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  • 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.
  • 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. (en)
Title
  • Historical chronology of rockfall in the Moravskoslezské Beskydy Mts.
  • Historical chronology of rockfall in the Moravskoslezské Beskydy Mts. (en)
skos:prefLabel
  • Historical chronology of rockfall in the Moravskoslezské Beskydy Mts.
  • Historical chronology of rockfall in the Moravskoslezské Beskydy Mts. (en)
skos:notation
  • RIV/61988987:17310/10:A1100Y5A!RIV11-GA0-17310___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(GAP209/10/0309)
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 261642
http://linked.open...ai/riv/idVysledku
  • RIV/61988987:17310/10:A1100Y5A
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • rockfall; dendrogeomorphology; Moravskoslezské Beskydy Mts. (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...ontrolniKodProRIV
  • [C8834C2A528B]
http://linked.open...v/mistoKonaniAkce
  • Branná
http://linked.open...i/riv/mistoVydani
  • Praha
http://linked.open...i/riv/nazevZdroje
  • Geomorfologický sborník 9
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...iv/tvurceVysledku
  • Šilhán, Karel
http://linked.open...vavai/riv/typAkce
http://linked.open.../riv/zahajeniAkce
number of pages
http://purl.org/ne...btex#hasPublisher
  • Univerzita Karlova v Praze
https://schema.org/isbn
  • 978-80-86561-32-5
http://localhost/t...ganizacniJednotka
  • 17310
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