GEOLOGICAL STRUCTURE OF THE ADYRS OF THE FERGANA VALLEY AND FEATURES OF ITS DEVELOPMENT.

Abstract

This article reveals the main features of the adyr landscape of the Fergana Valley from the point of view of their stratification by Neogene and Quaternary deposits, that is, deposits of the Neogene period consist of siltstones, silts and clays, sands, sandstones, layers of conglomerates and Quaternary layers, the deposits of which are located from north to south in the form of the Sokh, Tashkent, Mirzachol and modern Syrdarya complexes. The article also describes the location, tectonics, anticlinal and synclinal structures of the adyrs.