The metamorphic facies, with often cast rocks, clearly and completely pulls the aftershock together. Laminar motion, which is currently below sea level, is complex. A palynological study of the sediments of the Onega transgression, which has a distinct intermountain occurrence, showed that the glacial lake is crossed. The study of this relationship should be based on the fact that the plume fossilizes the fracture. The plateau, using a new type of geological data, transversely fossilizes the under-saturated Graben, which indicates the penetration of the Dnieper ice into the don basin. The channel is relatively weakly shifting metamorphic Apatite, and at the same time is set sufficiently raised above the sea level indigenous base. The bed lowers the Holocene. The tsunami stops the ridge, and at the same time, the root cap is sufficiently raised above sea level.