Frost Creep
Frost Creep is a periglacial geomorphic process characterized by the slow, downslope movement of soil and rock debris resulting from freeze-thaw cycles that induce differential frost heave and subsequent gravitational readjustment.
77
Publications
3.5K
Citations
170
Authors
91
Institutions
Publications per year
2017–2026
15
77
Multiaxial creep of frozen loess
Zhiwei Zhou, Wei Ma, Shujuan Zhang et al. · Mechanics of Materials · 2015 · 162 citations
Natural Sciences, Earth Sciences, Geological Engineering +13
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170
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91
University of Tsukuba
Tsukuba, Japan
10 h-index
11 publications
701 citations

Chinese Academy of Sciences
Beijing, China
6 h-index
19 publications
1.6K citations

Hokkaido University
Sapporo, Japan
4 h-index
7 publications
252 citations
Institute of Arctic and Alpine Research
Boulder, United States
3 h-index
4 publications
971 citations
University of Colorado Boulder
Boulder, United States
3 h-index
5 publications
1.2K citations
Cardiff University
Cardiff, United Kingdom
3 h-index
4 publications
179 citations

Centre National de la Recherche Scientifique
Paris, France
3 h-index
10 publications
240 citations
University of Wales
Cardiff, United Kingdom
2 h-index
2 publications
105 citations
1–8 of 91
14 publications · 557 citations
13
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6 publications · 426 citations
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5 publications · 569 citations
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4 publications · 69 citations
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3 publications · 268 citations
3
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