Tree-ring analysis in the reconstruction of slope instabilities associated with earthquakes and precipitation (the Crimean Mountains, Ukraine)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61988987%3A17310%2F12%3AA130152K" target="_blank" >RIV/61988987:17310/12:A130152K - 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

Tree-ring analysis in the reconstruction of slope instabilities associated with earthquakes and precipitation (the Crimean Mountains, Ukraine)

Popis výsledku v původním jazyce

The Crimean Mountains in Ukraine constitute a seismically active region that is abundant in various types of mass movement. One of these very active slopes is the area of the ancient Taraktash rockslide, characterised by active block-type movements (lateral spreading, toppling, and incipient sliding), rockfalls, ongoing sliding activities and debris flows. The aims of this study were (i) to employ tree-ring analysis to reconstruct a record of slope instabilities (mainly block-type movements, rockfalls,landslides and debris flows) within the Taraktash slope deformation over a period of more than two centuries and (ii) to establish the degree of correlation between periods of enhanced slope activity and both historical earthquakes and climatic data. Thetree-ring record reveals periods of increased activity of block-type movements, rockfalls and landslides during the major earthquakes in 1790, 1875, 1927 and 1986.

Název v anglickém jazyce

Tree-ring analysis in the reconstruction of slope instabilities associated with earthquakes and precipitation (the Crimean Mountains, Ukraine)

Popis výsledku anglicky

The Crimean Mountains in Ukraine constitute a seismically active region that is abundant in various types of mass movement. One of these very active slopes is the area of the ancient Taraktash rockslide, characterised by active block-type movements (lateral spreading, toppling, and incipient sliding), rockfalls, ongoing sliding activities and debris flows. The aims of this study were (i) to employ tree-ring analysis to reconstruct a record of slope instabilities (mainly block-type movements, rockfalls,landslides and debris flows) within the Taraktash slope deformation over a period of more than two centuries and (ii) to establish the degree of correlation between periods of enhanced slope activity and both historical earthquakes and climatic data. Thetree-ring record reveals periods of increased activity of block-type movements, rockfalls and landslides during the major earthquakes in 1790, 1875, 1927 and 1986.

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

<a href="/cs/project/GAP209%2F12%2F0317" target="_blank" >GAP209/12/0317: Pozdně kvartérní vývoj komplexních gravitačních svahových deformací jižních svahů Krymských hor (Ukrajina)</a><br>

Návaznosti

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

Rok uplatnění

2012

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

173-174

Číslo periodika v rámci svazku

listopad

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

11

Strana od-do

174-184

Kód UT WoS článku

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EID výsledku v databázi Scopus

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