Soil Creep
Soil Creep is a geomorphic process denoting the slow, downslope movement of soil and regolith under the influence of gravity, distinguished from other mass wasting processes by its gradual, continuous, and often imperceptible rate driven by biotic and abiotic disturbances.
210
Publications
10.3K
Citations
545
Authors
256
Institutions
Publications per year
2017–2026
70
210
Soil Creep and the Development of Hillside Slopes
W. E. H. Culling · The Journal of Geology · 1963 · 366 citations
1–5 of 210
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University of California, Santa Barbara, United States
4 publications · 319 citations
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4
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3
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1–5 of 545
256
University of California, Berkeley
Berkeley, United States
8 h-index
13 publications
2.4K citations

Centre National de la Recherche Scientifique
Paris, France
6 h-index
14 publications
426 citations

Chinese Academy of Sciences
Beijing, China
5 h-index
12 publications
558 citations
ETH Zurich
Zurich, Switzerland
5 h-index
6 publications
335 citations
China University of Geosciences
Wuhan, China
5 h-index
8 publications
337 citations

Hong Kong Polytechnic University
Hong Kong, Hong Kong
5 h-index
9 publications
426 citations

Central South University
Changsha, China
4 h-index
17 publications
381 citations
École Centrale de Nantes
Nantes, France
4 h-index
6 publications
204 citations
1–8 of 256
17 publications · 957 citations
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7 publications · 232 citations
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7 publications · 381 citations
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6 publications · 558 citations
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6 publications · 154 citations
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