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North Asia

From Wikipedia, the free encyclopedia
Subregion of Asia
Not to be confused withSiberia.
North Asia
Area13,100,000 km2 (5,100,000 sq mi)
Population37 million (2021 census)
Population density2.6 per km2 (7.4 per mi2)
GDP (PPP)$1.3 trillion (2022)
GDP (nominal)$600 billion (2022)[1]
GDP per capita$16,000 (2022)
Ethnic groupsMajoritySlavic
MinorityTungusic,Mongolic,Turkic, and otherindigenous peoples of Siberia
ReligionsMajorityOrthodox Christian
DemonymSiberian, North Asian
Countries Russia
Languages
Official languages
Time zones
InternetTLD.ru
Calling codeZone 7
Largest cities
UN M49 code151Eastern Europe
150Europe
001World
North Asia
Russian name
RussianСеверная Азия
RomanizationSevernaya Aziya

North Asia orNorthern Asia (Russian:Северная Азия) is the northern region ofAsia, which is defined ingeographical terms and consists of threefederal districts of Russia:Ural,Siberian, and theFar Eastern. North Asia is bordered by theArctic Ocean to its north; byEastern Europe to its west; byCentral Asia andEast Asia to its south; and by thePacific Ocean andNorthern America to its east. It covers an area of 13,100,000 square kilometres (5,100,000 sq mi), or 8.8% ofEarth's total land area; and is the largest subregion of Asia by area, occupying approx. 29.4% of Asia's land area, but is also the least populated, with a population of around 37 million, accounting for merely 0.74% of Asia's population.

Topographically, the region is dominated by theEurasian Plate, except for its eastern part, which lies on theNorth American,Amurian, andOkhotsk Plates. It is divided by three major plains: theWest Siberian Plain,Central Siberian Plateau, and Verhoyansk-Chukotka collision zone. TheUralian orogeny in the west raised Ural Mountains, the informalboundary between Asia and Europe. Tectonic and volcanic activities are frequently occurred in the eastern part of the region as part of theRing of Fire, evidenced by the formation ofisland arcs such as theKuril Islands and ultra-prominent peaks such asKlyuchevskaya Sopka,Kronotsky, andKoryaksky. The central part of North Asia is alarge igneous province called theSiberian Traps, formed by a massive eruption which occurred 250 million years ago. The formation of the traps coincided with thePermian–Triassic extinction event.

Geographically, North Asia is a subregion of Asia. Historically, it has been home to variousEast Asian-related ethnic groups from a diverse range of language families, including theAinu,Chukotko-Kamchatkan,Mongolic,Nivkh,Tungusic,Turkic,Uralic,Yeniseian,Yukaghir, andEskaleut peoples. However, due to theRussian conquest of Siberia, the entirety of North Asia was colonised and incorporated into Russia.European cultural influences, specificallyRussian, are predominant in the entire region, due to it experiencingRussian emigration from Europe starting from the 16th century.[2]Slavs and otherIndo-Europeans make up the vast majority of North Asia's population, and over 85% of the region's population is ofEuropean descent,[3][4] whereas theindigenous peoples comprise only about 5% of the North Asian population.[5]

History

[edit]
Further information:History of human settlement in the Ural Mountains,History of Siberia, andOuter Manchuria
Map of Northern Asia in 1921

The region was first populated byhominins in theLate Pleistocene, approximately 100,000 years ago,[6] and modern humans are confirmed to arrived in the region by 45,000 years ago[7][8] with the first humans in the region having West Eurasian origins.[9]

ItsNeolithic culture is characterized by characteristic stone production techniques and the presence of pottery of eastern origin.[9] TheBronze Age began during the 3rd millennium BCE,[10] with influences ofIndo-Iranian cultures as evidenced by theAndronovo culture. During the 1st millennium BCE,polities such as theScythians andXiongnus emerged in the region, who often clashed with its Persian andChinese neighbors in the south.

TheGöktürks dominated southern Siberia during the 1st millennium CE, while in the early 2nd millennium, theMongol Empire and itssuccessor states ruled the region. TheKhanate of Sibir was one of the last independentTurkic states in North Asia before itsconquest by theTsardom of Russia in the 16th century. Russia would then graduallyannex the region into its territory until theConvention of Peking was signed in 1860.

History of North Asia (1923–2025)

[edit]

Soviet consolidation and conflict (1923–1945)

[edit]

Following theRussian Civil War, theSoviet Union solidified control overSiberia and theRussian Far East. TheFar Eastern Republic, which had served as a buffer state, was dissolved and absorbed by theRussian SFSR in 1922, officially bringing the region under Soviet authority by 1923.[11]

Throughout the 1930s, the Soviet Union fortified the region militarily due to increasing tensions withJapan. TheSoviet–Japanese border conflicts culminated in theBattles of Khalkhin Gol in 1939, where Soviet GeneralGeorgy Zhukov led a decisive victory over Japanese forces, leading to theSoviet–Japanese Neutrality Pact in 1941.[a]

Cold War industrialization (1945–1991)

[edit]

AfterWorld War II, North Asia played a critical role in Soviet industrialization and military strategy. Major industrial centers were developed inNorilsk,Novosibirsk, andIrkutsk, supported by labor from theGulag system.[b]

TheTrans-Siberian Railway, which spanned fromMoscow toVladivostok, became vital for transporting natural resources such as timber, coal, and metals to western parts of the USSR.[12]

Post-Soviet transition and modern era (1991–2025)

[edit]

With the collapse of theSoviet Union in 1991, Eastern Russia faced economic turmoil and depopulation. Many towns built around single industries experienced sharp decline.[13]

In the 2000s and 2010s, the region gained strategic importance due to its vast reserves ofnatural gas,oil, andmineral resources. Russia began expanding infrastructure such as thePower of Siberia gas pipeline toChina, marking a strategic pivot to Asia.[14]

As of the 2020s, theRussian government continues efforts to develop the Russian Far East through the "Far Eastern Hectare" program andspecial economic zones, though progress remains mixed due to geographic challenges and demographic decline.[15]

Geography

[edit]
See also:Geography of Siberia
Further information:Geography of Russia § Northeast Siberia and Kamchatka
Kamchatka Peninsula
Putorana Plateau

For geographical and statistical reasons, theUnited Nations geoscheme and various other classification schemes will not subdivide countries, and thus place all of Russia inEurope or theEastern Europe subregion. There are no mountain chains in North Asia to prevent air currents from theArctic flowing down over theplains ofSiberia andTurkestan.[16]

Theplateau and plains of North Asia comprise theWest Siberian Lowlands; theAngara Shield, with theTaymyr Peninsula, the coastal lowlands (theEast Siberian Lowland and theNorth Siberian Lowland), and theCentral Siberian Plateau (theAnabar Plateau, theLena Plateau, theLena-Angara Plateau, thePutorana Plateau, theTunguska Plateau, and theVilyuy Plateau); and theCentral Yakutian Lowland.[17]Western Siberia is usually regarded as the Northwest Asia,Kazakhstan also sometimes included there. However, Northwest Asia sometimes refers to theSouth Caucasus or its nearby areas.[citation needed]

Geomorphology

[edit]
Further information:Geology of Asia andGeology of Russia

The geomorphology of Northern Asia in general is imperfectly known, although the deposits and mountain ranges are well known.[17]

To compensate for newsea floor having been created in the Siberian basin, the whole of theEurasian Plate has pivoted about a point in theNew Siberian Islands, causing compression in theVerkhoyansk mountains, which were formed along the eastern margin of the Angara Shield bytectonic uplift during theMesozoic Era. There is a southern boundary to this across the northern margin of theAlpine folds of Afghanistan, India, Nepal, and Bhutan, which at the east ofBrahmaputra turns to run south towards theBay of Bengal along the line of theNaga Hills and theArakan Yoma, continues aroundIndonesia, and follows the edge of thecontinental shelf along the eastern seaboard ofChina. TheEurasian Plate and theNorth American Plate meet across the neck ofAlaska, following the line of theAleutian Trench, rather than meeting at theBering Straits.[17]

Northern Asia is built around the Angara Shield, which lies between theYenisey River and theLena River. It developed from fragments ofLaurasia, whose rocks were mainlyPrecambrian crystalline rocks,gneisses, andschists, andGondwana. These rocks can be found in the Angara Shield, Inner Mongolian-Korean Shield, Ordes Shield, and Southeast Asia Shield. The fragments have been subject toorogenesis around their margins, giving a complex of plateaux and mountain ranges. One can findoutcrops of these rocks in unfolded sections of the Shields. Their presence has been confirmed below Mesozoic and later sediments.[17]

There are three main periods of mountain building in Northern Asia, although it has occurred many times. The outer fold mountains that are on the margins of the Shields and that only affected Asia north of the line of theHimalayas, are attributed to theCaledonian andHercynian orogenies of the latePalaeozoic Era. The Alpine orogeny caused extensive folding and faulting of Mesozoic and earlyTertiary sediments from theTethysgeosyncline. The Tibetan and Mongolian plateaux, and the structural basins ofTarim,Qaidam, andJunggar, are delimited by major east–west lithospheric faults that were probably the results of stresses caused by the impact of theIndian Plate against Laurasia. Erosion of the mountains caused by this orogeny has created a large amount of sediment, which has been transported southwards to produce thealluvial plains of India, China, and Cambodia, and which has also been deposited in large amounts in the Tarim andDzungarian basins.[17]

Physical map of Northern Asia
(with parts of Central and East Asia)

Northern Asia wasglaciated in thePleistocene, but this played a less significant part in the geology of the area compared to the part that it played inNorth America andEurope. The Scandinavian ice sheet extended to the east of the Urals, covering the northern two thirds of the Ob Basin and extending onto the Angara Shield between theYenisei River and theLena River. There are legacies of mountain glaciation to be found on the east Siberian mountains, on the mountains of theKamchatka Peninsula, on theAltai, onTian Shan, and on other small areas of mountains,ice caps remain on the islands ofSevernaya Zemlya andNovaya Zemlya, and severalCentral Asian mountains still have individual glaciers. North Asia itself haspermafrost, ranging in depths from 30 to 600 metres and covering an area of 9.6 million km2.[17]

Several of the mountainous regions are volcanic, with both theKoryak Mountains and the Kamchatka Peninsula having activevolcanoes. TheAnadyr Plateau is formed fromigneous rocks. TheMongolian Plateau has an area ofbasalticlavas andvolcanic cones.[17]

The Angara Shield also underlies the lowlands of theOb River, but to the south and east in the Central Asian mountains and in theEast Siberian Mountains there are folded and faulted mountains ofLower Palaeozoic rocks.[17]

Demographics

[edit]
Further information:Demographics of Siberia,Indigenous peoples of Siberia, andDemographics of the Russian Far East
Russians inVladivostok, on Russia's Pacific Coast

Most estimates are that there are around 33 millionRussian citizens living east of theUral Mountains, a widely recognized geographical divide between Europe and Asia. Of these Russian citizens of Siberia, most areSlavic-originRussians and RussifiedUkrainians.[18] TheTurkic peoples who are native to some parts of Siberia and nativeTungusic andMongolic peoples are now a minority in North Asia due to theRussification process during the last three centuries. Russian census records indicate they make up only an estimated 10% of the region's population, with the largest being theBuryats numbering at 445,175, and theYakuts at 443,852. According to the 2002 census, there are 500,000Tatars in Siberia, but 300,000 of them areVolga Tatars who settled in Siberia during periods of colonization.[19] Other ethnic groups that live in the region and make a significant portion include ethnicGermans numbering about 400,000.[20]

In 1875, Chambers reported the population of North Asia to be 8 million.[16] Between 1801 and 1914, an estimated 7 million settlers moved fromEuropean Russia toSiberia, 85% during the quarter-century beforeWorld War I.[21]

 
 
Largest cities or towns in North Asia
RankRegionPop.
1NovosibirskSiberia1,633,595
2YekaterinburgUral (region)1,544,376
3ChelyabinskUral (region)1,189,525
4KrasnoyarskSiberia1,187,771
5OmskSiberia1,125,695
6TyumenUral (region)847,488
7BarnaulSiberia630,877
8KhabarovskRussian Far East617,441
9IrkutskSiberia617,264
10VladivostokRussian Far East603,519

Administration

[edit]
Subdivisions of Asian Russia (Siberia)
Federal SubjectsCapitalArea
km2
Population
2010
Kurgan OblastKurgan71,000910,807
Sverdlovsk OblastYekaterinburg194,8004,297,747
Tyumen OblastTyumen143,5203,395,755
Khanty-Mansi Autonomous Okrug (Yugra)Khanty-Mansiysk534,8001,532,243
Chelyabinsk OblastChelyabinsk87,9003,476,217
Yamalo-Nenets Autonomous OkrugSalekhard750,300522,904
Ural Federal DistrictYekaterinburg1,818,50012,080,526
Altai RepublicGorno-Altaysk92,900206,168
Altai KraiBarnaul168,0002,419,755
Irkutsk OblastIrkutsk774,8002,248,750
Kemerovo OblastKemerovo95,7002,763,135
Krasnoyarsk KraiKrasnoyarsk2,366,8002,828,187
Novosibirsk OblastNovosibirsk177,8002,665,911
Omsk OblastOmsk141,1001,977,665
Tomsk OblastTomsk314,4001,047,394
Tuva RepublicKyzyl168,600307,930
Republic of KhakassiaAbakan61,600532,403
Siberian Federal DistrictNovosibirsk4,361,80017,178,298
Amur OblastBlagoveshchensk361,900830,103
Republic of BuryatiaUlan-Ude351,300971,021
Jewish Autonomous OblastBirobidzhan36,300176,558
Zabaykalsky KraiChita431,9001,107,107
Kamchatka KraiPetropavlovsk-Kamchatsky464,300322,079
Magadan OblastMagadan462,500156,996
Primorsky KraiVladivostok164,7001,956,497
Sakha RepublicYakutsk3,083,500958,528
Sakhalin OblastYuzhno-Sakhalinsk87,100497,973
Khabarovsk KraiKhabarovsk787,6001,343,869
Chukotka Autonomous OkrugAnadyr721,50050,526
Far Eastern Federal DistrictVladivostok6,952,6008,371,257
North Asia13,132,90037,630,081

See also

[edit]

Notes

[edit]
  1. ^SeeSoviet–Japanese border conflicts for further information
  2. ^SeeHistory of Siberia for further information

References

[edit]
  1. ^Валовой региональный продукт по субъектам Российской Федерации в 2016–2022 гг., rosstat.gov.ru
  2. ^Haywood, A. J. (2010).Siberia: A Cultural History. Oxford University Press.ISBN 978-0-19-975418-2.
  3. ^"ВПН-2010".Perepis-2010.ru. Archived fromthe original on 2012-01-18. Retrieved2016-04-03.
  4. ^"ВПН-2010".Gks.ru. Retrieved2016-04-03.
  5. ^"Национальный состав населения".Federal State Statistics Service. Retrieved30 December 2022.
  6. ^Slon V, Viola B, Renaud G, Gansauge M, Benazzi S, Sawyer S, Hublin J, Shunkov MV, Derevianko AP, Kelso J, Prüfer K, Meyer M, Pääbo S (July 2017)."A fourth Denisovan individual".Science Advances.3 (7) e1700186.Bibcode:2017SciA....3E0186S.doi:10.1126/sciadv.1700186.PMC 5501502.PMID 28695206.
  7. ^Callaway, Ewen & Nature magazine (23 October 2014)."45,000-Year-Old Man's Genome Sequenced".Scientific American. Retrieved24 October 2014.
  8. ^Fu, Q; Li, H; Moorjani, P; Jay, F; Slepchenko, SM; Bondarev, AA; Johnson, PL; Aximu-Petri, A; Prüfer, K; de Filippo, C; Meyer, M; Zwyns, N; Salazar-García, DC; Kuzmin, YV; Keates, SG; Kosintsev, PA; Razhev, DI; Richards, MP; Peristov, NV; Lachmann, M; Douka, K; Higham, TF; Slatkin, M; Hublin, JJ; Reich, D; Kelso, J; Viola, TB; Pääbo, S (October 23, 2014)."Genome sequence of a 45,000-year-old modern human from western Siberia".Nature.514 (7523):445–49.Bibcode:2014Natur.514..445F.doi:10.1038/nature13810.PMC 4753769.PMID 25341783.
  9. ^abKılınç, Gülşah Merve; Kashuba, Natalija; Yaka, Reyhan; Sümer, Arev Pelin; Yüncü, Eren; Shergin, Dmitrij; Ivanov, Grigorij Leonidovich; Kichigin, Dmitrii; Pestereva, Kjunnej (2018-06-12)."Investigating Holocene human population history in North Asia using ancient mitogenomes".Scientific Reports.8 (1): 8969.Bibcode:2018NatSR...8.8969K.doi:10.1038/s41598-018-27325-0.ISSN 2045-2322.PMC 5997703.PMID 29895902.
  10. ^Dupuy, Paula Doumani (2016-06-02)."Bronze Age Central Asia".Online Only -- Archaeology.doi:10.1093/oxfordhb/9780199935413.013.15.ISBN 978-0-19-993541-3.
  11. ^"Far Eastern Republic".Britannica. Retrieved2025-05-22.
  12. ^"Trans-Siberian Railway".Britannica. Retrieved2025-05-22.
  13. ^"The Siberian Exodus".The Moscow Times. Retrieved2025-05-22.
  14. ^"Russia's Power of Siberia pipeline opens new era in energy exports".Financial Times. Retrieved2025-05-22.
  15. ^"Russia's Far East: Empty Land, Empty Promises".Carnegie Endowment. Retrieved2025-05-22.
  16. ^abWilliam Chambers and Robert Chambers (1875).Chambers's Information for the People. London and Edinburgh: W. & R. Chambers. pp. 274–276.ISBN 978-0-665-46914-5.{{cite book}}:ISBN / Date incompatibility (help)
  17. ^abcdefghEdwin Michael Bridges (1990)."Northern Asia".World Geomorphology. Cambridge University Press. pp. 124–126.ISBN 978-0-521-28965-8.
  18. ^"Ukrainians in Russia's Far East try to maintain community lifeArchived 2016-03-04 at theWayback Machine".The Ukrainian Weekly. 4 May 2003.
  19. ^"Фотоатлас "Сибирские татары"". February 27, 2002. Archived fromthe original on 2002-02-27.
  20. ^"Siberian Germans".Encyclopedia.com.
  21. ^Fisher, Raymond H. (1958)."Reviewed work: The Great Siberian Migration: Government and Peasant in Resettlement from Emancipation to the First World War, Donald W. Treadgold".The American Historical Review.63 (4):989–990.doi:10.2307/1848991.JSTOR 1848991.
  22. ^"Оценка численности постоянного населения по субъектам Российской Федерации".Federal State Statistics Service. Retrieved20 July 2024.
  23. ^Russian Federal State Statistics Service (2011).Всероссийская перепись населения 2010 года. Том 1 [2010 All-Russian Population Census, vol. 1].Всероссийская перепись населения 2010 года [2010 All-Russia Population Census] (in Russian).Federal State Statistics Service.

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