Organogenic landforms on the regressive mires of the Lower Amur and Southern Priokhotie

Abstract The article examines the distribution features of specific organocryogenic landforms in the waterlogged areas of the cryolithozone of the Northwest Coast of the Pacific, within the borders of the Lower Amur and Southern Priokhotie. It is suggested that the considered landforms are closely related to the regressive processes occurring in certain mire areas due to thermokarst phenomena. Attention is focused on the specifics of morphometric features of the ridge-hollow reliefwith a parallel arrangement of elements formed in local runoff hollows and low-flow basins.