It is described the rock fall event occurred along the Gran Sasso massif (Central Apennines, Italy) on 22 August, 2006, when a limestone block, with an estimated volume of about 30,000 m(3), fell from the sub-vertical NE wall nearby the Como Grande peak, the highest peak of the Italian Apennines. Despite the small rock volume involved in the landslide, the rock fall deposits covered an area of about 35,000 m(2), a giant and abrasive dust cloud was generated by the atmospheric pressure waves (air blasts) induced by the rockfall impact and determined destructive effects over an area of about 110,000 m(2) at the base of the slope. Moreover the dust cloud covered a distance of about 3 km, thus reaching the village of Casale San Nicola and the A24 motorway that was temporarily closed for security reasons. The seismic noise generated by the rock fall was recorded by the National Institute of Nuclear Physics seismometric devices located in the Gran Sasso underground laboratories (LNGS).
The 22 August, 2006, anomalous rock fall along the Gran Sasso NE wall (Central Apennines, Italy) / BIANCHI FASANI, Gianluca; Esposito, Carlo; SCARASCIA MUGNOZZA, Gabriele; Stedile, Luigi; M., Pecci. - STAMPA. - 1:(2008), pp. 355-360. (Intervento presentato al convegno 10th International Symposium on Landslides and Engineered Slopes tenutosi a Xian; Peoples R China nel JUN 30-JUL 04, 2008) [10.1201/9780203885284-c33].
The 22 August, 2006, anomalous rock fall along the Gran Sasso NE wall (Central Apennines, Italy)
BIANCHI FASANI, Gianluca;ESPOSITO, CARLO;SCARASCIA MUGNOZZA, Gabriele;STEDILE, Luigi;
2008
Abstract
It is described the rock fall event occurred along the Gran Sasso massif (Central Apennines, Italy) on 22 August, 2006, when a limestone block, with an estimated volume of about 30,000 m(3), fell from the sub-vertical NE wall nearby the Como Grande peak, the highest peak of the Italian Apennines. Despite the small rock volume involved in the landslide, the rock fall deposits covered an area of about 35,000 m(2), a giant and abrasive dust cloud was generated by the atmospheric pressure waves (air blasts) induced by the rockfall impact and determined destructive effects over an area of about 110,000 m(2) at the base of the slope. Moreover the dust cloud covered a distance of about 3 km, thus reaching the village of Casale San Nicola and the A24 motorway that was temporarily closed for security reasons. The seismic noise generated by the rock fall was recorded by the National Institute of Nuclear Physics seismometric devices located in the Gran Sasso underground laboratories (LNGS).I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.