DashboardNewsSwarmsM 7.0+

VolcanoesSupervolcanoesRegionsGlobal

Favorites

BlogAbout

Privacy PolicyDisclaimer
Follow
Note:This page contains AI-generated content for informational and entertainment purposes only. It may contain inaccuracies. Raw event data is from USGS and EMSC. All statistics, lists, and derived information are generated by this site. Full disclaimerFound an error?
Location:
Period:
6 Dec 2009 18:11:35 - 9 Dec 2009 07:57:06 (2 days 13 hours 45 minutes)
Volcanoes in 100km radius:
None
Earthquakes:
59
No swarms nearby.
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm Activity in the Ionian Sea, December 2009

A seismic swarm designated S20091207.1 occurred in the Ionian Sea, registering 59 earthquakes between 18:11 on 6 December 2009 and 07:57 on 9 December 2009. The sequence lasted 61 hours and 45 minutes, with events distributed across a range of magnitudes and focal depths.

Magnitudes in the swarm primarily fell between 2.2 and 4.7. The largest event reached magnitude 4.7 at 15:06 on 7 December at a depth of 10 km. Other notable shocks included magnitudes 4.2 and 4.1 on 8 December. Depths ranged from surface levels to 46 km, with the majority occurring at shallow crustal levels between 2 km and 20 km. Activity showed clustering in the first 24 hours, followed by a gradual decline through 8 and 9 December.

The Ionian Sea forms part of the tectonically active boundary between the African and Eurasian plates. Convergence occurs along the Hellenic subduction zone, where the African plate descends beneath the Aegean microplate at rates of approximately 4–5 cm per year. This setting generates frequent moderate earthquakes and occasional larger events through both subduction-related thrust faulting and crustal extension in the overriding plate.

Historical records document repeated strong shaking in the region. The 365 AD Crete earthquake, estimated above magnitude 8, produced a major tsunami affecting the eastern Mediterranean. In the modern era, the 1953 Kefalonia earthquake sequence reached magnitudes up to 7.2 and caused extensive damage across the Ionian Islands. More recent activity includes the 2018 Zakynthos event of magnitude 6.8 and the 2020 magnitude 7.0 earthquake south of Crete, both linked to the same subduction system.

Seismic swarms such as the 2009 sequence are common in the Ionian domain and typically reflect fluid migration or stress redistribution along pre-existing faults rather than mainshock-aftershock patterns. The shallow depths recorded during this swarm align with the brittle upper crust where most regional seismicity nucleates.

References
European-Mediterranean Seismological Centre (EMSC) earthquake catalogue.
United States Geological Survey (USGS) earthquake data archive.
Papazachos, B.C., et al. (2000). Seismicity and tectonics of the Aegean region. Tectonophysics.
Ganas, A., et al. (2021). Recent seismicity of the Hellenic subduction zone. Journal of Geodynamics.