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Location:
Period:
8 Oct 2006 13:50:24 - 9 Oct 2006 00:09:59 (10 hours 19 minutes)
Volcanoes in 100km radius:
None
Earthquakes:
5
M 7.0+:
10 swarms found nearby.
2001
PS20011009.1(31.1km)
9 Oct
2 hours
5 earthquakes
2004
PS20040410.1(126.4km)
10 Apr
17 hours
5 earthquakes
2009
PS20090320.1(22.3km)
19 Mar
1 day 23 hours
10 earthquakes
2010
PS20100222.1(55.3km)
22 Feb
23 hours
6 earthquakes
2011
PS20110630.1(49.6km)
30 Jun
9 hours
5 earthquakes
2014
PS20140313.1(47.0km)
12 Mar
10 hours
6 earthquakes
2017
PS20171016.1(48.4km)
16 Oct
17 hours
7 earthquakes
2020
PS20200222.1(171.3km)
22 Feb
55 minutes
5 earthquakes
2023
PS20230616.1(59.3km)
16 Jun
2 days 9 hours
20 earthquakes
PS20230625.1(81.8km)
25 Jun
7 hours
5 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm PS20061009.1: Analysis of October 2006 Events Near Tonga

The seismic swarm designated PS20061009.1 occurred in the Tonga region of the southwest Pacific Ocean. It began at 13:50 on 8 October 2006 and concluded at 00:09 on 9 October 2006, spanning 10 hours and 19 minutes. The epicenter was located 236 km south-southwest of ‘Ohonua, Tonga. During this interval, five earthquakes were recorded, all at a focal depth of 10 km.

The sequence commenced with a magnitude 5.8 event at 13:50:24 on 8 October, followed by a 5.3 event at 14:10:16. Subsequent shocks included magnitudes of 5.2 at 14:46:54 and 18:54:55 on the same day. The swarm ended with a magnitude 4.7 earthquake at 00:09:59 on 9 October. These events clustered closely in both time and space, characteristic of swarm behavior where no single mainshock dominates.

Tonga lies along the Tonga-Kermadec subduction zone, where the Pacific Plate subducts westward beneath the Indo-Australian Plate at rates exceeding 15 cm per year. This tectonic setting produces frequent shallow seismicity, volcanic arcs, and occasional deeper events extending to 700 km. The 10 km depths of the swarm events align with typical upper-plate or interface activity in this convergent margin. Historical records indicate persistent seismic productivity, with the region contributing significantly to global earthquake catalogs.

Since 1 January 2000, only two swarms have been documented in the immediate area prior to 2006, occurring in 2001 and 2004. This low frequency underscores the episodic nature of swarm activity amid more continuous background seismicity. A notable larger event, magnitude 7.6, struck on 19 March 2009 approximately 191 km south of ‘Ohonua and 93 km from the swarm center, highlighting the potential for stronger earthquakes in the broader zone.

Such swarms provide insight into stress transfer along the subduction interface and may precede or accompany volcanic unrest, though no direct linkage was established in this case. Monitoring remains essential given Tonga’s position on the Pacific Ring of Fire.

References

SeismoSight internal swarm classification records.
USGS Earthquake Catalog (historical Tonga region data).
Global CMT Project (tectonic context for Tonga-Kermadec subduction).