Erosion Thresholds
Erosion Thresholds is a theoretical construct in geomorphology that denotes the minimum critical energy condition—such as shear stress, stream power, or land surface slope—required to initiate the detachment and transport of soil, sediment, or ice by erosional processes across glacial, fluvial, or hillslope environments.
127
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11.5K
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379
Authors
217
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2017–2026
25
127
Gully Erosion, Northwestern Colorado: A Threshold Phenomenon
Peter C. Patton, Stanley A. Schumm · Geology · 1975 · 350 citations
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Cooperative Institute for Research in Environmental Sciences, United States
6 publications · 1.3K citations
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National Oceanography Centre
Southampton, United Kingdom
5 h-index
9 publications
706 citations

Chinese Academy of Sciences
Beijing, China
5 h-index
14 publications
308 citations
Massachusetts Institute of Technology
Cambridge, United States
4 h-index
7 publications
2.1K citations

Centre National de la Recherche Scientifique
Paris, France
4 h-index
16 publications
3K citations
Arizona State University
Tempe, United States
3 h-index
7 publications
801 citations
University of Oxford
Oxford, United Kingdom
3 h-index
3 publications
657 citations
Cooperative Institute for Research in Environmental Sciences
Boulder, United States
3 h-index
7 publications
422 citations
Université Paris-Est Créteil
Créteil, France
3 h-index
9 publications
2.7K citations
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JGR · 8 publications · 1.6K citations
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6 publications · 1.1K citations
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5 publications · 156 citations
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5 publications · 257 citations
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