East Siberian Lowland in the context of Nizhneyansk

⭐ Core Definition: East Siberian Lowland

The East Siberian Lowland (Russian: Восточно-Сибирская низменность, romanized: Vostochno-Sibirskaya nizmennost), also known as Yana-Kolyma Lowland (Russian: Яно-Колымская низменность, romanized: Yano-Kolymskaya nizmennost), is a vast plain in North-eastern Siberia, Russia. The territory of the lowland is one of the Great Russian Regions. Administratively, it is a part of the Sakha Republic (Yakutia).

Owing to the harshness of the climate the East Siberian Lowland is largely unpopulated. Inhabited centers are small and widely scattered. Andryushkino, Argakhtakh, Chokurdakh, Nizhneyansk, Olenegorsk, Russkoye Ustye, Srednekolymsk, and Zyryanka are among the few towns in the area.

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East Siberian Lowland in the context of Siberia (continent)

Siberia, also known as Siberian Craton, Angaraland (or simply Angara) and Angarida, is an ancient craton in the heart of Siberia. Today forming the Central Siberian Plateau, it formed an independent landmass prior to its fusion into Pangaea during the late Carboniferous-Permian. The Verkhoyansk Sea, a passive continental margin, was fringing the Siberian Craton to the east in what is now the East Siberian Lowland.

Angaraland was named in the 1880s by Austrian geologist Eduard Suess who erroneously believed that in the Paleozoic Era there were two large continents in the Northern Hemisphere: "Atlantis", which was North America connected to Europe via a peninsula (Greenland and Iceland), and "Angara-land", which would have been eastern Asia, named after the Angara River in Siberia.

View the full Wikipedia page for Siberia (continent)

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