The Ob Plateau (, Priobskoye Plato), is one of the great of Siberia. Administratively it falls within Altai Krai and Novosibirsk Oblast, Siberian Federal District, Russia. The plateau is named after the Ob River and is part of its basin.Google Earth 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 grain crops as well as industrial crops. The Kulunda Main Canal, built at the time of the USSR, runs in a roughly southwest/northeast direction across the plateau. Kulunda Canal — Altaiskaya Pravda
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. Chernozem soils predominate in the open steppe spaces of the plateau.
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