Headwall Scarps
Headwall Scarps is a morphological feature denoting the steep, often arcuate, upslope boundary of a submarine landslide, distinguished by its position at the head of the failed mass and its formation through the initial rupture and displacement of seafloor sediment.
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2017–2026
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Headwall Scarp
Parents
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Monty A. Hampton, Homa J. Lee, Jacques Locat · Reviews of Geophysics · 1996 · 958 citations
Hillslope Evolution by Bedrock Landslides
Alexander L. Densmore, Robert S. Anderson, Brian G. McAdoo et al. · Science · 1997 · 120 citations · Full text
Widespread fluid expulsion along the seafloor of the Costa Rica convergent margin
Gerhard Bohrmann, K. Heeschen, Carmen Jung et al. · Terra Nova · 2002 · 102 citations
Shallow slides and pockmark swarms in the Eivissa Channel, western Mediterranean Sea
Galderic Lastras, Miquel Canals, Roger Úrgeles et al. · Sedimentology · 2004 · 100 citations · Full text
Climatic limits to headwall retreat in the Khumbu Himalaya, eastern Nepal
Dirk Scherler · Geology · 2014 · 78 citations
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University of California, Santa Cruz
Santa Cruz, United States
1 h-index
3 publications
360 citations

University of Parma
Parma, Italy
1 h-index
5 publications
90 citations
National Oceanic and Atmospheric Administration
Washington, United States
1 h-index
1 publications
42 citations
California Institute of Technology
Pasadena, United States
1 h-index
1 publications
78 citations

Durham University
Durham, United Kingdom
1 h-index
3 publications
132 citations
Oregon State University
Corvallis, United States
1 h-index
4 publications
168 citations
BP (United Kingdom)
London, United Kingdom
1 h-index
2 publications
88 citations
Eni (Italy)
Rome, Italy
1 h-index
4 publications
72 citations
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1 publications · 42 citations
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1 publications · 100 citations
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1 publications · 102 citations
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1 publications · 120 citations
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1 publications · 958 citations
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