RCIN and OZwRCIN projects

Object

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

Subtitle:

Geographia Polonica Vol. 96 No. 1 (2023)

Publisher:

IGiPZ PAN

Place of publishing:

Warszawa

Description:

24 cm

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.

References:

Beschel, R. E. (1950). Flechen als Alters mastab prezenter Moränen. Zeitschrift für Gletscherkunde und Glazialgeologie, 1(2), 152-161.
Beschel, R. E. (1957). Lichenometrie im Gletschervorfeld. Jahrbuch des Vereins zum Schutze Alpenpflanzen und Alpentiere, 22, 164-185.
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 DOI
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
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 DOI
Francou, B. (1991). Pentes, granulométrie et mobilité le long d'un talus d'éboulis en milieu alpin. Permafrost and Periglacial Processes, 2(3), 175-186. https://doi.org/10.1002/ppp.3430020302 DOI
Gądek, B., Grabiec, M., Kędzia, S., & Rączkowska, Z. (2010). Struktura wewnętrzna i morfodynamika wybranych stoków gruzowych Tatr w świetle wyników pomiarów georadarowych i lichenometrycznych. In A. Kotarba (Ed.), Nauka a zarządzanie obszarem Tatr i ich otoczeniem, t. 1: Nauki o Ziemi, Materiały IV Konferencji "Przyroda Tatrzańskiego Parku Narodowego a człowiek", Zakopane, 14-16 października 2010 (pp. 55-61). Zakopane: Tatrzański Park Narodowy.
Gądek, B., Grabiec, M., Kędzia, S., & Rączkowska, Z. (2016). Reflection of climate changes in the structure and morphodynamics of talus slopes (the Tatra Mountains, Poland). Geomorphology, 263, 39-49. https://doi.org/10.1016/J.GEOMORPH.2016.03.024 DOI
Hinchliffe, S., Ballantyne, C. K., & Walden, J. (1998). The structure and sedimentology of relict talus, Trotternish, northern Skye, Scotland. Earth Surface Processes and Landforms, 23(6), 545-560. https://doi.org/10.1002/(SICI)1096-9837(199806)23:6<545::AID-ESP876>3.0.CO;2-E DOI
Jonasson, C., Kot, M., & Kotarba, A. (1991). Lichenometrical studies and dating of derbis flow deposits in the High Tatra Mountains, Poland. Geografiska Annaler, 73(3-4), 141-146. https://doi.org/10.1080/04353676.1991.11880339 DOI
Kapusta, J. (2009). Sutinové prúdy vo Vysokých Tatrách (Velická dolina a Dolina Zeleného plesa). Univerzita Komenského v Bratislave, Katedra fyzickej geografie a geoekológie. Thesis.
Kapusta, J., Stankoviansky, M., & Boltižiar, M. (2010). Changes in activity and geomorphic effectiveness of debris flows in the High Tatra Mts. within the last six decades (on the example of the Velická Dolina and Dolina Zeleného Plesa Valleys. Studia Geomorphologica Carpatho-Balcanica, 44, 5-34.
Kaszowski, L., Krzemień, K., & Libelt, P. (1988). Postglacial modelling of glacial cirques in the Western Tatras. Zeszyty Naukowe Uniwersytetu Jagiellońskiego, Prace Geograficzne, 71, 121-141.
Kędzia, S. (2010). The age of debris surfaces on the Żółta Turnia Peak (the Polish Tatra Mts.). Geomorphologia Slovaca et Bohemica, 2, 29-38.
Kędzia, S. (2017). Zapis zmian klimatu w ostatnich 200 latach w morfodynamice stoków oraz kriosferze Tatr i Karkonoszy. Przegląd Geograficzny, 89(3), 353-376. https://doi.org/10.7163/PrzG.2017.3.1 DOI
Kędzia, S. (2021). Initial colonisation by Rhizocarpon geographicum in the Tatra Mountains. Journal of Mountain Science, 18(2), 407-415. https://doi.org/10.1007/s11629-020-6130-3 DOI
Kędzia, S., Hreško, J., & Bugár, G. (2020). Lichenometric curve for the southern slope of the Tatra Mountains (Slovak Tatras). Geographia Polonica, 93(4), 597-610. https://doi.org/10.7163/GPol.0187 DOI
Klimaszewski, M. (1978). Geomorfologia. Warszawa: Państwowe Wydawnictwo Naukowe.
Klimaszewski, M. (1988). Relief of the Polish Tatra Mountains. Państwowe Wydawnictwo Naukowe. Warszawa.
Kotarba, A. (1988). Lichenometria i jej zastosowanie w badaniach geomorfologicznych w Tatrach. Wszechświat, 89(1), 13-15.
Kotarba, A. (1989). On the age of debris slops in the Tatra Mountains. Studia Geomorphologica Carpatho-Balcanica, 23, 139-152.
Kotarba, A. (1991). On the ages and magnitude of derbis flows in the Polish Tatra Mountains. Bulletin of the Polish Academy of Science, 39(2), 129-135.
Kotarba, A. (1992). High energy geomorphologic events in the Polish Tatra Mountains. Geografiska Annaler, 74(2/3), 123-131. https://doi.org/10.2307/521290 DOI
Kotarba, A. (1995). Rapid mass wasting over the last 500 years in the High Tatra Mountains. Quaestiones Geographicae, Special Issue, 4, 177-183.
Kotarba, A. (1997). Formation of high mountain talus slope related to debris flow activity in the High Tatra Mountains. Permafrost and Periglacial Processes, 8(2), 191-204. https://doi.org/10.1002/(SICI)1099-1530(199732)8:2<191::AID-PPP250>3.0.CO;2-H DOI
Kotarba, A. (2001). Lichenometryczne oznaczanie wieku formy rzeźby wysokogórskiej. Prace Geograficzne, IGiPZ PAN, 179, 197-208.
Kotarba, A. (2004). Zdarzenia geomorfologiczne w Tatrach Wysokich podczas małej epoki lodowej. In A. Kotarba (Ed.), Rola małej epoki lodowej w przekształcaniu środowiska przyrodniczego Tatr (pp. 9-55). Prace Geograficzne, IGiPZ PAN, 197.
Kotarba, A., Kaszowski, L., & Krzemień, K. (1987). High-mountain denudational system in the Polish Tatra Mountains. Geographical Studies IGiPZ PAN. Special Issue, 3.
Kotarba, A., Kłapa, M., & Rączkowska, Z. (1983). Present-day transformation of Alpine granite slopes in the Polish Tatra Mountains. Dokumentacja Geograficzna, 1.
Kotarba, A., & Pech, P. (2002). The recent evolution of talus slopes in the High Tatra Mountains (with the Pańszczyca Valley as example). Studia Geomorphologica Carpatho-Balcanica, 36, 69-76.
Kotarba, A., Rączkowska, Z., Długosz, M., & Boltiźiar, M. (2013). Recent debris flows in the Tatra Mountains. In Loczy, D., Heidelberg, D. (Eds.), Geomorphological impacts of extreme weather. Case studies from Central and Eastern Europe (pp. 221-236). London - New York: Springer. https://doi.org/10.1007/978-94-007-6301-2_14 DOI
Kotarba, A., & Strömquist, L. (1984). Transport, sorting and deposition processes in the Polish Tatra Mountains. Geografiska Annaler, 66(4), 285-294. https://doi.org/10.2307/520851 DOI
Krautblatter, M., Moser, M., Schrott, L., Wolf, J., & Morche, D. (2012). Significance of rockfall magnitude and carbonate dissolution for rock slope erosion and geomorphic work on Alpine limestone cliffs (Reintal, German Alps). Geomorphology, 167-168, 21-34. https://doi.org/10.1016/J.GEOMORPH.2012.04.007 DOI
Krzemień, K. (1988). The dynamics of debris flows in the upper part of the Starorobociańska Valley (Western Tatra Mts.). Studia Geomorphologica Carpatho-Balcanica, 22, 123-144.
Krzemień, K., Libelt, P., & Mączka, T. (1995). Geomorphological conditions of the timberline in the Western Tatra Mountains. In O. Heikkinen, B. Obrebska-Starkel, & S. Tuhkanen (Eds.), Environmental aspects of the timberline in Finland and the Polish Carpathians (pp. 155-170). Zeszyty Naukowe Uniwersytetu Jagiellońskiego, Prace Geograficzne, 98.
Rączkowska, Z. (2006). Recent geomorphic hazards in the Tatra Mountains. Studia Geomorphologica Carpatho-Balcanica, 11, 45-60.
Rączkowska, Z., Łajczak, A., Margielewski, W., & Święchowicz, J. (2012). Recent landform evolution in the Polish Carpathians. In D. Loczy, A. Kotarba, & M. Stankoviansky (Eds.), Recent landform evolution (pp. 47-101). Dordrecht - Heidelberg - London - New York: Springer. https://doi.org/10.1007/978-94-007-2448-8_5 DOI
Sass, O., & Krautblatter, M. (2007). Debris-flow-dominated and rockfall-dominated scree slopes: genetic models derived from GPR measurements. Geomorphology, 86(1-2), 176-192. https://doi.org/10.1016/j.geomorph.2006.08.012 DOI

Relation:

Geographia Polonica

Volume:

96

Issue:

1

Start page:

69

End page:

77

Detailed Resource Type:

Article

Resource Identifier:

oai:rcin.org.pl:238338 ; doi:10.7163/GPol.0246 ; 0016-7282 (print) ; 2300-7362 (online) ; 10.7163/GPol.0246

Source:

CBGiOS. IGiPZ PAN, call nos.: Cz.2085, Cz.2173, Cz.2406 ; click here to follow the link

Language:

eng

Language of abstract:

eng

Rights:

Creative Commons Attribution BY 4.0 license

Terms of use:

Copyright-protected material. [CC BY 4.0] May be used within the scope specified in Creative Commons Attribution BY 4.0 license, full text available at: ; -

Digitizing institution:

Institute of Geography and Spatial Organization of the Polish Academy of Sciences

Original in:

Central Library of Geography and Environmental Protection. Institute of Geography and Spatial Organization PAS

Projects co-financed by:

European Union. European Regional Development Fund ; Programme Innovative Economy, 2010-2014, Priority Axis 2. R&D infrastructure

Access:

Open

Object collections:

Last modified:

Apr 21, 2023

In our library since:

Apr 21, 2023

Number of object content downloads / hits:

352

All available object's versions:

https://www.rcin.org.pl/igipz/publication/274441

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