Verkhoyansk Range

The Verkhoyansk Range is a mountain system in northeastern Siberia, Russia, extending roughly 1,000 kilometers between the Lena and Aldan river valleys and the Laptev Sea.

Sakha Republic: A federal republic of Russia occupying much of northeastern Siberia. Most of the range lies within this vast republic.
Verkhoyansk-Chukotka orogenic belt: A broad tectonic belt of deformed rocks across northeastern Siberia and Chukotka. The range forms part of this larger system of mountain-building structures.
Verkhoyansk: A small town in the Sakha Republic known for extreme winter cold and a long temperature record. It is a prominent settlement in the mountain region and a reference point for its climate.
Mount Mus-Khaya: A high peak in the Suntar-Khayata Range of northeastern Siberia. It illustrates the high-relief mountain terrain near the Verkhoyansk system.
Lena River: A major Siberian river flowing north from the Baikal region into the Laptev Sea. Its valley marks the range’s western side.
Mesozoic orogeny: Mountain-building deformation associated with tectonic convergence during the Mesozoic Era. Mesozoic tectonic events produced much of the range’s folded structure.
Arctic climate: A climate characterized by very cold conditions, short summers, and limited growing seasons. The range’s high latitude and elevation produce harsh Arctic and subarctic conditions.
Suntar-Khayata Range: A mountain range in northeastern Siberia, south of the Verkhoyansk Range. This neighboring range continues the region’s rugged mountain belt.
Aldan River: A major tributary of the Lena River in southeastern Siberia. Its valley helps define the range’s southern extent.
Permafrost: Ground that remains at or below 0°C for at least two consecutive years. Permafrost strongly influences slopes, soils, and drainage across the range.

Linked from 1 page