Джунгарский Алатау
It consists of two main parts – the plain that adjoins the right Bank of the Ili river and the mountain – the spurs of the Dzungarian Alatau and the macro-slope of the Altyn Emel range. Small island mountain ranges are located on the plains. On the territory of the Park, Carboniferous deposits (300 million years old) have been identified, which are mainly represented by volcanites, Permian and Carboniferous deposits, and the most ancient deposits are Silurian. The Park's mountains are mostly composed of Paleozoic rocks that are 200 to 400 million years old.