Channel Avulsion
Channel avulsion is a fluvial geomorphology process wherein a river or stream abruptly abandons its established channel in favor of a new course, typically due to sediment aggradation reaching a threshold that destabilizes flow continuity.
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9.2K
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293
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165
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2017–2026
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A simulation model of alluvial stratigraphy
John Bridge, Michael R. Leeder · Sedimentology · 1979 · 659 citations
Experimental study of avulsion frequency and rate of deposition
Madeline Bryant, Peter Falk, Chris Paola · Geology · 1995 · 360 citations
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Utrecht University
Utrecht, The Netherlands
8 h-index
17 publications
2.1K citations

Delft University of Technology
Delft, The Netherlands
6 h-index
11 publications
381 citations
Planetary Science Institute
Tucson, United States
5 h-index
7 publications
420 citations

University of Leeds
Leeds, United Kingdom
5 h-index
11 publications
1.3K citations
Indiana University Bloomington
Bloomington, United States
5 h-index
13 publications
631 citations

University of Minnesota
Minneapolis, United States
4 h-index
9 publications
1.8K citations

Pennsylvania State University
State College, United States
4 h-index
5 publications
1.1K citations
University of New Mexico
Albuquerque, United States
3 h-index
8 publications
312 citations
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JSR · 12 publications · 1.1K citations
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10 publications · 1.3K citations
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8 publications · 1.2K citations
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8 publications · 901 citations
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6 publications · 580 citations
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