Striated Bedrock
Striated Bedrock is a glacially scoured rock surface exhibiting parallel grooves and scratches formed by the abrasive action of debris-laden ice moving across the bedrock.
111
Publications
4.5K
Citations
317
Authors
160
Institutions
Publications per year
2017–2026
17
Parents
111
George Plafker, Warren J. Nokleberg, John S. Lull · Journal of Geophysical Research Atmospheres · 1989 · 318 citations
Beryllium-10 Dating of the Duration and Retreat of the Last Pinedale Glacial Sequence
John Gosse, J. Klein, Barbara Lawn et al. · Science · 1995 · 212 citations
A newly recognized type of slickenside striation
W. D. Means · Journal of Structural Geology · 1987 · 126 citations
1–5 of 111
317
Centre National de la Recherche Scientifique, France
2 publications · 96 citations
2
h-index
2
h-index
2
h-index
2
h-index
2
h-index
1–5 of 317
160
Geological Survey of Canada
Ottawa, Canada
5 h-index
8 publications
182 citations

Centre National de la Recherche Scientifique
Paris, France
4 h-index
6 publications
286 citations

Chinese Academy of Sciences
Beijing, China
3 h-index
9 publications
205 citations
University of California, Los Angeles
Los Angeles, United States
3 h-index
5 publications
191 citations
Mineral Resources
Canberra, Australia
2 h-index
2 publications
42 citations

University of Wollongong
Wollongong, Australia
2 h-index
5 publications
64 citations
École & Observatoire des Sciences de la Terre
Strasbourg, France
2 h-index
4 publications
192 citations
Purdue University West Lafayette
West Lafayette, United States
2 h-index
2 publications
97 citations
1–8 of 160
10 publications · 528 citations
10
h-index
5 publications · 106 citations
5
h-index
3 publications · 129 citations
3
h-index
3 publications · 86 citations
3
h-index
3 publications · 210 citations
3
h-index
1–5