Pleistocene periglacial structures and landforms in Western Czechoslovakia
作者:
Tadeáš Czudek,
期刊:
Permafrost and Periglacial Processes
(WILEY Available online 1993)
卷期:
Volume 4,
issue 1
页码: 65-75
ISSN:1045-6740
年代: 1993
DOI:10.1002/ppp.3430040106
出版商: John Wiley&Sons, Ltd
关键词: Pleistocene permafrost;Frost‐crack phenomena;Periglacial landforms
数据来源: WILEY
摘要:
AbstractThe paper describes periglacial structures and landforms developed under Pleistocene coldclimate conditions in western Czechoslovakia. The thickness of Upper Pleistocene permafrost in this territory may have been between 50 and 250 m. Climatically controlled valley asymmetry developed because of different cryogenic processes on opposite valley sides and lateral stream migration (mainly due to thermal erosion). In some cases cryopediment‐like foot‐slopes developed due to down‐wearing of river terraces and/or to the combined effect of down‐wearing and back
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