Udokan Plateau

Udokan Plateau is a volcanic region northeast of Lake Baikal marked by basaltic lava flows and numerous volcanic cones scattered across the terrain. The landscape displays clear evidence of repeated volcanic activity shaped over extended geological time periods.

The plateau formed through repeated lava eruptions during several volcanic episodes in the geological past. This activity shaped the region over millions of years and left the geological structures visible today.

The indigenous populations near the Udokan Plateau developed their traditions and practices in accordance with the harsh climate and mountainous environment.

The area sits in a remote region with harsh climate conditions and can be difficult to access. Visitors should prepare for isolated conditions and check local conditions before traveling.

Scientific studies have identified anomalies in the asthenosphere beneath the plateau, indicating variations in lithospheric thickness that influence volcanic processes.

Elevation above the sea: 2,180 m

Part of: Udokan

GPS coordinates: 56.28000,117.77000

Latest update: December 13, 2025 11:47