We present a combined geological-geophysical study on the lacustrine sequence of the Fucino Plain (central Italy). New
acquired data on liquefaction features and the recovery of a seismite in the lacustrine sequence are shown. Our preliminary
results suggest the occurrence of three seismic events in the last ca. 45 kyr. Moreover, a first attempt to find out the source deposit
responsible of the widespread liquefaction phenomena has been performed by means of shallow engine boreholes and ERT
profiles
