Coastal Accretion
Coastal Accretion is a geomorphological process characterized by the gradual accumulation of sediment along coastlines, leading to the extension or elevation of landforms through the deposition of sand, silt, and other materials by wave, current, or wind activity.
70
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2.8K
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224
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116
Institutions
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2017–2026
25
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Mirza Razi Imam Baig, Ishita Afreen Ahmad, Shahfahad et al. · Annals of GIS · 2020 · 175 citations · Full text
Tjeerd H. van Andel · Journal of Sedimentary Research · 1967 · 90 citations
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Royal Netherlands Institute for Sea Research, Netherlands
1 publications · 39 citations
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Centre National de la Recherche Scientifique
Paris, France
2 h-index
3 publications
60 citations
Louisiana State University
Baton Rouge, United States
2 h-index
4 publications
247 citations
University of Rhode Island
Kingston, United States
2 h-index
1 publications
11 citations
Oregon State University
Corvallis, United States
2 h-index
8 publications
488 citations
University of California, Santa Cruz
Santa Cruz, United States
2 h-index
3 publications
213 citations
Universidad de Cádiz
Cadiz, Spain
2 h-index
5 publications
124 citations
United States Geological Survey
Reston, United States
2 h-index
2 publications
90 citations

Chinese Academy of Sciences
Beijing, China
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6 publications
116 citations
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4 publications · 114 citations
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3 publications · 135 citations
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2 publications · 51 citations
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2 publications · 133 citations
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JCR · 2 publications · 23 citations
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