Historical chronology of rockfall in the Moravskoslezské Beskydy Mts.

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61988987%3A17310%2F10%3AA1100Y5A" target="_blank" >RIV/61988987:17310/10:A1100Y5A - isvavai.cz</a>
Result on the web
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DOI - Digital Object Identifier
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Result language
angličtina
Original language name
Historical chronology of rockfall in the Moravskoslezské Beskydy Mts.
Original language description
The rockfall isn´t so common type of slope process in Moravskoslezské Beskydy Mts. If there is any, it is usually presented by loosing individual fragments from rock wall. It is very intersting to investigate the intensity of rockfall, because of some factors, which can determinate these processes. Dendrogeomorphological research seems to bee the most efficient method of identification of slope processes. The rockfall was investigated at three places. Two of them were localized on the western slope of Smrk Mt. the last place of research is localized on north slope of Ropice. The difference in rate of rockfall shows totally different values. Each curve had a little bit different long, because of dissimilar age of constituent trees. Because of this, we can say, the climatic influence is the main reason of rockfall.
Czech name
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Czech description
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Project
<a href="/en/project/GAP209%2F10%2F0309" target="_blank" >GAP209/10/0309: Effect of historical climatic and hydrometeorological extremes on slope and fluvial processes in the Western Beskydy Mts. and their forefield</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Publication year
2010
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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