Location:
Period:
26 Oct 2002 23:22:31 - 28 Oct 2002 16:27:05 (1d 17h 4m)
Volcanoes in 100km radius:
Etna(10km), Vulcano(72km), Lipari(82km), Panarea(97km)
Earthquakes:
54
3 swarms found nearby.
2011
S20110505.1(15.0km)
4 May
2 days 22 hours
92 earthquakes
2018
S20181224.1(22.1km)
23 Dec
5 days 2 hours
91 earthquakes
2021
24 Jan
1 day 15 hours
35 earthquakes
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Seismic Swarm VS20021027.1: Analysis of Earthquake Activity in Sicily, Italy

A notable seismic swarm designated VS20021027.1 occurred in Sicily, Italy, between 23:22 UTC on 26 October 2002 and 16:27 UTC on 28 October 2002. Over 41 hours and 4 minutes, the sequence produced 54 earthquakes. This event cluster highlights the persistent tectonic stresses in the region.

Sicily lies at the convergent boundary between the African and Eurasian plates, where ongoing collision drives both seismic and volcanic activity. The island forms part of the central Mediterranean seismic belt, influenced by the subduction of the Ionian slab beneath the Calabrian Arc. Historical records document frequent moderate earthquakes, with notable events including the 1693 Sicily earthquake and the 1908 Messina-Reggio Calabria quake. Volcanic systems such as Mount Etna further contribute to localized stress fields through magma movement and flank instability.

The swarm initiated with a magnitude 2.3 event at 2 km depth. Activity intensified rapidly on 27 October, featuring multiple events above magnitude 3.0. The strongest shocks reached magnitudes 4.4 at 10 km depth and 4.3 at similar depths, occurring within the first few hours of peak activity. Depths ranged predominantly between 5 km and 20 km, consistent with crustal faulting in the area. Later events on 28 October showed reduced frequency and lower magnitudes, with the sequence concluding at magnitude 2.5.

Analysis of the temporal distribution reveals a classic swarm pattern: an abrupt onset followed by sustained high-rate occurrence without a single dominant mainshock. Most events clustered between 00:00 and 08:00 UTC on 27 October, after which rates declined steadily. Shallow focal depths suggest involvement of upper-crustal structures, possibly linked to regional strike-slip or normal fault systems accommodating plate convergence.

Such swarms provide valuable data for understanding stress transfer and fault interactions in tectonically active zones. Continued monitoring by networks such as those operated by Italy’s National Institute of Geophysics and Volcanology supports improved hazard assessment for populated areas of eastern Sicily.

References

  • Istituto Nazionale di Geofisica e Vulcanologia (INGV) seismic bulletins.
  • USGS Earthquake Catalog for Mediterranean region.
  • SeismoSight internal swarm classification records.