Recurrent landslides predisposed by fault-induced weathering of flysch in the Western Carpathians

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61988987%3A17310%2F10%3AA1100Z1L" target="_blank" >RIV/61988987:17310/10:A1100Z1L - isvavai.cz</a>

Výsledek na webu

—

DOI - Digital Object Identifier

—

Jazyk výsledku

angličtina

Název v původním jazyce

Recurrent landslides predisposed by fault-induced weathering of flysch in the Western Carpathians

Popis výsledku v původním jazyce

The interrelationship between slope deformation and fault-induced weathering as a predisposing factor for the development of sliding is analysed through several case studies from the Western Carpathians in the Czech Republic. The study area comprises flysch nappes with alternating sandstone and shale of different permeability. These lithological structures are affected by systems of faults. Recurring slope instability is found associated with zones of deep weathering in tectonically weakened areas. Climatic variability of landslide activity can be identified during the Holocene by means of radiocarbon dating and pollen analysis. Areas affected by recurring landsliding suggest gradual and cyclic landslide frequency.

Název v anglickém jazyce

Recurrent landslides predisposed by fault-induced weathering of flysch in the Western Carpathians

Popis výsledku anglicky

The interrelationship between slope deformation and fault-induced weathering as a predisposing factor for the development of sliding is analysed through several case studies from the Western Carpathians in the Czech Republic. The study area comprises flysch nappes with alternating sandstone and shale of different permeability. These lithological structures are affected by systems of faults. Recurring slope instability is found associated with zones of deep weathering in tectonically weakened areas. Climatic variability of landslide activity can be identified during the Holocene by means of radiocarbon dating and pollen analysis. Areas affected by recurring landsliding suggest gradual and cyclic landslide frequency.

Druh

C - Kapitola v odborné knize

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

—

Projekt

<a href="/cs/project/GAP209%2F10%2F0309" target="_blank" >GAP209/10/0309: Vliv historických klimatických a hydrometeorologických extrémů na svahové a fluviální procesy v oblasti Západních Beskyd a jejich předpolí</a><br>

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 knihy nebo sborníku

Weathering as a Predisposing Factor to Slope Movements

ISBN

978-1-86239-297-7

Počet stran výsledku

17

Strana od-do

—

Počet stran knihy

239

Název nakladatele

Geological Society, London

Místo vydání

London

Kód UT WoS kapitoly

—