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The Timpe Fault System is the source of very\udshallow but destructive earthquakes that affect several towns and villages on\udthe eastern flank of Mt. Etna (Italy). In 1984, several seismic events, and\udspecifically on 19 and 25 October, caused one fatality, 12 injuries and\udproduced serious damage in the Zafferana and Acireale territories. This\udseismicity was mainly related to the activity of the Fiandaca Fault, one of\udthe structures belonging to the Timpe Fault System.\ud  \udWe inverted ground deformation data collected by a geodimeter trilateration\udnetwork set up in 1977 at a low altitude along the eastern side of the\udvolcano in order to define the Timpe Fault System faulting mechanisms linked\udto the seismicity in 1984.\ud  \udWe have found that in the period May 1980–October 1984, the Fiandaca Fault\udwas affected by a strike-slip and normal dip-slip of about 20.4 and 12.7 cm\udrespectively. This result is kinematically consistent with field\udobservations of the coseismic ground ruptures along the fault but it is\udnotably large compared to displacements estimated by seismicity, then\udsuggesting that most of the slip over the fault plane was aseismic.\ud  \udThe results once again confirm how seismicity and its relation with ground ruptures and creep displacement represent a very high hazard to the several\udtowns and villages situated along the Timpe Fault System

Modeling ground deformation associated with the destructive earthquakes occurring on Mt. Etna's southeastern flank in 1984