Temporal behavior of deep-seated gravitational slope deformations: A review

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61988987%3A17310%2F16%3AA1701ICW" target="_blank" >RIV/61988987:17310/16:A1701ICW - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/67985891:_____/16:00464336

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Temporal behavior of deep-seated gravitational slope deformations: A review

Popis výsledku v původním jazyce

Deep-seated gravitational slope deformations DSGSDs)are slow moving, hillslope-scale mass movements featuring characteristic landforms such as double-crested ridges and upslope-facing scarps that occur in diverse landscapes throughout the world. Absolute age and monitoring data indicate that DSGSD movements are observable over long-term (>102 years) and short-term (&lt;102 years) intervals. Apart from creep, an episodic deformation also plays a crucial role, especially in regions with earthquakes and heavy rainfall. Our review also supports the notion of DSGSDs as precursors of catastrophic rock slope failures, given that many of theworld's largest rock avalanches have occurred in areas with diagnostic DSGSD features, indicating that sudden collapse was preceded by a prolonged stage of slope sagging. Detailed studies on DSGSDs have therefore the potential for better prediction of catastrophic rock slides and rock avalanches.

Název v anglickém jazyce

Temporal behavior of deep-seated gravitational slope deformations: A review

Popis výsledku anglicky

Deep-seated gravitational slope deformations DSGSDs)are slow moving, hillslope-scale mass movements featuring characteristic landforms such as double-crested ridges and upslope-facing scarps that occur in diverse landscapes throughout the world. Absolute age and monitoring data indicate that DSGSD movements are observable over long-term (>102 years) and short-term (&lt;102 years) intervals. Apart from creep, an episodic deformation also plays a crucial role, especially in regions with earthquakes and heavy rainfall. Our review also supports the notion of DSGSDs as precursors of catastrophic rock slope failures, given that many of theworld's largest rock avalanches have occurred in areas with diagnostic DSGSD features, indicating that sudden collapse was preceded by a prolonged stage of slope sagging. Detailed studies on DSGSDs have therefore the potential for better prediction of catastrophic rock slides and rock avalanches.

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/GA13-15123S" target="_blank" >GA13-15123S: Časoprostorová variabilita hlubokých svahových deformací v Tatrách (Západní Karpaty)</a><br>

Návaznosti

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

Rok uplatnění

2016

Kód důvěrnosti údajů

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

Název periodika

Earth-Science Reviews

ISSN

0012-8252

e-ISSN

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Svazek periodika

156

Číslo periodika v rámci svazku

May

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

25

Strana od-do

14-38

Kód UT WoS článku

000375516500002

EID výsledku v databázi Scopus

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