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Ob Plateau

The Ob Plateau (, Priobskoye Plato), is one of the great of . Administratively it falls within and Novosibirsk Oblast, Siberian Federal District, Russia. The plateau is named after the Ob River and is part of its basin. Geographical position, geological structure and surface topography of the south of Western Siberia (in Russian)

Most of the territory of the plateau has been agriculturally developed, yielding as well as . The Kulunda Main Canal, built at the time of the , runs in a roughly southwest/northeast direction across the plateau. Kulunda Canal — Altaiskaya Pravda


Geography
The Ob Plateau is located in Altai Krai and Novosibirsk Oblast at the southern edge of the West Siberian Plain. It extends roughly to the north of the foothills of the along the left bank of the north-flowing Ob River. To the west it descends gradually to the .

The average height of the Ob Plateau surface is between and , reaching a maximum height of at an unnamed summit. The plateau is dissected diagonally by wide ravines of glacial origin slanting towards the Ob river. They are about in width and between to deep, stretching parallel to each other in a roughly northeast to southwest direction. soils predominate in the open steppe spaces of the plateau.


Hydrography
Some of the main rivers of the plateau are the Aley, , Kulunda, Burla, Karasuk, Bagan and Kasmala among others. Within the glacial trenches there are a number of , such as Gorkoye (Chernokurynskoye), Gorkoye (Novichikhinsky District), Gorkoye (Tyumentsevsky District), and Gorkoye-Peresheyechnoye.


Flora
There are forests made up mostly of in the ravines, as well as remnants of coniferous in higher areas. and lakes are common in the river valleys cutting across the plateau. Приобское плато; Great Soviet Encyclopedia in 30 vols. — Ch. ed. A.M. Prokhorov. - 3rd ed. - M. Soviet Encyclopedia, 1969-1978. (in Russian)


See also
  • Geography of Russia § Topography and drainage


External links

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