M 7.1; 125 km W of Port-Vila, Vanuatu; (2 Feb 2012) (80km from the earthquake)
M 7.1; 64 km S of Port-Vila, Vanuatu; (20 Aug 2011) (87km from the earthquake)
M 7.2; 71 km SSW of Port-Vila, Vanuatu; (20 Aug 2011) (90km from the earthquake)
M 7.3; Vanuatu; (10 Aug 2010) (15km from the earthquake)
M 7.3; 33 km NW of Port-Vila, Vanuatu; (10 Aug 2010) (23km from the earthquake)
Seismic Activity Near Port-Vila, Vanuatu
Vanuatu occupies a tectonically active segment of the southwest Pacific, situated along the New Hebrides subduction zone. Here, the Australian Plate converges with and subducts beneath the Pacific Plate at rates exceeding 10 cm per year, generating frequent large-magnitude earthquakes. The capital, Port-Vila, lies near this plate boundary, where megathrust and intraslab events pose recurrent hazards. Crustal depths in the region typically range from shallow (less than 30 km) to intermediate, consistent with the 21 km depth recorded for the 2 January 2002 M7.2 earthquake located 50 km WNW of Port-Vila.
Instrumental records document multiple M7+ events within 100 km of Port-Vila since 2000. The 2 January 2002 M7.2 event remains a benchmark for local strong shaking, with its epicenter serving as the reference point for subsequent activity. On 10 August 2010, an M7.3 earthquake struck 33 km northwest of Port-Vila, only 23 km from the 2002 site. Two M7.1 events occurred on 20 August 2011—one 64 km south and another 71 km south-southwest of the capital—followed by an M7.1 on 2 February 2012 located 125 km west. The most recent event, an M7.3 on 17 December 2024 situated 24 km WNW of Port-Vila, occurred just 26 km from the 2002 epicenter, underscoring persistent strain accumulation along the subduction interface.
These earthquakes reflect the characteristic pattern of the New Hebrides arc, where both interplate thrust events and normal-faulting aftershocks occur. Depths between 15 km and 30 km align with the seismogenic zone above the subducting slab. Historical catalogs indicate that similar sequences have affected the island chain throughout the twentieth century, often accompanied by tsunami generation and localized coastal impacts.
Ongoing monitoring by regional seismic networks continues to track aftershock sequences and background seismicity. The close spatial clustering of recent M7+ events relative to the 2002 rupture zone highlights the potential for repeated loading of adjacent fault segments. Mitigation efforts in Vanuatu emphasize building-code enforcement and community preparedness given the high recurrence rate of strong ground motion near population centers.
References
USGS Earthquake Catalog (events 2002–2024)
Global CMT Project
Pacific Tsunami Warning Center historical bulletins