Periglacial Landforms

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Encyclopedia of Planetary Landforms

Definition

Landforms produced in cold, nonglacial environments (Harris et al. 1988 and references therein) where annual freezing and thawing is present.

Formation

Periglacial landforms and landscape features form in perennially frozen ground, i.e. “permafrost” by freeze-thaw cycling, iterative thermal-contraction cracking, and frost-action (Wasshburn 1980).

Commonplace landforms are solifluction lobes or terraces (freeze-thaw cycling), clastically unsorted polygons (thermal-contraction cracking), and clastically-sorted polygons/circles (frost action) (Harris et al. 1988).

Degradation

The rise of mean temperatures on a local or regional scale may deepen the active layer, lower the permafrost table, and could reduce the areal extent of permafrost (Harris et al. 1988 and references therein).

Surface/Structural Units

Active layer: (seasonally frozen ground) the uppermost, suprapermafrost horizon of ground (soil or rock) subject to annual thawing and freezing, in areas underlain by...

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References

  • Harris SA, French HM, Heginbottom JA, Johnston GH, Ladanyi B, Sego DC, van Everdingen RO (eds) (1988) Glossary of permafrost and related ground-ice terms. Technical memorandum No 142. Permafrost Subcommittee, National Research Council of Canada, Ottawa

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  • Levy JS, Marchant DR, Head JW (2010) Thermal contraction crack polygons on Mars: a synthesis from HiRISE, Phoenix, and terrestrial analog studies. Icarus 206:229–252

    Article  Google Scholar 

  • Lozinski W (1909) Über die mechanische Verwitterung der Sandstein im gemässtigen Klima. Bulletin international de l’académie des sceinces et des lettres de Cracovie, classe des sciences mathématiques et naturelles 1:1–25

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  • Muller SW (1947) Permafrost or permanently frozen ground and related engineering problems. U.S. Geological Survey, U.S. Army, Office of the Chief of Engineers, Strategic Engineering Study no. 62

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  • Washburn AL (1980) Permafrost features as evidence of climatic change. Earth Sci Rev 15:327–402

    Article  Google Scholar 

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Correspondence to Norikazu Matsuoka .

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Feuillet, T., Matsuoka, N. (2022). Periglacial Landforms. In: Hargitai, H., Kereszturi, Á. (eds) Encyclopedia of Planetary Landforms. Springer, New York, NY. https://doi.org/10.1007/978-1-4614-9213-9_258-2

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  • DOI: https://doi.org/10.1007/978-1-4614-9213-9_258-2

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Chapter history

  1. Latest

    Periglacial Landforms
    Published:
    18 October 2022

    DOI: https://doi.org/10.1007/978-1-4614-9213-9_258-2

  2. Original

    Periglacial Landforms
    Published:
    11 August 2014

    DOI: https://doi.org/10.1007/978-1-4614-9213-9_258-1

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