Aufeises of the Siberian permafrost zone and increase of the river channel nets
Aufeises (surface icings) formed by groundwater outflows are widespread on the territory of East Siberia and Far East. By their number, sizes, and the channel-forming role they considerably exceed the “classical” (sedimentary-metamorphic) form of glaciations. Relative coverage of territory by aufeis...
| Main Author: | |
|---|---|
| Format: | Article |
| Language: | Russian |
| Published: |
Nauka
2015-03-01
|
| Series: | Lëd i Sneg |
| Subjects: | |
| Online Access: | https://ice-snow.igras.ru/jour/article/view/57 |