M 7.1; 125 km W of Port-Vila, Vanuatu; (2 Feb 2012) (96km from the earthquake)
M 7.1; 64 km S of Port-Vila, Vanuatu; (20 Aug 2011) (85km from the earthquake)
M 7.2; 71 km SSW of Port-Vila, Vanuatu; (20 Aug 2011) (89km from the earthquake)
M 7.3; 33 km NW of Port-Vila, Vanuatu; (10 Aug 2010) (7km from the earthquake)
M 7.2; 50 km WNW of Port-Vila, Vanuatu; (2 Jan 2002) (15km from the earthquake)
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