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Location:
Magnitude:
7.6
Time:
19 Mar 2009 18:17:40
Depth:
31.0
There are 4 swarms found nearby.
2001
PS20011009.1(88.7km)
9 Oct
2 hours
5 earthquakes
2006
PS20061009.1(93.3km)
8 Oct
10 hours
5 earthquakes
2009
PS20090320.1(73.5km)
19 Mar
1 day 23 hours
10 earthquakes
2014
PS20140313.1(46.4km)
12 Mar
10 hours
6 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

The 2009 Magnitude 7.6 Earthquake South of Tonga

On 19 March 2009 at 18:17 UTC, a magnitude 7.6 earthquake struck 191 km south of ‘Ohonua, Tonga, at a depth of 31 km. This event stands as the sole M7.6 earthquake recorded in the region since 1 January 2000, highlighting the persistent seismic activity along the Tonga subduction zone. Tonga occupies a tectonically active segment of the Pacific Ring of Fire. The island arc formed where the Pacific plate subducts westward beneath the Australian plate at rates exceeding 15 cm per year along the Tonga Trench. This convergence produces intermediate-depth earthquakes and fuels arc volcanism. The 31 km focal depth of the 2009 event places it within the upper portion of the subducting slab, consistent with typical intraslab seismicity in this setting. Geological records document repeated large earthquakes and tsunamis throughout Tongan history. Oral traditions and early European accounts describe significant shaking and coastal inundation in the 19th and early 20th centuries. Modern instrumental monitoring since the mid-20th century confirms that the Tonga-Kermadec system regularly generates events above magnitude 7.0, often accompanied by aftershock sequences lasting weeks to months. The 2009 earthquake produced no reported casualties or major structural damage on nearby islands, owing to its offshore location and moderate depth. Regional seismic networks recorded numerous aftershocks, reinforcing the pattern of clustered activity along the plate interface and within the downgoing slab. Updated geophysical surveys continue to refine models of slab geometry and stress transfer in this rapidly converging margin. Volcanic features such as the active submarine volcanoes of the Tofua arc lie immediately west of the trench and remain linked to the same subduction dynamics. Ongoing GPS measurements show continued plate motion and elastic strain accumulation, indicating that future large earthquakes remain possible. References USGS Earthquake Hazards Program catalog entry for the 19 March 2009 event. Global CMT Project moment tensor solution for the Tonga region. Pacific Islands Applied Geoscience Commission regional tectonic summaries.