Periglacial Sedimentation

Periglacial Sedimentation is a geomorphological process characterized by the accumulation and deposition of sediments in cold-climate environments adjacent to glaciers, where freeze-thaw cycles and periglacial processes such as solifluction, frost heave, and aeolian deposition dominate sediment transport and emplacement.

104

Publications

4.4K

Citations

263

Authors

165

Institutions

Publications per year

2017–2026

7

Authors

263

  1. LS
    Lutz Schirrmeister

    Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Germany

    3 publications · 129 citations

    3

    h-index

  2. SA
    Stuart A. Harris

    University of Calgary, Canada

    3 publications · 94 citations

    3

    h-index

  3. JV
    Jef Vandenberghe

    Vrije Universiteit Amsterdam, Netherlands

    3 publications · 105 citations

    3

    h-index

  4. GØ
    Gunnar Østrem

    Stockholm University, Sweden

    3 publications · 76 citations

    3

    h-index

  5. HC
    Hans Chr. Olsen

    Norwegian Water, Norway

    3 publications · 76 citations

    3

    h-index

1–5 of 263

Venues

  1. 8

    h-index

  2. Journal of Quaternary Science

    JQS · 5 publications · 151 citations

    5

    h-index

  3. Permafrost and Periglacial Processes

    5 publications · 135 citations

    5

    h-index

  4. Earth Surface Processes and Landforms

    5 publications · 232 citations

    5

    h-index

  5. 4

    h-index

1–5