Fluvial incision is a geomorphological process characterized by the downward erosion of river channels into bedrock or alluvial material, driven by the erosive power of flowing water, thereby shaping mountain landscapes through the deepening of valleys and the adjustment of longitudinal profiles.
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Sediment and rock strength controls on river incision into bedrock
L. S. Sklar, W. E. Dietrich · Geology · 2001 · 858 citations
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Cooperative Institute for Research in Environmental Sciences, United States
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Centre National de la Recherche Scientifique
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Massachusetts Institute of Technology
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ETH Zurich
Zurich, Switzerland
13 h-index
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University of Potsdam
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Planetary Science Institute
Tucson, United States
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China Earthquake Administration
Beijing, China
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University of Colorado Boulder
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Reston, United States
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- Geomorphology
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- Earth Surface Processes and Landforms
24 publications · 2.1K citations
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- Journal of Geophysical Research Earth Surface
23 publications · 918 citations
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- Geological Society of America Bulletin
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