The features of the dynamics of karst and infiltration waters in various circulation zones of the Kungur cave according to monitoring observations are presented. Observations at hydrological sites allow accurate determination of the position of the karst water level in the transitional and horizontal circulation zones. With the general downward movement of infiltration waters, it is almost impossible to trace the entire path in each separate section of the geological section. It was possible to fix the intermediate level of standing of infiltration waters in the vertical circulation zone.