Location:
Period:
3 Apr 2007 20:26:09 - 4 Apr 2007 16:38:42 (20h 12m)
Volcanoes in 100km radius:
None
Earthquakes:
6
M 7.0+:
18 swarms found nearby.
2003
PS20031225.1(199.0km)
25 Dec
3 days 15 hours
27 earthquakes
2007
PS20070927.1(89.5km)
27 Sep
20 hours
26 earthquakes
2008
PS20080409.1(32.8km)
8 Apr
2 days 13 hours
17 earthquakes
PS20080411.2(33.2km)
11 Apr
2 hours
5 earthquakes
2010
PS20101225.1(144.0km)
25 Dec
3 days 20 hours
45 earthquakes
2011
PS20110109.1(154.7km)
9 Jan
9 hours
9 earthquakes
PS20110113.1(41.4km)
13 Jan
1 day 9 hours
15 earthquakes
PS20110429.1(184.6km)
29 Apr
5 hours
5 earthquakes
PS20110510.1(53.9km)
10 May
1 day 1 hours
23 earthquakes
2016
PS20160619.1(43.5km)
18 Jun
1 day 7 hours
6 earthquakes
2017
PS20171031.1(121.1km)
31 Oct
3 days 8 hours
21 earthquakes
PS20171104.1(107.6km)
4 Nov
11 hours
6 earthquakes
PS20171116.1(117.9km)
15 Nov
18 hours
12 earthquakes
PS20171119.1(82.3km)
19 Nov
16 hours
20 earthquakes
2018
PS20181016.1(144.7km)
16 Oct
1 day 0 hours
19 earthquakes
PS20181205.1(158.5km)
5 Dec
3 days 2 hours
41 earthquakes
2019
PS20190519.1(139.3km)
19 May
13 hours
5 earthquakes
2026
PS20260926.1(78.5km)
25 Sep
1 day 4 hours
13 earthquakes
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Seismic Swarm Analysis: April 2007 Event Southwest of Isangel, Vanuatu

The seismic swarm PS20070404.2 was recorded 129 km south-southwest of Isangel, Vanuatu. It began at 20:26 on 3 April 2007 and ended at 16:38 on 4 April 2007, lasting 20 hours and 12 minutes and producing six earthquakes. The sequence opened with a magnitude 6.2 event at 20:26 on 3 April at 12 km depth. On 4 April, a magnitude 6.2 shock occurred at 11:00 at 13 km depth, followed two minutes later by a magnitude 6.5 event at 10 km depth. Three additional events of magnitudes 4.9, 5.0 and 5.0 were recorded at 10 km depth between 13:05 and 16:38. Vanuatu occupies the central New Hebrides Arc, where the Australian Plate subducts eastward beneath the Pacific Plate at rates exceeding 10 cm per year. This convergent margin generates frequent intermediate-depth and shallow crustal seismicity. The April 2007 swarm occurred within the shallow portion of the Wadati-Benioff zone, consistent with stress release along the plate interface or within the overriding plate. Since 1 January 2000, only two prior swarms have been identified in the immediate area: one in 2003 and one in 2006. The 2007 swarm followed a magnitude 7.1 earthquake on 25 March 2007 located 52 km from the swarm centroid, suggesting possible aftershock triggering or continued adjustment of regional stress. Additional strong events within 100 km include magnitude 7.3 shocks on 9 April 2008, a magnitude 7.0 event on 13 January 2011, a magnitude 7.0 shock on 3 September 2011, a magnitude 7.0 earthquake on 19 November 2017, and a magnitude 7.1 event on 7 December 2023. Such swarms typically reflect transient increases in pore-fluid pressure or aseismic slip along the subduction thrust. Their low aftershock productivity relative to mainshock-aftershock sequences distinguishes them from classic foreshock-mainshock patterns, yet they remain valuable indicators of elevated seismic hazard in this rapidly deforming arc.

References

SeismoSight internal swarm catalogue PS20070404.2.
USGS Earthquake Catalog (events 2000–2023).
Bird, P. (2003). An updated digital model of plate boundaries. Geochemistry, Geophysics, Geosystems.