Ice wedges: Growth, thaw transformation, and palaeoenvironmental significance
作者:
D. G. Harry,
J. S. Gozdzik,
期刊:
Journal of Quaternary Science
(WILEY Available online 1988)
卷期:
Volume 3,
issue 1
页码: 39-55
ISSN:0267-8179
年代: 1988
DOI:10.1002/jqs.3390030107
出版商: John Wiley&Sons, Ltd
关键词: Permafrost;periglacial;ground ice;ice wedge;ice‐wedge cast
数据来源: WILEY
摘要:
AbstractFrost‐cracking and ice‐wedge growth are fundamental processes within the permafrost environment. Extensive areas of contemporary permafrost terrain are characterised by frost‐fissure polygons, formed by repeated thermal contraction‐cracking of the ground. The incremental growth of ice veins and wedges along the axes of contraction‐cracks contributes significantly to the volume of ground ice in near‐surface permafrost. In areas beyond the present limit of permafrost, the recognition of ice‐wedge pseudomorphs provides one of the few unambiguous indications of the former existence of permafrost conditions. An understanding of the processes of ice‐wedge growth and thaw transformation is essential if contemporary ice wedges are to be used as analogues for Pleistocene frost‐fissure structures, in palaeoenvironmenta
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