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Ice Wedge Polygon

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Definition

The surface expression of permafrost crosscut by integrated/intersecting polygonized fractures (formed by means of thermal-contraction) that are filled with frozen water, i.e., ice wedges.

Category

A type of nonsorted patterned ground

A type of periglacial landform

Morphometry

Ice-wedge polygon networks range from a few meters to tens of kilometers in reach (Fig. 1 ) (Washburn 1973; Mackay 1980; French 2007). Typically, individual ice-wedge polygons show diameters in the 5–40 m range (Washburn 1973; French 2007); however, ice-wedge polygons with diameters >100 m have been observed in Eastern Siberia (Geocryology of the USSR, Eastern Siberia and the far east 1989). Ice-wedge diameters at the apex range from <10 cm to >3 m, commonly tapering to a feather edge at a depth of 1 to >10 m (Harris et al. 1988).

Fig. 1
figure 1

An extensive outcrop of thermal-contraction polygons (~15–25 m in diameter) in the Tuktoyaktuk Coastlands (Photo by R. Soare)

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Fig. 1
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References

  • Black RF (1976) Periglacial features indicative of permafrost: ice and soil wedges. Quat Res 6(1):3–26

    CrossRef  Google Scholar 

  • French HM (2007) The periglacial environment. Wiley, West Sussex, 458 p

    CrossRef  Google Scholar 

  • French HM, Guglielman M (2000) Frozen ground phenomena in the vicinity of Terra Nova Bay, Northern Victoria Land, Antarctica, a preliminary report. Geogr Ann 821A:513–526

    CrossRef  Google Scholar 

  • Geocryology of the USSR, Eastern Siberia and the Far East (1989) Geokryologiya SSSR: Vostochnaya Sibir i Dalny Vostok. Nedra, Moscow, 515 p (in Russian)

    Google Scholar 

  • 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. Permafrost subcommittee, National Research Council of Canada. Technical memorandum no 142

    Google Scholar 

  • Lachenbruch AH (1962) Mechanics of thermal contraction cracks and ice wedge polygons in permafrost. Geological Society of America, Special paper 70. 69 p

    Google Scholar 

  • Mackay JR (1980) Deformation of ice-wedge polygons, Garry Island, Northwest Territories. Geological Survey of Canada, paper 80-1A, pp 297–301

    Google Scholar 

  • Mackay JR (2000) Thermally induced movements in ice-wedge polygons, western arctic coast: a long-term study. Géogr Phys Q 54:41–68

    Google Scholar 

  • Mutch TA, Arvidson RE, Binder AB, Guinness EA, Morris EC (1977) The geology of the Viking Lander 2 site. J Geophys Res 82:4452–4467

    CrossRef  Google Scholar 

  • Pina P, Vieira G, Christiansen HH, Barata MT, Oliva M, Neves M, Bandeira L, Lousada M, Jorge M, Saraiva J (2012) Analog studies of ice-wedge polygons in Svalbard: 2011 field campaign, topology and geometry. 43rd Lunar Planet Sci Conf, abstract #2353, Houston

    Google Scholar 

  • Seibert NM, Kargel JS (2001) Small-scale polygonal terrain: implications for liquid surface water. Geophys Res Lett. doi:10.1029/2000GL12093

    Google Scholar 

  • Séjourné A, Costard FN, Gargani J, Soare RJ, Federov A, Marmo C (2011) Scalloped terrain and small-sized polygons in western Utopia Planitia, Mars: A new formation hypothesis. Planetary and Space Science 59(5–6):412–422. doi:10.1016/j.pss.2011.01.007.

    CrossRef  Google Scholar 

  • Soare RJ, Conway SJ, Dohm JM (2014). Possible ice-wedge polygons and recent landscape modification by “wet” periglacial processes in and around the Argyre impact basin, Mars Icarus 233:214–228. doi:org/10.1016/j.icarus.2014.01.034

    Google Scholar 

  • Washburn AL (1973) Periglacial processes and environments. St. Martins Press, New York

    Google Scholar 

  • Williams RS Jr, Ferrigno JG (eds) (2012) State of the earth’s cryosphere at the beginning of the 21st century–Glaciers, global snow cover, floating ice, and permafrost and periglacial environments: U.S. Geological Survey professional paper 1386–A, 546 p

    Google Scholar 

  • Xie H, Ackley SF, Zeng Z, Qiu F (2007) Permafrost and its implication in ‘Louth’ crater (70.5 N, 103.2E) of Mars. Seventh international conference on Mars, #3200, Pasadena, California

    Google Scholar 

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Correspondence to Henrik Hargitai or Richard Soare .

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© 2014 Springer Science+Business Media New York

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Hargitai, H., Soare, R. (2014). Ice Wedge Polygon. In: Encyclopedia of Planetary Landforms. Springer, New York, NY. https://doi.org/10.1007/978-1-4614-9213-9_193-1

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  • DOI: https://doi.org/10.1007/978-1-4614-9213-9_193-1

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