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

Authors

317

  1. JG
    Jean‐François Ghienne

    Centre National de la Recherche Scientifique, France

    2 publications · 96 citations

    2

    h-index

  2. MW
    Marc W. Caffee

    Purdue University West Lafayette, United States

    2 publications · 97 citations

    2

    h-index

  3. MD
    Max Deynoux

    Centre National de la Recherche Scientifique, France

    2 publications · 96 citations

    2

    h-index

  4. NF
    Neil F. Glasser

    Aberystwyth University, United Kingdom

    2 publications · 49 citations

    2

    h-index

  5. DG
    David G. Gee

    Uppsala University, Sweden

    2 publications · 48 citations

    2

    h-index

1–5 of 317

Venues

  1. Geomorphology

    10 publications · 528 citations

    10

    h-index

  2. Canadian Journal of Earth Sciences

    5 publications · 106 citations

    5

    h-index

  3. Geological Magazine

    3 publications · 129 citations

    3

    h-index

  4. Annals of Glaciology

    3 publications · 86 citations

    3

    h-index

  5. Geological Society of America Bulletin

    3 publications · 210 citations

    3

    h-index

1–5