ABSTRACT: Method of the estimation of the average permeability and transmissivity from hydrochemical and geomorphometical characteristics of the descending springs has never been used to estimate hydraulic parameters of dolomites of other carbonates maybe because of the model requirements to which a lot of springs in carbonates are not suitable. In spite of the fact we tried to use this method for Ramsau dolomites (ladin) in the area of the Veporicum unit of the Branisko and Čierna hora Mts. The results of investigation show, that the practical application of this method for dolomites is possible, but it requires meticulous selection of the springs before estimation of hydraulic parameters. Besides, values interaction velocity wi and ma / me for dolomites will have to specify in order to real estimate of hydraulic parameters.