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The present paper explains the curve-fitting method developed as a method to estimate the geothermal equilibrium forming temperature. In the present method, that temperature is estimated by obtaining, by non-linear lest square, the model parameter to minimize the sum of remainders squared between the temperature actually measured after a lapse of certain time from the stoppage of mud water circulation and that calculated on the basis of Middleton model, mathematical model of temperature equilibrium well. In the Horner's plotting method currently in general use, temperature recovery data during a long period of about 120h are required for estimating the geothermal equilibrium forming temperature. However in the curve-fitting method, it is confirmed from the actual well data that the well recovery temperature is estimable from three logging data during 24h after the stoppage of mud water circulation within the largest error of 5%, and during 12h within 10%. 7 refs., 5 figs., 1 ...