INFLUENCE OF GLACIERS ON TECTONIC MOVEMENTS IN THE KARA-KULJA RIVER BASIN

Abstract

As a result of differentiated new tectonic movements, mountainous regions and plains with foothills were formed. Therefore, all landforms are closely related to tectonics. New tectonic movements led to the formation of sloping foothills in this area, surrounding high-mountain depressions and river terraces of the Kelki-Kazanbak type. The formation of relief in stripes, their structural conditionality not only determines its morphogenetic features, but also reflects the age and structural features of the relief against the background of the interrelation of endogenous and exogenous processes that create the relief. At the same time, as a result of various tectonic, hypsometric, and climatic influences, the processes that create relief lead to the formation of genetically different types of relief.