Cirque Erosion

Cirque Erosion is a geomorphological process denoting the glacial erosion mechanism responsible for the formation and deepening of cirques through frost wedging, plucking, and abrasion occurring preferentially on the leeward, high-elevation slopes of mountainous regions.

41

Publications

1.9K

Citations

98

Authors

61

Institutions

Publications per year

2017–2026

9

Authors

98

  1. BR
    Boris R. Krasnov

    Ben-Gurion University of the Negev, Israel

    4 publications · 288 citations

    4

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  2. MR
    Mary Rowen

    Ben-Gurion University of the Negev, Israel

    2 publications · 50 citations

    2

    h-index

  3. IS
    Ian S. Evans

    Durham University, United Kingdom

    2 publications · 97 citations

    2

    h-index

  4. DS
    David Saltz

    Ben-Gurion University of the Negev, Israel

    2 publications · 50 citations

    2

    h-index

  5. GI
    Georgy I. Shenbrot

    Ben-Gurion University of the Negev, Israel

    2 publications · 211 citations

    2

    h-index

1–5 of 98

Venues

  1. 5

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  2. Annals of Glaciology

    3 publications · 103 citations

    3

    h-index

  3. Journal of Glaciology

    3 publications · 87 citations

    3

    h-index

  4. Earth Surface Processes and Landforms

    2 publications · 97 citations

    2

    h-index

  5. Geology

    2 publications · 127 citations

    2

    h-index

1–5