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Statements

Subject Item
n2:RIV%2F67985891%3A_____%2F14%3A00438567%21RIV15-AV0-67985891
rdf:type
skos:Concept n13:Vysledek
dcterms:description
The gently concave piedmont of the marginal slope of the Flysch Carpathians in the Czech Republic has long been considered to comprise a system of pediments or coalescent alluvial fans. However, within one of the typical sections of this piedmont, large successive landslides with long travel distances of similar to 2.5km have been identified through geophysical measurements and the investigation of an extensive artificial exposure. Accelerator mass spectrometry (AMS) radiocarbon dating and pollen analysis demonstrate that the uppermost generations of landslide deposits have originated since similar to 56ka BP during the warmer and more humid interpleniglacial conditions of Marine Isotope Stage 3 (MIS 3). The geomorphological evidence for landsliding during MIS 3 has almost completely disappeared from this region due to intensive periglacial processes operating during the Last Glacial Maximum and subsequent fluvial and anthropogenic processes operating during the Holocene. The considerable antiquity of the studied terrestrial landslide bodies is unique within the context of Europe. This study shows the value of re-examining landscape development using new techniques and fresh exposures. The gently concave piedmont of the marginal slope of the Flysch Carpathians in the Czech Republic has long been considered to comprise a system of pediments or coalescent alluvial fans. However, within one of the typical sections of this piedmont, large successive landslides with long travel distances of similar to 2.5km have been identified through geophysical measurements and the investigation of an extensive artificial exposure. Accelerator mass spectrometry (AMS) radiocarbon dating and pollen analysis demonstrate that the uppermost generations of landslide deposits have originated since similar to 56ka BP during the warmer and more humid interpleniglacial conditions of Marine Isotope Stage 3 (MIS 3). The geomorphological evidence for landsliding during MIS 3 has almost completely disappeared from this region due to intensive periglacial processes operating during the Last Glacial Maximum and subsequent fluvial and anthropogenic processes operating during the Holocene. The considerable antiquity of the studied terrestrial landslide bodies is unique within the context of Europe. This study shows the value of re-examining landscape development using new techniques and fresh exposures.
dcterms:title
Large Late Pleistocene landslides from the marginal slope of the Flysch Carpathians Large Late Pleistocene landslides from the marginal slope of the Flysch Carpathians
skos:prefLabel
Large Late Pleistocene landslides from the marginal slope of the Flysch Carpathians Large Late Pleistocene landslides from the marginal slope of the Flysch Carpathians
skos:notation
RIV/67985891:_____/14:00438567!RIV15-AV0-67985891
n4:aktivita
n18:S n18:P n18:I
n4:aktivity
I, P(LM2010008), S
n4:cisloPeriodika
6
n4:dodaniDat
n8:2015
n4:domaciTvurceVysledku
n9:8228205 n9:6291031 n9:7489706
n4:druhVysledku
n16:J
n4:duvernostUdaju
n12:S
n4:entitaPredkladatele
n15:predkladatel
n4:idSjednocenehoVysledku
25663
n4:idVysledku
RIV/67985891:_____/14:00438567
n4:jazykVysledku
n5:eng
n4:klicovaSlova
fossil landslide; radiocarbon dating; electrical resistivity tomography; pollen analysis; Late Pleistocene; Flysch Carpathians; Marine Isotope Stage 3
n4:klicoveSlovo
n6:fossil%20landslide n6:Late%20Pleistocene n6:Flysch%20Carpathians n6:pollen%20analysis n6:electrical%20resistivity%20tomography n6:Marine%20Isotope%20Stage%203 n6:radiocarbon%20dating
n4:kodStatuVydavatele
DE - Spolková republika Německo
n4:kontrolniKodProRIV
[1A1E8B8D4DF6]
n4:nazevZdroje
Landslides
n4:obor
n10:DE
n4:pocetDomacichTvurcuVysledku
3
n4:pocetTvurcuVysledku
8
n4:projekt
n17:LM2010008
n4:rokUplatneniVysledku
n8:2014
n4:svazekPeriodika
11
n4:tvurceVysledku
Hradecký, J. Bubík, M. Hartvich, Filip Jankovská, Vlasta Tábořík, Petr Klimeš, Jan Pánek, T. Smolková, V.
n4:wos
000345324100004
s:issn
1612-510X
s:numberOfPages
12
n14:doi
10.1007/s10346-013-0463-8