EN
Late Vistulian and Holocene mollusc-bearing deposits, developed as solifluction sediments, travertines and calcareous tufa, occur in a valley of a small stream on NE slopes of the Ostrysz Hill near Małe Ciche in the Podhale Basin (S Poland). Several types of rich and differentiated mollusc assemblages, corresponding to consecutive phases of the evolution of climate and palaeogeographical conditions during the Late Vistulian and Holocene, were found in eleven profiles.