ОСОБЕННОСТИ СТРОЕНИЯ РЕЛЬЕФА СКАЛЬНОГО ЛОЖА ГОРНЫХ И ПОЛУГОРНЫХ ДОЛИН

Abstract

A particular class of channel landforms is described. It is represented by sculptured-erosion forms, created by channel flow cutting into bedrock of mountain and semi-mountain rivers. The main types of this landform class, their changes along the valley, and their dependence on channel type and lithology are considered.