Pingo Formation

Pingo Formation is a geomorphological process denoting the development of conical ice-cored hills in permafrost regions, distinguished by the upward growth of a frozen core due to hydrostatic or hydraulic pressure within saturated, unconsolidated sediments.

82

Publications

3K

Citations

187

Authors

111

Institutions

Publications per year

2017–2026

16

Authors

187

  1. JM
    Jenny Mackay

    University of British Columbia, Canada

    9 publications · 771 citations

    9

    h-index

  2. SW
    Sebastian Wetterich

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

    6 publications · 188 citations

    6

    h-index

  3. KY
    Kenji Yoshikawa

    University of Alaska Fairbanks, United States

    5 publications · 158 citations

    5

    h-index

  4. LS
    Lutz Schirrmeister

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

    4 publications · 131 citations

    4

    h-index

  5. AP
    Albert Pissart

    University of Liège, Belgium

    3 publications · 150 citations

    3

    h-index

1–5 of 187

Venues

  1. Permafrost and Periglacial Processes

    7 publications · 205 citations

    7

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  2. 7

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  3. Canadian Journal of Earth Sciences

    6 publications · 409 citations

    6

    h-index

  4. Arctic and Alpine Research

    4 publications · 109 citations

    4

    h-index

  5. Quaternary Research

    QR · 3 publications · 57 citations

    3

    h-index

1–5