Mountain Asymmetry
Mountain Asymmetry is a geomorphological construct that characterizes the differential slope steepness, elevation distribution, or topographic relief between opposing flanks of a mountain massif, arising from tectonic, climatic, or erosional heterogeneities.
15
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1.1K
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31
Authors
16
Institutions
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2017–2026
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Sapienza University of Rome
Rome, Italy
1 h-index
2 publications
732 citations
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
1 h-index
5 publications
400 citations
China Earthquake Administration
Beijing, China
1 h-index
3 publications
126 citations

Victoria University of Wellington
Wellington, New Zealand
1 h-index
2 publications
358 citations

British Geological Survey
Nottingham, United Kingdom
1 h-index
2 publications
32 citations
Boise State University
Boise, United States
1 h-index
4 publications
296 citations

The University of Melbourne
Melbourne, Australia
1 h-index
3 publications
537 citations
University of Washington
Seattle, United States
1 h-index
2 publications
96 citations
1–8 of 16
3 publications · 223 citations
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2 publications · 34 citations
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2 publications · 110 citations
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1 publications · 366 citations
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1 publications · 33 citations
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