Kame Formation
Kame Formation is a glacial depositional landform constituting a mound or hill of stratified sand and gravel deposited by meltwater streams in or on a glacier, typically distinguished from other glacial sediments by its localized, irregular topography and association with stagnant ice.
28
Publications
762
Citations
49
Authors
27
Institutions
Publications per year
2017–2026
1
Parents
28
Thermokarst — a mechanism of de‐icing ice‐cored moraines
Terry R. Healy · Boreas · 1975 · 33 citations
1–5 of 28
49
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27

University of Łódź
Lodz, Poland
2 h-index
2 publications
31 citations
The Ohio State University
Columbus, United States
2 h-index
2 publications
39 citations
Heriot-Watt University Malaysia
Putrajaya, Malaysia
1 h-index
1 publications
190 citations

Maria Curie-Skłodowska University
Lublin, Poland
1 h-index
1 publications
11 citations

University of Edinburgh
Edinburgh, United Kingdom
1 h-index
1 publications
10 citations
Geological Survey of Denmark and Greenland
Copenhagen, Denmark
1 h-index
2 publications
28 citations

University of Canterbury
Christchurch, New Zealand
1 h-index
1 publications
39 citations

University of Greenwich
London, United Kingdom
1 h-index
1 publications
29 citations
1–8 of 27
3 publications · 61 citations
3
h-index
2 publications · 39 citations
2
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JQS · 2 publications · 100 citations
2
h-index
2 publications · 33 citations
2
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NZJG · 1 publications · 39 citations
1
h-index
1–5