Seismic triggering of landslides, Part A: Field evidence from the Northern Tien Shan

Landslides triggered by strong earthquakes often caused most of the global damage and most of all casualties related to the events, such as shown by the <i>M</i> = 7.7 Peru earthquake in 1970, by the <i>M</i> = 7.6 El Salvador earthquake in 2001 or by the <i>M</i...

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Main Authors: H.-B. Havenith, A. Strom, D. Jongmans, A. Abdrakhmatov, D. Delvaux, P. Tréfois
Format: Article
Language:English
Published: Copernicus Publications 2003-01-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/3/135/2003/nhess-3-135-2003.pdf
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author H.-B. Havenith
A. Strom
D. Jongmans
D. Jongmans
A. Abdrakhmatov
D. Delvaux
P. Tréfois
author_facet H.-B. Havenith
A. Strom
D. Jongmans
D. Jongmans
A. Abdrakhmatov
D. Delvaux
P. Tréfois
author_sort H.-B. Havenith
collection DOAJ
description Landslides triggered by strong earthquakes often caused most of the global damage and most of all casualties related to the events, such as shown by the <i>M</i> = 7.7 Peru earthquake in 1970, by the <i>M</i> = 7.6 El Salvador earthquake in 2001 or by the <i>M</i> = 7.4 Khait (Tajikistan) earthquake in 1949. The obvious impact of a landslide on the population is directly related to its movement. Yet, prediction of future failure potential and hence future risk to population is necessary in order to avoid further catastrophes and involves the analyses of the origin of seismic instability. The seismic landslide potential is mainly determined by the interaction between the regional seismic hazard and local geological conditions. At a local scale, seismic factors interfering with geological conditions can produce site-specific ground motions. The influence of such Site Effects on instability is the principal topic of this paper, which is divided into two parts, A and B. The present Part A is concerned with the correlation of field data with observed instability phenomena. Field data were obtained on mainly three landslide sites in the Northern Tien Shan Mountains in Kyrgyzstan, Central Asia. Geophysical prospecting, earthquake recordings, geological observation, trenching and geotechnical tests were the main investigation tools. The collected information gives an insight in the geological background of the slope failure and allows us to roughly infer failure mechanisms from field evidence. A detailed analysis of the susceptibility of a mechanism to specific geological conditions will be shown in Part B.
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spelling doaj.art-b4e92800e46442d8b25efb1cb8f8e9ea2022-12-22T03:51:16ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812003-01-0131/2135149Seismic triggering of landslides, Part A: Field evidence from the Northern Tien ShanH.-B. HavenithA. StromD. JongmansD. JongmansA. AbdrakhmatovD. DelvauxP. TréfoisLandslides triggered by strong earthquakes often caused most of the global damage and most of all casualties related to the events, such as shown by the <i>M</i> = 7.7 Peru earthquake in 1970, by the <i>M</i> = 7.6 El Salvador earthquake in 2001 or by the <i>M</i> = 7.4 Khait (Tajikistan) earthquake in 1949. The obvious impact of a landslide on the population is directly related to its movement. Yet, prediction of future failure potential and hence future risk to population is necessary in order to avoid further catastrophes and involves the analyses of the origin of seismic instability. The seismic landslide potential is mainly determined by the interaction between the regional seismic hazard and local geological conditions. At a local scale, seismic factors interfering with geological conditions can produce site-specific ground motions. The influence of such Site Effects on instability is the principal topic of this paper, which is divided into two parts, A and B. The present Part A is concerned with the correlation of field data with observed instability phenomena. Field data were obtained on mainly three landslide sites in the Northern Tien Shan Mountains in Kyrgyzstan, Central Asia. Geophysical prospecting, earthquake recordings, geological observation, trenching and geotechnical tests were the main investigation tools. The collected information gives an insight in the geological background of the slope failure and allows us to roughly infer failure mechanisms from field evidence. A detailed analysis of the susceptibility of a mechanism to specific geological conditions will be shown in Part B.http://www.nat-hazards-earth-syst-sci.net/3/135/2003/nhess-3-135-2003.pdf
spellingShingle H.-B. Havenith
A. Strom
D. Jongmans
D. Jongmans
A. Abdrakhmatov
D. Delvaux
P. Tréfois
Seismic triggering of landslides, Part A: Field evidence from the Northern Tien Shan
Natural Hazards and Earth System Sciences
title Seismic triggering of landslides, Part A: Field evidence from the Northern Tien Shan
title_full Seismic triggering of landslides, Part A: Field evidence from the Northern Tien Shan
title_fullStr Seismic triggering of landslides, Part A: Field evidence from the Northern Tien Shan
title_full_unstemmed Seismic triggering of landslides, Part A: Field evidence from the Northern Tien Shan
title_short Seismic triggering of landslides, Part A: Field evidence from the Northern Tien Shan
title_sort seismic triggering of landslides part a field evidence from the northern tien shan
url http://www.nat-hazards-earth-syst-sci.net/3/135/2003/nhess-3-135-2003.pdf
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