Possibilities and limits of dendrogeomorphic data as a basis for defining thresholds for landslide triggering

Author:

Šilhán KarelORCID,Andrášik Richard,Nezval Vojtěch,Bíl Michal

Funder

Ministerstvo dopravy CR

Ministry of Transport of the People's Republic of China

Ostravská Univerzita v Ostravě

Publisher

Elsevier BV

Subject

Plant Science,Ecology

Reference63 articles.

1. Dendrochronological interpretation of geomorphic processes;Alestalo;Fennia,1971

2. AOPK, 2007. Soil map. 1:50 000. Web map available from: < http://mapy.geology.cz/pudy/>. WMS available from: < http://mapy.geology.cz/arcgis/services/Pudy/pudni_typy50/MapServer/WmsServer>. Agentura ochrany přírody a krajiny České republiky (Nature Conservation Agency of the Czech Republic), Praha.

3. Structure and dynamics of deep-seated slope failures in the Magura Flysch Nappe, outer Western Carpathians (Czech Republic);Baroň;Nat. Hazards Earth Syst. Sci.,2004

4. Baroň, I., Cílek, V., Melichar, R., Melka, K., 2003. Clay minerals in slope sediments of selected deep-seated landslides, Vsetín region, Moravia, Czech Republic. Geologické výzkumy na Moravě a ve Slezsku 89–91. (in Czech).

5. The origin of shallow landslides in Moravia (Czech Republic) in the spring of 2006;Bíl;Geomorphology,2008

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