The ice-wedges at Sławęcin

Authors

  • Anna Dylikowa University of Lodz, Institute of Geography, Poland

DOI:

https://doi.org/10.26485/BP/1956/3/5

Keywords:

frost-fissure networks, frost weathering, Kutno end-moraine

Abstract

An abundant occurrence of ice-wedges was observed in the Kutno terminal moraine near Sławęcin (Middle-Polish glaciation). The wedges were studied in the vertical sections as well as in the plane. The fissures in which the wedges are formed display a network pattern. The wedges themselves and the adjacent portions show such traces of the expansive action of ice as shoved boulders and effects of frost weathering.

References

1. Ducker A., 1954 - Die Periglazial-Erscheinungen im holsteinischen Pleistozan. Gott. Geogr. Abhandl., H. 16.

2. Dylik J., 1952 - Peryglacjalne struktury w plejstocenie środkowej Polski (summary: Periglacial structures in the Pleistocene deposits of Middle Poland). Biul. Państw. Inst. Geol., 66.

3. Jahn A., 1951 - Zjawiska krioturbacyjne współczesnej i plejstoceńskiej strefy peryglacjalnej (summary: Cryoturbate phenomena of the contemporary and of the Pleistocene periglacial zone). Acta Geol. Polonica, vol. 2.

4. Schafer J.P., 1949 - Some periglacial features in central Montana. Jour. Geol., vol. 57.

5. Taber S., 1943 - Perennially frozen ground in Alaska: its origin and history. Bull. Geol. Soc. Am., vol. 54.

Published

2025-12-17

Issue

Section

ARTICLES

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