New Hebrides Trench
The New Hebrides Trench is an oceanic trench which extends to over 7.6 km deep in the southern Pacific Ocean. It lies to the northeast of New Caledonia and the Loyalty Islands, to the southwest of Vanuatu, west of Australia, and south of Papua New Guinea and the Solomon Islands. The trench was formed as a result of the subduction zone. The Australian plate is being subducted under the New Hebrides Plate causing volcanism which produced the Vanuatu island chain.

The trench was first explored in 2013 by the University of Aberdeen's Oceanlab team. They found cusk-eels, prawns, and other eels, and crustaceans. This is significantly different from other deep sea trenches that have been studied.[1]
Tectonics
At the New Hebrides Trench, the Australian plate is being subducted underneath the New Hebrides microplate. The convergence rate ranges from 120 mm (4.7 in)/yr in the south, to 40 mm (1.6 in)/yr in the central section, to 170 mm (6.7 in)/yr in the north. The anomalous lack of convergence in the central section is caused by the subduction of the d'Entrecasteaux Ridge.
Associated seismicity
Major earthquakes associated with the subduction zone:[2][3]
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2009 Vanuatu earthquakes | |||
2013 Solomon Islands earthquake | |||
2021 Loyalty Islands earthquake |
References
- Morelle, Rebecca (3 March 2014). "New Hebrides trench: First look at unexplored deep sea". BBC News. Retrieved 25 January 2022.
- "Map of Magnitude 7.5+ along the New Hebrides Trench and Surrounding Areas". USGS. Retrieved 25 January 2022.
- Ioualalen, Mansour (May 2017). "Investigating the March 28th 1875 and the September 20th 1920 earthquakes/tsunamis of the Southern Vanuatu arc, offshore Loyalty Islands, New Caledonia". Tectonophysics. 709: 20. Bibcode:2017Tectp.709...20I. doi:10.1016/j.tecto.2017.05.006.