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Vanuatu subduction zone

The Vanuatu subduction zone is currently one of the most active subduction zones on Earth, producing great earthquakes, with potential for tsunami hazard to all coastlines of the Pacific Ocean. There are active volcanoes associated with arc volcanism.

Geography
The zone includes most of the islands of Vanuatu, the Santa Cruz islands of the southern Solomon Islands, and the Loyalty Islands. A number of ocean floor features are related to the zone, in particular the New Hebrides Trench (South New Hebridies Trench) and the North New Hebrides Trench (Torres Trench) which is separated from the southern trench by the d'Entrecasteaux Ridge and the island of Espiritu Santo. The d'Entrecasteaux Ridge is at this point of intersection two parallel, east–west trending ridges that are above the surrounding abyssal plain. ==Geology==
Geology
Shore based observations had characterised the islands of the volcanic arc as having typical lavas and being of early Miocene or younger in age. More recently marine surveys have supplemented this limited sampling. Reef terraces mantle on Espiritu Santo and Malekula show rapid late Quaternary terrace uplift of between . This material is lighter than the other subducted zone material except for West Torres Plateau material and this property is believed to be a factor in distortions of the island arc chain at these subduction points. The rest of the oceanic basalt crust of the Australian plate that is being subducted otherwise is Eocene in age. Tectonics The zone defines the plate boundary between the New Hebrides microplate, which is related to the Pacific plate, and the Australian plate. Ten million years ago the Vanuatu island chain had an almost east west orientation with Fiji and the spreading centers of the North Fiji Basin have created both the current separation and quite different orientation. The convergence rate in the subduction zone has a high rate of /year in the north at about latitude 11°S in the Solomon Island region, north of the Torres. The ridge may have been subducting for up to the last two million years. To the south subduction ceases at the triple junction with the Conway Reef microplate under the North Fiji Basin with the rest of the convergence being accommodated by less tectonically active rifting in the western stretch of the New Hebrides Trench, the Hunter Ridge to its north and the Hunter fracture zone which is a transform faulting fracture zone continuation of the trench towards Fiji. This triple junction is where from 3 million years ago the southernmost Central Spreading Ridge of the North Fiji Basin propagated southward and has now intersected with the New Hebrides Trench and the Hunter fracture zone. The epicenter was close to Matthew Island, to the north of the trench and was both preceded and followed by a seismic crisis of multiple events with greater than Other significant earthquakes may be found in the list of earthquakes in Vanuatu, list of earthquakes in the Solomon Islands archipelago and New Hebrides Trench articles. Tsunami hazard The tsunami resulting from the 2013 Solomon Islands earthquake was high at the town of Lata on Nendö in the Santa Cruz Islands and resulted in ten deaths. So did Epi and Ambae, which is Vanuatu's most voluminous active volcano. In 2022 Ambrym and the Gaua volcanoes erupted. ==References==
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