Glacial Polish is a geological surface phenomenon characterized by the smooth, finely abraded bedrock finish produced by the abrasive action of debris-laden glacial ice moving across underlying rock, distinguishing it from other glacial erosional features through its fine-grained texture and mirror-like appearance.
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2017–2026
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Publications
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The coating layer of glacial polish
Shalev Siman‐Tov, Greg M. Stock, E. E. Brodsky et al. · Geology · 2017 · 48 citations · Full text
Glacial geomorphology and ice ages in Tibet and the surrounding mountains
Matthias Kuhle · Island Arc · 2005 · 22 citations · Full text
Drift-Ice Abrasion Marks along Rocky Shores
Jean‐Claude Dionne · Journal of Glaciology · 1985 · 13 citations · Full text
Drift-Ice Abrasion Marks along Rocky Shores
Jean‐Claude Dionne · Journal of Glaciology · 1985 · 13 citations
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1–5 of 8
Institutions
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Université Laval
Québec, Canada
2 h-index
2 publications
26 citations
University of California, Santa Cruz
Santa Cruz, United States
1 h-index
2 publications
96 citations
University of Colorado Boulder
Boulder, United States
1 h-index
2 publications
88 citations
National Park Service
Washington, United States
1 h-index
1 publications
48 citations
University of Göttingen
Göttingen, Germany
1 h-index
1 publications
22 citations
University of New Brunswick
Fredericton, Canada
1 h-index
1 publications
48 citations
Institute of Arctic and Alpine Research
Boulder, United States
1 h-index
2 publications
88 citations
Ludwig-Maximilians-Universität München
Munich, Germany
1 h-index
1 publications
44 citations
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Venues
- Journal of Glaciology
2 publications · 26 citations
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- Island Arc
1 publications · 22 citations
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- Arctic Antarctic and Alpine Research
1 publications · 44 citations
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- Geology
1 publications · 48 citations
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