ГЕОМОРФОЛОГИЧЕСКИЙ ОЧЕРК ЮЖНОГО МАКРОСКЛОНА СТАНОВОГО ХРЕБТА

Abstract

Special geomorphologic investigations were carried out at the southern slope of Stanovoi ridge. Slopes are shown to play the main role in the tructure and zoning of landforms; the stable slope associations of different dynamic types, an important role of tectonic tilts of land surface, self-development capability are the main features of the relief.