Siberia

Coordinates: 61°0′N 105°0′E / 61.000°N 105.000°E / 61.000; 105.000
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Siberia
Сибирь
US$
480 billion)
 • Per capita₽953,871
(US$12951)

Siberia (/sˈbɪəriə/ sy-BEER-ee-ə; Russian: Сибирь, romanizedSibir', IPA: [sʲɪˈbʲirʲ] ) is an extensive geographical region comprising all of North Asia, from the Ural Mountains in the west to the Pacific Ocean in the east.[3] It has formed part of the sovereign territory of Russia and its predecessor states since the centuries-long conquest of Siberia, which began with the fall of the Khanate of Sibir in the late 16th century and concluded with the annexation of Chukotka in 1778. Siberia is vast and sparsely populated, covering an area of over 13.1 million square kilometres (5,100,000 sq mi), but home to roughly a quarter of Russia's population. Novosibirsk and Omsk are the largest cities in the area.[4]

Because Siberia is a geographic and historic concept and not a political entity, there is no single precise definition of its territorial borders. Traditionally, Siberia spans the entire expanse of land from the

Russian federal subjects), of which only the central one is officially referred to as "Siberian"; the other two are the Ural and Far Eastern federal districts, named for the Ural and Russian Far East
regions that correspond respectively to the western and eastern thirds of Siberia in the broader sense.

Siberia is known for its long, harsh winters, with a January average of −25 °C (−13 °F).

Indigenous small-numbered peoples
by the Russian government), among many others.

Etymology

The origin of the name is uncertain.

Siberian Khanate
.

Some sources say that "Siberia" originates from the

Nenets
.

Mongolist György Kara posits that "Siberia" is derived from a Mongolic word "sibir", cognate with modern Buryat "sheber" or "dense forest".[14]

History

Prehistory

horse trappings, southern Siberia, 280–180 BCE. Hermitage Museum.[15][16][17]

Siberia in

The

Earth's geological history. Their activity continued for a million years and some scientists consider it a possible cause of the "Great Dying" about 250 million years ago,[19] – estimated to have killed 90% of species existing at the time.[20]

The region has

Goldfuss cave lion cubs, Yuka the mammoth and another woolly mammoth from Oymyakon, a woolly rhinoceros from the Kolyma, and bison and horses from Yukagir have been found.[21] Remote Wrangel Island and the Taymyr Peninsula are believed to have been the last places on Earth to support woolly mammoths as isolated populations until their extinction around 2000 BC.[22]

At least three species of human lived in southern Siberia around 40,000 years ago:

In 2010, DNA evidence identified the last as a separate species.[24]

Late Paleolithic southern Siberians appear to be related to paleolithic Europeans and the paleolithic

Paleosiberian peoples and Ancient Native Americans, which later migrated towards the Beringian region, became isolated from other populations, and subsequently populated the Americas.[27][28]

Early history

Chukchi, one of many Indigenous peoples of Siberia. Representation of a Chukchi family by Louis Choris (1816)

During past millennia, different groups of

Yugur – inhabited various parts of Siberia. The Afanasievo and Tashtyk cultures of the Yenisey valley and Altay Mountains are associated with the Indo-European migrations across Eurasia.[29] The proto-Mongol Khitan people also occupied parts of the region. In the 13th century, during the period of the Mongol Empire, the Mongols conquered a large part of this area.[30]

With the breakup of the Golden Horde, the autonomous Khanate of Sibir formed in the late-15th century. Turkic-speaking Yakut migrated north from the Lake Baikal region under pressure from the Mongol tribes during the 13th to 15th century.[31] 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".[32]

The growing power of

which?] contend that the Sibe, an Indigenous Tungusic people, offered fierce resistance to Russian expansion beyond the Urals. Some suggest that the term "Siberia" is a russification of their ethnonym.[11]

Russian Empire

Coat of arms of Siberia, which was a part of the Russian Imperial Coat of Arms until 1917
Map of the Siberian Route in the 18th century (green) and the early 19th century (red)

By the mid-17th century, Russia had established areas of control that extended to the Pacific Ocean. Some 230,000 Russians had settled in Siberia by 1709.[34] Siberia became one of the destinations for sending internal exiles. Exile was the main Russian punitive practice with more than 800,000 people exiled during the nineteenth century.[35][36]

The first great modern change in Siberia was the

Nicholas II (r. 1894–1917). Around seven million Russians moved to Siberia from Europe between 1801 and 1914.[37] Between 1859 and 1917, more than half a million people migrated to the Russian Far East.[38] Siberia has extensive natural resources: during the 20th century, large-scale exploitation of these took place, and industrial towns cropped up throughout the region.[39]

At 7:15 a.m. on 30 June 1908, the

Tunguska Event felled millions of trees near the Podkamennaya Tunguska River (Stony Tunguska River) in central Siberia. Most scientists believe this resulted from the air burst of a meteor or a comet. Even though no crater has ever been found, the landscape in the (sparsely inhabited) area still bears the scars of this event.[40]

Soviet Union

In the early decades of the

internally deported to remote areas of the Soviet Union (including entire nationalities or ethnicities in several cases).[42]

Half a million (516,841) prisoners died in camps from 1941 to 1943[43] during World War II.[citation needed] At other periods, mortality was comparatively lower.[44] The size, scope, and scale of the Gulag slave-labour camps remain subjects of much research and debate. Many Gulag camps operated in extremely remote areas of northeastern Siberia. The best-known clusters included Sevvostlag (the North-East Camps) along the Kolyma and Norillag near Norilsk, where 69,000 prisoners lived in 1952.[45] Major industrial cities of Northern Siberia, such as Norilsk and Magadan, developed from camps built by prisoners and run by former prisoners.[46]

Geography

View from Haiyrakan mountain, Tuva
Altai, Lake Kutsherla in the Altai Mountains
The peninsula of Svyatoy Nos, Lake Baikal
The river Vasyugan in the southern West Siberian Plain
Koryaksky volcano towering over Petropavlovsk-Kamchatsky on the Kamchatka Peninsula

Siberia spans an area of 13.1 million square kilometres (5,100,000 sq mi), covering the vast majority of Russia's total territory, and almost 9% of Earth's land surface (148,940,000 km2, 57,510,000 sq mi). It geographically falls in Asia, but is culturally and politically considered European, since it is a part of Russia.[7] 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. 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 metre deep, except near rivers.

The highest point in Siberia is the active volcano Klyuchevskaya Sopka, on the Kamchatka Peninsula. Its peak reaches 4,750 metres (15,580 ft).

Mountain ranges

Geomorphological regions

Lakes and rivers

Grasslands

Geology

The West Siberian Plain, consisting mostly of

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 no longer visible.[why?
]

Belukha Mountain
Verkhoyansk Range

The Central Siberian Plateau is an ancient

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

Lower Jurassic basalt traps.[50]
: 244 

Climate

Siberian taiga

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

temperate forest
zone in the south.

The climate of Siberia varies dramatically, but it typically has warm but short summers and long, brutally cold winters. 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 route of the Trans-Siberian Railway. The climate in this southernmost part is humid continental climate (Köppen Dfa/Dfb or Dwa/Dwb) with cold winters but fairly warm summers lasting at least four months. The annual average temperature 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 exceed 20 °C (68 °F).[51][52] With a reliable growing season, an abundance of sunshine and exceedingly fertile chernozem soils, southern Siberia is good enough for profitable agriculture, as was demonstrated in the early 20th century.

By far the most commonly occurring climate in Siberia is continental subarctic (Koppen Dfc, Dwc, or Dsc), 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),[53] although this varies considerably, with a July average about 10 °C (50 °F) in the taiga–tundra ecotone. The business-oriented website and blog Business Insider lists Verkhoyansk and Oymyakon, in Siberia's Sakha Republic, as being in competition for the title of the Northern Hemisphere's Pole of Cold. Oymyakon is a village which recorded a temperature of −67.7 °C (−89.9 °F) on 6 February 1933. Verkhoyansk, a town further north and further inland, recorded a temperature of −69.8 °C (−93.6 °F) for three consecutive nights: 5, 6 and 7 February 1933. Each town is alternately considered the Northern Hemisphere's Pole of Cold – the coldest inhabited point in the Northern hemisphere. Each town also frequently reaches 30 °C (86 °F) in the summer, giving them, and much of the rest of Russian Siberia, the world's greatest temperature variation between summer's highs and winter's lows, often well over 94–100+ °C (169–180+ °F) between the seasons.[54][failed verification]

Southwesterly winds bring warm air from Central Asia and the Middle East. The climate in West Siberia (Omsk, or Novosibirsk) is several degrees warmer than in the East (Irkutsk, or Chita) where in the north an extreme winter subarctic climate (Köppen Dfd, Dwd, or Dsd) 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 has the lowest temperatures of all, with permafrost reaching 1,493 metres (4,898 ft). Nevertheless, Imperial Russian plans of settlement never viewed cold as an impediment. 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 millimetres (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 only 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
Mean daily maximum °C (°F) −12.2
(10.0)
−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
(72.0)
16.6
(61.9)
6.8
(44.2)
−2.9
(26.8)
−8.9
(16.0)
7.0
(44.6)
Daily mean °C (°F) −16.2
(2.8)
−14.7
(5.5)
−7.2
(19.0)
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
(21)
−12.7
(9.1)
2.4
(36.3)
Mean daily minimum °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
(32.0)
−9.1
(15.6)
−16.4
(2.5)
−2.3
(27.9)
Average precipitation mm (inches) 19
(0.7)
14
(0.6)
15
(0.6)
24
(0.9)
36
(1.4)
58
(2.3)
72
(2.8)
66
(2.6)
44
(1.7)
38
(1.5)
32
(1.3)
24
(0.9)
442
(17.4)
Source: [55]

Global warming

Researchers, including Sergei Kirpotin at

methane gas, which may be released into the atmosphere. Methane is a greenhouse gas 22 times more powerful than carbon dioxide.[56] In 2008 a research expedition for the American Geophysical Union detected levels of methane up to 100 times above normal in the atmosphere above 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 and the area between the Laptev Sea and East Siberian Sea.[57][58]

Since 1988, experimentation at Pleistocene Park has proposed to restore the grasslands of prehistoric times by conducting research on the effects of large herbivores on permafrost, suggesting that animals, rather than climate, maintained the past ecosystem. The nature reserve park also conducts climatic research on the changes expected from the reintroduction of grazing animals or large herbivores, hypothesizing that a transition from tundra to grassland would lead to a net change in energy emission to absorption ratios.[59]

According to Vasily Kryuchkov, approximately 31,000 square kilometers of the Russian Arctic has subjected to severe environmental disturbance.

Fauna

Birds

Capercaillies inhabit much of the Siberian taiga

Order Galliformes

Family Tetraonidae

Family Phasianidae

Mammals

Order
Artiodactyla

Two saddled Bactrian camels shedding their coats in the Altai mountain range
A muskox on Bolshoy Begichev Island in Laptev Sea

Order Carnivora

Family Canidae

Family Felidae

A Siberian tigress and cub

Family Mustelidae

Family Ursidae

Kamchatka brown bear at Kamchatka Peninsula
Polar bear on Wrangel Island

Flora

Siberian larch Larix sibirica trees in summer. Kuznetsk Alatau Nature Reserve, Kemerovo Oblast

Politics

Notable
sovereign states
in Siberia

Borders and administrative division

Map of the most populated area of Siberia with clickable city names (SVG)
Comparison of the nine biggest Siberian cities' growth in the 20th century

The term "Siberia" has both a long history and wide significance, and association. The understanding, and association of "Siberia" have gradually changed during the ages. Historically, Siberia was defined as the whole part of Russia and North Kazakhstan 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 Central Asia and the national borders of both Mongolia and China.[75]

Soviet-era sources (Great Soviet Encyclopedia and others)[5] and modern Russian ones[76] 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), as well as all Northern Kazakhstan is its subregion in the south-west[3] or a somewhat narrower one that limits Siberia to the Siberian Federal District (thus excluding all subjects of other districts).[77] In Russian, 'Siberia' is commonly used as a substitute for the name of the federal district by those who live in the district itself, but less commonly used to denote the federal district by people residing outside of it. Due to the different interpretations of Siberia, starting from Tyumen, to Chita, the territory generally defined as 'Siberia', some people will define themselves as 'Siberian', while others not.

A number of factors in recent years, including the fomenting of Siberian separatism have made the definition of the territory of Siberia a potentially controversial subject.

self-identification.[79]

Novosibirsk is the largest city in Siberia
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
 Irkutsk Oblast Irkutsk
 Khakassia Abakan
 Kemerovo Oblast Kemerovo
 Krasnoyarsk Krai Krasnoyarsk
 Novosibirsk Oblast Novosibirsk
 Omsk Oblast Omsk
 Tomsk Oblast Tomsk
 Tuva Kyzyl
Far Eastern Federal District
 Buryatia Ulan-Ude
 
Sakha (Yakutia)
Yakutsk
 Zabaykalsky Krai Chita
Amur waterfront in Khabarovsk
Vladivostok, Primorsky Krai
Yakutsk is the capital of the Sakha Republic
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. Present-day Novosibirsk is an important business, science, manufacturing and cultural center of the Asian part of Russia.

Omsk played an important role in the Russian Civil War serving as a provisional Russian capital, as well in the expansion into and governing of Central Asia. In addition to its cultural status, it has become a major oil-refining, education, transport and agriculture hub.

Other historic cities of Siberia include Tobolsk (the first capital and the only kremlin in Siberia), Tomsk (formerly a wealthy merchant's town) and Irkutsk (former seat of Eastern Siberia's governor general, near lake Baikal).

Other major cities include: Barnaul, Kemerovo, Krasnoyarsk, Novokuznetsk, Tyumen.

Wider definitions of geographic Siberia also include the cities of: Chelyabinsk and Yekaterinburg in the Urals, Khabarovsk and Vladivostok in the Russian Far East, and even Petropavlovsk in Kazakhstan and Harbin in China.

Economy

Russian oil and gas pipelines in use

Novosibirsk is the largest by population and the most important city for the Siberian economy; with an extra boost since 2000 when it was designated a regional center for the executive bureaucracy (Siberian Federal District). Omsk is a historic and currently the second largest city in the region, and since 1950s hosting Russia's largest oil refinery.

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.[80] Around 70% of Russia's developed oil fields are in the Khanty-Mansiysk region.[81] 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.[82]

Siberian agriculture is severely restricted by the short growing season of most of the region. However, in the southwest where soils consist of 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.[citation needed] 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 in 1991.[83]

Reported in 2009, the development of renewable energy in Russia is held back by the lack of a conducive government policy framework,[84][needs update] As of 2011, Siberia still offers special opportunities for off-grid renewable energy developments. Remote parts of Siberia are too costly to connect to central electricity and gas grids, and have therefore historically been supplied with costly diesel, sometimes flown in by helicopter. In such cases renewable energy is often cheaper.[85]

Sport

KHL game HC Sibir Novosibirsk vs Amur Khabarovsk

The

Yenisey Krasnoyarsk basketball team has played in the VTB United League
since 2011–12.

Russia's third most popular sport,

, are both based in the city.

The 2019 Winter Universiade was hosted by Krasnoyarsk.

Demographics

Population of Siberia[92][93]
Ethnicity Population %
Slavic 18,235,471 86.2%
Turkic 1,704,665 8.1%
Mongol 454,312 2.1%
Uralic
131,430 0.6%
Other 637,992 3.0%

According to the

Urals Federal District, together have a population of about 4.3 million. Thus, the whole region of Siberia (in the broadest usage of the term) is home to approximately 30 million people.[94]
It has a population density of about three people per square kilometre.

Tomsk, one of the oldest Siberian cities, founded in 1604

The largest ethnic group in Siberia is Slavic-origin

Mongol or Turkic people (mainly Buryats, Yakuts, Tuvans, Altai and Khakas
) or northern Indigenous people. Slavic-origin Russians outnumber all of the Indigenous peoples combined, except in the Republics of Tuva and Sakha.

According to the 2002 census there are 500,000

Yukaghirs
.

About seventy percent of Siberia's people live in cities, mainly in apartments.[99] Many people also live in rural areas, in simple, spacious, log houses. Novosibirsk[100] is the largest city in Siberia, with a population of about 1.6 million. Tobolsk, Tomsk, Tyumen, Krasnoyarsk, Irkutsk, and Omsk are the older, historical centers.

Religion

Transfiguration Cathedral, Khabarovsk

There are a variety of beliefs throughout Siberia, including

Jewish Autonomous Region.[103] The predominant religious group is the Russian Orthodox Church
.

Tradition regards Siberia the archetypal home of

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. Siberia can be reached through the Trans-Siberian Railway. The Trans-Siberian Railway operates from Moscow in the west to Vladivostok in the east. Cities that are located far from the railway are reached by air or by the separate Baikal–Amur Railway (BAM).

Culture

Cuisine

Indigenous people of northern Arctic Siberia made from raw, thin, long-sliced frozen fish.[106] It is a popular dish with native Siberians.[107] Siberia is also known for its pelmeni
dumpling; which in the winter are traditionally frozen and stored outdoors. In addition, there are various berry, nut and mushroom dishes making use of the riches of abundant nature.

See also

References

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