Recognition of former frost mounds in Pleistocene deposits and their use as indicators for past environments

Authors

  • Else Kolstrup Uppsala University, Physical Geography, Department of Earth Sciences, Uppsala, Sweden

DOI:

https://doi.org/10.26485/BP/1999/38/11

Keywords:

pingo and palsa mounds, periglacial deposits, palaeoenvironmental reconstructions

Abstract

Formerly active frost mounds (pingos, palsas) can sometimes be recognized as relicts in sediments from, areas that formed part of the periglacial zone during cold periods in the past. This is because the mounds can leave deformation structures indicative of the former growth and decay. Today active forms develop and decay under specific conditions within periglacial areas. Different form groups have different characteristics and associated local and regional environmental requirements. This means that if parallels can be made between a past and a corresponding present form with a fair degree of certainty, and further that the requirements for growth and decay of the present forms are well known, it might be possible to make reconstructions of past environments from Pleistocene remnants. Uncertainties with comparisons and assessments stem from the limited number of published open profiles representing frost mounds in present periglacial areas and Pleistocene formerly cold regions, as well as from insufficient knowledge of present environmental requirements of specific form groups, and, not least, discontinuous Pleistocene sedimentary records. Yet, once reconstructions can be made they may provide information for terrestrial areas otherwise poorly represented in relation to palaeoenvironmental reconstructions. Based upon literature this paper attempts to present a general outline of sedimentological and structural identifications of some presently active forms as well as some remnants.

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2025-06-30

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