THE FEATURE OF VERTICAL AND SPATIAL DEVELOPMENT OF EXOGENOUS MORPHOGENESIS PROCESSES OF ZARAFSHAN VALLEY

For the Zarafshan valley territory, where the activity and differentiation of new tectonic activities is very high is clearly seen that the formation of the relief happens under concerted action of internal (tectonic) and external (exogenous) factors of morphogenesis. In connection with this, within the scope of describing region for clarification genesis form types of the relief it is necessary to account of new tectonics. It is clearly stated the net of mountain ranges with anticline and horst anticline high. Large valleys of the Zarafshan valley time to synclinal, horst synclinal, long developing yield, within the scope of which the depth of bedding foundation is 3 km. Hereby the amplitude excursion of motion for new modern tectonic stage reached to 5-6 km.