Site has no vegetation, but surrounding territory can be classified as high mountain tundra
Landform:
Holocene moraine 12 m thickness, deeper bedrock – Paleozoic granites.
Lithology:
Holocene moraine 12 m thickness, deeper bedrock – Paleozoic granites. Predominant: gravel, fragments of stones and sand without soil layer. Ice content in the 12-meters upper layer varies from 5 to 40%. Between 10 and 12 m ice saturated permafrost, high ice content.
Morphology:
Southern slope near the mountain pass Zhusalykezen