Siberia

Coordinates: 60°0′N 105°0′E / 60.000°N 105.000°E / 60.000; 105.000

Siberia
Russian: Сибирь (Sibir)
Geographical region
Siberian Federal District        Geographic Russian Siberia        Siberia in its widest definition and historical use
Country	Russia
Region	North Asia
Borders on	West: Ural Mountains North: Arctic Ocean East: Pacific Ocean South: East Asia(Kazakhstan, Mongolia, PRC)
Parts	West Siberian Plain Central Siberian Plateau others...
Highest point	Klyuchevskaya Sopka
- elevation	4,649 m (15,253 ft)
Area	13,100,000 km2 (5,057,938 sq mi)
Population	40,000,000 (2010)
Density	3 / km2 (8 / sq mi)

Siberia (/saɪˈbɪəriə/; Russian: Сиби́рь, tr. Sibir'; IPA: [sʲɪˈbʲirʲ]) is an extensive geographical region, and by the broadest definition is also known as North Asia. Siberia has been historically part of Russia since the 17th century.

The territory of Siberia extends eastwards from the Ural Mountains to the watershed between the Pacific and Arctic drainage basins. Siberia stretches southwards from the Arctic Ocean to the hills of north-central Kazakhstan and to the national borders of Mongolia and China.^[1] With an area of 13.1 million square kilometres, Siberia accounts for 77% of Russia's land area, but it is home to just 40 million people – 27% of the country's population. This is equivalent to an average population density of about 3 inhabitants per square kilometre (approximately equal to that of Australia), making Siberia one of the most sparsely populated regions on Earth.

Etymology

Some sources say that "Siberia" originates from the Siberian Tatar word for "sleeping land" (Sib Ir).^[2] Another account sees the name as the ancient tribal ethnonym of the Sipyrs, a mysterious people later assimilated to Siberian Tatars. The modern usage of the name appeared in the Russian language after the conquest of the Siberian Khanate. A further variant claims that the region was named after the Xibe people.^[3] The Polish historian Chycliczkowski has proposed that the name derives from the proto-Slavic word for "north" (север, sever),^[4] but Anatole Baikaloff has dismissed this explanation^[5] on the grounds that the neighbouring Chinese, Arabs and Mongolians (who have similar names for the region) would not have known Russian. His own suggestion is that the name represents a combination of two words, "su" (water) and "bir" (wild land).

Pre-history

The region is of paleontological significance, as it contains bodies of prehistoric animals from the Pleistocene Epoch, preserved in ice or permafrost. Specimens of Goldfuss cave lion cubs, Yuka (mammoth) and another Woolly mammoth from Oymyakon, a Woolly rhinoceros from the Kolyma River, and bison and horses from Yukagir, were found here.^[6]

History

The Siberian Traps were formed by one of the largest known volcanic events of the last 500 million years of Earth's geological history. These continued for a million years and are considered the likely cause of the "Great Dying" about 250 million years ago,^[7] which is estimated to have killed 90% of species existing at the time.^[8]

At least three species of humans lived in Southern Siberia around 40,000 years ago: H. sapiens, H. neanderthalensis, and the Denisovans.^[9] The last was determined in 2010 by DNA evidence to be a new species.

Siberia was inhabited by different groups of nomads such as the Enets, the Nenets, the Huns, the Scythians and the Uyghurs. The Khan of Sibir in the vicinity of modern Tobolsk was known as a prominent figure who endorsed Kubrat as Khagan in Avaria in 630. The Mongols conquered a large part of this area early in the 13th century. With the breakup of the Golden Horde, the autonomous Siberia Khanate was established in the late 15th century. Turkic-speaking Yakuts migrated north from the Lake Baikal region under pressure from the Mongol tribes during the 13th to 15th century.^[10] Siberia remained a sparsely populated area. Historian John F. Richards wrote: "... it is doubtful that the total early modern Siberian population exceeded 300,000 persons."^[11]

The growing power of Russia in 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 farther and farther east. Towns such as Mangazeya, Tara, Yeniseysk and Tobolsk were developed, the last being declared the capital of Siberia. At this time, Sibir was the name of a fortress at Qashlik, near Tobolsk. Gerardus Mercator in a map published in 1595 marks Sibier both as the name of a settlement and of the surrounding territory along a left tributary of the Ob.^[12] Other sources contend that the Xibe, an indigenous Tungusic people, offered fierce resistance to Russian expansion beyond the Urals, and that Siberia is a Russification of their ethnonym.

By the mid-17th century, areas controlled by Russia had been extended to the Pacific. There were some 230,000 Russians in Siberia by 1709.^[13]

The first great modern change in Siberia was the Trans-Siberian Railway, constructed during 1891–1916. It linked Siberia more closely to the rapidly industrialising Russia of Nicholas II. Around seven million people moved to Siberia from European Russia between 1801 and 1914.^[14] From 1859 to 1917, over half a million people migrated to the Russian Far East.^[15] Siberia has extensive natural resources. During the 20th century, large-scale exploitation of these was developed, and industrial towns cropped up throughout the region.^[16]

At 7:15 a.m. on 30 June 1908, millions of trees were felled near the Podkamennaya Tunguska (Stony Tunguska) River in central Siberia in the Tunguska Event, which most scientists believe to have been the air burst of a meteoroid or a comet. Even though no crater has ever been found, the landscape in the (uninhabited) area still bears the scars of this event.

In the early decades of the Soviet Union (especially the 1930s and 1940s), the earlier katorga system of penal labour camps was replaced by a new one that was controlled by the GULAG state agency.^[17] According to semi-official Soviet estimates that were not made public in Soviet times, from 1929 to 1953 more than 14 million people passed through these camps and prisons, many of which were in Siberia. A further seven to eight million were internally deported to remote areas of the Soviet Union (including entire nationalities in several cases).^[18] 516,841 prisoners died in camps from 1941 to 1943^[19] due to food shortages caused by World War II. At other periods, mortality was comparatively lower.^[20] The size, scope, and scale of the GULAG slave labour camps remains a subject of much research and debate. Many Gulag camps were positioned in extremely remote areas of northeastern Siberia. The best known clusters are Sevvostlag (The North-East Camps) along the Kolyma River and Norillag near Norilsk, where 69,000 prisoners were kept in 1952.^[21] Major industrial cities of Northern Siberia, such as Norilsk and Magadan, were originally camps built by prisoners and run by ex-prisoners.^[22]

Geography

With an area of 13.1 million km² (5.1 million square miles), Siberia takes up roughly 77% of Russia's total territory. Major geographical zones include the West Siberian Plain and the Central Siberian Plateau. Siberia covers almost 10% of Earth's land surface (148,940,000 km²). While Siberia falls entirely within Asia, many authorities such as the UN geoscheme will not subdivide countries and will place all of Russia as part of Europe and/or Eastern Europe.

Eastern and central Sakha comprise 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 meters they are almost completely devoid of vegetation. The Verkhoyansk Range 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 the tundra dominates. Soils are mainly turbels (a type of gelisol). The active layer tends to be less than one meter deep, except near rivers.

The highest point in Siberia is the active volcano Klyuchevskaya Sopka, on the Kamchatka Peninsula. Its peak is at 4,649 meters (15,253 ft).

Mountain ranges

Lakes and rivers

Grasslands

• Ukok Plateau — part of a UNESCO World Heritage Site^[23]

Geology

The West Siberian Plain consists mostly of Cenozoic alluvial deposits and is somewhat flat. Many deposits on this plain result from ice dams which produced a large glacial lake. This mid- to late-Pleistocene lake blocked the northward flow of the Ob and Yenisei rivers, resulting in a redirection southwest into the Caspian and Aral seas via the Turgai Valley.^[24] The area 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, most of which is not visible anymore.

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. Much of the area includes the Siberian Traps—a large igneous province. This 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, covering a significant fraction of the entirety of Siberia.^[25] Soils here are mainly turbels, giving way to spodosols where the active layer becomes thicker and the ice content lower.

The Lena-Tunguska petroleum province includes the Central Siberian platform (some authors refer to it as the Eastern Siberian platform), bounded on the northeast and east by the Late Carboniferous through Jurassic Verkhoyansk foldbelt, on the northwest by the Paleozoic Taymr foldbelt, and on the southeast, south and southwest by the Middle Silurian to Middle Devonian Baykalian foldbelt.^[26]:228 A regional geologic reconnaissance study begun in 1932, followed by surface and subsurface mapping, revealed the Markova-Angara Arch (anticline in Russian), which led to the discovery of the Markovo Oil Field in 1962 with the Markovo 1 well, which produced from the Early Cambrian Osa Horizon bar-sandstone at a depth of 2,156 metres (7,073 ft).^[26]:243 The Sredne-Botuobin Gas Field was discovered in 1970, producing from the Osa and the Proterozoic Parfenovo Horizon.^[26]:244 The Yaraktin Oil Field was discovered in 1971, producing from the Vendian Yaraktin Horizon at depths of up to 1,750 metres (5,740 ft), which lies below Permian to Lower Jurassic basalt traps.^[26]:244

Climate

polar desert      tundra      alpine tundra      taiga      montane forest      temperate broadleaf forest      temperate steppe      dry steppe

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

The climate of Siberia varies dramatically, but all of it basically has short summers and long winters of very cold climate. On the north coast, north of the Arctic Circle, there is a very short (about one-month-long) summer.

Almost all the population lives in the south, along the Trans-Siberian Railway. The climate in this southernmost part is Humid continental climate (Köppen Dfb) with cold winters but fairly warm summers lasting at least four months. The annual average is about 0.5 °C (32.9 °F). January averages about −20 °C (−4 °F) and July about +19 °C (66 °F) while daytime temperatures in summer typically are above 20 °C.^[27][28] 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.

By far the most commonly occurring climate in Siberia is continental subarctic (Koppen Dfc or Dwc), with the annual average temperature about −5 °C (23 °F) and an average for January of −25 °C (−13 °F) and an average for July of +17 °C (63 °F),^[29] although this varies considerably, with a July average about 10 °C in the taiga–tundra ecotone. The Business oriented website and blog Business Insider lists Verkhoyansk and Oymyakon, Republic of Sakha, both of which towns are in Russian Siberia, as being in competition for the title of being the Northern Hemisphere's Pole of Cold. Oymyakon is a village with a population of 500 which recorded a temperature of −67.7 °C (−89.9 °F) on 6 February 1933. Verkhoyansk is a relatively nearby neighboring town of just over 1,000 people that recorded a temperature of −69.8 °C (−93.6 °F) for 3 consecutive nights, February 5, 6 and 7. Each town is alternately considered the Northern Hemisphere's Pole of Cold, meaning the coldest inhabited point in the Northern hemisphere. Each town also frequently reaches 86 °F (30 °C) in the summer, giving them, and the majority of the rest of Russian Siberia, the world's greatest temperature variation, between Summer's highs and Winter's lows, often being well over 170-180+ degrees between the seasons.^[30]

Southwesterly winds 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) where in the north an extreme winter subarctic climate (Köppen Dfd or Dwd) prevails. But summer temperatures in other regions can reach +38 °C (100 °F). In general, Sakha is the coldest Siberian region, and the basin of the Yana River has the lowest temperatures of all, with permafrost reaching 1,493 metres (4,898 ft). 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 500 millimeters (20 in) only in Kamchatka where moist winds flow from the Sea of Okhotsk onto high mountains – producing the region's only major glaciers, though volcanic eruptions and low summer temperatures allow limited forests to grow. Precipitation is high also in most of Primorye in the extreme south where monsoonal influences can produce quite heavy summer rainfall.

Climate data for Novosibirsk, Siberia's largest city
Month	Jan	Feb	Mar	Apr	May	Jun	Jul	Aug	Sep	Oct	Nov	Dec	Year
Average high °C (°F)	−12.2 (10)	−10.3 (13.5)	−2.6 (27.3)	8.1 (46.6)	17.5 (63.5)	24.0 (75.2)	25.7 (78.3)	22.2 (72)	16.6 (61.9)	6.8 (44.2)	−2.9 (26.8)	−8.9 (16)	7.0 (44.6)
Daily mean °C (°F)	−16.2 (2.8)	−14.7 (5.5)	−7.2 (19)	3.2 (37.8)	11.6 (52.9)	18.2 (64.8)	20.2 (68.4)	17.0 (62.6)	11.5 (52.7)	3.4 (38.1)	−6.0 (21.2)	−12.7 (9.1)	2.4 (36.3)
Average low °C (°F)	−20.1 (−4.2)	−19.1 (−2.4)	−11.8 (10.8)	−1.7 (28.9)	5.6 (42.1)	12.3 (54.1)	14.7 (58.5)	11.7 (53.1)	6.4 (43.5)	0.0 (32)	−9.1 (15.6)	−16.4 (2.5)	−2.3 (27.9)
Average precipitation mm (inches)	19 (0.75)	14 (0.55)	15 (0.59)	24 (0.94)	36 (1.42)	58 (2.28)	72 (2.83)	66 (2.6)	44 (1.73)	38 (1.5)	32 (1.26)	24 (0.94)	442 (17.4)
Source: [31]

Researchers, including Sergei Kirpotin at Tomsk State University and Judith Marquand at Oxford University, 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.^[32] 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 the result of methane clathrates being released through holes in a frozen 'lid' of seabed permafrost, around the outfall of the Lena River and the area between the Laptev Sea and East Siberian Sea.^[33][34]

Fauna

Order Artiodactyla

• Manchurian wapiti^[35]
• Siberian musk deer^[36]

Order Carnivora

Family Felidae

• Amur leopard^[37]
• Siberian tiger^[38]

Family Ursidae

• Asian black bear^[39]
• Ussuri brown bear^[40]

Flora

• Picea obovata^[41]
• Pinus pumila^[42]

Politics

Borders and administrative division

The term "Siberia" has a long history. Its meaning has gradually changed during ages. Historically, Siberia was defined as the whole part of Russia to the east of Ural Mountains, including the Russian Far East. According to this definition, Siberia extended eastward from the Ural Mountains to the Pacific coast, and southward from the Arctic Ocean to the border of Russian Central Asia and the national borders of both Mongolia and China.^[43]

Soviet-era sources (Great Soviet Encyclopedia and others)^[44] and modern Russian ones^[45] usually define Siberia as a region extending eastward from the Ural Mountains to the watershed between Pacific and Arctic drainage basins, and southward from the Arctic Ocean to the hills of north-central Kazakhstan and the national borders of both Mongolia and China. By this definition, Siberia includes the federal subjects of the Siberian Federal District, and some of the Ural Federal District, as well as Sakha (Yakutia) Republic, which is a part of the Far Eastern Federal District. Geographically, this definition includes subdivisions of several other subjects of Urals and Far Eastern federal districts, but they are not included administratively. 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)^[46] or a somewhat narrower one that limits Siberia to the Siberian Federal District (thus excluding all subjects of other districts).^[47] In Russian, the word for Siberia is used as a substitute for the name of the federal district by those who live in the district itself and less commonly used to denote the federal district by people residing outside of it.

Federal subjects of Siberia (GSE)

subject	administrative center
Ural Federal District
Khanty–Mansi Autonomous Okrug	Khanty-Mansiysk
Kurgan Oblast	Kurgan
Tyumen Oblast	Tyumen
Yamalo-Nenets Autonomous Okrug	Salekhard
Siberian Federal District
Altai Krai	Barnaul
Altai Republic	Gorno-Altaysk
Buryat Republic	Ulan-Ude
Irkutsk Oblast	Irkutsk
Republic of Khakassia	Abakan
Kemerovo Oblast	Kemerovo
Krasnoyarsk Krai	Krasnoyarsk
Novosibirsk Oblast	Novosibirsk
Omsk Oblast	Omsk
Tomsk Oblast	Tomsk
Tuva Republic	Kyzyl
Zabaykalsky Krai	Chita
Far Eastern Federal District
Sakha (Yakutia) Republic	Yakutsk

Federal subjects of Siberia (in wide sense)

subject	administrative center
Far Eastern Federal District
Amur Oblast	Blagoveshchensk
Chukotka Autonomous Okrug	Anadyr
Jewish Autonomous Oblast	Birobidzhan
Kamchatka Krai	Petropavlovsk-Kamchatsky
Khabarovsk Krai	Khabarovsk
Magadan Oblast	Magadan
Primorsky Krai	Vladivostok
Sakhalin Oblast	Yuzhno-Sakhalinsk
Ural Federal District
Chelyabinsk Oblast	Chelyabinsk
Sverdlovsk Oblast	Yekaterinburg

Major cities

The most populous city of Siberia, as well as the third most populous city of Russia, is the city of Novosibirsk. Other major cities include:

• Barnaul
• Irkutsk
• Kemerovo
• Krasnoyarsk
• Novokuznetsk
• Omsk
• Tomsk
• Tyumen

Wider definitions of Siberia also include:

• Chelyabinsk
• Khabarovsk
• Vladivostok
• Yekaterinburg

Economy

Siberia is extraordinarily rich in minerals, containing ores of almost all economically valuable metals. It has some of the world's largest deposits of nickel, gold, lead, coal, molybdenum, gypsum, diamonds, diopside, silver and zinc, as well as extensive unexploited resources of oil and natural gas.^[48] Around 70% of Russia's developed oil fields are in the Khanty-Mansiysk region.^[49] Russia contains about 40% of the world's known resources of nickel at the Norilsk deposit in Siberia. Norilsk Nickel is the world's biggest nickel and palladium producer.^[50]

Siberian 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 practiced by natives for over 10,000 years. Siberia has the world's largest forests. Timber remains an important source of revenue, even though many forests in the east have been logged much more rapidly than they are able to recover. The Sea of Okhotsk is one of the two or three richest fisheries in the world owing to its cold currents and very large tidal ranges, and thus Siberia produces over 10% of the world's annual fish catch, although fishing has declined somewhat since the collapse of the USSR.^[51]

Sport

Professional football teams include FC Tom Tomsk, FC Sibir Novosibirsk and FK Yenisey Krasnoyarsk.

The Yenisey Krasnoyarsk basketball team has played in the VTB United League since 2011.

Demographics

According to the Russian Census of 2010, the Siberian and Far Eastern Federal Districts, located entirely east of the Ural mountains, together have a population of about 25.6 million. Tyumen and Kurgan Oblasts, which are geographically in Siberia but administratively part of the Urals Federal District, together have a population of about 4.3 million. Thus, the whole region of Asian Russia (or Siberia in the broadest usage of the term) is home to approximately 30 million people.^[52] It has a population density of about three people per square kilometer.

Most Siberians are Russians and russified Ukrainians.^[53] There are approximately 400,000 russified ethnic Germans living in Siberia.^[54] Mongol and Turkic groups such as Buryats, Tuvinians, Yakuts, and Siberian Tatars^[55] lived in Siberia originally, and descendants of these peoples still live there.^[56] The Buryats, numbering approximately 500,000, are the largest indigenous group in Siberia, and are mainly concentrated in their homeland, the Buryat Republic.^[57] According to the 2002 census there were 443,852 Yakuts.^[58] Other ethnic groups include Kets, Evenks, Chukchis, Koryaks, Yupiks, and Yukaghirs. The Slavic Russians outnumber all of the native peoples in Siberia and its cities except in the Republic of Tuva, with the Slavic Russians making up the majority in the Buryat, Sakha, and Altai Republics, outnumbering the Buryats, Sakha, and Altai natives. The Buryat make up only 25% of their own republic, and the Sakha and Altai each are only one-third, and the Chukchi, Evenk, Khanti, Mansi, and Nenets are outnumbered by non-natives by 90% of the population.^[59]

About seventy percent of Siberia's people live in cities, mainly in apartments. Many people also live in rural areas, in simple, spacious, log houses. Novosibirsk is the largest city in Siberia, with a population of about 1.5 million. Tobolsk, Tomsk, Tyumen, Krasnoyarsk, Irkutsk and Omsk are the older, historical centers.

Religion

There are a variety of beliefs throughout Siberia,^[60] including Orthodox Christianity, other denominations of Christianity, Tibetan Buddhism and Islam.^[61] An estimated 70,000 Jews live in Siberia,^[62] some in the Jewish Autonomous Region.^[63] The predominant religious group is the Russian Orthodox Church.

Tradition regards Siberia the archetypal home of shamanism, and polytheism is popular.^[64] These native religions date back hundreds of years. The vast territory 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 Olkhon, an island in Lake Baikal.

Transport

Many cities in northern Siberia, such as Petropavlovsk-Kamchatsky, cannot be reached by road, as there are virtually none connecting 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 Vladivostok in the east. Cities not near the railway are best reached by air or by the separate Baikal-Amur-Railway (BAM).

References

Bibliography

• Batalden, Stephen K. (1997). The Newly Independent States of Eurasia: Handbook of Former Soviet Republics. Contributor Sandra L. Batalden (revised ed.). Greenwood Publishing Group. ISBN 0897749405. Retrieved 24 April 2014. 
• Bisher, Jamie (2006). White Terror: Cossack Warlords of the Trans-Siberian. Routledge. ISBN 1135765952. Retrieved 24 April 2014. 
• Bisher, Jamie (2006). White Terror: Cossack Warlords of the Trans-Siberian. Routledge. ISBN 1135765960. Retrieved 24 April 2014. 
• Black, Jeremy (2008). War and the World: Military Power and the Fate of Continents, 1450-2000. Yale University Press. ISBN 0300147694. Retrieved 24 April 2014. 
• Nicholas B. Breyfogle, Abby Schrader and Willard Sunderland (eds), Peopling the Russian Periphery: Borderland Colonization in Eurasian history (London, Routledge, 2007).
• Etkind, Alexander (2013). Internal Colonization: Russia's Imperial Experience. John Wiley & Sons. ISBN 0745673546. Retrieved 24 April 2014. 
• Forsyth, James (1994). A History of the Peoples of Siberia: Russia's North Asian Colony 1581-1990 (illustrated, reprint, revised ed.). Cambridge University Press. ISBN 0521477719. Retrieved 24 April 2014. 
• James Forsyth, A History of the Peoples of Siberia: Russia's North Asian Colony, 1581-1990 (Cambridge, Cambridge University Press, 1994).
• Jack, Zachary Michael, ed. (2008). Inside the Ropes: Sportswriters Get Their Game On. U of Nebraska Press. ISBN 0803219075. Retrieved 24 April 2014. 
• Steven G. Marks, Road to Power: The Trans-Siberian Railroad and the Colonization of Asian Russia, 1850-1917 (London, I.B. Tauris, 1991).
• Mote, Victor L. (1998). Siberia: Worlds Apart. Westview series on the post-Soviet republics (illustrated ed.). Westview Press. ISBN 0813312981. Retrieved 24 April 2014. 
• Igor V. Naumov, The History of Siberia. Edited by David Collins (London, Routledge, 2009) (Routledge Studies in the History of Russia and Eastern Europe).
• Stephan, John J. (1996). The Russian Far East: A History (illustrated, reprint ed.). Stanford University Press. ISBN 0804727015. Retrieved 24 April 2014. 
• Wood, Alan (2011). Russia's Frozen Frontier: A History of Siberia and the Russian Far East 1581 - 1991 (illustrated ed.). A&C Black. ISBN 034097124X. Retrieved 24 April 2014. 
• Alan Wood (ed.), The History of Siberia: From Russian Conquest to Revolution (London, Routledge, 1991).
• Condé Nast's Traveler, Volume 36. Condé Nast Publications. 2001. Retrieved 24 April 2014. 
• Yearbook. Contributor International Work Group for Indigenous Affairs. International Work Group for Indigenous Affairs. 1992. Retrieved 24 April 2014. 

External links

• Novosibirsk: the center of Siberia

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