Kolyma Mountains

The Kolyma Mountains are a mountain system in northeastern Siberia, Russia, spanning parts of Magadan Oblast, the Sakha Republic, and Chukotka.

Northeastern Siberia: Northeastern Siberia is the region of Russia east of the Lena River, extending to the Pacific and Arctic coasts. The Kolyma Mountains occupy a major part of this vast region.
Okhotsk–Chukotka Volcanic Belt: The Okhotsk–Chukotka Volcanic Belt is a Late Cretaceous arc of volcanic rocks across northeastern Russia. Its rocks record magmatism that contributed to the region’s geological structure.
Kolyma Highway: The Kolyma Highway is a road linking Yakutsk and Magadan through northeastern Siberia. It crosses difficult terrain near the mountain system and connects remote settlements.
Yukaghir people: The Yukaghir are Indigenous peoples of northeastern Siberia with distinct languages and cultural traditions. Yukaghir communities have long inhabited parts of the Kolyma region.
Kolyma River: The Kolyma is a major river in northeastern Siberia that flows northeast into the East Siberian Sea. Its basin gives the mountain system its name and drains much of the surrounding highlands.
Mesozoic tectonics of northeastern Asia: Mesozoic tectonics of northeastern Asia describes the plate interactions and mountain-building processes affecting the region during the Mesozoic Era. These processes shaped the geological framework beneath the Kolyma Mountains.
Kolyma Gold Belt: The Kolyma Gold Belt is a major gold-producing region in northeastern Russia. Gold deposits around the mountains have driven exploration, mining, and settlement.
Even people: The Even are a Tungusic-speaking Indigenous people of northeastern Siberia and the Russian Far East. Even communities live across the mountain region and neighboring areas.
Chersky Range: The Chersky Range is a mountain system in northeastern Siberia, west of the Kolyma Mountains. It is a neighboring highland system that helps define the region’s rugged relief.
Glaciation: Glaciation is the formation and movement of glaciers over land. Past and present cold-climate processes have sculpted high mountain terrain here.

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