2012
DOI: 10.5194/nhess-12-3631-2012
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The role of near-field interaction between seismic waves and slope on the triggering of a rockslide at Lorca (SE Spain)

Abstract: Abstract. A ∼1000 m 3 rockslide occurred close to Lorca (SE Spain) during the main shock (M w = 5.1) of the May 2011 seismic sequence. The location of the rockslide, within 10 km of the earthquake epicenter and along the southern slope of a valley in which similar geological conditions occur on both slopes of the valley, suggests a significant near-field effect due to local seismic response. This could be related to the specific interaction between the topography and the obliquely propagating seismic waves.A d… Show more

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Cited by 24 publications
(6 citation statements)
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“…Several studies have been conducted worldwide during the last few decades that report on ground failures triggered by earthquakes (Bommer and Rodriguez, 2002;Sepulveda et al, 2005;Porfido et al, 2007;Tosatti et al, 2008;Gorum et al, 2011;Tang et al, 2011;Alfaro et al, 2012; among many others) and that forecast, using predictive models, the distribution scenarios of earthquake-induced ground effects (Sassa et al, 1996;Jibson et al, 2000;Prestininzi and Romeo, 2000;Romeo, 2000;Jibson, 2007;Hsieh and Lee, 2011;among others). These studies provide inventory maps of the effects that have occurred or susceptibility maps of expected ground failures.…”
Section: Introductionmentioning
confidence: 99%
“…Several studies have been conducted worldwide during the last few decades that report on ground failures triggered by earthquakes (Bommer and Rodriguez, 2002;Sepulveda et al, 2005;Porfido et al, 2007;Tosatti et al, 2008;Gorum et al, 2011;Tang et al, 2011;Alfaro et al, 2012; among many others) and that forecast, using predictive models, the distribution scenarios of earthquake-induced ground effects (Sassa et al, 1996;Jibson et al, 2000;Prestininzi and Romeo, 2000;Romeo, 2000;Jibson, 2007;Hsieh and Lee, 2011;among others). These studies provide inventory maps of the effects that have occurred or susceptibility maps of expected ground failures.…”
Section: Introductionmentioning
confidence: 99%
“…These can involve localities distant up to tens or hundreds of kilometres from the earthquake epicentre (Keefer, 1984;Rodrıguez et al, 1999;Delgado et al, 2011;Jibson and Harp, 2012). During the last decades, they have been confirmed by several authors reporting on ground failures triggered by earthquakes (Bommer and Rodriguez, 2002;Sepúlveda et al, 2005;Porfido et al, 2007;Tosatti et al, 2008;Gorum et al, 2011;Tang et al, 2011;Alfaro et al, 2012;Martino et al, 2020a, among others). To preemptively reduce the risk associated with these processes, predictive models have been proposed to estimate the distribution of earthquake-triggered ground effects scenarios (Sassa, 1996;Jibson et al, 2000;Prestininzi and Romeo, 2000;Romeo, 2000;Jibson, 2007;Hsieh and Lee, 2011, among others) representative of a uniform hazard distribution or seismic shaking scenarios.…”
Section: Introductionmentioning
confidence: 76%
“…where b is the length of potential slip surface lock-up segment, m; and ρ is the curvature radius at the end of the failure surface, m. Under the cyclic shear loadings, seismic waves result in the fragmentation of the rock-soil body and reduce the rock-soil mass integrity and strength parameters (Alfaro et al, 2012). Moreover, in the process of progressive slope damage, the failure surface still has residual strength, which can provide part of the anti-slide force.…”
Section: Mechanism Of Dynamic Slope Failurementioning
confidence: 99%