Skip to main navigation
Skip to search
Skip to main content
Aberystwyth Research Portal Home
Help & FAQ
English
Welsh
Home
Researchers
Organisations
Research outputs
Theses
Impacts
Datasets
Projects
Equipment
Press/Media
Activities
Prizes
Search by expertise, name or affiliation
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
Fingerprint
Fingerprint
Dive into the research topics of 'How do big rivers come to be different?'. Together they form a unique fingerprint.
Sort by
Weight
Alphabetically
Earth and Planetary Sciences
Accessory
15%
Accretion
5%
Act
5%
Attention
5%
Bank Erosion
5%
Bar
5%
Bed
5%
Bedform
5%
Bedrock
5%
Catchment
5%
Chain
5%
Channel Morphology
5%
Complexity
5%
Continent
5%
Contrast
5%
Corridor
10%
Deposition
15%
Depth
5%
Determinant
5%
Difference
5%
Distance
5%
Domain
5%
Dyke (Water management)
5%
Erosion
5%
Experience
5%
Fill
5%
Fine Grained Sediment
5%
Flood Plain
42%
Gradient
5%
Input
10%
Investigation
5%
Lacustrine Environment
5%
Lake
5%
Measuring Instrument
5%
Mineral
5%
Mixing
5%
Morphology
15%
Need
5%
Quaternary
5%
Rate
10%
Ratio
5%
Rill
15%
River
100%
River Channel
5%
Route
5%
Satellite Imagery
5%
Sediment
36%
Sedimentation
21%
Set
5%
Show
5%
Sink
5%
Size
5%
Stable
5%
Stream
5%
Symbol
5%
Tectonics
5%
Timescale
5%
Transferring
5%
Tributary
15%
Variability
10%
Water
15%
Water Body
10%
Width
5%