Abstract
The landscape-climatic conditions of Ukraine in the Middle Neopleistocene (400-120 ths. y.) were characterized by the contrast changes of cold and warm epochs. These events are distinctly shown in the structure of loess-soil formation. In the territory of Ukraine for this period of time there have been established the traces of one glaciation that took place after the Chigirin (Zavadovka) interglacial. The last warm epoch at the end of the Middle Neopleistocene was marked by forming of Kaidaki (Korshevsk) paleosol and, later, by Tyasmin loess horizon. In the glacial zone they correspond to the Pripyat stadial deposits of the Dnieper glaciation and loess-like loams with two paleosols.
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