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Location:
Period:
2 Feb 2012 13:34:40 - 3 Feb 2012 06:01:38 (16 hours 26 minutes)
Volcanoes in 100km radius:
None
Earthquakes:
21
M 7.0+:
18 swarms found nearby.
2002
PS20020102.1(90.0km)
2 Jan
1 day 13 hours
9 earthquakes
PS20020106.1(86.3km)
6 Jan
9 hours
5 earthquakes
2004
PS20040422.1(80.2km)
22 Apr
9 hours
7 earthquakes
2005
PS20050925.1(40.2km)
25 Sep
12 hours
8 earthquakes
2009
PS20090602.1(74.6km)
1 Jun
18 hours
7 earthquakes
PS20090605.1(52.8km)
5 Jun
18 minutes
5 earthquakes
PS20090612.1(53.4km)
12 Jun
5 hours
7 earthquakes
2010
PS20100810.1(56.6km)
10 Aug
2 days 7 hours
23 earthquakes
2011
PS20110820.1(131.8km)
20 Aug
1 day 17 hours
18 earthquakes
PS20110825.1(137.2km)
24 Aug
1 day 12 hours
8 earthquakes
PS20110831.1(141.7km)
30 Aug
18 hours
5 earthquakes
2015
PS20150219.1(144.0km)
19 Feb
6 hours
5 earthquakes
2016
PS20160430.1(124.5km)
29 Apr
22 hours
5 earthquakes
2018
PS20181216.1(147.1km)
15 Dec
19 hours
8 earthquakes
2020
PS20200527.1(74.1km)
26 May
9 hours
5 earthquakes
2021
PS20210216.1(58.4km)
15 Feb
2 days 1 hours
14 earthquakes
2024
PS20241217.1(98.2km)
17 Dec
16 hours
8 earthquakes
2025
PS20250210.1(60.2km)
10 Feb
12 hours
5 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm PS20120202.1: February 2012 Activity West of Port-Vila, Vanuatu

A seismic swarm designated PS20120202.1 occurred 125 km west of Port-Vila, Vanuatu, beginning at 13:34 on 2 February 2012 and concluding at 06:01 on 3 February 2012. Over 16 hours and 26 minutes, the sequence produced 21 earthquakes. The initial event reached magnitude 7.1 at a depth of 23 km. Subsequent shocks included multiple magnitude 5.0–5.5 events clustered at shallow depths around 10 km, with later activity featuring a magnitude 6.1 event at 8 km depth on 3 February.

The swarm exhibited typical characteristics of clustered seismicity, with events distributed across depths from 3 km to 25 km. Magnitudes remained predominantly in the 5.0–5.5 range after the mainshock, indicating a rapid decay in energy release following the initial rupture.

Vanuatu occupies a tectonically active segment of the Pacific Ring of Fire, where the Indo-Australian Plate subducts beneath the Pacific Plate along the New Hebrides Trench. This convergence drives frequent earthquakes and volcanic activity throughout the archipelago. The region experiences high seismic strain accumulation, resulting in both isolated large events and episodic swarms.

Since 2000, eleven swarms have been recorded in the area, occurring in 2002 (two events), 2004 (one), 2005 (one), 2009 (three), 2010 (one), and 2011 (three). These episodes reflect the ongoing subduction dynamics and stress interactions along the plate boundary.

Notable strong earthquakes since 2000 include a magnitude 7.3 event on 17 December 2024 located 94 km from the swarm center, the 2012 magnitude 7.1 mainshock itself (46 km from center), two magnitude 7.3 shocks in August 2010 (82–89 km distant), and a magnitude 7.2 event in January 2002 (68 km from center). Such occurrences underscore the persistent seismic hazard in central Vanuatu.

The 2012 swarm contributed to the documented pattern of moderate-to-large events near the subduction interface, consistent with the area's long-term tectonic regime.

References
SeismoSight internal swarm classification records
USGS Earthquake Catalog (updated December 2024)