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Around seven million Russians moved to Siberia from Europe between 1801 and 1914. [45] Between 1859 and 1917, more than half a million people migrated to the Russian Far East. [46] Siberia has extensive natural resources: during the 20th century, large-scale exploitation of these took place, and industrial towns cropped up throughout the region ...
Most of Northwest Russia and Siberia has a subarctic climate, with extremely severe winters in the inner regions of Northeast Siberia (mostly Sakha, where the Northern Pole of Cold is located with the record low temperature of −71.2 °C or −96.2 °F), [31] and more moderate winters elsewhere.
The mountain ridges, elongated from north to south, effectively absorb sunlight thereby increasing the temperature. The areas west of the Ural Mountains are 1–2 °C (1.8–3.6 °F) warmer in winter than the eastern regions because the former are warmed by Atlantic winds whereas the eastern slopes are chilled by Siberian air masses.
European Russia [a] is the western and most populated part of the Russian Federation.It is geographically situated in Europe, as opposed to the country's sparsely populated and vastly larger eastern part, Siberia, which is situated in Asia, encompassing the entire northern region of the continent.
The map shows the origin of the first wave of humans into the Americas. Involved are the ANE (Ancestral Northern Eurasian, which represent a distinct Paleolithic Siberian population), and the NEA (Northeast Asians, which are an East Asian-related group). The admixture happened somewhere in Northeast Siberia. (from Indigenous peoples of Siberia)
North Asia or Northern Asia is the northern region of ... Map of Northern Asia in 1921. The region was first ... moved from European Russia to Siberia, ...
The North Siberian Lowland lies between the lower reaches of the Yenisey and Olenyok rivers in Krasnoyarsk Krai and Yakutia.It is 1,400 km long and up to 600 km wide. This lowland plain features flat-topped ridges approximately 200-300 m high, which rise over broad and heavily swamped degradations with a large number of thermokarst lakes.
The European part of Russia lies on the East European platform, a region up to 3,000 kilometres (1,900 mi) wide covered by more than 3 kilometres (1.9 mi) of metamorphosed sediments dating back to the Riphean stage (middle to late Proterozoic, from 1,400 to 800 million years ago).