Channel Incision
Channel incision is a geomorphological process characterized by the downward erosion of a riverbed into underlying strata, distinguished from lateral erosion by its vertical entrenchment of the channel profile in response to changes in flow, sediment load, or base level.
269
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22.7K
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781
Authors
396
Institutions
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2017–2026
65
Variants
Stream Incision
269
Floods, channel change, and the hyporheic zone
Steven M. Wondzell, Frederick J. Swanson · Water Resources Research · 1999 · 1.4K citations · Full text
Downstream Ecological Effects of Dams
F. K. Ligon, W. E. Dietrich, William J. Trush · BioScience · 1995 · 790 citations
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396
United States Geological Survey
Reston, United States
13 h-index
22 publications
1.6K citations

Centre National de la Recherche Scientifique
Paris, France
11 h-index
31 publications
2K citations
University of California, Berkeley
Berkeley, United States
10 h-index
14 publications
2.6K citations
The University of Texas at Austin
Austin, United States
9 h-index
12 publications
818 citations
National Sedimentation Laboratory
Oxford, United States
9 h-index
28 publications
2.5K citations

University of Minnesota
Minneapolis, United States
8 h-index
9 publications
919 citations
University of Illinois Urbana-Champaign
Urbana, United States
7 h-index
12 publications
730 citations

Polish Academy of Sciences
Warsaw, Poland
7 h-index
10 publications
616 citations
1–8 of 396
JGR · 22 publications · 4.1K citations
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24 publications · 2.1K citations
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20 publications · 1.1K citations
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12 publications · 1.2K citations
12
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11 publications · 2.5K citations
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