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Posted by / 19-Jan-2021 17:38

The rivers on the western slope carry more water than those of the east, particularly in the Northern and Nether-Polar Urals; the slowest rate of flow is on the eastern slope of the Southern Urals, reflecting intense evaporation as well as low precipitation.

The Ufa rivers of the Central and Southern Urals, which later join the Volga drainage basin, have their sources on the eastern slope.Russia and the major part of the traditional physiographic boundary between Europe and Asia.Extending some 1,550 miles (2,500 km) from the bend of the Ural River in the south to the low, severely eroded Pay-Khoy Ridge, which forms a 250-mile (400-km) fingerlike extension to the northern tip of the Urals proper, the mountains constitute the major portion of the Uralian orogenic belt, which stretches 2,175 miles (3,500 km) from the Aral Sea to the northernmost tip of Mughalzhar Hills, themselves part of the Uralian orogenic belt, are a broad, arrowhead-shaped southern extension in northwestern Kazakhstan that form the divide between the Caspian and Aral basins.In their upper reaches many rivers flow slowly through the mountains in wide, longitudinal troughs.Later they change to a latitudinal direction, cut through the ridges in narrow valleys, and descend to the plains, particularly in the Northern and Southern Urals.

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