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How do big rivers come to be different?
Philip Ashworth
, J. Lewin
University of Brighton
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peer-review
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Earth & Environmental Sciences
river
100%
floodplain
83%
sediment
76%
tributary
61%
sedimentation
33%
valley
23%
corridor
21%
water body
19%
channel morphology
14%
bank erosion
14%
lacustrine environment
13%
fine grained sediment
13%
bedform
12%
world
12%
levee
12%
river channel
12%
satellite imagery
10%
accretion
10%
water
10%
bedrock
10%
continent
9%
learning
9%
catchment
8%
timescale
8%
erosion
7%
hydraulics
7%
tectonics
7%
rate
7%
lake
6%
mineral
6%
material
4%