Deltaic Avulsion
Deltaic Avulsion is a geomorphological process denoting the sudden and permanent diversion of a fluvial channel within a deltaic system from one course to a new, topographically lower pathway, distinguished from other channel adjustments by its abrupt nature and reorganization of sediment dispersal patterns.
13
Publications
860
Citations
38
Authors
18
Institutions
Publications per year
2017–2026
6
Parents
13
1–5 of 13
38
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California Institute of Technology
Pasadena, United States
7 h-index
16 publications
1.6K citations
University of Illinois Urbana-Champaign
Urbana, United States
5 h-index
5 publications
476 citations

Rice University
Houston, United States
3 h-index
7 publications
526 citations
Utrecht University
Utrecht, The Netherlands
2 h-index
4 publications
166 citations
University of California, Santa Barbara
Santa Barbara, United States
2 h-index
3 publications
186 citations
Chevron (United States)
San Ramon, United States
1 h-index
3 publications
60 citations
Skagit Valley Hospital
Mount Vernon, United States
1 h-index
1 publications
27 citations

Bureau of Economic Analysis
Washington D.C., United States
1 h-index
1 publications
20 citations
1–8 of 18
3 publications · 392 citations
3
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1 publications · 27 citations
1
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1 publications · 20 citations
1
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PNAS · 1 publications · 78 citations
1
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JSR · 1 publications · 40 citations
1
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1–5