GEER findings – ground motions

We have not looked at individual records yet, but we have the motions for the mainshock, largest aftershock, and triggered event from a DPC website. The mainshock data have been forwarded to PEER and CESMD for processing. We have 56 mainshock recordings, including 4 in the immediate vicinity of L’Aquila. Three of those are west of the city in a sparsely developed valley (however, this is near the hospital). The fourth is near the historic center of L’Aquila. The center sits on a Pleistocene terrace. There is a swale east of the center, and the instrument is above a pedestrian tunnel portal on the edge slope of the Pleistocene terrace (nearby structure is a car park). We were not able to walk up to the instrument because access to the car park is  denied.  This instrument recorded about 0.35 g. The instruments W of L’Aquila recorded 0.5-0.7 g.