Terminal Moraine is a glacial landform composed of unsorted glacial till that is deposited at the maximum advance position of a glacier’s terminus, marking the farthest extent of glacial progression during a specific period of glacial advance.
223
Publications
9.4K
Citations
493
Authors
233
Institutions
Publications per year
2017–2026
25
Variants
End Moraines
Publications
223
Permafrost creep and rockglaciers
Dietrich Barsch · Permafrost and Periglacial Processes · 1992 · 179 citations
1–5 of 223
Authors
493
- JA
7
h-index
- JS
6
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- RN
5
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- JA
5
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- JB
5
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1–5 of 493
Institutions
233
University of Bergen
Bergen, Norway
11 h-index
27 publications
1.6K citations
United States Geological Survey
Reston, United States
8 h-index
11 publications
240 citations
University of Wisconsin–Madison
Madison, United States
7 h-index
10 publications
207 citations
University of Edinburgh
Edinburgh, United Kingdom
7 h-index
9 publications
344 citations
Durham University
Durham, United Kingdom
6 h-index
12 publications
621 citations
University of Copenhagen
Copenhagen, Denmark
6 h-index
7 publications
336 citations
British Antarctic Survey
Cambridge, United Kingdom
6 h-index
14 publications
756 citations
Stockholm University
Stockholm, Sweden
5 h-index
11 publications
281 citations
1–8 of 233
Venues
- Boreas
14 publications · 537 citations
13
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- Quaternary Research
QR · 13 publications · 934 citations
13
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- Journal of Glaciology
15 publications · 701 citations
12
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- Geografiska Annaler Series A Physical Geography
11 publications · 322 citations
10
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- Annals of Glaciology
10 publications · 330 citations
10
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1–5