2010
DOI: 10.1016/j.enggeo.2010.03.006
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Seismically-induced landslide susceptibility evaluation: Application of a new procedure to the island of Ischia, Campania Region, Southern Italy

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Cited by 38 publications
(28 citation statements)
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“…Rapolla et al (2010Rapolla et al ( , 2012 proposed a quick procedure to assess the seismic slope stability at different scales/levels that accounts for (A) the seismicrelevant property of the rocks/soils that crop out -expressed as transversal seismic velocity (Vs), (B) the incline angle of slopes -obtained from high-resolution digital elevation models of the topography of the investigated areas, (C) the seismic intensity that most likely will affect the study area -expressed in terms of European Macroseismic Scale (EMS-98), which is based on the the Mercalli-Cancani-Sieberg (MCS) and Medvedev-Sponheuer-Karnik (MSK-64) scales. The seismically-induced landslide susceptibility level of an area can be obtained from the average of factors A and B, considered as predisposing factor, multiplied by the triggering factor C. Referring to the above cited literature for details about the procedure, we would like to note here that a crucial point of the procedure is a correct evaluation of the A parameter, the lithology index.…”
Section: Evaluating the Geo-lithological Properties For Seismic-inducmentioning
confidence: 99%
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“…Rapolla et al (2010Rapolla et al ( , 2012 proposed a quick procedure to assess the seismic slope stability at different scales/levels that accounts for (A) the seismicrelevant property of the rocks/soils that crop out -expressed as transversal seismic velocity (Vs), (B) the incline angle of slopes -obtained from high-resolution digital elevation models of the topography of the investigated areas, (C) the seismic intensity that most likely will affect the study area -expressed in terms of European Macroseismic Scale (EMS-98), which is based on the the Mercalli-Cancani-Sieberg (MCS) and Medvedev-Sponheuer-Karnik (MSK-64) scales. The seismically-induced landslide susceptibility level of an area can be obtained from the average of factors A and B, considered as predisposing factor, multiplied by the triggering factor C. Referring to the above cited literature for details about the procedure, we would like to note here that a crucial point of the procedure is a correct evaluation of the A parameter, the lithology index.…”
Section: Evaluating the Geo-lithological Properties For Seismic-inducmentioning
confidence: 99%
“…7a Rapolla et al (2010Rapolla et al ( , 2012 (Fig. 7a), landslides occur mainly in the areas characterized by flysch lithologies, represented by the 2nd, the 3rd and the 4th litho-seismic units in Table 4.…”
Section: Nat Hazards Earthmentioning
confidence: 99%
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