STRATIGRAPHY AND CHRONOLOGY OF THE GEOLOGICAL EVENTS OF THE MIDDLE NEOPLEISTOCENE
The landscape-climate conditions of Ukraine in the Middle Neopleistocene (400-120 ths. y.) were characterized by the contrast changes of cold and warm epochs. There events are distinctly shown in the structure of loess-soil formation. In the territory of Ukraine of this period at time there have been established the traces of the glaciations that took place after the Lixvin interglacial. The last warm epoch at the end at the Middle-Neopleistocene was marked by farming of Kaidaki paleosol end, later by Tyas-min loess horizon. In the glacial zone they corresponded to the Pripyat stadial deposits of the Dnepr glaciations.