Continental Glaciation is a glacial process characterized by the extensive accumulation and flow of ice sheets across vast continental regions, distinguished from alpine glaciation by its large-scale, continent-covering extent and dominance during Quaternary ice age cycles.
2.6K
Publications
182.3K
Citations
6.3K
Authors
1.6K
Institutions
Publications per year
2017–2026
378
Variants
Ice Sheet Glaciation
Parents
Publications
2.6K
A Neoproterozoic Snowball Earth
Paul F. Hoffman, Alan J. Kaufman, Galen P. Halverson et al. · Science · 1998 · 2.7K citations
Cesare Emiliani · The Journal of Geology · 1955 · 1.6K citations
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Authors
6.3K
- WR
16
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- GP
15
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- FA
14
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- JTJohn T. Andrews
Institute of Arctic and Alpine Research, United States
14 publications · 783 citations
14
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- JA
13
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Institutions
1.6K
United States Geological Survey
Reston, United States
41 h-index
132 publications
10.5K citations
Centre National de la Recherche Scientifique
Paris, France
40 h-index
167 publications
16.4K citations
Lamont-Doherty Earth Observatory
Sparkill, United States
36 h-index
109 publications
13.4K citations
Chinese Academy of Sciences
Beijing, China
36 h-index
205 publications
21.5K citations
Geological Survey of Canada
Ottawa, Canada
35 h-index
85 publications
5.8K citations
University of Cambridge
Cambridge, United Kingdom
34 h-index
80 publications
8.1K citations
Planetary Science Institute
Tucson, United States
34 h-index
88 publications
22.4K citations
Columbia University
New York, United States
32 h-index
90 publications
8.8K citations
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Venues
- Geology
107 publications · 10.2K citations
61
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- Quaternary Research
QR · 109 publications · 9.6K citations
57
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- Geological Society of America Bulletin
110 publications · 8.5K citations
50
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- Quaternary Science Reviews
100 publications · 7.2K citations
46
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- Palaeogeography Palaeoclimatology Palaeoecology
62 publications · 4.5K citations
38
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