The largest prehistoric landslide in northwestern Slovakia: Chronological constraints of the Kykula long-runout landslide and related dammed lakes

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61988987%3A17310%2F10%3AA1100YA1" target="_blank" >RIV/61988987:17310/10:A1100YA1 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

The largest prehistoric landslide in northwestern Slovakia: Chronological constraints of the Kykula long-runout landslide and related dammed lakes

Popis výsledku v původním jazyce

This study deals with the chronology of the largest long-runout landslide in the northwesterrn part of theWestern Flysch Carpathians (Kysucké Beskydy Mts, Slovakia). Despite the impossibility of using direct radiocarbon dating method, time constraints for the evolution of the landslide were determined on the basisof the dating of variou sedimentological/geomorphological elements situated on and adjacent to the landslide body. The results show that the landslide evolved between ~10.3 and 9.0 ka 14C BP, i.e. in the wider transitional phase between the Late Glacial (LG) and the Holocene. The main mass movement activity took place at the turn of the Younger Dryas/Preboreal chronozones, whereas retrogressive activity continued up to the Preboreal/Boreal transition. The study confirms that the LG/Holocene transition represented a favourable period for the evolution of large landslides not only in glaciated high mountain areas, but also in medium-high mountains of Central Europe.

Název v anglickém jazyce

The largest prehistoric landslide in northwestern Slovakia: Chronological constraints of the Kykula long-runout landslide and related dammed lakes

Popis výsledku anglicky

This study deals with the chronology of the largest long-runout landslide in the northwesterrn part of theWestern Flysch Carpathians (Kysucké Beskydy Mts, Slovakia). Despite the impossibility of using direct radiocarbon dating method, time constraints for the evolution of the landslide were determined on the basisof the dating of variou sedimentological/geomorphological elements situated on and adjacent to the landslide body. The results show that the landslide evolved between ~10.3 and 9.0 ka 14C BP, i.e. in the wider transitional phase between the Late Glacial (LG) and the Holocene. The main mass movement activity took place at the turn of the Younger Dryas/Preboreal chronozones, whereas retrogressive activity continued up to the Preboreal/Boreal transition. The study confirms that the LG/Holocene transition represented a favourable period for the evolution of large landslides not only in glaciated high mountain areas, but also in medium-high mountains of Central Europe.

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DE - Zemský magnetismus, geodesie, geografie

OECD FORD obor

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Projekt

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2010

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

GEOMORPHOLOGY

ISSN

0169-555X

e-ISSN

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Svazek periodika

120

Číslo periodika v rámci svazku

3-4

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

15

Strana od-do

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Kód UT WoS článku

000281095500012

EID výsledku v databázi Scopus

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