Glaciolacustrine Landforms
Glaciolacustrine Landforms is a geomorphological landform category defined by the deposition of sediments in glacial lakes, distinguished from other glacial landforms by its formation through the settling of fine-grained, often varved, sediments in standing water bodies dammed or influenced by glacial ice.
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5.2K
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337
Authors
165
Institutions
Publications per year
2017–2026
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165
Geological Survey of Canada
Ottawa, Canada
10 h-index
17 publications
522 citations

University of Toronto
Toronto, Canada
6 h-index
10 publications
488 citations

Lund University
Lund, Sweden
6 h-index
15 publications
365 citations

Adam Mickiewicz University in Poznań
Poznan, Poland
5 h-index
5 publications
136 citations

University of British Columbia
Vancouver, Canada
4 h-index
9 publications
628 citations

British Geological Survey
Nottingham, United Kingdom
4 h-index
8 publications
305 citations
Lithuanian Geological Survey
Vilnius, Lithuania
3 h-index
10 publications
207 citations

Aarhus University
Aarhus, Denmark
3 h-index
3 publications
103 citations
1–8 of 165
22 publications · 962 citations
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13 publications · 654 citations
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7 publications · 224 citations
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6 publications · 352 citations
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5 publications · 124 citations
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