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West Siberian Plain, large alluvial plain between the Urals to the west and the Yenisei River to the east, beyond which rises the Central Siberian Plateau. The lowland is bound by the coast of the Kara Sea to the north and by the foothills of the Altai Mountains to the southeast.
Typical view of the Central Russian Upland (Belgorod Oblast) The Central Russian Upland (also Middle Russian Upland and East European Upland) is an upland area of the East European Plain and is an undulating plateau with an average elevation of 230–250 m (750–820 ft). Its highest peak is measured at 293 m (961 ft).
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The Central Siberian Plateau (Russian: Среднесибирское плоскогорье, romanized: Srednesibirskoye ploskogorye; Yakut: Орто Сибиир хаптал хайалаах сирэ, romanized: Orto Sibîr xaptal xayalâx sire) is a vast mountainous area in Siberia, one of the Great Russian Regions.
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It may, for example, refer to European Russia (except the North Caucasus and Kaliningrad). [citation needed] The 1967 book by Stephen P. Dunn and Ethel Dunn The Peasants of Central Russia [1] defines the area as the territory from Novgorod Oblast to the north to the border with Ukraine in the south and from Smolensk Oblast to the west and Volga to
The East European Plain (also called the Russian Plain, [1] or historically the Sarmatic Plain) [2] is a vast interior plain extending east of the North European Plain, [3] and comprising several plateaus stretching roughly from 25 degrees longitude eastward.
Central European Uplands: Hibernian Uplands Cornish-Welsh Uplands Pennine Chain: Scottish Highlands: Armorican Massive South Central Plateau (Massif Central) Central Plateau (Meseta Central) Jura Range: Vosges Mountains and Black Forest Mountains: Swiss-Bavarian Plateau: Rhenish Massif: West Hesse Highlands: East Hesse Highlands: Weser Uplands ...