Ablation Till
Ablation Till is a type of glacial sediment deposited directly by the melting of stagnant or slowly moving ice, distinguished from other tills by its lack of stratification and its formation primarily through the downwasting of the glacier rather than by active flow or transport.
11
Publications
643
Citations
26
Authors
15
Institutions
Publications per year
2017–2026
0
Variants
Ablation MoraineAblation MorainesAblation Tills
11
Karst Topography on Stagnant Glaciers
Lee Clayton · Journal of Glaciology · 1964 · 116 citations · Full text
Karst Topography on Stagnant Glaciers
Lee Clayton · Journal of Glaciology · 1964 · 53 citations
1–5 of 11
26
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1–5 of 26
15

University of Canterbury
Christchurch, New Zealand
2 h-index
2 publications
169 citations
University of Pennsylvania
Philadelphia, United States
1 h-index
1 publications
10 citations

Aarhus University
Aarhus, Denmark
1 h-index
2 publications
44 citations
University of Copenhagen
Copenhagen, Denmark
1 h-index
2 publications
44 citations
University of Illinois Chicago
Chicago, United States
1 h-index
2 publications
212 citations
North Carolina State University
Raleigh, United States
1 h-index
1 publications
47 citations
University of Illinois Urbana-Champaign
Urbana, United States
1 h-index
1 publications
18 citations
Universidad Complutense de Madrid
Madrid, Spain
1 h-index
1 publications
10 citations
1–8 of 15
QR · 2 publications · 79 citations
2
h-index
2 publications · 169 citations
2
h-index
2 publications · 128 citations
2
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JG · 1 publications · 183 citations
1
h-index
1 publications · 40 citations
1
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1–5