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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.
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). [6]
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).
Typical trees are the Siberian pine (Pinus sibirica). At the latitude of the Central Siberian Reserve (60 degrees North), the Siberian pine grows at 100–200 meters in altitude; farther south into Mongolia it is a mountain tree growing at 1,000-2,000 meters. There are stands of larch and other pine in the reserve.
The Central Siberian Plateau is an ancient craton (sometimes named Angaraland) that formed an independent continent before the Permian (see the Siberian continent). It is exceptionally rich in minerals, containing large deposits of gold, diamonds, and ores of manganese, lead, zinc, nickel, cobalt, and molybdenum.
Pages in category "Central Siberian Plateau" The following 34 pages are in this category, out of 34 total. This list may not reflect recent changes. ...
January has packed a frigid punch for many in the central and eastern states so far and the "Siberian Express" will pile onto the bone-chilling month as we head into the weekend and next week ...
Siberia, also known as Siberian Craton, Angaraland (or simply Angara) and Angarida, [1] is an ancient craton in the heart of Siberia. Today forming the Central Siberian Plateau , it formed an independent landmass prior to its fusion into Pangea during the Late Carboniferous - Permian .