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Location:
Magnitude:
7.3
Time:
10 Aug 2010 05:23:51
Depth:
80.0
M 7.0+:
There are 14 swarms found nearby.
2002
PS20020102.1(41.6km)
2 Jan
1 day 13 hours
9 earthquakes
6 Jan
9 hours
5 earthquakes
2004
PS20040422.1(18.7km)
22 Apr
9 hours
7 earthquakes
2005
PS20050925.1(45.4km)
25 Sep
12 hours
8 earthquakes
2009
PS20090602.1(32.8km)
1 Jun
18 hours
7 earthquakes
PS20090605.1(31.9km)
5 Jun
18 minutes
5 earthquakes
PS20090612.1(29.2km)
12 Jun
5 hours
7 earthquakes
2010
PS20100810.1(26.3km)
10 Aug
2 days 7 hours
23 earthquakes
2011
PS20110820.1(90.3km)
20 Aug
1 day 17 hours
18 earthquakes
2012
PS20120202.1(82.5km)
2 Feb
16 hours
21 earthquakes
2020
PS20200527.1(49.3km)
26 May
9 hours
5 earthquakes
2021
PS20210216.1(24.1km)
15 Feb
2 days 1 hours
14 earthquakes
2024
PS20241217.1(22.6km)
17 Dec
16 hours
8 earthquakes
2025
PS20250210.1(23.2km)
10 Feb
12 hours
5 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Activity in Vanuatu: Tectonic Setting and Major Earthquakes

Vanuatu lies along the Pacific Ring of Fire in the southwestern Pacific Ocean, where the Indo-Australian Plate subducts beneath the Pacific Plate at a rate of approximately 7–10 cm per year. This convergent boundary produces an active volcanic arc and generates frequent moderate-to-large earthquakes, many at intermediate depths within the subducting slab. The capital, Port-Vila, sits near the plate interface, exposing the region to repeated strong shaking. On 10 August 2010 at 05:23 UTC, a magnitude 7.3 earthquake occurred at 80 km depth beneath Vanuatu. Two closely spaced solutions place the hypocenter either directly beneath the islands or 7 km northwest of Port-Vila. The event produced felt intensities up to VII in the capital and triggered minor landslides on nearby islands, yet casualties remained low owing to the depth and the relatively sparse population. Instrumental records since 2000 document several additional M 7+ events within 100 km of Port-Vila. On 2 January 2002 a magnitude 7.2 earthquake struck 50 km west-northwest of the capital. Two magnitude 7.1 events occurred on 20 August 2011, one 64 km south and the other accompanied by a magnitude 7.2 shock 71 km south-southwest of Port-Vila. A magnitude 7.1 earthquake took place on 2 February 2012, 125 km west of the city. Most recently, a magnitude 7.3 event was recorded on 17 December 2024, centered 24 km west-northwest of Port-Vila. These earthquakes cluster along the steeply dipping Wadati-Benioff zone that extends to depths exceeding 200 km beneath the arc. Intermediate-depth events such as the 2010 mainshock typically produce less surface damage than shallow crustal shocks of comparable magnitude, yet they still pose tsunami and liquefaction hazards along the coast. Ongoing subduction ensures that Vanuatu will continue to experience large earthquakes. Modern seismic monitoring by regional and global networks now provides rapid location and magnitude estimates, supporting improved early-warning capabilities for the island nation.

References

United States Geological Survey Earthquake Catalog Global CMT Project Moment Tensor Solutions