Реликтовый криогенный микрорельеф южной части Брянской области

Аннотация

Results are presented of geological and geomorphological study of relict cryogenic microrelief Microrelief is well pronounced, the hummocks centers being 1,2-1,7 meters above the depressions floor. Geological base of the microrelief is cryogenic veins system which is clearly seen in sections. Cryogenic deformations study reveals two phases of Late Pleistocene cold period.