Deglaciation Landforms

Deglaciation Landforms is a geomorphological construct denoting a category of landforms that originate from the retreat and melting of glacial ice, distinguished by their formation through processes such as meltwater erosion, sediment deposition, and isostatic rebound associated with the loss of ice mass.

183

Publications

9K

Citations

576

Authors

295

Institutions

Publications per year

2017–2026

31

Authors

576

  1. MW
    Marc W. Caffee

    Purdue University West Lafayette, United States

    4 publications · 140 citations

    4

    h-index

  2. JK
    Johan Klemån

    Stockholm University, Sweden

    4 publications · 264 citations

    4

    h-index

  3. DE
    David E. Sugden

    University of Edinburgh, United Kingdom

    4 publications · 299 citations

    4

    h-index

  4. DF
    Derek Fabel

    Scottish Universities Environmental Research Centre, United Kingdom

    4 publications · 193 citations

    4

    h-index

  5. CÓ
    Colm Ó Cofaigh

    Durham University, United Kingdom

    3 publications · 113 citations

    3

    h-index

1–5 of 576

Venues

  1. Quaternary Science Reviews

    16 publications · 793 citations

    16

    h-index

  2. Boreas

    16 publications · 649 citations

    13

    h-index

  3. Geografiska Annaler Series A Physical Geography

    15 publications · 519 citations

    12

    h-index

  4. Geomorphology

    12 publications · 512 citations

    11

    h-index

  5. Journal of Quaternary Science

    JQS · 6 publications · 312 citations

    6

    h-index

1–5