Groundwater
As a result of non-tectonic movements, intermountain depressions and mountain uplifts were formed. The depressions consist of weakly cemented and loose deposits, while the mountain uplifts, composed of Proterozoic and Paleozoic rocks, have undergone complex tectonic disturbances and are permeated by numerous various fractures. Groundwater is concentrated in the fractured zones, emerging as springs on the surface and being used for water supply. The main (predominant) groundwater resources in