Ice-pushed Ridges
Ice-Pushed Ridges is a glacial landform consisting of elongated, arcuate to linear accumulations of sediment and bedrock that are thrust or bulldozed by advancing glacial ice, distinguished from other morainic features by their structural continuity and deformational origin at the glacier front.
35
Publications
2.1K
Citations
118
Authors
58
Institutions
Publications per year
2017–2026
2
Variants
Ice-push Ridges
Parents
35
1–5 of 35
118
3
h-index
2
h-index
2
h-index
Netherlands Organisation for Applied Scientific Research, Netherlands
2 publications · 48 citations
2
h-index
2
h-index
1–5 of 118
58
The Ohio State University
Columbus, United States
3 h-index
3 publications
1.1K citations
Netherlands Organisation for Applied Scientific Research
Delft, The Netherlands
2 h-index
5 publications
202 citations
Geological Survey of Canada
Ottawa, Canada
2 h-index
2 publications
40 citations
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Bremerhaven, Germany
2 h-index
12 publications
12.1K citations
University of Copenhagen
Copenhagen, Denmark
2 h-index
4 publications
132 citations

British Antarctic Survey
Cambridge, United Kingdom
1 h-index
2 publications
2.2K citations
University of California, Irvine
Irvine, United States
1 h-index
4 publications
4.4K citations
University of Malta
Msida, Malta
1 h-index
1 publications
18 citations
1–8 of 58
8 publications · 257 citations
8
h-index
3 publications · 35 citations
3
h-index
3 publications · 84 citations
3
h-index
JG · 2 publications · 133 citations
2
h-index
NJG · 2 publications · 85 citations
2
h-index
1–5