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Typ záznamu * :	článek v odborném periodiku (J)
Domácí pracoviště * :	Přírodovědecká fakulta (31000)
Název * :	Late Holocene evolution of landslides in the frontal part of the Magura Nappe: Hlavatá Ridge, Moravian-Silesian Beskids (Czech Republic)
Citace :	Pánek, T., Smolková, V., Hradecký, J. a Šilhán, K. Late Holocene evolution of landslides in the frontal part of the Magura Nappe: Hlavatá Ridge, Moravian-Silesian Beskids (Czech Republic). Moravian Geographical Reports. 2009, roč. 17, s. 2-11. ISSN 1210-8812.

Podnázev :
Rok * :	2009
Obor * :	Zemský magnetismus, geodesie, geografie
Kód ISSN * :	1210-8812
Oficiální název periodika * :	Moravian Geographical Reports
Stát vydavatele periodika * :	Česká republika
Svazek periodika * :	Neuveden
Číslo periodika v rámci svazku * :	4
Ročník :	17
Počet stran článku * :	10
Strana od * :	2
Strana do * :	11
Kód UT WoS :
EID :
Poddruh recenzovaného článku :

Klíčová slova anglicky * :	landslide; earthflow; retrogressive evolution; landslide-dammed palaeolake; Magura nappe; Moravian-Silesian Beskids; Czech Republic
Popis v původním jazyce * :	Frontal parts of nappes and overthrusts belong to the most exposed environments in the evolution of slope deformations. The frontal part of the Magura Nappe creates a distinct morphotectonical and lithological boundary characterized by occurrence of various types of slope deformations. A representative example of such failures is on the northern slope of the Hlavatá Ridge (Moravskoslezské Beskydy Mts.). Radiocarbon dating of peat bogs and lacustrine deposits of a fossil landslide-dammed lake enabled us to constrain the chronology of a retrogressive landslide. The main phase of the landslide evolution took place ~1.6 ka BP; secondary distinctly retrogressive reactivation of the landslide occurred in 0.8-0.9 ka BP. Our case study demonstrates dynamic Late Holocene geomorphic evolution in the area of the Flysch Carpathians and re-evaluates the chronology of landforms previously considered as of the Pleistocene age.
Popis v anglickém jazyce * :	Frontal parts of nappes and overthrusts belong to the most exposed environments in the evolution of slope deformations. The frontal part of the Magura Nappe creates a distinct morphotectonical and lithological boundary characterized by occurrence of various types of slope deformations. A representative example of such failures is on the northern slope of the Hlavatá Ridge (Moravskoslezské Beskydy Mts.). Radiocarbon dating of peat bogs and lacustrine deposits of a fossil landslide-dammed lake enabled us to constrain the chronology of a retrogressive landslide. The main phase of the landslide evolution took place ~1.6 ka BP; secondary distinctly retrogressive reactivation of the landslide occurred in 0.8-0.9 ka BP. Our case study demonstrates dynamic Late Holocene geomorphic evolution in the area of the Flysch Carpathians and re-evaluates the chronology of landforms previously considered as of the Pleistocene age.

Typ zdroje financování výsledku * :

Projekty CEP/Záměry CEZ

Seznam projektů :

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Ohlas

R01:	RIV/61988987:17310/09:A1000WJ7