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[[Image:Siberia-FederalSubjects.png|thumb|right|250px|       Siberian Federal District       Geographic Russian Siberia       Historical Siberia (and present Siberia in some usages)]]

Siberia ( ), is the vast region constituting almost all of Northern Asia and for the most part currently serving as the massive central and eastern portion of the Russian Federationmarker, having served in the same capacity previously for the USSRmarker from its beginning, and the Russian Empiremarker beginning in the 16th century.

It includes a large part of the Eurasian Steppe and extends eastward from the Ural Mountainsmarker to the watershed between Pacificmarker and Arcticmarker drainage basins, and southward from the Arctic Oceanmarker to the hills of north-central Kazakhstanmarker and the national borders of both Mongoliamarker and Chinamarker. It makes up about 77% of Russia's territory (13.1 million square kilometres), but only 25% of Russia's population (36 million people).

Origin of the name

Some sources say that it originates from the Turkic for "sleeping land." Another version is that this name was the tribal name of the Sibilla, ancient Turkic nomads later assimilated to Siberian Tatars. It has also been asserted that the name Siberia is connected to the Sabir people. Shaman Akkanat, one of the last shamans in western Siberia and a leading figure in the indigenous society of the region, claims that Siberia got its name from his nation, the Sibirga people. The modern usage of the name appeared in the Russian language after the conquest of the Siberia Khanate.

Borders and administrative division

with clickable city names (SVG).
The term Siberia has a very long history, and its meaning has gradually changed during ages.Historically, Siberia was defined as the whole part of Russia to the east of Ural Mountainsmarker, including the Russian Far East. According to this definition, Siberia extended eastward from the Ural Mountainsmarker to the Pacific coast, and southward from the Arctic Ocean to the border of Russian Central Asia and the national borders of both Mongolia (which included Tuvamarker) and China.

Soviet-era sources (GSE and others) and modern Russian ones usually define Siberia as a region extending eastward from the Ural Mountains to the watershed between Pacificmarker and Arcticmarker drainage basins, and southward from the Arctic Ocean to the hills of north-central Kazakhstanmarker and the national borders of both Mongoliamarker and Chinamarker. Correspondingly, Siberia includes the federal subjects of the Siberian Federal District, and some of the Urals Federal District, as well as Sakha Republic, which is a part of the Far Eastern Federal District. This definition also includes geographically (but not administratively) subdivisions of several other subjects of Urals and Far Eastern federal districts. This definition excludes Sverdlovsk Oblast and Chelyabinsk Oblast, both of which are included in some wider definitions of Siberia.

Other sources may use either a somewhat wider definition that states the Pacific coast, not the watershed, is the eastern boundary (thus including the whole Russian Far East) or a somewhat narrower one that confines Siberia to the Siberian Federal District (thus excluding all subjects of other districts). However, in Russian the word for Siberia is never used to substitute the name of the federal district.

Federal subjects]] of Siberia (GSE)
subject administrative center
Urals Federal District
Khanty-Mansi Autonomous Okrugmarker Khanty-Mansiyskmarker
Kurgan Oblast Kurganmarker
Tyumen Oblast Tyumenmarker
Yamalo-Nenets Autonomous Okrugmarker Salekhardmarker
Siberian Federal District
Altai Kraimarker Barnaulmarker
Altai Republic Gorno-Altayskmarker
Buryat Republic Ulan-Udemarker
Chita Oblast Chitamarker
Irkutsk Oblastmarker Irkutskmarker
Republic of Khakassia Abakanmarker
Kemerovo Oblast Kemerovomarker
Krasnoyarsk Kraimarker Krasnoyarskmarker
Novosibirsk Oblast Novosibirskmarker
Omsk Oblastmarker Omskmarker
Tomsk Oblast Tomskmarker
Tuva Republicmarker Kyzylmarker
Far Eastern Federal District
Sakha Republic Yakutskmarker

Federal subjects]] of Siberia (in wide sense)
subject administrative center
Far Eastern Federal District
Amur Oblastmarker Blagoveshchenskmarker
Chukotka Autonomous Okrugmarker Anadyrmarker
Jewish Autonomous Oblastmarker Birobidzhanmarker
Kamchatka Kraimarker Petropavlovsk-Kamchatskymarker
Khabarovsk Krai Khabarovskmarker
Magadan Oblast Magadanmarker
Primorsky Kraimarker Vladivostokmarker
Sakhalin Oblast Yuzhno-Sakhalinskmarker
Urals Federal District
Chelyabinsk Oblast Chelyabinskmarker
Sverdlovsk Oblast Yekaterinburgmarker

Major cities include:


Siberia was occupied by differing groups of nomads such as the Yenets, the Nenets, the Huns, the Iranian Scythians, and the Turkic Uyghurs. The Khan of Sibir in the vicinity of modern Tobolskmarker was known as a prominent figure who endorsed Kubrat as Khagan in Avar in 630. The area was conquered by the Mongols early in the 13th century. With the break up of the Golden Horde, the autonomous Siberia Khanate was established in late 14th century.
The growing power of Russiamarker to the west began to undermine the Siberian Khanate in the 16th century. First, groups of traders and Cossacks began to enter the area, and then the Russian army began to set up forts further and further east. Towns like Mangazeyamarker, Taramarker, Yeniseyskmarker, and Tobolskmarker sprang up, the latter being declared the capital of Siberia. By the mid-17th century, the Russian-controlled areas had been extended to the Pacificmarker. The total Russian population of Siberia in 1709 was 230,000.

Siberia remained a mostly undocumented and sparsely populated area. During the following few centuries, only a few exploratory missions and traders entered Siberia. The other group that was sent to Siberia consisted of prisoners exiled from western Russia or Russian-held territories like Polandmarker (see katorga). In the 19th century, around 1.2 million prisoners were deported to Siberia.

The first great modern change to Siberia was the Trans-Siberian railway, constructed in 1891–1916. It linked Siberia more closely to the rapidly-industrializing Russia of Nicholas II. Between 1801 and 1914 an estimated 7 million settlers moved from European Russia to Siberia, 85% during the quarter-century before World War I. Siberia is filled with natural resources and during the 20th century large scale exploitation of these was developed, and industrial towns cropped up throughout the region.

Katorga and Gulag

Russia, later the Soviet Union, operated a series of labor camps, known as the GULAG, which is an acronym for Main Camp Administration. They became so common that "Siberia" came to be used as a reference for exile and punishment, e.g., "a bureaucratic Siberia." Soviet authorities deported millions of people, including entire nationalities, from western areas of the USSR to Central Asia and Siberia. More than 18 million people passed through the Gulag from 1929 to 1953, with a further 6 million being deported and exiled to remote areas of the Soviet Union.

By analogy, one working-class district of downtown Stockholmmarker, Swedenmarker, earned the name Sibirien (Siberia) in the late 19th century, referring to its low-cost tenement houses being built in outlying areas.

Geography and geology

With an area of 13.1 million km² (5.1 million square miles), Siberia makes up roughly 77% of the total area of Russia. Major geographical zones include the West Siberian Plain and the Central Siberian Plateaumarker. Siberia covers almost 10% of Earth's land surface (14,894,000 km²).

The West Siberian Plain consists mostly of Cenozoic alluvial deposits and is extraordinarily low-lying, so much so that a sea level rise of fifty metres would cause all land between the Arctic Ocean and Novosibirskmarker to be inundated. Many of the deposits on this plain result from ice dams; having reversed the flow of the Ob and Yenisei Rivers, so redirecting them into the Caspian Seamarker (perhaps the Aralmarker as well). It is very swampy and soils are mostly peaty Histosols and, in the treeless northern part, Histels. In the south of the plain, where permafrost is largely absent, rich grasslands that are an extension of the Kazakh Steppe formed the original vegetation (almost all cleared now).

The Central Siberian Plateau is an extremely ancient craton (sometimes named Angaraland) that formed an independent continent before the Permian (see Siberia ). It is exceptionally rich in minerals, containing large deposits of gold, diamonds, and ores of manganese, lead, zinc, nickel, cobalt and molybdenum. Much of the area includes the Siberian Traps which is a large igneous province. The massive eruptive period was approximately coincident with the Permian–Triassic extinction event. The volcanic event is said to be the largest known volcanic eruption in Earth's history. Only the extreme northwest was glaciated during the Quaternary, but almost all is under exceptionally deep permafrost and the only tree that can thrive, despite the warm summers, is the deciduous Siberian Larch (Larix sibirica) with its very shallow roots. Outside the extreme northwest, the taiga is dominant. Soils here are mainly Turbels, giving way to Spodosols where the active layer becomes thicker and the ice content lower.

Eastern and central Sakha comprise numerous north-south mountain ranges of various ages. These mountains extend up to almost three thousand metres in elevation, but above a few hundred metres they are almost completely devoid of vegetation. The Verkhoyansk Rangemarker was extensively glaciated in the Pleistocene, but the climate was too dry for glaciation to extend to low elevations. At these low elevations are numerous valleys, many of them deep, and covered with larch forest except in the extreme north, where tundra dominates. Soils are mainly Turbels and the active layer tends to be less than one metre deep except near rivers.

The highest point in Siberia is the active volcano Klyuchevskaya Sopkamarker, in the Kamchatkamarker peninsula. Its peak is at .

Russian researchers warn that Western Siberia has begun to thaw as a result of global warming. The frozen peat bogs in this region may hold billions of tons of methane gas, which may be released into the atmosphere. Methane is a greenhouse gas 22 times more powerful than carbon dioxide. In 2008, a research expedition for the American Geophysical Union detected levels of methane up to 100 times above normal in the Siberian Arctic, likely being released by methane clathrates being released by holes in a frozen 'lid' of seabed permafrost, around the outfall of the Lena Rivermarker and the area between the Laptev Seamarker and East Siberian Seamarker.


Vegetation in Siberia is mostly taiga, with a tundra belt on the northern fringe, and a temperate forest zone in the south.

Almost all the population lives in the south, along the Trans-Siberian Railway. The climate here is subarctic (Koppen Dfc or Dwc), with the annual average temperature about and roughly average in January and in July. With a reliable growing season, an abundance of sunshine and exceedingly fertile chernozem soils, Southern Siberia is good enough for profitable agriculture, as was proven in the early twentieth century.

The southwesterly winds of Southern Siberia bring warm air from Central Asia and the Middle East. The climate in West Siberia (Omsk, Novosibirsk) is several degrees warmer than in the East (Irkutsk, Chita). With a lowest record temperature of , Oymyakonmarker (Sakha Republic) has the distinction of being the coldest town on Earth. But summer temperatures in other regions reach . In general, Sakha is the coldest Siberian region, and the basin of the Yana River has the lowest temperatures of all, with permafrost reaching . Nevertheless, as far as Imperial Russian plans of settlement were concerned, cold was never viewed as an issue. In the winter, southern Siberia sits near the center of the semi-permanent Siberian High, so winds are usually light in the winter.

Precipitation in Siberia is generally low, exceeding only in Kamchatkamarker where moist winds flow from the Sea of Okhotskmarker onto high mountains – producing the region's only major glaciers – and in most of Primorye in the extreme south where monsoonal influences can produce quite heavy summer rainfall. Despite the region's notorious cold winters, snowfall is generally quite light, especially in the eastern interior of the region.

Lakes and rivers

Mountain ranges



Siberia is extraordinarily rich in minerals, containing ores of almost all economically valuable metals—largely because of the absence of Quaternary glaciation outside highland areas. It has some of the world's largest deposits of nickel, gold, lead, coal, molybdenum, gypsum, diamonds, silver and zinc, as well as extensive unexploited resources of oil and natural gas. Most of these are in the cold and remote eastern part of the region, with the result that extraction has proven difficult and expensive.

Agriculture is severely restricted by the short growing season of most of the region. However, in the southwest where soils are exceedingly fertile black earths and the climate is a little more moderate, there is extensive cropping of wheat, barley, rye and potatoes, along with the grazing of large numbers of sheep and cattle. Elsewhere food production, owing to the poor fertility of the podzolic soils and the extremely short growing seasons, is restricted to the herding of reindeer in the tundra — which has been practised by natives for over ten thousand years. Siberia has the world's largest forests. Timber remains an important source of revenue despite the fact that many forests in the east have been logged much more rapidly than they are able to recover. The Sea of Okhotskmarker is one of the two or three richest fisheries in the world owing to its cold currents and extremely large tidal ranges, and thus Siberia produces over 10 percent of the world's annual fish catch, though fishing has declined somewhat since the collapse of the USSR.


Siberia has a population density of about three people per square kilometer. Most Siberians are Russians and Russified Ukrainians. There are approximately 400,000 ethnic Germans living in Siberia. Such Mongol and Turkic groups as Buryats, Tuvinians, Yakuts, and Siberian Tatars lived in Siberia originally, and descendants of these peoples still live there. The Buryats number 445,175, which makes them the largest ethnic minority group in Siberia. According to the 2002 census there are 443,852 Yakuts. Other ethnic groups include Kets, Evenks, Chukchis, Koryaks, and Yukaghirs. See the Northern indigenous peoples of Russia article for more. Officially, 40,000 Chinese live in the Russian Far East, but the actual figure is believed to be much higher.

About 70% of Siberia's people live in cities. Most city people live in apartments. Many people in rural areas live in simple, but more spacious, log houses. Novosibirskmarker is the largest city in Siberia, with a population of about 1.5 million. Tobolskmarker, Tomskmarker, Krasnoyarskmarker, Irkutskmarker and Omskmarker are the older, historical centers.


There are a variety of beliefs throughout Siberia including Orthodox Christianity, Islam, Tibetan Buddhism, and other denominations of Christianity. An estimated 70,000 Jews live in Siberia. The predominant group is the Russian Orthodox Church. However, native religion dates back hundreds of years. The vast terrority of Siberia has many different local traditions of gods. These include: Ak Ana, Anapel, Bugady Musun, Kara Khan, Khaltesh-Anki, Kini'je, Ku'urkil, Nga, Nu'tenut, Numi-Torem, Numi-Turum, Pon, Pugu, Todote, Toko'yoto, Tomam, Xaya Iccita, Zonget. Places with sacred areas include Olkhonmarker, an island in Lake Baikalmarker.


Many cities in Siberia, such as Petropavlovsk-Kamchatskymarker, cannot be reached by road from other major cities in Russia or Asia. The best way to tour Siberia is through the Trans-Siberian Railway. The Trans-Siberian Railway operates from Moscow in the West to Vladivostokmarker in the East. The train has 2nd class 4-berth compartments, 1st class 2-berth compartments, and a restaurant car. Cities not nearby the Railway are best reached by air.

See also


External links

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