f On constituents of incrust pressure in the depths of South-East Caucasus

As it's known, the majority of modern geodynamik processes are the reflections of deep mental movements which infuence the stabiliti of the earth crust. Besides it is considered that one of the main causes of these movements is the pressure in the earth crust, consisting of vertical and horisontal constituents. The vertical constituents of the pressure in definite depth- is a function of the weight of upper intervals of the rocks and pressure, resulted by regional geological processes. The horisontal constituent is defined, first of oil, by tectonic processes. The summary action of these constituents causes plastical and elastic deformations of the litospere defining the formation of the surface relief.