Point Bars
Point Bar is a fluvial depositional landform that constitutes a curved, typically crescent-shaped accumulation of sediment on the inner bank of a river meander, distinguished from other channel sediments by its formation through the deceleration of flow and consequent deposition of suspended and bedload material in zones of reduced shear stress.
193
Publications
12.7K
Citations
459
Authors
223
Institutions
Publications per year
2017–2026
39
Variants
Point Bar
193
How do gravel-bed rivers braid?
Peter Ashmore · Canadian Journal of Earth Sciences · 1991 · 366 citations
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459
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223

University of Calgary
Calgary, Canada
11 h-index
26 publications
1.5K citations

University of Padua
Padua, Italy
10 h-index
37 publications
1.4K citations
The University of Texas at Austin
Austin, United States
7 h-index
14 publications
995 citations

University of Leeds
Leeds, United Kingdom
7 h-index
14 publications
972 citations
Binghamton University
Binghamton, United States
6 h-index
9 publications
1.4K citations

University of Alberta
Edmonton, Canada
5 h-index
8 publications
505 citations

University of Turku
Turku, Finland
5 h-index
11 publications
862 citations
Cardiff University
Cardiff, United Kingdom
5 h-index
5 publications
486 citations
1–8 of 223
26 publications · 2.5K citations
22
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JSR · 18 publications · 1.6K citations
17
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11 publications · 762 citations
11
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7 publications · 612 citations
7
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6 publications · 518 citations
6
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1–5