The asymmetry of periglacial covers in the Izera Mts.

Authors

  • Elżbieta Mycielska University of Warsaw, Faculty of Biology and Earth Sciences, Poland
  • Teresa Nowakowska University of Warsaw, Faculty of Biology and Earth Sciences, Poland

DOI:

https://doi.org/10.26485/BP/1955/2/9

Keywords:

slope cover deposits, Sudetes

Abstract

The Kamieniecki ridge in the Izera Mts. (Sudetes) displays an asymmetrical distribution of covering material. The origin of the rubble covers on the southern and western slopes and that of the detrital  covers on the opposite slopes, the writers attribute to periglacial conditions.

References

1. Borisow A., 1949 - Klimatołogija. Leningrad.

2. Fetzer F., 1953 - Schuttmassen, Blockdecken und Talformen im nordlichen Schwarzwald. Gott. Geogr. Abhandl., H. 14.

3. Flohr E., 1934 - Alter Entstehung und Bewegungserscheinungen der Blockmeere des Riesengebirges. Wrocław.

4. Kerner F., 1891 - Die Anderungen der Bodentemperatur mit der Exposition. Sitz.-Ber. Wiener Akad., 100.

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Published

2025-12-17

Issue

Vol. 2 (1955)

Section

ARTICLES

License

Creative Commons License

This work is licensed under a Creative Commons Attribution 4.0 International License.