Definition
Landforms produced in cold, nonglacial environments (Harris et al. 1988 and references therein) where annual freezing and thawing is present.
Formation
Periglacial landforms form by frost action, the alternate freezing and thawing of moisture in unconsolidated or consolidated materials, or by permafrost processes, deformation, or cracking in perennially frozen ground Washburn (1980).
Frost action may result in cryoturbation, movements in an unconsolidated material resulting from water-ice phase changes in the active layer (Harris et al. 1988 and references therein), which are responsible for sorted patterned ground or small nonsorted patterned ground (earth hummock).
On slopes, frost action also induces downslope movement of superficial materials that may produce solifluction feature.
Thermal contraction cracking is responsible for polygonal patterned ground, whereas deformation of permafrost on slopes may produce rock glacier. On Earth, periglacial environments are...
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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
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
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
Washburn AL (1980) Permafrost features as evidence of climatic change. Earth Sci Rev 15:327–402
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Feuillet, T., Matsuoka, N. (2015). Periglacial Landforms. In: Hargitai, H., Kereszturi, Á. (eds) Encyclopedia of Planetary Landforms. Springer, New York, NY. https://doi.org/10.1007/978-1-4614-3134-3_258
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