church influence. The sources of the paper are unpublished documents taken from the historical Archives in Mendoza (Argentine and Santiago (Chile.

    El artículo examina la historia de vida y muerte de doña Melchora Lemos, singular empresaria del siglo XVIII. Ella era la única mujer que poseía una pulpería; levantó el entonces único molino harinero de la ciudad; y administró la bodega más moderna de la región desde el punto de vista de la tecnología. Estos hechos se produjeron en el contexto de una intensa vida religiosa como terciaria de la orden de Santo Domingo. El estudio se ha realizado a través de fuentes originales inéditas del Archivo Nacional de Chile y el Archivo Histórico de Mendoza.

  2. El temprano desarrollo de la vitivinicultura en Mendoza y en Canelones (1870-1930. Un análisis comparado

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    Daniele Bonfanti

    2005-01-01

    Full Text Available Starting from the end of XIX century, wine producing was a decisive factor in the process of modernization of Rio de la Plata area, contributing in differentiating the production and causing a fast industrialization in this particular field. Besides, local economies were revitalized by inserting them as specialized production areas in the national market. This article represents a first attempt of comparative analysis of the development of this field in two of the main wine producing areas in Rio de la Plata region: the Canelones department (Uruguay and Mendoza province (Argentine.A partir de finales del siglo XIX, la vitivinicultura cumplió un rol determinante en el proceso de modernización rioplatense contribuyendo a la diferenciación de la producción y provocando una rápida industrialización de un sector agrícola. Además, revitalizó a las economías locales, que se reinsertaron en los mercados nacionales como zonas especializadas. El artículo representa un primer intento de análisis comparativo del desempeño del sector en las dos principales áreas vitivinícolas rioplatenses: el departamento de Canelones (Uruguay y la provincia de Mendoza (Argentina.

  3. Mercado de trabajo y condiciones de vida en Mendoza a comienzos del siglo XX

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    Juan Manuel Cerdá

    2006-01-01

    Full Text Available El propósito del presente trabajo es analizar los cambios y las continuidades en el proceso de formación del mercado de trabajo en la provincia de Mendoza a comienzos del siglo XX. La incorporación de un número significativo de inmigrantes a finales del siglo XIX junto a un proceso de reorganización productiva asociado al desarrollo de la industria vitivinícola, implicó cambios en las relaciones sociales y en las condiciones de vida de amplios sectores de la población mendocina. Iniciado el siglo XX, la vitivinicultura se convirtió en la principal actividad productiva de la provincia y la más importante en su rubro a nivel nacional. Los viñateros, productores agroindustriales, industriales bodegueros, contratistas de viñas , etc., fueron constituyéndose en parte de una sociedad cada vez más heterogénea y diversa, producto del desarrollo capitalista que experimentó la región desde el último tercio del siglo XIX y que se insertó en el proceso de incorporación de la economía Argentina al mercado mundial. Este período resulta de suma importancia porque se determinó un sistema productivo en torno a la actividad vitivinícola de la provincia que dio forma al mercado de trabajo regional. En este contexto, la inserción de los trabajadores se dio de una manera muy dispar en el proceso productivo, caracterizado por una alta estacionalidad y una escasa especialización de la mano de obra requerida.The aim of this work is to analyze the changes and continuities during the process of formation of the labor market in the province of Mendoza in the early 1900s. Wide sectors of the Mendoza population saw their life conditions and social interactions change as a result of the absorption of a significant amount of immigrants by the end of 19 th century, together with a restructuring of production connected to the development of the wine industry. Shortly after the turn of the century, wine had become the main productive activity of that

  4. Plantas Fósiles del Grupo Choiyoi, Cordillera Frontal a la Latitud del río Mendoza

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    Magdalena Koukharsky

    2011-06-01

    Full Text Available En este trabajo se dan a conocer los primeros restos fósiles hallados en sedimentitas, cuyo componente clástico es de origen volcánico, intercaladas en la Formación Tambillos del Grupo Choiyoi, Cordillera Frontal de Mendoza. Los mismos consisten en abundantes improntas de Sphenophyta en estado de preservación regular a malo. En la zona estudiada, las rocas de la Formación Tambillos, que son dominantemente volcánicas ácidas y de edad pérmica temprana a media según correlaciones regionales, se depositaron sobre una discordancia erosiva labrada en lavas andesíticas intensamente propilitizadas que se atribuyen a la Formación Portezuelo del Cenizo. Los restos vegetales se encuentran a unos 23 metros de la base, contenidos en niveles de areniscas finas y pelitas depositadas en un ambiente fluvial (microdelta, en los bordes de un lago y fueron coetáneas con los primeros episodios de volcanismo riolítico en la región. Si bien la flora encontrada no permite definir la edad, las formas presentes son comunes en niveles del Carbonífero superior-Pérmico y Triásico de Argentina.

  5. ESTUDIO ARQUEOHISTÓRICO DEL REGISTRO VÍTREO EN SITIOS MINEROS (MENDOZA, ARGENTINA) (Archaeohistorical Study of the Vitreous Record in Mining Sites (Mendoza, Argentina))

    National Research Council Canada - National Science Library

    Osvaldo Sironi

    2017-01-01

    ... medicinales entre la clase trabajadora minera de la Precordillera de Mendoza (Argentina). ENGLISH: Results of the analysis of the vitreous record from Minas Paramillos Sur and Mina La Atala are presented...

  6. The Andes: A Geographical Portrait

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    Anthony Bebbington

    2016-05-01

    Full Text Available Reviewed: The Andes: A Geographical Portrait. By Axel Borsdorf and Christoph Stadel. Translated by Brigitte Scott and Christoph Stadel. Cham, Switzerland: Springer International Publishing, 2015. xiv + 368 pp. US$ 139.00. Also available as an e-book. ISBN 978-3-319-03529-1.

  7. Charles Darwin in the Andes

    Science.gov (United States)

    Bizzo, Nelio; Bizzo, Luis Eduardo Maestrelli

    2006-01-01

    Considering geological time as an important epistemological obstacle to the construction of ideas on biological evolution, a study was carried out on the so-called "Darwin Papers". The conclusion was that Charles Darwin's excursion in the Andes during March-April 1835 was a crucial step in this regard. An expedition was carried out in…

  8. Charles Darwin in the Andes

    Science.gov (United States)

    Bizzo, Nelio; Bizzo, Luis Eduardo Maestrelli

    2006-01-01

    Considering geological time as an important epistemological obstacle to the construction of ideas on biological evolution, a study was carried out on the so-called "Darwin Papers". The conclusion was that Charles Darwin's excursion in the Andes during March-April 1835 was a crucial step in this regard. An expedition was carried out in…

  9. Hydrological Modeling of Highly Glacierized Basins (Andes, Alps, and Central Asia

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    Nina Omani

    2017-02-01

    Full Text Available The Soil and Water Assessment Tool (SWAT was used to simulate five glacierized river basins that are global in coverage and vary in climate. The river basins included the Narayani (Nepal, Vakhsh (Central Asia, Rhone (Switzerland, Mendoza (Central Andes, Argentina, and Central Dry Andes (Chile, with a total area of 85,000 km2. A modified SWAT snow algorithm was applied in order to consider spatial variation of associated snowmelt/accumulation by elevation band across each subbasin. In previous studies, melt rates varied as a function of elevation because of an air temperature gradient while the snow parameters were constant throughout the entire basin. A major improvement of the new snow algorithm is the separation of the glaciers from seasonal snow based on their characteristics. Two SWAT snow algorithms were evaluated in simulation of monthly runoff from the glaciered watersheds: (1 the snow parameters are lumped (constant throughout the entire basin and (2 the snow parameters are spatially variable based on elevation bands of a subbasin (modified snow algorithm. Applying the distributed SWAT snow algorithm improved the model performance in simulation of monthly runoff with snow-glacial regime, so that mean RSR decreased to 0.49 from 0.55 and NSE increased to 0.75 from 0.69. Improvement of model performance was negligible in simulations of monthly runoff from the basins with a monsoon runoff regime.

  10. Peritidal cyclic sedimentation from La Manga Formation (Oxfordian), Neuquén Basin, Mendoza, Argentina

    Science.gov (United States)

    Palma, Ricardo M.; Kietzmann, Diego A.; Bressan, Graciela S.; Martín-Chivelet, Javier; López-Gómez, José; Farias, María E.; Iglesias Llanos, María P.

    2013-11-01

    The La Manga Formation consists of marine carbonates and represents most of the sedimentary record of the Callovian-Oxfordian in the Neuquén Basin. Three localities in the southern Mendoza province were studied and their cyclicity was determined by means of facies analysis and their vertical arrangement. Facies of inner ramp, that were deposited in extremely shallow-water environments with intermittent subaerial exposures have been broken down into shallow subtidal, and intertidal-supratidal environments. Shallow subtidal facies are arranged into decimetre scale upward-shallowing cycles composed of marls, laminated or massive mudstones or bioclastic wackestones and intraclastic wackestone-packstones. Intertidal-supratidal centimetre-scale cycles consist of an upward-shallowing succession of restricted facies, overlaid by horizontal or crinkle microbial laminites, flat pebble conglomerates or breccias beds. The defined cycles show a shallowing upward trend in which the evidence of relative sea-level lowering is accepted. The interpretation of Fischer plots allowed the recognition of changes in accommodation space.

  11. Seismic reflection survey at Llancanelo region (Mendoza, Argentina) and preliminary interpretation of Neogene stratigraphic features

    Science.gov (United States)

    Osella, A.; Onnis, L.; de la Vega, M.; Tassone, A.; Violante, R. A.; Lippai, H.; López, E.; Rovere, E. I.

    2015-07-01

    A shallow multichannel seismic survey reaching depths of 700/800 m was performed for the first time in the Llancanelo Lake region (Southern Mendoza Province, Argentina), in order to depict the major Neogene sedimentary-volcanic sequences that form the final infilling of the tectonic-volcanic basin where the lake is located. The seismic survey advances on the results of previous geoelectric and electromagnetic surveys carried out at early stages of the research that reached the uppermost 80-100 m of the sequences (Quaternary), and therefore they go deeper in the subsoil. All the surveys were supported by surface and subsoil geological observations. After explaining the details of the performed seismic methodology, the obtained results are discussed, which indicate the presence of three major sedimentary units with increasing volcanic (basaltic layers) intercalations with depth, that accommodate to the geometry of the depocenter. The entire sequence encompasses most of the Neogene. This research sets the methodological basis for future, more detailed shallow seismic surveys in the region.

  12. Mineralización de talco asociada a los cuerpos ultramáficos de la Faja del Río de Las Tunas, Cordillera Frontal de Mendoza

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    Gargiulo, María Florencia

    2011-12-01

    Full Text Available Talc mineralization related to the ultramafic bodies of the Río de Las Tunas belt, Frontal Cordillera of Mendoza province. This contribution shows the main characteristics of the talc mineralization related to the Río de Las Tunas ultramafic bodies in the Salamanca Mining District, Frontal Cordillera of Mendoza province. According to the parageneses defined on the studied samples, three generations of talc were established: 1º crystallized in metaperidotites and related to the prograde stage of the regional metamorphism; 2º crystallized inreaction zones (mostly in the talc zone developed at the boundary between metaperidotites and their country-rocks.These reaction zones evidence a metasomatic process due to geochemical gradient between the ultramafic body and their country-rocks. This process was developed during the retrogression of the regional metamorphic cycle. 3º Talc present in shear-zones that cut across the ultramafic bodies. The extreme serpentinization of the ultramaficbodies is concentrated in shear-zones where the serpentine is subsequently replaced by talc ± carbonates related with a hydrothermal stage. Aqueous fluids relatively enriched in CO2 flowed through these shear-zones causing the cease of serpentine formation favoring the talc and/or carbonates. Mined talc deposits are those in shear zones and reaction zones. They are mostly industrial-, asbestine- or talcschist-type. The talc related to the hydrothermal stage can locally reach first and extra qualities.

  13. Paleoseismic investigations at the Cal thrust fault, Mendoza, Argentina

    Science.gov (United States)

    Salomon, Eric; Schmidt, Silke; Hetzel, Ralf; Mingorance, Francisco

    2010-05-01

    Along the active mountain front of the Andean Precordillera between 30°S and 34°S in western Argentina several earthquakes occurred in recent times, including a 7.0 Ms event in 1861 which destroyed the city of Mendoza and killed two thirds of its population. The 1861 event and two other earthquakes (Ms = 5.7 in 1929 and Ms = 5.6 in 1967) were generated on the Cal thrust fault, which extends over a distance of 31 km north-south and runs straight through the center of Mendoza. In the city, which has now more than 1 million inhabitants, the fault forms a 3-m-high fault scarp. Although the Cal thrust fault poses a serious seismic hazard, the paleoseismologic history of this fault and its long-term slip rate remains largely unknown (Mingorance, 2006). We present the first results of an ongoing paleoseismologic study of the Cal thrust at a site located 5 km north of Mendoza. Here, the fault offsets Late Holocene alluvial fan sediments by 2.5 m vertically and exhibits a well developed fault scarp. A 15-m-long and 2-3-m-deep trench across the scarp reveals three east-vergent folds that we interpret to have formed during three earthquakes. Successive retrodeformation of the two youngest folds suggests that the most recent event (presumably the 1861 earthquake) caused ~1.1 m of vertical offset and ~1.8 m of horizontal shortening. For the penultimate event we obtain a vertical offset of ~0.7 m and a horizontal shortening of ~1.9 m. A vertical displacement of ~0.7 m observed on a steeply west-dipping fault may be associated with an older event. The cumulative vertical offset of 2.5 m for the three inferred events is in excellent agreement with the height of the scarp. Based on the retrodeformation of the trench deposits the fault plane dips ~25° to the west. In the deepest part of the trench evidence for even older seismic events is preserved beneath an angular unconformity that was formed during a period of erosion and pre-dates the present-day scarp. Dating of samples to

  14. 78 FR 24228 - Lake Andes National Wildlife Refuge Complex, Lake Andes, SD; Final Comprehensive Conservation Plan

    Science.gov (United States)

    2013-04-24

    ... Fish and Wildlife Service Lake Andes National Wildlife Refuge Complex, Lake Andes, SD; Final Comprehensive Conservation Plan AGENCY: Fish and Wildlife Service, Interior. ACTION: Notice of availability... conservation plan and finding of no significant impact (FONSI) for the Lake Andes National Wildlife...

  15. Plantas Fósiles del Grupo Choiyoi, Cordillera Frontal a la Latitud del río Mendoza Fossil plants from the Choiyoi Group, Frontal Cordillera at the latitude of the Mendoza River

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    Magdalena Koukharsky

    2011-06-01

    Full Text Available En este trabajo se dan a conocer los primeros restos fósiles hallados en sedimentitas, cuyo componente clástico es de origen volcánico, intercaladas en la Formación Tambillos del Grupo Choiyoi, Cordillera Frontal de Mendoza. Los mismos consisten en abundantes improntas de Sphenophyta en estado de preservación regular a malo. En la zona estudiada, las rocas de la Formación Tambillos, que son dominantemente volcánicas ácidas y de edad pérmica temprana a media según correlaciones regionales, se depositaron sobre una discordancia erosiva labrada en lavas andesíticas intensamente propilitizadas que se atribuyen a la Formación Portezuelo del Cenizo. Los restos vegetales se encuentran a unos 23 metros de la base, contenidos en niveles de areniscas finas y pelitas depositadas en un ambiente fluvial (microdelta, en los bordes de un lago y fueron coetáneas con los primeros episodios de volcanismo riolítico en la región. Si bien la flora encontrada no permite definir la edad, las formas presentes son comunes en niveles del Carbonífero superior-Pérmico y Triásico de Argentina.In this contribution we report the discovery of the first fossil remains in sedimentary strata belonging to the Tambillos Formation, Choiyoi Group, Cordillera Frontal of Mendoza. In the studied area the Tambillos Formation, which is formed dominantly by acid volcanics rocks of alleged Early to the Middle Permian, were deposited over an erosive unconformity on top of propilytic andesites of the Portezuelo del Cenizo Formation. The vegetal remains were found about 23 meters from the base of the formation, hosted in fine-grained sandstones and shales that were deposited in a fluvial environment (microdelta, along the borders of a lake during the first episodes of the rhyolitic volcanism of the region. The fossil flora includes abundant, poorly preserved impressions of Sphenophyta that does not permit to assign a precise age, although these forms are common in the Upper

  16. La lacertofauna de Mendoza: lista actualizada, distribución y riqueza

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    Corbalán, Valeria

    2008-04-01

    Full Text Available La provincia de Mendoza posee una rica fauna de lagartos pertenecientes a las familias Leiosauridae, Liolaemidae, Teiidae, Scincidae y Gekkonidae. Algunos son propios del Monte, Puna, Payunia o región andina, mientras que otros poseen una amplia distribución, ocupando dos o más ecosistemas. El objetivo de este trabajo fue actualizar la lista lacertofaunística de la provincia y determinar las áreas de mayor riqueza de especies en relación a estos cuatro tipos de ecosistemas. Se utilizaron datos de procedencia de 43 especies de lagartos a partir de colecciones herpetológicas y de bibliografía. Las localidades fueron georreferenciadas y mapeadas. Una primera estimación de las áreas de mayor riqueza fue realizada sobre la base de las distribuciones de acuerdo a los puntos de colecta. En un segundo análisis, se generaron modelos predictivos de distribución utilizan-do 26 variables ambientales. Estas áreas potenciales fueron superpuestas a fin de obtener el número de especies en cuadrículas de 4,6 km x 4,6 km. Los resultados de ambos métodos indican que la mayor riqueza de especies se encuentra en la Payunia, probablemente en relación a la mayor heterogeneidad ambiental de la zona, ya que es considerada un área ecotonal entre la región fitogeográfica de la Patagonia y el Monte. Un análisis de similitud (Índice de Morisita demuestra que la similitud entre ecosistemas en cuanto a la composición de especies es baja, conformándose dos grupos: el Monte y Patagonia por un lado, y el ecosistema Andino y Puneño por otro. Mendoza province has a rich fauna of lizards that belongs to the Leiosauridae, Liolaemidae, Teiidae, Scincidae and Gekkonidae families. Some of them are typical of the Monte, Puna, Payunia or Andean region, whereas some others are widespread, inhabiting two or more ecosystems. The objective of this work is to perform an updating of the Mendoza lizard fauna and to determine the most highly species-rich areas related to

  17. The Wine Clusters of Mendoza and Serra Gaúcha: A Local Development Perspective

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    María Verónica ALDERETE

    2014-01-01

    Full Text Available This paper consists of a descriptive analysis that explains how the successful performance of the wine cluster is followed by improvements in local development indicators. To this end, certain local development indicators are proposed to describe and compare the wine clusters of Mendoza (Argentina and Serra Gaúcha (Brazil. In Argentina, the Mendoza wine cluster has stimulated the local development of the region. For its part, Serra Gaúcha is the most successful wine center in Brazil and regards Mendoza as the benchmark in terms of local development.

  18. El palacio de don Antonio de Mendoza en Guadalajara. Aspectos decorativos y formales

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    Rodríguez Rebollo, Ángel

    2002-09-01

    Full Text Available The Palace of Don Antonio de Mendoza in Guadalajara was constructed at the beginning of the sixteenth century. In spite of the absence of documentation, there are clear stylistic similarities between this palace and the Calahorra Palace (Granada and the tomb of Cardinal Mendoza. The Codex Escurialensis was used for the decoration of the first floor column capitals as well as the façade decoration.

    El Palacio de Don Antonio de Mendoza en Guadalajara fue construido a principios del XVI. Pese a no estar documentado, las similitudes estilísticas con el Palacio de la Calahorra (Granada y el sepulcro del Cardenal Mendoza son claros. El Codex Excurialensis fue usado en la decoración de los capiteles del primer piso y en la decoración de la fachada principal.

  19. Historia, historiografia y gestion cultural del patrimonio vitivinicola de Mendoza, Argentina

    National Research Council Canada - National Science Library

    Moretti-Baldin, Graciela

    2008-01-01

    La industria vitivinicola ha sido en Mendoza la base de la economia regional y sello inequivoco de su identidad, generando una verdadera cultura en torno al cultivo de la vid y a la produccion del vino...

  20. La zona de alteración Arroyo La Chilca-Zanjón del Buitre, bloque de San Rafael, Mendoza The Arroyo La Chilca-Zanjón del Buitre alteration zone, San Rafael Massif, Mendoza

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    Nora Rubinstein

    2012-06-01

    Full Text Available La zona de alteración Arroyo La Chilca-Zanjón del Buitre está ubicada en el bloque de San Rafael (35°24'8" S; 68°19'25,8" O, Mendoza. Estudios previos definieron preliminarmente que corresponde a un sistema de tipo pórfro cuprífero vinculado genéticamente al magmatismo gondwánico. Esta área de alteración se desarrolla en una secuencia compuesta por brechas ignimbríticas e ignimbritas traquiandesíticas con intercalaciones de areniscas tobáceas y coladas andesíticas a las que intruyen cuerpos subvolcánicos andesíticos y traquiandesítico-dacíticos. La litología de la secuencia volcánica así como sus características geoquímicas confirman su correlación con la sección inferior del ciclo magmático Choiyoi (Pérmico inferior. El área de alteración presenta una zona potásica con una asociación compuesta por feldespato potásico-cuarzo-magnetita. A ésta se superpone alteración fílica con una asociación de cuarzo-muscovita-pirita-(rutilo acompañada por venillas de cuarzo-pirita. Por último se reconoce una carbonatización tardía. En las proximidades de la zona de alteración aforan vetillas con mineralización de pirita-calcopirita-galena-esfalerita en ganga de cuarzo. La geoquímica de metales indica moderadas anomalías de Ag y Au y pequeñas anomalías de Cu, Mo, Pb y Zn. El análisis estadístico permite definir la existencia de un pulso mineralizante de Cu-Mo y un segundo pulso de Mo reconocido solamente en Zanjón del Buitre. Asimismo se definen dos pulsos de Zn, uno de los cuales estaría genéticamente vinculado al Cu.The Arroyo La Chilca-Zanjón del Buitre alteration zone is located in the San Rafael Massif (35°24'8" S; 68°19'25,8" W, Mendoza. Previous works defined preliminary this deposit as a porphyry copper system genetically linked to the gondwanan magmatism. This alteration zone is hosted by a sequence composed of ignimbritic breccias and ignimbrites of trachyandesitic composition with interbedded

  1. Impact of volcanic processes on the cryospheric system of the Peteroa Volcano, Andes of southern Mendoza, Argentina

    Science.gov (United States)

    Liaudat, Dario Trombotto; Penas, Pablo; Aloy, Gustavo

    2014-03-01

    Soil temperatures of the active Volcanic Complex Peteroa situated in the Cordillera Principal between Chile and Argentina at 35°15‧ S and 70°35‧ W (approximately) were monitored in the area, and local geomorphology (periglacial geomorphology, presence of permafrost, and cryoforms) was studied. The present contribution also resulted in a comparison of two consecutive analyses of the volcano peak carried out with special thermocameras (AGEMA TVH 550, FUR P660) in order to study the thermal range of different hot and cold sites selected in 2009. The thermocameras were used ascending by foot and also during flights with a Cessna 180. A night expedition to the volcanic avalanche caldera, at up to 3900 m asl (approximately), completed the monitoring activity of 2010. Hot zones were associated to present volcanism and cold zones to the presence of glacier ice and shadowy slopes with possible presence of permafrost. Identifying and mapping uncovered and covered ice was possible with the help of monitoring and geomorphological interpretation related to the upper englacement, which is severely affected by volcanism. Glaciers are retreating toward the north or approaching the rims of the volcanic avalanche caldera leaving islands of ice associated with superficial permafrost. The cryogenic area with slope permafrost was identified through active protalus and sedimentary cryogenic slopes. Craters have undergone considerable thermal changes in comparison to the year 2009; and new, much more vigorous fumaroles have appeared in hot areas detected in 2009 following a tendency toward the west. New subaquatic heat columns that appeared in crater 3, crater walls, and glaciated areas vanished, supplying cold water and thus contributing to the formation of a new lake in crater 4. A possible post-seismic shift of the volcanic activity may provide geodynamical evidence of the changes registered in other areas after the earthquake of 27 February 2010.

  2. Discontinuity surfaces in the Lower Cretaceous of the high Andes (Mendoza, Argentina): Trace fossils and environmental implications

    Science.gov (United States)

    Mangano, M. G.; Buatois, L. A.

    The paleoecologic and paleoenvironmental significance of trace fossils related to discontinuity surfaces in the Lower Cretaceous marine deposits of the Aconcagua area are analysed here. Carbonate-evaporite shoaling-upward cycles, developed by high organic production in a shallow hypersaline restricted environment, make up the section. Two types of cycles are defined, being mainly distinguished by their subtidal unit. Cycle I begins with a highly dolomitized lower subtidal unit (Facies A), followed upward by an intensely bioturbated upper subtidal unit (Facies B). The nodular packstone facies (B 1) is capped by a discontinuity surface (firmground or hardground) and occasionally overlain by an oystreid bed (Facies C). Cycle II is characterized by a pelletoidal subtidal unit (Facies B 2) with an abnormal salinity impoverished fauna. Both cycles end with intertidal to supratidal evaporite deposits (Facies D and E, respectively). Attention is particularly focused on cycle I due to its ichologic content. The mode of preservation and the distribution of trace fossils in nodular packstone facies are controlled by original substrate consolidation. Thalassinoides paradoxicus (pre-omission suite) represents colonization in a soft bottom, while Thalassinoides suevicus (omission suite pre-lithification) is apparently restricted to firm substrates. When consolidation processes are interrupted early, only an embryonic hard-ground that represents a minor halt in sedimentation was developed. Sometimes, consolidation processes continued leading to an intraformational hardground. Colonization by Trypanites solitarius (omission suite post-lithification) and Exogyra-like oystreids possibly characterizes hard substrate stage. When two discontinuity surfaces follow closely, a post-omission suite may be defined in relation to the lower cemented surface. As trace fossils are so closely related to changes in the degree of bottom lithification, they prove to be very useful as indicators of substrate evolution. The presence of discontinuity surfaces, evidenced by trace fossil association, suggests changes of sedimentary rate and environmental conditions that should be taken into account in future studies seeking to erect depositional models for these Cretaceous deposits.

  3. Comercio y producción en el proceso de desarrollo capitalista en la provincia de Mendoza, Argentina, 1850-1915, De fábrica de carne y grasa a fábrica de vinos

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    Rodolfo Richard-Jorba

    2010-06-01

    Full Text Available El trabajo estudia los dos modelos económicos y sociales que tuvieron vigencia en Mendoza entre 1870 y 1915. El primero, de ganadería comercial con agricultura subordinada, estaba centrado en el negocio de compra de ganado en el este del país, su engorde en los oasis mendocinos y su exportación a Chile. La modernización capitalista impuso el modelo agroindustrial vitivinícola orientado al mercado interno formando una de las primeras economías regionales de Argentina. El análisis de los modelos muestra las características centrales de cada uno y el proceso de grandes transformaciones económicas, sociales, políticas y territoriales que experimentó la provincia.This paper studies the two economical and social models that were in vogue in Mendoza between 1870 and 1915 which was oudined by the author's research. The commercial livestock with subordinate agriculture was centered on the buying of cattle in the eastern part of the country, its fattening in the oasis of Mendoza and its export to Chile. The capitalist modernization imposed the viticulture agro industrial model directed to the internal market. This model developed one of the regional economy of Argentine. The analysis of these two models shows the principal characteristics of each and the process of great economical, social, politics and territorial transformations of the province.

  4. Western Slope of Andes, Peru

    Science.gov (United States)

    2008-01-01

    Along the western flank of the Andes, 400 km SE of Lima Peru, erosion has carved the mountain slopes into long, narrow serpentine ridges. The gently-sloping sediments have been turned into a plate of worms wiggling their way downhill to the ocean. The image was acquired September 28, 2004, covers an area of 38 x 31.6 km, and is located near 14.7 degrees south latitude, 74.5 degrees west longitude. The U.S. science team is located at NASA's Jet Propulsion Laboratory, Pasadena, Calif. The Terra mission is part of NASA's Science Mission Directorate.

  5. The ANDES Deep Underground Laboratory

    CERN Document Server

    Bertou, X

    2013-01-01

    ANDES (Agua Negra Deep Experiment Site) is a unique opportunity to build a deep underground laboratory in the southern hemisphere. It will be built in the Agua Negra tunnel planned between Argentina and Chile, and operated by the CLES, a Latin American consortium. With 1750m of rock overburden, and no close- by nuclear power plant, it will provide an extremely radiation quiet environment for neutrino and dark matter experiments. In particular, its location in the southern hemisphere should play a major role in understanding dark matter modulation signals.

  6. Urban mobility regulation in metropolitan area of Mendoza

    Directory of Open Access Journals (Sweden)

    Lía Martínez

    2016-11-01

    Full Text Available Achieving the paradigm of sustainable urban mobility requires institutional capacities, appropriate policies and a regulatory framework that contains them. This work aims to contribute to the knowledge of the regulation of urban mobility in the metropolitan area of Mendoza. To this end, the current mobility regulations are assessed through indicators that are classified into three key areas: institutional and political organization, urban system and financial setup. The purpose is to account for the existence, or not, of regulatory capacities contained in the paradigm of sustainable mobility. Among the results, the absence of a policy of sustainable urban mobility is noteworthy, as well as the lack of sectorial coordination. Also of note is the absence of coordination between the urban planning system and the public transport provision. Lastly, in the financial sector, the results point to a promotion of sustainable transport modes but without such an explicit purpose.

  7. Quaternary basaltic volcanism in the Payenia volcanic province, Argentina

    DEFF Research Database (Denmark)

    Søager, Nina

    The extensive Quaternary volcanism in the Payenia volcanic province, Mendoza, Argentina, is investigated in this study by major and trace element analyses, Sr, Nd, Hf and Pb-isotopic analyses and Zr-Hf isotope dilution data on samples from almost the entire province. The samples are mainly...... in basalts from all the studied volcanic fields in Payenia is signs of lower crustal contamination indicating assimilation of, in some cases, large amounts of trace element depleted, mafic, plagioclase-bearing rocks. The northern Payenia is dominated by backarc basalts erupted between late Pliocene to late...

  8. Graptolitos ordovícicos en el Sur de la Cordillera frontal de Mendoza

    Directory of Open Access Journals (Sweden)

    Hugo Tickyj

    2009-04-01

    Full Text Available En el flanco sudoriental de la Cordillera Frontal mendocina aflora un conjunto plegado de metasedimentitas conocido como Formación Las Lagunitas, cuyos afloramientos se extienden entre los ríos Diamante por el sur y Tunuyán por el norte, alcanzando un ancho máximo de 15 km a la latitud del volcán Maipo. El perfil estudiado en el arroyo Cortaderas (34º23'S está compuesto por una secuencia silicoclástica marina integrada por tres conjuntos litológicos, que de este a oeste son: a areniscas gruesas a medias, bien seleccionadas, y areniscas conglomerádicas, b vaques de grano grueso a fino y c areniscas finas a medias, con intercalaciones de pelitas negras laminadas. En la última unidad fueron colectados graptolitos en regular estado de preservación. Su estudio sistemático permitió definir una asociación correspondiente a la Biozona de Climacograptus bicornis, por lo que la Formación Las Lagunitas es asignada al Ordovícico Superior (Sandbiano o Caradociano. La completa extensión cronoestratigráfica de la Formación Las Lagunitas no ha sido establecida, debido a que en el perfil estudiado no es clara la relación entre la unidad portadora de graptolitos y el resto de la secuencia. Este registro de graptolitos en el sur de la Cordillera Frontal mendocina constituye un aspecto novedoso para el análisis del Ordovícico, con implicancias en el contexto de la evolución tectónica de las cuencas sedimentarias ordovícicas del oeste argentino.Outcrops of a folded sedimentary unit known as the Las Lagunitas Formation lie along the southeastern part of the Frontal Cordillera of Mendoza Province. The main exposures of the unit lie between the Diamante River in the south and Tunuyán in the north, reaching 15 km wide at the latitude of the Maipo volcano. At the Cortaderas Creek (34º23'S the studied section is a marine siliciclastic sequence comprising three lithological units: a well-sorted, coarse- to medium-grained sandstones and

  9. Geología de la región del Cerro Guanaquero, Río Diamante, Mendoza Geology of Cerro Guanaquero region, Diamante River, Mendoza

    Directory of Open Access Journals (Sweden)

    Federico Fuentes

    2008-03-01

    Full Text Available El estudio realizado presenta nuevos datos sobre un sector poco conocido de la Cordillera Principal de Mendoza, en la alta cuenca del río Diamante en las adyacencias del cerro Guanaquero, y los primeros datos geocronológicos de sus rocas volcánicas. Las unidades geológicas presentes en el área se dividen en cuatro grupos principales: secuencias sedimentarias mesozoicas marinas y continentales intensamente plegadas y falladas; intrusivos y volcanitas intermedias de edad neógena; rocas volcánicas pliocenas a recientes de composición intermedia a básica, y depósitos cuaternarios inconsolidados. El cerro Guanaquero, un estratovolcán pliocuaternario intensamente erosionado por glaciares pleistocenos, con sus 4.841 metros es el rasgo orográfico más prominente. Está constituido esencialmente por andesitas grises porfíricas, piroxénicas a biotíticas. Intercaladas con las coladas andesíticas se presentan depósitos piroclásticos, aglomerados volcánicos, ignimbritas y basaltos. La datación de una andesita por el método K-Ar en roca total arrojó una edad de 1,4 ± 0,1 Ma. La deformación ándica comenzó en forma de una faja plegada y corrida de piel fina, con pliegues por despegue en el sector occidental y por propagación de falla en el oriental. La compresión al oeste de los 69º47´O terminó por invertir la fallas normales del rift mesozoico. A lo largo de este meridiano se encuentra la falla más importante de la región, la que se ha correlacionado con la falla Malargüe, bien desarrollada en latitudes más australes. Esta falla limita la faja plegada y corrida del Aconcagua, de naturaleza epidérmica, y la faja plegada y corrida de Malargüe, controlada por la inversión tectónica del basamento. El volcanismo fue muy intenso en el Plioceno y el Cuaternario, correspondiendo a un período de empinamiento de la placa oceánica subducida, en el que la región ha sido levantada pasivamente. La alta resistencia a la erosión de

  10. Aconcagua peak geodynamics from GPS observations, Mendoza, Argentina: preliminary results

    OpenAIRE

    2009-01-01

    In 2005, the SIGMA Program (Mount Aconcagua GNSS Research System) was implemented to investigate the geodynamics of the Aconcagua mountain region in the Central Andes. For this purpose, a continuously recording GPS station, ACON, was installed on the summit of Mount Aconcagua at 6.292 m a.s.l. The installation required special technology to support the equipment under extreme climatic conditions. The power supply system was optimized in 2008, so that a greater quantity of d...

  11. Subsurface architecture of Las Bombas volcano circular structure (Southern Mendoza, Argentina) from geophysical studies

    Science.gov (United States)

    Prezzi, Claudia; Risso, Corina; Orgeira, María Julia; Nullo, Francisco; Sigismondi, Mario E.; Margonari, Liliana

    2017-08-01

    The Plio-Pleistocene Llancanelo volcanic field is located in the south-eastern region of the province of Mendoza, Argentina. This wide back-arc lava plateau, with hundreds of monogenetic pyroclastic cones, covers a large area behind the active Andean volcanic arc. Here we focus on the northern Llancanelo volcanic field, particularly in Las Bombas volcano. Las Bombas volcano is an eroded, but still recognizable, scoria cone located in a circular depression surrounded by a basaltic lava flow, suggesting that Las Bombas volcano was there when the lava flow field formed and, therefore, the lava flow engulfed it completely. While this explanation seems reasonable, the common presence of similar landforms in this part of the field justifies the need to establish correctly the stratigraphic relationship between lava flow fields and these circular depressions. The main purpose of this research is to investigate Las Bombas volcano 3D subsurface architecture by means of geophysical methods. We carried out a paleomagnetic study and detailed topographic, magnetic and gravimetric land surveys. Magnetic anomalies of normal and reverse polarity and paleomagnetic results point to the occurrence of two different volcanic episodes. A circular low Bouguer anomaly was detected beneath Las Bombas scoria cone indicating the existence of a mass deficit. A 3D forward gravity model was constructed, which suggests that the mass deficit would be related to the presence of fracture zones below Las Bombas volcano cone, due to sudden degassing of younger magma beneath it, or to a single phreatomagmatic explosion. Our results provide new and detailed information about Las Bombas volcano subsurface architecture.

  12. ESTRATEGIAS ALIMENTARIAS Y DE SUBSISTENCIA PREHISPÁNICA EN EL CENTRO-OESTE DE MENDOZA: CONSUMO Y DESCARTE EN EL SITIO ARQUEOLÓGICO AGUA AMARGA / Food and subsistence strategies in the prehispanic Mendoza Midwest: Consumption and discard at Agua Amarga

    Directory of Open Access Journals (Sweden)

    María José Ots

    2011-12-01

    Full Text Available Se presenta el análisis de un depósito de desechos asociados a la alimentación en Agua Amarga (departamento de Tupungato, en el Centro Oeste de la provincia de Mendoza. Agua Amarga es un sitio residencial de actividades múltiples ubicado en el piedemonte del Valle de Uco, a 1000 msnm. Los fechados obtenidos sobre cerámica y restos vegetales del contexto lo ubican en el período tardío y de dominación incaica regional. El propósito del trabajo es estudiar estrategias de procesamiento, consumo y descarte de alimentos que asimismo contribuyan a la discusión sobre las estrategias de subsistencia prehispánicas en el Norte y Centro de Mendoza. Se aplican métodos y técnicas específicos para la identificación y el análisis de los restos, y se proponen hipótesis alternativas sobre dicho contexto. Los materiales recuperados, la mayoría de ellos termoalterados y muy fragmentados, incluyen macrorrestos arqueobotánicos (principalmente Zea mays y Phaseulus vulgaris, restos óseos (algunos elementos identificados como Lama sp., fragmentos de distintos recipientes cerámicos y de artefactos de molienda.  Finalmente, se discuten prácticas asociadas con la alimentación y la subsistencia, con especial referencia a la producción y consumo de maíz en el área.   Palabras clave: alimentación, subsistencia, maíz, Mendoza   Abstract We present the study of a refuse deposit associated with feeding activities in the archaeological site Agua Amarga (Tupungato department, Middle West of Mendoza province. This is a residencial site of multiple activities located in the foothill in Valle de Uco, to 1000 masl. We dated ceramics and vegetal remains that locate the context in the late period and during regional inca domination. Our goal is to study strategies of processing, consumption and discarding of foods that also contribute in the discussion on the prehispanic strategies of subsistence in the North and Center of Mendoza province. In this paper

  13. Scientific development and modern wine industry: the origins and consolidation of Enology Station of Mendoza (Argentina, 1904-1920 Desarrollo científico e industria vitivinícola moderna: orígenes y consolidación de la Estación Enológica de Mendoza (Argentina, 1904- 1920

    Directory of Open Access Journals (Sweden)

    Florencia Rodríguez Vázquez

    2009-01-01

    Full Text Available In this article we propose to undertake a reconstruction of the development of the 'Estación Enológica', next to 'Escuela Nacional de Vitivinicultura', between 1904 to 1920 in Mendoza province. This study is of vital importance as we consider this place was a pioneer center in the achievement of scientific and technical studies. These were the basis for the consolidation of quality wine industry , which had many shortcomings by then, and they triggered changes in Mendoza's agroindustry. Besides, Estación Enológica became a meeting place for people who graduated from that school to share experiences and concerns. Apart from carrying out the reconstruction of the development, we will also investigate possibilities of applying these studies to vineyardsEn el presente artículo nos proponemos realizar una reconstrucción de la trayectoria de la Estación Enológica de Mendoza, anexa a la Escuela Nacional de Vitivinicultura, desde 1904 a 1920. El mismo cobra vital importancia en tanto la consideramos un centro pionero en la realización de estudios científicos y técnicos que sirvieron de base a la consolidación de una vitivinicultura de calidad -y que por entonces contaba con múltiples deficiencias- y un impulsor de cambios técnicos en la agroindustria local. A su vez, su importancia radicaría en que fue un espacio aglutinador de las experiencias e inquietudes de los enólogos graduados de la mencionada Escuela. Por último, nos referiremos a las posibilidades de recepción y divulgación de los estudios entre los vitivinicultores

  14. Lake Andes National Wildlife Refuge Complex : Lake Andes National Wildlife Refuge, Karl Mundt National Wildlife Refuge, Lake Andes Wetland Management District : 1998 Annual narrative report

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR, Karl Mundt NWR, and Lake Andes WMD outlines Refuge accomplishments during the 1998 calendar year. The report begins...

  15. Lake Andes National Wildlife Refuge Complex : Lake Andes National Wildlife Refuge, Karl Mundt National Wildlife Refuge, Lake Andes Wetland Management District : 1999 Annual narrative report

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR, Karl Mundt NWR, and Lake Andes WMD outlines Refuge accomplishments during the 1999 calendar year. The report begins...

  16. Lake Andes National Wildlife Refuge Complex : Lake Andes National Wildlife Refuge, Karl Mundt National Wildlife Refuge, Lake Andes Wetland Management District : 2002 Annual narrative report

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR, Karl Mundt NWR, and Lake Andes WMD outlines Refuge accomplishments during the 2002 calendar year. The report begins...

  17. Lake Andes National Wildlife Refuge Complex : Lake Andes National Wildlife Refuge, Karl Mundt National Wildlife Refuge, Lake Andes Wetland Management District : 2001 Annual narrative report

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR, Karl Mundt NWR, and Lake Andes WMD outlines Refuge accomplishments during the 2001 calendar year. The report begins...

  18. Lake Andes National Wildlife Refuge Complex : Lake Andes National Wildlife Refuge, Karl Mundt National Wildlife Refuge, Lake Andes Wetland Management District : 1994 Annual narrative report

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR, Karl Mundt NWR, and Lake Andes WMD outlines Refuge accomplishments during the 1994 calendar year. The report begins...

  19. Lake Andes National Wildlife Refuge Complex : Lake Andes National Wildlife Refuge, Karl Mundt National Wildlife Refuge, Lake Andes Wetland Management District : 1997 Annual narrative report

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR, Karl Mundt NWR, and Lake Andes WMD outlines Refuge accomplishments during the 1997 calendar year. The report begins...

  20. Lake Andes National Wildlife Refuge Complex : Lake Andes National Wildlife Refuge, Karl Mundt National Wildlife Refuge, Lake Andes Wetland Management District : Updated- 2003 annual narrative report

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR, Karl Mundt NWR, and Lake Andes WMD outlines Refuge accomplishments during the 2003 calendar year. The report begins...

  1. Lake Andes National Wildlife Refuge Complex : Lake Andes National Wildlife Refuge, Karl Mundt National Wildlife Refuge, Lake Andes Wetland Management District : 1995 Annual narrative report

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR, Karl Mundt NWR, and Lake Andes WMD outlines Refuge accomplishments during the 1995 calendar year. The report begins...

  2. Lake Andes National Wildlife Refuge Complex : Lake Andes National Wildlife Refuge, Karl Mundt National Wildlife Refuge, Lake Andes Wetland Management District : 2000 Annual narrative report

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR, Karl Mundt NWR, and Lake Andes WMD outlines Refuge accomplishments during the 2000 calendar year. The report begins...

  3. Lake Andes National Wildlife Refuge Complex : Lake Andes National Wildlife Refuge, Karl Mundt National Wildlife Refuge, Lake Andes Wetland Management District : 1996 Annual narrative report

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR, Karl Mundt NWR, and Lake Andes WMD outlines Refuge accomplishments during the 1996 calendar year. The report begins...

  4. Lake Andes NWR Water Use Report- 1979

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This report contains locations and water use at Lake Andes NWR for 1979. General water uses are discussed for 1979 for each unit, impoundment data is tabulated...

  5. Lake Andes NWR Water Use Report- 2010

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This report contains locations and water use at Lake Andes NWR for 2010. Short forms are supplied for the years water use report / management plan. These forms cover...

  6. Lake Andes NWR Water Use Report- 1958

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This report contains locations and water use at Lake Andes NWR for 1958. The report highlights the weather, water, habitat, and wildlife conditions for the year of...

  7. Lake Andes NWR Water Use Report- 1987

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This report contains locations and water use at Lake Andes NWR for 1987. General water uses are discussed for 1987 for each unit, impoundment data is tabulated...

  8. Lake Andes NWR Water Use Report- 1984

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This report contains locations and water use at Lake Andes NWR for 1984. General water uses are discussed for 1984 for each unit, impoundment data is tabulated...

  9. Lake Andes NWR Water Use Report- 1985

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This report contains locations and water use at Lake Andes NWR for 1985. General water uses are discussed for 1985 for each unit, impoundment data is tabulated...

  10. Lake Andes NWR Water Use Report- 1983

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This report contains locations and water use at Lake Andes NWR for 1983. General water uses are discussed for 1983 for each unit, impoundment data is tabulated...

  11. Lake Andes NWR Water Use Report- 1986

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This report contains locations and water use at Lake Andes NWR for 1986. General water uses are discussed for 1986 for each unit, impoundment data is tabulated...

  12. Lake Andes NWR Water Use Report- 1982

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This report contains locations and water use at Lake Andes NWR for 1982. General water uses are discussed for 1982 for each unit, impoundment data is tabulated...

  13. Lake Andes NWR Water Use Report- 1971

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This report contains locations and water use at Lake Andes NWR for 1971. General water uses are discussed for 1971 for each unit, impoundment data is tabulated...

  14. Discussion of "The Internal Correlation: Its Applications in Statistics and Psychometrics" by G. W. Joe and J. L. Mendoza.

    Science.gov (United States)

    Bargmann, Rolf

    1989-01-01

    Use of internal correlation for statistical analysis--as proposed by G. W. Joe and J. L. Mendoza (1989)--is discussed. Use of the bootstrap technique to deal with the distributional problem is questioned. Joe and Mendoza attempt the interpretation of the two linear composites that produce the largest internal correlation. (TJH)

  15. Discussion of "The Internal Correlation: Its Applications in Statistics and Psychometrics" by G. W. Joe and J. L. Mendoza.

    Science.gov (United States)

    Bargmann, Rolf

    1989-01-01

    Use of internal correlation for statistical analysis--as proposed by G. W. Joe and J. L. Mendoza (1989)--is discussed. Use of the bootstrap technique to deal with the distributional problem is questioned. Joe and Mendoza attempt the interpretation of the two linear composites that produce the largest internal correlation. (TJH)

  16. La vegetación saxícola y de taludes del flanco oriental del Cordón del Plata (Luján de Cuyo, Mendoza, Argentina Saxicolous and talus vegetation on the eastern slope of Cordón del Plata (Luján de Cuyo, Mendoza, Argentina

    Directory of Open Access Journals (Sweden)

    Eduardo Méndez

    2010-06-01

    Full Text Available A fin de complementar estudios de vegetación de la vertiente oriental del Cordón del Plata de los altos Andes Centrales de Luján de Cuyo, Mendoza, Argentina, se determina y analiza, las comunidades saxícolas y de taludes a lo largo de un gradiente altitudinal de 1200 a 3200 m s.n.m. El estudio fitosociológico revela la existencia de 17 comunidades vegetales: 7 saxícolas y 12 de taludes, caracterizadas por especies diagnósticas exclusivas, diferenciales y acompañantes. Análisis de dispersión y de conglomerados permiten, utilizando las altitudes y temperaturas, diferenciar a 3 grupos de comunidades las que se corresponden, y confirman el análisis fitosociológico, a los ambientes fitogeográficos del Monte, Andino y Andino Superior. Existe una fuerte relación florística-ecológica de estas comunidades saxícolas y de taludes con los espectros de los ambientes fitogeográficos, las formas de vida y los orígenes de las especies desarrolladas en el gradiente altitudinal del área analizada. Se registraron 63 especies endémicas: 7 endemismos locales, 28 regionales y 26 nacionales. Las comunidades vegetales obtenidas se comparan con la de otras áreas de Argentina.In order to supplement studies of the vegetation on the eastern slope of Cordón del Plata in the high Central Andes of Luján de Cuyo, Mendoza, Argentina, saxicolous and talus plant communities are determined and analyzed along the altitudinal gradient from 1200 to 3200 m a. s. l. Phytosociological study reveals occurrence of 17 plant communities: 7 saxicolous and 12 talus communities, characterized by exclusive, differential and accompanying diagnostic species. Conglomerate and dispersal analyses, using altitude and temperature, allow differentiation of three groups of communities which correspond, corroborating the phytosociological analysis, to the Monte, Andean and High Andean phytogeographic environments. There is a strong floristic-ecological relationship of these

  17. Orographic effects related to deep convection events over the Andes region

    Science.gov (United States)

    Hierro, R.; Pessano, H.; Llamedo, P.; de la Torre, A.; Alexander, P.; Odiard, A.

    2013-02-01

    In this work, we analyze a set of 39 storms which took place between 2006 and 2011 over the South of Mendoza, Argentina. This is a semiarid region situated at mid-latitudes (roughly between 32S and 36S) at the east of the highest Andes tops which constitutes a natural laboratory where diverse sources of gravity waves usually take place. We consider a cultivated subregion near San Rafael district, where every summer a systematic generation of deep convection events is registered. We propose that the lift mechanism required to raise a parcel to its level of free convection is partially supplied by mountain waves (MWs). From Weather Research and Forecasting (WRF) mesoscale model simulations and radar network data, we calculate the evolution of convective available potential energy and convective inhibition indices during the development of each storm. Global Final Analysis is used to construct initial and boundary conditions. Convective inhibition indices are compared with the vertical kinetic energy capable of being supplied by the MWs, in order to provide a rough estimation of this possible triggering mechanism. Vertical velocity is chosen as an appropriate dynamical variable to evidence the presence of MWs in the vicinity of each detected first radar echo. After establishing a criterion based on a previous work to represent MWs, the 39 storms are split into two subsets: with and without the presence of MWs. 12 cases with considerable MWs amplitude are retained and considered. Radar data differences between the two samples are analyzed and the simulated MWs are characterized.

  18. La producción y función de la cerámica indígena durante la dominación incaica y la colonia en Mendoza (Argentina The production and function of indigenous ceramic during the inca domination and the colony in Mendoza, Argentina

    Directory of Open Access Journals (Sweden)

    Cristina Prieto Olavarría

    2012-07-01

    Full Text Available A partir del análisis tecnológico de las elecciones de manufactura tomadas para confeccionar la cerámica Viluco (provincia de Mendoza, Argentina, evaluamos aspectos vinculados a los contextos producción, uso y consumo de las vasijas, los que estuvieron influenciados por la dominación que ejercieron incas y espanoles sobre la población local huarpe entre los siglos XV y XVII. Los resultados obtenidos permiten sostener que la cerámica Viluco surgió y se desarrolló bajo presiones sociales, políticas, económicas y simbólicas impuestas por los incas y que, si bien su producción fue descentralizada en los contextos del valle de Mendoza, refleja las relaciones sostenidas entre esta población y los dominadores. Por otra parte, su función estuvo ligada al estatus e identidad, ya que se usó como mediador visual entre las jefaturas locales y entre éstas y los dominadores. Este desempeno se proyectó al período colonial, cuando este conjunto permitió a los grupos huarpe mantener un nexo de identidad con la anterior dominación inca, si bien existen indicadores de que la producción alfarera pudo estar bajo control espanol.Aspects related to production environments, use and consumption of Viluco ceramics from Mendoza province, Argentina, are evaluated on the basis of the technological analysis of manufacturing choices, which were influenced by the Inca and Spanish domination of the local Huarpe population between the fifteenth and sixteenth centuries AD. The results show that Viluco pottery emerged and developed under social, political, economic and symbolic pressure imposed by the Incas, and while its production was decentralized in the Mendoza valley contexts, it reflects sustained relationships among this population and the dominant power. The function of the pottery was linked to status and identity, and was used as a visual mediator among local leaders and between these and their Inca rulers. This performance was continued into the

  19. Rural workers in the Uco Valley (Mendoza, Argentina Asalariados rurales en el Valle de Uco (Mendoza, Argentina

    Directory of Open Access Journals (Sweden)

    Elena Mingo

    2009-01-01

    Full Text Available This paper analyze labor insertion of agricultural workers in the Uco Valley, Mendoza. We assume that agricultural labor market characteristics determine labor insertions generating occupational social practices which arises in dispositions, layouts and strategies of these workers. These workers are characterized by his insertion in precarious and/or unstable jobs, by getting low and discontinuous incomes and by the frequent social vulnerability of the households they belongs to. This article describes labor relations as a social field in which Uco Valley's agricultural workers participate. Then, we analyze some elements associated to socialization at work, a relevant aspect to understand social relationships that underlies the constitution of agricultural labor market and dispositions of agricultural workers. Next, we describe and analyze some elements that condition labor insertion forming agricultural worker's labor strategies. Finally, we examined household influence in labor insertion of their members.El objetivo de este artículo es analizar la inserción laboral de los trabajadores agrícolas asalariados en el Valle de Uco, provincia de Mendoza. Partimos de entender que las características del mercado de trabajo agrícola condicionan las inserciones laborales generando prácticas sociales ocupacionales que se expresan en disposiciones, orientaciones y estrategias de estos trabajadores. Estos trabajadores se caracterizan por una inserción laboral precaria y/o inestable y la percepción de ingresos insuficientes y discontinuos, a lo que se suman las frecuentes condiciones de vulnerabilidad social de sus hogares de pertenencia. El artículo contiene una descripción de la esfera laboral en tanto campo social en que se desempeñan los trabajadores agrícolas en el Valle de Uco. Luego analizamos algunos elementos vinculados a la socialización en el trabajo, aspecto importante para comprender las relaciones sociales que fundamentan la

  20. Isotopic composition of river waters and early stage carbonates crusts along an elevation transect at 33 degrees south latitude, southern central Andes

    Science.gov (United States)

    Hoke, G. D.; Williams, K.; Garzione, C. N.; Araneo, D.; Strecker, M. R.

    2008-12-01

    We assess the quality of the transfer of elevation specific isotopic information into the rock record by comparing the stable isotopic composition of Quaternary to recent authigenic carbonates and river waters along a 3000 m elevation transect across the Andes at 33°S. Carbonate and water samples are from the Río Aconcagua (Chile) and Río Mendoza (Argentina) watersheds. Isotopic data from small tributaries of these rivers show similar elevation gradients on both sides of the range despite different initial moisture sources. The δ18O of authigenic carbonates correlate well with elevation and yield an elevation gradient which is shallower than that of the rivers. These data confirm that carbonate material is indeed an accurate recorder of information about elevation, and show that in some instances, different moisture sources do not result in drastically different isotope-elevation gradients.

  1. Capitalist modernization and poverty in Mendoza, Argentina. Agroindustrial development and working class life conditions, 1890-1918

    Directory of Open Access Journals (Sweden)

    Rodolfo Richard-Jorba

    2012-08-01

    Full Text Available During the last decade of the XIX century and the first two decades of the XX, the argentine province of Mendoza underwent substantial territorial, economical and society changes due to the advance of the capitalism, that formed one of the first regional economy of the country: the viticulture industry. The capitalist development produced an unknown economic expansion in which all the indicators increased in number: extent of the agrarian cultivation, wine vault installment, raise of the capacity of wine elaboration, technological improvement. Pertaining to society land subdivision, enterprise class arising and enlargement of the middle class. However, the majority of the popular sectors, enlarged by the overseas immigration, suffered life conditions characterized by low incomes which were maintained in face values during the studied period, and home and health problems that derived in the propagation of serious contagious disease and high children death rate. This article shows the contrast between a powerful productive forces development and the miserable conditions of population life.

  2. New postcranial remains of large toxodontian notoungulates from the late Oligocene of Mendoza, Argentina and their systematic implications

    Directory of Open Access Journals (Sweden)

    Santiago Hernández Del Pino

    2017-03-01

    Full Text Available During the last decade, the Deseadan (late Oligocene Quebrada Fiera locality, Mendoza Province, Argentina, has provided a large amount of mammal remains. Taxonomic studies have shown the presence of faunal elements common with other Deseadan associations from Patagonia and lower latitudes (Salla, Bolivia, as well as endemic taxa of different groups of mammals (Notohippidae, Leontiniidae, Homalodotheriidae, Hegetotheriidae, and Metatheria and even a gastropod. In this work, we present a taxonomic and phylogenetic analysis of a set of postcranial fossils of three families of the suborder Toxodontia (Notoungulata. The postcranial elements are assigned to taxa previously recognized at Quebrada Fiera, such as the leontiniid Gualta cuyana and the homalodotheriid Asmodeus petrasnerus, but also to the family Toxodontidae that is represented by Proadinotherium sp. and another larger toxodontid; a few dental remains of Proadinotherium are also included as this is the first time that toxodontids from Quebrada Fiera are described. In the case of A. petrasnerus, an almost complete calcaneum allows us to expand the diagnosis of this taxon. The bones assigned to G. cuyana enlarge the anatomical knowledge of this species. In turn, the presence of the genus Proadinotherium extends its geographic distribution in Argentina and adds to the extra-Patagonian record of P. saltoni from Salla, Bolivia. Phylogenetic results do not differ much from previous analyses using postcranial characters, and the obtained consensus trees show low node supports. The various phylogenetic analyses performed here provide a more robust framework to interpret the relationships of the studied taxa.

  3. Eduardo Mendoza y la parodia del género de la novela policiaca

    OpenAIRE

    Brezmes Calderón, Nicolás

    2015-01-01

    El tema que se va a tratar en estas páginas es el tratamiento humorístico que hace Eduardo Mendoza respecto a los elementos del género de la novela policíaca, en sus obras El misterio de la cripta embrujada (1979), El laberinto de las aceitunas (1982) y La aventura del tocador de señoras (2001). Se han elegido estas tres obras para el trabajo porque conforman una trilogía donde queda patente la maestría de Mendoza para narrar una historia a través del humor, y porque la primera de ellas supus...

  4. Flujos de detritos recientes en la cordillera frontal de Mendoza: Un ejemplo de riesgo natural en la ruta 7 Recent debris flows in the Frontal Cordillera of Mendoza: an example of natural risk on the Road 7

    Directory of Open Access Journals (Sweden)

    Emmanuel Wick

    2010-06-01

    Full Text Available Se expone un estudio sobre los flujos de detritos ocurridos en enero de 2005, en el km 1.118,5 de la ruta nacional 7 en la provincia de Mendoza. La zona se ubica en la Cordillera Frontal, próxima al límite con la Precordillera. Se realizó un mapa geomorfológico detallado, sobre la base de una imagen Quickbird del año 2006. Además, se hicieron cálculos de volúmenes, velocidades y caudales, con mediciones en el campo y con ayuda de un sistema de información geográfico (SIG. El estudio de la geomorfología permitió proponer tres escenarios para el caso de un nuevo evento, a partir de los cuáles se creó un mapa de susceptibilidad a los flujos de detritos para el tramo de ruta analizado. Finalmente, se proponen medidas de protección y de mitigación ante la posibilidad de recurrencia de estos eventos en el sector.In this paper is presented a study dealing with the debris flows that reached the national road 7 in January 2005, in the km 1,118.5, Mendoza province. The area is located in the Frontal Cordillera near the limit of the Precordillera. A detailed geomorphologic map has been realized for this study using a Quickbird satellite imagery of the year 2006. Various calculations of volumes, velocities and peak discharges have been performed with the field data and using a geographic information system (GIS. The geomorphologic survey has permitted to propose three propagation scenarios in case of a new event. These allowed creating a map of debris flows susceptibility for the stretch of the road that has been studied. Finally, it has been proposed protection and mitigation measures, based on the results of the study, to protect the road from a new event.

  5. Fish Population Investigation: Lake Andes, Charles Mix County

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — Brief background on Lake Andes fishing history, and data on current fish populations. Lake Andes was a much larger body of water prior to the construction of an...

  6. Formalized morphostructural zoning of the mountain zone of the Andes

    Energy Technology Data Exchange (ETDEWEB)

    Gabrielov, A.M.; Gvishiani, A.D.; Zhidkov, M.P.

    1982-01-01

    A plan is presented for morphostructural zoning of the Andes compiled according to formalized signs for purposes of seismic forecasting. Characteristics are presented for the basic morphostructural subdivisions of the Andes.

  7. Recreational Fishery Management Plan for Lake Andes National Wildlife Refuge

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — Current condition of lake Andes (1996) and highlights potential problems and recommendations for improving the lake as a hatchery. Lake Andes was a much larger body...

  8. Fishery Management Plan for Lake Andes National Wildlife Refuge

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — Lake Andes was a much larger body of water prior to the construction of an artificial outlet structure that lowered the water level by 13 feet. Since Lake Andes is...

  9. Rincón del Atuel-1 (San Rafael, Mendoza: evidencias arqueológicas e implicancias regionales Rincon Del Atuel-1 (San Rafael, Mendoza: Archaeological Evidence And Regional Implications

    Directory of Open Access Journals (Sweden)

    Adolfo Gil

    2008-12-01

    Full Text Available El sitio Rincón del Atuel 1 (RA-1 fue uno de los primeros estudiado sistemáticamente en los inicios de la arqueología del sur de Mendoza y del que se conocía solo información proveniente de la superficie. Sobre la base de excavaciones recientes se detallan las evidencias arqueológicas del sitio. Asimismo se incorporan datos disponibles de colecciones previas. Sus ocupaciones se registran en los últimos 1500-1700 años AP y mostrarían dos momentos distintos; el más tardío desde hace unos 1000-1200 años AP y el otro desde esa fecha a unos 1500-1700 años AP. El conjunto más tardío se asocia a un suelo y mostraría características de "sitio somero" mientras que el conjunto inferior se relacionaría depositacionalmente con la planicie de inundación del río Atuel por lo que presentaría mejor resolución temporal. El registro arqueobotánico y los valores isotópicos en muestras humanas avalan una dieta mixta de maíz con otras plantas silvestres al menos para el conjunto más antiguo. La evidencia no es concordante con lo esperable para un patrón semi-sedentario o sedentario propuesto previamente para entender las ocupaciones agrícolas del área. Este registro es significativo para comprender la estructura arqueológica en valles fluviales de zonas áridas, y discutir temas como la intensificación regional y el significado de los cultígenos.Rincón del Atuel-1 is an open air archaeological site located in the current alluvial valley of the Atuel River, Mendoza Province (Argentina. The site was studied during the first stage of archaeological research in southern Mendoza. However, only the surface archaeological record was studied and no information was published about the material in stratigraphic context. Recently, excavations were carried out in order to explore issues related to the Late Holocene human occupation. The results presented here show that the site was occupied from 1500-1700 14C years BP until recently (at least ca

  10. ESTUDIO ARQUEOHISTÓRICO DEL REGISTRO VÍTREO EN SITIOS MINEROS (MENDOZA, ARGENTINA (Archaeohistorical Study of the Vitreous Record in Mining Sites (Mendoza, Argentina

    Directory of Open Access Journals (Sweden)

    Osvaldo Sironi

    2017-06-01

    Full Text Available Se presentan los resultados de los análisis de los registros vítreos de los sitios Minas Paramillos Sur y Mina La Atala, localizados en la Reserva Natural Villavicencio y Divisadero Largo. A partir del conocimiento de la materialidad cultural vítrea de esta región, se evidencian patrones de consumo vinculados a diversos tipos de bebidas y productos medicinales entre la clase trabajadora minera de la Precordillera de Mendoza (Argentina. ENGLISH: Results of the analysis of the vitreous record from Minas Paramillos Sur and Mina La Atala are presented. These sites are located in the Villavicencio and Divisadero Largo natural reserves. Knowledge of the vitreous cultural material of this region allows us to show consumption patterns of various types of beverages and medicines among the mining working class of the Mendoza Precordillera, Argentina.

  11. Diversity of aquatic insects and other associated macroinvertebrates in an arid wetland (Mendoza Province, Argentina

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    Erica E. SCHEIBLER

    2013-01-01

    Full Text Available El objetivo del trabajo fue expandir la evaluación de la diversidad de insectos acuáticos y macroinvertebrados asociados a lo largo del Bañado Carilauquen, usando red de mano para la columna de agua y draga de Petersen para el bentos. Adicionalmente, se exploraron diferencias y similitudes espacio-temporales en la composición cualitativa de los ensambles de invertebrados. Se realizaron muestreos estacionales en cinco tramos del Bañado Carilauquen, desde la cabecera hasta la desembocadura. Se identificaron 47 taxa; 37 fueron insectos, principalmente Coleoptera, Diptera y Hemiptera, en ese orden. La composición de macroinvertebrados estuvo mejor condicionada por la variable espacial que por la temporal, en los extremos del gradiente espacial estudiado. Fueron detectados tres grupos faunísticos: cabecera, tramo medio y desembocadura. La mayor riqueza detectada en la cabecera se correspondió con los valores más bajos de conductividad del Bañado Carilauquen. La menor diversidad y la mayor diferencia en la composición faunística fueron observadas en la desembocadura (mayores niveles de conductividad. En el tramo medio, la riqueza fue mayor a la esperada según niveles de conductividad, debido posiblemente, a la presencia de especies transitorias.

  12. Diversity of aquatic insects and other associated macroinvertebrates in an arid wetland (Mendoza Province, Argentina)

    OpenAIRE

    2015-01-01

    The goal of this work was to expand the evaluation of diversity of aquatic insects and associated macroinvertebrates along the Bañado Carilauquen using hand net for water column and Petersen dredge for benthos. Additionally, we explored seasonal and spatial differences and similarities of macro invertebrate assemblages' qualitative composition. Samplings were conducted seasonally in five reaches of the Bañado Carilauquen, from headwaters to outlet. A total of 47 taxa were identified; 37 of th...

  13. Aconcagua peak geodynamics from GPS observations, Mendoza, Argentina: preliminary results

    Directory of Open Access Journals (Sweden)

    M. L. Mateo

    2009-12-01

    Full Text Available In 2005, the SIGMA Program (Mount Aconcagua GNSS Research System was implemented to investigate the geodynamics of the Aconcagua mountain region in the Central Andes. For this purpose, a continuously recording GPS station, ACON, was installed on the summit of Mount Aconcagua at 6.292 m a.s.l. The installation required special technology to support the equipment under extreme climatic conditions. The power supply system was optimized in 2008, so that a greater quantity of data could be recorded. This, in turn, will lead to more accurate estimates of displacement of the Aconcagua peak. Preliminary results from the ACON station indicate an average horizontal velocity of 0.023±0.0001 m/yr toward NE in 2 time windows between 2006 and 2008.

  14. Estructura de los Andes Nordpatagónicos en los cordones Piltriquitrón y Serrucho y en el valle de El Bolsón (41º 30´ - 42 º 00´ S, Río Negro Structure of the North Patagonian Andes in the Piltriquitrón and Serrucho ranges and in the El Bolsón valley (41º30´-42º00´S, Río Negro province

    Directory of Open Access Journals (Sweden)

    Raúl E. Giacosa

    2004-03-01

    Full Text Available La deformación compresiva cenozoica estructuró la vertiente argentina de los Andes Nordpatagónicos como una faja plegada y corrida con corrimientos de vergencia este y retrocorrimientos. El sector ubicado al oeste de 71º 15´O está caracterizado por la presencia de sistemas de retrocorrimientos, que en su interacción con los corrimientos vergentes hacia el este, conforman zonas triangulares. Los dos sistemas de retrocorrimientos más importantes estructuraron los cordones Piltriquitrón (2.284 m y Serrucho (2.120 m respectivamente. En el primero se reconocen tres retrocorrimientos importantes con zonas de intensa deformación, en tanto que la estructura del segundo consiste en al menos dos retrocorrimientos de rumbo norte que forman la gran escarpa occidental del cordón. Como consecuencia de la interacción entre corrimientos y retrocorrimientos, las sedimentitas del valle de El Bolsón se estructuraron como un gran sinclinal de arrastre de rumbo norte. En ambos casos estas estructuras exponen rocas ígneo-metamórficas del basamento premesozoico. El diseño cartográfico sugiere el enraizamiento en profundidad de ambos sistemas con el corrimiento Ventana-Catedral, la estructura regional que limita los sectores oeste y este de la faja plegada y corrida. Se interpreta que la estructuración descripta podría representar en profundidad un modelo de zona triangular de piel gruesa, y que su localización estaría relacionada con la inversión tectónica cenozoica de fallas normales mesozoicas, las que controlaron la distribución paleogeográfica de los depósitos volcano-sedimentarios jurásicos de la región.The Cenozoic structure of the North Patagonian Andes of Argentina (41º- 42º S is characterised by an E-verging imbricated fold and thrust belt with some important back-thrusts. The western sector (west of 71º 15´ W exhibits back-thrust systems that interact with the E-verging thrusts conforming triangular areas. There are two

  15. Programa de Desarrollo Productivo y Competitividad de la Provincia de Mendoza (AR-L1003)

    OpenAIRE

    Gobierno de Mendoza

    2005-01-01

    Presentación que da a conocer el programa de desarrollo productivo del Gobierno de Mendoza: diagnóstico, finalidad, objetivo, fases del programa, infraestructura pública, acceso al financiamiento, capacitación laboral y promoción de clusters.

  16. Programa de Desarrollo Productivo y Competitividad de la Provincia de Mendoza (AR-L1003)

    OpenAIRE

    Gobierno de Mendoza

    2005-01-01

    Presentación que da a conocer el programa de desarrollo productivo del Gobierno de Mendoza: diagnóstico, finalidad, objetivo, fases del programa, infraestructura pública, acceso al financiamiento, capacitación laboral y promoción de clusters.

  17. Petrografic description of some igneous rocks from the Cordillera of South Mendoza, in the Argentine

    NARCIS (Netherlands)

    Kuenen, Ph.H.

    1926-01-01

    Comparatively little is yet known of the intricate igneous history of the Cordillera of South Mendoza. Almost all the knowledge we have is due to the field- and stratigraphical work of Dr. H. Gerth of Leiden (bibl. 1 and 2), and the petrographic studies of Dr. H. G. Backlund (bibl. 3 and 4) on the

  18. Social boundaries and asymmetries in today's winemaking in Mendoza/Fronteras sociales y asimetrias en la vitivinicultura mendocina actual/Les frontieres sociales et les asymetries dans la viticulture actuelle de Mendoza, Argentine

    National Research Council Canada - National Science Library

    Altschuler, Barbara

    2012-01-01

    The aim of this paper is to investigate the social and symbolic boundaries of the new winemaking configuration of Mendoza, Argentina, which resulted from its restructuration and globalization from the nineties onwards...

  19. A Reply to Thomas W. Mendoza-Harrell, "The Foreign Language Laboratory and the Future of Language Teaching"

    Science.gov (United States)

    Allen, John R.

    1976-01-01

    Portions of Mendoza-Harrell's article, which is a rebuttal of an earlier article by Allen, are mentioned and criticized. Allen's earlier article discussed the efficacy of language laboratories and proposed student use of cassette recorders. (RM)

  20. A Reply to Thomas W. Mendoza-Harrell, "The Foreign Language Laboratory and the Future of Language Teaching"

    Science.gov (United States)

    Allen, John R.

    1976-01-01

    Portions of Mendoza-Harrell's article, which is a rebuttal of an earlier article by Allen, are mentioned and criticized. Allen's earlier article discussed the efficacy of language laboratories and proposed student use of cassette recorders. (RM)

  1. El volcanismo del Terciario superior del sur de Mendoza

    Directory of Open Access Journals (Sweden)

    F. E. Nullo

    2002-06-01

    Full Text Available Se describe por primera vez la petrografía y geoquímica de unidades volcánicas terciarias del sur de la provincia de Mendoza. Se analizan la nomenclatura estratigráfica y sus edades, estableciéndose una secuencia de eventos magmáticos ocurridos durante el Neógeno, comenzando con la evolución de un retro-arco, seguido por un arco magmático más joven. Se intenta respetar la nomenclatura estratigráfica existente, sin embargo, la definición de unidades se ha realizado sobre la base de las edades radimétricas y sus edades de cristalización, más sobre sus características petrográficas. La actividad magmática se extiende desde el Oligoceno superior al Mioceno superior, correspondiendo a el Ciclo Eruptivo Molle y el Ciclo Eruptivo Huincán, y comenzó con un episodio magmático basáltico inicial (CEM. Esta actividad se generó en la corteza inferior dominada por la concentración de gabros, dioritas y rocas híbridas (granulitas máficas. Debido a un engrosamiento de la corteza como consecuencia de la actividad tectónica durante Mioceno superior o por el estancamiento de magmas o por la combinación de ambos procesos, la formación de granulitas granatíferas resultó un producto distintivo de la corteza inferior. Con el desarrollo del arco magmático (CEH en el Mioceno superior, los magmas ascendieron desde la fuente mantélica, encontrándose con una corteza inferior granatífera, perdiendo capacidad de ascenso por falta de contraste de densidades, produciéndose una fusión extendida, la homogeinización y el ascenso, en equilibrio con la corteza baja, proceso que caracteriza el volcanismo de un arco magmático.

  2. Flood Risk in Motozintla de Mendoza, Chiapas: An Approximation

    Science.gov (United States)

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

    2012-12-01

    The town of Motozintla de Mendoza (15o 22' N and 92o 15' W) is located southern Chiapas, Mexico, and it is highly exposed to flood hazards. This community has suffered the impact of two disaster events due to this natural hazard in less than ten years, the first one in 1998 and the second one in 2005. The objective of this research is to assess the level of flood risk in the community of Motozintla. The methodology consisted of four steps: (1) Identification of the level of flood hazard; (2) Vulnerability assessment considering weighted variables according to their level of incidence on the local risk conditions; (3) Preparation of risk matrices for each area exposed to floods; and 4) Cartographic representation and spatial analysis of the results. We obtained a Geographical Information System (GIS) map for each group of analyzed vulnerabilities (structural, public services, socio-economic, existing plans in case of contingencies, and risk perception) and one map associated to global vulnerability (overposing of all estimated vulnerabilities). These maps demonstrates that the local conditions of structural vulnerability have a high incidence in the generation of risk, differing from the lack of public basic services, which although unfavorable for the population, it is not a deciding factor for preserving life or housing. Another interesting result is that the lack of preparation of the community to face a disaster generates a higher risk level than the other analyzed socioeconomic conditions. The global vulnerability allowed us to determine with greater detail the flood risk levels in the community. Our results indicate that the area in Motozintla with the highest level of flood risk is located in the margins of the Xelajú river, particularly the region that was flooded in 2005, which is precisely the area where the rivers Xelajú, Allende and La Mina meet and the river flow increases. Unfortunately, the northeasters part of this zone had been populated by people

  3. Grenvillian remnants in the Northern Andes: Rodinian and Phanerozoic paleogeographic perspectives

    Science.gov (United States)

    Cardona, A.; Chew, D.; Valencia, V. A.; Bayona, G.; Mišković, A.; Ibañez-Mejía, M.

    2010-01-01

    Grenvillian crust is encountered in several basement inliers in the northern Andes of Colombia, Ecuador and Peru and is also represented as a major detrital or inherited component within Neoproterozoic to Paleozoic sedimentary and magmatic rocks. This review of the tectonic and geochronological record of the Grenvillian belt in the northern Andes suggests that these crustal segments probably formed on an active continental margin in which associated arc and back-arc magmatism evolved from ca. 1.25 to 1.16 Ga, possibly extending to as young as 1.08 Ga. The lithostratigraphic and tectonic history of the Grenvillian belt in the northern Andes differs from that of the Sunsas belt on the southwest Amazonian Craton and from the Grenvillian belt of Eastern Laurentia. It is considered that this belt, along with similar terranes of Grenvillian age in Middle America and Mexico define a separate composite orogen which formed on the northwestern margin of the Amazonian Craton. Microcontinent accretion and interaction with the Sveconorwegian province on Baltica is a feasible tectonic scenario, in line with recent paleogeographic reconstructions of the Rodinian supercontinent. Although Phanerozoic tectonics may have redistributed some of these terranes, they are still viewed as para-autocthonous domains that remained in proximity to the margin of Amazonia. Paleogeographic data derived from Phanerozoic rocks suggest that some of the Colombian Grenvillian fragments were connected to northernmost Peru and Ecuador until the Mesozoic, whereas the Mexican terranes where attached to the Colombian margin until Pangea fragmentation in Late Triassic times.

  4. Flora y vegetación del valle superior del Rió Atuel (Mendoza-Argentina Flora and vegetation of the Upper Valley of the Atuel River (Mendoza-Argentina

    Directory of Open Access Journals (Sweden)

    Ernesto A Morici

    2010-06-01

    Full Text Available El valle superior del Río Atuel presenta variaciones altitudinales y topográficas, siendo un territorio de confluencia de elementos propios de las provincias fitogeográficas Andina, del Monte, de la estepa Patagónica y de la Payunia. En este trabajo se estudia su flora y vegetación, a través de censos florísticos siguiendo la metodología de Braun-Blanquet (1979. A partir de la matriz de especies por censos se determinó el espectro biológico ponderado y la diversidad florística. Además, se estimó la cobertura basal registrándose los porcentajes de vegetación, broza, suelo desnudo, roca y fragmentos de roca. El estudio se desarrolló en un área restringida a la vertiente norte del Río Atuel entre su intersección con la Ruta Nacional 40 y las inmediaciones de la Planta de Azufre. En los censos se registraron un total de 89 especies pertenecientes a 36 familias, siendo las más numerosas Asteraceae, Poaceae, Verbenaceae, Fabaceae y Solanaceae. El 96% de las especies son nativas y sólo el 4% exóticas. Se diferenciaron 15 comunidades: 12 matorrales, 1 pastizal, 1 herbazal y 1 estepa de cojines.In this study we present a description of the flora and vegetation of the upper valley of Rio Atuel, Mendoza Province. In this area, characteristic taxa fron the Andina, Monte, Payunia and Patagonia Phytogeographical Provinces overlap their ranges. Considering that Atuel river high valley shows relevant altitudinal and topographical variations and a confluence of typical components from Andina, Monte, Patagonia and Payunia phytogeographic provinces, we plained to study, flora and vegetation. Floristic censuses were performed according to Braun-Blanquet (1979 and the matrix at coverage species was used to obtain cover data, weighted biological spectrum and floristic diversity. Furthermore, basal cover was estimated and vegetation, litter, bare soil, stones and stone pieces were recorded. This research was developed in an area restricted to the

  5. Control estructural en la distribución de las mineralizaciones de uranio del ciclo Choiyoi, bloque de San Rafael, Mendoza Structural control on the distribution of uranium mineralizations of the Choiyoi cycle, San Rafael Massif, Mendoza

    Directory of Open Access Journals (Sweden)

    María S. Japas

    2008-06-01

    Full Text Available Las mineralizaciones más importantes del distrito uranífero Sierra Pintada (Bloque de San Rafael, Mendoza se asocian a las rocas pertenecientes al ciclo magmático Choiyoi. En la sección inferior de este ciclo predominan los yacimientos alojados en areniscas de origen epiclástico. En la sección superior, en cambio, se encuentran pequeñas mineralizaciones vetiformes de escasa importancia económica. Durante el emplazamiento y la acumulación de estas volcanitas y sedimentitas pérmicas prevalecieron dos regímenes de esfuerzo diferentes: transpresional (fase orogénica San Rafael y transtensional (etapa postorogénica, los cuales condicionaron los sistemas mineralizantes. Mediante un estudio de fábrica deformacional se evaluó el grado de control ejercido por las estructuras sobre la distribución de las mineralizaciones de uranio durante estas dos etapas de deformación. De esta forma, se intenta aportar nuevos conocimientos sobre la génesis de estos depósitos en la provincia magmática Choiyoi y generar nuevas guías de exploración. A través de este análisis se pudieron definir tres órdenes de magnitud en el control estructural sobre los depósitos asociados al ciclo Choiyoi inferior, cuyo desarrollo fue condicionado por la fábrica de la fase orogénica sanrafaélica. En el caso de las mineralizaciones alojadas en rocas de la sección superior del ciclo Choiyoi, el campo transtensional post-sanrafaélico ejerció un control, directo o indirecto, durante el proceso mineralizante.The main mineralizations of the Sierra Pintada uranium district, San Rafael Massif, Mendoza, are associated with the Choiyoi volcanic province. In the lower section of this magmatic cycle uranium deposits hosted by epiclastic sandstones are predominant. In the upper section, small vein-type deposits of low economic significance are found instead. During the emplacement of these Permian volcanic and sedimentary sequences two different stress regimes, which

  6. La zona de alteración Arroyo La Chilca-Zanjón del Buitre, bloque de San Rafael, Mendoza

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    Nora Rubinstein

    2012-06-01

    Full Text Available La zona de alteración Arroyo La Chilca-Zanjón del Buitre está ubicada en el bloque de San Rafael (35°24'8" S; 68°19'25,8" O, Mendoza. Estudios previos definieron preliminarmente que corresponde a un sistema de tipo pórfro cuprífero vinculado genéticamente al magmatismo gondwánico. Esta área de alteración se desarrolla en una secuencia compuesta por brechas ignimbríticas e ignimbritas traquiandesíticas con intercalaciones de areniscas tobáceas y coladas andesíticas a las que intruyen cuerpos subvolcánicos andesíticos y traquiandesítico-dacíticos. La litología de la secuencia volcánica así como sus características geoquímicas confirman su correlación con la sección inferior del ciclo magmático Choiyoi (Pérmico inferior. El área de alteración presenta una zona potásica con una asociación compuesta por feldespato potásico-cuarzo-magnetita. A ésta se superpone alteración fílica con una asociación de cuarzo-muscovita-pirita-(rutilo acompañada por venillas de cuarzo-pirita. Por último se reconoce una carbonatización tardía. En las proximidades de la zona de alteración aforan vetillas con mineralización de pirita-calcopirita-galena-esfalerita en ganga de cuarzo. La geoquímica de metales indica moderadas anomalías de Ag y Au y pequeñas anomalías de Cu, Mo, Pb y Zn. El análisis estadístico permite definir la existencia de un pulso mineralizante de Cu-Mo y un segundo pulso de Mo reconocido solamente en Zanjón del Buitre. Asimismo se definen dos pulsos de Zn, uno de los cuales estaría genéticamente vinculado al Cu.

  7. Quaternary volcanic-sedimentary sequences and evolution of the Llancanelo Lake region (Southern Mendoza, Western Argentina) evidenced from geoelectric methods

    Science.gov (United States)

    de la Vega, Matias; Lopez, Ernesto; Osella, Ana; Rovere, Elizabeth I.; Violante, Roberto A.

    2012-12-01

    Llancanelo Lake region (Southern Mendoza Province, Western Argentina) is a key area for investigating the regional evolution of a tectonic basin affected by intense arc- and back-arc volcanism. However, the lack of enough outcrops makes it difficult to perform such reconstructions. In order to solve this problem, and with the aim of depicting the subsurface stratigraphy, 22 geoelectric surveys reaching more than 100 m depth were performed. The applied methodology, that combined geoelectrical measurements and field observations, is a continuation of previous works carried out in the region, and allowed for the first time to establish a near-surface stratigraphy that records the last evolutive stages of the lake. The studied region is mainly composed of Quaternary volcanic and sedimentary sequences. Four units were recognized on the basis of the geoelectrical differences (resistivity signal) supported by field observations where they crop out. Two of them have very high resistivity and are composed of basaltic lava flows, hence indicating the volcanic influence in the region. The other two have very low resistivity and correspond to sedimentary deposits, being the uppermost one composed of lacustrine sediments. The units were named according to the well-known stratigraphic scheme valid for the region. The studied stratigraphic sequence encompasses the time-span from the Pliocene to the present, and its interpretation allowed to establish the main evolutive stages, characterized by a complex interaction among tectonic, volcanic and climatic factors. The damming of the lake by basaltic flows and the consequent reduction of the lake's extension at times of intensive volcanic activity is one of the most significant events in its evolution.

  8. Geología de la región del Cerro Guanaquero, Río Diamante, Mendoza Geology of Cerro Guanaquero region, Diamante River, Mendoza

    OpenAIRE

    Federico Fuentes; Ramos,Victor A.

    2008-01-01

    El estudio realizado presenta nuevos datos sobre un sector poco conocido de la Cordillera Principal de Mendoza, en la alta cuenca del río Diamante en las adyacencias del cerro Guanaquero, y los primeros datos geocronológicos de sus rocas volcánicas. Las unidades geológicas presentes en el área se dividen en cuatro grupos principales: secuencias sedimentarias mesozoicas marinas y continentales intensamente plegadas y falladas; intrusivos y volcanitas intermedias de edad neógena; rocas volcánic...

  9. Peltephilidae and Mesotheriidae (Mammalia) from late Miocene strata of Northern Chilean Andes, Caragua

    Science.gov (United States)

    Montoya-Sanhueza, Germán; Moreno, Karen; Bobe, René; Carrano, Matthew T.; García, Marcelo; Corgne, Alexandre

    2017-04-01

    Until now, only one Cenozoic fossil mammal from the Chilean Precordillera (Arica and Parinacota Region) has been reported, Caraguatypotherium munozi (Mesotheriidae: Notoungulata). In this study, we describe a fourth specimen of C. munozi and a new armadillo species, Epipeltephilus caraguensis (Peltephilidae: Cingulata), both collected from a new site closer to the fossiliferous outcrops of the Caragua area (Serravallian - Tortonian). E. caraguensis differs from other members of the family in having: two sulci in the articular surface of the mobile osteoderm; having a tubular, rough and raised anterior edge; a conspicuous transverse depression; and four widely spaced foramina. This taxon represents the youngest known peltephilid from intermediate latitudes and indicates a wide geographic distribution (Patagonia to Central Andes) of the family just prior to its extinction. The new mesothere specimen is 19% larger than previous records. The revision of the dental features of C. munozi allowed the identification of an ambiguous trait in its original diagnosis, i.e. an enamel fracture was misinterpreted with the presence of a posterior sulcus on the talonid of the m3, suggesting that further taxonomic and systematic revision for the Caragua mesothere is necessary. Although the fossil record from the Caragua area is still scarce, mesotheriines seem to be abundant at this latitude, just as has been observed at several early to late Miocene sites such as Chucal (Chile), Cerdas and Nazareno (Bolivia), as well as in southern regions such as Arroyo Chasicó and Mendoza (Argentina). The presence of a new peltephilid species in Caragua sustains the hypothesis of provincialism during the Miocene in intermediate latitudes. Our findings also provide further support for probable faunal movements between intermediate and higher latitudes rather than to lower ones.

  10. Los espinelos del complejo alcalino puestoLa Peña, provincia de Mendoza

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    Eduardo O. Zappettini

    2009-06-01

    Full Text Available En este trabajo sedan a conocer datos mineralógicos y condiciones de cristalización de los espinelos,además de ilmenita, presentes en el Complejo Alcalino Puesto La Peña, provinciade Mendoza. El estudio fue realizado con una microsonda electrónica e incluyelos espinelos: magnetita, ulvöespinelo y espinelo s.s. ferífero.

  11. A Terrestrial Reference Frame (TRF), coordinates and velocities for South American stations: contributions to Central Andes geodynamics

    Science.gov (United States)

    Mackern, M. V.; Mateo, M. L.; Robin, A. M.; Calori, A. V.

    2009-12-01

    Satellite positioning systems allow the fixing of the location of a point on the Earth's surface with very good precision and accuracy. To do this, however, it is necessary to determine the point coordinates taking account the reference system and the movements that affect them because of tectonic plate movements. These reference systems are materialized by a significant number of continuous measurement stations in South America. In SIRGAS (Sistema de Referencia Geocéntrico para las Américas), there are four Analysis Centers that process the data collected from satellites of the Global Navigation Satellite Systems (GNSS), with the primary purpose to maintain the international terrestrial reference frame through calculation of the coordinates and velocities of the continuous GNSS stations of the SIRGAS-CON Network. In this work, we demonstrate the quality of the solutions from CIMA, one of the SIRGAS official processing centers operating in Mendoza, Argentina, in comparison with other South American processing centers. The importance of precise calculations of coordinates and velocities in a global frame is also shown. Finally, we give estimations of velocities from stations located within deformation zones in the Central Andes.

  12. What drives orogeny in the Andes?

    OpenAIRE

    Sobolev, Stephan V.; Andrey Babeyko; [Amhurst, Nicholas] 

    2005-01-01

    The Andes, the world's second highest orogenic belt, were generated by the Cenozoic tectonic shortening of the South American plate margin overriding the subducting Nazca plate. We use a coupled thermomechanical numerical modeling technique to identify factors controlling the intensity of the tectonic shortening. From the modeling, we infer that the most important factor was accelerated westward drift of the South American plate; changes in the subduction rate were less important. Other impor...

  13. Andes Altiplano, Northwest Argentina, South America

    Science.gov (United States)

    1993-01-01

    This view of the Andes Altiplano in northwest Argentina (25.5S, 68.0W) is dominated by heavily eroded older and inactive volcano peaks. The altiplano is a high altitude cold desert like the Tibetan Plateau but smaller in area. It is an inland extension of the hyperarid Atacama Desert of the west coast of South America and includes hundreds of volcanic edifices (peaks, cinder cones, lava flows, debris fields, lakes and dry lake beds (salars).

  14. [Frequency of dermatophytes in a sample of cats in the urban area of Gran Mendoza, Argentina].

    Science.gov (United States)

    López, María Florencia; Grilli, Diego; Degarbo, Stella; Arenas, Graciela; Telechea, Adriana

    2012-01-01

    The cat, considered the main reservoir of Microsporum canis, lives in urban areas, and also plays an important role in the emergence of dermatomycoses. To determine and analyse the frequency of zoonotic dermatophytes in a sample of cats in an urban area of the Gran Mendoza region. The animals selected were household cats and cats less than one year old that came from shelters and kennels from urban areas in the Gran Mendoza region. A total of 45 samples from cats with and without dermatological lesions were analysed. These samples were collected through skin scraping, hair removal and Mackenzie brush, respectively. Direct observation was made with KOH and glycerol after heat exposure. Samples were cultured on Sabouraud and Lactrimel agar slants with chloramphenicol and cycloheximide for 30 days. The frequency of dermatophytes isolated in this preliminary study was 13.3%. There were not statistically significant differences by source, age, sex, race or dermatological condition. Zoonotic dermatophytes were found in 2 household cats out of the 21 that had direct contact with children or the elderly. M. canis was isolated in 83.3% cases. The frequency of isolation of zoonotic dermatophytes in the sample of cats in an urban area of the Gran Mendoza region was 13.3%, a value higher than expected. M. canis was the most isolated species. Copyright © 2011 Revista Iberoamericana de Micología. Published by Elsevier Espana. All rights reserved.

  15. Petrografía y geoquímica de las rocas gondwánicas del proyecto minero Don Sixto, Mendoza Petrography and geochemistry of the gondwanic rock units from Don Sixto mining project, Mendoza

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    Ana Cecilia Mugas Lobos

    2010-11-01

    Full Text Available El proyecto minero Don Sixto es un depósito epitermal de Au-Ag de baja sulfuración ubicado al sureste de la provincia de Mendoza; el recurso aurífero de este depósito es próximo a las 900.000 onzas. La mineralización en el área se encuentra principalmente diseminada y está alojada mayormente en volcanitas y piroclastitas riolíticas de la Formación Choique Mahuida y diques riolíticos del Grupo El Portillo, ambos representantes de la sección superior del Grupo Choiyoi. Los datos obtenidos por el relevamiento geológico y los estudios petrográficos realizados en las volcanitas-piroclastitas del área de estudio, permiten indicar que la Formación Choique Mahuida está representada por riolitas, intercaladas con mantos ignimbríticos y niveles aislados de depósitos lenticulares piroclásticos. Por su parte, los diques riolíticos del Grupo El Portillo, de rumbo general noroeste-sureste y norte-sur, están probablemente vinculados a la evolución de zonas de falla de carácter regional. La geoquímica de estas riolitas gondwánicas, de acuerdo a la distribución de sus elementos traza y tierras raras, indica que están genéticamente vinculadas entre sí y pertenecerían a una suite cosanguínea proveniente de magmas diferenciados más evolucionados que los conocidos hasta la fecha para rocas de la sección superior del Grupo Choiyoi. Las características geoquímicas de estos magmas concuerdan además con los datos conocidos para rocas equivalentes fuera del área de estudio, en base a los cuales se asigna la sección superior del Grupo a un ambiente geotectónico transicional entre uno de arco volcánico y uno de intraplaca.Don Sixto mining project is a low sulphidation epithermal Au-Ag ore deposit located at the southeast of Mendoza province; the gold resource of the deposit is close to 900.000 ounces. In the study area, the mineralization is mainly disseminated and it is hosted by rhyolitic volcanic and pyroclastic sequences of the

  16. Oncoides tipo Osagia en la Formación La Manga (Oxfordiano y su significado paleoecológico, arroyo La Vaina, Mendoza Osagids-types oncoids from La Manga Formation and their paleoecological significance, La Vaina Creek, Mendoza

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    R.M. Palma

    2007-11-01

    del mar.Microbial oncoids have been found in the Oxfordian limestones of the La Manga Formation in the La Vaina section at Potimalal River, Mendoza province. The oncoids ocurr either in packstone or floatstone-rudstone or are scattered in the wackestones. They are mostly elliptical, ameboidal and subordinately spherical in shape. Different types of oncoids were recognized, according to their features of envelopes: (1 micritic laminations, (2 grumose laminations, and (3 organism-bearing laminations. Molluscs and echinoid fragments, peloids, and intraclasts acted as oncoid nuclei. Laminae follow the shape of nuclei, especially in the inner zone of the cortices. However, in the outer zones the laminae contain encrusting organisms dominated by nubeculariids and serpulids. Some oncoids, especially the ameboidal or elliptical forms, are characterized by multiple nuclei, represented by small oncoids. The oncoids are associated with bivalves, echinoderms, forams, and serpulids. The fauna is indicative of calm, shallow conditions and the excellent preservation of echinoderms suggests minimal transport prior to burial. Growth histories are in evidence. The oncoids grew in a shallow, low energy, slightly to moderate agitated subtidal normal sea water environment. The limited rolling growth oncoids was probably accompanished by intermittent currents that reoriented the oncoids parallel to stratification. The discontinuous organisms-bearing laminations reflect periods of non-agitation and litification, which facilitated the growth of encrusting organisms on static oncoid particles during a period of low sedimentation rate. Deposition of the oncoidbearing limestones took place during shallowing of the carbonate interval and associated with emersion, subaerial exposition and paleokarst as consequence of sea level fluctuations.

  17. Inserciones laborales tempranas: Los jóvenes trabajadores agrícolas en el Valle de Uco, Mendoza, Argentina Early labor markets incorporations: Agricultural young workers in the Uco Valley, Mendoza, Argentina

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    Gabriel I Bober

    2011-06-01

    Full Text Available Este artículo presenta las diferentes formas de inserción laboral de trabajadores jóvenes en el Valle de Uco, en la provincia de Mendoza. Durante las últimas décadas, el Valle de Uco basó su patrón de desarrollo agrícola en un modelo intensivo y empresarial de sus tres principales cultivos: los viñedos, los frutales y las hortalizas. En la actualidad, atraviesa un proceso de profunda reconversión productiva, orientada mayoritariamente hacia el mercado externo, que entre otras consecuencias pasó a modificar el funcionamiento del mercado de trabajo local. En este artículo, se contemplan las diferentes situaciones que llevan al ingreso laboral de los jóvenes en este contexto, según el momento etáreo que atraviesen. Se analiza la relación que este proceso guarda con el tamaño y la estructura de las familias y la situación socio-económica del hogar al que pertenecen. También, se examina el vínculo entre las características de los hogares y la forma de inserción de los jóvenes en el mercado de trabajo, de acuerdo al tipo de ocupación en la que se desempeñan y al destino que le dan a sus ingresos. A partir de la realización de entrevistas en profundidad a trabajadores jóvenes y a informantes clave se pudo dar cuenta de las preferencias de los jóvenes con respecto a distintos tipos de trabajos, con particular énfasis en ciertos trabajos agrícolas y, también en relación a su futuro laboral.This article deals with the different ways that young workers in the Uco Valley, at the province of Mendoza, enter to the agrarian local labour market. During the last decadas, the Uco Valley based its pattern of agricultural development in an intensive business model of its three main crops: vineyards, orchards, and vegetables. Currently, it is undergoing a process of profound restructuring of production, mainly oriented towards foreign markets, which among different consequences has modified the functioning of local labour markets. In

  18. Changing Student Attitudes using Andes, An Intelligent Homework System

    Science.gov (United States)

    van de Sande, Brett; Vanlehn, Kurt; Treacy, Don; Shelby, Bob; Wintersgill, Mary

    2007-03-01

    The size of introductory physics lectures often inhibits personal homework assistance and timely corrective feedback. Andes, an intelligent homework help system designed for two semesters of introductory physics, can fill this need by encouraging students to use sound problem solving techniques and providing immediate feedback on each step of a solution. On request, Andes provides principles-based hints based on previous student actions. A multi-year study at the U.S. Naval Academy demonstrates that students using Andes perform better than students working the same problems as graded pencil and paper homeworks. In addition, student attitude surveys show that Andes is preferred over other homework systems. These findings have implications for student attitudes toward, and mastery of, physics. See http://www.andes.pitt.edu for more information.

  19. Social stratification in a global successful activity: the case of wine industry in Mendoza (1995-2011

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    Mariana Heredia

    2013-12-01

    Full Text Available In order to contribute to the knowledge of social inequalities in contemporary Argentina, this article examines how the restructuring of the wine from Mendoza (which begun in the late eighties and consolidated in the year two thousand resulted in the restructuring of different socio-professional categories and their ties. The speed and depth of these transformations, in a relatively limited space and in an economic activity that is judged as a successful case of integration into the international market make Mendoza wine’s industry a privileged case to discuss social impact of agribusiness’ transnationalization

  20. Geología de la región del Cerro Guanaquero, Río Diamante, Mendoza

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    Federico Fuentes

    2008-03-01

    Full Text Available El estudio realizado presenta nuevos datos sobre un sector poco conocido de la Cordillera Principal de Mendoza, en la alta cuenca del río Diamante en las adyacencias del cerro Guanaquero, y los primeros datos geocronológicos de sus rocas volcánicas. Las unidades geológicas presentes en el área se dividen en cuatro grupos principales: secuencias sedimentarias mesozoicas marinas y continentales intensamente plegadas y falladas; intrusivos y volcanitas intermedias de edad neógena; rocas volcánicas pliocenas a recientes de composición intermedia a básica, y depósitos cuaternarios inconsolidados. El cerro Guanaquero, un estratovolcán pliocuaternario intensamente erosionado por glaciares pleistocenos, con sus 4.841 metros es el rasgo orográfico más prominente. Está constituido esencialmente por andesitas grises porfíricas, piroxénicas a biotíticas. Intercaladas con las coladas andesíticas se presentan depósitos piroclásticos, aglomerados volcánicos, ignimbritas y basaltos. La datación de una andesita por el método K-Ar en roca total arrojó una edad de 1,4 ± 0,1 Ma. La deformación ándica comenzó en forma de una faja plegada y corrida de piel fina, con pliegues por despegue en el sector occidental y por propagación de falla en el oriental. La compresión al oeste de los 69º47´O terminó por invertir la fallas normales del rift mesozoico. A lo largo de este meridiano se encuentra la falla más importante de la región, la que se ha correlacionado con la falla Malargüe, bien desarrollada en latitudes más australes. Esta falla limita la faja plegada y corrida del Aconcagua, de naturaleza epidérmica, y la faja plegada y corrida de Malargüe, controlada por la inversión tectónica del basamento. El volcanismo fue muy intenso en el Plioceno y el Cuaternario, correspondiendo a un período de empinamiento de la placa oceánica subducida, en el que la región ha sido levantada pasivamente. La alta resistencia a la erosión de

  1. La transición de periferia a frontera: mendoza en el siglo XVII

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    Margarita Gasc\\u00F3n

    2001-01-01

    Full Text Available El análisis de la evolución de Mendoza en el siglo XVII permite diferenciar las características de un asentamiento en la periferia de aquellas características que corresponden a una sociedad de frontera. Fundada en 1561 en la periferia imperio español en América a principios del siglo XVII, Mendoza era una comunidad con escasa población, con reducido comercio y de lento desarrollo urbano; todas características de las colonias periféricas. A lo largo de la primera parte del siglo XVII, sin embargo, Mendoza se fue configurando como una sociedad de frontera. Las causas de este devenir frontera se relacionan con la revuelta araucana y con las consecuencias del establecimiento de la frontera geográfico-militar en el río Biobio. El trabajo comienza con una revisión de los términos frontera y periferia tal como se encuentran empleados en los análisis de algunos autores representativos de la historiografía sobre fronteras para las Américas. Luego se reconstruye la evolución de periferia a frontera en Mendoza; un proceso que comenzó varias décadas después de su fundación en 1561. Tal fundación no estuvo guiada por la necesidad de consolidar o de proteger una zona de frontera, de modo que no fue fundada ni como presidio ni como misión, que son las típicas instituciones de frontera y que encontramos en numerosas fronteras del imperio español, como ser en la Florida y en el norte de México. A fines del siglo XVI Mendoza fue fundada como uno de los tantos asentamientos que permitirían a los españoles seguir avanzando en la conquista y colonización de nuevos territorios. Sin embargo, la revuelta araucana de 1598-1599 provocó el quiebre de tal desenvolvimiento de la conquista porque truncó la esperanza de una futura expansión española hacia el sur. Más allá del fiasco militar de la derrota de Curalaba, la rebelión nativa obligó a la coronaa establecer un ejército profesional de alrededor de 2.000 hombres, cuya permanencia

  2. La resignificación del muralismo mexicano en Mendoza : (1952-1961)

    OpenAIRE

    Marquet, María Clara

    2002-01-01

    El movimiento plástico desarrollado en Mendoza en la década del '50 congregó a un grupo de jóvenes artistas con un ideal común: acercar el arte a la mayoría, partiendo de la consideración de la producción artística como trabajo colectivo. Constituyeron el Club de Grabados y Taller de Murales, emprendimientos originados en el pequeño taller del maestro Luis Quesada, quien congregaba a estudiantes de arte e intelectuales para experimentar la técnica del grabado y debatir sobre temas que colocab...

  3. The ataxioceratid ammonite fauna of the Tithonian (Upper Jurassic) of Casa Pincheira, Mendoza (Argentina)

    Science.gov (United States)

    Parent, Horacio

    2003-07-01

    The Tithonian Ataxioceratids from Casa Pincheira (Mendoza) are described in the framework of a period of global relative high sea level stand, with Andean basins well communicated with Central and Western Tethys. The family Ataxioceratidae is interpreted including the subfamily Torquatisphinctinae Tavera ( Katroliceras Spath, Torquatisphinctes Spath, and Pachysphinctes Dietrich). The original specimens of ' Perisphinctes' densestriatus Steuer, Paraulacosphinctes striolatus (Steuer), Paraulacosphinctes? mangaensis (Steuer), and Torquatisphinctes proximus (Steuer) are photographically refigured, and their types are designated. Type specimens are also designated for Euvirgalithacoceras malarguense (Spath) and Choicensisphinctes choicensis (Burckhardt). The genus Euvirgalithacoceras is used for the first time for lowermost Tithonian Andean forms, and Choicensisphinctes is suggested as a derivated genus.

  4. Serie de balances energéticos de la provincia de Mendoza, Argentina

    OpenAIRE

    Castillo, Javier

    2011-01-01

    Esta investigación interdisciplinaria dentro del campo de la Ingeniería y la Economía de la Energía, aborda aspectos conceptuales, metodológicos y empíricos en relación con la elaboración de una Serie de Balances Energéticos (BE) para Mendoza para el período 1980/2009. Parte de estudios metodológicos (Fundación Bariloche [1984], OLADE [2004], EUROSTAT [2007], “Balance Energético Nacional. Serie 1960- 2007" [2008] de Argentina) y de BE elaborad...

  5. Primer registro de Tityus trivittatus (Scorpiones: Buthidae en la provincia de Mendoza (Argentina

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    Florencia FERNÁNDEZ CAMPÓN

    2009-01-01

    Full Text Available En la siguiente nota se informa sobre el primer registro delescorpión Tityus trivittatus Kraepelin en la provincia de Mendoza en el Barrio Campo Papa, departamento de Godoy Cruz. T. trivittatus es dentro de nuestro país una de las especies de escorpiones con importancia médica, debido a que su veneno neurotóxico puede causar lesiones en el sistema nervioso y en algunos casos la muerte, particularmente en niños.

  6. Análisis del campo de esfuerzos en una secuencia lacustre de Precordillera oriental, San Juan-Mendoza Analysis of the stress field in a lacustrine sequence of eastern Precordillera, San Juan-Mendoza

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    Laura P. Perucca

    2008-06-01

    Full Text Available En la quebrada del río Acequión, ubicada en el sur de la provincia de San Juan y norte de Mendoza (32º 10' S, en el centrooeste argentino, se efectuó el análisis de las fallas que afectan depósitos lacustres de edad holocena. Estas fallas se encuentran asociadas a estructuras de licuefacción y avalanchas de roca indicadoras de paleoterremotos, lo que permite extender el registro sísmico de la región hasta el Holoceno temprano. Al comparar el campo de esfuerzos regional actual (determinado por sismicidad instrumental, con el cálculo del mecanismo focal de los terremotos recientes ocurridos en la región con el campo de esfuerzos local, se observó que mientras el primero se caracteriza por la compresión, el campo local de la secuencia lacustre es extensional. Esto indicaría que aunque el esfuerzo regional actual es compresivo y de dirección NE-SO debido a la convergencia entre las placas de Nazca y Sudamérica, el antiguo lago adosado a las sierras de Pedernal y Los Pozos, está afectado por fallas normales, principalmente debido a esfuerzos locales distensivos originados por el reacomodamiento de estos depósitos durante el levantamiento de las zonas montañosas aledañas.An analysis of faults affecting Late Neogene lacustrine deposits was made in Acequión area, placed in the south of the province of San Juan. These faults are associated with liquefaction structures and rock avalanche deposits originated by paleoearthquakes, extending the earthquake records until the early Holocene in this region. By comparing the present regional stress field (determined by instrumental seismicity, with the focal mechanism analysis of recent earthquakes occurred in the region with the local stress field, it was observed that whereas the first one is characterized by compression, the local field on the lacustrine sequence is normal. The current regional stress field is compressive due to the subduction of Nazca plate under South America plate. The

  7. Descripción de una nueva especie de Phymaturus del grupo de P. palluma de la provincia de Mendoza, Argentina

    Directory of Open Access Journals (Sweden)

    Lobo, Fernando

    2007-05-01

    Full Text Available Se describe una nueva especie del género Phymaturus, grupo de P. palluma. Este nuevo taxón fue colectado en la Sierra del Nevado y en la Payunia, Provincia de Mendoza, Argentina. El nuevo Phymaturus se caracteriza por presentar un patrón de coloración único en el género, con un reticulado grueso en todo el dorso, coloración de fondo castaño claro o gris, con tenues matices amarillentos en los lados del cuerpo y cola, algunos ocelos son evidentes, principalmente en las hembras. Esta especie, a diferencia de las restantes del grupo, no presenta un "capuchón melánico" en la cabeza. La presencia de la escama rostral dividida en muchos de sus individuos (69%, y un número elevado de escamas alrededor del cuerpo también diferencian a este nuevo taxón de las otras especies del grupo. El patrón de coloración y los caracteres de lepidosis diferencian este nuevo Phymaturus del resto de las especies del género. A new species of Phymaturus belonging to the P. palluma group is described. This new taxon was collected in Sierra del Nevado and Payunia, Mendoza Province, Argentina. The new Phymaturus exhibit an unique dorsal pattern for the genus formed by a thick dark reticulation over light brown or gray background coloration. Light yellow color is present on flanks and over the dorsal surface of tail and in most of females a coupled series of dark ocelli is present. This species distinctly lack a melanic cover over the head as all other members of the group. Characters of squamation different in this taxon are the presence in most individuals of a rostral scale divided and the high number of scales around midbody. Those characters of pattern and lepidosis described above make different this new Phymaturus from all other species.

  8. Permafrost distribution map of San Juan Dry Andes (Argentina) based on rock glacier sites

    Science.gov (United States)

    Esper Angillieri, María Yanina

    2017-01-01

    Rock glaciers are frozen water reservoirs in mountainous areas. Water resources are important for the local populations and economies. The presence of rock glaciers is commonly used as a direct indicator of mountain permafrost conditions. Over 500 active rock glaciers have been identified, showing that elevations between 3500 and 4500 m asl., a south-facing or east-facing aspect, areas with relatively low solar radiation and low mean annual air temperature (-4 to 0 °C) favour the existence of rock glaciers in this region. The permafrost probability model, for Dry Andes of San Juan Province between latitudes 28º30‧S and 32°30‧S, have been analyzed by logistic regression models based on the active rock glaciers occurrence in relation to some topoclimatic variables such as altitude, aspect, mean annual temperature, mean annual precipitation and solar radiation, using optical remote sensing techniques in a GIS environment. The predictive performances of the model have been estimated by known rock glaciers locations and by the area under the receiver operating characteristic curve (AUROC). This regional permafrost map can be applied by the Argentinean Government for their recent initiatives which include creating inventories, monitoring and studying ice masses along the Argentinean Andes. Further, this generated map provides valuable input data for permafrost scenarios and contributes to a better understanding of our geosystem.

  9. Annual narrative report: Lake Andes National Wildlife Refuge, Karl Mundt National Wildlife Refuge, and Lake Andes Wetland Management District: Calendar year 1975

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This collection of monthly activity reports summarizes activities on Lake Andes NWR, Lake Andes WMD, and Karl E. Mundt NWR during the 1975 calendar year. Resource...

  10. La dinámica de la sustentabilidad fiscal en los municipios urbanos de la Provincia de Mendoza

    Directory of Open Access Journals (Sweden)

    Raúl Molina

    2016-11-01

    Full Text Available La finalidad del trabajo es revisar el comportamiento fiscal comparado de los departamentos urbanos que forman parte del “Gran Mendoza” (Capital, Guaymallén, Godoy Cruz y Las Heras, así como analizar distintos indicadores de sustentabilidad fiscal y su aplicación a la situación actual y futura de los mismos. A partir del análisis de la deuda pública consolidada y su relación con los resultados financieros de los respectivos municipios, se analizan las perspectivas de solvencia de cada uno de ellos, para determinar, en su caso, los esfuerzos fiscales necesarios para retomar la senda de la sustentabilidad. Sin duda, la efectividad de la política presupuestaria y tributaria, y el nivel del gasto público, repercuten claramente en los resultados de la gestión, pero hay también otros aspectos, como la selección de formas alternativas para financiar el gasto público y el manejo del endeudamiento, que impactan en los resultados financieros de los municipios. Clasificación JEL: H7.Palabras clave: Finanzas Públicas Intergubernamentales; Estados sub-nacionales; Solvencia fiscal; Sustentabilidad; Déficits. The dynamics of fiscal sustainability in the urban municipalities of the Province of MendozaAbstractThe purpose of this paper is to review the fiscal performance compared to urban municipalities of “Gran Mendoza” (Capital, Guaymallén, Godoy Cruz and Las Heras and to analyze different indicators of fiscal sustainability and its application to the current and future situation of them. From the analysis of the consolidated public debt and its relationship to the financial performance of the respective municipalities, the prospects solvency of each of them are analyzed to determine the necessary fiscal efforts to resume the path of sustainability. Certainly the effectiveness of budgetaryl and tax policy, and the level of public spending clearly affect the results of management, but there are also other aspects such as the selection

  11. Early Callovian ingression in southwestern Gondwana. Palaeoenvironmental evolution of the carbonate ramp (Calabozo Formation) in southwestern Mendoza, Neuquen basin, Argentina

    Science.gov (United States)

    Armella, Claudia; Cabaleri, Nora G.; Cagnoni, Mariana C.; Panarello, Héctor O.

    2013-08-01

    The carbonatic sequence of the Calabozo Formation (Lower Callovian) developed in southwestern Gondwana, within the northern area of the Neuquén basin, and is widespread in thin isolated outcrops in southwestern Mendoza province, Argentina. This paper describes the facies, microfacies and geochemical-isotopic analysis carried out in five studied localities, which allowed to define the paleoenvironmental conditions of a homoclinal shallow ramp model, highly influenced by sea level fluctuations, where outer, mid and inner ramp subenvironments were identified. The outer ramp subenvironment was only recognized in the south of the depocenter and is characterized by proximal outer ramp facies with shale levels and interbedded mudstone and packstone layers. The mid ramp subenvironment is formed by low energy facies (wackestone) affected by storms (packstones, grainstones and floatstones). The inner ramp subenvironment is the most predominant and is characterized by tidal flat facies (wackestones, packstones and grainstones) over which a complex of shoals (grainstones and packstones) dissected by tidal channels (packstone, grainstones and floatstones) developed. In the north area, protected environment facies were recorded (bioturbated wackestones and packstones). The vertical distribution of facies indicates that the paleoenvironmental evolution of the Calabozo Formation results from a highstand stage in the depocenter, culminating in a supratidal environment, with stromatolitic levels interbedded with anhydrite originated under restricted water circulation conditions due to a progressive isolation of the basin. δ13C and δ18O values of the carbonates of the Calabozo Formation suggest an isotopic signature influenced by local palaeoenvironmental parameters and diagenetic overprints. The δ13C and δ18O oscillations between the carbonates of the different studied sections are related with lateral facies variations within the carbonate ramp accompanied with dissimilar

  12. Mendoza, Argentina. El terremoto de 1861 como disparador del cambio de representación social de la identidad de una ciudad al pie de los Andes

    National Research Council Canada - National Science Library

    Jorge Ricardo Ponte

    2007-01-01

    The definition of a town´s identity is a contemporary problematic. The process of economic globalization, far from devastating with the regional or national particularities seems to have exacerbated them...

  13. Antonio de Mendoza; First Viceroy of Mexico. The Tinker Pamphlet Series for the Teaching of Mexican American Heritage.

    Science.gov (United States)

    Miller, Hubert J.

    As Mexico's first viceroy, Antonio de Mendoza's most noteworthy achievement was his laying the basis of colonial government in New Spain which continued, with modifications, for 300 years. Although he was lenient in dealing with the shortcomings of his Indian and Spanish subjects, he took a firm stand in dealing with the rebellious Indians in the…

  14. Plagas de la agricultura en Mendoza: la langosta en los comienzos de la vitivinicultura moderna (1890-1900

    Directory of Open Access Journals (Sweden)

    Eduardo Pérez Romagnoli

    2011-12-01

    Full Text Available El trabajo se refiere a la presencia de la langosta en Mendoza en los comienzos de la especialización vitivinícola, en la década de 1890. Comprende aspectos sobre su biogeografía, antecedentes del insecto en nuestro país, los primeros inventos nacionales para enfrentar sus ataques. Con relación a las invasiones de la Schistocerca americana en Mendoza, se indaga sobre la organización estatal y la participación de la sociedad para combatirla, incluyendo algunos problemas y daños causados en la agricultura.The study refers to the presence of locust in Mendoza at the beginning of wine specialization, in the decade of 1890. It includes aspects on biogeography, precedents of the insect in our country, and first national inventions to face its assaults. In relation to invasions of Schistocercaamericana in Mendoza, the study researches on state organization and social participation to attack the plague, including some problems and damages caused in agriculture.

  15. Modelos historiográficos latinos en la Historia de la Guerra de Granada de Diego Hurtado de Mendoza

    OpenAIRE

    Abad Mellizo, Alejandro

    2016-01-01

    Se analizan los modelos que basándose en los historiadores latinos (fundamentalmente Salustio y Tácito) utiliza Diego Hurtado de Mendoza (1503-1575) al escribir su monografía acerca de la Rebelión de las Alpujarras (1568-1571).

  16. Doña Mencía de Mendoza y su residencia en el castillo de Jadraque

    Directory of Open Access Journals (Sweden)

    Hidalgo Ogáyar, Juana

    2005-06-01

    Full Text Available El castillo de Jadraque, conocido como castillo del Cid, es una de las fortalezas situadas en la cuenca del río Henares. El Cardenal Mendoza, don Pedro de Mendoza, lo adquirió, siendo Obispo de Sigüenza, el 27 de enero de 1470, ante Alonso Dávila, por permuta con don Alonso Carrillo, Arzobispo de Toledo, a quien dio la villa de Maqueda y la Alcaldía Mayor de Toledo. Este castillo fue uno de los que se salvaron de la demolición ordenada por los Reyes Católicos, a finales del siglo xv, de todos aquellos enclaves estratégicos que suponían un peligro para la monarquía. De ahí que el Cardenal decidiera reconstruirlo y años más tarde lo legó a su hijo don Rodrigo de Mendoza, 1° Marqués del Cénete y éste, a su vez, a su primogénita, doña Mencía de Mendoza. El castillo de Jadraque, aún hoy día, se levanta sobre una elevada atalaya, está rodeado…

  17. Water in the Mendoza, Argentina, food processing industry: water requirements and reuse potential of industrial effluents in agriculture

    Directory of Open Access Journals (Sweden)

    Alicia Elena Duek

    2016-04-01

    Full Text Available This paper estimates the volume of water used by the Mendoza food processing industry considering different water efficiency scenarios. The potential for using food processing industry effluents for irrigation is also assessed. The methodology relies upon information collected from interviews with qualified informants from different organizations and food-processing plants in Mendoza selected from a targeted sample. Scenarios were developed using local and international secondary information sources. The results show that food processing plants in Mendoza use 19.65 hm3 of water per year; efficient water management practices would make it possible to reduce water use by 64%, i.e., to 7.11 hm3. At present, 70% of the water is used by the fruit and vegetable processing industry, 16% by wineries, 8% by mineral water bottling plants, and the remaining 6% by olive oil, beer and soft drink plants. The volume of effluents from the food processing plants in Mendoza has been estimated at 16.27 hm3 per year. Despite the seasonal variations of these effluents, and the high sodium concentration and electrical conductivity of some of them, it is possible to use them for irrigation purposes. However, because of these variables and their environmental impact, land treatment is required.

  18. Diezmos, producción agraria y mercados: Mendoza y Cuyo, 1710-1830

    Directory of Open Access Journals (Sweden)

    Juan Carlos Garavaglia

    2007-12-01

    Full Text Available En este trabajo exponemos los primeros resultados de una investigación destinada a analizar la estructura agraria de la región del oasis mendocino desde los años cincuenta del siglo XVIII a 1861. El estudio está enfocado sobre todo en Mendoza, pero abarca también el resto de la región cuyana. Centrado en especial sobre la serie de diezmos eclesiásticos entre 1710 y 1830, el trabajo deja ver la influencia de los ciclos climáticos en la producción agraria, como también los cambios en los mercados para los productos cuyanos durante ese largo siglo, mostrando de qué modo hay a fines del período una reorientación productiva y mercantil.This work expounds the initial results of research that analyzes agrarian structures in the region of the Mendozan Oasis from the 1750s to 1861. The study is centered in Mendoza, but it also includes the rest of the Cuyana region. By examining an archival series of ecclesiastical tithes between 1710 and 1830, the article brings into focus the influence of climatic cycles on agrarian production in addition to the changes in the market for Cuyano products over this long century. By so doing, it demonstrates how a productive and mercantile reorientation had taken place by the end of the period.

  19. Novel Strain of Andes Virus Associated with Fatal Human Infection, Central Bolivia

    Science.gov (United States)

    Cruz, Cristhopher D.; Vallejo, Efrain; Agudo, Roberto; Vargas, Jorge; Blazes, David L.; Guevara, Carolina; Laguna-Torres, V. Alberto; Halsey, Eric S.; Kochel, Tadeusz J.

    2012-01-01

    To better describe the genetic diversity of hantaviruses associated with human illness in South America, we screened blood samples from febrile patients in Chapare Province in central Bolivia during 2008–2009 for recent hantavirus infection. Hantavirus RNA was detected in 3 patients, including 1 who died. Partial RNA sequences of small and medium segments from the 3 patients were most closely related to Andes virus lineages but distinct (1 hantaviruses; the highest prevalence was among agricultural workers. Because of the high level of human exposure to hantavirus strains and the severity of resulting disease, additional studies are warranted to determine the reservoirs, ecologic range, and public health effect of this novel strain of hantavirus. PMID:22515983

  20. Comprehensive Conservation Plan: Lake Andes National Wildlife Refuge Complex

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This Comprehensive Conservation Plan (CCP) was written to guide management on Lake Andes NWR Complex for the next 15 years. This plan outlines the Refuge vision and...

  1. Totals of crude oil, natural gas and gas condensates listed by province. [Argentina]. Totales de petroleo, gas natural y gasolina natural detallados por

    Energy Technology Data Exchange (ETDEWEB)

    1976-01-01

    Statistics on total mineral and petroleum production in Argentina during the year 1976 are presented. Production totals for petroleum, natural gas, and gas condensates are listed by province and by category. The province production records include Chubut, Jujuy, La Pampa, Mendoza, Neuquen, Rio Negro, Salta, Santa Cruz, Territorio National de la Tierra del Fuego, the Antarctic, and islands of the S. Atlantic. Total production amounted to 23,148,339 cu m of petroleum, 10,879,906,919 cu m of natural gas, and 69,790 cu m of gas condensates. Information on petroleum sector employment in the years 1967 through 1976 also is provided.

  2. Totals of crude oil, natural gas and gas condensates listed by province. [Argentina]. Totales de petroleo, gas natural y gasolina natural detallados por

    Energy Technology Data Exchange (ETDEWEB)

    1975-01-01

    Statistics on total mineral and petroleum production in Argentina during the year 1975 are presented. Production totals for petroleum, natural gas, and gas condensates are listed by province and by category. The province production records include Chubut, Jujuy, La Pampa, Mendoza, Neuquen, Rio Negro, Salta, Santa Cruz, and Tierre del Fuego. Total production amounted to 22,968,224 cu m of petroleum, 10,275,106,000 cu m of natural gas, and 30,883 cu m of gas condensates. Information on petroleum sector employment in the years 1966 through 1975 also is provided.

  3. The Glaciation of the Ecuadorian Andes

    Science.gov (United States)

    Schubert, Carlos

    This pleasing book fills the gap in the knowledge about Pleistocene and recent glaciation between Colombia and Peru. A significant amount of data exists already for Colombia and Venezuela and for Peru, Bolivia, and, particularly, Chile. Hastenrath has now given us a description of glaciers and glaciation underneath the equator in the Andes.The book begins with brief summaries of the physiography and the atmospheric circulation, which give the general setting of Ecuador. Then follow detailed descriptions of the glaciers and glacial morphology of all the important mountains of the Western and Eastern Cordilleras. These are well illustrated, and a particularly useful feature is the comparison of old photographs and paintings of glaciers with modern photographs, many taken by the author. All illustrate the spectacular retreat of the glaciers in the Ecuadorian Andes during the last century and correlate quite well with observations elsewhere. This retreat is snown quantitatively in Table 4, in terms of decrease in glacier-covered area since the glacial advance of moraine stage III. The area of present-day glaciers is about 10% of the area during that stage (compared with about 1.5% in the Sierra Nevada de Mérida, Venezuela). A series of maps show the glacial morphology of the mountains (unfortunately, some of the maps have been included within the binding, thus losing some information; they could have been reduced somewhat to fit a single page or, if too large, could have been included in the pocket, together with the map of Chimborazo-Carihuairazo).

  4. El bienestar social durante el peronismo clasico. La expansion de los servicios de salud hacia las areas rurales de los municipios de la provincia de Mendoza

    National Research Council Canada - National Science Library

    Hirschegger, Ivana

    2010-01-01

    ... metas principales del gobierno de Juan Domingo Peron. A partir de esto, nuestro objetivo central es estudiar las politicas sanitarias en los municipios de la provincia de Mendoza durante el periodo 1946-1955, atendiendo a dos aspectos...

  5. Vinos de Mendoza : relación precio en góndola versus calidad en degustación a ciegas

    OpenAIRE

    Antoniolli, Ester R.; Alturria, Laura V.; Ceresa, Alejandro M.; Solsona, Juan E.; de Winter, Patricia; Galiotti, Hugo; Fonzar, Alfredo

    2011-01-01

    Cuando un posible consumidor de vinos decide su compra, lo hace influenciado por factores relacionados no sólo con la calidad del producto sino también con el conocimiento que tiene de la marca. Esta investigación se inició con un mapeo de vinos ofrecidos en puntos de venta minorista del Gran Mendoza, para luego realizar una degustación a ciegas con panelistas de la provincia de Mendoza, de sectores de ...

  6. A Colonial Cacicazgo: the Mendozas of Seventeenth-Century Tepexí de la Seda

    Directory of Open Access Journals (Sweden)

    Rik Hoekstra

    2010-10-01

    Full Text Available The cacicazgo, or indigenous lordship, was a pivotal institution in colonial Mexican Indian pueblos. Caciques, or Indian nobles, played a role, both in the largely indigenous world of the pueblo and in the regional economy that was dominated by Spaniards. This subject of this essay is the analysis of the evolution and daily operation and of a cacicazgo from the Indian settlement of Tepexí de la Seda near the city of Puebla de los Ángeles and the life of its caciques in the sixteenth and seventeenth centuries. In the sixteenth century the cacicazgo was in upheaval because of discord between the cacicazgos and their dependent Indians. A number of long-running accounts from the 1620s record in detail the daily operations of the cacicazgo of Doña Ana de Santa Bárbara of the Mendoza family, thus illustrating how caciques negotiated their positions and coped with their lives and the changes in it.   Resumen: Un cacicazgo colonial: los Mendoza de Tepexí de la Seda en el siglo 17 El cacicazgo, o señorío indígena, fue una institución fundamental en los pueblos indios de México colonial. Los caciques, o nobles indígenas, desempeñaron un papel tanto en el mundo en gran parte indígena del pueblo y en la economía regional dominada entonces por los españoles. El tema de este ensayo es el análisis de la evolución y operación cotidianas de un cacicazgo del asentamiento indígena de Tepexí de la Seda cerca de la ciudad de Puebla de los Ángeles y la vida de sus caciques en los siglos 16 y 17. En el siglo 16, el cacicazgo vivió tiempos convulsos debido a los conflictos entre los caciques y sus dependientes indios. Varias extensas cuentas de los años veinte del siglo 17 registran en detalle las operaciones diarias del cacicazgo de doña Ana de Santa Bárbara, de la familia Mendoza, mostrando así cómo negociaban los caciques sus posiciones y se adaptaban a los cambios en sus vidas.

  7. Biodiversidad de la flora del flanco oriental del Cordón del Plata (Luján de Cuyo, Mendoza, Argentina. Catálogo florístico Biodiversity of the flora of the eastern slope of the Cordón del Plata (Luján de Cuyo, Mendoza, Argentina

    Directory of Open Access Journals (Sweden)

    Eduardo Méndez

    2009-07-01

    Full Text Available La biodiversidad de la flora de la vertiente oriental del Cordón del Plata, Luján de Cuyo, Mendoza, Argentina se analizó a lo largo de un gradiente altitudinal, entre los 1200 y 4500 m s.n.m. Para ello se utilizó la lista florística de las especies de 89 comunidades vegetales distribuidas en 14 unidades de vegetación, 5 pisos de vegetación y 3 unidades fitogeográficas. Para cada especie se consideró su distribución en los grupos de comunidades vegetales, ubicación fitogeográfica, formas de vida, origen y registro de colección. La flora examinada contiene 667 especies vegetales que se corresponden con 338 géneros y 82 familias. Las familias están representadas por 8 Pteridophyta, 1 Gymnospermae y 73 Angiospermae, con 12 Monocotyledoneae y 61 Dicotyledoneae. Las familias mejor representadas son Asteraceae y Poaceae que tienen en conjunto 110 géneros y 249 especies. Los géneros Senecio, Baccharis y Adesmia son los más ricos en especies. Aproximadamente el 20 % de las especies son endémicas de Argentina. La flora del área se la compara con la del país, la provincia y la de otras áreas.Floristic catalogue. The floristic biodiversity of the eastern slope of the Cordón del Plata, Luján de Cuyo, Mendoza, Argentina, was studied along an altitudinal gradient, between 1200 and 4500 m a.s.l. For this we used a floristic list of 89 plant communities, distributed in 14 vegetation types, 5 vegetation belts and 3 phytogeographic units. For each of the species, its distribution in the groups of plant communities, phytogeographic position, life form, biogeographical origin, and registration of each collection was considered. The studied flora has 667 species, corresponding to 338 genera and 82 families. There are 8 Pteridophyta, 1 Gymnospermae, and 73 Angiospermae, of which 12 are Monocotyledons and 61 Dicotyledons. The most represented families are Asteraceae and Poaceae, which in total have 110 genera and 249 species. The most species

  8. Seismological Parameters in the Northern Andes, Venezuela

    Science.gov (United States)

    Sobiesiak, M.; Palme de Osechas, C.; Choy, J. E.; Morandi S., M. T.; Campo, M.; Granado Ruiz, C.

    2001-12-01

    Venezuelas tectonic setting as part of the plate boundary between the Caribbean and the South American plate causes two major seismologically active fault systems: the roughly west - east trending strike slip fault system along the coast with numerous sub-parallel faults and the Bocono fault system, which dominates the Venezuelan southwest - northeast striking Andes. The main Bocono fault reaches a total length of about 500 km and has a width of approximately 100 km between the southern and northern baseline of the mountain slopes which are marked by inverse faults. This is believed to be due to strain partitioning, a concept which seems to apply as well to the Bocono fault system. The whole fault system is characterized by a high seismicity rate of small scale and intermediate event magnitudes ranging from 1.5 to 6.3 in the last fifty years. In this study we would like to present an investigation on 39 focal mechanism solutions and a b-value mapping of the Andean region with the main goal to throw light on the stess and strain situation. For recompiling the focal memchanisms calculated from first motion polarities, various sources had to been used: seismograms from stations of the local and regional networks of the Seismological Center of ULA, the national seismic network operated by FUNVISIS, the seismic network Lago Maracaibo of PDVSA and the local seismic network of DESURCA. For the b-value mapping we used the two catalogues of ULA and DESURCA of which the last one registered more than 6500 events from 1994 to 1999. The set of focal mechanism solutions studied showed normal, strike slip, and reverse faulting mechanisms concentrated in distinct areas of the Bocono fault system and thus resulting in a zonation also supported by the determinations of the azimuths of the maximum horizontal stress SHmax. This hypothesis of the zonation of the Andes region is strongly supported by the results of the b-value mapping. The zonation as seen in the varying major stress

  9. The Medical Vocabulario terminológico of Manuel Hurtado de Mendoza

    Directory of Open Access Journals (Sweden)

    Bertha M. Gutiérrez Rodilla

    2012-12-01

    Full Text Available From the early nineteenth century, Spanish physicians started to sense a «threat» to the language of medicine which they used, due in part to the large number of foreign terms they were forced to import from other languages, particularly French. Many voices emerged to denounce this situation and propose potential solutions such as those which would be derived from the creation of a terminological dictionary which would fix precise meanings for medical terms. It was Manuel Hurtado de Mendoza who eventually dared to take on this task and develop the first modern terminological dictionary of medicine in Spanish. The intention of this paper is to present from a philological viewpoint the process by which a lexicographical work that deserves to be better known and used in studies on historical lexicography came to be constructed.

  10. Nueva ruralidad en territorios periféricos: los productores caprinos del noreste de Mendoza (Argentina

    Directory of Open Access Journals (Sweden)

    Laura María Torres

    2008-07-01

    Full Text Available Lately, several authors have been analyzing the changes in rural areas triggered by globalization. The concepts of new rurality and pluriactivity have allowed progress along these lines, highlighting the new difficulties facing the most vulnerable sectors. This study explores the transformation of peripheral rural territories in Mendoza (Argentina, particularly those that have been thought of as isolated and traditional. This research develops from a case study, combines quantitative and qualitative methods, and takes the production undertakings happening in those lands as units of analysis. Production and economic situations of the past are compared to those in the present. The tendency toward pluriactivity is here considered as a response to the new conditions, and also as an expression of the process of articulation with the capitalist system.

  11. Prevalence and infection intensity of Rickettsia massiliae in Rhipicephalus sanguineus sensu lato ticks from Mendoza, Argentina.

    Science.gov (United States)

    Monje, Lucas D; Linares, María Cielo; Beldomenico, Pablo M

    2016-11-01

    Rickettsia massiliae belongs to the spotted fever group and in the New World is commonly associated with the brown dog tick, Rhipicephalus sanguineus. Herein we investigate the presence of R. massiliae in Rh. sanguineus sensu lato ticks in a location near the Andean foothills (Mendoza, Argentina), to provide a prevalence estimate and to assess the infection intensity of this pathogen. Rickettsia massiliae infection was found in 5.1% of the Rh. sanguineus s.l ticks analyzed, all with high infection intensities. Molecular analysis determined that all R. massiliae-infected Rh. sanguineus s.l. ticks belonged to the temperate lineage. Copyright © 2016 Institut Pasteur. Published by Elsevier Masson SAS. All rights reserved.

  12. Geofisica del cuerpo ultramáfico de la mina Salamanca, provincia de Mendoza

    Directory of Open Access Journals (Sweden)

    J. Kostadinoff

    2004-03-01

    Full Text Available La faja de rocas máficas-ultramáficas de la Cordillera Frontal de Mendoza es considerada como una ofiolita desmembrada. La presencia en las rocas ultramáficas serpentinízadas portadoras de mineralizaciónes de talco, sulfuros polimetálicos y de elementos del grupo del platino (EGP constituyen un atractivo para la realización de prospecciones geofísicas. La metodología de trabajo consistió en medir una red de estaciones geofísicas (gravimetría y magnetometría, en el área de la mina Salamanca. Los resultados permitieron evaluar las reservas de talco y calibrar un modelo de prospección geofísica para los sulfuros polimetálicos presentes en la faja de rocas máficas - ultramáficas de la Cordillera Frontal.

  13. Lake Andes National Wildlife Refuge Complex : Annual narrative report : Calendar year 1993

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR, Karl Mundt NWR, and Lake Andes WMD outlines Refuge accomplishments during the 1993 calendar year. The report begins...

  14. Lake Andes National Wildlife Refuge: Annual narrative report: Calendar year 1982

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR, Lake Andes WMD, and Karl E. Mundt NWR outlines Refuge accomplishments during the 1982 calendar year. The report...

  15. Lake Andes National Wildlife Refuge: Annual narrative report: Calendar year 1984

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR, Lake Andes WMD, and Karl E. Mundt NWR outlines Refuge accomplishments during the 1984 calendar year. The report...

  16. Lake Andes National Wildlife Refuge Complex : Annual narrative report : Calendar year 1991

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR, Karl Mundt NWR, and Lake Andes WMD outlines Refuge accomplishments during the 1991 calendar year. The report begins...

  17. Lake Andes National Wildlife Refuge: Annual narrative report: Calendar year 1990

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR, Lake Andes WMD, and Karl E. Mundt NWR outlines Refuge accomplishments during the 1990 calendar year. The report...

  18. Lake Andes National Wildlife Refuge: Annual narrative report: Calendar year 1983

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR, Lake Andes WMD, and Karl E. Mundt NWR outlines Refuge accomplishments during the 1983 calendar year. The report...

  19. Lake Andes National Wildlife Refuge: Annual narrative report: Calendar year 1989

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR, Lake Andes WMD, and Karl E. Mundt NWR outlines Refuge accomplishments during the 1989 calendar year. The report...

  20. Lake Andes National Wildlife Refuge: Annual narrative report: Calendar year 1988

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR, Lake Andes WMD, and Karl E. Mundt NWR outlines Refuge accomplishments during the 1988 calendar year. The report...

  1. Lake Andes National Wildlife Refuge: Annual narrative report: Calendar year 1985

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR, Lake Andes WMD, and Karl E. Mundt NWR outlines Refuge accomplishments during the 1985 calendar year. The report...

  2. Lake Andes National Wildlife Refuge : Annual narrative report : Calendar year 1992

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR, Karl Mundt NWR, and Lake Andes WMD outlines Refuge accomplishments during the 1992 calendar year. The report begins...

  3. Lake Andes National Wildlife Refuge: Annual narrative report: Calendar year 1987

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR, Lake Andes WMD, and Karl E. Mundt NWR outlines Refuge accomplishments during the 1987 calendar year. The report...

  4. Lake Andes National Wildlife Refuge: Annual narrative report: Calendar year 1986

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR, Lake Andes WMD, and Karl E. Mundt NWR outlines Refuge accomplishments during the 1986 calendar year. The report...

  5. Lake Andes National Wildlife Refuge: Annual narrative report: Calendar year 1981

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR, Lake Andes WMD, and Karl E. Mundt NWR outlines Refuge accomplishments during the 1981 calendar year. The report...

  6. Regional climate change scenarios applied to viticultural zoning in Mendoza, Argentina

    Science.gov (United States)

    Cabré, María Fernanda; Quénol, Hervé; Nuñez, Mario

    2016-09-01

    Due to the importance of the winemaking sector in Mendoza, Argentina, the assessment of future scenarios for viticulture is of foremost relevance. In this context, it is important to understand how temperature increase and precipitation changes will impact on grapes, because of changes in grapevine phenology and suitability wine-growing regions must be understood as an indicator of climate change. The general objective is to classify the suitable areas of viticulture in Argentina for the current and future climate using the MM5 regional climate change simulations. The spatial distribution of annual mean temperature, annual rainfall, and some bioclimatic indices has been analyzed for the present (1970-1989) and future (2080-2099) climate under SRES A2 emission scenario. In general, according to projected average growing season temperature and Winkler index classification, the regional model estimates (i) a reduction of cool areas, (ii) a westward and southward displacement of intermediate and warm suitability areas, and (iii) the arise of new suitability regions (hot and very hot areas) over Argentina. In addition, an increase of annual accumulated precipitation is projected over the center-west of Argentina. Similar pattern of change is modeled for growing season, but with lower intensity. Furthermore, the evaluation of projected seasonal precipitation shows a little precipitation increase over Cuyo and center of Argentina in summer and a little precipitation decrease over Cuyo and northern Patagonia in winter. Results show that Argentina has a great potential for expansion into new suitable vineyard areas by the end of twenty-first century, particularly due to projected displacement to higher latitudes for most present suitability winegrowing regions. Even though main conclusions are based on one global-regional model downscaling, this approach provides valuable information for implementing proper and diverse adaptation measures in the Argentinean viticultural

  7. Geophysical characterization of circular structures in Chubut and Mendoza (Argentina): Impact vs. Volcanism

    Science.gov (United States)

    Prezzi, C.; Orgeira, M. J.; Risso, C.; Acevedo, R.; Ponce, F.; Nullo, F.; Martinez, O.; Rabassa, J.; Margonari, L.; Corbella, H.

    2013-05-01

    This work focuses on two main objectives. One of them is to provide information to discern the genesis of the circular structures present in Bajada del Diablo (Chubut, Argentina) considered as impact craters, and the other one is to contribute to a better knowledge of the circular structures located in the volcanic fields of Llancanelo and Payunia (Mendoza, Argentina). Chubut circular structures have been attributed to the collision of an extraterrestrial body, possibly an asteroid. However, doubts persist about their genesis because of the lack of direct geological evidences. Since detailed geomorphological studies have ruled out an origin by wind deflation, the prevailing alternative hypothesis attributes these circular structures to a volcanic process. On the other hand, the study of the volcanic fields of Payunia and Llancanelo (Mendoza) will contribute to the knowledge of the mechanics of hydromagmatic processes in the area, and the origin of circular structures morphologically similar to those located in Chubut. In the Payunia volcanic field at least 27 cones with evidences of hydromagmatism, in a field of more than 800 pure magmatic cones, have been recognized. This study tries to determine if a relationship between the observed volcanic circular structures and participation of water during the eruption exists. Magnetic and gravity field surveys of the circular volcanic structures in Llancanelo and Payunia volcanic fields were performed in order to determine their relationship with the type of eruption. Electromagnetic, magnetic and gravity field surveys were also carried out in Chubut circular structures. The comparative analysis of geological and geophysical results obtained in the circular structures of Chubut and those obtained in the circular structures in the volcanic areas of Llancanelo and Payunia suggest an impact origin for the circular structures of Chubut.

  8. Regional climate change scenarios applied to viticultural zoning in Mendoza, Argentina.

    Science.gov (United States)

    Cabré, María Fernanda; Quénol, Hervé; Nuñez, Mario

    2016-09-01

    Due to the importance of the winemaking sector in Mendoza, Argentina, the assessment of future scenarios for viticulture is of foremost relevance. In this context, it is important to understand how temperature increase and precipitation changes will impact on grapes, because of changes in grapevine phenology and suitability wine-growing regions must be understood as an indicator of climate change. The general objective is to classify the suitable areas of viticulture in Argentina for the current and future climate using the MM5 regional climate change simulations. The spatial distribution of annual mean temperature, annual rainfall, and some bioclimatic indices has been analyzed for the present (1970-1989) and future (2080-2099) climate under SRES A2 emission scenario. In general, according to projected average growing season temperature and Winkler index classification, the regional model estimates (i) a reduction of cool areas, (ii) a westward and southward displacement of intermediate and warm suitability areas, and (iii) the arise of new suitability regions (hot and very hot areas) over Argentina. In addition, an increase of annual accumulated precipitation is projected over the center-west of Argentina. Similar pattern of change is modeled for growing season, but with lower intensity. Furthermore, the evaluation of projected seasonal precipitation shows a little precipitation increase over Cuyo and center of Argentina in summer and a little precipitation decrease over Cuyo and northern Patagonia in winter. Results show that Argentina has a great potential for expansion into new suitable vineyard areas by the end of twenty-first century, particularly due to projected displacement to higher latitudes for most present suitability winegrowing regions. Even though main conclusions are based on one global-regional model downscaling, this approach provides valuable information for implementing proper and diverse adaptation measures in the Argentinean viticultural

  9. Metasomatismo en ortoanfibolitas de la Faja máfica-ultramáfica del río de las tunas, Mendoza Metasomatism in orthoamphibolites from the Río de Las Tunas mafic-ultramafic belt, Mendoza

    Directory of Open Access Journals (Sweden)

    M. Florencia Gargiulo

    2012-06-01

    áticos y la secuencia de reemplazo observada en ellos, sugieren que tales asociaciones se generaron a causa de un proceso metasomático, acontecido en condiciones de bajo grado a una presión menor a 4 kbar, durante los estadios finales del ciclo de metamorfismo regional evidenciado en el área.In this contribution, petro-mineralogical and chemical evidences of metasomatism in orthoamphibolites from the Río de Las Tunas mafic-ultramafic belt in Frontal Cordillera of Mendoza province are provided. These orthoamphibolites integrate the metamorphic basement of the Frontal Cordillera and they belong to the Guarguaráz Metamorphic Complex. These rocks show mineral associations and textural relationships indicating disequilibrium conditions between some of the mineral phases. Hornblendic amphibole crystals show a reaction border with development of clinopyroxene (ferroan dioside; meanwhile the calcicplagioclase is mostly replaced by a fine-grained matrix integrated by the mineral association of garnet-epidotes.l -prehnite-pumpellyite- albite. The amphibole and clinopyroxene crystals are also partially replaced by pumpellyite and/or chlorite, meanwhile the matrix is slightly replaced by muscovite and calcite. Garnet compositions belong to the grossular-andradite series and their average composition is: Alm05Adr53Prp01Sps04Grs36Uv01. Some crystals with Cr2O3 content between 11.69-13.17 wt.% and with a subtle chemical zonation (uvarovitic core: Alm03Adr13Prp00Sps02Grs35Uv47 with more grossularic border: Alm03Adr12 Prp00Sps01Grs44Uv40 occur in relationship with magnetite crystals with up to 20% of the chromite component. Pressure estimations based on the compositional zoning of amphibole crystals gave values between 2.5-4.5 kbar. The observed mineral associations together with the textural and chemical characteristics of these rocks show that this kind of orthoamphibolites is completely different from the classical amphibolites of igneous protoliths outcropping in the study area

  10. Public health against a centralized state: institutions and welfare services in the province of Mendoza during the first Peronism

    Directory of Open Access Journals (Sweden)

    Ivana Hirschegger

    2016-10-01

    Full Text Available This research analyzes the state action in public health during the first Peronism and engages on some factors that determined the success or failure of policies at provincial level. The work also refers , through concrete examples , to smaller territorial units such as municipalities , while application areas of public policy or executors of them. Some of the questions that were attempted to answer what extent the new changes in the state structure were accompanied by concrete actions that have a bearing on the living conditions of the population? What obstacles limited government action? the realization of public works will be included in this analysis by the state , staff in charge , as well as investments in other resources necessary for adequate medical care.

  11. Diversification of clearwing butterflies with the rise of the Andes.

    Science.gov (United States)

    De-Silva, Donna Lisa; Elias, Marianne; Willmott, Keith; Mallet, James; Day, Julia J

    2016-01-01

    Despite the greatest butterfly diversity on Earth occurring in the Neotropical Andes and Amazonia, there is still keen debate about the origins of this exceptional biota. A densely sampled calibrated phylogeny for a widespread butterfly subtribe, Oleriina (Nymphalidae: Ithomiini) was used to estimate the origin, colonization history and diversification of this species-rich group. Neotropics. Ancestral elevation and biogeographical ranges were reconstructed using data generated from detailed range maps and applying the dispersal-extinction-cladogenesis model using stratified palaeogeographical time slice matrices. The pattern of diversification through time was examined by comparing constant and variable rate models. We also tested the hypothesis that a change in elevation is associated with speciation. The Oleriina likely originated in the Andes in the Early to Middle Miocene and rapidly diversified to include four genera all of which also originated in the Andes. These clades, together with four species groups, experienced varying spatial and temporal patterns of diversification. An overall early burst and decreasing diversification rate is identified, and this pattern is reflected for most subclades. Changes in the palaeogeological landscape, particularly the prolonged uplift of the Andes, had a profound impact on the diversification of the subtribe. The Oleriina mostly remained within the Andes and vicariant speciation resulted in some instances. Dynamic dispersal occurred with the disappearance of geological barriers such as the Acre System and the subtribe exploited newly available habitats. Our results confirm the role of the Andean uplift in the evolution of Neotropical biodiversity.

  12. The first ANDES elements: 9-DOF plate bending triangles

    Science.gov (United States)

    Militello, Carmelo; Felippa, Carlos A.

    1991-01-01

    New elements are derived to validate and assess the assumed natural deviatoric strain (ANDES) formulation. This is a brand new variant of the assumed natural strain (ANS) formulation of finite elements, which has recently attracted attention as an effective method for constructing high-performance elements for linear and nonlinear analysis. The ANDES formulation is based on an extended parametrized variational principle developed in recent publications. The key concept is that only the deviatoric part of the strains is assumed over the element whereas the mean strain part is discarded in favor of a constant stress assumption. Unlike conventional ANS elements, ANDES elements satisfy the individual element test (a stringent form of the patch test) a priori while retaining the favorable distortion-insensitivity properties of ANS elements. The first application of this formulation is the development of several Kirchhoff plate bending triangular elements with the standard nine degrees of freedom. Linear curvature variations are sampled along the three sides with the corners as gage reading points. These sample values are interpolated over the triangle using three schemes. Two schemes merge back to conventional ANS elements, one being identical to the Discrete Kirchhoff Triangle (DKT), whereas the third one produces two new ANDES elements. Numerical experiments indicate that one of the ANDES element is relatively insensitive to distortion compared to previously derived high-performance plate-bending elements, while retaining accuracy for nondistorted elements.

  13. Geochronological, morphometric and geochemical constraints on the Pampas Onduladas long basaltic flow (Payún Matrú Volcanic Field, Mendoza, Argentina)

    Science.gov (United States)

    Espanon, Venera R.; Chivas, Allan R.; Phillips, David; Matchan, Erin L.; Dosseto, Anthony

    2014-12-01

    The Pampas Onduladas flow in southern Mendoza, Argentina, is one of the four longest Quaternary basaltic flows on Earth. Such flows (> 100 km) are relatively rare on Earth as they require special conditions in order to travel long distances and there are no recent analogues. Favourable conditions include: a gentle topographic slope, an insulation process to preserve the melt at high temperature, and a large volume of lava with relatively low viscosity. This study investigates the rheological and geochemical characteristics of the ~ 170 km long Pampas Onduladas flow, assessing conditions that facilitated its exceptional length. The study also reports the first geochronological results for the Pampas Onduladas flow. 40Ar/39Ar step-heating analyses of groundmass reveal an eruption age of 373 ± 10 ka (2σ), making the Pampas Onduladas flow the oldest Quaternary long flow. The methods used to assess the rheological properties include the application of several GIS tools to a digital elevation model (DEM) to determine the length, width, thickness, volume and topographic slope of the flow as well as algorithms to determine its density, viscosity and temperature. The slope of the Pampas Onduladas flow determined from the initial part of the flow on the eastern side of La Carbonilla Fracture to its end point in the province of La Pampa is 0.84% (0.29°), the steepest substrate amongst long Quaternary flows. The rheological properties, such as density viscosity and temperature from the Pampas Onduladas flow are similar to values reported for other long Quaternary flows. However, the minimum volume calculated is relatively low for its length compared with other long Quaternary flows. Therefore, the extension of the Pampas Onduladas flow was probably controlled by a steep slope, combined with an insulating mechanism, which helped in providing optimal conditions for a travel length of almost 170 km.

  14. Evaluación del desempeño ambiental de dos bodegas en Mendoza (Argentina. Propuesta de reacondicionamiento térmico y energético

    Directory of Open Access Journals (Sweden)

    Carolina Ganem Karlen

    2015-07-01

    Full Text Available This article evaluates the thermal and energy performance of two wineries in the province of Mendoza, Argentina (32° 40’ S, 68° 51’ W, 750m above sea level. The grape harvesting period (February–March was selected for analysis because cooling demand at that time is higher: tons of hot raw material (at approximately 26-30°C enter the wineries to be processed at 8°C, while outdoor temperatures are around 38°C. The selected wineries have similar-sized buildings and the same quantity and quality of production, but different management and envelope materiality. Winery P was built with walls of traditional bricks, single pane windows and a metal roof with thermal insulation; while winery H´s walls were partially built of reinforced concrete panels with thermal insulation, insulated metal roofs and double pane windows. Air, envelope surface, relative humidity and solar radiation temperatures were measured in situ and studied in relation to the energy consumption records of each winery. Then, with the data obtained, a model was generated with Energy Plus software, which was used to simulate envelope improvement alternatives. As a result, both wineries showed improved performance. The temperatures measured in winery P reached an average of 18.89 °C without the use of auxiliary energy. In the case of winery H, temperatures were optimized, thereby achieving an average of 21.77 °C, once again without the use of auxiliary energy. Moreover, it is possible to integrate night ventilation strategies using outdoor temperatures that decrease 9.78 °C in the period analyzed. The thermal and energy refurbishment proposal, which integrates building and envelope improvements, results in minimum indoor temperatures of 15.65 °C without the use of auxiliary energy--optimal for wine production.

  15. Doña Mencía de Mendoza y su residencia en el Palacio del Real en Valencia

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    Hidalgo Ogáyar, Juana

    2011-03-01

    Full Text Available Documents preserved in the Archivo del Palau reveal the furnishings that Mencía de Mendoza had in the Royal Palace at Valencia, particularly luxury beds such as those of the Empress Isabel of Portugal and Queen Mary of France. Painters active at her court, especially Juan de Bolaños, are also discussed.

    Con la ayuda de varios documentos conservados en el Archivo del Palau, se dan a conocer diferentes enseres que Doña Mencía de Mendoza tenía en el Palacio del Real en Valencia, destacando camas de lujo como la de la Emperatriz Isabel de Portugal o la de María de Francia. Se dan a conocer algunos pintores activos en su corte como Juan de Bolaños.

  16. Cenozoic basin thermal history reconstruction and petroleum systems in the eastern Colombian Andes

    Science.gov (United States)

    Parra, Mauricio; Mora, Andres; Ketcham, Richard A.; Stockli, Daniel F.; Almendral, Ariel

    2017-04-01

    Late Mesozoic-Cenozoic retro-arc foreland basins along the eastern margin of the Andes in South America host the world's best detrital record for the study of subduction orogenesis. There, the world's most prolific petroleum system occur in the northernmost of these foreland basin systems, in Ecuador, Colombia and Venezuela, yet over 90% of the discovered hydrocarbons there occur in one single province in norteastern Venezuela. A successful industry-academy collaboration applied a multidisciplinary approach to the study of the north Andes with the aim of investigating both, the driving mechanisms of orogenesis, and its impact on hydrocarbon accumulation in eastern Colombia. The Eastern Cordillera is an inversion orogen located at the leading edge of the northern Andes. Syn-rift subsidence favored the accumulation of km-thick organic matter rich shales in a back-arc basin in the early Cretaceous. Subsequent late Cretaceous thermal subsidence prompted the accumulation of shallow marine sandstones and shales, the latter including the Turonian-Cenomanian main hydrocarbon source-rock. Early Andean uplift since the Paleocene led to development of a flexural basin, filled with mainly non-marine strata. We have studied the Meso-Cenozoic thermal evolution of these basins through modeling of a large thermochronometric database including hundreds of apatite and zircon fission-track and (U-Th)/He data, as well as paleothermometric information based on vitrinite reflectance and present-day temperatures measured in boreholes. The detrital record of Andean construction was also investigated through detrital zircon U-Pb geochronometry in outcrop and borehole samples. A comprehensive burial/exhumation history has been accomplished through three main modeling strategies. First, one-dimensional subsidence was used to invert the pre-extensional lithospheric thicknesses, the magnitude of stretching, and the resulting heat flow associated to extension. The amount of eroded section and

  17. Glacial recession in the Tropical Andes from the Little Ice Age: the case of Ampato Volcanic Complex (Southern Peru

    Science.gov (United States)

    Alcalá, J.; Palacios, D.; Zamorano, J. J.

    2010-03-01

    Europa (Cordillera Cantábrica, NO de España). Análisis morfológico y reconstrucción del avance glaciar histórico. Rev. C & G., 19 (3-4), 79-94. Hastenrath, S. L. (2009): Past glaciation in the tropics. Quaternary Science Reviews, 28: 790-798. Jomelli, V.; Favier, V.; Rabatel, A.; Brunstein, D.; Hoffmann, G.; and Francou, B. (2009): Fluctuations of glaciers in the tropical Andes over the last millennium and palaeoclimatic implications: A review. Palaeogeography, Palaeoclimatology, Palaeoecology, doi: 10.1016/j.palaeo.2008.10.033. Kaser, G., Osmaston, H.A., 2002. Tropical glaciers. Cambridge University Press, Cambridge. Mark, B. (2008): Tracing tropical Andean glaciers over space and time: Some lessons and transdisciplinary implications. Global and Planetary Change, 60: 101-114. Osmaston, H. (2005): Estimates of glacier equilibrium line altitudes by the Area _ Altitude, the Area _ Altitude Balance Ratio and the Area _ Altitude Balance Index Methods and their validation. Quaternary International, 138-139: 22-31. Rabatel, A., Jomelli, V., Naveau, P., Francou, B., Grancher, D. (2005). Dating of Little Ice Age glacier fluctuations in the tropical Andes: Charquini glaciers, Bolivia, 16ºS. C. R. Geoscience, 337: 1311-1322. Rabatel, A., Francou, B., Jomelli, V., Naveau, P., Grancher, D. (2008). A chronology of the Little Ice Age in the tropical Andes of Bolivia (16º S) and its implications for climate reconstruction. Quaternary Research, 70: 198-212. Ramirez, E., Francou, B., Ribstein, P., Descloitres, M., Guerin, R., Mendoza, J., Gallaire, R., Pouyaud, B., Jordan, E., 2001. Small glaciers disappearing in the tropical Andes: a case study in Bolivia: Glaciar Chacaltaya (16°S). Journal of Glaciology 47 (157), 187-194. Soruco, A.; Vincent, C.; Francou, B.; Ribstein, P.; Berger, T.; Sicart, J. E.; Wagnon, P.; Arnaud, Y.; Favier, V.; and Lejeune, Y. (2009): Mass balance of Glacier Zongo, Bolivia, between 1956 and 2006, using glaciological, hydrological and geodetic methods

  18. Centralización de la represión, violencia paraestatal y redes internacionales represivas en la Mendoza predictatorial

    Directory of Open Access Journals (Sweden)

    Laura Rodriguez Aguero

    2014-04-01

    Full Text Available Durante el tercer gobierno peronista (1973-1976 comenzó a montarse el dispositivo represivo que marcó los prolegómenos del Terrorismo de Estado llevado adelante por la dictadura militar de 1976. En Mendoza, la violencia paraestatal fue llevada a cabo por el CAM (Comando Anticomunista Mendoza, y el Comando Moralizador Pío XII. En este trabajo nos proponemos realizar a partir del uso de fuentes escritas y del testimonio de algunos/as sobrevivientes, una reconstrucción del accionar paraestatal, en vistas a analizar, por un lado, cómo se constituyeron en la dinámica local, las redes de relaciones implicadas en la práctica represiva y la inflexión que implicó noviembre de 1975 en la centralización de la represión; y por otro lado, cómo se manifestó el carácter internacional de la represión y la idea de aniquilación del “enemigo interno” en Mendoza, partiendo de la hipótesis de que la misma adquirió proporciones inusitadas debido a su carácter de provincia de frontera y su cercanía con Chile, en un momento de articulación de redes represivas en el Cono Sur.

  19. Los Censos históricos como fuente para el estudio de la participación femenina en el mercado: El caso de la provincia de Mendoza a comienzos del siglo XX

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    Juan Manuel Cerdá

    2009-07-01

    Full Text Available La inserción femenina en el mercado de trabajo a comienzos del siglo XX es un espacio escasamente explorado por los historiadores tradicionales, que amerita un análisis particular no solo desde la visión de género sino también como un grupo social que se vio afectado por el desarrollo capitalista de la Argentina agroexportadora. El propósito del presente trabajo es analizar las posibilidades y las limitaciones que brindan los Censos Nacionales históricos (1869, 1895 y 1914 para la reconstrucción de la participación femenina en el mercado de trabajo. Este proceso implicó un cambio en el mercado de trabajo en general, que, según algunos estudios, significó la disminución de la participación femenina durante las primeras décadas del siglo XX. Este trabajo pone en duda estas conclusiones sobre la base del análisis del caso particular de Mendoza. Esta provincia es importante, ya que a comienzos del siglo XX la vitivinicultura se convirtió en la principal actividad productiva de la provincia y la más importante en su rubro a nivel nacional, transformando el mercado de trabajo en general e influyendo de manera muy particular sobre las mujeres.The insertion of women in the labor market in the early 20th century is an issue scarcely explored by traditional historians and it deserves an individual analysis, not only from the point of view of the gender, but also as a social group that was affected by the capitalist development of the agro-exporting Argentina. The purpose of this paper is to evaluate the potential and the limitations of the information provided by the national census of 1896, 1895, and 1914 in order to recreate the female contribution to the labor market. The forementioned process determined a change in the labor market as a whole that, according to some papers, brought along the reduction of the female share in the first decades of the 20th century. This paper aims to argue that point, based on the study of the province

  20. ‘Large Igneous Provinces (LIPs)’: Definition, recommended terminology, and a hierarchical classification

    Science.gov (United States)

    Sheth, Hetu C.

    2007-12-01

    This article is an appeal for the adoption of a correct and appropriate terminology with respect to the so-called Large Igneous Provinces (LIPs). The term LIP has been widely applied to large basaltic provinces such as the Deccan Traps, and the term Silicic Large Igneous Province (SLIP) to volcanic provinces of dominantly felsic composition, such as the Whitsunday Province. However, neither term (LIP, SLIP) has been applied to the large granitic batholiths of the world (e.g., Andes) to which both terms are perfectly applicable. LIP has also not been applied to broad areas of contemporaneous basalt magmatism (e.g., Indochina, Mongolia) and sizeable layered mafic intrusions (e.g., Bushveld) which in many significant respects may also be considered to represent 'Large Igneous Provinces'. Here, I suggest that the term LIP is used in its broadest sense and that it should designate igneous provinces with outcrop areas ≥ 50,000 km 2. I propose a simple hierarchical classification of LIPs that is independent of composition, tectonic setting, or emplacement mechanism. I suggest that provinces such as the Deccan and Whitsunday provinces should be called Large Volcanic Provinces (LVPs), whereas large intrusive provinces (mafic-ultramafic intrusions, dyke/sill swarms, granitic batholiths) should be called Large Plutonic Provinces (LPPs). LVPs and LPPs thus together cover all LIPs, which can be felsic, mafic, or ultramafic, of sub-alkalic or alkalic affinity, and emplaced in continental or oceanic settings. LVPs are subdivided here into four groups: (i) the dominantly/wholly mafic Large Basaltic Provinces (LBPs) (e.g., Deccan, Ontong Java); (ii) the dominantly felsic Large Rhyolitic Provinces (LRPs) (e.g., Whitsunday, Sierra Madre Occidental); (iii) the dominantly andesitic Large Andesitic Provinces (LAPs) (e.g., Andes, Indonesia, Cascades), and (iv) the bimodal Large Basaltic-Rhyolitic Provinces (LBRPs) (e.g., Snake River-High Lava Plains). The intrusive equivalents of LRPs

  1. La vegetación de los Altos Andes II: Las Vegas del flanco oriental del Cordón del Plata (Mendoza, Argentina Vegetation of the high Andes II: The meadows on the eastern slope of the Cordón del Plata (Mendoza, Argentina

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    Eduardo Méndez

    Full Text Available Para completar estudios de vegetación de la vertiente oriental del Cordón del Plata, se analizaron las comunidades vegetales de sitios húmedos de vegas. Se determinaron dos tipos de vegas: de baja altura, entre los 1200- 2000 m s.m. y de altura, por encima de los 2000 m s.m. representadas por 9 y 11 comunidades respectivamente. Estas se describieron fisonómica, florística y ecológicamente. Se establecieron relaciones de distribuciones de las vegas entre altitudes y temperaturas, involucrando también a procesos de congelamiento de los suelos. Además, se consideraron aspectos biológicos, de origen y corológica de las especies. En coincidencia con los pisos de vegetación del área sobre las vegas de altura se reconocen tentativamente una de mediana altura distribuída entre los 2000 a 3200 m s. m. y una de tundra que no fue considerada en este trabajo , por encima de 3200 m s.m.. Se elaboró un mapa de localización de las vegas del área de estudio.In this study I present a description of the plant communities of humid sites of vegas or mallines of the eastern slope of the Cordón del Plata were analyzed. Two types of vegas were identified: 1 low altitude vegas between 1200- 2000 m a.s.l. represented by 9 communities; and 2 high altitude vegas above 2000 m a.s.l. represented by 11 communities. These communities were described through their physiognomy, floristic composition, and ecology. In order to analize the distribution of the vegas, relationships were drawn among altitude, temperature, and soil freezing processes. In addition, biological and chorological characteristics of the species, as well as their origins were considered. With respect to the vegetation distribution, high-altitude vegas occur at a intermediate altitudes between 2000 and 3,200 meters above sea level, and tundra (which was not considered as part of the study occurs above 3,200 meter above sea level. A map was produced of the location of the area's wetlands.

  2. Satellite images and geodetic measurements applied to the monitoring of the Horcones Inferior Glacier, Mendoza, Argentina

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    M. Gabriela Lenzano

    2011-06-01

    Full Text Available This work analyzes the monitoring of the covered and regenerated Horcones Inferior Glacier (HIG since the implementation of a semi-permanent GNSS station (HISS on its surface during the summer seasons of 2009 and 2010. The glacier is located at 32° 41's and 69° 57'w, at the foot of the south wall of Mt. Aconcagua, Aconcagua Provincial Park, Mendoza, Argentina. The average velocities obtained from the HISS station were of 1.3 cm/d and 3.5 cm/d during the 2009 and 2010 seasons respectively. The data procured using satellite images during the last surges (1984 and 2003 gave average velocities for the HIG front of 8.7 m/d for the first event and 11.5 m/d for the second one. These results allowed getting accurate and reliable movement tendency at the terminal part of the HIG during the 1984-2010 period.El presente trabajo realiza el monitoreo del glaciar Horcones Inferior, cubierto y regenerado a partir de la implementación de una estación GNSS semi-permanente (HISS, instalada sobre su superficie durante las temporadas de verano de 2009 y 2010 respectivamente. El glaciar se encuentra ubicado a los 32° 41's y 69° 57'w, al pie de la pared sur del C° Aconcagua, en el Parque Provincial Aconcagua, Mendoza, Argentina. La estación HISS registró valores de velocidades medias de 1.3 cm/d y 3.5 cm/d durante las temporadas de 2009 y 2010. Se utilizaron imágenes satelitales para el seguimiento del frente del glaciar durante los últimos surges (1984 y 2003, cuyas velocidades medias fueron de 8.7 m/d para el primero y de 11.5 m/d para el segundo evento. Estos resultados permitieron obtener de manera precisa y confiable la tendencia de movimiento de la parte terminal del GHI durante el periodo 1984-2010.

  3. Desarrollo poblacional de Diaspidiotus perniciosus (Hemiptera: Diaspididae en cultivos de manzano de San Carlos, Mendoza, Argentina

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    Guillermo P. LOPEZ GARCIA

    2011-01-01

    Full Text Available Se estudió la bionomía de Diaspidiotus perniciosus Comstock (“escama de San José”, en manzanos de la variedad “Red delicious” de San Carlos, Mendoza, Argentina, durante los ciclos productivos 2007-2008 y 2008-2009. Se determinó el número de generaciones anuales y se estudiaron las fluctuaciones poblacionales asociadas a la integral térmica para la especie en esta región. D. perniciosus presenta dos generaciones superpuestas al ciclo del cultivo, mientras que las ninfas (N1 y N2 de la tercera generación se desarrollan solamente hasta el final de la temporada estival y pasan al estado de quiescencia, en el que permanecen durante el invierno. El desarrollo de D. perniciosus en esta zona coincide con el de esta especie en la zona frutícola del centro de Chile en cuanto al número de generaciones y al periodo de quiescencia invernal. La población quiescente en Chile está integrada predominantemente por ninfas del primer estadio (N1, mientras que en San Carlos, Mendoza, la población quiescente está integrada principalmente por ninfas del segundo estadio (N2. La similitudes entre ambas poblaciones se deben, probablemente, a las coincidencias en latitud, clima y especie hospedera. El impacto económico de D. perniciosus en la zona de estudio tiene mayor relevancia durante los meses de diciembre y enero, cuando se observa una alta incidencia de daños en los frutos y las hojas; este es el momento decisivo para implementar medidas de control fitosanitario. Estas deberán aplicarse en función de los máximos poblacionales de N1 que se producen con 600-650 Grados-Día (oD en diciembre y con 1.170-1.270oD en enero. En las temporadas en las que la densidad poblacional de la plaga es especialmente alta, podrían incorporarse medidas adicionales de control con 1.800-2.000oD durante el mes de abril. Los resultados de estos estudios representan una herramienta predictiva, que permitirá elaborar estrategias para el control de poblaciones de

  4. Rapid millennial-scale vegetation changes in the tropical Andes

    NARCIS (Netherlands)

    Urrego, D.H.; Hooghiemstra, H.; Rama-Corredor, O.; Martrat, B.; Grimalt, J.O.; Thompson, L.

    2015-01-01

    We compare eight pollen records reflecting climatic and environmental change from the tropical Andes. Our analysis focuses on the last 50 ka, with particular emphasis on the Pleistocene to Holocene transition. We explore ecological grouping and downcore ordination results as two approaches for extra

  5. Andes hantavirus variant in rodents, southern Amazon Basin, Peru.

    Science.gov (United States)

    Razuri, Hugo; Tokarz, Rafal; Ghersi, Bruno M; Salmon-Mulanovich, Gabriela; Guezala, M Claudia; Albujar, Christian; Mendoza, A Patricia; Tinoco, Yeny O; Cruz, Christopher; Silva, Maria; Vasquez, Alicia; Pacheco, Víctor; Ströher, Ute; Guerrero, Lisa Wiggleton; Cannon, Deborah; Nichol, Stuart T; Hirschberg, David L; Lipkin, W Ian; Bausch, Daniel G; Montgomery, Joel M

    2014-02-01

    We investigated hantaviruses in rodents in the southern Amazon Basin of Peru and identified an Andes virus variant from Neacomys spinosus mice. This finding extends the known range of this virus in South America and the range of recognized hantaviruses in Peru. Further studies of the epizoology of hantaviruses in this region are warranted.

  6. Gastrointestinal parasites of Lamas in the Bolivian Andes

    DEFF Research Database (Denmark)

    Nissen, Anne Malene; Nees, Ellinor Spörndly; Monrad, Jesper

    A cross sectional study was conducted to determine prevalences and intensities of gastrointestinal (GIT) parasites in lamas in the Bolivian Andes. A quantitative and qualitative necro-copro-parasitlogical study was performed on 33 lamas between October and December 2007. At the time of necropsy the...

  7. Lithospheric scale model of Merida Andes, Venezuela (GIAME Project)

    Science.gov (United States)

    Schmitz, M.; Orihuela, N. D.; Klarica, S.; Gil, E.; Levander, A.; Audemard, F. A.; Mazuera, F.; Avila, J.

    2013-05-01

    Merida Andes (MA) is one of the most important orogenic belt in Venezuela and represents the northern culmination of South America Andes. During the last 60 years, several models have been proposed to explain the shallow and deep structure, using different geological, geophysical, seismological, geochemical and petrologic concepts; nevertheless, most of them have applied local observation windows, and do not represent the major structure of MA. Therefore, a multidisciplinary research group, coordinated by FUNVISIS, in close cooperation with UCV, ULA and PDVSA, is proposed in order to get the outlined goals in the project entitled GIAME ("Geociencia Integral de los Andes de MErida") was established, which aims to generate a lithospheric scale model and the development of a temporal dynamic model for the MA. As a base for lithospheric investigations of the Merida Andes, we are proposing three wide angle seismic profiles across the orogen on three representative sites, in order to determine the inner structure and its relation with the orogen's gravimetric root. To the date, there are no seismic studies at lithospheric scale which cross MA. The wide angle seismic will be complemented with the re-processing and re-interpretation of existing reflection seismic data, which will allow to establish a relationship between MA and its associated flexural basins (Maracaibo and Barinas-Apure basins). Depending on the results of the VENCORP Project (VENezuelan COntinental Reflection Profiling), which might show some reliable results about crustal features and Moho reflectors along three long seismic profiles at Caribbean Moutain system, a reflection seismic profile across the central portion of MA is proposed. Additional tasks, consisting in MA quaternary deformation studies, using research methods like neotectonics and paleoseismology, georadar, numerical modeling, cinematic GPS, SAR interferometry, thermocronology, detailed studies on regional geology, flexural modeling

  8. Flood risk assessment. Case of study: Motozintla de Mendoza, Chiapas, Mexico

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    David A. Novelo-Casanova

    2016-09-01

    Full Text Available Due to its geographical location, the community of Motozintla de Mendoza (Motozintla in the State of Chiapas, Mexico, is continuously exposed to the impact of natural hazards. In this work, we assessed the flood risk of Motozintla considering the structural, socioeconomic, organizational, and global (structural, socioeconomic, and organizational vulnerabilities. In addition, we also measured the local risk perception. Spatial maps were generated to determine the most vulnerable and risk areas of this community. Our results indicate that the population has a high level of risk to flooding mainly because (1 the majority of the local houses has high structural vulnerability; (2 a high percentage of the families has a daily income less than the official Mexican minimum wage and lacks of basic public services as well as of proper social security services; (3 most of the community does not know any existing Civil Protection Plan; and (4 the community organization for disaster mitigation and response is practically non-existent. For these reasons, we believe that it is necessary for local authorities to establish in the short-term, preparedness, mitigation and response plans as well as land-use measures to reduce the risk to floods in Motozintla.

  9. Projectile motion in Diego Hurtado de Mendoza's Mecánica and new Renaissance dynamics

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    Iommi Echeverría, Virginia

    2011-06-01

    Full Text Available This article considers Diego Hurtado de Mendoza’s translation of the Aristotelian Mechanics in relation to the humanistic and scientific Italian environment of the Renaissance. From the analysis of the last problems on dynamics, it demonstrates the affinity with the works of Piccolomini and Cardano. It also shows the originality of the exegesis made by the Spanish author of Problem XXXIV, in which he combines latemedieval physics with the Aristotelian explanation.Este artículo examina la traducción hecha por Diego Hurtado de Mendoza de la Mecánica aristotélica en el contexto del ambiente científico-humanista italiano de mediados del siglo XVI. A partir del análisis de los últimos problemas sobre dinámica, se demuestra su estrecha relación con las obras de Piccolomini y Cardano; sugiriéndose además la originalidad de la interpretación hecha por el autor español del problema XXXIV basada en la combinación de la física tardomedieval y la explicación aristotélica.

  10. Hilos de agua, lazos de sangre: enfrentando la escasez en el desierto de Lavalle (Mendoza, Argentina

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    L.M. Torres

    2008-01-01

    Full Text Available En el trabajo se analizan las posibles relaciones existentes entre las dinámicas de uso de los recursos naturales y las estrategias de localización de las unidades domésticas en el territorio, dentro de espacios rurales de desierto que poseen una oferta ambiental limitada. ¿Cómo, en el marco de qué estrategias, los grupos humanos convierten distintas porciones de la naturaleza en recurso natural? y ¿cómo usan y administran esos recursos en procura de asegurar su propia reproducción social? Para avanzar en esta dirección se analiza un estudio de caso (el desierto de Lavalle, provincia de Mendoza, Argentina y, dentro de él, se procede con las técnicas cualitativas de entrevista en profundidad y observación participante. Los datos que se presentan sugieren que en los territorios analizados rurales, emplazados en tierras secas, afectados por desertificación y con elevados índices de pobreza- las limitaciones que impone el medio ambiente son sobrellevadas –en alguna medida- mediante una estrategia de localización íntimamente relacionada con el proceso de producción, que maximiza el acceso de determinados recursos naturales y que "ordena" la competencia por ellos con los vecinos y parientes.

  11. Diseño participativo de espacios urbanos bioclimáticos. Experiencia en Mendoza (Argentina

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    Claudia Fernanda Martinez

    2015-04-01

    Full Text Available El presente trabajo reconoce los beneficios de las técnicas participativas de diseño para la producción social y sustentable del hábitat, al equilibrar soluciones bioclimáticas con los intereses de los beneficiarios. Como metodología, se aplicaron talleres comunitarios orientados tradicionalmente solo a la vivienda, para el diseño participativo de espacios urbanos conexos y sus redes en un conjunto habitacional de la provincia de Mendoza (Argentina. El desarrollo de talleres de diseño participativo pone de manifiesto la importancia de transferir a la comunidad beneficiaria de planes de vivienda de interés social los conceptos de la arquitectura bioclimática y sus implicaciones en la calidad de vida de las personas, el ahorro energético y la sustentabilidad ambiental. Los resultados indican que es posible conciliar el diseño de espacios urbanos eficientes energética y ambientalmente con cero sobrecosto y que, al mismo tiempo satisfagan las expectativas de los usuarios.

  12. Longitudinal Taphonomic Studies of Mammal Carcasses from the Rio Salado Valley, Mendoza, Argentina

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    Clara Otaola

    2016-02-01

    Full Text Available Taphonomic studies aid in understanding the transition of organic matter from living contexts (the biosphere to geological contexts (the lithosphere, and how agents and processes affect skeletal remains in the archaeological record. Archaeological research in the Atuel River valley, Mendoza, Argentina, has been carried out for several years. However, actualistic approaches to examine local and regional taphonomic processes have only been recently developed in this area. Longitudinal studies of disarticulation and dispersion of bones from carcasses are presented here in order to understand how skeletal materials are naturally added to, subtracted from, and mixed within the archaeological record. In this paper we explore variability in the influence of taphonomic processes in different microhabitats of the valley and how these mechanisms impact the potential of mixing during bone deposition in the archaeological record. There are some qualitative differences between carcasses deposited in different landforms, showing that each place has its own taphonomic history, principally influenced by the geomorphic and ecologic processes that operate in different landforms.

  13. Osteoporosis Self-Assessment Tool Performance in a Large Sample of Postmenopausal Women of Mendoza, Argentina

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    Fernando D. Saraví

    2013-01-01

    Full Text Available The Osteoporosis Self-assessment Tool (OST is a clinical instrument designed to select patients at risk of osteoporosis, who would benefit from a bone mineral density measurement. The OST only takes into account the age and weight of the subject. It was developed for Asian women and later validated for European and North American white women. The performance of the OST in a sample of 4343 women from Greater Mendoza, a large metropolitan area of Argentina, was assessed. Dual X-ray absorptiometry (DXA scans of lumbar spine and hip were obtained. Patients were classified as either osteoporotic (N=1830 or nonosteoporotic (n=2513 according to their lowest T-score at any site. Osteoporotic patients had lower OST scores (P<0.0001. A receiver operating characteristic (ROC curve showed an area under the curve of 71% (P<0.0001, with a sensitivity of 83.7% and a specificity of 44% for a cut-off value of 2. Positive predictive value was 52% and negative predictive value was 79%. The odds ratio for the diagnosis of osteoporosis was 4.06 (CI95 3.51 to 4.71; P<0.0001. It is concluded that the OST is useful for selecting postmenopausal women for DXA testing in the studied population.

  14. Pollution trends using bark of morus alba in the cities of buenos aires and mendoza (Argentina Tendências de poluição usando cascas de morus alba nas cidades de buenos aires e mendoza (Argentina

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    Patricia Perelman

    2010-06-01

    Full Text Available A comparative study of elements deposited on tree bark was carried out for urban and periurban areas of two of the most important cities in Argentina. The content of Fe, Mg, Al, Mn, Zn, Pb, Ba, Cr, Hg, Cu, Ni, Cd and Sb was determined by inductively coupled plasma atomic emission spectrometry (ICP-OES in Morus alba tree bark collected in the cities of Buenos Aires and Mendoza. The main air pollutants detected in the Buenos Aires urban area were Ba, Cr, Cu and Ni and indicate significative difference from the Mendoza urban and periurban areas. Significantly, higher concentrations of Zn, Ba, Cr and Cu were recorded in the periurban area of the city of Buenos Aires than in Mendoza. Bark samples were strongly influenced by dust and show Al, Fe, Mg and other element accumulations that indicate that soil particles were carried out by wind. Elements like Ba and Zn, commonly linked to traffic emissions, showed the highest concentrations in the Buenos Aires metropolitan area, possibly due to more intensive vehicular traffic. Our results indicated that intensity of vehicular traffic and not city structure is responsible for air pollution.Um estudo comparativo dos elementos depositados nas cascas das árvores foi realizado nas áreas urbanas e na periferia de duas cidades das mais importantes da Argentina. Os índices do Fe, Mg, Al, Mn, Zn, Pb, Ba, Cr, Cu, Ni e do Sb foram determinados pela espectrometria da emissão atômica com plasma acoplado indutivamente (ICP-OES nas cascas da árvore Morus alba, coletados nas cidades de Buenos Aires e Mendoza. Os principais elementos da contaminação do ar detectadas na área urbana de Buenos Aires foram Ba, Cr, Cu e Ni, que indicaram diferenças significativas nas áreas urbanas e na periferia de Mendoza. Uma concentração do Zn, Ba, Cr e do Cu foi achada na periferia da cidade de Buenos Aires, significativamente mais elevada do que em Mendoza. As amostras da casca foram influenciadas fortemente pela poeira e

  15. Abastecimiento y producción lítica en el sitio Valle Hermoso 1 (Malargüe, Mendoza) Lithic procurement and production in Valle Hermoso 1 Site, Malargüe, Mendoza

    OpenAIRE

    Gustavo Federico Bonnat

    2011-01-01

    En el presente texto se darán a conocer los resultados obtenidos del análisis del registro lítico del sitio Valle Hermoso 1 (Malargüe, provincia de Mendoza). El objetivo general de este trabajo es, desde una perspectiva organizacional de la tecnología, estudiar las estrategias de abastecimiento y producción lítica desarrolladas en el sitio por grupos cazadores-recolectores que habitaron el área de Valle Hermoso durante los últimos 2000 años. Los resultados obtenidos en el análisis del conjunt...

  16. Capacitación docente e innovación : Experiencia en la Universidad Tecnológica Nacional. Facultad Regional Mendoza

    OpenAIRE

    Carbonari, Daniela Beatriz; Correa, Claudia Roxana; Bruno, Andrea Paula; Sejas, Diego Martin

    2011-01-01

    En este trabajo se presenta una reflexión a partir de la experiencia obtenida con el curso “Creando espacios de aprendizaje con Moodle” que se desarrolla con modalidad a distancia y es ofrecido a los docentes de las distintas carreras de ingeniería, tecnicaturas y licenciaturas que se dictan en la Facultad Regional Mendoza de la Universidad Tecnológica Nacional. A su vez, este curso se enmarca dentro de un plan de capacitación integral que lleva adelante la Regional Mendoza para todos sus doc...

  17. Organización territorial urbana y transporte público masivo: Metrópolis del Gran Mendoza

    OpenAIRE

    María Emilia García Schilardi

    2015-01-01

    Existe acuerdo entre los expertos en transporte, planificación y urbanismo que la movilidad urbana es consecuencia de la organización espacial que adopta la ciudad y viceversa. Es decir, existe una estrecha relación entre las políticas de transporte y el ordenamiento del territorio. El objetivo de este trabajo es caracterizar la relación existente en la actualidad entre la organización territorial urbana de la zona del Gran Mendoza y el sistema de transporte masivo que opera en ella. Se estud...

  18. La obra lexicográfica de Manuel Hurtado de Mendoza: sus diccionarios enciclopédicos de medicina

    OpenAIRE

    Bertha M. Gutiérrez Rodilla

    2012-01-01

    [ES]La figura de Manuel Hurtado de Mendoza ya se ha analizado suficientemente en relación con sus aportaciones a la anatomía española de la primera mitad del siglo XIX o a la introducción en España de algunas novedades europeas. Sin embargo, todavía queda por estudiar buena parte de su obra, como ocurre con los diccionarios de medicina que compuso, dos enciclopédicos y uno terminológico. De los dos primeros nos ocupamos en este trabajo, en el que ponderaremos su importancia en ...

  19. La obra lexicográfica de Manuel Hurtado de Mendoza: sus diccionarios enciclopédicos de medicina

    OpenAIRE

    Bertha M. Gutiérrez Rodilla

    2012-01-01

    The figure of Manuel Hurtado de Mendoza has been sufficiently analyzed in connection with his contributions to Spanish anatomy during the first half of the 19th century or to the introduction of some European innovations in Spain. However, there is still much of his work to be studied, such as the medical dictionaries he wrote, two encyclopedic and one terminological. We deal with the first two in this essay, where we will speak highly of his significance in an age in which specialized lexico...

  20. Nuevas tendencias en la dinamica demografica y en el crecimiento urbano de la Provincia de Mendoza, Argentina

    OpenAIRE

    Cozzani, Maria Rosa

    2017-01-01

    El texto relaciona la evolución de los sistemas espaciales urbanos con la dinámica de crecimiento de la población y sus componentes. Ambos procesos son analizados en el territorio de la provincia de Mendoza, situada en el centro oeste Argentino, que presentaba un sistema urbano altamente jerarquizado desde el punto de vista demográfico y funcional por una aglomeración metropolitana, y ciudades intermedias, de tamaño menor según la concentración de habitantes y el espacio que estructuran. El e...

  1. Geología de la región del Cerro Guanaquero, Río Diamante, Mendoza

    OpenAIRE

    Federico Fuentes; Ramos,Victor A.

    2008-01-01

    El estudio realizado presenta nuevos datos sobre un sector poco conocido de la Cordillera Principal de Mendoza, en la alta cuenca del río Diamante en las adyacencias del cerro Guanaquero, y los primeros datos geocronológicos de sus rocas volcánicas. Las unidades geológicas presentes en el área se dividen en cuatro grupos principales: secuencias sedimentarias mesozoicas marinas y continentales intensamente plegadas y falladas; intrusivos y volcanitas intermedias de edad neógena; rocas volcánic...

  2. MEDICINAL PLANTS USED IN TRADITIONAL HERBAL MEDICINE IN THE PROVINCE OF CHIMBORAZO, ECUADOR.

    Science.gov (United States)

    Morales, Fátima; Padilla, Susana; Falconí, Félix

    2017-01-01

    Phyto-therapy studies on Chimborazo province in Ecuador are really limited. This area, located within the Andes, is considered a millenarian and intercultural province, where multiples cultures and ethnic groups coexist. The study was conducted through direct interviews with 84 ancestral healers from the Province of Chimborazo, Ecuador. We presented ten most used species by ancestral healers of Chimborazo province to cure different illnesses and their medicinal uses. We also provided the application mode and some features of healing that should be emphasized. The nettle was the medicinal plant employed for more different illness and the chamomile was the one with higher prevalence. We could confirm that the Native Ecuadorians have a vast variety of traditions and popular medicinal practices that have great value and are needed to be researched and studied extensively.

  3. Sr, Nd, Pb and Hf isotopic constraints on mantle sources and crustal contaminants in the Payenia volcanic province, Argentina

    DEFF Research Database (Denmark)

    Søager, Nina; Holm, Paul Martin; Thirlwall, Matthew F.

    2015-01-01

    The presented Sr, Nd, Hf and double-spike Pb-isotopic analyses of Quaternary basalts from the Payenia volcanic province in southern Mendoza, Argentina, confirm the presence of two distinct mantle types feeding the Payenia volcanism. The southern Payenia mantle source feeding the intraplate-type Río...... is suggested to be caused by step-wise melt extraction due to repeated injections of subduction zone fluids and melts. The lower crustal contamination trends found in the trace element variations of basalt groups from all parts of the Payenia province are also recognized in isotopic space and the dominant...... isotope assimilation trends indicate lower crustal contaminants with more unradiogenic Pb, lower 143Nd/144Nd and 176Hf/177Hf and higher or similar 87Sr/86Sr as the mantle melts. These characteristics are similar to those found in lower crustal xenoliths from the northern Proterozoic Cuyania terrane...

  4. Ceremonial tobacco use in the Andes: implications for smoking prevention among indigenous youth.

    Science.gov (United States)

    Alderete, Ethel; Erickson, Pamela I; Kaplan, Celia P; Pérez-Stable, Eliseo J

    2010-04-01

    The purpose of this study was to identify Andean youth's beliefs regarding ceremonial tobacco use and to discuss potential applications of findings in tobacco control interventions. The study was conducted in the Province of Jujuy, Argentina among 202 boys and girls, 10 to 20 years of age, living in rural and urban areas. The world of beliefs and meanings became accessible by asking youth to focus on tangible experiences regarding the Pachamama ceremony, a ritual honoring Mother Earth. Concepts such as reciprocity, the unity of material and spiritual realms, and the complementary nature of opposite forces were linked to beliefs about ceremonial tobacco use. Three domains for understanding smoking behaviour beliefs and norms were identified including mechanisms of production, conceptual tenants and behavioural expressions. These findings suggest that tobacco control interventions based on solidarity, reciprocity, and non-rational ways of learning are more culturally appropriate for native populations in the Andes than the current individual behaviour change models and have the potential applications with other indigenous populations. The research methods also have the potential for generalized application in cross-cultural studies of health behaviours in understudied populations in middle and low-income countries.

  5. Zeolitización de rocas andesíticas

    Directory of Open Access Journals (Sweden)

    Plana, F.

    1989-12-01

    Full Text Available The study of some andesites from King George Island (South Shetland Islands, Anctartica has pointed out the existence of a hydrothermal alteration process going rise to a zeolitic secondary minerals of low-temperature assemblages. Two paragenesis have been identified (Smectite-Bytownite-Mordenite, Smectite-Albite-Laumontite which reflecting different conditions durign the hydrothermal alteration of these andesitic rocksEl estudio de rocas andesíticas de la Isla King George (Archipiélago de las Shetland del Sur, Antártida pone de manifiesto la existencia de procesos de alteración hidrotermal con la formación de minerales zeolíticos secundarios pertenecientes a asociaciones de baja temperatura. Se han identificado dos paragénesis (Esmectitas-Bytownita-Mordenita, Esmectitas-AlbitaLaumontita que reflejan distintas condiciones durante la alteración hidrotermal de dichas rocas andesíticas.

  6. Glacier shrinkage and water resources in the Andes

    Science.gov (United States)

    Francou, Bernard; Coudrain, Anne

    For more than a century glaciers around the world have been melting as air temperatures rise due to a combination of natural processes and human activity. The disappearance of these glaciers can have wide-ranging effects, such as the creation of new natural hazards or changes in stream flow that could threaten water suppliesSome of the most dramatic melting has occurred in the Andes mountain range in South America. To highlight the climatic and glacial change in the Andes and to encourage the scientific community to strengthen the glacier observation network that stretches from Colombia to the Patagonian ice fields, the Instituto Nacional de Recursos Naturales (INRENA), Perú, and the Institute of Research and Development (IRD), France, recently organized the second Symposium on Mass Balance of Andean Glaciers in Huaráz,Perú.

  7. Migrating deformation in the Central Andes from enhanced orographic rainfall

    Science.gov (United States)

    Norton, Kevin; Schlunegger, Fritz

    2011-12-01

    Active shortening in the Central Andes shifted from the western to the eastern margin between 10-7Ma. Here we propose that this shift was primarily controlled by changes in erosion patterns. The uplift of the Andes blocked easterly winds, resulting in enhanced orographic rainfall on the eastern margin and reduced rainfall on the western margin. Lower erosion rates, associated with the arid conditions, caused the western margin to steepen inhibiting internal deformation and the migration of deformation to the eastern margin where it is active today. River channel profiles on the western margin are indicative of long-term transience from an older tectonic event whereas those on the eastern margin reflect ongoing coupled climatic-tectonic feedback. Both critical wedge theory and local-scale fault friction calculations support this interpretation. This work emphasizes the role that orographic rainfall and erosion can have on the orogen-scale development of mountain belts.

  8. Controles estatales a la industria del vino en Mendoza, 1890-1914

    Directory of Open Access Journals (Sweden)

    PATRICIA BARRIO DE VILLANUEVA

    2013-05-01

    Full Text Available El artículo estudia los controles del Estado nacional y provincial a la agroindustria mendocina del vino entre la década de 1890 y 1914. En este período se detectan dos momentos. En el primero, entre 1890 y 1904, se analiza el mercado de vinos y cómo el Estado nacional utilizó los impuestos (aduaneros e internos para proteger a la naciente industria. También se reconstruye la legislación nacional y provincial que reguló la producción, la comercialización y el cobro de los impuestos al vino; y los mecanismos utilizados por ambas jurisdicciones para el cumplimiento de dichas leyes. En el segundo, se examinan los cambios ocurridos en la vitivinicultura durante los años de auge, entre 1904 y 1912, cuando los Estados provincial y nacional desplegaron estrictas normativas para evitar el fraude vínico y el pago del impuesto; y las primeras medidas tomadas con la llegada de una nueva crisis, entre 1913 y 1914. Abstract The article examines the controls of the national and provincial state to agribusiness Mendoza wine between the 1890 and 1914. In this period two points are detected. In the first, between 1890 and 1904, analyzes the wine market and how the national government used taxes (customs and internal to protect the nascent industry. Also reconstructs the national and provincial legislation that regulates the production, marketing and collection of taxes on wine, and the mechanisms used by both jurisdictions to comply with such laws. The second examines changes in the wine industry during the boom years between 1904 and 1912, when provincial and national States deployed strict standards to prevent wine fraud and tax payments, and the first steps taken with the arrival of a new crisis between 1913 and 1914.

  9. Above-ground wineries and interior thermal stability: traditional and contemporary envelope analysis in Mendoza, Argentina

    Directory of Open Access Journals (Sweden)

    Carolina Ganem Karlen

    2013-06-01

    Full Text Available El control en el intercambio de flujos energéticos interior-exterior y la inercia térmica de los materiales constructivos son características claves de la envolvente de los edificios de bodegas. Esta situación es particularmente importante en el caso de los edificios construidos sobresuelo en climas con temperaturas diarias y estacionales muy variables. En el caso de que la arquitectura no provea la respuesta adecuada, indefectiblemente se recurre al consumo de energía auxiliar. La bodega S.A., ubicada en Mendoza, Argentina, consume energía auxiliar equivalente a 2.500 kW por año. Dicha bodega sobresuelo presenta dos tipos de envolvente vertical: una tradicional en adobe (λ = 0.81W/mK y otra contemporánea en chapa galvanizada sin aislación (λ = 45 W/mK. El objetivo de este trabajo es analizar los aspectos de materialidad, inercia térmica e intercambio de flujos energéticos de envolventes tradicionales y contemporáneas y, comparar los resultados obtenidos con un caso teórico de bodega subterránea. Entre los resultados obtenidos se observa que la envolvente tradicional mantiene las temperaturas interiores entre 8,5 ºC y 10 ºC por debajo de las temperaturas exteriores, mientras que los nuevos espacios con envolventes contemporáneas lo hacen solamente 3 ºC a 5 ºC por debajo de las temperaturas exteriores. En el caso de una bodega subterránea, las temperaturas estarían estables durante el año en 16,5 ºC; esto es, en verano, 20 ºC por debajo de las temperaturas exteriores.

  10. La doctrina sobre el poder del príncipe en Alfonso Hojeda de Mendoza

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    Salustiano de DIOS

    2009-12-01

    Full Text Available RESUMEN: Alfonso Hojeda fue un notable canonista sevillano que en 1576 publicó en Venecia un libro acerca de los beneficios eclesiásticos. La obra se divide en dos partes: la primera está dedicada a argumentar en contra de la pluralidad de beneficios en una misma persona, de acuerdo con los decretos tridentinos de reforma, mientras la segunda trata en cambio de la compatibilidad de beneficios mediante dispensa papal. Los propios términos en que se manifiestan las dos partes ya están indicando las contradicciones en que ha de moverse el autor, difíciles de salvar. La doctrina de la causa es, además de la distinción entre órdenes normativos, la principal herramienta conciliatoria para Hojeda. El papa está desligado del derecho positivo o humano, pues de otro modo no podría dispensar, o privilegiar, mas sólo puede hacerlo con justa causa.ABSTRACT: Alfonso Hojeda de Mendoza was an outstanding canonist that in 1576 published a book in Venice on the eclesiástica benefits. The book is divided into two parts: the first one is devoted to argue against the plurality of benefits in the same person, according to Trento's decrees, while the second one deals, however, with the compatibility of benefits by the Pope's dispense. The own terms in which both parts are expressed reveal the contradictions, in which the author must move, always difficult to avoid. The doctrine of the cause, as well as the distinction among normative orders, is the main conciliatory tool for Hojeda. The Pope is unlinked to human or positive right, otherwise he could not dispense or privilege, however he can only do it for a just cause.

  11. Relaciones biológicas entre las poblaciones tardías del sur de Mendoza

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    Barrientos, Gustavo

    2005-01-01

    Full Text Available En el presente, se encuentra en desarrollo un proyecto orientado a analizar la dinámica evolutiva de las poblaciones humanas de la porción central de Argentina y de Patagonia Continental durante el Holoceno, mediante la integración de diferentes líneas de evidencia morfológica (i.e. rasgos de variación continua y discontinua a nivel craneofacial, dental y postcraneal. El objetivo de este trabajo es presentar resultados parciales de esta investigación, obtenidos a partir del análisis del esqueleto craneofacial (morfometría geométrica y de piezas dentales permanentes (morfometría tradicional de 50 individuos adultos de ambos sexos, procedentes de sitios arqueológicos del Sur de Mendoza asignables a diferentes momentos del Holoceno tardío. Se registraron coordenadas de landmarks y semilandmarks sobre el esqueleto craneofacial en norma frontal y basilar y se relevaron los diámetros mesiodistal y bucolingual a nivel del cuello dental. Estas variables fueron empleadas en análisis de componentes principales. Los resultados obtenidos indican que, a nivel dental, se observó una diferenciación entre las muestras del Holoceno tardío inicial y final, caracterizándose las primeras por presentar mayores tamaños dentales. A nivel craneofacial también se observaron diferencias temporales, aunque con un patrón diferencial entre y dentro de cada sexo.

  12. Crustal-thickness variations in the central Andes

    Science.gov (United States)

    Beck, Susan L.; Zandt, George; Myers, Stephen C.; Wallace, Terry C.; Silver, Paul G.; Drake, Lawrence

    1996-05-01

    We estimated the crustal thickness along an east-west transect across the Andes at lat 20°S and along a north-south transect along the eastern edge of the Altiplano from data recorded on two arrays of portable broadband seismic stations (BANJO and SEDA). Waveforms of deep regional events in the downgoing Nazca slab and teleseismic earthquakes were processed to isolate the P-to-S converted phases from the Moho in order to compute the crustal thickness. We found crustal-thickness variations of nearly 40 km across the Andes. Maximum crustal thicknesses of 70 74 km under the Western Cordillera and the Eastern Cordillera thin to 32 38 km 200 km east of the Andes in the Chaco Plain. The central Altiplano at 20°S has crustal thicknesses of 60 to 65 km. The crust also appears to thicken from north (16°S, 55 60 km) to south (20°S, 70 74 km) along the Eastern Cordillera. The Subandean zone crust has intermediate thicknesses of 43 to 47 km. Crustal-thickness predictions for the Andes based on Airy-type isostatic behavior show remarkable overall correlation with observed crustal thickness in the regions of high elevation. In contrast, at the boundary between the Eastern Cordillera and the Subandean zone and in the Chaco Plain, the crust is thinner than predicted, suggesting that the crust in these regions is supported in part by the flexural rigidity of a strong lithosphere. With additional constraints, we conclude that the observation of Airy-type isostasy is consistent with thickening associated with compressional shortening of a weak lithosphere squeezed between the stronger lithosphere of the subducting Nazca plate and the cratonic lithosphere of the Brazilian craton.

  13. Paleoatimetry of southern Tibet and the central Andes

    Science.gov (United States)

    Quade, J.; Dettinger, M. P.; DeCelles, P. G.; Leary, R.; Kapp, P. A.

    2011-12-01

    Here we explore a variety of isotopic systems to reconstruct paleoatitude in southern Tibet and the central Andes. A multi-system approach is essential since the necessary mineral archives are not always available, and because diagenetic resetting of some systems clearly occurs. In the central Andes at ~24°S, carbonate is rare due to hyperaridity, and where present, evaporation in soils and lakes completely alters the primary meteoric signal. Waters of hydration of volcanic glass are a much more promising target in this region given the prevalence of volcanic tuffs. We have analyzed the δD value of a suite of modern and ancient glasses back to 34 Ma that show little change in elevation in the western Cordillera of the Andes. By contrast, the eastern Cordillera of the Andes rose in the last 15 Ma. This pattern is consistent with gradual eastward propagation of the whole orogen at this latitude, including the trench, forearc, magmatic arc, and foreland. The paleoaltimetry of Tibet poses quite different challenges to those in South America. Volcanic glass archives are so far unavailable, whereas carbonate archives are common but in some cases diagenetically reset. We have focused on records of conventional δ18O values and clumped isotope thermometry. One must treat both archives with great caution due to resetting, especially clumped isotopes. Available evidence suggests that southern Tibet has been near current elevations since the early Miocene. For the pre- Miocene we present new isotopic/paleosol records found along the suture zone of India and Asia that we believe partly chronicle the rise of the suture zone from near sea-level to >4000 m today.

  14. Diversification of clearwing butterflies with the rise of the Andes

    OpenAIRE

    De‐Silva, Donna Lisa; Elias, Marianne; Willmott, Keith; Mallet, James; Day, Julia J.

    2015-01-01

    Abstract Aim Despite the greatest butterfly diversity on Earth occurring in the Neotropical Andes and Amazonia, there is still keen debate about the origins of this exceptional biota. A densely sampled calibrated phylogeny for a widespread butterfly subtribe, Oleriina (Nymphalidae: Ithomiini) was used to estimate the origin, colonization history and diversification of this species‐rich group. Location Neotropics. Methods Ancestral elevation and biogeographical ranges were reconstructed using ...

  15. Diversification of clearwing butterflies with the rise of the Andes

    OpenAIRE

    De‐Silva, Donna Lisa; Elias, Marianne; Willmott, Keith; Mallet, James; Day, Julia J.

    2015-01-01

    Abstract Aim Despite the greatest butterfly diversity on Earth occurring in the Neotropical Andes and Amazonia, there is still keen debate about the origins of this exceptional biota. A densely sampled calibrated phylogeny for a widespread butterfly subtribe, Oleriina (Nymphalidae: Ithomiini) was used to estimate the origin, colonization history and diversification of this species‐rich group. Location Neotropics. Methods: Ancestral elevation and biogeographical ranges were reconstructed using...

  16. Permafrost Distribution Modeling in the Semi-Arid Chilean Andes

    OpenAIRE

    Azócar, Guillermo F.; Brenning, Alexander; Bodin, Xavier

    2016-01-01

    Mountain permafrost and rock glaciers in the dry Andes are of growing interest due to the increase in human activities in this remote area. Empirical models of mountain permafrost distribution based on the spatial analysis of intact and relict rock glaciers and mean annual air temperature (MAAT) have been established as a tool for regional-scale assessments of permafrost favorability across entire mountain ranges; however, this kind of model approach has never been applied for a large portion...

  17. Lights and shadows of sustainable development and combat against desertification: economic rationalities in the eye of the storm. Case study involving goat producers in drylands (Mendoza, Argentina Claroscuros del desarrollo sustentable y la lucha contra la desertificación: las racionalidades económicas en el ojo de la tormenta: Estudio de caso con productores caprinos de tierras secas [Mendoza, Argentina

    Directory of Open Access Journals (Sweden)

    Laura Torres

    2010-01-01

    Full Text Available This work analyses the conflict situation present in the province's drylands between goat producers and programmes to combat desertification regarding production practices and the use producers make of natural resources. The case study tackled comprises the north-eastern extreme of Mendoza province. The , which is the hyperarid spot of the region, severely affected by desertification processes, covering an extent of 10,007 km2, and with 3015 inhabitants, where small goat breeding farms predominate. Previous studies indicate that the major causes of desertification in the area are logging of the native woodland and overgrazing which have led to improper livestock production practices. In response to this, the actions to combat desertification commonly point out the need to "raise awareness" and "build capacities" of the producers by initiating processes of change in the production systems. The proposals insist that, if the current level of pressure on resources is maintained, the already serious poverty conditions will grow worse in the future. Nevertheless, despite the efforts and funds invested, the producers seem to stubbornly persist in their present production strategies and in the dynamics of natural resource use derived from them. How to explain their refusal to consider other production options likely to result in higher profit and better environmental balance? How to explain that they act, at least apparently, against their own benefits? Against the explanations that place the producers' "culture" is the most important problem, the present work seeks to cooperate in clarifying these questions through an analysis of the different rationalities that, held by different actors, converge in the area. By using a mixed methodology, the paper analyse three dimensions: 1- The environmental resource supply, which is the basis of production activities, 2- The income attained by goat production units, and 3- The expenditures they face in terms of

  18. GasAndes pipeline construction moves to Chilean side

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1996-11-18

    Construction of Gasoducto GasAndes, the 287 mile, 24-in. gas pipeline from La Mora, Argentina, to Santiago, Chile, is well along in advance of its mid-1997 start-up target. By mid-September, all 194 miles of pipe in Argentina had been welded, lowered, and back filled, according to project manager NOVA Gas International Ltd., Calgary. On the Chilean side of the project at the end of September, 38% of the 93 miles of pipeline was complete. By October, crews had completed 28 of the 40 water crossings, including 8 of the 9 difficult crossings of the River Maipo. More than 70 miles of right-of-way have been graded, 35 miles ditched, 26 miles of pipe welded, and 17 miles lowered and backfilled. NOVA Gas International said construction is being carried out in areas with inclines as steep as 30--40{degree}. Approximately 600 people are working on the Chilean section of GasAndes. Meanwhile, engineers are working to complete route selection for the 68-mile GasAndes extension to Quillota in Region 5, 19 miles from Chile`s Pacific coast near Valparaiso.

  19. Novedosos registros de aves exhumadas del sitio arqueológico Laguna El Sosneado (LS-3 para el Holoceno tardío en el sur de Mendoza: aspectos tafonómicos NEW RECORDS OF BIRDS RECOVERED FROM THE LATE HOLOCENE ARCHAEOLOGICAL SITE LAGUNA EL SOSNEADO (LS-3, SOUTHERN MENDOZA: TAPHONOMIC ASPECTS

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    Fernando Julián Fernández

    2009-12-01

    Full Text Available Los aspectos tafonómicos vinculados con los restos de avifauna en contextos arqueológicos no han sido documentados para el área bajo estudio, hasta el presente. Los principales objetivos de este trabajo son efectuar una caracterización taxonómica cualitativa y cuantitativa de una muestra de aves, principalmente Passeriformes, proveniente de sedimentos holocénicos del sur de la provincia de Mendoza y elaborar un estudio sobre los procesos tafonómicos que intervinieron en el contexto arqueofaunístico. La muestra arqueofaunística fue comparada con muestras de egagrópilas actuales, a los fines de establecer el proceso de acumulación de los agregados óseos. El principal agente responsable de la acumulación habría sido un ave Strigiformes, posiblemente Tyto alba. Los agentes y procesos postdepositacionales que tuvieron mayor incidencia en la formación del agregado arqueofaunístico fueron el pisoteo, la acción corrosiva de las raíces y los efectos de la humedad del suelo, que habrían contribuido a destruir con mayor rapidez los elementos óseos. Es importante resaltar la baja representación de Passeriformes en los contextos arqueofaunísticos, debido, en gran medida, a sus características osteológicas. Según las características ecológicas de los taxones recuperados, los cuales se distribuyen actualmente en el área, podemos concluir que la zona donde se encuentra el sitio representa un área ecotonal, conformada hacia el Holoceno tardío.Until now, no record of the taphonomic aspects of bird remains in an archaeological context had been documented for the study area. The main goals of this paper are to conduct the qualitative and quantitative taxonomical characterization of a sample of birds, mainly Passeriformes, from Holocene sediments of southern Mendoza Province, and to study the intervening taphonomic processes in an archaeofaunal context. The archaeofaunistic sample was compared to modern owl pellet samples in order to

  20. Caracterización de rocas ultramáficas, máficas y metasedimentarias del cordón del Peñasco, Precordillera Occidental, Mendoza Characterization of ultramafic, mafic and metasedimentary rocks of the Cordón del Peñasco, western Precordillera, Mendoza

    Directory of Open Access Journals (Sweden)

    Florencia L Boedo

    2012-06-01

    Full Text Available En el cordón del Peñasco, ubicado en el sector norte de la provincia de Mendoza, dentro del ámbito de la Precordillera Occidental, aforan metasedimentitas en contacto tectónico con una asociación máfica-ultramáfica. Dentro de las metasedimentitas en facies esquistos verdes se han reconocido dos asociaciones: metalimolitas carbonáticas y metaareniscas y metapelitas. Las rocas máficas-ultramáficas están representadas por serpentinitas derivadas de harzburgitas y dunitas, gabros bandeados metamorfizados en facies granulita; diabasas constituyendo diques o filones capa, metabasaltos amigdaloides y metahialoclastitas con bajo grado de metamorfismo. Se realizaron estimaciones termométricas en una granulita máfica (gabro bandeado utilizando el par granate-clinopiroxeno, obteniéndose temperaturas de 884°C. Las mismas permiten estimar que estos cuerpos experimentaron metamorfismo de alta temperatura, para posteriormente retrogradar a facies esquistos verdes, sobre la base de aspectos mineralógicos y texturales. Con respecto a las unidades metasedimentarias, el paleoambiente inferido para la unidad de metaareniscas y metapelitas corresponde a pie de talud continental con predominio de sedimentación gravitacional sobre la base de estructuras sedimentarias reconocidas. Mientras que la unidad de metalimolitas carbonáticas pertenecerían a un ambiente marino profundo. Estas unidades han sido asignadas al Eopaleozoico a partir de criterios estratigráficos y deformadas y metamorfizadas hacia fines del Devónico como consecuencia de la orogenia Chánica.In Cordón del Peñasco area, located in northern Mendoza province, western Precordillera, metasedimentites are in tectonic contact with a mafic-ultramafic association. The former have been under greenschist facies metamorphism and two associations have been recognized: carbonate metasiltstones and metasandstones and metapelites. The mafic-ultramafic association is represented by serpentinized

  1. Review of Arciaga, Juárez y Mendoza (Coords. (2013. Introducción a la Psicología Social

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    Ali Lara

    2014-11-01

    Full Text Available Reseña del libro: Salvador Arciaga Bernal, Juana Juárez Romero y Jorge Mendoza Garcia  (coord. (2013. Introducción a la Psicología Social. México: UAM-MAPorrúa. ISBN 978-607-28-0109-7

  2. The impact of different cooling strategies on urban air temperatures: the cases of Campinas, Brazil and Mendoza, Argentina

    Science.gov (United States)

    Alchapar, Noelia Liliana; Cotrim Pezzuto, Claudia; Correa, Erica Norma; Chebel Labaki, Lucila

    2016-07-01

    This paper describes different ways of reducing urban air temperature and their results in two cities: Campinas, Brazil—a warm temperate climate with a dry winter and hot summer (Cwa), and Mendoza, Argentina—a desert climate with cold steppe (BWk). A high-resolution microclimate modeling system—ENVI-met 3.1—was used to evaluate the thermal performance of an urban canyon in each city. A total of 18 scenarios were simulated including changes in the surface albedo, vegetation percentage, and the H/W aspect ratio of the urban canyons. These results revealed the same trend in behavior for each of the combinations of strategies evaluated in both cities. Nevertheless, these strategies produce a greater temperature reduction in the warm temperate climate (Cwa). Increasing the vegetation percentage reduces air temperatures and mean radiant temperatures in all scenarios. In addition, there is a greater decrease of urban temperature with the vegetation increase when the H/W aspect ratio is lower. Also, applying low albedo on vertical surfaces and high albedo on horizontal surfaces is successful in reducing air temperatures without raising the mean radiant temperature. The best combination of strategies—60 % of vegetation, low albedos on walls and high albedos on pavements and roofs, and 1.5 H/W—could reduce air temperatures up to 6.4 °C in Campinas and 3.5 °C in Mendoza.

  3. Minerales de mena del depósito epitermal de baja sulfuración Don Sixto, Mendoza

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    Ana Cecilia Mugas Lobos

    2012-03-01

    Full Text Available El proyecto minero Don Sixto es un depósito epitermal de baja sulfuración de Au-Ag, ubicado en el bloque de San Rafael, en el SE de la provincia de Mendoza. En este depósito, cuyo recurso aurífero es próximo a las 900.000 onzas, se ha identificado una asociación de minerales de metales preciosos que incluye: uytenbogaardtita, stromeyerita, naumannita, acantita, polibasita, stützita y cervelleita. Estos minerales son escasos y se encuentran frecuentemente asociados a oro y plata de variable fineza, diseminados en vetas de cuarzo hidrotermal y en unidades volcánicas-piroclásticas de los Grupos Choiyoi y El Portillo. En este depósito se encuentra abundante pirita, con cantidades menores de arsenopirita, calcopirita, esfalerita, magnetita, hematita y, en forma subordinada, pirrotina, galena, marcasita, bornita y boulangerita, junto con calcosina, digenita y covellina. La presencia de uytenbogaardtita, stützita, cervelleita y polibasita constituye la primera mención de estos minerales para la provincia de Mendoza.

  4. La obra lexicográfica de Manuel Hurtado de Mendoza: sus diccionarios enciclopédicos de medicina

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    Gutiérrez Rodilla, Bertha M.

    2012-12-01

    Full Text Available The figure of Manuel Hurtado de Mendoza has been sufficiently analyzed in connection with his contributions to Spanish anatomy during the first half of the 19th century or to the introduction of some European innovations in Spain. However, there is still much of his work to be studied, such as the medical dictionaries he wrote, two encyclopedic and one terminological. We deal with the first two in this essay, where we will speak highly of his significance in an age in which specialized lexicography took off in Europe, while it did not reach but a timid development in Spain.

    La figura de Manuel Hurtado de Mendoza ya se ha analizado suficientemente en relación con sus aportaciones a la anatomía española de la primera mitad del siglo XIX o a la introducción en España de algunas novedades europeas. Sin embargo, todavía queda por estudiar buena parte de su obra, como ocurre con los diccionarios de medicina que compuso, dos enciclopédicos y uno terminológico. De los dos primeros nos ocupamos en este trabajo, en el que ponderaremos su importancia en un siglo en que la lexicografía especializada despegó en Europa, mientras que en España no alcanzó más que un tímido desarrollo.

  5. A review of the geology of the Argentinian Fuegian Andes

    Science.gov (United States)

    Olivero, Eduardo B.; Martinioni, Daniel R.

    2001-06-01

    Seven stratigraphic units reflect the tectonic evolution of the Argentinian Fuegian Andes: Basement (Paleozoic-Jurassic); Lemaire Formation (Upper Jurassic); Yahgan-Beauvoir formations (Lower Cretaceous); Cerro Matrero Formation (Upper Cretaceous); Rı´o Claro Formation (Paleocene); La Despedida Group (Eocene); and Cabo Peña Formation (uppermost Eocene-Lower Oligocene). Basement rocks (garnet, quartz-sericite, and chlorite schists; and amphibolites) are unconformably covered by the Lemaire Formation (rhyolites; basalts; slates; and acidic volcaniclastic breccias, tuffs, conglomerates, and turbidites), formed during extensional tectonism. The post-rift Yahgan Formation (deep-marine black mudstones, andesitic volcaniclastic turbidites and tuffs) interfingers northward with the Beauvoir Formation (slope and platform black mudstones), and covers the Lemaire Formation unconformably. The Yahgan Formation represents an andesitic, volcaniclastic apron, coeval with a Pacific volcanic-arc, filling a marginal basin floored with oceanic crust. The Late Cretaceous compressional orogeny resulted in tectonic inversion, closure of the marginal basin, peak metamorphism and folding, and initial uplifting of the Fuegian Andes. By the latest Cretaceous-earliest Paleogene, the Andes were exposed to subaerial erosion, and the lowest Danian Rı´o Claro Formation bears clear evidence of an Andean clastic provenance. The Rı´o Claro Formation represents the first molasse deposits of the foreland stage of evolution of the Fuegian Andes. Earliest Paleogene north-verging thrust propagation deformed the Rı´o Claro Formation and older units, producing northward depocenter migration. La Despedida Group rests unconformably on the Rı´o Claro Formation and is involved in the thrust and fold belt. Important Eocene compression resulted in thrusting of central Andean basement schists and the Lemaire Formation over Lower Cretaceous and continental Paleogene rocks, respectively. In the

  6. Las ignimbritas del complejo volcánico Coranzuli (Puna Argentina-Andes Centrales

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    Martí, J.

    1987-12-01

    Full Text Available The Coranzulí is a large Upper Miocene volcanic complex located on a NE-SW and NW-SE regional faults intersection, at 66º 15' W 23º S, in the Northwest of Argentina in Jujuy province. It corresponds to one of four large volcanic complexes which represent the end of Transversal Volcanic Chaines in La Puna Argentina in the Central Andes. The volcanic activity was characterized by at least four separate ignimbrite eruptions which produced four different ignimbrite sheets. These are well welded, very crystal-rich, lithie poor ignimbrites and have a moderate to high pumice content. The total volume of the Coranzuli ignimbrites exeededs 650 Km3. Preliminary data indicate that the eruption oeeurred from a homogeneous magmatic chamber without zoning. The emplacement characteristics of the ignimbrites and the lack of basal or interbedded plinian fall deposits suggest that the eruptions developed quickly to massive proportions.El Coranzuli es uno de los grandes complejos volcánicos que representan el remate final de las Cadenas Volcánicas Transversales de la Puna Argentina, en los Andes Centrales. Se trata de un complejo volcánico del Mioceno superior situado a los 66º 15' W 23º S en el NW de Argentina en la provincia de Jujuy, en la intersección entre dos fallas regionales de dirección NE-SW y NW-SE, respectivamente. La actividad eruptiva se caracterizó por la existencia de, al menos, cuatro erupciones ignimbríticas que produjeron cuatro diferentes mantos ignimbríticos. Se trata de ignimbritas bien soldadas, muy ricas en cristales, pobre en fragmentos líticos y que presentan un contenido en fragmentos pumíticos de moderado a alto. El volumen total que representan estas ignimbritas supera los 650 km3. Los datos preliminares indican que el magma juvenil deriva de una cámara magmática homogénea no zonada. Las características de emplazamiento de estas ignimbritas, así como la falta de depósitos plinianos de caída en la base o

  7. Eduardo Pérez Romagnoli; Los Guardianes de Baco. Artesanos toneleros e industrias de recipientes de vino en Mendoza y San Juan, Argentina (1885-1930, Rosario, Prohistoria ediciones, 2008

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    ANDRÉS CARMINATI

    2013-05-01

    Full Text Available Eduardo Pérez Romagnoli; Los Guardianes de Baco. Artesanos toneleros e industrias de recipientes de vino en Mendoza y San Juan, Argentina (1885-1930, Rosario, Prohistoria ediciones, 2008

  8. Los Mares Interiores. (Libro de Poemas del Académico Juan Mendoza Vega

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    Efraim Otero Ruiz

    2001-12-01

    Full Text Available

    (Presentación del libro en la Fundación Santillana para Iberoamérica, Bogotá, Noviembre 23, 2001.

    Ha querido la deferencia del señor  exPresidente Belisario Betancur, Presidente de la Fundación Santillana para lberoamérica, que sea yo quien les presente el libro "Los mares interiores" del médico, periodista y poeta Juan Mendoza Vega. Tarea que acometo con singular afecto, nacido de una amistad que supera ya los 40 años y de una admiración continua por las dotes intelectuales y artísticas que lo colocan en un sitial especial entre los médicos de Colombia.

    Nacido en Chinácota y bachiller en Pamplona, su infancia y adolescencia transcurrieron en esos paisajes idílicos que se extienden entre el río Pamplonita y las colinas de Iscalá, donde ha trasegado la vida de muchos hijos ilustres del Norte de Santander. Después cursó sus estudios de Medicina en la Universidad
    Nacional, en Bogotá, entre 1952 y 1957, habiéndose graduado de médico en 1960 a los dos años de haber iniciado su especialización en neurología y neurocirugía, temas que constituirían la mayor dedicación de su vida. Pues de ahí saltó a la cátedra de la especialidad en la Facultad de Medicina del Rosario entre 1969 y 1985, siendo además iniciador de la cátedra y profesor de Historia de la Medicina en la misma Universidad desde 1980 hasta el presente; al tiempo, ha sido profesor de Etica Médica allí mismo desde 1983. A estas actividades de planta ha unido su participación como catedrático invitado en numerosas instituciones y universidades de dentro y fuera del país. Y la autoría de 55 publicaciones científicas en revistas nacionales e internacionales sobre temas de neurología y neurocirugía, ética médica e historia de la medicina...


  9. Geochemical composition of river loads in the Tropical Andes: first insights from the Ecuadorian Andes

    Science.gov (United States)

    Tenorio Poma, Gustavo; Govers, Gerard; Vanacker, Veerle; Bouillon, Steven; Álvarez, Lenín; Zhiminaicela, Santiago

    2015-04-01

    Processes governing the transport of total suspended material (TSM), total dissolved solids (TDS) and particulate organic carbon (POC) are currently not well known for Tropical Andean river systems. We analyzed the geochemical behavior and the budgets of the particulate and dissolved loads for several sub-catchments in the Paute River basin in the southern Ecuadorian Andes, and examined how anthropogenic activities influenced the dynamics of riverine suspended and dissolved loads. We gathered a large dataset by regularly sampling 8 rivers for their TSM, POC, and TDS. Furthermore, we determined the major elements in the dissolved load and stable isotope composition (δ13C) of both the POC, and the dissolved inorganic carbon (DIC). The rivers that were sampled flow through a wide range of land uses including: 3 nature conservation areas (100 - 300 Km²), an intensive grassland and arable zone (142 Km²); downstream of two cities (1611 and 443 Km²), and 2 degraded basins (286 and 2492 Km²). We described the geochemical characteristics of the river loads both qualitatively and quantitatively. Important differences in TSM, POC and TDS yields were found between rivers: the concentration of these loads increases according with human activities within the basins. For all rivers, TSM, TDS and POC concentrations were dependent on discharge. Overall, a clear relation between TSM and POC (r²=0.62) was observed in all tributaries. The C:N ratios and δ13CPOC suggest that the POC in most rivers is mainly derived from soil organic matter eroded from soils dominated by C3 vegetation (δ13CPOC < -22‰). Low Ca:Si ratios (<1)and high δ13CDIC (-9 to -4) in the Yanuncay, Tomebamba1 and Machángara, rivers suggest that weathering of silica rocks is dominant in these catchments, and that the DIC is mainly derived from the soil or atmospheric CO2. In contrast, the Ca:Si ratio was high for the Burgay and Jadán rivers (1-13), and the low δ13CDIC values (-9 to -15) suggest that

  10. Evolución del potencial atlético en la provincia de Mendoza (Argentina durante los años 1973 - 2001 = The evolution of athletic potential in the province of Mendoza from 1973 to 2001

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    Ana María Destefanis

    2013-03-01

    Full Text Available Estudio exploratorio descriptivo con diseño no experimental, longitudinal, retrospectivo que analiza los cambios producidos en el potencial atlético mendocino desde 1973 hasta 2001. Los resultados obtenidos por la aplicación de la prueba estadística “t” student, significativamente inferiores entre la media del potencial atlético entre el 2000-2001, respecto de la década del 80 (prueba “t” 80/00 = 0,0423. No sucedió lo mismo al compararlos con las décadas del 70 y 90 que registraron entre sí valores similares en sus rendimientos atléticos (“t” 70/00 = 0,3995 y “t” 90/00 = 0,2013. Se concluyó que la diferencia significativa en el rendimiento atlético provincial se produjo al comparar la década del 80 con los años 2000 y 2001. Por lo tanto se rechazó la Hi y se aceptó la H alternativa. Se midieron las variables que influyeron sobre la evolución de este potencial, concluyendo que su disminución tiene relación con el estado que presentan las pistas en uso, insuficientes elementos atléticos, escasa cantidad de profesores especialistas, déficit en la administración de recursos físicos y humanos de los responsables del atletismo federado y falta de proyectos que canalicen la cantidad de jóvenes que compiten en instancias escolares y no ingresan al circuito federado.-------------------------------------------------------------------------Descriptive exploratory study with non experimental longitudinal retrospective design that analyzes the changes in the athletic potential of Mendoza’s population from 1973 to 2001. The results obtained by the application of the "t" student statistic test are significantly lower for the average athletic potential between 2000 and 2001, compared with the decade of the 80s (t-test 80/00 = 0.0423. It was not the same when compared to the decades of 1970 and 1990, which showed similar values to each other in their athletic performance ("t" 70/00 = 0.3995 and t = 0.2013 90/00. The conclusion was that the significant difference in provincial athletic performance was obtained when comparing the decade of the 80s with the years 2000 and 2001. Thus, the Hi was rejected and the alternative H was accepted. The variables that influenced the evolution of this potential were measured, concluding that its decline is related to the state of the tracks in use, insufficient athletic items, lack of specialist teachers, a deficit in the administration of physical and human resources by those responsible for the athletics federation and a lack of projects to channel the number of young people competing at school level that fail to enter the federate circuit.

  11. El sistema lacustre de la Formación Mollar en el depocentro triásico de Santa Clara (provincia de Mendoza, Argentina The lacustrine system of the Mollar Formation in the Triassic Santa Clara Depocenter (Mendoza Province, Argentina

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    Luis A Spalletti

    2009-07-01

    Full Text Available El depocentro triásico de Santa Clara, Cuenca Cuyana, se caracteriza por espesos depósitos generados en ambiente lacustre. Uno de ellos, con un registro de más de 345 m, corresponde a la Formación Mollar. El tramo inferior a medio está caracterizado por una monótona sucesión de lutitas bituminosas acumuladas por decantación suspensiva en el 'off shore' anóxico de un cuerpo lacustre hidrológicamente cerrado y que muestra alto contenido de materia orgánica amorfa de origen algal y de restos de plantas terrestres muy degradadas junto a sulfuros de hierro autígenos. Intercalan areniscas finas debidas a corrientes de turbidez diluidas y carbonatas estromatolíticos. En esta sucesión se definen ciclos granocrecientes de pequeña escala (PACs que se atribuyen a episodios de expansión-retracción lacustre controlados por cambios climáticos. Asociaciones de facies heterolíticas representan los depósitos de la transición entre los ambientes de 'nearshore' y 'offshore' lacustre. La sección superior de la Formación Mollar se compone de sucesiones pelíticas con profusa bioturbación que sugieren mayor oxigenación del sustrato y se asignan a ambiente de costa afuera de un sistema lacustre holomíctico hidrológicamente abierto. Intercalan areniscas producto de flujos hiperpicnales. Depósitos de areniscas con abundantes trazas fósiles y estructuras de olas y flujos unidireccionales, representan a sectores marginales del ambiente lacustre. Además de los ciclos de alta frecuencia, en la Formación Mollar se definen tres secuencias asimétricas de mayor escala atribuidas a episodios mayores de expansión-contracción lacustre debidos a la interacción entre factores climáticos y tectónicos. El diseño de superposición granocreciente de la Formación Mollar y la gradual transición a depósitos fluviales de la sobreyacente Formación Montaña refleja asimismo una constante reducción del espacio de acomodación sedimentaria en el depocentro de Santa Clara a medida que se produjo la acumulación de los depósitos estudiados.The Triassic Santa Clara depocenter, Cuyo Basin, is characterised by thick fine-grained deposits formed in lacustrine systems. One of them, represented by the Mollar Formation, exceeds the 345 m. The lower to middle section of this unit is dominated by a monotonous succession of black shales having a high content of amorphous organic matter produced by algae and highly degraded plant remains. These deposits were formed by suspensión fallout in the anoxic 'offshore' sector of a hydrologically closed lake. Thin and fine-grained turbiditic beds and stromatolitic carbonates are intercalated in the fine-grained succession. Small-scale coarsening-upward cycles (PACs are attributed to episodes of lake expansion-retraction driven by climate change. A facies association composed of an heterolithic package represents the deposits of the transition between 'nearshore' and 'offshore' settings. The upper section of the Mollar Formation essentially consists of bioturbated mudstones suggesting a greater oxygenation of the substrate. They are assigned to the 'offshore' environment of a holomictic hydrologically open lake system. Sporadic hyperpycnal flows are documented by intercalations of sandy turbidites. Bioturbated sandstone beds with primary structures indicative of both normal and storm wave action and unidirectional flows, represent the marginal deposits of the lacustrine system. In addition to the high-frequency cycles, three larger scale asymmetrical sequences are identified in the Mollar Formation. These sequences suggest episodes of major expansion-contraction of the lake system due to the interaction between climatic and tectonic factors. The overall shallowing up stacking pattern of the Mollar Formation and the gradual transition to fluvial deposits of the overlying Montaña Formation reflects a steady reduction of accommodation space in the Santa Clara depocenter during the accumulation of the studied succession.

  12. Neotectónica y sismicidad en el sector norte de la depresión de Tunuyán, provincia de Mendoza Neotectonic and seismicity in the northern portion of Tunuyán Depresion, Mendoza province

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    Laura Perucca

    2009-04-01

    Full Text Available El objetivo de este trabajo es analizar las fallas ubicadas en las lomas del Jaboncillo, del Peral y Sola del Diablo, en el extremo noroeste de la depresión de Tunuyán y su posible actividad tectónica durante el Pleistoceno tardío-Holoceno. En la loma Sola del Diablo (sector norte de las lomas del Peral se ubicaron dos fallas inversas con vergencia al este que sobreponen sedimentitas indiferenciadas del Neógeno sobre depósitos fanglomerádicos de la Formación Los Mesones (Pleistoceno inferior, Polanski 1963. En las lomas del Jaboncillo se identificaron tres escarpas de rumbo submeridianal que miran al oeste, la de mayor desarrollo se ubica al este y se denomina falla Chupasangral. No fue posible determinar la cinemática de estas fallas aunque se infiere un carácter inverso para las mismas. No se han podido reconocer rasgos de actividad neotectónica en la cubierta eólica mantiforme holocena (Formación El Zampal que circunda las lomadas analizadas. Las fallas observadas no afectarían a las unidades holocenas presentes en el área ni estarían asociadas con la sismicidad actual. Sin embargo, constituyen fuentes sismogénicas potenciales para la región mendocina.This paper is focused on a series of faults occurring in the NW Tunuyán depression (localities of Lomas del Jaboncillo, Loma del Peral, Loma Sola del Diablo and its possible tectonic activity during the late Pleistocene-Holocene. Two east verging reverse faults were found in Loma Sola del Diablo (northern sector of Lomas del Peral which caused the superposition of undifferentiated Neogene sediments on top of fanglomeradic deposits of Los Mesones Formation (lower Pleistocene, Polanski 1963. Three scarps of nearly NS trend that face west were identified at Lomas del Jaboncillo, the largest situated eastward being known as Chupasangral fault. The cinematic of these faults was inferred to be reverse. No neotectonic activity was identified in the Holocene eolian cover (El Zampal Formation which surrounds the studied elevations. The faults analyzed do not apparently affect the Holocene deposits and seem not to be related with present seismicity, although they constitute a potential seismogenic source for the studied area.

  13. Carbonatos subtropicales de la Formación Calabozo (Caloviano y su diagénesis, Cuenca Neuquina, Mendoza Subtropical carbonates from the Callovian Calabozo Formation, and their diagenesis, Neuquen Basin, Mendoza province

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    R.M. Palma

    2007-06-01

    Full Text Available El estudio de los carbonatos calovianos de la Formación Calabozo (30 m procedente del centro-oeste de Argentina revela la abundancia de partículas carbonáticas bentónicas producidas por organismos fotodependientes y de granos no-esqueletales tales como ooides y peloides. La biota está representada por bivalvos, dasicladáceas (Salpingoporella annulata Carozzi, Cylindroporella annulata Carozzi, y Heteroporella sp., corales escleractínidos, equinodermos, cianobacterias (Cayeuxia (Rivularia piae Rech-Frollo, y Cayeuxia (Rivularia kurdistanensis Elliot, oncoides, gastrópodos, foraminíferos, calciesferas y en menor cantidad, briozoos y ostrácodos. Las partículas aloquímicas sugieren para las calizas marinas someras de la Formación Calabozo una asociación Photozoan de aguas subtropicales. Las características petrográficas permitieron reconocer siete microfacies diferenciadas de acuerdo al tipo de partículas, fósiles y textura depositacional: 1 bindstone criptalgal; 2 wackestone bioclástico-peloidal; 3 wackestone bioclástico-intraclástico; 4 wackestone bioclástico-peloidal-terrígeno, 5 boundstone coralino, 6 packstone bioclástico-peloidal-intraclástico, y 7 packstone/grainstone oolítico-bioclástico-peloidal. El reconocimiento de grupos de microfacies constituyen dos asociaciones paleoambientales: rampa interna y rampa media. Los procesos de micritización y precipitación de micrita peloidal y cemento acicular son sinsedimentarios. Estos cementos son previos a la fase de cementación de calcita granular y sintaxial. Estudios de cátodoluminiscencia permitieron identificar tres tipos de cementos: (1 acicular, (2 calcita granular, y (3 cemento sintaxial en partículas de equinodermos. La cátodoluminiscencia permitió determinar cementos no luminiscente, cemento con luminiscencia opaca (roja/naranja y cemento con luminiscencia amarilla brillante. El cemento acicular es no luminiscente (marino, en tanto que la luminiscencia opaca a brillante típica de las cavidades inter-intraparticulares y del cemento sintaxial indica un ambiente diagenético meteórico-freático.Detailed study of Callovian carbonates of the Calabozo Formation (30 m in western Argentina, reveals the abundance of benthic carbonates particles produced by organisms that are light dependent, and non-skeletal grains such as ooids and peloids. The biota consists of bivalves, dasyclads (Salpingoporella annulata Carozzi, Cylindroporella annulata Carozzi, and Heteroporella sp., scleractinian corals, echinoderms, cyanobacteria (Cayeuxia (Rivularia piae Rech-Frollo, and Cayeuxia (Rivularia kurdistanensis Elliot, oncoids, gastropods, forams, and calcispheres as well as ostracods, and bryozoans in relatively minor quantities. Allochemical particles suggest for the shallow marine limestones of the Calabozo Formation a Photozoan Association under subtropical seawater conditions. The petrographic features allow to recognize seven microfacies, differentiated by particle types, fossils and depositional texture: 1 criptalgal bindstone; 2 bioclastic-peloidal wackestone; 3 bioclastic-intraclastic wackestone; 4 bioclastic-peloidal-terrigenous wackestone, 5 coral framestone, 6 peloidal-bioclastic-intraclastic packstone, and 7 oolitic-bioclastic-peloidal packstone-grainstone. The recognition of microfacies groups constitute two palaeoenvironmental associations: inner ramp and middle ramp settings. Diagenetic studies are based on examination of stained thin sections, through conventional petrography and under cathodoluminescence. Early diagenetic processes are micritization and precipitation of peloidal micrite and acicular calcite. These cements predate granular and syntaxial calcite cements. Cathodoluminescent petrography allows to identify three morphologic types of clear cements: (1 fine acicular crystals, (2 granular cements, and (3 syntaxial cement rims on echinoderm particles. Description of the CL signature has evolved to discrimination as either, non-luminescent, dully luminescent red/orange, or brightly luminescent yellow. The earlier acicular calcite cement is non-luminescent, on the other hand, the predominantly dully luminescent red/orange, or brightly luminescent yellow of interparticular and intraparticular granular calcite and syntaxial cements indicate a shallow burial meteoric-phreatic diagenetic environment.

  14. Is tourism damaging ecosystems in the Andes? Current knowledge and an agenda for future research.

    Science.gov (United States)

    Barros, Agustina; Monz, Christopher; Pickering, Catherine

    2015-03-01

    Despite the popularity of tourism and recreation in the Andes in South America and the regions conservation value, there is limited research on the ecological impacts of these types of anthropogenic use. Using a systematic quantitative literature review method, we found 47 recreation ecology studies from the Andes, 25 of which used an experimental design. Most of these were from the Southern Andes in Argentina (13 studies) or Chile (eight studies) with only four studies from the Northern Andes. These studies documented a range of impacts on vegetation, birds and mammals; including changes in plant species richness, composition and vegetation cover and the tolerance of wildlife of visitor use. There was little research on the impacts of visitors on soils and aquatic systems and for some ecoregions in the Andes. We identify research priorities across the region that will enhance management strategies to minimise visitor impacts in Andean ecosystems.

  15. PROFUNDIZACIÓN DEL TOPE DE PERMAFROST Y TENDENCIAS EN LA DINÁMICA CRIOGÉNICA, A PARTIR DE 1989, EN EL GLACIAR DE ESCOMBROS COMPUESTO DEL VALLE DE MORENAS COLORADAS, MENDOZA, ARGENTINA.

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    Darío Trombotto Liaudat

    2007-12-01

    Full Text Available Los glaciares de escombros (rockglaciers son las geoformas periglaciales con permafrost reptante más típicas e importantes, por su volumen en criosedimentos congelados y hielo, de los Andes Centrales. La presente contribución muestra ejemplos de la marcha de las temperaturas y la profundización del tope de permafrost en dos puntos de monitoreo (Balcón I y II del glaciar de escombros compuesto de Morenas Coloradas, Cordillera Frontal, en la provincia de Mendoza, Argentina. El engrosamiento de la capa activa en la lengua terminal, o límite inferior del creeping permafrost en este valle, de 4,9 m a 7,5 / 7,8 m en los últimos años, así como la tendencia de la dinámica criogénica desde 1992, y la geomorfología (termokarst inactivos en los frentes, expresan el fenómeno de calentamiento que se está detectando también en otros lugares del mundo. Estas variaciones térmicas sugieren cambios en la estructura interna de estas mesoformas. Asimismo, como otra situación geofísica paralela, el cálculo de difusividad térmica en Balcon II ( ̃ = 0.14 × 10-6 m2/s; Trombotto y Borzotta, 2007, a 3770 m de altura, permite correlacionar el bajo valor obtenido con una mejor y más larga conservación del hielo por debajo de los criorregolitos que son en este caso, principalmente, de origen volcánico. Los cambios térmicos detectados en esta zona piloto tendrían una consecuencia directa en el ambiente criogénico local y son un ejemplo para la situación regional del permafrost andino de los glaciares de escombros. Las variaciones descriptas se expresan a través de la profundización del tope de permafrost, formación de termokarst y reactivación de los más antiguos a lo largo del valle, y pérdida de movimiento, o de la criodinámica, en los taludes frontales (“narices” en la parte inferior y de menor altura de las geoformas investigadas. El trabajo promueve también a colocar mayor atención en la posible influencia que pueden tener estos

  16. Geología y evolución tectónica del frente cordilleranoa los 36º30'S: bloques de Vihuin-Huaca y Puntilla de Huincán. Mendoza Geology and tectonic evolution of thecordilleran front at 36ª39'S: The Yihuin-Huaca y Puntilla de Huincán blocks, Mendoza

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    Bruno J Galarza

    2009-10-01

    unidades posteriores. A toda esta estructuración se le atribuyeuna edad miocena superior, acotada por i la presencia de volcanitas del GrupoMolle de edad miocena media a superior, involucradas en la deformación, y porvolcanitas sin deformar que las cubren de edad pliocenas a cuaternarias, y iila edad basal de las secuencias sinorogénicas acumuladas inmediatamente al esteen el valle del río Grande correspondiente a 18 Ma. Se propone una relacióngenética entre el arribo a esta zona del arco volcánico mioceno acotado entre19 y 17 Ma en el marco de un ciclo de somerización de la losa oceánicasubducida y el desarrollo de transiciones frágiles dúctiles en este sector queconformaron el decollement de las principales estructuras de basamento.De todas formas la determinación del carácter sinorogénico de las secuenciasdel Cretácico Superior en la zona identifica a la Puntilla de Huincán como unrasgo mesozoico.The easternmost sector of the Malargüe fold and thrustbelt, between 70° and 69°40'W, in southern Mendoza Province at the Puntilla deHuincán area, is characterized by the development of thick-skinned structures.Three main thrusts are defining the orogenic front. The westernmost thrust hasa distinctive east-vergence in contraposition to the other two backthrusts. Thesecondary structures are thin-skinned thrusts, with decollements located at themiddle Cretaceous Huitrín Formation. These structures are modified at surfaceby the emplacement of the Miocene Molle Formation intrusives. The Andean upliftat the orogenic front in these latitudes was mainly Late Miocene, and wascoetaneous to the emplacement of a volcanic arc between 19 and 17 Ma in thearea, expansion generated by the shallowing of the subducted plate. However, thePuntilla de Huincán constitutes an older late Cretaceous structure associatedwith synorogenic sedimentation.

  17. Efectos del Barrio La Gloria: Experiencias del lugar y estrategias simbólicas de los sectores populares en el Gran Mendoza Efeitos do "Barrio de La Gloria": As experiências do lugar e estratégias simbólicas das classes populares na Grande Mendoza Effects of "Barrio La Gloria": The "experience of place" and symbolic strategies of the popular classes in the Greater Mendoza

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    Magdalena Tosoni

    2011-12-01

    Full Text Available En este artículo describo las transformaciones en el espacio urbano y su relación con las desigualdades sociales y simbólicas en el Gran Mendoza. Las políticas de vivienda y los cambios en el mercado inmobiliario promovieron la suburbanización de los sectores populares y la jerarquización del territorio durante los últimos treinta años. A partir de un estudio de caso sobre el Barrio La Gloria ubicado en el sudeste del municipio de Godoy Cruz describo las " experiencias dellugar", es decir, cómo viven las desigualdades materiales y simbólicas los habitantes de un barrio popular del Gran Mendoza, y analizo las estrategias que ensayan las organizaciones para acumular capital simbólico en un área sentida como insegura por sus habitantes y calificada de "peligrosa" por la prensa.Neste artigo vou abordar as transformações no espaço urbano e os usos do local por setores populares e suas organizações na Grande Mendoza. As políticas de habitação e mudanças no mercado imobiliário têm promovido a suburbanização da classes média e popular, e da hierarquia dos territórios. A partir de um estudo de caso do Bairro La Gloria localizado na municipalidade de Godoy Cruz descrever a "experiência do lugar", ou seja, como vivem material e simbólica das desigualdades pessoas em cidade de Mendoza e analisar estratégias que as organizações de teste para acumular capital simbólico em uma área se sentiam inseguros para os seus habitantes e qualificados "perigoso" pela imprensa .In this article I search the transformations in urban space and the uses of the place by popular sectors and their organizations in the Greater Mendoza. Housing policies and changes in the housing market have caused the suburbanization of the middle and popular classes and hierarchy of the territories during the last thirty years. In this work we study the case of Barrio La Gloria is located in the southeastern city of Godoy Cruz, an area characterized by the

  18. Estrés nutricional, hipoplasia y explotación de recursos en el centro sur de Mendoza (Argentina Nutritional stress, enamel hypoplasia, and resource exploitation in south-central Mendoza

    Directory of Open Access Journals (Sweden)

    Paula Novellino

    2007-12-01

    Full Text Available Recientemente, se ha propuesto la existencia de un proceso de intensificación en la explotación de recursos para el alto valle del río Atuel durante los últimos 2000 años (Neme et al. 2005. Si bien se han registrado cambios similares en el resto del sur de Mendoza, han surgido algunos cuestionamientos sobre el reflejo arqueológico del mismo (Borrero 2002. Hasta el momento, la discusión de este problema había sido abordada desde el registro arqueofaunístico y desde los patrones de asentamiento (Neme 2002a, 2002b. En este trabajo, se presenta el estudio de las líneas de hipoplasia dental en los restos humanos de la región, como una línea de corroboración independiente para evaluar la existencia de estrés nutricional asociado a las etapas iniciales de un proceso de intensificación. Se presentan los resultados del análisis de 1505 piezas dentales permanentes en 128 individuos del centro sur de Mendoza, comparándose con estudios similares previos en la misma región y regiones vecinas. Se discute la tendencia cronológica de las hipoplasias registradas en el contexto de la intensificación propuesta. Los resultados no son concordantes con el estrés nutricional esperado y por ello se discuten explicaciones alternativas y problemas que podrían estar produciendo este patrón distinto al esperado.The existence of an intensification process in the exploitation of resources in the upper valley of the Atuel River during the last 2000 years has recently been proposed (Neme et al. 2005. Although similar changes have been registered in the rest of southern Mendoza, doubts about the archaeological record reflective of this process have arisen (Borrero 2002. Until now discussion of this problem had been approached from the archaeofaunal record and settlement patterns (Neme 2002a, 2002b. In this paper, the study of dental enamel hypoplasia in human remains of the region as an independent test to evaluate the existence of nutritional stress

  19. Permafrost distribution modelling in the semi-arid Chilean Andes

    Science.gov (United States)

    Azócar, Guillermo F.; Brenning, Alexander; Bodin, Xavier

    2017-04-01

    Mountain permafrost and rock glaciers in the dry Andes are of growing interest due to the increase in mining industry and infrastructure development in this remote area. Empirical models of mountain permafrost distribution based on rock glacier activity status and temperature data have been established as a tool for regional-scale assessments of its distribution; this kind of model approach has never been applied for a large portion of the Andes. In the present study, this methodology is applied to map permafrost favourability throughout the semi-arid Andes of central Chile (29-32° S), excluding areas of exposed bedrock. After spatially modelling of the mean annual air temperature distribution from scarce temperature records (116 station years) using a linear mixed-effects model, a generalized additive model was built to model the activity status of 3524 rock glaciers. A permafrost favourability index (PFI) was obtained by adjusting model predictions for conceptual differences between permafrost and rock glacier distribution. The results indicate that the model has an acceptable performance (median AUROC: 0.76). Conditions highly favourable to permafrost presence (PFI ≥ 0.75) are predicted for 1051 km2 of mountain terrain, or 2.7 % of the total area of the watersheds studied. Favourable conditions are expected to occur in 2636 km2, or 6.8 % of the area. Substantial portions of the Elqui and Huasco watersheds are considered to be favourable for permafrost presence (11.8 % each), while in the Limarí and Choapa watersheds permafrost is expected to be mostly limited to specific sub-watersheds. In the future, local ground-truth observations will be required to confirm permafrost presence in favourable areas and to monitor permafrost evolution under the influence of climate change.

  20. Macro-ecología de los Andes peruanos

    OpenAIRE

    Salaverry Llosa, José A.

    2015-01-01

    El libro presenta los aspectos referidos a la dinámica de cambio que ha impuesto la naturaleza sobre las condiciones macro-ecológicas de los Andes desde la era arcaica y formativa de las culturas agrarias andinas peruanas que ocuparon el territorio peruano. Principalmente se ocupa de las modificaciones en las condiciones geo-hidrográficas y de clima-vegetación que se han producido, relacionadas a los periodos de cambio climático universales repercutiendo en el paisaje y el Hombre en las zona...

  1. The viticulture labor in Mendoza (Argentina during the capitalist modernization, 1880-1914 El mundo del trabajo vitivinícola en Mendoza (Argentina durante la modernización capitalista, 1880-1914

    Directory of Open Access Journals (Sweden)

    Rodolfo Richard-Jorba

    2009-01-01

    Full Text Available This paper outlines the development process of the capitalist viticulture in Mendoza. Using different primary and secondary sources, this study determines the composition of the viticulture labor and its quantitative and qualitative evolution. The introduction of up to date technology forced the training of manual labor with visible improvements in the workers' pay checks. This market became more complex through time showing multiple hierarchies in every rank of the work force, from peasants to wine makers. Several workers ascended the social ladder becoming managers due to diverse strategies traced through our various sources. Finally the workers' labor conditions indicate the vulnerability in which they were involved and their helplessness due to the lack of unions that could represent themEste artículo traza un breve panorama del proceso de desarrollo de la vitivinicultura capitalista en Mendoza y luego, utilizando diversas fuentes primarias y secundarias, determina la composición del mercado de trabajo vitivinícola y su evolución cuantitativa y cualitativa. La introducción de equipamiento técnico de avanzada obligó a la capacitación de la mano de obra con mejoras en los ingresos de los asalariados. Este mercado se complejizó con el tiempo y aparecieron múltiples jerarquías, desde el peón al enólogo o director técnico de las bodegas, pasando por los contratistas de viñas o los capataces. Muchos trabajadores ascendieron socialmente y se convirtieron en empresarios, en itinerarios que respondieron a diversas estrategias rastreables en las fuentes. Finalmente, las condiciones laborales que tuvieron los trabajadores muestran la precariedad en la que se desenvolvían y la indefensión en la que estaban inmersos por la ausencia de colectivos gremiales que asumieran la representación del trabajo frente al capital

  2. Desarrollo poblacional de Diaspidiotus perniciosus (Hemiptera: Diaspididae en cultivos de manzano de San Carlos, Mendoza, Argentina Population development of Diaspidiotus perniciosus (Hemiptera: Diaspididae in apple orchards in San Carlos, Mendoza, Argentina

    Directory of Open Access Journals (Sweden)

    Guillermo P. Lopez Garcia

    2011-12-01

    Full Text Available Se estudió la bionomía de Diaspidiotus perniciosus Comstock ("escama de San José", en manzanos de la variedad "Red delicious" de San Carlos, Mendoza, Argentina, durante los ciclos productivos 2007-2008 y 2008-2009. Se determinó el número de generaciones anuales y se estudiaron las fluctuaciones poblacionales asociadas a la integral térmica para la especie en esta región. D. perniciosus presenta dos generaciones superpuestas al ciclo del cultivo, mientras que las ninfas (N1 y N2 de la tercera generación se desarrollan solamente hasta el final de la temporada estival y pasan al estado de quiescencia, en el que permanecen durante el invierno. El desarrollo de D. perniciosus en esta zona coincide con el de esta especie en la zona frutícola del centro de Chile en cuanto al número de generaciones y al periodo de quiescencia invernal. La población quiescente en Chile está integrada predominantemente por ninfas del primer estadio (N1, mientras que en San Carlos, Mendoza, la población quiescente está integrada principalmente por ninfas del segundo estadio (N2. La similitudes entre ambas poblaciones se deben, probablemente, a las coincidencias en latitud, clima y especie hospedera. El impacto económico de D. perniciosus en la zona de estudio tiene mayor relevancia durante los meses de diciembre y enero, cuando se observa una alta incidencia de daños en los frutos y las hojas; este es el momento decisivo para implementar medidas de control fitosanitario. Estas deberán aplicarse en función de los máximos poblacionales de N1 que se producen con 600-650 Grados-Día (ºD en diciembre y con 1.170-1.270ºD en enero. En las temporadas en las que la densidad poblacional de la plaga es especialmente alta, podrían incorporarse medidas adicionales de control con 1.800-2.000ºD durante el mes de abril. Los resultados de estos estudios representan una herramienta predictiva, que permitirá elaborar estrategias para el control de poblaciones de D

  3. Evapofacieshalítica en el Salar del Rincón, departamento Los Andes, Salta Halitefacies in the salar del Rincon, Andes Department, Salta

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    Alberto Ovejero Toledo

    2009-06-01

    Full Text Available El salar delRincón se encuentra ubicado en el departamento Los Andes, provincia de Salta enel extremo noroeste de la Puna Austral, a una altura media de 3.660 m s.n.m. Eneste trabajo se dan a conocer los resultados de la correlación de sondeos, quepermitieron determinar facies de halita, texturas, estructuras, materialesclásticos intersticiales, mineralogía, composición química de la salmuera y losparámetros hidráulicos del acuífero, determinados a lo largo de una transectaeste-oeste que cubre aproximadamente 30 km². La fase cristalina estácompuesta mayoritariamente de halita, con yeso, mirabilita, thenardita,glauberita, hidroglauberita, eugsterita, calcita y ulexita solo en el sectoroeste de la transecta. Se identificaron las siguientes evapofacies halítica:costra salina, geodas y halita bandeada. Las texturas observadas incluyen:cristales hoppers, pirámides chevron, halita intersticial muddyhalite y halita cloudy. La composición de la salmuera es denaturaleza clorurada sódica con variaciones en profundidad de sulfato y borato.Los cationes son Ca, Mg, Li y K, la relación K/Li es de 20/1. El cálculo dereserva a nivel de recurso mineral, en sectores con distinta porosidad eficaz,dio para Li+ 208,2 kt y para K+ 4231,9 kt (> 30 %; yLi+ 14,9 kt y K+ 302, 9 kt (Salar del Rincón is located at 3,660 m.a.s.l. in the Andes district, Salta province, andnortheast of the Southern Puna. This paper shows the results of theborehole correlation that helped determine the halite facies, textures,structures, interstitial clastic material, mineralogy, chemical composition ofthe brine and the aquifer hydraulic parameters determineted in an E-W transectthat covers approximately 30 km². The crystalline phase is mainlymade up of halite with gypsum, mirabilite, thenardite, glauberite,hydroglauberite, eugsterite, calcite, and ulexite only in the western area oftransect. The following halite evapofacies were identified: saline crust,geodes and banded

  4. El tropero y el origen de la burguesía en el Cono Sur (Mendoza, siglo XVIII

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    Lacoste, Pablo

    2005-01-01

    Full Text Available Este artigo aprofunda a análise sobre a carreta e o tropeiro, para definir em que medida contribuíram para o processo de construção de uma cultura empresarial na América Colonial, levando ao surgimento de uma burguesia. Atenta-se, em especial, para temas como mobilidade social, riscos empresariais, fomento do crédito em confiança ou por hipoteca de carretas, circulação de idéias e configuração de um ethos capitalista. Este trabalho constitui a continuação e a conclusão de um anterior intitulado "Carretas y transporte terrestre bioceánico: la ruta Buenos Aires-Mendoza en el siglo XVIII" (Estudos Ibero-Americanos, vol. XXXI, nº 1, 2005

  5. Representaciones, turismo y Estado. Imágenes y discursos en torno de los paisajes culturales de Mendoza (Argentina

    Directory of Open Access Journals (Sweden)

    Cecilia Raffa

    2012-01-01

    Full Text Available En los últimos años, la provincia de Mendoza ha logrado consolidarse como uno de los principales destinos turísticos de Argentina: su paisaje la ha posicionado como lugar elegido por los turistas tanto nacionales como extranjeros. El trabajo que presentamos se propone refl exionar sobre los procesos dominantes que impulsaron la construcción del paisaje de la capital provincial, a través de la acción pública promovida por el Estado. Se analizan los procesos que los conducen, los actores que los encarnan y las imágenes resultantes que dan origen a la vez que nutren y renuevan las representaciones sociales sobre una ciudad que encuentra la clave de su identidad y gran parte de su desarrollo turístico, en el control y uso del agua.

  6. Carretas y transporte terrestre bioceánico: la ruta Buenos Aires-Mendoza en el siglo XVIII

    Directory of Open Access Journals (Sweden)

    Lacoste, Pablo

    2005-01-01

    Full Text Available A carreta foi o principal meio de transporte terrestre na América colonial entre os séculos XVI e XIX. Uma das rotas mais utilizadas foi Buenos Aires-Mendoza, estabelecendo uma ligação entre os mercados do Atlântico e do Pacífico. Este artigo examina essas rotas, ao final do século XVIII, com base no processamento das viagens de 16. 000 carretas. O tema será aprofundado em um segundo trabalho intitulado "Los troperos y los orígenes de la burguesía en el Cono Sur de América colonial" (previsto para o próximo número de Estudos Ibero-Americanos

  7. A probability index for surface zonda wind occurrence at Mendoza city through vertical sounding principal components analysis

    Science.gov (United States)

    Otero, Federico; Norte, Federico; Araneo, Diego

    2016-10-01

    The aim of this work is to obtain an index for predicting the probability of occurrence of zonda event at surface level from sounding data at Mendoza city, Argentine. To accomplish this goal, surface zonda wind events were previously found with an objective classification method (OCM) only considering the surface station values. Once obtained the dates and the onset time of each event, the prior closest sounding for each event was taken to realize a principal component analysis (PCA) that is used to identify the leading patterns of the vertical structure of the atmosphere previously to a zonda wind event. These components were used to construct the index model. For the PCA an entry matrix of temperature (T) and dew point temperature (Td) anomalies for the standard levels between 850 and 300 hPa was build. The analysis yielded six significant components with a 94 % of the variance explained and the leading patterns of favorable weather conditions for the development of the phenomenon were obtained. A zonda/non-zonda indicator c can be estimated by a logistic multiple regressions depending on the PCA component loadings, determining a zonda probability index widehat{c} calculable from T and Td profiles and it depends on the climatological features of the region. The index showed 74.7 % efficiency. The same analysis was performed by adding surface values of T and Td from Mendoza Aero station increasing the index efficiency to 87.8 %. The results revealed four significantly correlated PCs with a major improvement in differentiating zonda cases and a reducing of the uncertainty interval.

  8. Protoplanetary Disk Structure With Grain Evolution: the ANDES Model

    CERN Document Server

    Akimkin, V; Wiebe, D; Semenov, D; Pavlyuchenkov, Ya; Vasyunin, A; Birnstiel, T; Henning, Th

    2013-01-01

    We present a self-consistent model of a protoplanetary disk: 'ANDES' ('AccretioN disk with Dust Evolution and Sedimentation'). ANDES is based on a flexible and extendable modular structure that includes 1) a 1+1D frequency-dependent continuum radiative transfer module, 2) a module to calculate the chemical evolution using an extended gas-grain network with UV/X-ray-driven processes surface reactions, 3) a module to calculate the gas thermal energy balance, and 4) a 1+1D module that simulates dust grain evolution. For the first time, grain evolution and time-dependent molecular chemistry are included in a protoplanetary disk model. We find that grain growth and sedimentation of large grains to the disk midplane lead to a dust-depleted atmosphere. Consequently, dust and gas temperatures become higher in the inner disk (R 50 AU), in comparison with the disk model with pristine dust. The response of disk chemical structure to the dust growth and sedimentation is twofold. First, due to higher transparency a partl...

  9. GEOMORPHOLOGIC HAZARD AND DISASTERS IN THE SOUTH AMERICAN ANDES

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    Ekaterina V. Lebedeva

    2014-01-01

    Full Text Available Geological-and-tectonic and physiographical features of the South American Pacific coast caused high intensity of morpholitogenesis including disaster-like way of some geomorphologic processes. Their complex, interaction, and intensity of conductive factors increase the risk of disaster. The Andean terrain morphology and rock lithology, precipitation type, and vegetation status are the main drivers that influence the character and high potential intensity of the geomorphologic processes. The enormous hydrometeorological events, frequent seismic shocks, volcanic eruptions, and human impact cause disasters development. A schematic map of disaster and hazardous processes for the Central sector of Andes was compiled. 16 areas with different spectra of the dominant catastrophic processes were identified. The South American Andes extension allows drawing out principles of geomorphologic disasters of these continental marginal mountains in various natural zones - from temporal to subequatorial latitudes, which are characterized by the individual unique heat-moisture rate, which governs both typical and extreme geomorphologic processes. An important feature of the study area is the asymmetric distribution of geomorphologic processes within coastal and inland slopes of the mountain system, as well as latitudinal zoning of this distribution.

  10. The paradigm of paraglacial megafans of the San Juan river basin, Central Andes, Argentina

    Science.gov (United States)

    Suvires, Graciela M.

    2014-11-01

    The spatial distribution and several morphometric characteristics of the Quaternary alluvial fans of the San Juan River, in the province of San Juan, at the Central and Western part of Argentina, have been studied to classify them as paraglacial megafans, as well to ratify its depositional environmental conditions. The high sedimentary load exported by San Juan river from the Central Andes to the foreland depressions is estimated about 3,682,200 hm3. The large alluvial fans of Ullum-Zonda and Tulum valleys were deposited into deep tectonic depressions, during the Upper Pleistocene deglaciation stages. The outcome of collecting remotely sensed data, map and DEM data, geophysical data and much fieldwork gave access to morphometric, morphographic and morphogenetic data of these alluvial fans. The main drainage network was mapped on processed images using QGis (vers.2.0.1). Several fan morphometric parameters were measured, such as the size, the shape, the thickness, the surface areas and the sedimentary volume of exported load. The analyzed fans were accumulated in deep tectonic depressions, where the alluvium fill reaches 700 to 1200 m thick. Such fans do not reach the large size that other world megafans have, and this is due to tectonic obstacles, although the sedimentary fill average volume surpasses 514,000 hm3. The author proposes to consider Ullum-Zonda and Tulum alluvial fans as paraglacial megafans. According to the stratigraphic relationships of the tropical South American Rivers, the author considers that the San Juan paraglacial megafans would have occurred in the period before 24 ka BP , possibly corresponding to Middle Pleniglacial (ca 65-24ka BP). They record colder and more humid conditions compared with the present arid and dry conditions.

  11. La desaparecida Capillade don Lope de Mendoza: nuevos datos sobre sus retablos, los sepulcros, su coro alto y la sacristía

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    Fernández González, Alberto

    2005-12-01

    Full Text Available Very little precise information remains on the exact characteristics of the no longer existing early medieval chapel founded by Archbishop Lope de Mendoza in the Cathedral of Santiago. Following the discovery of new documentary findings including descriptions, contracts, wills and a significant map of 1739, interesting facts about certain aspects of its architecture and tombs have been brought to light and, above all, we are able to reconstruct the furnishing of this important cathedral enclosure.

    De la desaparecida capilla bajomedieval que el arzobispo don Lope de Mendoza fundó en la catedral de Santiago apenas tenemos información precisa que permita conocer adecuadamente sus características. A partir del hallazgo de nuevas noticias documentales, que incluyen descripciones, contratos, testamentos y un significativo plano de 1739, se pueden aportar interesantes datos sobre algunos aspectos de su arquitectura y sepulcros y, sobre todo, reconstruir el amueblamiento de este importante recinto catedralicio.

  12. Los territorios de la violencia en la novela policial y la narcoliteratura latinoamericana: Mario Mendoza, Peter Elmore y Alejandro Páez

    Directory of Open Access Journals (Sweden)

    Danilo Santos López

    2015-12-01

    Full Text Available El artículo expone la problemática de la violencia en las sociedades latinoamericanas a través de su representación en una serie de novelas publicadas a partir de los años noventa. Para ello se seleccionó las novelas policiales Enigma de los cuerpos (1995 de Peter Elmore, Satanás (2002 de Mario Mendoza y las narconovelas Corazón de Kalashnikov (2009, El reino de las moscas (2012 y Música para perros (2013 de Alejandro Páez Varela. Ellos son textos que recogen la situación de los personajes-víctimas de la novela criminalizada a través de la mirada narrativa sobre territorios muy delimitados como la Lima de Elmore, la Bogotá de Mendoza y Ciudad Juárez de Páez Varela.

  13. Lineamientos para la definición de un modo de crecimiento urbano sostenible: el Caso de Mendoza (Argentina), provincia de tierras secas

    OpenAIRE

    Sammartino, Mariana Silvina

    2016-01-01

    Actualmente, la globalización está generando procesos territoriales que modifican sustancialmente los sistemas urbanos. En Mendoza, los procesos de ocupación han generado un territorio fragmentando producto de la interacción histórica naturaleza-sociedad, existiendo espacios dominantes (los oasis) sobre otros dominados (las tierras secas no irrigadas). Esto ha producido un modelo territorial de concentración difusa desequilibrada, reflejo de una región subdesarrollada con una estructura...

  14. The cultural heritage of the metropolitan area of Mendoza (Argentina). Methodological suggestions for their evaluation as a resource in local development project

    OpenAIRE

    Raffa, Cecilia; Conicet Argentina.; Cirvini, Silvia Augusta; Conicet Argentina.

    2014-01-01

    The research methodology proposal as presented, articulate and transfer of applied research results about EnvironmentalHeritage (pca) of the Metropolitan Area of Mendoza (amm). Our general hypothesis argues that the cultural heritage associatedwith the Territory (real estate: architectural, urban, landscape, with its accessories and environment) is a resource and a toolin local development processes, which in the case of the amm is not taken into account by the main actors involved. That is w...

  15. Looking for periodicities in the hail intensity in the Andes region

    Energy Technology Data Exchange (ETDEWEB)

    Prieto, R; Herrera, R; Doussel, P [Inaiglia, Mendoza (Argentina); Gimeno, L; Ribera, P [Univerisdad de Vigo, Orense (Spain); Garcia, R; Hernandez, E [Universidad Complutense de Madrid, Madrid (Spain)

    2001-04-01

    Documental sources and categorization techniques were used to construct a series of the annual hail intensity in Mendoza area (Argentina). When the temporal series by means of Singular Spectrum Analysis (SSA) and the Maximum Entropy Method (MEM) was analyzed, we found interdecadal oscillations of periods of about 20 years and interannual oscillations of about 4 and 9 years. In addition when detrented-data were used a low frequency oscillation of about 72 years also appears. [Spanish] Para construir una serie de intensidades de granizo en el area de Mendoza (Argentina), se emplearon fuentes documentales y tecnicas de caracterizacion. Cuando se analizaron las series temporales, mediante el Analisis Singular del Expectro (SSA), y el Metodo de Maxima Entropia, encontramos oscilaciones decadales con periodos de aproximadamente 20 anos y oscilaciones interanuales de alrededor de 4 a 9 anos. Ademas cuando la variacion por tendencia de los datos se elimino, se puso de manifiesto una oscilacion de frecuencia de cerca de 72 anos.

  16. Oroclinal Bending and Mountain Uplift in the Central Andes

    Science.gov (United States)

    Mpodozis, C.; Arriagada, C.; Roperch, P.

    2007-05-01

    The large paleomagnetic database now available for the Central Andes permits a good understanding of the overall spatial and temporal variations of rotations. Mesozoic to Early Paleogene rocks along the forearc of northern Chile (23°-28°S) record significant clockwise rotations (>25°) [Arriagada et al., 2006, Tectonics, doi:10.1029/2005TC001923]. Along the forearc of southern Peru, counterclockwise rotations recorded within flat lying red-beds (Moquegua Formation) increase from about -30° at 17.5°S to - 45° at15.5°S and decrease through time from the late Eocene to the late Oligocene-early Miocene [Roperch et al., 2006, Tectonics, doi:10.1029/2005TC001882]. Recently published thermo-chronological studies show evidence for strong exhumation within Bolivian Eastern Cordillera and the Puna plateau starting in the Eocene while structural studies indicate that the majority of crustal shortening in the Eastern Cordillera occurred during the Eocene-Oligocene, although the final stages of deformation may have continued through the Early Miocene. Rotations in the Peruvian and north Chilean forearc thus occurred at the same time than deformation and exhumation/uplift within the Eastern Cordillera. In contrast Neogene forearc rocks in southern Peru and northern Chile do not show evidences of rotation but low magnitude (10°) counterclockwise rotations are usually found in mid to late Miocene rocks from the northern Altiplano. These Neogene rotations are concomitant with shortening in the Sub-Andean zone and sinistral strike-slip faulting along the eastern edge of the northern Altiplano. We interpret the rotation pattern along the southern Peru and north Chile forearc as a result of strong late Eocene- late Oligocene oroclinal bending of the Central Andes associated with shortening gradients along the Eastern Cordillera associated both with the Abancay deflection and the Arica bend. The amount and spatial distribution of pre-Neogene shortening needed to account for

  17. Did growth of high Andes slow down Nazca plate subduction?

    Science.gov (United States)

    Quinteros, J.; Sobolev, S. V.

    2010-12-01

    The convergence velocity rate of the Nazca and South-American plate and its variations during the last 100 My are quite well-known from the global plate reconstructions. The key observation is that the rate of Nazca plate subduction has decreased by about 2 times during last 20 Myr and particularly since 10 Ma. During the same time the Central Andes have grown to its present 3-4 km height. Based on the thin-shell model, coupled with mantle convection, it was suggested that slowing down of Nazca plate resulted from the additional load exerted by the Andes. However, the thin-shell model, that integrates stresses and velocities vertically and therefore has no vertical resolution, is not an optimal tool to model a subduction zone. More appropriate would be modeling it with full thermomechanical formulation and self-consistent subduction. We performed a set of experiments to estimate the influence that an orogen like the Andes could have on an ongoing subduction. We used an enhanced 2D version of the SLIM-3D code suitable to simulate the evolution of a subducting slab in a self-consistent manner (gravity driven) at vertical crossections through upper mantle, transition zone and shallower lower mantle. The model utilizes non-linear temperature- and stress-dependant visco-elasto-plastic rheology and phase transitions at 410 and 660 km depth. We started from a reference case with a similar configuration as both Nazca and South-America plates. After some Mys of slow kinematicaly imposed subduction, to develop a coherent thermo-mechanical state, subduction was totally dynamic. On the other cases, the crust was slowly thickened artificially during 10 My to generate the Andean topography. Although our first results show no substantial changes on the velocity pattern of the subduction, we, however, consider this result as preliminary. At the meeting we plan to report completed and verified modeling results and discuss other possible cases of the late Cenozoic slowing down of

  18. GARGANTA SECA Y ARENA EN LAS BOTAS: PROSPECTANDO ANTECEDENTES ARQUEOLÓGICOS DE LAS TIERRAS ÁRIDAS DEL NORESTE MENDOCINO (CENTRO OESTE ARGENTINO (Dry throat and sand in the boots: Prospecting archaeological backgrounds of the Mendoza Northeastern drylands, Argentinian Center South

    Directory of Open Access Journals (Sweden)

    Horacio Chiavazza

    2009-03-01

    Full Text Available Aquí se presenta un detallado estado de las investigaciones arqueológicas desarrolladas en el noreste de la provincia argentina de Mendoza. Esta zona es objeto de estudios desde principios del siglo XX. Sin embargo los pulsos de la investigación han registrado etapas de abandono total y de intervenciones selectivas. Los investigadores han partido de los trabajos precedentes para explicar por extensión las modalidades de asentamiento en la totalidad del territorio norte y, sobre todo, del occidente montañoso, que era donde concentraban sus campañas. Esto acabó generando un cuadro de antecedentes desequilibrado y superficial en el conocimiento de dicha área, con implicaciones en el cuadro interpretativo general de la prehistoria local. En este caso, indagamos las posibles causas que dieron lugar a tal proceso, sus vínculos con los enfoques teóricos y metodologías dominantes a lo largo del siglo XX y su relación con la selección de zonas para llevar a cabo estudios de campo en el norte de la provincia. Reflexionamos críticamente sobre los alcances, límites y posibilidades que ofrece la región para profundizar los análisis arqueológicos del poblamiento prehispánico en relación con las condiciones del ambiente y los procesos históricos documentados, proponiendo discutir los enfoques que basan sus explicaciones en hechos dados por sentados y que merecerían antes una discusión en base a la evidencia disponible. ENGLISH: Here is a detailed state of archaeological research developed in the northeastern Argentine province of Mendoza. This area is the subject of studies since the early twentieth century. However, the pulses of the investigation have been stages of total abandonment and selective interventions. This ended up creating an unbalanced picture of history and superficial knowledge of that area, with implications for the general picture of prehistory interpreted locally. In this case, we investigate the possible causes

  19. [Lake Andes Wetland Management District: Aerial Photograph of Easement 38x in Hyde County, SD, 1984

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This oblique aerial photograph from the Lake Andes Wetland Management District was taken from Easement 38x (Sec. 7 Lot 1 looking NW) in Hyde County, SD in 1984. It...

  20. [Lake Andes Wetland Management District: Aerial Photograph Series, Charles Mix County, SD, 1967-1988

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This series consists of 10 oblique aerial photographs from the Lake Andes Wetland Management District. All photographs were taken in Charles Mix County, South Dakota...

  1. Lake Andes Wetland Management District: Annual narrative report : Calendar year 1977

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report for Lake Andes Wetland Management District outlines Refuge accomplishments during the 1977 calendar year. The report begins with an...

  2. Annual narrative report: Lake Andes National Wildlife Refuge and Management District: Calendar year 1974

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report summarizes activities on Lake Andes NWR during the 1974 calendar year. Monthly activities reports are provided. Resource management- including...

  3. Lake Andes Wetland Management District: Annual narrative report : Calendar year 1978

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report for Lake Andes Wetland Management District outlines Refuge accomplishments during the 1978 calendar year. The report begins with an...

  4. Lake Andes Waterfowl Production Area: Narrative report: January 1 through December 31, 1967

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR- Waterfowl Production Area outlines Refuge accomplishments during the 1967 calendar year. The report begins by...

  5. Lake Andes Wetlands District: Narrative report: January 1 through December 31, 1971

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes Wetlands District outlines Refuge accomplishments during the 1971 calendar year. The report begins by summarizing the...

  6. Lake Andes [Wetland Management District]: Narrative report: January 1 through December 31, 1972

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes Wetlands District outlines Refuge accomplishments during the 1972 calendar year. The report begins by summarizing the...

  7. [Lake Andes Wetland Management District: Narrative report : July 1, 1975 through December 31, 1976

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report for Lake Andes Wetland Management District outlines Refuge accomplishments during the 1976 calendar year. The report begins with an...

  8. Lake Andes Wetland District: Narrative report: January 1 through December 31, 1970

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes Wetlands District outlines Refuge accomplishments during the 1970 calendar year. The report begins by summarizing the...

  9. Lake Andes Wetlands District: Narrative report: January 1 through December 31, 1969

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes Wetlands District outlines Refuge accomplishments during the 1969 calendar year. The report begins by summarizing the...

  10. Planning and accomplishment narrative: Lake Andes Wetlands District: July 1, 1972 through June 30, 1973

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes Wetlands District describes Refuge activities during the 1973 fiscal year. Highlights and accomplishments are described.

  11. Lake Andes Wetlands District: Narrative report: January 1 through December 31, 1968

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes Wetlands District outlines Refuge accomplishments during the 1968 calendar year. The report begins by summarizing the...

  12. Lake Andes Wetland Management District: Annual narrative report : Calendar year 1979

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report for Lake Andes Wetland Management District outlines Refuge accomplishments during the 1979 calendar year. The report begins with an...

  13. Litterfall production under pine plantations in the southern Andes region of Ecuador

    Directory of Open Access Journals (Sweden)

    Pablo Quichimbo

    2016-09-01

    Full Text Available Litterfall research is an interesting aspect in environmental studies due to its significance in nutrient cycling specially in regions like the Andes where the interactions between biomass production and its decomposition is poorly understood. This study is focusing in the litterfall biomass production under pine plantations in southern Ecuador. The litterfall production was studied for five months at two-week intervals in three pine forest sites located in the southern Andes region of Ecuador. Monthly litterfall production ranged between 1067-1907 kg ha-1, in comparison with other coniferous stands around the world, this study revealed a higher litterfall production for tropical areas and particularly the highest production under pine plantations in the Andes region. This high litterfall production highlights the upmost importance of this forest component as a potential nutrient reservoir involved in the global nutrient cycling under landscapes dominated by this exotic forest specie in the tropical Andes.

  14. Phase 1 Watershed Assessment Final Report: Lake Andes Watershed, Charles Mix County, South Dakota.

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — Lake Andes was included in the 1998 South Dakota 303(d) list as an impairment-related Total Maximum Daily Load waterbody. In 1922 Congress passed a bill that...

  15. Lake Assessment Project Report, Lake Andes: Charles Mix County, South Dakota

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — Lake Andes was included in the 1998 South Dakota 303(d) list as an impairment-related Total Maximum Daily Load waterbody. In 1922 Congress passed a bill that...

  16. Narrative report: May, June, July, and August, 1962: Lake Andes National Wildlife Refuge

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report for Lake Andes NWR outlines Refuge accomplishments from May through August of 1962. The report begins by summarizing the weather conditions,...

  17. Narrative report: Lake Andes National Wildlife Refuge: May 1, to August 31, 1956

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report for Lake Andes NWR outlines Refuge accomplishments from May through August of 1956. The report begins by summarizing the weather conditions,...

  18. Lake Andes Wetland Management District Annual narrative report: Calendar year 1983

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report for Lake Andes Wetland Management District outlines District accomplishments during the 1983 calendar year. The report begins with an...

  19. Lake Andes Wetland Management District Annual narrative report: Calendar year 1984

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report for Lake Andes Wetland Management District outlines District accomplishments during the 1984 calendar year. The report begins with an...

  20. Lake Andes Wetland Management District Annual narrative report : Calendar year 1981

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report for Lake Andes Wetland Management District outlines District accomplishments during the 1981 calendar year. The report begins with an...

  1. Lake Andes National Wildlife Refuge: Narrative report: January 1 through December 31, 1966

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR outlines Refuge accomplishments during the 1966 calendar year. The report begins by summarizing the weather...

  2. [Lake Andes National Wildlife Refuge: Narrative report: September to December, 1953

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report for Lake Andes NWR outlines Refuge accomplishments from September through December of 1953. The report begins by summarizing the weather...

  3. [Lake Andes Wetland Management District: Aerial Photograph Series, Lake County, SD, 1967-1968

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This series consists of 3 oblique aerial photographs from the Lake Andes Wetland Management District. All photographs were taken in Lake County, South Dakota in 1967...

  4. Lake Andes Wetland Management District Annual narrative report: Calendar year 1987

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report for Lake Andes Wetland Management District outlines District accomplishments during the 1987 calendar year. The report begins with an...

  5. Narrative report: Lake Andes National Wildlife Refuge: January 1 through April 30, 1960

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report for Lake Andes NWR outlines Refuge accomplishments from January through April of 1960. The report begins by summarizing the weather conditions,...

  6. [Lake Andes National Wildlife Refuge: Narrative report: January to April, 1959

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report for Lake Andes NWR outlines Refuge accomplishments from January through April of 1959. The report begins by summarizing the weather conditions,...

  7. Lake Andes Wetland Management District : Annual narrative report : Calendar year 1980

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report for Lake Andes WMD outlines Refuge accomplishments during the 1980 calendar year. The report begins with an introduction to the Refuge and...

  8. A new species of Trechisibus from Peruvian Andes (Coleoptera: Carabidae, Trechinae

    Directory of Open Access Journals (Sweden)

    Pedro Delgado

    2016-06-01

    Full Text Available In this work the new species Trechisibus (s. str. delestali sp. n., is described from the southern Peruvian Andes. The morphological differences with the geographically closest species of the subgenus are also presented and discussed.

  9. Lake Andes National Wildlife Refuge: Annual narrative report: Calendar year 1980

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report for Lake Andes NWR outlines Refuge accomplishments during the 1980 calendar year. The report begins with an introduction to the Refuge and...

  10. Lake Andes National Wildlife Refuge: Annual narrative report: Calendar year 1979

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report for Lake Andes NWR outlines Refuge accomplishments during the 1979 calendar year. The report begins with an introduction to the Refuge and...

  11. Narrative report: September, October, November, and December, 1962: Lake Andes National Wildlife Refuge

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report for Lake Andes NWR outlines Refuge accomplishments from September through December of 1962. The report begins by summarizing the weather...

  12. Lake Andes National Wildlife Refuge: Narrative report: January 1 through December 31, 1967

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR outlines Refuge accomplishments during the 1967 calendar year. The report begins by summarizing the weather...

  13. Lake Andes National Wildlife Refuge: Narrative report: January 1 through December 31, 1969

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR outlines Refuge accomplishments during the 1969 calendar year. The report begins by summarizing the weather...

  14. Narrative report: January, February, March, and April, 1963: Lake Andes National Wildlife Refuge

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report for Lake Andes NWR outlines Refuge accomplishments from January through April of 1963. The report begins by summarizing the weather conditions,...

  15. Lake Andes Wetland Management District Annual narrative report : Calendar year 1982

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report for Lake Andes Wetland Management District outlines District accomplishments during the 1982 calendar year. The report begins with an...

  16. Lake Andes Wetland Management District: Annual narrative report: Calendar year 1992

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes Wetland Management District outlines Refuge accomplishments during the 1992 calendar year. The report begins with a...

  17. Narrative report: January 1 through December 31, 1964: Lake Andes National Wildlife Refuge

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR outlines Refuge accomplishments during the 1964 calendar year. The report begins by summarizing the weather...

  18. Narrative report: January, February, March, and April, 1962: Lake Andes National Wildlife Refuge

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report for Lake Andes NWR outlines Refuge accomplishments from January through April of 1962. The report begins by summarizing the weather conditions,...

  19. Narrative report: Lake Andes National Wildlife Refuge: May 1 through August 31, 1959

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report for Lake Andes NWR outlines Refuge accomplishments from May through August of 1959. The report begins by summarizing the weather conditions,...

  20. Lake Andes National Wildlife Refuge: Narrative report: January 1 through December 31, 1965

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR and WPA outlines Refuge accomplishments during the 1965 calendar year. The report begins by summarizing the weather...

  1. The Trail Inventory of Lake Andes Wetland Management District [Cycle 1

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — The purpose of this report is to create a baseline inventory of all non-motorized trails on Lake Andes Wetland Management District. Trails in this inventory are...

  2. [Lake Andes National Wildlife Refuge: Narrative report: January to April, 1955

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report for Lake Andes NWR outlines Refuge accomplishments from January through April of 1955. The report begins by summarizing the weather conditions,...

  3. Lake Andes Wetland Management District Annual narrative report: Calendar year 1988

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report for Lake Andes Wetland Management District outlines District accomplishments during the 1988 calendar year. The report begins with an...

  4. Sedimentation Survey Report: South Unit, Lake Andes, Charles Mix County, South Dakota.

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This report addresses the procedures used to obtain sediment data, how they analyzed the data, and the potential restoration alternatives for Lake Andes. The purpose...

  5. Gastrointestinal parasites of Lamas in the Bolivian Andes

    DEFF Research Database (Denmark)

    Nissen, Anne Malene; Nees, Ellinor Spörndly; Monrad, Jesper

    A cross sectional study was conducted to determine prevalences and intensities of gastrointestinal (GIT) parasites in lamas in the Bolivian Andes. A quantitative and qualitative necro-copro-parasitlogical study was performed on 33 lamas between October and December 2007. At the time of necropsy the......  lamas were aged 1½  to >4 years. They originated from 14 different farms in the most lama dense areas of Bolivia: Oruro, Potosi, La Paz and the highlands above Cochabamba. In total 16 different species of nematodes, one cestode species, one trematode species, and one coccidian genus were detected...... %); in the liver: Fasciola hepatica (12 %); in faeces Eimeria spp. (82 %). Pathological changes in the liver were ascribed to be most probably caused by L. chavezi larva migration. The latter species, considered to be the very most pathogenic of all lama GIT nematode species, was also the species detected...

  6. Record Solar UV Irradiance in the Tropical Andes

    Directory of Open Access Journals (Sweden)

    Nathalie A. Cabrol

    2014-07-01

    Full Text Available High elevation, thin ozone layer, and clear sky produce intense ultraviolet (UV radiation in the tropical Andes. Recent models suggest that tropical stratospheric ozone will slightly decrease in the coming decades, potentially resulting in more UV anomalies. Data collected between 4,300-5,916 m above sea level (asl in Bolivia show how this trend could dramatically impact surface solar irradiance. During 61 days, two Eldonet dosimeters recorded extreme UV-B irradiance equivalent to a UV index (UVI of 43.3, which is the highest ground value ever reported. If they become more common, events of this magnitude may have societal and ecological implications, which make understanding the process leading to their generation critical. Our data show that this event and other major UV spikes were consistent with rising UV-B/UV-A ratios in the days to hours preceding the spikes, trajectories of negative ozone anomalies (NOAs, and radiative transfer modeling.

  7. Agricultura y ganaderia en Taya, pueblo de los Andes Peruanos

    OpenAIRE

    Pouget, Cécile

    1988-01-01

    Mémoire de fin d'études présentant les activités agricoles des paysans de Taya, village des Andes péruviennes situé sur des pentes très fortes entre 3000 et 3500 mètres d'altitude. Les paysans y cultivent le maïs et les pommes de terre pour leur propre consommation, mais aussi la luzerne destinée aux vaches laitières. Avec le lait, ils font des fromages qu'ils vendent. L'organisation de l'occupation du sol montre que malgré l'érosion, le manque d'eau et d'argent, les paysans continuent ce typ...

  8. 20 years of mass balances on the Piloto glacier, Las Cuevas river basin, Mendoza, Argentina

    Science.gov (United States)

    Leiva, J. C.; Cabrera, G. A.; Lenzano, L. E.

    2007-10-01

    Climatic changes of the 20th century have altered the water cycle in the Andean basins of central Argentina. The most visible change is seen in the mountain glaciers, with loss of part of their mass due to decreasing thickness and a substantial recession in the last 100 years. This paper briefly describes the results of glacier mass balance research since 1979 in the Piloto Glacier at the Cajón del Rubio, in the headwaters of Las Cuevas River, presenting new results for the period 1997-2003. Very large interannual variability of net annual specific balance is evident, due largely to variations in winter snow accumulation, with a maximum net annual value of + 151 cm w.e. and a minimum value of - 230 cm w.e. Wet El Niño years are normally associated with positive net annual balances, while dry La Niña years generally result in negative balances. Within the 24-year period, 67% of the years show negative net annual specific balances, with a cumulative mass balance loss of - 10.50 m water equivalent (w.e.). Except for exceptions normally related to El Niño events, a general decreasing trend of winter snow accumulation is evident in the record, particularly after 1992, which has a strong effect in the overall negative mass balance values. The glacier contribution to Las Cuevas River runoff is analysed based on the Punta de Vacas River gauge station for a hypothetical year without snow precipitation (YWSP), when the snowmelt component is zero. Extremely dry years similar to a YWSP have occurred in 1968-1969, 1969-1970 and 1996-1997. The Punta de Vacas gauge station is located 62 km downstream from Piloto Glacier, and the basin contains 3.0% of uncovered glacier ice and 3.7% of debris-covered ice. The total glacier contribution to Las Cuevas River discharge is calculated as 82 ± 8% during extremely dry years. If glacier wastage continues at the present trend as observed during the last 2 decades, it will severely affect the water resources in the arid central Andes of

  9. PROTOPLANETARY DISK STRUCTURE WITH GRAIN EVOLUTION: THE ANDES MODEL

    Energy Technology Data Exchange (ETDEWEB)

    Akimkin, V.; Wiebe, D.; Pavlyuchenkov, Ya. [Institute of Astronomy of the RAS, Pyatnitskaya str. 48, Moscow (Russian Federation); Zhukovska, S.; Semenov, D.; Henning, Th. [Max-Planck-Institute for Astronomy, Koenigstuhl 17, D-69117 Heidelberg (Germany); Vasyunin, A. [Department of Chemistry, The University of Virginia, VA (United States); Birnstiel, T., E-mail: akimkin@inasan.ru, E-mail: dwiebe@inasan.ru, E-mail: pavyar@inasan.ru, E-mail: zhukovska@mpia.de, E-mail: semenov@mpia.de, E-mail: henning@mpia.de, E-mail: anton.vasyunin@gmail.com, E-mail: tbirnstiel@cfa.harvard.edu [Harvard-Smithsonian Center for Astrophysics, 60 Garden Street, Cambridge, MA 02138 (United States)

    2013-03-20

    We present a self-consistent model of a protoplanetary disk: 'ANDES' ('AccretioN disk with Dust Evolution and Sedimentation'). ANDES is based on a flexible and extendable modular structure that includes (1) a 1+1D frequency-dependent continuum radiative transfer module, (2) a module to calculate the chemical evolution using an extended gas-grain network with UV/X-ray-driven processes and surface reactions, (3) a module to calculate the gas thermal energy balance, and (4) a 1+1D module that simulates dust grain evolution. For the first time, grain evolution and time-dependent molecular chemistry are included in a protoplanetary disk model. We find that grain growth and sedimentation of large grains onto the disk midplane lead to a dust-depleted atmosphere. Consequently, dust and gas temperatures become higher in the inner disk (R {approx}< 50 AU) and lower in the outer disk (R {approx}> 50 AU), in comparison with the disk model with pristine dust. The response of disk chemical structure to the dust growth and sedimentation is twofold. First, due to higher transparency a partly UV-shielded molecular layer is shifted closer to the dense midplane. Second, the presence of big grains in the disk midplane delays the freeze-out of volatile gas-phase species such as CO there, while in adjacent upper layers the depletion is still effective. Molecular concentrations and thus column densities of many species are enhanced in the disk model with dust evolution, e.g., CO{sub 2}, NH{sub 2}CN, HNO, H{sub 2}O, HCOOH, HCN, and CO. We also show that time-dependent chemistry is important for a proper description of gas thermal balance.

  10. Late Pleistocene glacial fluctuations in Cordillera Oriental, subtropical Andes

    Science.gov (United States)

    Martini, Mateo A.; Kaplan, Michael R.; Strelin, Jorge A.; Astini, Ricardo A.; Schaefer, Joerg M.; Caffee, Marc W.; Schwartz, Roseanne

    2017-09-01

    The behavior of subtropical glaciers during Middle to Late Pleistocene global glacial maxima and abrupt climate change events, specifically in Earth's most arid low-latitude regions, remains an outstanding problem in paleoclimatology. The present-day climate of Cordillera Oriental, in arid northwestern Argentina, is influenced by shifts in subtropical climate systems, including the South American Summer Monsoon. To understand better past glacier-subtropical climates during the global Last Glacial Maximum (LGM, 26.5-19 ka) and other time periods, we combined geomorphic features with forty-two precise 10Be ages on moraine boulders and reconstructed paleo-equilibrium line altitudes (ELA) at Nevado de Chañi (24°S) in the arid subtropical Andes. We found a major glacial expansion at ∼23 ± 1.6 ka, that is, during the global LGM. Additional glacial expansions are observed before the global LGM (at ∼52-39 ka), and after, at 15 ± 0.5 and 12 ± 0.6 ka. The ∼15 ka glacial event was found on both sides of Chañi and the ∼12 ka event is only recorded on the east side. Reconstructed ELAs of the former glaciers exhibit a rise from east to west that resembles the present subtropical climate trajectory from the Atlantic side of the continent; hence, we infer that this climate pattern must have been present in the past. Based on comparison with other low-latitude paleoclimate records, such as those from lakes and caves, we infer that both temperature and precipitation influenced past glacial occurrence in this sector of the arid Andes. Our findings also imply that abrupt deglacial climate events associated with the North Atlantic, specifically curtailed meridional overturning circulation and regional cooling, may have had attendant impacts on low subtropical Southern Hemisphere latitudes, including the climate systems that affect glacial activity around Nevado de Chañi.

  11. Complex brittle deformation pattern along the Southern Patagonian Andes (Argentina)

    Science.gov (United States)

    Barberón, Vanesa; Sue, Christian; Ronda, Gonzalo; Ghiglione, Matías

    2016-04-01

    The Southern Patagonian Andes is located in the southern extreme of the Pacific subduction zone, where the Antartic oceanic plate sinks underneath South America. The history of the area begins with compression during Paleozoic, Jurassic extension associated to the rift and opening of the South Atlantic Ocean, then a sag stage in the Lower Cretaceous followed by a foreland phase as a result of plate tectonics (Ghiglione et al., 2016). The kinematic study is concentrated in the Argentinean foothills, between 46°40' and 48° SL. We measured around 800 fault planes and their striaes with the sense of movement in order to characterize the stress field. The software used to make the stress inversion were Tensor (Delvaux, 2011) and Multiple Inverse Method MIM (Yamaji et al., 2011). The stress field map was built with the results of the MIM. We present new data from 48 sites located in the northern sector of the Southern Patagonian Andes. The measurements were made in several rocks from Paleozoic to Lower Cretaceous, even though most were taken in pyroclastic jurassic rocks from El Quemado Complex. Paleostress tensors obtained are mostly strike-slip, although a 25% is normal and there are a few compresional. The pattern of faults found is complex. In some sites the tensor can be locally linked to satellite images and observations from the field or be related to a major thrust front. There is no clear correlation between the age and/or lithology with the tensor since the youngest rocks measured are Lower Cretaceous. Probably there are several generations of family faults connected to different and recent tectonic phases then the paleostress tensors might correspond to the latest tectonic events.

  12. Síndrome pulmonar por hantavirus Andes en Chile CARDIOPULMONARY SYNDROME DUE TO ANDES VIRUS IN CHILE

    Directory of Open Access Journals (Sweden)

    CONSTANZA CASTILLO H.

    2002-01-01

    Full Text Available Desde 1993 han ocurrido 204 casos de Síndrome Cardiopulmonar por Hantavirus (SCPH en Chile. Los brotes epidémicos comenzaron en el sur y avanzan hacia el norte del país. Los más afectados son varones jóvenes, obreros agrícolas o forestales. En Chile, el SCPH es causado por el virus Andes, cuyo reservorio es el Oligorizomys longicaudatus (ratón de cola larga, que se distribuye desde la III Región al sur. El cuadro clínico es similar al descrito en EE.UU., caracterizado por una fase prodrómica que simula un estado gripal o cuadro gastrointestinal febril y que agrava por la aparición de edema pulmonar agudo e inestabilidad hemodinámica (fase cardiopulmonar. Sin embargo, cursa con mayores alteraciones hemorragí-paras y compromiso renal. La mortalidad inicial fue sobre 50% y actualmente es de alrededor del 33,3%. La presente revisión incluye: historia de la enfermedad, reservorio, modos de transmisión, patogenia, cuadro clínico, diagnóstico, tratamiento y medidas de prevenciónSince 1993, 204 cases of Hantavirus cardiopulmonary syndrome (HCPS occurred in Chile. Epidemic began in the south and moved thereafter to the northern regions. The disease affected predominantly young males, who worked in agricultural labours or as timber workers. The HCPS in Chile is caused by the Andes virus. The reservoir is the wild rat Oligoryzomis longicaudatus distributed from the III to the XII Region. The clinical features are similar to those described for Sin Nombre Virus. The disease has a prodromal stage characterised by fever, muscular pain, with or without gastrointestinal manifestations, followed by the rapid onset of respiratory insufficiency and haemodynamic unstability. Andes virus courses more often with haemorrhagic disorders and overt renal failure, than Sin Nombre Virus. The initial mortality was over 50% and declined to 33,3% in the last year. History of hantavirus-diseases, reservoir, and mode of contagion, pathogenesis, clinical

  13. Las Órdenes religiosas en espacio urbano colonial - Mendoza (Argentina. El caso de la la Compañía de Jesús

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    Cirvini, Silvia A.

    2012-12-01

    Full Text Available The purpose of this article is to study the presence and the action of the regular clergy, in particular The Society of Jesus in Mendoza, which was a peripheral city and part of the Spanish empire in South America, from the urban history point of view. We recognize the Society of Jesus as a special and relevant character in Mendocinian colonial times because of the importance of their buildings and properties, their spatial location in the city and their connection with the community and the other members of the regular clergy. The Jesuits were the founders of the first school and the first public library. They were important providers of basic food such as beef and wheat, because they had an efficient network of productive establishments (farms, vineyards and mills devoted to agricultural and livestock farming. These farms were situated not only in the oasis of Mendoza but also in the Uco Valley (which is the oasis of the Tunuyán River.Este artículo propone abordar desde la perspectiva de la historia urbana, la presencia y la acción del clero regular, y en particular la Compañía de Jesús en Mendoza, ciudad periférica del Imperio español en el cono sur latinoamericano. Un recorrido de sus edificios y propiedades, su ubicación espacial en la ciudad, así como las conexiones con otros actores de la vida comunitaria y las otras órdenes religiosas nos permiten reconocer la manera en que la Compañía de Jesús se convirtió en un actor relevante del mundo colonial de Mendoza. Los jesuitas fueron los fundadores del primer colegio y la primera biblioteca pública que tuvo la ciudad, eran proveedores de alimentos básicos como la carne y el trigo ya que poseyeron una eficiente red de establecimientos productivos (haciendas, viñas y molinos dedicados a la actividad agrícola y ganadera, ubicados no sólo en el oasis del Río Mendoza sino también en el Valle de Uco (oasis del Río Tunuyán.

  14. An elusive new species of Marsupial Frog (Anura: Hemiphractidae: Gastrotheca from the Andes of northern Peru

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    William E. Duellman

    2013-06-01

    Full Text Available A new species of marsupial frog, genus Gastrotheca, is described from high-elevation grasslands in the Andes in Región Amazonas in northernPeru, where even calling males are well hidden in deep moss. The new species is distinguished from all congeners by its unique color pattern that includes a narrow, blackbordered, yellow middorsal stripe. The species apparently belongs to the Gastrotheca plumbea Group, which ranges in the Andes from northern Colombia to northern Peru.

  15. Glaciation and topographic evolution of the Central Patagonian Andes since 6 Ma

    Science.gov (United States)

    Christeleit, E. C.; Laemel, R.; De Wolf, W. E.; Shuster, D. L.; Brandon, M. T.

    2013-12-01

    New and existing thermochronological data are used to model glacial erosion and topographic evolution of the central Patagonian Andes (~47S) over the last 6 Ma. The modern Andes are cut by large valleys and fjords with local valley relief of at least 2.5 km. It is currently thought that a formerly uniformly high Andes was 'buzzed' down to the elevation of the equilibrium line altitude, presumably in the last 2 Ma concurrent with late Cenozoic global cooling. However, studies of glacial debris show that glaciers were present in Patagonia as early as 6 Ma. The extent of these early glaciations is unclear, but recent work suggests that glacial valleys in the central Patagonian Andes were carved at a steady rate beginning at 6 Ma, implying that valley incision may be an important process in the topographic evolution of glaciated mountain ranges, rather than cirque retreat. To understand how valley relief has formed in the Andes, we dated 30 samples from Steffen Fjord in Chile using apatite (U-Th)/He thermochronology. We use this new data and existing thermochronological data in the region to estimate the topographic form of the central Andes at 6 Ma and model how the valley relief has evolved since the initiation of glaciation using Pecube.

  16. Crustal deformation in the south-central Andes backarc terranes as viewed from regional broad-band seismic waveform modelling

    Science.gov (United States)

    Alvarado, Patricia; Beck, Susan; Zandt, George; Araujo, Mario; Triep, Enrique

    2005-11-01

    The convergence between the Nazca and South America tectonic plates generates a seismically active backarc region near 31°S. Earthquake locations define the subhorizontal subducted oceanic Nazca plate at depths of 90-120 km. Another seismic region is located within the continental upper plate with events at depths Sierras Pampeanas and is responsible for the large earthquakes that have caused major human and economic losses in Argentina. South of 33°S, the intense shallow continental seismicity is more restricted to the main cordillera over a region where the subducted Nazca plate starts to incline more steeply, and there is an active volcanic arc. We operated a portable broad-band seismic network as part of the Chile-Argentina Geophysical Experiment (CHARGE) from 2000 December to 2002 May. We have studied crustal earthquakes that occurred in the back arc and under the main cordillera in the south-central Andes (29°S-36°S) recorded by the CHARGE network. We obtained the focal mechanisms and source depths for 27 (3.5 Sierras Pampeanas, over the flat-slab segment is dominated by reverse and thrust fault-plane solutions located at an average source depth of 20 km. One moderate-sized earthquake (event 02-117) is very likely related to the northern part of the Precordillera and the Sierras Pampeanas terrane boundary. Another event located near Mendoza at a greater depth (~26 km) (event 02-005) could also be associated with the same ancient suture. We found strike-slip focal mechanisms in the eastern Sierras Pampeanas and under the main cordillera with shallower focal depths of ~5-7 km. Overall, the western part of the entire region is more seismically active than the eastern part. We postulate that this is related to the presence of different pre-Andean geological terranes. We also find evidence for different average crustal models for those terranes. Better-fitting synthetic seismograms result using a higher P-wave velocity, a smaller average S-wave velocity and a

  17. Política habitacional comparada: Mendoza y San Luis en el marco de la descentralización

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    Delia Palero

    2006-01-01

    Full Text Available El artículo plantea un análisis comparado entre las políticas habitacionales desarrolladas por dos provincias argentinas: Mendoza y San Luis. La federalización de los recursos del FONAVI en el país, ocurrida en l992, puso fin a una prolongada etapa de política habitacional centralizada en Argentina. El período analizado abarca la década comprendida entre ese año y el 2002. A nivel internacional se consolida el proceso de globalización que, en el terreno de la vivienda, se tradujo en el predominio del enfoque facilitador. Los casos elegidos representan dos modelos diametralmente distintos que, sin embargo, alcanzaron resultados que podrían calificarse de exitosos en el concierto nacional. Mientras el primero se inscribe en el paradigma central-sectorial, el segundo adhiere en forma predominante al enfoque facilitador. El análisis de política comparada ha sido contextualizado en los escenarios político, social, cultural y económico que le dieron marco, sentido y viabilidad a ambos modelos, que marcaron tanto sus fortalezas como sus debilidades y que explican los resultados alcanzados. Vinculación con la formación universitaria: La Cátedra Problemática de la Vivienda se encuentra en la Facultad de Ciencias Políticas y Sociales (U.N.Cuyo e incluye en su programa unidades referidas a política habitacional en Argentina y en la provincia de Mendoza. En tal sentido, se estima que los resultados obtenidos a partir de este trabajo resultan un insumo de interés para estudiantes de trabajo social, sociología y ciencia política, en tanto permiten analizar en profundidad conceptos como centralizacióndescentralización, participación, articulación de actores, focalización, eficiencia y eficacia en la gestión de la política habitacional, entre otros, y cómo éstos se manifiestan en la práctica política concreta.

  18. Fault spacing in the El Teniente Mine, Central Chile, the fold style inversion method, fold segmentation and fault linkage of the Barrancas/Lunlunta-Carrizal anticlinal complex, Mendoza, Argentina

    Science.gov (United States)

    Brooks, Benjamin Armstead

    1999-11-01

    An interval counting technique and standard cumulative statistics, in concert with residual and differential slope analysis, are employed on multiple parallel scanlines to test the applicability of fractal fault spacing at the El Teniente Mine, Central Chile. A negative exponential distribution best describes fault spatial distribution at the mine, while the interval counting method gives deceptively good fits to a fractal distribution. The results are consistent for the majority of the scanlines over thousands of square meters. These data provide an important counterexample to previously studied fractal spacing distributions and suggest that faulting is not a uniquely self-similar process and/or that faulting is not a consistently self-similar process through time. The "Fold Style Inversion" (FSI) method is developed to place quantitative bounds on balanced cross-sections used in the analysis of blind thrust faults. The method employs a discretized dip isogon construction, in combination with Monte Carlo simulations of seismic reflection depth-conversion errors, to assess a data sets' goodness of fit to bulk hangingwall similar or parallel fold geometry. This enables an objective choice to be made between the Arbitrarily Inclined Simple Shear (AISS) and Constant Bed Length (CBL) fault inversion routines which are specific to similar and parallel fold geometry, respectively. The method performs successfully for a variety of synthetic examples including a synthetic seismic line. The FSI method is applied to seismic reflection lines crossing the Barrancas and Lunlunta-Carrizal anticlines, active fault-bend folds in the Andean foreland of Mendoza Province, Argentina, and the proposed site of the 1985 Mw 5.9 Mendoza earthquake. For the Barrancas anticline, FSI analysis establishes a preference for similar fold style whereas no preference can be established for the Lunlunta-Carrizal anticline. With FSI-constrained cross-sections, it is shown that the earthquake most

  19. Coupled geohazards at Southern Andes (Copahue-Lanín volcanoes): Chile's GEO supersite proposal

    Science.gov (United States)

    Lara, Luis E.; Cordova, Loreto

    2017-04-01

    Southern Andes are a young and active mountain belt where volcanism and tectonic processes (and those related to the hydrometeorological conditions controlled by this geological setting) pose a significant threat to the growing communities nearby. This proposal focus on a ca. 200 km long segment of the Southern Andes where 9 stratovolcanoes and 2 distributed volcanic fields are located, just along a tectonic corridor defined by the northern segment of the Liquiñe-Ofqui Faul System (LOFS), a long-lived active strike-slip fault running for 1200 km. Volcanoes in this area take part of the central province of the Andean Southern Volcanic Zone (37-41°S), particularly the northermost portion that is limited at the south by an Andean tranverse fault (Lanalhue Fault, which define the Villarrica-Lanin volcanic chain) and run along the horse-tail array of the LOFS to the north. Most of the stravolcanoes are atop of the LOFS main branch with only 3 exceptions (Callaqui, Tolhuaca and Lanín) 15-20 km away, but related to transverse faults. Hazards in the segment derive from the activity of some of the most active volcanoes in South America (e.g., Villarrica, Llaima), others with long-lasting weak activity (e.g., Copahue) or some volcanoes with low frequency but high magnitude eruptions in the geological record. Only since the beggining of the 20th century 80 eruptions have been recorded in this area. In addition, activity of the LOFS has been detected prior to some eruptions and coeval with some others (e.g., Lonquimay 1989). A strong two-way coupling between tectonics and volcanism has been proposed for the segment but only recently detected by geophysical techniques or numerical modelling. Tectonic triggered landslides are frequent in this region together with debris flows at erupting ice-covered volcanoes or stream headed at high altitude basins. The latter scenario seems to be worst at present because of global climate change. Ground-based monitoring networks for both

  20. El “Estado Mamá”: estudio histórico del Acogimiento Familiar en Mendoza (Argentina/ The “Mother State”: a historical study of the Foster Care System in Mendoza (Argentina

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    Carolina Farias-Carracedo

    2017-04-01

    Full Text Available Este artículo es producto de una investigación que tuvo el objetivo de reconstruir el recorrido histórico de los primeros 20 años de existencia del programa “Amas Externas” en la ciudad de Mendoza (Argentina. La metodología corresponde a la categoría de estudios ex post facto retrospectivo, bajo un estudio de caso instrumental y en análisis del discurso de estos actores. Las unidades de análisis utilizadas han sido fuentes primarias documentales y orales (testimonios o informantes claves. El programa “Amas Externas” se inició en el año 1978 con el objetivo de brindar un espacio de albergue alternativo a las macro-instituciones (MI de niños, y consistía en seleccionar una mujer de la comunidad para que acogiera en su propio hogar un niño pequeño por un tiempo limitado. A pesar de las múltiples limitaciones del programa podría concluirse que constituyó una modalidad de albergue rupturista en relación a las MI.

  1. Geophysical studies applied to the exploration of the Aqua de las Liebres uranium deposit, Mendoza, Argentina; Estudios geofisicos en la exploracion de yacimientos de uranio Aqua de las Liebres, mendoza, Argentina

    Energy Technology Data Exchange (ETDEWEB)

    Pastore, Silvio Augusto; Rocco, Guillermo Felix E.; Ponti, Norberto [Instituto Sismologico F.S. Volponi (Argentina)

    1995-12-31

    The aim of this work was to apply a geophysical methodology, which let us make exploration studies of Uranium ore deposit, with good results and minimal costs. This technique will be used by the National Commission of Atomic Energy of Argentina (CNEA). This study was made at Agua de las Liebres site, Sierra Pintada-San Rafael-Mendoza, over an existing seismic path. Besides, there were three roles, digged up to the interesting level with a medium depth about 400 m. This investigation was made using the Vertical Electrical Sounding with a maximum AB = 3870 m. It could be used in the zone knowing that there were sub horizontal layered strata, with very important resistivity contrasts for its identification. The use of this methodology led us to obtain a more detailed knowledge of the existing geology, besides to take into account a helpful method, to increase the studied zones, optimizing ins such a way, the obtained results, found with another exploration techniques. (author). 4 refs., 4 figs., 4 tabs.

  2. The Cordon del Portillo Permian magmatism, Mendoza, Argentina, plutonic and volcanic sequences at the western margin of Gondwana

    Science.gov (United States)

    Gregori, Daniel; Benedini, Leonardo

    2013-03-01

    The Cerro Punta Blanca, Cerro Bayo and Cerro Punta Negra stocks, parts of the Cordillera Frontal Composite Batholith, cropping out in the Cordón del Portillo, records the Gondwana magmatic development of the Cordillera Frontal of Mendoza, in western Argentina. In this area, the San Rafael Orogenic phase, that represents the closure of the Late Carboniferous-Early Permian marine basins, begins at 284 Ma, and ceased before 276 Ma. The Cerro Punta Blanca, Cerro Bayo and Cerro Punta Negra stocks represent a post-orogenic magmatism and are equivalents to the Choiyoi Group. The Gondwana magmatic activity in the Cordón del Portillo area can be divided into two stages. The Cerro Punta Blanca stock (c.a. 276 Ma) represents an early post-orogenic, subduction-related magmatism similar to the basic-intermediate section of the Choiyoi Group (c.a. 277 Ma). The late post-orogenic second event was recorded by the Cerro Bayo (262 Ma) and Cerro Punta Negra stocks which represent a transition between subduction-related and intra-plate magmatism. This event represents the intrusive counterpart of the acidic facies of the upper section of the Choiyoi Group (c.a. 273 Ma). This extensional condition continued during the Triassic when the Cacheuta basin developed.

  3. Biodiversidad y TIC: experiencia de capacitación virtual para profesores de secundaria en la provincia de Mendoza, Argentina.

    Directory of Open Access Journals (Sweden)

    Gabriela Diaz Isenrath

    2015-12-01

    Full Text Available Educar para el conocimiento y conservación de la biodiversidad es complejo. Entre las numerosas estrategias didácticas disponibles, el uso de las TIC puede ser una poderosa herramienta para los procesos de enseñanza-aprendizaje. El curso virtual “Biodiversidad y TIC” se ofreció a través del portal educativo de la provincia de Mendoza, Argentina. Este fue parte de los cursos ofrecidos para la formación continua y permanente de docentes de secundaria. Los objetivos planteados fueron: generar una espacio de reflexión crítica sobre el uso de las TIC en la construcción de conceptos relacionados a la biodiversidad; brindar herramientas y materiales que promuevan actualización y contextualización regional de ideas centrales sobre la biodiversidad y su conservación y promover la innovación pedagógica. Se presenta la experiencia, su marco teórico, la organización del curso, los contenidos seleccionados y las estrategias utilizadas. Luego se analiza el proceso ocurrido en el aula virtual, y se plantean los logros y dificultades encontradas. Se proponen mejoras a implementar basadas en esta primera experiencia.

  4. Fission-track dating of the punta de vacas glaciation in the Rı´o Mendoza valley, Argentina.

    Science.gov (United States)

    Espizua, L. E.; Bigazzi, G.

    Fission-track dating of three tephra samples related to mappable drifts and non-glacial sediments, including alluvium, in the Rı´o Mendoza valley, Argentina, places limiting ages on the oldest two glacial events. A tephra-layer interstratified with fan alluvium that surrounds and cuts the outermost Uspallata moraine has an age of 170,000±50,000 yr, implying that the drift predates marine oxygen isotope stage (OIS) 6. A tephra dated at 134,000±32,000 yr, that was deposited on alluvial fan sediments, underlies Punta de Vacas drift, which is inferred to equate with Isotope Stage 6. The Punta de Vacas outwash, which likely correlates with the Rı´o Colorado drift, overlies another tephra unit that dates to 260,000±150,000 yr. Although the error limits of the dates preclude definitive correlations, all three tephra units may have been deposited during an interval prior to the maximum advance of the Punta de Vacas glaciation during OIS 6 or maybe in the Stage 7 interglacial period.

  5. Health and working conditions of high school and university teachers in Mendoza: between commitment and emotional distress

    Directory of Open Access Journals (Sweden)

    Patricia Alejandra Collado

    2016-06-01

    Full Text Available Con el objetivo de analizar los aspectos vinculados con la percepción sobre las condiciones de trabajo y su impacto en la salud de los docentes que pertenecen a la Universidad Nacional de Cuyo (UNCuyo, Mendoza, Argentina, este artículo analiza los resultados del Primer Censo de Condiciones y Salud Laboral, realizado a fines del año 2013, en dos unidades académicas (una de enseñanza media y otra de nivel universitario que abarcó a 193 docentes. El sondeo se dedicó a caracterizar el plantel de trabajadores/as y las condiciones que afectan su salud, principalmente en sus aspectos psicosociales, para lo cual se aplicó un cuestionario autoadministrado, cuyas dimensiones fueron debatidas en talleres de sensibilización con docentes que colaboraron en la preparación del instrumento de recolección. Entre sus principales resultados emerge el desgaste físico y emocional de trabajadores altamente calificados, por el efecto combinado de la respuesta comprometida a las exigencias de su labor con la degradación (material y simbólica de las condiciones en que la desempeña.

  6. Flujos de detritos recientes en la cordillera frontal de Mendoza: Un ejemplo de riesgo natural en la ruta 7

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    Emmanuel Wick

    2010-06-01

    Full Text Available Se expone un estudio sobre los flujos de detritos ocurridos en enero de 2005, en el km 1.118,5 de la ruta nacional 7 en la provincia de Mendoza. La zona se ubica en la Cordillera Frontal, próxima al límite con la Precordillera. Se realizó un mapa geomorfológico detallado, sobre la base de una imagen Quickbird del año 2006. Además, se hicieron cálculos de volúmenes, velocidades y caudales, con mediciones en el campo y con ayuda de un sistema de información geográfico (SIG. El estudio de la geomorfología permitió proponer tres escenarios para el caso de un nuevo evento, a partir de los cuáles se creó un mapa de susceptibilidad a los flujos de detritos para el tramo de ruta analizado. Finalmente, se proponen medidas de protección y de mitigación ante la posibilidad de recurrencia de estos eventos en el sector.

  7. Análisis del campo de esfuerzos en una secuencia lacustre de Precordillera oriental, San Juan-Mendoza

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    Laura P. Perucca

    2008-06-01

    Full Text Available En la quebrada del río Acequión, ubicada en el sur de la provincia de San Juan y norte de Mendoza (32º 10' S, en el centrooeste argentino, se efectuó el análisis de las fallas que afectan depósitos lacustres de edad holocena. Estas fallas se encuentran asociadas a estructuras de licuefacción y avalanchas de roca indicadoras de paleoterremotos, lo que permite extender el registro sísmico de la región hasta el Holoceno temprano. Al comparar el campo de esfuerzos regional actual (determinado por sismicidad instrumental, con el cálculo del mecanismo focal de los terremotos recientes ocurridos en la región con el campo de esfuerzos local, se observó que mientras el primero se caracteriza por la compresión, el campo local de la secuencia lacustre es extensional. Esto indicaría que aunque el esfuerzo regional actual es compresivo y de dirección NE-SO debido a la convergencia entre las placas de Nazca y Sudamérica, el antiguo lago adosado a las sierras de Pedernal y Los Pozos, está afectado por fallas normales, principalmente debido a esfuerzos locales distensivos originados por el reacomodamiento de estos depósitos durante el levantamiento de las zonas montañosas aledañas.

  8. Organización territorial urbana y transporte público masivo: Metrópolis del Gran Mendoza

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    María Emilia García Schilardi

    2015-04-01

    Full Text Available Existe acuerdo entre los expertos en transporte, planificación y urbanismo que la movilidad urbana es consecuencia de la organización espacial que adopta la ciudad y viceversa. Es decir, existe una estrecha relación entre las políticas de transporte y el ordenamiento del territorio. El objetivo de este trabajo es caracterizar la relación existente en la actualidad entre la organización territorial urbana de la zona del Gran Mendoza y el sistema de transporte masivo que opera en ella. Se estudia, particularmente, la existencia o no de las condiciones urbanas que propenden al uso del transporte masivo, ya que se considera que éste es de fundamental importancia para el desarrollo sustentable de las ciudades. Con este fin se utiliza el modelo conceptual de ciudades orientadas al transporte masivo, propuesto por Julio Pozueta (2000, y se aplica al caso en estudio. Se revisan también trabajos de otros autores tanto los referidos a la zona analizada, como aquellos de carácter más general que dan luz sobre las tendencias urbanas en el mundo y en particular en las ciudades de Latinoamérica.

  9. Caracterización y evolución metamórfica de las rocas ultramáficas de la faja del río de las Tunas, Cordillera Frontal de Mendoza Characteristics and metamorphic evolution of the ultramafic rocks from Río de Las Tunas Belt, Frontal Cordillera of Mendoza.

    Directory of Open Access Journals (Sweden)

    M. Florencia Gargiulo

    2011-12-01

    penetrativa de los cuerpos ultramáficos, dando lugar a verdaderas serpentinitas. El posterior aumento en la proporción de CO2 del fluido mineralizante, inhibe la cristalización de Srp y da lugar a la cristalización conspicua de Tlc concentrado en estas zonas de cizalla, acompañado localmente por la presencia de carbonato.The goal of this contribution is to present the petro-mineralogical and chemical study of metaperidotites and serpentinites from the río de Las Tunas belt in Frontal Cordillera, Mendoza province. The metaperidotites preserve relictic magmatic minerals Ol, Cpx, (brownish-redSpls.l., scarce Opx with different modal proportions allowing to define the ultramafic protoliths: dunites, spinel-dunites, clinopyroxenitic-dunites, wehrlites, olivine-clinopyroxenites and clinopyroxenites. The crystallization sequence Srp+Mgt(±Brc±Chl→Tr±Tlc→�}Athà±(greenSpls.s./Ple±Opx evidence the metamorphic evolution of the ultramafic rocks. The initial serpentinization with pseudomorphic textures is followed by prograde metamorphism reaching the transition between the upper amphibolite facies and the granulite facies conditions. A second serpentinization process is evidenced by pseudomorphic textures after Amp and Chl and non-pseudomorphic and recrystallization textures, in agreement with the sequence a FeChrà→CrMgt→àMgt and b Spls.s./Ple(greenàMgt, which altogether indicate the low grade conditions during the retrogressive stage. During this stage reaction zones at metaperidotite-schist, -gneiss or -orthoamphibolite interfaces also were developed due to metasomatism between these lithologies. At the same time, local but pervasive carbonatization of the ultramafics near carbonatic levels of the Guarguaráz Complex took place. The emplacement of gondwanic igneous bodies in the study area occurred during the final stage of the metamorphic cycle. This magmatic event provides the physic-chemical conditions to allow elements mobilization, minerals concentration

  10. Fray Domingo de Mendoza y el convento de San Pedro Mártir de Las Palmas. Una aproximación historiográfica = Domingo de Mendoza and the convent of San Pedro Mártir de Las Palmas. A historiographical approach

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    Barrado Barquilla, José

    2016-01-01

    Full Text Available Resumen: Este nuevo estudio sobre los dominicos en Canarias, el segundo de los que hemos publicado hasta ahora, se centra en la figura de fray Domingo de Mendoza, uno de los principales artífices de la implantación de la Orden en el Nuevo Mundo (América y principalmente en las Islas Canarias, de cuyo convento de Las Palmas de Gran Canaria fue el fundador = Abstract: This new study on the Dominicans in the Canary Islands, the second we have published until now, it focuses on the figure of fray Domingo de Mendoza, one of the main architects of the implantation of the Order in the New World (America and principally in the Canary Islands, whose Las Palmas de Gran Canaria convento, was the founder.

  11. VER Y SER VISTO: METÁFORA DE LA MIRADA EN EL PERRO DE ESCRIBANA, DE MARÍA LUISA MENDOZA It sees and is seen: scopic metaphor in El perro de la escribana by María Luisa Mendoza

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    Mariana Libertad Suárez

    2011-12-01

    Full Text Available Este artículo propone una lectura de la novela El perro de la escribana (1982 de María Luisa Mendoza, un texto donde la arbitrariedad y la voluntad del sujeto --o, lo que es lo mismo, “su mirada”-- se establecerán como herramientas básicas para arraigar las identidades nacionales, culturales y de género. Por lo mismo, el valor del pasado, así como el de los discursos asociados al mismo, dependerá únicamente de la autoridad simbólica de quienes los enuncien.This article proposes an analysis of the novel “El perro de la escribana” (1982 by Maria Luisa Mendoza, a text in which arbitrary and subject’s gaze will become basic tools where national, cultural and gender identities take root. In this book, its past depends only on the symbolic authority of those speeches outlining the memory.

  12. Into the Andes: multiple independent colonizations drive montane diversity in the Neotropical clearwing butterflies Godyridina.

    Science.gov (United States)

    Chazot, Nicolas; Willmott, Keith R; Condamine, Fabien L; De-Silva, Donna Lisa; Freitas, André V L; Lamas, Gerardo; Morlon, Hélène; Giraldo, Carlos E; Jiggins, Chris D; Joron, Mathieu; Mallet, James; Uribe, Sandra; Elias, Marianne

    2016-11-01

    Understanding why species richness peaks along the Andes is a fundamental question in the study of Neotropical biodiversity. Several biogeographic and diversification scenarios have been proposed in the literature, but there is confusion about the processes underlying each scenario, and assessing their relative contribution is not straightforward. Here, we propose to refine these scenarios into a framework which evaluates four evolutionary mechanisms: higher speciation rate in the Andes, lower extinction rates in the Andes, older colonization times and higher colonization rates of the Andes from adjacent areas. We apply this framework to a species-rich subtribe of Neotropical butterflies whose diversity peaks in the Andes, the Godyridina (Nymphalidae: Ithomiini). We generated a time-calibrated phylogeny of the Godyridina and fitted time-dependent diversification models. Using trait-dependent diversification models and ancestral state reconstruction methods we then compared different biogeographic scenarios. We found strong evidence that the rates of colonization into the Andes were higher than the other way round. Those colonizations and the subsequent local diversification at equal rates in the Andes and in non-Andean regions mechanically increased the species richness of Andean regions compared to that of non-Andean regions ('species-attractor' hypothesis). We also found support for increasing speciation rates associated with Andean lineages. Our work highlights the importance of the Andean slopes in repeatedly attracting non-Andean lineages, most likely as a result of the diversity of habitats and/or host plants. Applying this analytical framework to other clades will bring important insights into the evolutionary mechanisms underlying the most species-rich biodiversity hotspot on the planet.

  13. Influence of the Andes Mountains on South American moisture transport, convection, and precipitation

    Energy Technology Data Exchange (ETDEWEB)

    Insel, Nadja; Poulsen, Christopher J. [University of Michigan, Department of Geological Sciences, Ann Arbor, MI (United States); Ehlers, Todd A. [University of Michigan, Department of Geological Sciences, Ann Arbor, MI (United States); Universitaet Tuebingen, Institut fuer Geowissenschaften, Tuebingen (Germany)

    2010-12-15

    Mountain ranges are known to have a first-order control on mid-latitude climate, but previous studies have shown that the Andes have little effect on the large-scale circulation over South America. We use a limited-domain general circulation model (RegCM3) to evaluate the effect of the Andes on regional-scale atmospheric dynamics and precipitation. We present experiments in which Andean heights are specified at 250 m, and 25, 50, 75, and 100% of their modern values. Our experiments indicate that the Andes have a significant influence on moisture transport between the Amazon Basin and the central Andes, deep convective processes, and precipitation over much of South America through mechanical forcing of the South American low-level jet (LLJ) and topographic blocking of westerly flow from the Pacific Ocean. When the Andes are absent, the LLJ is absent and moisture transport over the central Andes is mainly northeastward. As a result, deep convection is suppressed and precipitation is low along the Andes. Above 50% of the modern elevation, a southward flowing LLJ develops along the eastern Andean flanks and transports moisture from the tropics to the subtropics. Moisture drawn from the Amazon Basin provides the latent energy required to drive convection and precipitation along the Andean front. Large northerly moisture flux and reduced low-level convergence over the Amazon Basin leads to a reduction in precipitation over much of the basin. Our model results are largely consistent with proxy evidence of Andean climate change, and have implications for the timing and rate of Andean surface uplift. (orig.)

  14. Large slope failures in the La Paz basin, Bolivian Andes

    Science.gov (United States)

    Roberts, N. J.; Hermanns, R. L.; Rabus, B.; Guzmán, M. A.; Minaya, E.; Clague, J. J.

    2014-12-01

    The La Paz basin in the eastern Bolivian Andes has been a hotspot for large-scale, deep-seated gravitational slope deformation during the Holocene. In less than 2 Ma, a network of steep-sided valleys up to 800 m deep formed in sediments of the Altiplano Plateau and underlying basement rocks. We characterize the distribution, extent, mechanisms, and modern activity of large-scale failures within this landscape using optical image interpretation, existing geologic maps, synthetic RADAR interferometry (InSAR), and field investigation. Deposits of nearly 20 landslides larger than 100 Mm3 occur within the basin. Most failures have occurred in weakly lithified Late Miocene to Pliocene sedimentary rocks and include earth flows, translational and rotational landslides, and plug flows. Failures in underlying tectonized Paleozoic sedimentary rocks include bedding-parallel rockslides. The largest failure is the 3 km3 Achcocalla earth flow (ca. 11 ka BP), which ran out ~20 km. Other dated events span the period from the early Holocene to nearly the Colonial historic period. InSAR results show that many large slope failures, including the Achocalla earth flow, are currently moving at rates of a few centimeters to a few decimeters per year. Rapid deposition, shallow burial, and rapid incision of the basin fills produced steep slopes in weak geologic materials that, coupled with groundwater discharge from the valley walls, are the primary controls on instability. In contrast, the Altiplano surface has changed little in 2 Ma and the adjacent slopes of the Cordilleran Real, although steep, are relatively stable. Of the over 100 landslides that have occurred in the city of La Paz since the early twentieth century, most are at the margins of large, deep-seated prehistoric failures, and two of the most damaging historic landslides (Hanko-Hanko, 1582; Pampahasi, 2011) were large-scale reactivations of previously failed slopes. Improved understanding of large, deep-seated landslides in

  15. Geochemical variations in the Quaternary Andean back-arc volcanism, southern Mendoza, Argentina

    Science.gov (United States)

    Espanon, Venera R.; Chivas, Allan R.; Kinsley, Leslie P. J.; Dosseto, Anthony

    2014-11-01

    The Payenia Basaltic Province (PBP) is located 450 km east of the Chile-Peru trench in central west Argentina, behind the Andean arc front, constituting the back-arc. In order to evaluate the influence of the subducting slab as well as the magmatic source of this region, two volcanic fields located at comparable distance to the trench, having abundant basaltic products and similar eruptive timeframes were chosen. The Llancanelo (LLVF) and the Payún Matrú (PMVF) volcanic fields are part of the PBP and exhibit abundant basaltic activity during the Pleistocene. The geochemical data suggest that the LLVF has some arc signatures which have been described as weak as they are not as pronounced as in the Andean arc. The weak arc signature is not derived from slab dehydration as high Th enrichment relative to U cannot be explained by this process. We relate the Th enrichment as well as the lack of large residual garnet signatures, to slab sediments in the source. In the case of the PMVF, no arc signature has been inferred despite being only 30 km south of the LLVF. However the PMVF has a composition similar to that of the local intraplate end member, represented by the Rio Colorado volcanic field. The two volcanic fields, LLVF and PMVF, show indications of lower crustal assimilation as they trend towards the lower continental crust end member in Nb/U vs Ce/Pb and Nb/Yb vs Th/Yb diagrams. The geochemical differences between the LLVF and the PMVF as well as between several volcanic fields are illustrated using spatial distribution maps of geochemical ratios. Using this new approach, the decrease in arc signature can be traced in the back-arc and the higher enrichment in high field strength elements (HFSE) relative to large ion lithophile elements (LILE) in the PMVF compared to the LLVF is explicitly shown. These geospatial maps provide a graphical manner to illustrate the presence of two distinct types of volcanism (OIB-like and arc-like) occurring in the same Quaternary

  16. Facies analysis of a Toarcian-Bajocian shallow marine/coastal succession (Bardas Blancas Formation) in northern Neuquén Basin, Mendoza province, Argentina

    Science.gov (United States)

    Bressan, Graciela S.; Kietzmann, Diego A.; Palma, Ricardo M.

    2013-04-01

    Strata of the Bardas Blancas Formation (lower Toarcian-lower Bajocian) are exposed in northern Neuquén Basin. Five sections have been studied in this work. Shoreface/delta front to offshore deposits predominate in four of the sections studied exhibiting a high abundance of hummocky cross-stratified, horizontally bedded and massive sandstones, as well as massive and laminated mudstones. Shell beds and trace fossils of the mixed Skolithos-Cruziana ichnofacies appear in sandstone beds, being related with storm event deposition. Gravel deposits are frequent in only one of these sections, with planar cross-stratified, normal graded and massive orthoconglomerates characterizing fan deltas interstratified with shoreface facies. A fifth outcrop exhibiting planar cross-stratified orthoconglomerates, pebbly sandstones with low-angle stratification and laminated mudstones have been interpreted as fluvial channel deposits and overbank facies. The analysis of the vertical distribution of facies and the recognition of stratigraphic surfaces in two sections in Río Potimalal area let recognized four transgressive-regressive sequences. Forced regressive events are recognized in the regressive intervals. Comparison of vertical distribution of facies also shows differences in thickness in the lower interval among the sections studied. This would be related to variations in accommodation space by previous half-graben structures. The succession shows a retrogradational arrangement of facies related with a widespread transgressive period. Lateral variation of facies let recognize the deepening of the basin through the southwest.

  17. Geochemical and isotopic constraints on the petrogenesis of the Puesto La Peña undersaturated potassic complex, Mendoza province, Argentina: Geodynamic implications

    Science.gov (United States)

    Zappettini, Eduardo O.; Villar, Luisa M.; Hernández, Laura B.; Santos, João O.

    2013-03-01

    Major and trace element and radiogenic and stable isotope data are reported for the Miocene Puesto La Peña undersaturated potassic complex, located in the Argentine Precordillera. The complex is composed of a pyroxenite core surrounded by a malignite-borolanite association, followed by radial and ring dikes composed of alkaline lamprophyres, tephrite to phonolite and intermediate varieties, porphyritic microledmorite, benmoreite, alkaline trachyte and a swarm of ultrabasic ouachitite dikes. Late trachytic to phonolitic volcanic necks and associated dikes crop out surrounding the malignitic-borolanitic massif. Major and trace element data are consistent with their derivation by partial melting from an enriched, probably lithospheric, metasomatized heterogeneous mantle involving spinel- and garnet-facies mantle sources. The trace element and isotope data indicate that all rock types are derived from a common parental magma and are thus cogenetic. Sr, Nd and Pb variations in the different studied lithologies are restricted, except for the evidence of Sr decoupling in the ouachitite samples. Their Sr-Nd isotope compositions follow the "mantle array" defined by oceanic basalts, within the OIB field, consistent with an intraplate depleted source. The genesis of the ouachitite is interpreted to be related to mixing between asthenospheric magma and melts from the lower lithosphere consisting of K-rich metasomatic layers. The Dupal like Pb isotopes signature suggests a mantle modification by introduction of continental crust material in the upper mantle; this is consistent with the Sr-Nd isotope data from the late silica-undersaturated felsic dikes and volcanic necks. Multistage mantle extraction would have occurred by the end of Neoproterozoic to lower Paleozoic times as indicated by the isotopic data. Partial melting was initiated by mantle upwelling decompression during lithosphere extension. Back-arc extensional conditions during the latest Early Miocene (19 Ma), related to the geometry of the Pacific subducted plate beneath the South American plate, favored the tectonic conditions for magma ascent from a magmatic reservoir located at around 30 km depth in the crust. A fractional crystallization process, primarily of clinopynoxene, plagioclase, alkali feldspar, nepheline and lesser biotite, magnetite, and apatite, first yielded the cumulate clinopyroxenite, followed by the malignite-borolanite association and the late dikes and volcanic necks. The morphology of the complex, as well as the relationship between their different facies, points to a cauldron subsidence model of emplacement.

  18. Conflictos sociales en Mendoza entre dos crisis, 1890-1916: Una larga lucha de los trabajadores por la conquista de sus derechos laborales

    Directory of Open Access Journals (Sweden)

    Rodolfo Richard-Jorba

    2010-06-01

    Full Text Available Este artículo contribuye a la reconstrucción de la historia del mundo de los trabajadores en Mendoza. Las fuentes revisadas y la sistematización de información dispersa han permitido profundizar en los conocimientos hasta ahora generados, sacando a luz una parte significativa del desarrollo capitalista centrado en la agroindustria vitivinícola. Las fuentes principales para seguir los conflictos han sido los diarios mendocinos, por lo que nuestro abordaje constituye una aproximación que esperamos poder ampliar en el futuro. En este artículo presentamos los conflictos sociales en el contexto de períodos de crisis y de auge económico. Comenzamos por la crisis de 1890 y concluimos con la crisis provocada por la Primera Guerra Mundial y los cambios políticos que sobrevendrían a partir de 1916-1918This article contributes to reconstructing the history of the world of labour in Mendoza. The revision of sources and the systematization of the scattered information available resulted in a deeper insight on the subject and a better understanding of capitalist development based on vitivicultural agroindustry. Articles from Mendoza newspapers have been the main historical sources used to follow these conflicts, and are expected to be widened in future investigations. Currently, social troubles are presented in a context of a period of economic growth and crisis. We start with the crisis of 1890, to conclude with the World War I crisis and the political changes that would come after 1916-1918

  19. Paleomagnetism of Permian and Triassic rock, central Chilean Andes

    Science.gov (United States)

    Forsythe, Randall D.; Kent, Dennis V.; Mpodozis, Constantino; Davidson, John

    The first paleomagnetic data from Permian and Triassic formations west of the Andean divide are presented. Four formations of Permian or Triassic age in the central Chilean Andes have been investigated: two are located in the coastal ranges, and two are in the main cordillera. Of the formations in the main cordillera (Pastos Blancos and Matahuaico formations), only the Pastos Blancos Formation has yielded characteristic directions. While a fold test is absent, magnetizations are most likely secondary and yield pre-tilt corrected concordant inclinations, but yield declinations discordant 30° clockwise in comparison to the South American apparent polar wander path. Both formations from the coastal ranges (Cifuncho and Pichidangui formations) yielded stable directions. Postfolding magnetizations in the Cifuncho Formation also show declinations discordant 30° clockwise and concordant inclinations. The Pichidangui Formation has two stable components: one of postfolding age is concordant to apparent polar wander path data, and one of probable prefolding (Late Triassic) age is concordant in declination, but discordant in inclination. Further work is needed to better define the prefolding magnetizations in the Pichidangui Formation, but at present these preliminary results are the first paleomagnetic signs of displaced terranes along the Pacific margin of Chile. If correct, the results suggest that the Pichidangui Formation was some 15° of latitude farther south during the Late Triassic and had likely moved northward to its present latitudinal position with respect to cratonic South America by Middle to Late Jurassic.

  20. Gravity modelling of the Ramadas Caldera (Argentinean Puna, central Andes)

    Energy Technology Data Exchange (ETDEWEB)

    Casas, A. [Barcelona Univ. (Spain). Facultad de Geologia; Hernandez, E.; Marti, J. [Consejo Superior de Investigaciones Cientificas, Barcelona (Spain). Inst. de Ciencias de la Terra Jaume Almera; Petrinovic, I. [Universidad Nacional de Salta (Argentina)

    1995-12-31

    In order to identify and characterize the event area of abundant Upper Miocene proximal rhyolitic pyroclastic deposits and extrusive domes which concentrate in the Ramadas area, near Sant`Antonio de los Cobres (Salta) at the Puna Altiplano (Central Andes), a detailed gravity survey has been carried out. Regional Bouguer gravity data were augmented with new 173 gravity observations measured sufficiently close-spaced to resolve the short wavelength produced by the structure of interest. Besides, the geophysical survey was done in conjunction with geologic and geochemical studies which were critically important to our interpretation. After the separation of the regional trend, the residual anomaly map displays a circular gravity low reaching-80 m Gal centered over scarce outcrops of rhyolitic and pyroclastic. This gravity low is interpreted as produced by block subsidence along ring fractures during eruption and/or deflation of the chamber. As the accumulation of thick, low density rock types in the zone of collapse is responsible of the prominent negative gravity anomalies, them has been used to estimated the thickness of caldera infill. (author). 8 refs., 4 figs

  1. The Grenville-age basement of the Andes

    Science.gov (United States)

    Ramos, Victor A.

    2010-01-01

    The analysis of the basement of the Andes shows the strong Grenville affinities of most of the inliers exposed in the different terranes from Colombia to Patagonia. The terranes have different histories, but most of them participated in the Rodinia supercontinent amalgamation during the Mesoproterozoic between 1200 and 1000 Ma. After Rodinia break-up some terranes were left in the Laurentian side such as Cuyania and Chilenia, while others stayed in the Gondwanan side. Some of the terranes once collided with the Amazon craton remained attached, experiencing diverse rifting episodes all along the Phanerozoic, as the Arequipa and Pampia terranes. Some other basement inliers were detached in the Neoproterozoic and amalgamated again to Gondwana in the Early Cambrian, Middle Ordovician or Permian times. A few basement inliers with Permian metamorphic ages were transferred to Gondwana after Pangea break-up from the Laurentian side. Some of them were part of the present Middle America terrane. An exceptional case is the Oaxaquia terrane that was detached from the Gondwana margin after the Early Ordovician and is now one of the main Mexican terranes that collided with Laurentia. These displacements, detachments, and amalgamations indicate a complex terrane transfer between Laurentia and Gondwana during Paleozoic times, following plate reorganizations and changes in the absolute motion of Gondwana.

  2. [Medical education at Universidad de los Andes, Santiago, Chile].

    Science.gov (United States)

    Orrego Vicuña, F

    1997-07-01

    Universidad de los Andes School of Medicine started in 1991 with a new medical curriculum aimed at providing a medical education for its students, that is, it attempts to give, together with technical proficiency in medical matters, formation of character and a strong ethical attitude. The curriculum lasts for seven years: five of basic, pre-clinical and clinical theoretical and practical courses, followed by two years of internships in Internal Medicine, Surgery, Obstetrics and Pediatrics, plus a four month period of an elective internship. The courses have an integrated design, in which each matter is presented from multiple perspectives, e.g. in Internal Medicine together with the clinical aspects of disease, the pathophysiology and the pharmacology of the drugs used are presented. Also the Pathology of each disease is given in coordination in the Pathology course. General educational matters such as Anthropology, Psychology, Origin of Living Beings, Theology and Medical Ethics are interspersed in the curriculum. An important feature is the personal counselling system, in which each student may choose an academic counsellor and discuss with him (her) the subjects of his choosing. Clinical practice is given in a system that includes five hospitals and five private clinics that range from general medical practice to Psychiatry or Ophthalmology.

  3. Meteorological Conditions of Floods In The Chilean Andes Mountains

    Science.gov (United States)

    Vergara, J.

    Catastrophic floods occurred on mountains River during 2000 and 2001. The meteo- rological conditions of flood during the last five years have analyzed. For example, the flood of June 29 of 2000 occurred after one of extremely wettest June of the last 40 years were snowfall was 991cm in the Aconcagua Valley. Infrequently storms activ- ity generated a huge snowfall and rainfall over the Andes mountains on June of 2000 (1525mm in El Maule Valley) and the end of the unusually period, the flood was trig- gered by rising temperatures on the mountains and heavy rain (199mm in 24 hours) fall over the fresh snow on the morning of June 29 and floods wave developed and moved down along of the all river located on Central part of Chile, the foods peak was 2970.5m3/s on the El Maule basin in the morning of June 29. The regional meteoro- logical models with the hydrological forecasting was used for alert of the floods.

  4. A sorte da carne. Topologia animal nos Andes meridionais

    Directory of Open Access Journals (Sweden)

    Francisco Pazzarelli

    Full Text Available Resumo: Este artigo apresenta uma análise etnográfica das relações estabelecidas durante a matança e as carneadas de animais de criação em uma comunidade aborígine do noroeste da Argentina, na região dos Andes meridionais. Argumenta-se que a topologia que se exprime a partir desses processos expõe os modos em que o espíritu (ou ánimu dos animais e a relação de sorte que eles compartilham com os pastores devem ser tirados para fora dos corpos, na tentativa de transformá-los em carne comestível. Assim, as operações de separar, dobrar e envolver, junto com o processo de desidratação, tornam-se relevantes na hora de compreender as relações entre distintos corpos e as conexões potenciais entre diferentes lados do mundo.

  5. Bofedales: high altitude peatlands of the central Andes Bofedales: turberas de alta montaña de los Andes centrales

    Directory of Open Access Journals (Sweden)

    FRANCISCO A SQUEO

    2006-06-01

    Full Text Available There is an exceptional group of alpine peatlands in the world situated in the arid grasslands of the central Andes. The peatlands in northern Chile occur in the most arid part of their range. Members of the Juncaceae are the primary peat-forming plant species. Fresh and mildly saline groundwaters originate from glaciers, snowmelt and rain are the water sources for the northern Chile peatlands. Paleoecological investigations suggest that some peatlands are recent features of the landscape having developed within the last three thousand years or less. These peatlands are unique, extremely fragile water features sensitive to climate changes and human disturbances such as regional mining activity. Much more work is required to develop scientifically based sound management and conservation programs for the rare plants and animals that live in them and to ensure the future livelihoods of the indigenous peoples who depend on themExiste un grupo excepcional de turberas (bofedales de alta montaña en el mundo situados en la estepa árida de los Andes centrales. Los bofedales en el norte de Chile están presentes en la parte más árida de su rango. Las principales especies de plantas responsables de la formación de turba corresponden a miembros de Juncaceae. El agua fresca y medianamente salina de los bofedales proviene de agua subterránea asociada a riachuelos proveniente de glaciares, derretimiento de nieve y lluvia. Investigaciones paleoecológicas sugieren que algunos bofedales son integrantes recientes del paisaje, habiéndose desarrollado durante los últimos tres mil años o menos. Estos bofedales son entidades únicas, extremadamente frágiles por su dependencia del agua, sensibles a los cambios climáticos y vulnerables a la alteración humana tal como la actividad minera en la región. Se requiere mucho más trabajo para desarrollar programas de manejo y conservación, con sólidas bases científicas, de las plantas y animales que viven en

  6. Linchamientos y conflicto político en Los Andes Lynchings and Political conflict in The Andes

    Directory of Open Access Journals (Sweden)

    Carlos M. Vilas

    2007-06-01

    Full Text Available En 2004, los alcaldes de dos municipalidades de la región aimara de los Andes fueron linchados en la aparente culminación de agudos conflictos políticos internos y entre las respectivas comunidades y el Estado central. En este artículo se discuten ambos casos con el fin de ilustrar las transformaciones experimentadas en años recientes en la organización y la dinámica interna de las comunidades andinas, y de la articulación conflictiva de la política local en los procesos e instituciones de más amplio alcance. Precariedad social e incapacidad o renuencia del Estado para responder con eficacia a demandas básicas de determinados grupos de población configuran enmarcamientos socioeconómicos e institucionales de los linchamientos. En contraste con enfoques que enfatizan en factores culturales tradicionales o en un supuesto nacionalismo indígena, en el artículo se destaca la gravitación de fenómenos y procesos político- institucionales recientes en la transformación cultural y política de las comunidades, en el modo en que éstas procesan sus conflictos internos y con el Estado central.In 2004, two municipalitys mayors form the aimara Andes of Peru and Bolivia were subjected to mass lynchings as a result of the apparent culmination of violent political confrontations. This paper deals with these events as dramatic illustrations of the transformations the Andean communities experienced during recent decades in their internal dynamics, as well as in the articulation of local politics to processes and institutions beyond the communal limits. Structural precariousness combined with the state's inability or reluctance to come to terms with social or political demands from relevant segments of the people in the communities set the socioeconomic and institutional stage for lynchings. In contrast with approaches relating these events to an alleged indigenous cultural identity, the analysis points to the impact of the communities' political

  7. Distribución espacio-temporal de larvas de Chironomidae (Diptera en un arroyo andino (Uspallata, Mendoza, Argentina Spatial and temporal distribution of larvae of Chironomidae (Diptera in an Andean stream (Uspallata, Mendoza, Argentina

    Directory of Open Access Journals (Sweden)

    Erica E. Scheibler

    2008-12-01

    Full Text Available Se realizó un estudio sobre la composición larval de la familia Chironomidae en un arroyo andino en la localidad de Uspallata (Mendoza, Argentina. Se realizaron muestreos estacionales durante un ciclo anual completo (2001/2002 en tres sitios, siguiendo un gradiente altitudinal. Se midieron variables físico-químicas en campo y laboratorio. La relación entre presencia y abundancia de quironómidos y parámetros ambientales se exploró mediante un análisis de Correspondencia Canónica. Se identificaron siete géneros pertenecientes a cuatro subfamilias: Chironominae, Orthocladiinae, Podonominae y Tanypodinae. Orthocladiinae fue la subfamilia que tuvo mayor riqueza genérica (Cricotopus van der Wulp, Onconeura Andersen & Saether y Parametriocnemus Goetghebuer, densidad y frecuencia de aparición a nivel estacional y espacial. Podonominae (Podonomus Philippi y Podonomopsis Brundin se halló únicamente en SA mientras que Chironominae (Polypedilum Kieffer estuvo presente en UD. Tanypodinae (Pentaneura Philippi se encontró en los tres sitios de muestreo aunque con una densidad menor. Se detectó incremento de la conductividad y temperatura del agua, y disminución del tamaño del sustrato desde SA a UD, lo que coincide con la desaparición de Podonomus y Podonomopsis y la aparición de Polypedilum hacia UD. De este estudio se concluye que el sistema presenta baja riqueza genérica comparada con otros sistemas montañosos de Argentina.A study was conducted on the larval composition of the family Chironomidae in an Andean stream in Uspallata locality (Mendoza, Argentina. Seasonal samplings were performed over a full annual cycle (2001/2002 at three sites, along an altitudinal gradient. Physical and chemical variables were measured in both the field and the laboratory. Relationship between presence and abundance of chironomids and environmental parameters was explored using a Canonical Correspondence analysis. Seven genera were identified

  8. Characteristics of Precipitation Features and Annual Rainfall during the TRMM Era in the Central Andes

    Science.gov (United States)

    Mohr, Karen I.; Slayback, Daniel; Yager, Karina

    2014-01-01

    The central Andes extends from 7 deg to 21 deg S, with its eastern boundary defined by elevation (1000m and greater) and its western boundary by the coastline. The authors used a combination of surface observations, reanalysis, and the University of Utah Tropical Rainfall Measuring Mission (TRMM) precipitation features (PF) database to understand the characteristics of convective systems and associated rainfall in the central Andes during the TRMM era, 1998-2012. Compared to other dry (West Africa), mountainous (Himalayas), and dynamically linked (Amazon) regions in the tropics, the central Andes PF population was distinct from these other regions, with small and weak PFs dominating its cumulative distribution functions and annual rainfall totals. No more than 10% of PFs in the central Andes met any of the thresholds used to identify and define deep convection (minimum IR cloud-top temperatures, minimum 85-GHz brightness temperature, maximum height of the 40-dBZ echo). For most of the PFs, available moisture was limited (less than 35mm) and instability low (less than 500 J kg(exp -1)). The central Andes represents a largely stable, dry to arid environment, limiting system development and organization. Hence, primarily short-duration events (less than 60 min) characterized by shallow convection and light to light-moderate rainfall rates (0.5-4.0 mm h(exp -1)) were found.

  9. Mapa bioclimático para las travesías de Mendoza (Argentina) basado en la fenología foliar

    OpenAIRE

    González Loyarte, María Margarita; Menenti, Massimo; Diblasi, Ángela

    2009-01-01

    El objetivo fue generar un mapa bioclimático de la llanura de Mendoza que reflejara las diferencias climáticas expresadas por la actividad de la vegetación (fenología foliar) a escala regional. Se partió de la imagen digital del índice bioclimático de aridez P/ETP, generada en una etapa anterior a partir de una serie temporal de imágenes de índice verde (IVDN), y se recodificó en clases bioclimáticas. Se evaluó en...

  10. Evidencias de la zona de contacto entre los terrenos de Precordillera y Pie de Palo, Provincias de San Juan y Mendoza

    Directory of Open Access Journals (Sweden)

    Maximiliano García Torrejón

    2011-12-01

    Full Text Available Se realizó un estudio gravimétrico en la región norte de la cuenca Cuyana, entre las provincias de San Juan y Mendoza. Mediante relaciones de gradientes gravimétricos tales como señal analítica, Tilt y fase del Tilt, se observó un marcado gradiente, que fue interpretado como un cambio lateral de litologías, que coincidiría con el área de una probable paleosutura del margen proto-andino, que separa en el terreno compuesto de Cuyania, al terreno de Precordillera con el terreno de Pie de Palo.

  11. Caracterización SEMEDS de inclusiones piroclásticas y opacos de la cerámica Viluco (Mendoza, Argentina)

    OpenAIRE

    Prieto Olavarría, Cristina Alejandra; D`angelo, José Alejandro

    2015-01-01

    Realizamos una aproximación exploratoria a la caracterización por SEM-EDS de las inclusiones de 10 fragmentos de cerámica Viluco recuperados de contextos datados entre el siglo XV y XVII del norte de Mendoza y dos tiestos producidos durante la dominación incaica procedentes de un alero precordillerano mendocino (Centro Oeste argentino). Analizamos inclusiones piroclásticas y otras ricas en Fe, para conocer su microestructura y composición química (semicuantitativa). Los resultados permiten do...

  12. La migración estacional a producciones agrarias de un área de la Argentina: el Valle de Uco, provincia de Mendoza

    OpenAIRE

    Bardomas, Silvia Monica

    2016-01-01

    En este trabajo se analiza la problemática del trabajador migrante estacional que arriba a un área específica de la provincia de Mendoza (Valle de Uco), en la República Argentina; para ello se considera el tipo de inserción laboral a la que acceden, la articulación de esas ocupaciones con las de su lugar de origen, así como las condiciones de trabajo y de vida durante la permanencia en dicha área. El proceso de reestructuración de las producciones agrícolas del área, fuertemente integradas a ...

  13. Narcocultura y crisis de la identidad en «El amante de Janis Joplin», de Élmer Mendoza

    OpenAIRE

    Salazar Quintana, Luis Carlos; Yáñez Félix, Ricardo Antonio

    2017-01-01

    A través del presente estudio se busca interpretar las formaciones discursivas inscritas en la novela de Élmer Mendoza, El amante de Janis Joplin (2001), como trasunto de la identidad colectiva alrededor del fenómeno de la narcocultura. Para ello, nos serviremos de la reflexión foucaultiana, sobre los aspectos que comporta el proceso de gestación del discurso como eje heurístico sobre el que se constituyen los saberes del imaginario social inscritos en el texto.

  14. Manuel Tolosa Latour (1857-1919 y Elisa Mendoza Tenorio (1856-1929: precursores de la protección a la infancia en España

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    Juan Félix Rodríguez Pérez

    2014-10-01

    La famosa actriz Elisa Mendoza Tenorio, esposa de Manuel Tolosa Latour, abandonó la escena teatral y se unió a la campaña de su marido. Estableció premios de higiene y fundó instituciones dedicadas a divulgar las normas higiénicas domésticas. Junto a Tolosa participó en la Sociedad Protectora de los Niños, él como secretario general y ella como integrante destacada de la Junta de Damas de la institución benéfica.

  15. FORMACIÓN, CRISIS Y REORIENTACIONES DE LA VITIVINICULTURA EN MENDOZA Y SAN JUAN, 1970-2000. APORTES PARA EL ESTUDIO DEL SECTOR EN LA ARGENTINA

    Directory of Open Access Journals (Sweden)

    Rodolfo Richard-Jorba

    2006-12-01

    Full Text Available Las actuales provincias de Mendoza y San Juan, localizadas en el árido centro-oeste argentino, llevan a cabo sus actividades económicas principales en grandes oasis de regadío, pequeñas porciones del territorio, en las cuales se concentra más del 95% de la población. A lo largo de su historia los productos de sus viñedos fueron dotándolas de una clara identidad hasta conformar lo que hoy conocemos como la gran Región Vitivinícola Argentina.

  16. Panamericanismo femenino y protestantismo en México a través de la vida de la profesora Adelia Palacios Mendoza

    OpenAIRE

    Lau Jaiven, Ana; Rodríguez,Roxana

    2014-01-01

    El siguiente artículo explora el panamericanismo y el protestantismo desde la actuación femenina de una mujer metodista, maestra y científica: Adelia Palacios Mendoza. La importancia de estudiar la participación de esta mujer en el ámbito público, educativo y político radica en que Palacios transgredió el deber ser femenino de su época. A finales del siglo XIX y principios del XX, periodo en que Adelia sobresalió, el orden de género imperante recluía a las mujeres al espacio do...

  17. Las complejidades sociales de la globalización en los debates sobre la minería metalífera en los municipios de Mendoza

    OpenAIRE

    Levantino, Belén

    2010-01-01

    A través de las complejidades sociales que la globalización desempeña en los debates sobre la minería metalífera en Mendoza, el presente trabajo intentará demostrar, por medio de un análisis cualitativo, que este fenómeno mundial posiciona diferentes actores sociales respecto de los del Estado nacional y popular. La evidencia empírica nos indica que la lógica dominante de la «sociedad red» tiene un comportamiento disímil en cada contexto institucional y cultural. En tales contextos, el rol de...

  18. Strategies for energetic and environmental sustainability in cities with dry climates. Comparative assessment for updating the Urban and Building Code for the City of Mendoza, Argentina.

    OpenAIRE

    Carlos Rosa; Mariela Arboit

    2015-01-01

    Se presentan los resultados de un estudio dirigido a determinar las consecuencias energético ambientales de la implementación de un proyecto de reformas al Código Urbano y de Edificación preparado por la Municipalidad de la ciudad de Mendoza (Argentina). El objetivo principal de la reforma al código ha sido densificar el tejido urbano, que permitiría mejorar la eficacia funcional, controlando la expansión urbana periférica. Después de una evaluación de la propuesta municipal (PM), se concluyó...

  19. LA PARTICIPACIÓN DE LAS MUJERES EN LA REVOLUCIÓN MEXICANA: JUANA BELÉN GUTIÉRREZ DE MENDOZA (1875-1942)

    OpenAIRE

    Ana Lau Jaiven

    2005-01-01

    Este artículo constituye una biografía de una revolucionaria y las etapas por las cuales transita su pensamiento. Juana B. Gutiérrez de Mendoza nacida en el estado de Durango, participó destacadamente en la historia de las mujeres en México debido a su oposición al régimen dictatorial de Porfirio Díaz. Se dedicó al magisterio y al periodismo como muchas mujeres de su tiempo. Atacó furiosamente a la religión y pugnó por la educación para las mujeres.

  20. Ser en el tiempo : cúpulas y bóvedas en el país del vino (Mendoza, siglos XVII-XIX)

    OpenAIRE

    Lacoste, Pablo; Premat, Estela; Navarrete,Sandra

    2016-01-01

    Las construcciones de tierra que se utilizaron en la región y en el área rural mendocina que analizamos, fueron también herencia de la tradición española. Sus usos fueron predominantemente rurales, pero han evidencias de que la ciudad de Mendoza también tuvo su cielo recortado por las curvas de los techos abovedados. Las más abundantes se hallaron en las haciendas vitivinícolas y cerealeras. La casa de las bóvedas del San Martín en El Barreal, fue una construcción notable provista de voluntad...

  1. Constitución y actividades de la Mesa Provincial de Educación Ambiental en la provincia de Mendoza, Argentina.

    OpenAIRE

    Gabriela Diaz Isenrath; T Bilbao; Cristian Barbosa; Susana Lagos Silnik; Nora Marlia; Silvia Musso; Oscar Ongay Ugarteche; Mirta Zarate; Elba Alicia Pescetti de Cristaldo; Mauricio Bucheri; Flora Bertolotti

    2015-01-01

    La Educación Ambiental como actividad interdisciplinaria e interinstitucional, requiere de la planificación estratégica participativa, que permita la concreción de esfuerzos que suelen realizarse de manera aislada. Se expone el proceso llevado a cabo para la constitución de la Mesa de Educación Ambiental en la provincia de Mendoza, Argentina. A partir de la discusión sobre la problemática local del Cambio Climático y los requerimientos de  medidas de adaptación, se propone el espacio en el añ...

  2. Recuperación y desigualdad económica en el interior rural argentino del siglo XIX. Un examen sobre la composición y distribución de la riqueza en la campaña de Mendoza a través de fuentes fiscales (1866

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    Beatriz Bragoni

    2011-06-01

    Full Text Available La relación entre crecimiento económico y diferenciaciones regionales en la experiencia histórica argentina de los siglos XIX y XX refiere a un problema regularmente visitado por la literatura académica. En particular, la desigualdad entre las regiones pampeanas y extrapampeanas generó el interés de especialistas preocupados por identificar las características de procesos no equivalentes o asimétricos con el fin de trazar una suerte de mapa económico (y político interpretativo que repara en los límites del crecimiento argentino oponiendo a la riqueza sobre todo bonaerense y de la región pampeana en su conjunto, el deterioro económico del "Interior". Este artículo se propone contribuir al debate antes enunciado para lo cual ofrece indicadores estadísticos sobre la composición y distribución personal de la riqueza en la campaña de la provincia de Mendoza hacia 1870 los cuales permiten apreciar aspectos poco atendidos de las diferenciaciones microrregionales previas a la transformación agroindustrial vitivinícola de finales del siglo XIX.The relation between economic growth and regional differentiations in the Argentine historical experience of the 19th and 20th centuries refers to a problem regularly visited by the academic literature. Particularly, the disparity between the pampean and extra-pampean regions originated the interest of specialists, concerned in identifying the characteristics of non-equivalent or asymmetric processes. This, with the object of drawing some type of an interpretative economic (and politic map, that considers the limits of the Argentine growth opposing to the richness -mostly of Buenos Aires- and of the pampean region, the economic deterioration of the "Interior". The goal of this article is contributing to the priorly announced debate, offering statistical indicators of the personal composition and distribution of the field richness in the province of Mendoza, toward 1870. Said indicators allow

  3. Uranium Provinces in China

    Institute of Scientific and Technical Information of China (English)

    2000-01-01

    Three uranium provinces are recognized in China, the Southeast China uranium province, the Northeast China-lnner Mongolia uranium province and the Northwest China (Xinjiang) uranium province. The latter two promise good potential for uranium resources and are major exploration target areas in recent years. There are two major types of uranium deposits: the Phanerozoic hydrothermal type (vein type) and the Meso-Cenozoic sandstone type in different proportions in the three uranium provinces. The most important reason or prerequisite for the formation of these uranium provinces is that Precambrian uranium-enriched old basement or its broken parts (median massifs) exists or once existed in these regions, and underwent strong tectonomagmatic activation during Phanerozoic time. Uranium was mobilized from the old basement and migrated upwards to the upper structural level together with the acidic magma originating from anatexis and the primary fluids, which were then mixed with meteoric water and resulted in the formation of Phanerozoic hydrothermal uranium deposits under extensional tectonic environments. Erosion of uraniferous rocks and pre-existing uranium deposits during the Meso-Cenozoic brought about the removal of uranium into young sedimentary basins. When those basins were uplifted and slightly deformed by later tectonic activity, roll-type uranium deposits were formed as a result of redox in permeable sandstone strata.

  4. Dental status and dental treatment demands in preschoolers from urban and underprivileged urban areas in Mendoza city, Argentina.

    Science.gov (United States)

    Fernández, Claudia N; Squassi, Aldo; Bordoni, Noemí

    2015-04-01

    The aim of this study was to establish the association between dental status and demand for dental care in preschoolers at urban and underprivileged urban schools in the city of Mendoza. Dental status was diagnosed in a purposive sample of preschoolers at urban schools (Group U: n = 148) and underprivileged urban schools (Group UnU: n = 155) in Greater Mendoza city, by determining the following indicators: (a) caries-free children (%), and (b) dmft/DMFT and its discriminated components, including active non-cavitated enamel caries. The characteristics of demand for care were determined using an ad hoc structured questionnaire. The following were determined: frequency distributions and confidence intervals for categorical variables, measures of central tendency and dispersion, tests for differences in means (Student's t test), association (chi squared) and correlation among variables (Pearson's r), at a significance level p<0.05. Comparison of dental status variables between groups showed significantly higher values in group UnU for: d+D tooth (ẋ = 5.4} 3.8; t = 2.887; p = 0.004); dmft+DMFT (ẋ = 5.7}4.1; t = 0.466; p = 0.020); d+D surface (ẋ = 7.62} 6.2; t = 0.956; p = 0.014); f+F surface (ẋ = 0.12}4.5; t = 2.71; p = 0.007) and percentage of caries-free children (x2= 25.377; p= 0.018). The following trends were found in this group: higher demand on the government subsystem, fewer visits to the dentist (x2 = 7.02, p = 0.008) and greater difficulty in getting appointments (x2 = 19.91, pẋ0.001). Frequency of visits was associated to the severity of dental status (x2 = 19.412; pẋ0.001), but no correlation was found between frequency of visits during the past year and dmft+DMFT (Pearson's r coefficient = 0.091; p = 0.0426) Group U showed preferential demand for the private or "obra social" (trade union managed health insurance) systems (x2 = 78.85 p = 0.00) and there was no statistically significant association between visits to the dentist and dmft

  5. A further contribution to the knowledge of two inadequately known species of geophilid centipedes from the Andes of South-Central Chile, currently assigned to the genus Plateurytion Attems, 1909 (Chilopoda: Geophilomorpha).

    Science.gov (United States)

    Pereira, Luis Alberto

    2015-10-06

    Two poorly known species of geophilid centipedes from the Andes of South-Central Chile, i.e., Plateurytion mundus (Chamberlin, 1955) and Plateurytion zapallar (Chamberlin, 1955) (Myriapoda: Chilopoda: Geophilomorpha), are herein redescribed and illustrated after type specimens of both taxa and new material of the latter, rectifying the condition of the coxosternites of the second maxillae, which are medially joined through a narrow, hyaline and non-areolate membranous isthmus only (instead of "broadly fused as in Pachymerium", as stated by Chamberlin), this being consistent with the current generic assignment of these species under Plateurytion Attems, 1909. New data on many morphological features of specific value, until now unknown, are also given for both taxa. Plateurytion zapallar is reported for the first time from Coquimbo region, 11 Km N of Los Vilos (Elqui province), Valparaíso region, Quebrada Huaquén, Pichicuy (Petorca province), La Campana National Park (Quillota province), and Quebrada el Tigre, Cachagua (Valparíso province). A key for identification of the South American species currently included in Plateurytion is given.

  6. Interannual variability of hail-days in the Andes region since 1885

    Science.gov (United States)

    Prieto, Rosario; Gimeno, Luis; García, Ricardo; Herrera, Roberto; Hernández, Emiliano; Ribera, Pedro

    1999-09-01

    Using documentary sources, a series of the annual number of hail-days in a region near Mendoza, Argentina was constructed. The analysis of the temporal series by means of singular spectrum analysis (SSA) and the maximum entropy method (MEM) found that the number of hail-days exhibits a similar interannual variability as the global surface temperature [M. Ghil, R. Vautard, Nature 350 (1991) 324-327]. The oscillations exhibit interdecadal periods of 22 years and interannual oscillations of about 4 and 8 years.

  7. Structure and tectonic evolution of the Fuegian Andes (southernmost South America) in the framework of the Scotia Arc development

    Science.gov (United States)

    Torres Carbonell, Pablo J.; Dimieri, Luis V.; Olivero, Eduardo B.; Bohoyo, Fernando; Galindo-Zaldívar, Jesús

    2014-12-01

    The major structural and tectonic features of the Fuegian Andes provide an outstanding onshore geological framework that aids in the understanding of the tectonic evolution of the Scotia Arc, mainly known from offshore studies. The orogenic history of the Fuegian Andes (Late Cretaceous-Miocene) is thus compared and integrated with the tectonic history of the Scotia Sea. Late Cretaceous-Paleocene structures in the Fuegian Andes suggest a N-directed contraction consistent with an oroclinal bending of the southernmost South America-Antarctic Peninsula continental bridge. This N-directed contraction in the Fuegian Andes continued during the spreading of the West Scotia Ridge, between 40-50 and 10 Ma ago. The onset of major strike-slip faulting in Tierra del Fuego is considered here to be not older than the late Miocene, consistent with the recent history of the North Scotia Ridge; thus forming part of a tectonic regime superposed to the prior contraction in the Fuegian Andes.

  8. Distribución espacio-temporal de larvas de Chironomidae (Diptera en un arroyo andino (Uspallata, Mendoza, Argentina

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    Erica E. SCHEIBLER

    2008-01-01

    Full Text Available Se realizó un estudio sobre la composición larval de la familia Chironomidae en un arroyo andino en la localidad de Uspallata (Mendoza, Argentina. Se realizaron muestreos estacionales durante un ciclo anual completo (2001/2002 en tres sitios, siguiendo un gradiente altitudinal. Se midieron variables físico-químicas en campo y laboratorio. La relación entre presencia y abundancia de quironómidos y parámetros ambientales se exploró mediante un análisis de Correspondencia Canónica. Se identificaron siete géneros pertenecientes a cuatro subfamilias: Chironominae, Orthocladiinae, Podonominae y Tanypodinae. Orthocladiinae fue la subfamilia que tuvo mayor riqueza genérica (Cricotopus van der Wulp, Onconeura Andersen & Saether y Parametriocnemus Goetghebuer, densidad y frecuencia de aparición a nivel estacional y espacial. Podonominae (Podonomus Philippi y Podonomopsis Brundin se halló únicamente en SA mientras que Chironominae (Polypedilum Kieffer estuvo presente en UD. Tanypodinae (Pentaneura Philippi se encontró en los tres sitios de muestreo aunque con una densidad menor. Se detectó incremento de la conductividad y temperatura del agua, y disminución del tamaño del sustrato desde SA a UD, lo que coincide con la desaparición de Podonomus y Podonomopsis y la aparición de Polypedilum hacia UD. De este estudio se concluye que el sistema presenta baja riqueza genérica comparada con otros sistemas montañosos de Argentina.

  9. Evaluation of summer thermal conditions and the environmental efficiency of different urban square designs in Mendoza, Argentina

    Directory of Open Access Journals (Sweden)

    Susana Stocco

    2015-03-01

    Full Text Available El objetivo de este trabajo es evaluar las consecuencias de las decisiones de diseño sobre el comportamiento térmico y la eficiencia ambiental de las plazas de la ciudad de Mendoza. A tal fin se seleccionaron tres casos de estudio, donde se evaluó el comportamiento de distintas estructuras presentes en las plazas. Para ello se desarrollaron mediciones de temperatura del aire mediante sensores fijos, durante un periodo de 40 días en la estación verano de 2012, los sensores fueron ubicados en las diferentes estructuras (bosque, prado y centro de la plaza y en su entorno urbano, siguiendo un eje en sentido norte-sur. Además se determinó el valor del factor de visión de cielo (SVF y la digitalización hemisférica de la trayectoria solar para todos los puntos evaluados. Los resultados ponen de manifiesto la necesidad de reflexionar y revisar las estructuras de plazas existentes, en cuanto a sus esquemas de diseño, dado que el esquema tradicional que plantea una distribución de espacios en forma simétrica, parece no ser el que combina en forma más eficiente las distintas variables involucradas en el comportamiento térmico de la plaza: materialidad, distribución de la vegetación y exposición solar. Además se observa que a menor densidad edilicia del entorno urbano en el cual se inserta la plaza, sus condiciones térmicas y su eficiencia ambiental pueden mejorarse, casi con independencia de otros factores, mediante un diseño apropiado del espacio.

  10. Municipio, identidad cultural y comunidades indígenas. El caso huarpe en el noreste de Mendoza

    Directory of Open Access Journals (Sweden)

    Leticia Saldi

    2013-06-01

    Full Text Available En el presente artículo analizamos cómo funcionarios de la Municipalidad de Lavalle representan e interpelan a las comunidades indígenas huarpe situadas en el área no irrigada del noreste de Mendoza, área situada en el departamento de Lavalle. Éste se encuentra dividido socioterritorialmente en dos espacios. Uno irrigado, caracterizado como área de progreso, de producción agrícola y de herencia europea y el otro no irrigado, representado como área de atraso, de producción ganadera y de herencia precolonial. A partir de un análisis etnográfico, analizamos cómo el municipio gestiona local y cotidianamente la diversidad étnica, cultural, económica y política. Concluimos que las formas con que los funcionarios interpelan a las comunidades indígenas y a sus integrantes son en base a un doble movimiento, uno de reconocimiento explícito y el otro de individualización, invisibilización y deslegitimación hacia las mismas. Al invisibilizar a las comunidades como sujetos colectivos, funcionarios municipales intentan dar una identidad común que incorpore a los espacios irrigados y no irrigados y a sus poblaciones como pertenecientes a un mismo territorio, el departamental, a la vez que mantenga la jerarquización entre ambos. Al realizar este movimiento, el municipio se erige como el unificador y contenedor de ambos espacios y de los distintos grupos socio-étnicos que los integran.

  11. Glacier surface mass balance and freshwater runoff modeling for the entire Andes Cordillera

    Science.gov (United States)

    Mernild, Sebastian H.; Liston, Glen E.; Yde, Jacob C.

    2017-04-01

    Glacier surface mass balance (SMB) observations for the Andes Cordillera are limited and, therefore, estimates of the SMB contribution from South America to sea-level rise are highly uncertain. Here, we simulate meteorological, snow, glacier surface, and hydrological runoff conditions and trends for the Andes Cordillera (1979/80-2013/14), covering the tropical latitudes in the north down to the sub-polar latitudes in the far south, including the Northern Patagonia Ice Field (NPI) and Southern Patagonia Ice Field (SPI). SnowModel - a fully integrated energy balance, blowing-snow distribution, multi-layer snowpack, and runoff routing model - was used to simulate glacier SMBs for the Andes Cordillera. The Randolph Glacier Inventory and NASA Modern-Era Retrospective Analysis for Research and Applications products, downscaled in SnowModel, allowed us to conduct relatively high-resolution simulations. The simulated glacier SMBs were verified against independent directly-observed and satellite gravimetry and altimetry-derived SMB, indicating a good statistical agreement. For glaciers in the Andes Cordillera, the 35-year mean annual SMB was found to be -1.13 m water equivalent. For both NPI and SPI, the mean SMB was positive (where calving is the likely reason for explaining why geodetic estimates are negative). Further, the spatio-temporal freshwater river runoff patterns from individual basins, including their runoff magnitude and change, were simulated. For the Andes Cordillera rivers draining to the Pacific Ocean, 86% of the simulated runoff originated from rain, 12% from snowmelt, and 2% from ice melt, whereas, for example, for Chile, the water-source distribution was 69, 24, and 7%, respectively. Along the Andes Cordillera, the 35-year mean basin outlet-specific runoff (L s-1 km-2) showed a characteristic regional hourglass shape pattern with highest runoff in both Colombia and Ecuador and in Patagonia, and lowest runoff in the Atacama Desert area.

  12. Carbon stabilization mechanisms in soils in the Andes

    Science.gov (United States)

    Jansen, Boris; Cammeraat, Erik

    2015-04-01

    The volcanic ash soils of the Andes contain very large stocks of soil organic matter (SOM) per unit area. Consequently, they constitute significant potential sources or sinks of the greenhouse gas CO2. Climate and/or land use change potentially have a strong effect on these large SOM stocks. To clarify the role of chemical and physical stabilisation mechanisms in volcanic ash soils in the montane tropics, we investigated carbon stocks and stabilization mechanisms in the top- and subsoil along an altitudinal transect in the Ecuadorian Andes. The transect encompassed a sequence of paleosols under forest and grassland (páramo), including a site where vegetation cover changed in the last century. We applied selective extraction techniques, performed X-ray diffraction analyses of the clay fraction and estimated pore size distributions at various depths in the top- and subsoil along the transect. In addition, from several soils the molecular composition of SOM was further characterized with depth in the current soil as well as the entire first and the top of the second paleosol using GC/MS analyses of extractable lipids and Pyrolysis-GC/MS analyses of bulk organic matter. Our results show that organic carbon stocks in the mineral soil under forest a páramo vegetation were roughly twice as large as global averages for volcanic ash soils, regardless of whether the first 30cm, 100cm or 200cm were considered. We found the carbon stabilization mechanisms involved to be: i) direct stabilization of SOM in organo-metallic (Al-OM) complexes; ii) indirect protection of SOM through low soil pH and toxic levels of Al; and iii) physical protection of SOM due to a very high microporosity of the soil (Tonneijck et al., 2010; Jansen et al. 2011). When examining the organic carbon at a molecular level, interestingly we found extensive degradation of lignin in the topsoil while extractable lipids were preferentially preserved in the subsoil (Nierop and Jansen, 2009). Both vegetation

  13. Long-term carbon accumulation in Andes peatlands

    Science.gov (United States)

    Huaman, Yizet; Moreira-turq, Patricia; Willems, Bram; Espinoza, Raul; Turq, Bruno; Apaéstegui, James; Llanos, Romina

    2017-04-01

    High-altitude peatlands of the Andes still remain relatively unexplored since most of the studies on carbon capture in tropical soils have focused on peatlands in low altitude areas, leaving aside the importance of the study of high mountain wetlands, currently called "bofedales" located between 3000 and 5000 masl, covering most of the Andes mountains in South America. These peatlands in turn may also represent important paleoclimatic records. In this study, we investigated three peatland cores (APA-01, APA2-01, and APA2-02) at different altitudes (4210 m, 4420 m and 4432 m, respectively) in high Andean Peatlands of southern Peru. The peatland studied is located at the headwater basin Cachi River, in the town of Ayacucho, Peru. The aim of this study was to evaluate the role played by past climatic changes on the peatlands carbon accumulation. Each core was sectioned centimeter by centimeter and sub samples (n = 31) were collected for radiocarbon dating by AMS (acceleration mass spectrometer) and were used to create a sedimentological model based on the program Clam2.2R. The concentrations of carbon and nitrogen were determined from a C / H / N elemental analyzer and the stable carbon and nitrogen isotopes (δ13C and δ15N) were also analyzed. The bulk density was determined based on the volume occupied by the sediment (g /cm3). Finally, the carbon accumulation rate (gC m-2año-1) was determined. The three cores were characterized by two sedimentary units, the results present in the first sedimentary unit of APA01 an average long-term carbon accumulation rate of 59 gC m-2año-1, APA2-01 with 32 gC m-2año-1 and finally APA2-02 with 24 gC m-2año-1; for the second sedimentary unit we have: APA01 on average 17 gC m-2año-1, APA2-01 with 33 gC m-2año-1 and finally APA2-02 with 49 gC m-2año-1. In conclusion, we can say that the carbon accumulation rate for the first sedimentary unit of the three cores decreases as the altitude increases; on the other hand, we have the

  14. Possible future lakes in the Andes of Peru

    Science.gov (United States)

    Colonia, Daniel; Haeberli, Wilfried; Torres, Judith; Giraldez, Claudia; Schauwecker, Simone; Santiago, Alexzander; Cochachin, Alejo; Huggel, Christian

    2015-04-01

    Climate change has caused large losses of glacier mass in the Andes of Peru. Also, given the projected changes in climate, based on different IPCC scenarios for 2050 and 2080, simulations with a tropical glacier-climate model indicate that glaciers will continue to retreat. According to the national Peruvian glacier inventories 43% of glacier area has disappeared between 1970 and 2003-2010 in the 19 snowy mountain ranges and a total of 8 355 new lakes have formed in deglaciating terrain. With glacier retreat new lakes form in parts of the glacier tongue where there is an overdeepening, and these lakes can be a source of natural hazards to downstrean populations. Therefore, the identification of possible future lakes is important to plan for preventive measures concerning possible lake outbursts as well as to understand changes in freshwater storage in the corresponding source areas. Modeling of glacier-bed overdeepenings and possible future lakes forming in such topographic depressions when becoming ice-free was done using the SRTM DEM from the year 2000 with a 90 m resolution and the 2003-2010 glacier outlines from the recently published national glacier inventory of Perú. The GIS-based analysis followed three main steps: (1) identification of flat glacier areas with less than 10° surface slope as a first-order spatial approximation to possible occurrences of glacier-bed overdeepenings; (2) application, using Google Earth, of three morphological indications of glacier-bed overdeepenings following Frey et al. (2010): steepening surface slope, onset of crevasse formation, lateral flow-narrowing; and (3) verification of the results from steps (1) and (2) by comparison with GlabTop modeling of bed topographies following Linsbauer et al. (2012) using the SRTM DEM, contour lines and constructed branch lines for all glaciers. A pilot study has already been carried out for the Cordillera Blanca. The results show that 31 major new lakes may form in the future. The total

  15. The nature of orogenic crust in the central Andes

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    Beck, Susan L.; Zandt, George

    2002-10-01

    The central Andes (16°-22°S) are part of an active continental margin mountain belt and the result of shortening of the weak western edge of South America between the strong lithospheres of the subducting Nazca plate and the underthrusting Brazilian shield. We have combined receiver function and surface wave dispersion results from the BANJO-SEDA project with other geophysical studies to characterize the nature of the continental crust and mantle lithospheric structure. The major results are as follows: (1) The crust supporting the high elevations is thick and has a felsic to intermediate bulk composition. (2) The relatively strong Brazilian lithosphere is underthrusting as far west (65.5°W) as the high elevations of the western part of the Eastern Cordillera (EC) but does not underthrust the entire Altiplano. (3) The subcrustal lithosphere is delaminating piecemeal under the Altiplano-EC boundary but is not completely removed beneath the central Altiplano. The Altiplano crust is characterized by a brittle upper crust decoupled from a very weak lower crust that is dominated by ductile deformation, leading to lower crustal flow and flat topography. In contrast, in the high-relief, inland-sloping regions of the EC and sub-Andean zone, the upper crust is still strongly coupled across the basal thrust of the fold-thrust belt to the underthrusting Brazilian Shield lithosphere. Subcrustal shortening between the Altiplano and Brazilian lithosphere appears to be accommodated by delamination near the Altiplano-EC boundary. Our study suggests that orogenic reworking may be an important part of the "felsification" of continental crust.

  16. Evolution of Irruputuncu volcano, Central Andes, northern Chile

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    Rodríguez, I.; Roche, O.; Moune, S.; Aguilera, F.; Campos, E.; Pizarro, M.

    2015-11-01

    The Irruputuncu is an active volcano located in northern Chile within the Central Andean Volcanic Zone (CAVZ) and that has produced andesitic to trachy-andesitic magmas over the last ˜258 ± 49 ka. We report petrographical and geochemical data, new geochronological ages and for the first time a detailed geological map representing the eruptive products generated by the Irruputuncu volcano. The detailed study on the volcanic products allows us to establish a temporal evolution of the edifice. We propose that the Irruputuncu volcanic history can be divided in two stages, both dominated by effusive activity: Irruputuncu I and II. The oldest identified products that mark the beginning of Irruputuncu I are small-volume pyroclastic flow deposits generated during an explosive phase that may have been triggered by magma injection as suggested by mingling features in the clasts. This event was followed by generation of large lava flows and the edifice grew until destabilization of its SW flank through the generation of a debris avalanche, which ended Irruputuncu I. New effusive activity generated lavas flows to the NW at the beginning of Irruputuncu II. In the meantime, lava domes that grew in the summit were destabilized, as shown by two well-preserved block-and-ash flow deposits. The first phase of dome collapse, in particular, generated highly mobile pyroclastic flows that propagated up to ˜8 km from their source on gentle slopes as low as 11° in distal areas. The actual activity is characterized by deposition of sulfur and permanent gas emissions, producing a gas plume that reaches 200 m above the crater. The maximum volume of this volcanic system is of ˜4 km3, being one of the smallest active volcano of Central Andes.

  17. The Little Ice Age in the tropical Andes

    Science.gov (United States)

    Jomelli, V.; Cooley, D.; Naveau, P.; Rabatel, A.

    2003-12-01

    The period known as the Little Ice Age, from the 17th to the 19th century, brought a cooling of around 0.5 degrees Celsius as well as varyingly humid episodes Eurasia and North America. Because of a lack of long paleoclimatic time series in the tropical Andes, it is still unclear if similar cooling occurred over these tropical and Southern Hemisphere regions. Furthermore, if changes did take place, it is currently not well established if they were temporally synchronous or shifted with respect of the variations in the Northern Hemisphere or the globe. To look into this important climatic question and for advancing our understanding of the past climate links between the tropics and higher latitudes, 25 glaciers located in Bolivia and in Peru were carefully selected. Glacial activity and environmental changes were analyzed using lichenometry. Largest lichen diameters were measured in the different glacial basins. To better analyze these maximum diameters and to more appropriately represent uncertainty and the character of this collected data, age estimates of the different moraine systems were derived using extreme value theory rather than the traditional averaging. The results reveal two particular phases of glacier growth, 1550-1600 and 1800-1850. These two phases have also been identified in other proxy records, such as ice-cores and documentary data (particularly from church chronicles). In order to understand the climatic changes that could have contributed to the glacial variations, a simple model based on both precipitations and temperatures is applied to estimate mass balance questions in the basins. A cooling of the order of 0.5 C seems to be the most consistent with the data. Finally, these findings are compared with the better-known histories of Northern Hemisphere mid-latitude glaciers.

  18. Bayesian spatiotemporal interpolation of rainfall in the Central Chilean Andes

    Science.gov (United States)

    Ossa-Moreno, Juan; Keir, Greg; McIntyre, Neil

    2016-04-01

    Water availability in the populous and economically significant Central Chilean region is governed by complex interactions between precipitation, temperature, snow and glacier melt, and streamflow. Streamflow prediction at daily time scales depends strongly on accurate estimations of precipitation in this predominantly dry region, particularly during the winter period. This can be difficult as gauged rainfall records are scarce, especially in the higher elevation regions of the Chilean Andes, and topographic influences on rainfall are not well understood. Remotely sensed precipitation and topographic products can be used to construct spatiotemporal multivariate regression models to estimate rainfall at ungauged locations. However, classical estimation methods such as kriging cannot easily accommodate the complicated statistical features of the data, including many 'no rainfall' observations, as well as non-normality, non-stationarity, and temporal autocorrelation. We use a separable space-time model to predict rainfall using the R-INLA package for computationally efficient Bayesian inference, using the gridded CHIRPS satellite-based rainfall dataset and digital elevation models as covariates. We jointly model both the probability of rainfall occurrence on a given day (using a binomial likelihood) as well as amount (using a gamma likelihood or similar). Correlation in space and time is modelled using a Gaussian Markov Random Field (GMRF) with a Matérn spatial covariance function which can evolve over time according to an autoregressive model if desired. It is possible to evaluate the GMRF at relatively coarse temporal resolution to speed up computations, but still produce daily rainfall predictions. We describe the process of model selection and inference using an information criterion approach, which we use to objectively select from competing models with various combinations of temporal smoothing, likelihoods, and autoregressive model orders.

  19. High resolution precipitation climatology for the Andes of South Ecuador

    Science.gov (United States)

    Trachte, Katja; Bendix, Jörg

    2014-05-01

    The climate of Ecuador is strongly dominated by the complex structure of the Andes Mountains. Due to their heights and north-south orientation they act like a barrier, which cause delineation between the western and eastern flanks, as well as the inner-Andean areas. Commonly the Ecuadorian climate is classified in three zones, Costa, Interandina and Oriente. Existing precipitation products such as the GPCC or TRMM data are enabled to represent these climate zones, but because of their spatial resolution, they pass to capture the different regimes within a zone. Especially the inner-Andean region (Interandina) with its characteristic complex terrain shows spatially high climate variability. Local circulation systems, e.g. mountain-valley breezes as well as effects of windward and lee-side, drive the climate conditions allowing for the differentiation of air temperature and rainfall distribution on relative small scales. These highly variable patterns are also reflected by the diversity of ecosystems, e.g. rainforest, dry forest and Paramo, in a relative small area. In order to represent the local systems a dynamical downscaling approach for the Ecuadorian region is applied. In doing so the Weather Research and Forecasting (WRF) model is used. A suitable model setup was evaluated within a sensitivity study, where various parametrization schemes were tested. The most suitable physics combination was used for a 30 year hint cast simulation. The poster presents first results of the high resolution climate simulations. On the basis of the spatial distribution of rainfall patterns distinct precipitation regimes within the Interandina will be shown. The aim is to highlight and discuss the importance of the adequately representation of the terrain in mountainous regions like the Andean Mountains.

  20. Glacier loss and emerging hydrologic vulnerabilities in the Peruvian Andes

    Science.gov (United States)

    Mark, B. G.; McKenzie, J. M.; Baraer, M.; Lagos, P.; Lautz, L.; Carey, M.; Bury, J.; Crumley, R.; Wigmore, O.; Somers, L. D.

    2015-12-01

    Accelerating glacier recession in the tropical Andes is transforming downstream hydrology, while increasing demands for water by end-users (even beyond the watershed limits) is complicating the assessment of vulnerability. Future scenarios of hydro-climatic vulnerability require a better understanding of coupled hydrologic and human systems, involving both multiscale process studies and more robust models of glacier-climate interactions. We synthesize research in two proglacial valleys of glacierized mountain ranges in different regions of Peru that are both in proximity to growing water usage from urban sectors, agriculture, hydroelectric generation, and mining. In both the Santa River watershed draining the Cordillera Blanca and the Shullcas River watershed below Hyuatapallana Mountain in Junin, glaciers have receded over 25% since the 1980s. Historical runoff and glacier data, combined with glacier-climate modeling, show a long-term decrease in discharge resulting from a net loss of stored water. We find evidence that this altered hydrology is transforming proglacial wetland ecology and water quality, even while water resource use has intensified. Beyond glaciers, our results show that over 60% of the dry season base flow in each watershed is groundwater sourced from heterogeneous aquifers. Municipal water supply in Huancayo already relies on 18 groundwater wells. Perceptions of water availability and actual water use practices remain relatively divorced from the actual water resources provided from each mountain range. Critical changes in glacier volume and water supply are not perceived or acknowledged consistently amongst different water users, nor reflected in water management decisions. In order to identify, understand, model, and adapt to climate-glacier-water changes, it is vital to integrate the analysis of water availability and groundwater processes (the domain of hydrologists) with that of water use (the focus for social scientists). Attention must be

  1. Remote sensing and climate data as a key for understanding fasciolosis transmission in the Andes: review and update of an ongoing interdisciplinary project

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    Màrius V. Fuentes

    2006-11-01

    Full Text Available Fasciolosis caused by Fasciola hepatica in various South American countries located on the slopes of the Andes has been recognized as an important public health problem. However, the importance of this zoonotic hepatic parasite was neglected until the last decade. Countries such as Peru and Bolivia are considered to be hyperendemic areas for human and animal fasciolosis, and other countries such as Chile, Ecuador, Colombia and Venezuela are also affected. At the beginning of the 1990s a multidisciplinary project was launched with the aim to shed light on the problems related to this parasitic disease in the Northern Bolivian Altiplano. A few years later, a geographic information system (GIS was incorporated into this multidisciplinary project analysing the epidemiology of human and animal fasciolosis in this South American Andean region. Various GIS projects were developed in some Andean regions using climatic data, climatic forecast indices and remote sensing data. Step by step, all these GIS projects concerning the forecast of the fasciolosis transmission risk in the Andean mountain range were revised and in some cases updated taking into account new data. The first of these projects was developed on a regional scale for the central Chilean regions and the proposed model was validated on a local scale in the Northern Bolivian Altiplano. This validated mixed model, based on both fasciolosis climatic forecast indices and normalized difference vegetation index values from Advanced Very High Resolution Radiometer satellite sensor, was extrapolated to other human and/or animal endemic areas of Peru and Ecuador. The resulting fasciolosis risk maps make it possible to show the known human endemic areas of, mainly, the Peruvian Altiplano, Cajamarca and Mantaro Peruvian valleys, and some valleys of the Ecuadorian Cotopaxi province. Nevertheless, more climate and remote sensing data, as well as more accurate epidemiological reports, have to be

  2. Detrital Zircon Provenance Record of Pre-Andean to Modern Tectonics in the Northern Andes: Examples from Peru, Ecuador, and Colombia

    Science.gov (United States)

    George, S. W. M.; Jackson, L. J.; Horton, B. K.

    2015-12-01

    Detrital zircon U-Pb age distributions from modern rivers and Mesozoic-Cenozoic basin fill in the northern Andes provide insights into pre-Andean, Andean, and active uplift and exhumation of distinctive sediment source regions. Diagnostic age signatures enable straightforward discrimination of competing sediment sources within the Andean magmatic arc (Western Cordillera-Central Cordillera), retroarc fold-thrust belt (Eastern Cordillera-Subandean Zone), and Amazonian craton (composed of several basement provinces). More complex, however, are the mid/late Cenozoic provenance records generated by recycling of basin fill originally deposited during early/mid Mesozoic extension, late Mesozoic thermal subsidence, and early Cenozoic shortening. Although subject to time-transgressive trends, regionally significant provenance patterns in Peru, Ecuador, and Colombia reveal: (1) Triassic-Jurassic growth of extensional subbasins fed by local block uplifts (with commonly unimodal 300­-150 Ma age peaks); (2) Cretaceous deposition in an extensive postrift setting fed by principally cratonic sources (with common 1800-900 Ma ages); and (3) Cenozoic growth of a broad flexural basin fed initially fed by magmatic-arc rocks (100-0 Ma), then later dominance by thrust-belt sedimentary rocks with progressively greater degrees of basin recycling (yielding diverse and variable age populations from the aforementioned source regions). U-Pb results from modern rivers and smaller subbasins prove useful in evaluating source-to-sink relationships, downstream mixing relationships, hinterland-foreland basin connectivity, paleodrainage integration, and tectonic/paleotopographic reconstructions. Most but not all of the elevated intermontane basins in the modern hinterland of the northern Andes contain provenance records consistent with genesis in a broader foreland basin developed at low elevation. Downstream variations within modern axial rivers and Cenozoic axial basins inform predictive models of

  3. Two New Species of Black Flies (Diptera: Simuliidae) from the High Andes of Colombia.

    Science.gov (United States)

    Mantilla, Juan S; Moncada, Ligia I; Matta, Nubia E; Adler, Peter H

    2013-01-01

    The females, males, pupae, and larvae of two new species of Simulium are described and illustrated from a small stream 3950 m above sea level in the Lake Otún area of the Colombian Andes Mountains. Simulium (Pternaspatha) quimbayium n. sp. represents a 630-km northeastern extension of the distributional range of previously known members of the subgenus Pternaspatha, and Simulium (Psilopelmia) machetorum n. sp. represents the highest altitude recorded for a species of the subgenus Psilopelmia. These species illustrate the unique simuliid biodiversity in the páramo ecosystem of the high northern Andes.

  4. Thermochronology and tectonics of the Mérida Andes and the Santander Massif, NW South America

    Science.gov (United States)

    van der Lelij, Roelant; Spikings, Richard; Mora, Andrés

    2016-04-01

    New apatite U-Pb and multiphase 40Ar/39Ar data constrain the high to medium temperature (~ 500 °C-~ 300 °C) thermal histories of igneous and metamorphic rocks exposed in the Mérida Andes of Venezuela, and new apatite and zircon fission track data constrain the ~ 500 °C-~ 60 °C thermal histories of pre-Jurassic igneous and metamorphic rocks of the adjacent Santander Massif of Colombia. Computed thermal history envelopes using apatite U-Pb dates and grain size information from an Early Palaeozoic granodiorite in the Mérida Andes suggest that it cooled from > 500 °C to histories. The generally accepted timing of amalgamation of Pangaea along the Ouachita-Marathon suture pre-dates Late Permian to Triassic cooling recorded in basement rocks of the Mérida Andes by > 30 Ma, and its effect on rocks preserved in north-western South America is unknown. We interpret late Permian to Triassic cooling in the Mérida Andes to be driven by exhumation. Previous studies have suggested that a short phase of shortening and anatexis is recorded at ~ 253 Ma in the Maya Block, which may have been adjacent to the basement rocks of the Mérida Andes in the Late Permian. The coeval onset of exhumation in the Mérida Andes may be a result of increased coupling in the magmatic arc, which was located along the western margin of Pangaea. Triassic extension is documented in the Central Cordillera of Colombia and Ecuador between ~ 240 Ma and ~ 215 Ma, although extension at this time has not been clearly identified in the Mérida Andes or the Santander Massif. Permian to Triassic cooling is not recorded in the structurally isolated Caparo Block in the southern Mérida Andes, suggesting that it may have constituted a distinct fault block in the Triassic. New fission track data from the Santander Massif suggest that it started exhuming at ~ 40 Ma during a period of accelerated convergence between the Nazca/Farallòn Plate and the western margin of South America. Exhumation in the Santander

  5. El problema de los robos: de los temores de la élite a las prácticas de subsistencia de los sectores subalternos. Mendoza (Río de la Plata, 1820-1831

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    Molina, Eugenia

    2014-04-01

    Full Text Available This essay focuses on a specific study of thefts that occurred in the jurisdiction of Mendoza at the time of the formation of the provincial state. To do this, we will analyze judicial cases and government documents preserved in the Historical Archive of Mendoza. The aim of the study is to determine if the fears of the local elite, in the face of what they interpreted as growing post-revolutionary social conflict, were borne out by the information given in the sources; furthermore, we also aim to detect on which offenses against property they prioritized surveillance and punishment.En este trabajo nos centramos en un estudio específico de los robos ocurridos en la jurisdicción de Mendoza en el momento de conformación del estado provincial. Para ello analizaremos expedientes judiciales y documentos gubernamentales conservados en el Archivo Histórico de Mendoza. El objetivo del estudio apunta a determinar si los temores de la élite local, ante lo que ella interpretaba como una creciente conflictividad social pos revolucionaria, se correspondieron con lo planteado en las fuentes; no obstante, también buscamos detectar sobre qué atentados contra la propiedad focalizaron la vigilancia y punición.

  6. Lista de sírfidos afidófagos y primeros registros de Pseudodoros clavatus y Eupeodes rojasi (Diptera: Syrphidae, potenciales agentes de control biológico en la provincia de Mendoza, Argentina

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    Guillermo P. LÓPEZ GARCÍA

    2013-01-01

    Full Text Available Se presenta la primera lista de sírfidos afidófagos para la provincia de Mendoza y se reportan primeros registros de Pseudodoros clavatus Fabricius y Eu - peodes rojasi Marnef, potenciales agentes para el control biológico de áfidos plagas.

  7. Detrital and volcanic zircon U-Pb ages from southern Mendoza (Argentina): An insight on the source regions in the northern part of the Neuquén Basin

    Science.gov (United States)

    Naipauer, Maximiliano; Tapia, Felipe; Mescua, José; Farías, Marcelo; Pimentel, Marcio M.; Ramos, Victor A.

    2015-12-01

    The infill of the Neuquén Basin recorded the Meso-Cenozoic geological and tectonic evolution of the southern Central Andes being an excellent site to investigate how the pattern of detrital zircon ages varies trough time. In this work we analyze the U-Pb (LA-MC-ICP-MS) zircon ages from sedimentary and volcanic rocks related to synrift and retroarc stages of the northern part of the Neuquén Basin. These data define the crystallization age of the synrift volcanism at 223 ± 2 Ma (Cerro Negro Andesite) and the maximum depositional age of the original synrift sediments at ca. 204 Ma (El Freno Formation). Two different pulses of rifting could be recognized according to the absolute ages, the oldest developed during the Norian and the younger during the Rhaetian-Sinemurian. The source regions of the El Freno Formation show that the Choiyoi magmatic province was the main source rock of sediment supply. An important amount of detrital zircons with Triassic ages was identified and interpreted as a source area related to the synrift magmatism. The maximum depositional age calculated for the Tordillo Formation in the Atuel-La Valenciana depocenter is at ca. 149 Ma; as well as in other places of the Neuquén Basin, the U-Pb ages calculated in the Late Jurassic Tordillo Formation do not agree with the absolute age of the Kimmeridgian-Tithonian boundary (ca. 152 Ma). The main source region of sediment in the Tordillo Formation was the Andean magmatic arc. Basement regions were also present with age peaks at the Carboniferous, Neoproterozoic, and Mesoproterozoic; these regions were probably located to the east in the San Rafael Block. The pattern of zircon ages summarized for the Late Jurassic Tordillo and Lagunillas formations were interpreted as a record of the magmatic activity during the Triassic and Jurassic in the southern Central Andes. A waning of the magmatism is inferred to have happened during the Triassic. The evident lack of ages observed around ca. 200 Ma suggests

  8. Resistencias al orden formalizado por la Constitución de Mendoza de 1854 en el ámbito de la campaña

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    Inés Sanjurjo de Driollet

    2004-01-01

    Full Text Available The work analyzes the effective application of the principles of the modern constitutionalism in Mendoza after it was formalized the liberal order by means of the Constitution of 1854. The investigation tries to quarrel if in the period of this constitution life (1854-1895, nevertheless the bigger complexity of the state mechanisms and the politics of strengthening the legal authority on the territory, there were spaces that escaped to this power, or practices resistant to the principles in vogue. The work has put on particular attention to the rural localities, which for the distances or small accessibility, is estimated they were less inclined to the changes and less exposed to the state control.El trabajo analiza la efectiva aplicación de los principios del moderno constitucionalismo en Mendoza luego de formalizado el orden liberal mediante la carta magna provincial de 1854. Trata de averiguar, si en el período de su vigencia (1854-1895, no obstante el proceso de complejización del aparato estatal y la política de afianzamiento de su potestad sobre el territorio, quedaron espacios que escaparon a ese poder, o se dieron prácticas resistentes a los principios en boga. Se ha puesto particular atención a las localidades de la campaña, que por las distancias o la poca accesibilidad, se estima eran poco proclives a los cambios y estaban menos expuestas al control estatal.

  9. ALGUNAS CONCEPTUALIZACIONES Y ENFOQUES DOMINANTES EN LA GESTIÓN HÍDRICA DEL OASIS NORTE DE LA PROVINCIA DE MENDOZA, ARGENTINA

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    Virgínia Grosso

    2012-08-01

    Full Text Available  Mendoza, provincia árida del centro oeste de la República Argentina, ha vivenciado en los últimos tiempos la profundización del debate sobre la problemática de la escasez de agua. Este trabajo tiene por objetivo aproximarse a las respuestas de las siguientes preguntas: ¿qué factores han construido y construyen la denominada escasez hídrica en la provincia? ¿Se presenta de manera homogénea en todo el territorio mendocino? Para abordarlas, primeramente, se analizarán y correlacionarán los aportes teóricos de la nueva economía y cultura del agua y de la teoría y problación-recursos en torno a la noción de escasez. Y en segundo lugar, se identificarán las problemáticas hídricas (de apropiación, gestión y uso que se observan a lo largo de la cuenca del río Mendoza.

  10. La colección de armas de Íñigo López de Mendoza, V duque del Infantado

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    González Ramos, Roberto

    2014-12-01

    Full Text Available Don Íñigo López de Mendoza, 5th Duke of the Infantado, was one of the major arms collectors of his day. This essay deals with the content of his armoury, as well as the reasons and mechanism of its creation in the 16th Century. Further more, the text focuses on the uses of the arms of Don Iñigo and with the degree of knowledge Infantado had of what today we understand as modern collectionism.Don Íñigo López de Mendoza, V duque del Infantado, fue uno de los coleccionistas de armas más importantes de la Europa del Siglo XVI. Este artículo se centra en el estudio de su armería analizando su contenido y explicándolo para entender los mecanismos y las razones de su creación, así como de su uso y adecuación a lo que hoy entendemos como coleccionismo moderno.

  11. LA PROFUNDIZACIÓN DE LA RACIONALIDAD INSTRUMENTAL COMO ESTRATEGIA DE LOS PODEROSOS FRENTE AL CAMBIO AMBIENTAL GLOBAL EN MENDOZA – ARGENTINA

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    Jorge Daniel Ivars

    2012-12-01

    Full Text Available En el presente artículo nos proponemos describir la racionalidad subyacente a las estrategias de adaptación al cambio ambiental global de los agentes poderosos de la vitivinicultura en Mendoza, Argentina. En términos estrictamente físicos, el Cambio Ambiental Global se presenta como un aumento de las temperaturas promedio a nivel global, las repercusiones de este cambio serán diferentes según sea la zona geográfica del planeta que se considere. En el oasis norte de la Provincia de Mendoza se espera una reducción en los caudales del Río que lo alimenta. Frente a esta situación, los actores poderosos de la vitivinicultura mendocina han optado por estrategias de adaptación tendientes a profundizar la racionalidad instrumental, característica de estos grupos, para hacer frente al cambio ambiental global: obtener aguas en mayor cantidad y calidad a través del traslado de sus explotaciones a zonas de montaña ubicadas aguas arriba del río  y búsqueda de mercados internacionales, entre otras.

  12. Les variations récentes (1975-2000 de l’englacement dans le Massif de l’Aconcagua (Mendoza, Argentine

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    Julie Le Gall

    2008-03-01

    Full Text Available La région de Mendoza est particulièrement vulnérable au réchauffement climatique. Les glaciers du massif de l’Aconcagua ont amorcé un important retrait depuis la fin du Petit Âge de Glace. Or la disparition de ces glaciers risque d’entraîner une modification des régimes hydrologiques qui, jusqu’à présent, se caractérisaient par de hautes eaux estivales. Ce pic estival pourrait à l’avenir être atténué et remettre en cause les stratégies de gestion de la ressource en eau. Nous faisons ici le point sur les variations récentes de l’englacement et tentons de dessiner un scénario prospectif.Mendoza area is highly vulnerable to the global warming. The glaciers of the Aconcagua massif are currently shrinking, this trend of retreat began at the end of the Little Ice Age. The disappearance of glaciers may modify hydrological regimes. The discharge is currently at maximum during summer (related to glacier melt, but the peak discharge may occur during spring (related to snow melt in the next future. In this paper we synthesize the recent variations of the glaciers and propose a pattern of future variations.

  13. Active orogeny of the south-central Andes studied with GPS geodesy Orogenia activa de los Andes centro-australes estudiada mediante geodesia de GPS

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    E. Kendrick

    2006-12-01

    Full Text Available We present GPS measurements of the crustal velocity field in the southern Central Andes between the Santa Cruz corner and the Malargüe fold and thrust belt, and model this interseismic velocity field as the combination of an ephemeral, elastic signal associated with locking of the main plate boundary, and a steady and non-reversing component of displacement associated with localized backarc convergence and growth of the mountain belt. We find that this second component, i.e. the ongoing and permanent displacement of the forearc and the high Andes relative to the craton, can be modeled very well as a steady clockwise rotation of an Andean microplate about a pole located in southern Argentina. Near the Malargüe Basin, this microplate (or block is moving nearly parallel to the strike of the orogen, transporting material towards the bend in the central Andes. Farther north, in the southern limb of the Central Andes, the motion of this same crustal block is directed nearly perpendicular to the strike of the mountain belt. Our results suggest that permanent deformation rates in the backarc range from a maximum of ~ 6-7 mm/yr in the Bolivian Subandes to less than ~ 3 mm/yr in the Argentine Precordillera and Malargue fold and thrust belt. It is likely that most active backarc deformation is accruing in a narrow zone (~ 50 km wide associated with the backarc boundary (usually defined as the thrust front though at this stage it is impossible to distinguish whether specific backarc structures are actively accruing strain.Se presentan mediciones GPS del campo de velocidad en los Andes centro-australes entre el extremo norte de Santa Cruz y la faja plegada de Malargüe. Se modela el campo de velocidad intersísmico como la combinación de una señal elástico/efímera asociada con el anclaje del límite principal de placas, y una componente constante, no reversible de desplazamiento asociada con una convergencia localizada en el retroarco y crecimiento del

  14. Evolución tectonomagmática de los Andes bolivianos Tectonomagmaticevolution of the Bolivian Andes

    Directory of Open Access Journals (Sweden)

    Néstor Jiménez

    2009-10-01

    Full Text Available Los Andes bolivianos ocuparonuna posición de retroarco durante gran parte del Fanerozoico. En su evoluciónse reconoce una primera etapa, restringida al Paleozoico inferior, en la quehubo una gran transferencia de material sedimentario en la corteza superior, yuna segunda en la que predominó el reciclaje de la masa cortical. A lo largodel Paleozoico inferior, una cuenca marina epicratónica se formó entre elcratón de Amazonia, el macizo Arequipa-Antofalla, y el macizo Pampeanofuncionando inicialmente como cuenca de retroarco y luego como cuenca deantepaís hasta colmatarse en el Paleozoico superior. En este lapso ocurrierontres etapas de deformación: La fase oclóyica (límite Ordovícico-Silúrico decarácter restringido, la fase eohercínica (límite Devónico-Carbonífero, y lafase hercínica (Carbonífero Superior también de influencia areal restringida.En el Mesozoico, se registraron aún breves incursiones marinas antes que en elEoceno comience a edificarse una protocordillera. El solevantamiento general detoda la región centroandina, se inició en el Oligoceno Superior afectando alAltiplano y la Cordillera Oriental actuales. Este solevantamiento ocurrió entres etapas limitadas por la formación de superficies de erosión datadas en 18y 10 Ma. La ladera oeste de la Cordillera Oriental, denominada faja de Huarina,tuvo un rol muy importante en la evolución de la región centroandina. Además decobijar a gran parte del magmatismo de retroarco, en esta faja ocurrió la mayorsubsidencia de la cuenca paleozoica. En esta faja ocurrieron preferentementedurante el Mesozoico, procesos de rifting y de adelgazamiento litosférico. Enel Paleógeno, la faja de Huarinas fue la primera en ser solevantada aislando lacuenca altiplánica del interior del continente, y durante el OligocenoSuperior, se constituyó en el cinturón retrocabalgante del orógeno. Ladeformación en el Altiplano y la Cordillera Oriental concluyó hace 10 Ma cuandose form

  15. La realización práctica del origen: Algunas razones del devenir étnico y campesino en Mendoza The accomplishment of the origin: A few reasons to become ethnic and peasant in Mendoza

    Directory of Open Access Journals (Sweden)

    Germán Darío Fernández

    2010-06-01

    Full Text Available En la misma dirección de las políticas de acción afirmativa norteamericanas, la Universidad Nacional de Cuyo otorga, desde 2003, becas y cupos a estudiantes de zonas rurales y de comunidades originarias. La Universidad privilegia el criterio de origen geográfico y cultural antes que el criterio socioeconómico. Así, migran a la ciudad de Mendoza jóvenes becarios, los cuales interactúan, en mejores condiciones de acceso a bienes y servicios, con un nuevo entorno sociocultural. Hacen realidad y practican en la ciudad su pertenencia a las categorías étnica, campesina y estudiantil. Se habla de "origen" en este artículo como un hacer situado en lugar de considerarlo como el hecho de "haber nacido en". Describiendo la experiencia intercultural de los becarios, dos ideas son postuladas. En primer término, el origen se actúa día a día (es una performance ante tribunales informales, utilizando un conocimiento práctico de reglas comunes. En segundo lugar, el origen se merece según la labor y el esfuerzo del actor. De este modo, en la experiencia de los becarios mendocinos, ser étnico o campesino es más bien un asunto del hacer en situaciones concretas con otros, antes que un hecho de nacimiento, de esencia o de herencia.Similar to affirmative action politics in North America, the University of Cuyo, in Argentina, provides scholarships and quotas since 2003 to indigenous and peasant students. The criterion of geographic and cultural origin is more important than socio-economical criterion. Thus, Huarpes indigenous young people migrate to the downtown area, where they found new social benefits and had the opportunity to experience intercultural encounters. They accomplish in downtown area their membership to three categories, indigenous, peasant and student. "Origin" is considered in this paper as a situated doing instead of considering it as the fact of "being born in". In describing students' experience, two ideas are stated. First, the

  16. Immune Serum Produced by DNA Vaccination Protects Hamsters against Lethal Respiratory Challenge with Andes Virus

    Science.gov (United States)

    2008-02-01

    pulmonary syndrome in Argentina. Possibility of person to person transmission. Medicina (Buenos Aires) 56: 709–711. 8. Ferres, M., P. Vial, C. Marco, L...transmission of Andes virus. Medicina (Buenos Aires) 58(Suppl. 1):27–36. 20. Padula, P. J., A. Edelstein, S. D. Miguel, N. M. Lopez, C. M. Rossi, and R

  17. Millennial-scale vegetation changes in the tropical Andes using ecological grouping and ordination methods

    NARCIS (Netherlands)

    Urrego, D.H.; Hooghiemstra, H.; Rama-Corredor, O.; Martrat, B.; Grimalt, J.O.; Thompson, L.; Bush, M.B.; González-Carranza, Z.; Hanselman, J.; Valencia, B.; Velásquez-Ruiz, C.

    2016-01-01

    We compare eight pollen records reflecting climatic and environmental change from northern and southern sites in the tropical Andes. Our analysis focuses on the last 30 000 years, with particular emphasis on the Pleistocene to Holocene transition. We explore ecological grouping and downcore ordinati

  18. High altitude C4 grasslands in the northern Andes: relicts from glacial conditions?

    NARCIS (Netherlands)

    Boom, A.; Mora, G.; Cleef, A.M.; Hooghiemstra, H.

    2001-01-01

    The altitudinal vegetation distribution in the northern Andes during glacial time differed from the present-day conditions as a result of temperature and precipitation change. New evidence indicate that as a response to a reduced atmospheric partial CO2 pressure (pCO2), the competitive balance betwe

  19. Cloud forest restoration for erosion control in a Kichwa community of the Ecuadorian central Andes Mountains

    Science.gov (United States)

    Backus, L.; Giordanengo, J.; Sacatoro, I.

    2013-12-01

    The Denver Professional Chapter of Engineers Without Borders (EWB) has begun conducting erosion control projects in the Kichwa communities of Malingua Pamba in the Andes Mountains south of Quito, Ecuador. In many high elevation areas in this region, erosion of volcanic soils on steep hillsides (i.e., teach these skills to adjacent villages.

  20. The forest vegetation of Ramal de Guaramacal in the Venezuelan Andes

    NARCIS (Netherlands)

    Cuello A., N.L.; Cleef, A.M.

    2009-01-01

    Montane forest community composition of Ramal de Guaramacal, Venezuelan Andes, was studied along the altitudinal gradient on both sides of the range with different slope expositions. Thirty five 0.1 ha plots were surveyed, with variable intervals of 30 to 150 meters between 1350 m and 2890 m and

  1. The forest vegetation of Ramal de Guaramacal in the Venezuelan Andes

    NARCIS (Netherlands)

    Cuello, A.N.L.; Cleef, A.M.

    2009-01-01

    Montane forest community composition of Ranial de Guaramacal, Venezuelan Andes, was studied along the altitudinal gradient on both sides of the range with different slope expositions. Thirty five 0.1 ha plots were Surveyed, with variable intervals of 30 to 150 meters between 1350 in and 2890 in and

  2. Climate Change in the High Andes:implications and adaptation strategies for small-scale farmers

    NARCIS (Netherlands)

    Perez, C.; Nicklin, C.; Dangles, O.; Vanek, S.; Sherwood, S.G.; Halloy, S.; Garrett, K.A.; Forbes, G.A.

    2010-01-01

    Abstract: Global climate change represents a major threat to sustainable farming in the Andes. Farmers have used local ecological knowledge and intricate production systems to cope, adapt and reorganize to meet climate uncertainty and risk, which have always been a fact of life. Those traditional

  3. A millennium of metallurgy recorded by lake sediments from Morococha, Peruvian Andes.

    Science.gov (United States)

    Cooke, Colin A; Abbott, Mark B; Wolfe, Alexander P; Kittleson, John L

    2007-05-15

    To date, information concerning pre-Colonial metallurgy in South America has largely been limited to the archaeological record of artifacts. Here, we reconstruct a millennium of smelting activity in the Peruvian Andes using the lake-sediment stratigraphy of atmospherically derived metals (Pb, Zn, Cu, Ag, Sb, Bi, and Ti) and lead isotopic ratios (206Pb/ 207Pb) associated with smelting from the Morococha mining region in the central Peruvian Andes. The earliest evidence for metallurgy occurs ca. 1000 A.D., coinciding with the fall of the Wari Empire and decentralization of local populations. Smelting during this interval appears to have been aimed at copper and copper alloys, because of large increases in Zn and Cu relative to Pb. A subsequent switch to silver metallurgy under Inca control (ca. 1450 to conquest, 1533 A.D.) is indicated by increases in Pb, Sb, and Bi, a conclusion supported by further increases of these metals during Colonial mining, which targeted silver extraction. Rapid development of the central Andes during the 20th century raised metal burdens by an order of magnitude above previous levels. Our results represent the first evidence for pre-Colonial smelting in the central Peruvian Andes, and corroborate the sensitivity of lake sediments to pre-Colonial metallurgical activity suggested by earlier findings from Bolivia.

  4. Angiosperm flora and biogeography of the páramo region of Colombia, northern Andes

    NARCIS (Netherlands)

    Londoño, C.; Cleef, A.; Madriñan, S.

    2014-01-01

    Páramo is the neotropical high elevation ecosystem in the northern Andes and Central America consisting of multiple dissected open areas above 3000 m a.s.l. Complex evolutionary processes that occurred within these ecosystems gave rise to a unique tropical Andean flora. Previous phytogeographical cl

  5. Hybrid Literacies: The Case of a Quechua Community in the Andes

    Science.gov (United States)

    de la Piedra, Maria Teresa

    2009-01-01

    Drawing on data from an ethnographic study in a Quechua rural community in the Peruvian Andes, this article examines hybrid literacy practices among bilingual rural speakers in the context of the household and the community. I examine the coexistence of two types of textual practices that operate side by side, at times integrated in the same…

  6. Natural gas across the Andes : a case study of an international business venture

    Energy Technology Data Exchange (ETDEWEB)

    Figueroa, E.B.; Smith, B.

    2002-07-01

    This book describes the challenges and complexities of constructing the GasAndes pipeline from Argentinian gas fields across the Andes to Santiago in Chile. The project was a joint international effort between Canada's NOVA Corporation, Chile's Gasco and Gener, and Argentina's Compania General de Combustibles and Techint Compania Tecnica Internacional. The book relates how NOVA Gas International, together with its partners, accomplished the task of constructing the first major natural gas pipeline across the Andes mountains despite significant challenges such as steep mountain slopes, many river crossings, high altitude, high winds and bitter cold. It describes how the partnership developed and how political and socio-economic issues were dealt with. It demonstrates how business practices were modified to deal with local conditions and to ensure that the fragile environment of the Andean meadows was protected. It also describes how the builders of the pipeline addressed the concerns of communities along the pipeline route. The pipeline was constructed at a time when democracy was returning and market economies were shifting from a reduced role of government in the energy sector. The 463 km GasAndes pipeline has been in operation since August 7, 1997. refs., tabs., figs.

  7. Evolution of crustal thickening in the central Andes, Bolivia

    Science.gov (United States)

    Eichelberger, Nathan; McQuarrie, Nadine; Ryan, Jamie; Karimi, Bobak; Beck, Susan; Zandt, George

    2015-09-01

    Paleoelevation histories from the central Andes in Bolivia have suggested that the geodynamic evolution of the region has been punctuated by periods of large-scale lithospheric removal that drive rapid increases in elevation at the surface. Here, we evaluate viable times and locations of material loss using a map-view reconstruction of the Bolivian orocline displacement field to forward-model predicted crustal thicknesses. Two volumetric models are presented that test assumed pre-deformation crustal thicknesses of 35 km and 40 km. Both models predict that modern crustal thicknesses were achieved first in the northern Eastern Cordillera (EC) by 30-20 Ma but remained below modern in the southern EC until ≤10 Ma. The Altiplano is predicted to have achieved modern crustal thickness after 10 Ma but only with a pre-deformation thickness of 50 km, including 10 km of sediment. At the final stage, the models predict 8-25% regional excess crustal volume compared to modern thickness, largely concentrated in the northern EC. The excess predicted volume from 20 to 0 Ma can be accounted for by: 1) crustal flow to the WC and/or Peru, 2) localized removal of the lower crust, or 3) a combination of the two. Only models with initial crustal thicknesses >35 km predict excess volumes sufficient to account for potential crustal thickness deficits in Peru and allow for lower crustal loss. However, both initial thickness models predict that modern crustal thicknesses were achieved over the same time periods that paleoelevation histories indicate the development of modern elevations. Localized removal of lower crust is only necessary in the northern EC where crustal thickness exceeds modern by 20 Ma, prior to paleoelevation estimates of modern elevations by 15 Ma. In the Altiplano, crustal thicknesses match modern values at 10 Ma and can only exceed modern values by 5 Ma, post-dating when modern elevations were thought to have been established. Collectively, these models predict that

  8. Refractory Minerals in Henan Province

    Institute of Scientific and Technical Information of China (English)

    JIN Qinguo; LI Jing; LIU Jiehua; LIU Yanjun

    2004-01-01

    Henan province is very rich in refractory minerals of many varieties including silica, dolomite, graphite,pearlite, sepiolite, olivine, and sillimanite group minerals, besides the abundant reserves of fireclay and bauxite,which lay a good foundation for the development of the refractories industry of the province. The paper introduces the reserves, distribution and character of the refractory minerals in Henan province.

  9. Episodic subgreenschist facies metamorphism in the Andes of Chile - is it a valid model?

    Science.gov (United States)

    Bevins, R. E.; Robinson, D.; Aguirre, L.; Vergara, M.

    2003-04-01

    The Central Andes of Chile are characterized by subgreenschist facies burial metamorphism that is reported as having developed in up to seven episodic cycles of some 40Myr duration. The main evidence in support of the model is reported as mineralogical breaks at major stratigraphic boundaries that are interpreted as documenting sharp breaks in metamorphic grade. Here we test this model by examination of the progressive secondary mineral development, reaction progress in mafic phyllosilicates, and topological variations of the low-grade assemblages in metabasites for Jurassic to Miocene sequences east of Santiago. The mafic phyllosilicates (smectite - mixed-layer chlorite/smectite - chlorite) show increasing reaction progress with stratigraphic age and there is a continuum across the main stratigraphic boundaries, such there is no offset or gap in the reaction progress at these boundaries. There are some differences in mineral assemblages between the various stratigraphic units, such as between prehnite+pumpellyite+/-laumonite or amphibole-bearing and non amphibole bearing rocks, from which contrasting subgreenschist facies can be recognised. However, consideration of the controls on mineral parageneses at subgreenschist facies conditions demonstrates that these different facies cannot be used solely as evidence of sharp breaks in metamorphic grade at unconformities, as has been reported in many previous publications for the Andes. The presently accepted model for the Central Andes, involving repeated cycles of episodic metamorphism developing in extensional basins, is, therefore, partly unfounded. Consideration of the overall tectonic evolution of this part of the Andes concurs that the burial metamorphism developed in extensional settings, but in only two events, namely in mid-late Cretaceous and Late Miocene times respectively. The results from this work suggest that the record of sharp metamorphic breaks and the episodic model of metamorphism reported for many

  10. Un réseau d'observation des glaciers dans les Andes tropicales

    Directory of Open Access Journals (Sweden)

    1995-01-01

    Full Text Available Par leur grande sensibilité au changement climatique, les glaciers tropicaux sont d’excellents indicateurs de l’évolution du climat et, en même temps, des objets hydrologiques susceptibles d’évoluer rapidement dans le futur. On montre que l’actuel recul accéléré des glaciers dans les Andes centrales et les conséquences qu’il peut avoir en matière hydrologique et de risques naturels rendent nécessaire un programme de surveillance de ces glaciers au niveau de toute la chaîne, ce que l’ORSTOM contribue à faire depuis 1991. UNA RED DE OBSERVACIÓN DE LOS GLACIARES EN LOS ANDES TROPICALES. Por su gran sensibilidad al cambio climático, los glaciares tropicales son excelentes indicadores de la evolución del clima, así como objectos hidrológicos susceptibles de una evolución rápida en el futuro. Considerando el actual retroceso acelerado de los glaciares en los Andes centrales y las consecuencias que puede tener a nivel hidrológico así como en el campo de los riesgos naturales, es necesario un programa de monitoreo de los glaciares a nivel de toda la cordillera, que es lo que ORSTOM contribuye a hacer desde 1991. A GLACIER MONITORING NETWORK IN THE TROPICAL ANDES. The high sensibility of Tropical glaciers to climatic forcing make it possible to use them as reliable indicators of climate evolution, as well as hydrological systems which could change rapidly in the future. Considering the present increase in glacier retreat in central Andes and the consequences induced by this evolution on water resources and natural hazards, a monitoring program at a large scale appears to be highly desirable. This has been the objective of ORSTOM since 1991.

  11. Hydrological cycles and trends in the NW Argentine Andes since 1940

    Science.gov (United States)

    Castino, Fabiana; Bookhagen, Bodo; Strecker, Manfred

    2016-04-01

    Strong spatiotemporal variability characterizes the hydrometeorological pattern in the NW Argentine Andes, draining parts of the most populated and economically important areas of South America. During the summer monsoon season (DJF), the eastern flanks of the central Andes are characterized by deep convection, exposing them to extreme hydrometeorological events. These often result in floods and landslides with disastrous effects on the local populations. Here, we analyze river discharge to explore long-term hydrological variability in NW Argentine Andes and the linked climate controlling processes. We rely on 13 daily river discharge time series relevant to drainage basins spanning several size orders (102-104 km2) starting in 1914 and define different hydro-climate indices both for the mean and the extreme hydrological events. We apply quantile regression to investigate long-term trends and spectral analysis associated with cross-correlation with SST-based climate indices to identify links to large-scale climate variability modes. River discharge presents a pronounced and coherent variability signal in South America, particularly for wide drainage basins, such as the Amazon and Paraná/La Plata rivers, strongly associated to Pacific and Atlantic Oceans Sea Surface Temperature (SST) anomalies (i.e. ENSO, PDO, AMO). Our analysis evidences that in the NW Argentine Andes, mean discharge values are characterized by statistically significant, mostly positive, long-term trends since 1940, whereas the extreme events present a more non-unidirectional trend pattern. Also, coherent multi-annual to multi-decadal cycles characterizing the discharge pattern have been identified, suggesting that processes linked to SST anomaly-modes strongly control the hydrometeorology variability in the NW Argentina Andes.

  12. Emplacement history and inflation evidence of a long basaltic lava flow located in Southern Payenia Volcanic Province, Argentina

    Science.gov (United States)

    Bernardi, Mauro I.; Bertotto, Gustavo W.; Jalowitzki, Tiago L. R.; Orihashi, Yuji; Ponce, Alexis D.

    2015-02-01

    The El Corcovo lava flow, from the Huanul shield volcano in the southern Mendoza province (central-western Argentina) traveled a distance of 70 km and covered a minimum area of ~ 415 km2. The flow emplacement was controlled both by extrinsic (e.g., topography) and intrinsic (e.g., lava supply rate, lava physicochemical characteristics) factors. The distal portion of the lava flow reached the Colorado River Valley, in La Pampa Province, where it spread and then was confined by earlier river channels. Cross-sections through the flow surveyed at several localities show two vesicular layers surrounding a dense central section, where vesicles are absent or clustered in sheet-shaped and cylindrical-shaped structures. Lavas of the El Corcovo flow are alkaline basalts with low values of viscosity. The morphological and structural characteristics of the flow and the presence of landforms associated with lava accumulation are the evidence of inflation. This process involved the formation of a tabular sheet flow up to 4 m of thick with a large areal extent in the proximal sectors, while at terminal sectors frontal lobes reached inflation values up to 10 m. The numerous swelling structures present at these portions of the flow suggest the movement of lava in lava tubes. We propose that this aspect and the low viscosity of the lava allowed the flow travel to a great distance on a gentle slope relief.

  13. Don Juan de Palafox y Mendoza, promotor del libre acceso a la información en el siglo XVII novo-hispano Don Juan de Palafox y Mendoza promoter of free access to information in the eighteenth century in New Spain

    OpenAIRE

    Rosa María Fernández de Zamora

    2011-01-01

    Don Juan de Palafox y Mendoza, arzobispo y virrey de la Nueva España y obispo de Puebla en el siglo XVII, ha sido motivo de numerosos estudios, pero lo que se desea resaltar en este escrito es su labor como fundador de la primera biblioteca pública de México y del continente americano, misma que hoy conocemos como Biblioteca Palafoxiana, y como promotor del libre acceso a la información. En el siglo XVIII, el obispo de Puebla, Francisco Fabián y Fuero, seguidor de las ideas de Palafox, enriqu...

  14. Migraciones en la puna: su relación con el uso de los recursos naturales del departamento Los Andes Migraciones en la puna: su relación con el uso de los recursos naturales del departamento Los Andes

    Directory of Open Access Journals (Sweden)

    Francisco R. Barbarán

    2009-12-01

    Full Text Available From an historic and demographic perspective, as well as the use of natural resources, we analyzed the relationship between human migrations and the economic activities of Los Andes Department, West of the Salta Province, in NW Argentina. Using the residual method, we calculated migratory balances between Argentinean population censuses carried out in 1947,1960, 1970, 1980 and 2001. The migratory balances were negative for all the periods studied. When the train started to run through Ramal C-14, the workers who built it have to find jobs somewhere else. At the same time, the railway made easier for the natives, to find better economicopportunities out of the Puna. The close of mine La Casualidad by the end of the 70’s, the low creation of jobs by the remaining mining operations, focused in to hire qualified technicians no available in Los Andes and the privatization of the railway in early 90’s, were important factors of emigration. Despite of cattle rising as the main economic activity in rural areas, it is practiced without any technology of management. The overgrazing caused for that reason, has reduced almost to the half the quantity of sheep by inhabitant between 1947 and 2001. That is why the local people have to press more on the wildlife, trading illegally with vicuña (Vicugna vicugna fiber. Despite of a touristic development plan, a law promoting sheep rising and a census of vicuña population carried out by the provincial government, these recent actions should be part of a development project of regional scale, oriented to the sustainable use of the natural resources of Los Andes Department. That project would create jobs and discourage emigration.Desde una perspectiva histórica, demográfica y del uso de los recursos naturales, analizamos la relación existente entre las migraciones humanas y las actividades económicas en el departamento Los Andes, ubicado al W de la provincia de Salta, en el Noroeste Argentino. Usando el m

  15. The High Andean Cordillera of central Argentina and Chile along the Piuquenes Pass-Cordon del Portillo transect: Darwin's pioneering observations compared with modern geology La Alta Cordillera de los Andes del centro de Argentina y Chile a lo largo de la transecta del Paso Piuquenes-Cordón del Portillo: Las observaciones pioneras de Darwin comparadas con la geología moderna

    Directory of Open Access Journals (Sweden)

    Laura Giambiagi

    2009-04-01

    Full Text Available The geological observations made by Darwin in 1835 during his crossing of the Andes from Santiago to Mendoza via the Piuquenes Pass and Cordón del Portillo are compared with the present geological knowledge of the Cordillera Principal and Cordillera Frontal at 33°-34°S. The analysis of the complex stratigraphy of the Cordillera Principal, the imbricated structure of the Aconcagua fold and thrust belt, as well as the stratigraphy and structure of the inter mountain foreland Tunuyán Basin, allows to assess the pioneer observations of Darwin. He recognized the old metamorphic basement and the granitoids and volcanic sequences of late Paleozoic to Triassic age of the Cordillera Frontal, established the Cretaceous age of the marine successions cropping out along the eastern Cordillera Principal and studied the conglomeratic deposits associated with the uplift of the Cordillera in the Alto Tunuyán Basin. Based on the study of clast provenance of the synorogenic deposits of the Alto Tunuyán Basin, Darwin recognized that the Cordillera Frontal was uplifted later than the Cordillera Principal. The present knowledge of this sector of the Andean Cordillera confirms his pioneer observations and show that Darwin was one of the first scientists ever in realizing that in an orogenic system the sequence of uplift and deformation proceeds from hinterland towards foreland, according to a process that is exceptionally well-illustrated along the Piuquenes-Cordón del Portillo transect.Las observaciones geológicas efectuadas por Darwin en 1935 durante su cruce de la Cordillera de Los Andes entre Santiago y Mendoza realizado en 1835 a través de los pasos del Portillo y Piuquenes son examinadas y comparadas con el conocimiento actual existente de las Cordilleras Principal y Frontal entre los 33°-34°S. El análisis de la compleja estratigrafía de la Cordillera Principal, la estructura de las diferentes láminas imbricadas de la faja plegada y corrida del

  16. Paleozoic evolution of active margin basins in the southern Central Andes (northwestern Argentina and northern Chile)

    Science.gov (United States)

    Bahlburg, H.; Breitkreuz, C.

    The geodynamic evolution of the Paleozoic continental margin of Gondwana in the region of the southern Central Andes is characterized by the westward progression of orogenic basin formation through time. The Ordovician basin in the northwest Argentinian Cordillera Oriental and Puna originated as an Early Ordovician back-arc basin. The contemporaneous magmatic arc of an east-dipping subduction zone was presumably located in northern Chile. In the back-arc basin, a ca. 3500 meter, fining-up volcaniclastic apron connected to the arc formed during the Arenigian. Increased subsidence in the late Arenigian allowed for the accomodation of large volumes of volcaniclastic turbidites during the Middle Ordovician. Subsidence and sedimentation were caused by the onset of collision between the para-autochthonous Arequipa Massif Terrane (AMT) and the South American margin at the Arenigian-Llanvirnian transition. This led to eastward thrusting of the arc complex over its back-arc basin and, consequently, to its transformation into a marine foreland basin. As a result of thrusting in the west, a flexural bulge formed in the east, leading to uplift and emergence of the Cordillera Oriental shelf during the Guandacol Event at the Arenigian-Llanvirnian transition. The basin fill was folded during the terminal collision of the AMT during the Oclóyic Orogeny (Ashgillian). The folded strata were intruded post-tectonically by the presumably Silurian granitoids of the "Faja Eruptiva de la Puna Oriental." The orogeny led to the formation of the positive area of the Arco Puneño. West of the Arco Puneño, a further marine basin developed during the Early Devonian, the eastern shelf of which occupied the area of the Cordillera Occidental, Depresión Preandina, and Precordillera. The corresponding deep marine turbidite basin was located in the region of the Cordillera de la Costa. Deposition continued until the basin fill was folded in the early Late Carboniferous Toco Orogeny. The basin

  17. Trends and ENSO/AAO Driven Variability in NDVI Derived Productivity and Phenology alongside the Andes Mountains

    National Research Council Canada - National Science Library

    Willem JD VanLeeuwen; Kyle Hartfield; Marcelo Miranda; Francisco J Meza

    2013-01-01

      Increasing water use and droughts, along with climate variability and land use change, have seriously altered vegetation growth patterns and ecosystem response in several regions alongside the Andes Mountains...

  18. Lake Andes National Wildlife Refuge Waterfowl Production Area District: Narrative report: January 1 through December 31, 1966

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This annual narrative report for Lake Andes NWR- Waterfowl Production Area District outlines Refuge accomplishments during the 1966 calendar year. The report begins...

  19. Lake Andes National Wildlife Refuge Complex Refuge Lands Geographic Information System (RLGIS) habitat mapping project : 2008 season

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — Mapping of all of the vegetation on the uplands present on the Waterfowl Production Areas (WP As) and Refuge lands managed by the Lake Andes NWR began in June of...

  20. Fort Niobrara Easement Refuges: Lake Andes, Lake Arconge, Carr, Eagle Creek: May 1, 1942 to August 31, 1942

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report summarizes activities on Lake Andes NWR between May and August of 1942. Lake Arconge Refuge, Carr Refuge, and Eagle Creek Refuge are also...

  1. Fort Niobrara Easement Refuges: Lake Andes, Lake Arconge, Carr, Eagle Creek: Narrative report: Sept. to Dec. 1943

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This narrative report summarizes activities on Lake Andes, Lake Arconge, Carr, and Eagle Creek Refuges between September and December of 1943. Weather conditions,...

  2. Screening for new accumulator plants in Andes Range mines

    Science.gov (United States)

    Bech, Jaume; Roca, Núria

    2016-04-01

    accumulated considerable concentrations of Cu and Zn. The species from the genus Bidens (Asteraceae) were able not only to accumulate high shoot As concentrations (> 1000 μg g-1 in B. cynapiifolia from Peru) but also considerable amounts of Pb (B. humilis from Chile). The highest Cu shoot concentrations were found in Mullinum spinosum (870 μg g-1) and in B. cynapiifolia (620 μg g-1). The shoot accumulation of Zn was highest in Baccharis amdatensis (>1900 μg g-1) and in Rumex crispus (1300 μg g-1) from the Ag mine in Ecuador (Bech et al., 2002). In the Peruvian Andes, B. triplinervia can be considered interesting for phytostabilization, due to its capacity to restrict the accumulation of elevated amounts of Pb and Zn in the shoots.

  3. The Largest Holocene Eruption of the Central Andes Found

    Science.gov (United States)

    Fernandez-Turiel, J.; Rodriguez-Gonzalez, A.; Saavedra, J.; Perez-Torrado, F.; Carracedo, J.; Osterrieth, M.; Carrizo, J.; Esteban, G.

    2013-12-01

    We present new data and interpretation about a major eruption -spreading ˜110 km3 ashes over 440.000 km2- long thought to have occurred around 4200 years ago in the Cerro Blanco Volcanic Complex (CBVC) in NW Argentina. This eruption may be the biggest during the past five millennia in the Central Volcanic Zone of the Andes, and possibly one of the largest Holocene eruptions in the world. The environmental effects of this voluminous eruption are still noticeable, as evidenced by the high content of arsenic and other trace elements in the groundwaters of the Chacopampean Plain. The recognition of this significant volcanic event may shed new light on interpretations of critical changes observed in the mid-Holocene paleontological and archaeological records, and offers researchers an excellent, extensive regional chronostratigraphic marker for reconstructing mid-Holocene geological history over a wide geographical area of South America. More than 100 ashes were sampled in Argentina, Chile and Uruguay during different field campaigns. Ash samples were characterized by scanning electron microscope (SEM), X-ray diffraction (XRD), grain size distributions laser diffraction, and geochemically by electron microprobe (EMPA) and laser ablation-HR-ICP-MS. New and published 14C ages were calibrated to calendar years BP. The age of the most recent CBVC eruption is 4407-4093 cal y BP, indirectly dated by 14C of associated organic sediment within the lower part of a proximal fall deposit of this event (26°53'16.05"S-67°44'48.68"W). This is the youngest record of a major volcanic event in the Southern Puna. This age is consistent with other radiocarbon dates of organic matter in palaeosols underlying or overlying distal ash fall deposits. Based on their products, all of rhyolitic composition, we have distinguished 8 main episodes during the evolution of the most recent CBVC eruption: 1) the eruption began with a white rhyolite lava dome extrusion; 2) followed by a Plinian

  4. Conflictos sociales en Mendoza entre dos crisis, 1890-1916: Una larga lucha de los trabajadores por la conquista de sus derechos laborales

    Directory of Open Access Journals (Sweden)

    Rodolfo Richard-Jorba

    2010-06-01

    Full Text Available Este artículo contribuye a la reconstrucción de la historia del mundo de los trabajadores en Mendoza. Las fuentes revisadas y la sistematización de información dispersa han permitido profundizar en los conocimientos hasta ahora generados, sacando a luz una parte significativa del desarrollo capitalista centrado en la agroindustria vitivinícola. Las fuentes principales para seguir los conflictos han sido los diarios mendocinos, por lo que nuestro abordaje constituye una aproximación que esperamos poder ampliar en el futuro. En este artículo presentamos los conflictos sociales en el contexto de períodos de crisis y de auge económico. Comenzamos por la crisis de 1890 y concluimos con la crisis provocada por la Primera Guerra Mundial y los cambios políticos que sobrevendrían a partir de 1916-1918

  5. RECOMPOSICIÓN ECONÓMICA DE LAS BURGUESÍAS REGIONALES: LA BURGUESÍA VITIVINÍCOLA EN LA PROVINCIA DE MENDOZA, ARGENTINA (1990-2011

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    ADRIANA CHAZARRETA

    2014-01-01

    Full Text Available Este artículo se propone comprender la recomposición de la burguesía vitivinícola en Mendoza a partir de la reestructuración de la actividad que comienza a principios de los `90. Este trabajo permite mostrar el peso relevante que en la estructura económica, aún conservan los sectores ligados a capitales locales y/o nacionales, pese al considerable ingreso de empresas transnacionales y extranjeras. El diseño de investigación se basa en una estrategia de triangulación metodológica, combinando técnicas de recolección de datos cuantitativos y cualitativos, y el uso de distintas fuentes de datos secundarias y primarias.

  6. Justicia de proximidad y gobierno político-militar en la frontera. Equipamiento institucional del Valle de Uco (Mendoza durante el proceso revolucionario (1810-1820

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    Eugenia Molina

    2014-12-01

    Full Text Available El trabajo reconstruye el proceso de equipamiento institucional de la campaña sur de Mendoza durante el proceso revolucionario. Focaliza la atención en la trama de funcionarios designados para la villa de San Carlos y el Valle de Uco, con el objetivo de  mostrar las articulaciones entre justicia de proximidad, gobierno político-militar y construcción de la legitimidad. La hipótesis es que las propias características de un espacio de frontera se complejizaron en el contexto de guerra, atravesaron la territorialización de este ámbito de la jurisdicción mendocina al hacer que la solución de la cuestión de la distancia tuviera un rol clave en las estrategias para gobernarlo.

  7. Necesidad de transparencia y legalidad en la gestión y uso de las aguas subterráneas (El reciente caso de la Provincia de Mendoza

    Directory of Open Access Journals (Sweden)

    María Valentina Erice

    2013-12-01

    Full Text Available En Mendoza las aguas subterráneas son un recurso natural indispensable para la subsistencia y de gran importancia para el desarrollo provincial, ya que tienen un valor no solo económico y estratégico, sino también social y ambiental. La prevención de la sobreexplotación de los acuíferos y de la contaminación de estas aguas constituye una de las preocupaciones más serias a la que se enfrentan los encargados de gestionar su uso eficiente. Para ello resulta necesario aplicar políticas de ahorro y conservación, contar con un moderno Derecho de aguas preciso, claro, coherente y conservacionista, encaminado a dar soluciones eficaces a los problemas que hoy se nos presentan y que la gestión se realice con rectitud, transparencia y respetando la Constitución y la leyes.

  8. Solar energy use feasibility and foreseeable impacts of the recent reforms to the urban and building code: Proposals for the city of Mendoza, Argentina

    Directory of Open Access Journals (Sweden)

    Mariela Edith Arboit

    2012-06-01

    Full Text Available El objetivo del trabajo es generar conocimientos que permitan realizar propuestas conducentes a una mayor sostenibilidad energético-ambiental de los sistemas urbanos regionales, en función de sus características morfológicas y del recurso solar disponible. En una primera etapa se ha realizado un análisis de las zonas de alta densidad edilicia a partir de los resultados de indicadores relevantes y su análisis estadístico. Los indicadores expresan relaciones entre morfología urbana y acceso al recurso solar en el Área Metropolitana de Mendoza (AMM, e incluyen: Factor de Asoleamiento Efectivo (FAE y el Factor de Asoleamiento Volumétrico (FAV. Los resultados del análisis estadístico han permitido evaluar las correlaciones de cada variable morfológica sobre cada indicador, según distintas alternativas morfológicas y combinaciones de las mismas, lo que constituye la parte sustancial de este trabajo. En una segunda etapa se presentan los resultados parciales de un estudio que tiene como objetivo determinar los impactos energéticos ambientales de las recientes reformas del Código Urbano y de Edificación de la ciudad en estudio, en función del FAV y estimar la reducción del acceso al recurso solar respecto a la situación de referencia (actual, sin cambios y situación futura, en una ciudad con el carácter único de Mendoza como “ciudad-oasis”. Los resultados obtenidos hasta el momento indican que la reducción de la energía solar disponible por unidad de volumen construido sería sustancial: 46,32% para muros al norte y 60,38% techos.

  9. Morfometría de la escarpa de falla histórica identificada al norte del cerro La Cal, zona de falla La Cal, Mendoza

    Directory of Open Access Journals (Sweden)

    F. Mingorance

    2006-12-01

    Full Text Available Investigación morfométrica y paleosísmica histórica fue llevada a cabo en el Norte de Mendoza con el objeto de caracterizar y cuantificar a las evidencias geomorfológicas de ruptura superficial histórica identificadas en el sector septentrional de la zona de falla La Cal. Integración e interpretación de datos e información científica multidisciplinaria, sugieren fuertemente que la ruptura superficial histórica identificada estuvo asociada al terremoto destructivo de Mendoza ocurrido en 1861. La deformación superficial histórica ocurrió casi en su totalidad a lo largo de una escarpa prehistórica previa, mediante una combinación de fallamiento de corrimiento y plegamiento cercano a la superficie. Dos elementos de pendiente históricos de bajo relieve fueron reconocidos en la escarpa compuesta Villavicencio Sur, los cuales se diferencian de la típica secuencia de formas desarrollada en escarpas de falla normal históricas. El "remanente de cara libre", el elemento de pendiente superior, y la "pendiente de colapso", el elemento inferior, son controlados por la fricción interna y por la gravedad y la fricción de deslizamiento del material aluvial, respectivamente. La metodología paleosísmica histórica discutida en este trabajo, parece ser particularmente útil en el período de tiempo que cubre la mayor parte del registro histórico de terremotos destructivos en Argentina, los pasados 350 años, lapso en el cual la mayoría de los métodos de datación absoluta no son muy efectivos.

  10. Phylogeny and biogeography of the New World siskins and goldfinches: rapid, recent diversification in the Central Andes.

    Science.gov (United States)

    Beckman, Elizabeth J; Witt, Christopher C

    2015-06-01

    Time-calibrated molecular phylogenies can help us to understand the origins of the diverse and unique Andean avifauna. Previous studies have shown that the tempo of diversification differed between the Andes and adjacent lowland regions of South America. Andean taxa were found to have speciated more recently and to have avoided the decelerated diversification that is typical of Neotropical lowland clades. The South American siskins, a Pleistocene finch radiation, may typify this Andean pattern. We investigated the phylogenetic biogeography of all the New World siskins and goldfinches in new detail. To understand the specific role of the Andes in siskin diversification, we asked: (1) Was diversification faster in Andean siskin lineages relative to non-Andean ones? (2) Did siskin lineages move into and out of the Andes at different rates? We found that siskin lineages in the Andes had higher diversification rates and higher outward dispersal rates than siskin lineages outside the Andes. We conclude that páramo expansion and contraction in response to Pleistocene climatic cycles caused accelerated diversification and outward dispersal in Andean siskins. The younger average age of bird species in the Andes compared to lowland South America may be attributable to bursts of recent diversification in siskins and several other vagile, open-habitat clades. Copyright © 2015 Elsevier Inc. All rights reserved.

  11. Nine Provinces Submerged

    Institute of Scientific and Technical Information of China (English)

    LIU YUNYUN

    2010-01-01

    @@ After being plagued with severe drought earlier this year,the southern part of China has been ravaged by heavy rainfall since May. According to the China Meteorological Administration (CMA),from June 23-25 a new round of storms swept the southern part of the country including all nine provinces in the south.It was the 11th round of storms since May 5,said CMA.

  12. Don Juan de Palafox y Mendoza, promotor del libre acceso a la información en el siglo XVII novo-hispano Don Juan de Palafox y Mendoza promoter of free access to information in the eighteenth century in New Spain

    Directory of Open Access Journals (Sweden)

    Rosa María Fernández de Zamora

    2011-08-01

    Full Text Available Don Juan de Palafox y Mendoza, arzobispo y virrey de la Nueva España y obispo de Puebla en el siglo XVII, ha sido motivo de numerosos estudios, pero lo que se desea resaltar en este escrito es su labor como fundador de la primera biblioteca pública de México y del continente americano, misma que hoy conocemos como Biblioteca Palafoxiana, y como promotor del libre acceso a la información. En el siglo XVIII, el obispo de Puebla, Francisco Fabián y Fuero, seguidor de las ideas de Palafox, enriqueció y embelleció la biblioteca y continuó con el espíritu de apertura propuesto por el fundador. También se menciona el reconocimiento que el ilustre jesuita Clavijero hizo de las obras de Palafox.Don Juan de Palafox y Mendoza, Viceroy and Archbishop of New Spain, and Bishop of Puebla in the XVII century, has been studied by many specialists. However, the purpose of this paper is to highlight his role as founder of the first public library in Mexico and in the American Continent and promoter of free acces to information. In the XVIII Century Francisco Fabián y Fuero, Bishop of Puebla, enriched and embellished the Palafoxiana library and continued the policies of its founder. Attention is also drawn to the recognition that the renowned Jesuit Clavijero made of the work of Palafox.

  13. Tecnología cerámica y estrategias de movilidad entre cazadores-recolectores de altura: El caso del sitio Valle Hermoso 1 (Malargüe, Mendoza Ceramic technology and mobility strategies among high altitude hunter-gatherers: the case of Valle Hermoso 1 site, Malargue, Mendoza

    Directory of Open Access Journals (Sweden)

    Nuria Sugrañes

    2011-12-01

    Full Text Available En este trabajo presentamos los resultados del análisis cerámico de los tiestos recuperados en el sitio Valle Hermoso 1 (Malargüe, Mendoza. A través de estos se discuten las estrategias de movilidad de cazadores-recolectores con cerámica en ambientes de altura. El sitio muestra una ocupación inicial de ca. 1900 años AP, y los resultados obtenidos sugieren la presencia de dos conjuntos con materiales cerámicos diversos, que corresponderían a grupos con una alta movilidad con reocupación estacional del valle.This paper draws on the results of analyses of ceramics recovered from the Valle Hermoso 1 site, Malargüe, Mendoza. The mobility strategies of hunter-gatherers with pottery in a high altitude environment are discussed on the basis of these data. The site was initially occupied ca. 1900 BP, and evidence suggests that there are two assemblages with different ceramic materials associated with highly mobile groups that reoccupied the valley seasonally.

  14. Comparative approaches on the shops metallurgists for the modern viniculture. The pioneer Antonio Baldé, Gil Miret and Carlos Berri in Mendoza Aproximaciones comparativas sobre los talleres metalúrgicos para la vitivinicultura moderna. Los pioneros Antonio Baldé, Gil Miret y Carlos Berri en Mendoza

    Directory of Open Access Journals (Sweden)

    Eduardo Pérez Romagnoli

    2007-01-01

    Full Text Available This paper proposes a comparison among the main characteristics of the two shops pioneer metallurgists in the production of instruments and equipment for wineries and industrial stills, in the beginnings of the modern viniculture in Mendoza . The Catalan partners Antonio Baldé and Gil Miret began in 1885 and the Italian Carlos Berri in 1888. A general panorama is presented on the equipment of the shops and the objects produced, the characteristics of the labor, the formation in metallurgy of the proprietors, the insert of the two firms in the region, a reference to other economic activities developed by the managers and some complementary questions.Este trabajo propone una comparación entre las características principales de los dos talleres metalúrgicos pioneros en la producción de instrumentos y equipamiento para bodegas y destilerías industriales, en los comienzos de la vitivinicultura moderna en Mendoza. Los socios catalanes Antonio Baldé y Gil Miret comenzaron en 1885 y el italiano Carlos Berri en 1888. Se presenta un panorama general sobre el equipamiento de los talleres y los objetos que producían, las características de la mano de obra, la formación metalúrgica de los propietarios, la inserción de las dos firmas en la región, una referencia a otras actividades económicas desarrolladas por los empresarios y algunas cuestiones complementarias.

  15. Essential oils of medicinal plants from the central andes of Argentina: chemical composition, and antifungal, antibacterial, and insect-repellent activities.

    Science.gov (United States)

    Lima, Beatriz; López, Sandra; Luna, Lorena; Agüero, María B; Aragón, Liliana; Tapia, Alejandro; Zacchino, Susana; López, María L; Zygadlo, Julio; Feresin, Gabriela E

    2011-05-01

    The antifungal, antibacterial, and insect-repellent activities of the essential oils (EOs) of Acantholippia seriphioides, Artemisia mendozana, Gymnophyton polycephalum, Satureja parvifolia, Tagetes mendocina, and Lippia integrifolia, collected in the Central Andes area, province of San Juan, Argentina, were investigated. The dermatophytes Microsporum gypseum, Trichophyton mentagrophytes, and T. rubrum were inhibited by the EOs of G. polycephalum, L. integrifolia, and S. parvifolia, with minimum inhibitory concentrations (MICs) between 31.2 and 1000 μg/ml. Moreover, all EOs presented moderate activity against the bacteria tested, and the L. integrifolia and G. polycephalum EOs showed excellent repellent properties against Triatoma infestans, the Chagas disease vector, with repellency values between 60 and 100%. The A. seriphioides, G. polycephalum, and L. integrifolia EOs, obtained by hydrodistillation, were characterized by GC-FID and GC/MS analyses. The highest number of components (40) was identified in L. integrifolia EO, which, along with that of A. seriphioides, contained important amounts of oxygenated monoterpenes (44.35 and 29.72%, resp.). Thymol (27.61%) and carvacrol (13.24%) were the main components of A. seriphioides EO, and borneol, lippifoli-1(6)-en-5-one, and terpinen-4-ol (>8.5%) were the principal compounds of L. integrifolia EO. These results support the idea that oxygenated monoterpenes are the bioactive fractions of the EOs. Finally, the study shows that these Andean species might be used to treat superficial fungal infections and to improve the local Chagas disease situation by vector-control.

  16. A new species of Psychrophrynella (Amphibia, Anura, Craugastoridae from the humid montane forests of Cusco, eastern slopes of the Peruvian Andes

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    Alessandro Catenazzi

    2016-03-01

    Full Text Available We describe a new species of Psychrophrynella from the humid montane forest of the Department Cusco in Peru. Specimens were collected at 2,670–3,165 m elevation in the Área de Conservación Privada Ukumari Llakta, Japumayo valley, near Comunidad Campesina de Japu, in the province of Paucartambo. The new species is readily distinguished from all other species of Psychrophrynella but P. bagrecito and P. usurpator by possessing a tubercle on the inner edge of the tarsus, and from these two species by its yellow ventral coloration on abdomen and limbs. Furthermore, the new species is like P. bagrecito and P. usurpator in having an advertisement call composed of multiple notes, whereas other species of Psychrophrynella whose calls are known have a pulsed call (P. teqta or a short, tonal call composed of a single note. The new species has a snout-vent length of 16.1–24.1 mm in males and 23.3–27.7 mm in females. Like other recently described species in the genus, this new Psychrophrynella inhabits high-elevation forests in the tropical Andes and likely has a restricted geographic distribution.

  17. A new species of Psychrophrynella (Amphibia, Anura, Craugastoridae) from the humid montane forests of Cusco, eastern slopes of the Peruvian Andes.

    Science.gov (United States)

    Catenazzi, Alessandro; Ttito, Alex

    2016-01-01

    We describe a new species of Psychrophrynella from the humid montane forest of the Department Cusco in Peru. Specimens were collected at 2,670-3,165 m elevation in the Área de Conservación Privada Ukumari Llakta, Japumayo valley, near Comunidad Campesina de Japu, in the province of Paucartambo. The new species is readily distinguished from all other species of Psychrophrynella but P. bagrecito and P. usurpator by possessing a tubercle on the inner edge of the tarsus, and from these two species by its yellow ventral coloration on abdomen and limbs. Furthermore, the new species is like P. bagrecito and P. usurpator in having an advertisement call composed of multiple notes, whereas other species of Psychrophrynella whose calls are known have a pulsed call (P. teqta) or a short, tonal call composed of a single note. The new species has a snout-vent length of 16.1-24.1 mm in males and 23.3-27.7 mm in females. Like other recently described species in the genus, this new Psychrophrynella inhabits high-elevation forests in the tropical Andes and likely has a restricted geographic distribution.

  18. Migración y tributación en los Andes: Chichas y Lípez a fines del siglo XVII

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    Gil Montero, Raquel

    2013-06-01

    Full Text Available The article makes a comparative analysis of the visita veneral of viceroy La Palata (1683 to two provinces located in the south of the present-day Bolivia. The main objective is to contribute to the general discussion on the causes of migration in the seventeenth Century in the Andes. Our analysis shows, how the mita system not only affected the movements of the indigenous tributary population, but also contributed to the formation of a group of migrants related to mining activities.El artículo analiza en forma comparativa la visita general del duque de La Palata realizada en dos corregimientos del sur de la actual Bolivia en 1683. El objetivo general es contribuir a la discusión sobre las causas de las migraciones del siglo XVII. El análisis muestra cómo la mita influyó no solamente como una de las causas principales de las huidas de la población tributaria, sino también conformando un colectivo de migrantes relacionados con la actividad minera.

  19. Interseismic Rates From the CTO cGPS Andes and Nepal Networks

    Science.gov (United States)

    Genrich, J. F.; Galetzka, J.; Chowdhury, F.; Avouac, J.; Simons, M.; Barrientos, S. E.; Comte, D.; Norabuena, E. O.; Sapkota, S. N.

    2009-12-01

    To study crustal deformation at converging plate margins the Caltech Tectonics Observatory (CTO), together with partner institutions in the host countries, operates continuously observing GPS stations in the central Andes (northern Chile and southern Peru) and in Nepal. The currently 20-site Andes network was established in 2005 with 7 stations. Efforts are underway to provide data streaming links at near real time for the majority of sites. The Nepal network started with 10 sites in 2004 and has been expanded to 23 sites in the last couple of years. Dual frequency code and phase data from all sites are processed with the GAMIT/GLOBK processing package. Reliable interseismic velocities are now available for the majority of sites. Network metadata, rinex data files, processed time series and velocity estimates can be found online thru links at the CTO website: tectonics.caltech.edu.

  20. Surface uplift in the Central Andes driven by growth of the Altiplano Puna Magma Body

    Science.gov (United States)

    Perkins, Jonathan P.; Ward, Kevin M.; de Silva, Shanaka L.; Zandt, George; Beck, Susan L.; Finnegan, Noah J.

    2016-10-01

    The Altiplano-Puna Magma Body (APMB) in the Central Andes is the largest imaged magma reservoir on Earth, and is located within the second highest orogenic plateau on Earth, the Altiplano-Puna. Although the APMB is a first-order geologic feature similar to the Sierra Nevada batholith, its role in the surface uplift history of the Central Andes remains uncertain. Here we show that a long-wavelength topographic dome overlies the seismically measured extent of the APMB, and gravity data suggest that the uplift is isostatically compensated. Isostatic modelling of the magmatic contribution to dome growth yields melt volumes comparable to those estimated from tomography, and suggests that the APMB growth rate exceeds the peak Cretaceous magmatic flare-up in the Sierran batholith. Our analysis reveals that magmatic addition may provide a contribution to surface uplift on par with lithospheric removal, and illustrates that surface topography may help constrain the magnitude of pluton-scale melt production.