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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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Keyphrases
Alluvial Environment
7%
Bank Accretion
7%
Bank Erosion
7%
Bed Sediment
7%
Catchment Scale
7%
Channel Morphology
7%
Channel Pattern
7%
Channel Shifting
7%
Channel System
7%
Continental Surfaces
7%
Control Channel
7%
Control Variables
7%
Depth-to-width Ratio
7%
Distinctive Character
7%
Feed Rate
7%
Fine-grained Sediment
7%
Floodplain
28%
Floodplain Morphology
14%
Floodplain Sedimentation
7%
Floodplain Water Bodies
7%
Fluid Mixing
7%
Fluvial Erosion
7%
Four Modes
7%
Hydraulics
7%
Internal Complexity
7%
Lacustrine Environment
7%
Large Rivers
100%
Levee
7%
Long Distance
7%
Low Gradient
7%
Main Channel
28%
Main River
7%
Material Input
7%
Organic Matter Deposition
7%
Palaeo-channel
14%
Partially Decoupled
7%
Ponding
7%
Reach Scale
7%
River Branches
7%
River Channel Pattern
7%
River Morphology
7%
River Pattern
21%
River Processes
7%
Satellite Imagery
7%
Sediment Discharge
7%
Sediment Exchange
14%
Sediment Supply
7%
Sediment Systems
7%
Sediment Transfer
7%
Small Rivers
14%
Small Waters
7%
Swale
7%
Tectonics
7%
Tributary Channel
7%
Tributary Input
7%
Unit Bar
7%
Water Bodies
7%
Water Discharge
7%
Water-filling
7%
Earth and Planetary Sciences
Bank Erosion
12%
Bedform
12%
Channel Morphology
12%
Continent
12%
Fine Grained Sediment
12%
Flood Plain
100%
Lacustrine Environment
12%
River Channel
12%
Satellite Imagery
12%
Tectonics
12%
Water Body
25%