Ice-marginal Landforms

Ice-Marginal Landforms is a geomorphological construct denoting a class of sedimentary or erosional landforms that are formed at or near the terminus of a glacier, distinguished by their spatial association with the ice margin and their genesis under the influence of glacial meltwater, sediment transport, and ice-flow dynamics.

204

Publications

10.1K

Citations

467

Authors

207

Institutions

Publications per year

2017–2026

36

Authors

467

  1. JL
    Jonathan L. Carrivick

    University of Leeds, United Kingdom

    7 publications · 406 citations

    7

    h-index

  2. DJ
    David J. A. Evans

    Durham University, United Kingdom

    6 publications · 198 citations

    6

    h-index

  3. JK
    Johan Klemån

    Stockholm University, Sweden

    5 publications · 1K citations

    5

    h-index

  4. PK
    Peter Knight

    Keele University, United Kingdom

    5 publications · 164 citations

    5

    h-index

  5. DJ
    Duncan J. Quincey

    University of Leeds, United Kingdom

    5 publications · 311 citations

    5

    h-index

1–5 of 467

Venues

  1. Journal of Glaciology

    17 publications · 777 citations

    16

    h-index

  2. Canadian Journal of Earth Sciences

    13 publications · 495 citations

    13

    h-index

  3. Boreas

    13 publications · 506 citations

    12

    h-index

  4. Quaternary Science Reviews

    11 publications · 1.2K citations

    11

    h-index

  5. Annals of Glaciology

    10 publications · 230 citations

    10

    h-index

1–5