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Debris-flow activity in five adjacent gullies in a limestone mountain range

Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Debris-flows are infrequent geomorphic phenomena that shape steep valleys and can represent a severe hazard for human settlements and infrastructure. In this study, a debris-flow event chronology has been derived at the regional scale within the Gesäuse National Park (Styria, Austria) using dendrogeomorphic techniques. Sediment sources and deposition areas were mapped by combined field investigation and aerial photography using an Unmanned Aerial Vehicle (UAV). Through the analysis of 384 trees, a total of 47 debris-flows occurring in 19 years between AD 1903 and 2008 were identified in five adjacent gullies. Our results highlight the local variability of debris-flow activity as a result of local thunderstorms and the variable availability of sediment sources.
Wydawca
Czasopismo
Rocznik
Strony
60--66
Opis fizyczny
Bibliogr. 47 poz., rys., wykr.
Twórcy
autor
  • Institute of Mountain Risk Engineering, University of Natural Resources and Life Sciences, Peter Jordanstrasse 82, A-1190 Vienna, Austria
  • Institute of Mountain Risk Engineering, University of Natural Resources and Life Sciences, Peter Jordanstrasse 82, A-1190 Vienna, Austria
autor
  • Dendrolab.ch, Institute of Geological Sciences, University of Berne, Baltzerstrasse 1+3, CH-3012 Berne, Switzerland
  • Institute for Environmental Sciences, University of Geneva, 7 chemin de Drize, CH-1227 Carouge-Geneva, Switzerland
autor
  • Institute of Mountain Risk Engineering, University of Natural Resources and Life Sciences, Peter Jordanstrasse 82, A-1190 Vienna, Austria
autor
  • Institute of Mountain Risk Engineering, University of Natural Resources and Life Sciences, Peter Jordanstrasse 82, A-1190 Vienna, Austria
Bibliografia
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Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-df733e83-d717-41a8-88ac-b069174f4351
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