Teleseismic and strong motion data are used to derive the source parameters of the September 9, 1998 Castelluccio earthquake (M5.6). Teleseismic body-wave modeling indicates normal faulting (Plane 1: strike = 328°, dip = 50°, rake = −75°; Plane 2: strike = 126°, dip = 42°,...

The increasing of the strong motion records not only in Greece but everywhere in the world and the need for the data and the information to be dispersed forced the Geodynamic Institute of the National Observatory of Athens to develop a friendly-to-user database, which includes all the available...