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Science

Rock glaciers in the Western and High Tatra Mountains, Western Carpathians

ORCID Icon & ORCID Icon
Pages 844-857 | Received 31 Oct 2016, Accepted 07 Sep 2017, Published online: 25 Oct 2017
 

ABSTRACT

A detailed map of rock glaciers at a scale of 1 : 40 000 is produced for the Western and High Tatra Mts., Western Carpathians, based on remotely sensed mapping. We inventoried a total of 383 rock glaciers, covering a total area of 13.84 km2. Most rock glaciers (85 %) are considered relict (without permafrost). These landforms have an average lower limit of 1684 m asl and occupy a total area of 12.50 km2. In contrast, intact rock glaciers (containing permafrost) cover a total area of 1.34 km2 and their average lower limit is located at 1986 m asl, which is 56 m above the previously suggested lower limit of discontinuous permafrost. The inventory adds new information about rock-glacier occurrence in the European high-mountain areas and improves the understanding of present and past environmental conditions in the region.

Software

The mapping, digitizing, analyses of DEM and map compilation were all carried out using ESRI ArcMap 10.3. Final merger of vector and raster map elements was done in Adobe Acrobat Pro DC.

Data availability

The shapefiles of rock-glacier outlines and contributing areas are available on request by the authors. Data users are requested to inform the data owners about the planned activities and invite them to contribute to any work that would lead to a co-authorship.

Acknowledgements

We would like to sincerely thank Marek Křížek for selfless financial support with payment of an article publishing charge. We also thank Bieke Cattoor, Daniel Falaschi and especially Andreas Kellerer-Pirklbauer for their thorough reviews that helped us to substantially improve both the article and the map. The Associate Editor, Jan-Christoph Otto, and the Editor-in-Chief, Mike J. Smith, are thanked for their editorial assistance.

Disclosure statement

No potential conflict of interest was reported by the authors.

Additional information

Funding

This work was supported by the Charles University [grant numbers GAUK 1312214; SVV 260438].