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Typ záznamu:	stať ve sborníku (D)
Domácí pracoviště:	Katedra fyzické geografie a geoekologie (31600)
Název:	Large-scale landslides in the culmination part of the Czech flysch Carpathians
Citace	Pánek, T. a Hradecký, J. Large-scale landslides in the culmination part of the Czech flysch Carpathians. In: Regional Conference on Geomorphology, Vol. I. Goiania: International Association of Geomorphologists, 2006. International Association of Geomorphologists, 2006. s. 84-84.

Podnázev
Rok vydání:	2006
Obor:	Zemský magnetismus, geodesie, geografie
Počet stran:	1
Strana od:	84
Strana do:	84
Forma vydání:
Kód ISBN:
Kód ISSN:
Název sborníku:	Regional Conference on Geomorphology, Vol. I
Sborník:
Název nakladatele:	International Association of Geomorphologists
Místo vydání:	Goiania
Stát vydání:	Sborník vydaný v zahraničí
Název konference:	Regional Conference on Geomorphology
Místo konání konference:	Goiania, Brazil
Datum zahájení konference:
Typ akce podle státní příslušnosti účastníků:	Celosvětová akce
Kód UT WoS:
EID:

Klíčová slova anglicky:	Western Carpathians; landslides; landslide activity; 14C dating
Popis v původním jazyce:	Deep seated slope deformations play an essential role at forming the morphology of mountain ridges of flysch Carpathians. They occurred continuously throughout the Quaternary and currently represent the main source of hazards connected with the emergence of shallow landslides. Despite a large number of slope deformations in the Czech Carpathians little is known about these geomorphologic phenomena from the point of their geomorphologic effect. Our research of slope deformations is of a multidisciplinary character and apart from traditional geomorphologic methods it uses geologic, geophysical, sedimentologic and geoinformatic instruments.
Popis v anglickém jazyce:	Deep seated slope deformations play an essential role at forming the morphology of mountain ridges of flysch Carpathians. They occurred continuously throughout the Quaternary and currently represent the main source of hazards connected with the emergence of shallow landslides. Despite a large number of slope deformations in the Czech Carpathians little is known about these geomorphologic phenomena from the point of their geomorphologic effect. Our research of slope deformations is of a multidisciplinary character and apart from traditional geomorphologic methods it uses geologic, geophysical, sedimentologic and geoinformatic instruments.

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