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The features of engineer-geological conditions on a site of break of Dnieper through the Ukrainian shield are considered. This territory tested anthropogenic influence since olden times. Most changes happened after building of a dam of multifunction Dnieper water-storage basin. The problem of navigation was decided at flooding of the Dnieper rapids. The engineer-geological problems of adjoining to this area of valley territory are also related to distribution of grounds of loess structure (periglyacial area of the Dnieper glacier).

ENGINEERING-GEOLOGICAL CONDITIONS OF DNIEPER VALLEY ON AREA OF DNIEPER WATER-STORAGE BASIN