Cirque Erosion
Cirque Erosion is a geomorphological process denoting the glacial erosion mechanism responsible for the formation and deepening of cirques through frost wedging, plucking, and abrasion occurring preferentially on the leeward, high-elevation slopes of mountainous regions.
41
Publications
1.9K
Citations
98
Authors
61
Institutions
Publications per year
2017–2026
9
Parents
41
Late Cenozoic Glaciation of the Central Brooks Range
Thomas D. Hamilton · Pages · 1986 · 112 citations
Periglacial weathering and headwall erosion in cirque glacier bergschrunds
J. W. Sanders, Kurt M. Cuffey, Jeffrey R. Moore et al. · Geology · 2012 · 112 citations
1–5 of 41
98
4
h-index
2
h-index
2
h-index
2
h-index
2
h-index
1–5 of 98
61
Ben-Gurion University of the Negev
Beersheba, Israel
7 h-index
16 publications
968 citations
University of Colorado Boulder
Boulder, United States
3 h-index
3 publications
77 citations

Stockholm University
Stockholm, Sweden
3 h-index
6 publications
95 citations
Institute of Arctic and Alpine Research
Boulder, United States
3 h-index
3 publications
77 citations

Centre National de la Recherche Scientifique
Paris, France
2 h-index
7 publications
122 citations

Durham University
Durham, United Kingdom
2 h-index
2 publications
97 citations

University of British Columbia
Vancouver, Canada
2 h-index
2 publications
79 citations
University of Lausanne
Lausanne, Switzerland
2 h-index
2 publications
56 citations
1–8 of 61
5 publications · 82 citations
5
h-index
3 publications · 103 citations
3
h-index
3 publications · 87 citations
3
h-index
2 publications · 97 citations
2
h-index
2 publications · 127 citations
2
h-index
1–5