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Record type:	stať ve sborníku (D)
Home Department:	Katedra fyzické geografie a geoekologie (31600)
Title:	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.

Subtitle
Publication year:	2006
Obor:	Zemský magnetismus, geodesie, geografie
Number of pages:	1
Page from:	84
Page to:	84
Form of publication:
ISBN code:
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Proceedings title:	Regional Conference on Geomorphology, Vol. I
Proceedings:
Publisher name:	International Association of Geomorphologists
Place of publishing:	Goiania
Country of Publication:	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
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Key words in English:	Western Carpathians; landslides; landslide activity; 14C dating
Annotation in original language:	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.
Annotation in english language:	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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