Cryogeological phenomena in the North Pamir (Central Trans-Alai)

Authors

  • Josef Sekyra Geological Survey, Prague, Czechoslovakia

DOI:

https://doi.org/10.26485/BP/1964/14/15

Keywords:

Pamir, Trans-Alai, cryogenic processes, solifluction, permafrost, frost structures, glaciation, aeolian processes

Abstract

The paper presents results of cryogeological investigations conducted in the North Pamir (Central Trans-Alai) during the summer of 1961 as part of an international expedition to Lenin Peak (7,134 m). The author describes aeolian, glacial and periglacial processes within the Achik-Tash Valley and Alai Depression, analysing river terraces and glacigenic and solifluction deposits. Numerous cryogenic forms were observed – micro- and macro-polygons, thufurs, fossil solifluction structures and glaciosolifluction forms – along with evidence of frost weathering and aeolian erosion at high altitudes. These findings significantly contribute to the understanding of contemporary periglacial processes and the extent of mountain permafrost in the Pamir region.

References

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Published

2025-12-17

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