Site effects in Saletta damaged area of Amatrice municipality (Central Italy) after the 24th August 2016 earthquake

Gaudiosi I.; Vignaroli G.; Mancini M.; Moscatelli M.; Simionato M.; Sirianni P.; Razzano R.; Peronace E.; Piscitelli S.; Madiai C.; Cavinato G. P.; Cosentino G.; Di Salvo C.; Giallini S.; Polpetta F.; Putignano M. L.; Scionti V.; Stigliano F.; Bardotti R.; Facciorusso J.; Gargini E.; Bellanova J.; Calamita G.; Perrone A.; Gallipoli M. R.; Gueguen E.; Stabile T. A.; Romano G.; AMOROSO S.; Bordoni P.; Bucci A.; Cara F.; Carannante S.; Cogliano R.; Cultrera G.; D’Alema E.; D’Amico M.; Di Giulio G.; Di Naccio D.; Famiani D.; Felicetta C.; Fodarella A.; Franceschina G.; Lanzano G.; Lovati S.; Luzi L.; Mascandola C.; Massa M.; Mercuri A.; Milana G.; Pacor F.; Picaredda D.; Pischiutta M.; Pucillo S.; Puglia R.; Riccio G.; Vassallo M.; Boniolo G.; Caielli G.; Corsi A.; de Franco R.; Tento A.; Boni M. P.; Compagnoni M.; Munda S.; Pergalani F.; Cercato M.; Bucci F.; Cardinali M.; Fiorucci F.; Santangelo M.

This work presents the results from numerical analyses in the damaged area of Saletta hamlet (Amatrice municipality), aiming at discussing factors leading to the observed damages after the 24th August 2016 Mw 6.0 earthquake and the following aftershocks. The area of Saletta was in fact highly ravaged by the first earthquake and during the whole seismic sequence. Geological-technical detailed field investigations were combined with an Electrical Resistivity Tomography and several noise measurements for better evaluating the main geologicalmorphological variability over the study area. Following insights from the reconstructed geological setting, a continuous coring borehole was drilled and a down-hole test performed together with a passive 2D small array and an active 1D MASW measurement. All these data were used to obtain the subsoil model for the numerical analyses that were carried out using both 1D and 2D approaches, including linear and equivalent linear ones, aiming at evaluating site effects.