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How do big rivers come to be different?
Philip J. Ashworth,
John Lewin
Department of Geography and Earth Sciences
University of Brighton
Research output
:
Contribution to journal
›
Article
›
peer-review
126
Citations (Scopus)
Overview
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Earth and Planetary Sciences
River
100%
Flood Plain
42%
Sediment
36%
Sedimentation
21%
Morphology
15%
Accessory
15%
Deposition
15%
Water
15%
Rill
15%
Tributary
15%
Rate
10%
Variability
10%
Water Body
10%
Corridor
10%
Input
10%
Difference
5%
Sink
5%
Continent
5%
Need
5%
Gradient
5%
Determinant
5%
Bedform
5%
Bar
5%
Contrast
5%
Fill
5%
Domain
5%
Catchment
5%
Lacustrine Environment
5%
Tectonics
5%
Stream
5%
Transferring
5%
Bedrock
5%
Experience
5%
Investigation
5%
Mineral
5%
Bed
5%
Ratio
5%
Accretion
5%
Lake
5%
Chain
5%
Attention
5%
Mixing
5%
Fine Grained Sediment
5%
Bank Erosion
5%
Show
5%
Symbol
5%
Measuring Instrument
5%
Complexity
5%
River Channel
5%
Width
5%
Size
5%
Erosion
5%
Route
5%
Stable
5%
Act
5%
Depth
5%
Set
5%
Channel Morphology
5%
Satellite Imagery
5%
Distance
5%
Dyke (Water management)
5%
Timescale
5%
Quaternary
5%