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The concept of cryo-conditioning in landscape evolution – Comment to the paper published by Ivar Berthling and Bernd Etzelmüller, Quaternary Research 75 (2011) 378–384

Published online by Cambridge University Press:  20 January 2017

Wojciech Dobiński
Wojciech Dobiński*
Affiliation:
Department of Geomorphology, Faculty of Earth Sciences, University of Silesia, Ul. Bedzinska 60, 41-200 Sosnowiec, Poland
*
*Fax: + 48 32 2915865. E-mail address:[email protected].
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Abstract

The term "cryo-conditioning," proposed by the authors for classifying specific landform association in periglacial landscapes, needs to be defined more precisely. A starting point could be the proper understanding of the term "Cryo-" in the various compound words found in various disciplines. This is also important for a correct understanding of the proposed concepts, since it concerns one of the most important processes in nature: the phase transition of water between solid and liquid. Cold-temperate transition surfaces in polythermal glaciers and at the permafrost base in their forelands can act as a specific hub between the glacial and periglacial domains.

Type
Letter to the Editor
Information
Quaternary Research , Volume 77 , Issue 1 , January 2012 , pp. 211 - 212
Copyright
University of Washington

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References

Dobinski, W., (2006). Ice and environment: a terminological discussion. Earth-Science Reviews 79, 229–240.CrossRefGoogle Scholar
Dobrowolski, A.B., (1958). Mój życiorys naukowy. Ossolinski Zakład Narodowy, Wroclaw.Google Scholar
Etzelmüller, B., Hagen, J.O. (2005). Glacier–permafrost interaction in Arctic and alpine mountain environments with examples from southern Norway and Svalbard.CrossRefGoogle Scholar
Everdigen, R.O. van. (1998). Definitions. Multi-language Glossary of Permafrost and Related Ground-ice Terms. International Permafrost Association, University of Calgary, 1–78.Google Scholar
French, H., Thorn, C.E., (2006). The changing nature of periglacial geomorphology. Geomorphologie Relief Processes Environnement 3, 165–173.Google Scholar
Pettersson, R., Jansson, P., Huwald, H., Blatter, H., (2007). Spatial pattern and stability of the cold surface layer of Storglaciären, Sweden. Journal of Glaciology 53, 180, 99–109.Google Scholar
Seligman, G., (1947). Kryology. Journal of Glaciology 1, 1, 35.CrossRefGoogle Scholar
Washburn, A.L., (1973). Periglacial Processes and Environments. Edward Arnold, London.Google Scholar