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Location:
Period:
1 Apr 2007 20:39:58 - 3 Apr 2007 21:34:56 (2 days 54 minutes)
Volcanoes in 100km radius:
Coleman Seamount(35km), Kana Keoki(46km), Kavachi(65km), Unnamed(67km)
Earthquakes:
20
M 7.0+:
5 swarms found nearby.
2004
PS20040828.1(12.8km)
28 Aug
7 hours
5 earthquakes
2007
PS20070404.1(192.9km)
4 Apr
10 hours
5 earthquakes
2010
PS20100103.1(49.4km)
3 Jan
2 days 7 hours
23 earthquakes
PS20100109.1(57.6km)
8 Jan
1 day 7 hours
8 earthquakes
PS20100119.1(57.6km)
18 Jan
1 hours
5 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm PS20070401.1 Near Gizo, Solomon Islands

The Solomon Islands occupy a tectonically active segment of the Pacific Ring of Fire, where the Pacific Plate converges with and subducts beneath the Australian Plate along the New Britain–San Cristobal trench system. This convergent margin produces frequent large earthquakes and associated tsunamis. The Gizo region, located on the western edge of the archipelago, lies directly above the subducting slab and experiences elevated seismicity at depths typically between 10 and 30 km.

Seismic swarm PS20070401.1 was recorded 49 km northeast of Gizo between 20:39 UTC on 1 April 2007 and 21:34 UTC on 3 April 2007. Within 48 hours and 54 minutes the sequence comprised 20 events. The swarm initiated with an Mw 8.1 earthquake at 24 km depth, followed by a rapid succession of aftershocks. Magnitudes ranged from 5.0 to 8.1, with the majority occurring at depths of 10–20 km. Notable events included two Mw 6.2 earthquakes on 2 April at depths of 14 km and 18 km, respectively. Activity declined steadily, with the final recorded event reaching Mw 5.2 at 20 km depth.

The 2007 sequence occurred within a broader pattern of regional seismicity. Historical records maintained by SeismoSight indicate that only one prior swarm has been identified in the area since 1 January 2000, occurring in 2004. Two strong earthquakes have also been documented since that date: an Mw 7.1 event on 3 January 2010 located 94 km southeast of Gizo and 13 km from the swarm centroid, and the Mw 8.1 mainshock of 1 April 2007 itself, situated 53 km from the swarm center.

Geological interpretation of the swarm suggests it represents a clustered release of stress along the plate interface following the primary rupture. The shallow focal depths and rapid temporal decay are consistent with aftershock sequences in subduction-zone settings. Continued monitoring remains essential because the Solomon Islands margin retains the potential for future large-magnitude events.

References
USGS Earthquake Catalog (earthquake.usgs.gov)
Global CMT Catalog (globalcmt.org)
SeismoSight internal swarm classification database