The results of a multidisciplinary research on historical landslides reactivated by earthquakes in the NW Apennines (Italy) are discussed. Investigations have led to the collection of 12 landslides reactivated by seismic shocks ranging from 3.3 to 6.5 magnitude. The rock-types involved are weak rocks, lithologically and/or structurally complex (flysch, clay shale and debris). In the study cases, earthquakes are considered as a triggering cause of reactivation of landslides controlled by rainfall.
Historical Landslides Reactivated by Earthquake in the NW Apennines (northern Italy) / Castaldini, Doriano; D'Amato Avanzi, G.; Mandrone, G.; Panizza, Mario; Pellegrini, Maurizio; Puccinelli, A.; Tellini, C.; Tosatti, Giovanni; Barbieri, Massimo. - STAMPA. - 22 (4):(2001), pp. C - 35-C - 35. (Intervento presentato al convegno Japanese Geomorphological Union tenutosi a Tokyo nel 23-28 agosto 2001).
Historical Landslides Reactivated by Earthquake in the NW Apennines (northern Italy)
CASTALDINI, Doriano;PANIZZA, Mario;PELLEGRINI, Maurizio;TOSATTI, Giovanni;BARBIERI, Massimo
2001
Abstract
The results of a multidisciplinary research on historical landslides reactivated by earthquakes in the NW Apennines (Italy) are discussed. Investigations have led to the collection of 12 landslides reactivated by seismic shocks ranging from 3.3 to 6.5 magnitude. The rock-types involved are weak rocks, lithologically and/or structurally complex (flysch, clay shale and debris). In the study cases, earthquakes are considered as a triggering cause of reactivation of landslides controlled by rainfall.
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