Paleoclimatic significance of fossil ice wedges

Authors

  • Troy L. Péwé Department of Geology, Arizona State University, Tempe, Arizona, U.S.A.

DOI:

https://doi.org/10.26485/BP/1966/15/8

Keywords:

ice wedge casts, annual air temperature, former presence of permafrost

Abstract

Fossil ice wedges (ice wedge casts, fente en glace remplie, etc.) have been described from temperate latitudes (Illinois, Poland, Germany, etc.) for decades but interpretations of their paleoclimatic significance are not strictly reliable because of lack of knowledge of the present day climatic significance of existing ice wedges in polar areas. It has been agreed, however, that fossil ice wedges indicate the former presence of permafrost.

Present work indicates  that although permafrost will form in areas that have a mean annual air temperaturę of about 0°C or colder, it is thought that ice wedges form only when the mean annual air temperature is -6 to - 8 ° or colder many years, although in certain local environments ice wedges may form at slightly warmer temperatures.

Ice wedges may exist in an inactive state after climatic warming for thousands of years as long as permafrost remains. In general, permafrost thaws and ice wedges melt when mean annual air temperature warms to more than 0°C. Large areas of the subarctic contain dormant ice wedges.

References

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2025-12-17

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