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We relocated seismicity that occurred from 2000 to 2005 inside a sector ofMt. Etna, comprising the town of Zafferana Etnea, using the double-differencetechnique. This approach revealed some spatial clusters of events atdepths of 3.0 km to 5.5 km b.s.l., which suggested NE-SW-oriented andNNW-SSE-oriented active structures located west and north-west with respectto Zafferana Etnea. We also calculated 64 fault plane solutions, andazimuth and dip distributions of maximum compression P axes. The datainclude eight events with magnitudes between 3.1 and 3.7 that caused damageto Zafferana Etnea. This approach has allowed the definition of thegeometry of structures that show no surface evidence, but are potentiallyhazardous for this territory. These faults might be linked to the regionaltectonics, although they were activated by stress changes related to a generalpressurizing of the Mt. Etna magma system between 2000 and 2005

annals of geophysics

Buried active faults in the Zafferana Etnea territory (south-eastern flank of Mt. Etna): geometry and kinematics by earthquake relocation and focal mechanisms