Basal Till is a type of glacial sediment deposited directly by glacial ice through the lodgment, melt-out, or deformation of supraglacial and englacial debris at the glacier bed, distinguished from other glacial till by its subglacial origin and association with basal ice flow processes.
194
Publications
10.3K
Citations
371
Authors
174
Institutions
Publications per year
2017–2026
11
Publications
194
Deformation of till beneath ice stream B, West Antarctica
Richard B. Alley, D. D. Blankenship, Charles R. Bentley et al. · Nature · 1986 · 609 citations
Deforming-bed origin for southern Laurentide till sheets?
Richard B. Alley · Journal of Glaciology · 1991 · 267 citations · Full text
1–5 of 194
Authors
371
- DM
7
h-index
- NR
7
h-index
- RL
7
h-index
- JA
6
h-index
- RB
6
h-index
1–5 of 371
Institutions
174
University of Wisconsin–Madison
Madison, United States
8 h-index
17 publications
3K citations
Aarhus University
Aarhus, Denmark
8 h-index
15 publications
934 citations
University of Minnesota
Minneapolis, United States
7 h-index
14 publications
609 citations
University of Alaska Fairbanks
Fairbanks, United States
6 h-index
14 publications
803 citations
Geological Survey of Finland
Espoo, Finland
6 h-index
12 publications
253 citations
University of Wales
Cardiff, United Kingdom
6 h-index
10 publications
603 citations
Technical University of Denmark
Kongens Lyngby, Denmark
5 h-index
21 publications
713 citations
Pennsylvania State University
State College, United States
5 h-index
8 publications
623 citations
1–8 of 174
Venues
- Journal of Glaciology
26 publications · 1.6K citations
20
h-index
- Boreas
27 publications · 1.1K citations
19
h-index
- Annals of Glaciology
9 publications · 429 citations
9
h-index
- Canadian Journal of Earth Sciences
9 publications · 239 citations
9
h-index
- Journal of Quaternary Science
JQS · 8 publications · 372 citations
8
h-index
1–5