Are sackungen diagnostic features of (de)glaciated mountains?

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61988987%3A17310%2F15%3AA1601EKE" target="_blank" >RIV/61988987:17310/15:A1601EKE - isvavai.cz</a>
Alternative codes found
RIV/49777513:23420/15:43925673
Result on the web
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DOI - Digital Object Identifier
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Result language
angličtina
Original language name
Are sackungen diagnostic features of (de)glaciated mountains?
Original language description
Deep-seated gravitational slope deformations (DSGSDs) with characteristic sackung landforms (e.g., double crests, trenches, uphill-facing scarps, and toe bulging) are considered by some researchers to be diagnostic features indicating past mountain glaciations. However, an extensive literature review on sackung features throughout the world reveals that in some regions, paraglacial processes are not the causes of such phenomena. Sackungen occur across a diverse spectrumofmountain types, with differentmorphoclimatic histories, including regions that have never experienced glaciation.
Czech name
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Czech description
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Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DE - Earth magnetism, geodesy, geography
OECD FORD branch
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Project
<a href="/en/project/GA13-15123S" target="_blank" >GA13-15123S: Spatial and temporal variation of rock mass sagging in the Tatra Mountains (Western Carpathians)</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Publication year
2015
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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