ROLE OF POZDNEPLEYSTOTSENOVYKH PERIGLYATSIALNYKH''S CONDITIONS IN DEVELOPMENT OF LANDSCAPES OF CASPIAN DEPRESSION
In article the role of verkhnepleystotsenovy periglyatsialny conditions is proved in development of landscapes of the Caspian lowland. According to the author after completion of early and pozdnekhvalynsky transgression the main role in formation of forms meso - and a microrelief was played by cryoarid climatic conditions of a late pleistocene. The merzlotny processes which have predetermined the main physiognomical lines of a relief of Caspian Depression, namely processes of tetragonal cracking of the top horizons of crust with formation of a lattice of the polygonal and vein ices which have dismembered the uniform surface of Caspian Depression on blocks and interblock which have directed further the course of all exogenous processes were the leading relyefoobrazuyushchy exogenous processes shown right after completion of hvalynsky transgression. Mechanisms of formation large-block, lozhbinny, zapadinny, paleoalasny, gryadovy (Baire knolls) paleokriogenny Prikaspiya's relief are allocated and proved.