2014
DOI: 10.1007/s11069-014-1163-y
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Seismic-event-based methodology to obtain earthquake-induced translational landslide regional hazard maps

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Cited by 18 publications
(7 citation statements)
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“…When the accelerated velocity of an earthquake surpasses the critical acceleration of an unstable slope under the conditions of an earthquake, the slope may slip along the failure plane, and permanent displacement will amass in the downward orientation [54]. The critical acceleration can be obtained from Equation (7) [55]:ac=(Fs1)gsinα, where α is the gradient of the slope; g is the gravitational acceleration; and Fs is the static safety factor, which can be represented by Equation (8) [56,57]:FS=Cγtsinα+tanφtanαmγwtanφγtanα, where C’ is the efficient cohesion (MPa); φ’ is the internal friction angle (°); γ is weight of rock-soil body (N/m 3 ); γ W is the weight of water (N/m 3 ); t is the sliding plane thickness (m); and m is the thickness ratio of the failure plane under water.…”
Section: Methodsmentioning
confidence: 99%
“…When the accelerated velocity of an earthquake surpasses the critical acceleration of an unstable slope under the conditions of an earthquake, the slope may slip along the failure plane, and permanent displacement will amass in the downward orientation [54]. The critical acceleration can be obtained from Equation (7) [55]:ac=(Fs1)gsinα, where α is the gradient of the slope; g is the gravitational acceleration; and Fs is the static safety factor, which can be represented by Equation (8) [56,57]:FS=Cγtsinα+tanφtanαmγwtanφγtanα, where C’ is the efficient cohesion (MPa); φ’ is the internal friction angle (°); γ is weight of rock-soil body (N/m 3 ); γ W is the weight of water (N/m 3 ); t is the sliding plane thickness (m); and m is the thickness ratio of the failure plane under water.…”
Section: Methodsmentioning
confidence: 99%
“…Therefore, with the results obtained, by combining all the factors mentioned above in equation 1, the value of the indicator of the threat of landslide HI can be classified and evaluated based on the values in Table 7 [31], [36]. In effect, the susceptibility index for the basin in question is calculated by adding the two maps [20], [24], [37], as shown in equation 3.…”
Section: ) Determination Of Landslide Susceptible Areasmentioning
confidence: 99%
“…For example, the Province of Orellana registered a total of 151 spills until 2011, from which 50.10% have occurred in the Francisco de Orellana Canton (El Coca), 49.79% in the Joya de Los Sacha canton, and 0.21% in the Aguarico canton. These events are from natural or social origin have caused an imbalance in the environment and the waters of the Coca River and its effluents, putting the population, assets and resources at risk [12], [13], [20]. In this context, it is important to understand the capacities and vulnerabilities of the abiotic, biotic and social components to reduce the environmental risks of oil activities [16].…”
Section: Introductionmentioning
confidence: 99%
“…More details about this methodology are presented in Jaimes et al [2013] and Niño et al [2014]. • Hazard assessment for tsunami induced by earthquake.…”
Section: Intensity Measures and Exceedance Rate Functions For Multi-hmentioning
confidence: 99%