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  2. Central Siberian Plateau - Wikipedia

    en.wikipedia.org/wiki/Central_Siberian_Plateau

    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.

  3. Great Russian Regions - Wikipedia

    en.wikipedia.org/wiki/Great_Russian_Regions

    North Siberian Lowland, a plain with a relatively flat relief separating the Byrranga Mountains of the Taymyr Peninsula in the north from the Central Siberian Plateau in the south. Area approximately 400,000 km 2 (150,000 sq mi).

  4. Central Russian Upland - Wikipedia

    en.wikipedia.org/wiki/Central_Russian_Upland

    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).

  5. Siberia - Wikipedia

    en.wikipedia.org/wiki/Siberia

    Major geographical zones within Siberia include the West Siberian Plain and the Central Siberian Plateau. Eastern and central Sakha comprises numerous north–south mountain ranges of various ages. These mountains extend up to almost 3,000 metres (9,800 ft), but above a few hundred metres they are almost completely devoid of vegetation.

  6. East European Plain - Wikipedia

    en.wikipedia.org/wiki/East_European_Plain

    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.

  7. Siberia (continent) - Wikipedia

    en.wikipedia.org/wiki/Siberia_(Continent)

    About 2.5 billion years ago (in the Siderian Period), Siberia was part of a continent called Arctica, along with the Canadian Shield.Around 1.1 billion years ago (in the Stenian Period), Siberia became part of the supercontinent of Rodinia, a state of affairs which lasted until the Tonian about 750 million years ago when it broke up, and Siberia became part of the landmass of Protolaurasia.

  8. Geology of Russia - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Russia

    The Siberian craton (or West-Siberian craton) coincides with the Central Siberian plateau that lies between the Yenisei and Lena rivers. In the west it borders the West Siberian basin. The Yenisei-Katanga trough lies in the north. In the south lies the Central Asian fold belt, the Baikal rift and the Mongol-Okhotsk fold belt. The eastern border ...

  9. Central Russia - Wikipedia

    en.wikipedia.org/wiki/Central_Russia

    Central Russia is, broadly, the various areas in European Russia. Historically, the area of Central Russia varied based on the purpose for which it is being used. It may, for example, refer to European Russia (except the North Caucasus and Kaliningrad ).