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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.
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.
Template: Siberia physical labelled map. 4 languages. ... Physical map of Northern Asia (with parts of Central and East Asia) This page was ...
== Summary == {{en|Main cities of Siberia with population about 500,000 and more. The areas of the circles indicathe the cities' sizes. The cities include Omsk, Novosibirsk, Tomsk, [[:en:Barna: 11:41, 23 June 2006: 974 × 447 (252 KB) Siberiano {{en|Main cities of Siberia with population about 500,000 and more. The areas of the circles ...
The extent of the Siberian Traps (map in German). The Siberian Traps (Russian: Сибирские траппы, romanized: Sibirskiye trappy) are a large region of volcanic rock, known as a large igneous province, in Siberia, Russia.
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), [30] and more moderate winters elsewhere.
US military map 1947. The Chukchi Peninsula (also Chukotka Peninsula or Chukotski Peninsula ; Russian : Чуко́тский полуо́стров , Chukotskiy poluostrov , short form Russian : Чуко́тка , Chukotka ), at about 66° N 172° W, is the easternmost peninsula of Asia .
About 2.5 billion years ago (in the Siderian Period), Siberia was part of a continent called Arctica, along with the Canadian Shield.Around 1.1 billion years ago (in the Stenian Period), Siberia became part of the supercontinent of Rodinia, a state of affairs which lasted until the Tonian about 750 million years ago when it broke up, and Siberia became part of the landmass of Protolaurasia.