Debris flow activity in the Slovak part of the High Tatras in the light of lichenometric dating-Reference-Cited by-同舟云学术

Debris flow activity in the Slovak part of the High Tatras in the light of lichenometric dating

Published:2023-04-14 Issue:1 Volume:96 Page:69-77
ISSN:2300-7362
Container-title:Geographia Polonica
language:en
Short-container-title:Geogr. Pol.

Author:

Kędzia Stanisław¹^ORCID,Hreško Juraj²^ORCID,Bugár Gabriel²^ORCID

Affiliation:

1. Institute of Geography and Spatial Organization Polish Academy of Sciences

2. Department of Ecology and Environmental Sciences, Faculty of Nature Constantine The Philosopher University in Nitra

Abstract

Rock walls and talus slopes, which are the most common features of high-mountain relief, have been researched for many years. Geomorphologists have taken particular interest in debris flows, which play a major role in the development of talus slopes. This paper presents the results of the first lichenometric dating of debris flows on the southern slopes of the Tatra Mountains. The greatest debris flow activity took place in the Little Ice Age and in the last two decades.

Publisher

Institute of Geography and Spatial Organization, Polish Academy of Sciences

Subject

General Earth and Planetary Sciences,Geography, Planning and Development,Urban Studies,Cultural Studies

Link

https://rcin.org.pl/Content/238338/WA51_274441_r2023-t96-no1_G-Polonica-Kedzia.pdf

Reference38 articles.

1. Beschel, R. E. (1950). Flechen als Alters mastab prezenter Moränen. Zeitschrift für Gletscherkunde und Glazialgeologie, 1(2), 152-161.

2. Beschel, R. E. (1957). Lichenometrie im Gletschervorfeld. Jahrbuch des Vereins zum Schutze Alpenpflanzen und Alpentiere, 22, 164-185.

3. Curry, A. M., & Morris, Ch. J. (2004). Lateglacial and Holocene talus slope development and rockwall retreat on Mynydd Du, UK. Geomorphology, 58(1-4), 85-106. https://doi.org/10.1016/S0169-555X(03)00226-5

4. Ferber, T. (2002). The age and origin of talus cones in the light of lichenometric research. The Skalnisty and Zielony talus cones, High Tatra Mountains, Poland. Studia Geomorphologica Carpatho-Balcanica, 36, 77-89. https://www.igipz.pan.pl/tl_files/igipz/ZGiHGiW/sgcb/sgbc_36/36_5.pdf

5. Fort, M., Cossart, E., Deline, P., Dzikowski, M., Nicoud, G., Ravanel, L., Schoeneich, P., & Wassmer, P. (2009). Geomorphic impacts of large and rapid mass movements: A review. Geomorpholgie, 15(1), 47-63. https://doi.org/10.4000/geomorphologie.7495

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