West Mata

West Mata can be found in the northeastern portion of Tonga, in between Fiji and Samoa. It is located approximately southwest of the Samoan Islands and around northeast of the Lau Islands of Fiji. Structure With data from bathymetric surveys, the structure of the West Mata volcano was made more clear. The West Mata vent has a common structure with most volcanic structures in the area, mostly dominated by a prominent rift zone that extends away from the summit, which is the peak of a conical structure with a circular base on the seafloor. Therefore, meanwhile the northeast and southwest flanks are rugged, the northwest and southeast flanks are rather smooth. This structure can also be seen on the East Mata volcano. The rift zones on the flanks consist of stair-like lava platforms piled on each other. The east-northeast rift zone curves towards the east as it deepens, and the west-southwest rift zone is west‐oriented towards its end. The summit area of West Mata is a narrow ridge aligned with those two rift zones. There are no structures similar to a crater at the summit although remnants of a former caldera seem to exist. Other conical volcanic features are limited and can only be found on the lower parts of both rift zones. ==Geologic setting==

. The Western Pacific Ocean is filled with many island-arc systems and trenches that come along them. Usually island arcs in this area are claimed to be chains of islands which are detached from continental masses. Between the island-arcs and the continental margins, still liquidated areas of seafloor are exposed out. These areas of seafloor are called back-arc basins. Most back-arc basins are rather shallow regions of ocean crust that are younger than the subducted crust in the adjacent trench. Back-arc basins can be found in between inactive and extinct volcanic arcs and the currently active volcanic island arcs that form as a result of the subduction. The Lau Basin, which West Mata can be found in, is one of the best examples of back-arc basins. The Lau Basin consists of an area of oceanic crust which separates the now remnant and extinct Lau-Colville Ridge volcanic arc and the Tofua volcanic arc with very active volcanism. The seaward rollback of the Tonga Trench is thought to be the main reason of the diverging action in this region. The basin lies above the westward-dipping seismically active area of subduction where the Pacific Plate slips under the Australian Plate. West Mata, specifically, is located in the northern part of the Lau Basin, defined as the Northeastern (NE) Lau Basin. The NE Lau Basin borders several spreading centers on the west, including the NE Lau Spreading Center, the Mangatolu Triple Junction and the Fonualei Rift Spreading Center from north to south, respectively. On the northern border of the basin can be found the area where the Kermadec-Tonga subduction zone transitions into a convergent strike-slip boundary. Meanwhile the plate boundary transitions, the faulting direction also changes from north-south to northwest-southeast directed faulting. The rollback of the trench which has also created the back-arc Lau basin created an area of oblique shear that has generated a whole zone of spreading centers and rifts with active hydrothermal vents along the northern boundary. West Mata can be considered one of them. The NE Lau Basin has one of the highest upper mantle temperatures in the world, has one of Earth's coolest slab thermal parameters (which is caused by the age and the speed of slab convergence), and has among the highest slab water flux values of any oceanic subduction zone. These factors cause the area's tectonism and volcanism to be complex compared to other places and cause the large amount of volcanic systems that exist in the NE Lau Basin. Composition Most volcanic extrusions in the NE Lau Basin region structures usually erupt dacite lavas, some with unusual morphologies, which are quite rare in submarine volcanoes. Other than dacitic lavas, rift zones in the region have been also found to erupt basaltic andesite compositions. However, in the Mata volcano group, the main composition of eruptions in the Matas consists of mostly boninite, which is a type of extrusive rock usually seen in the Izu-Bonin Island Arc. ==Fauna==

West Mata and the surrounding NE Lau Basin are home to many hydrothermal vents, meaning that the area hosts a hydrothermal vent environment, which hosts organisms that use hydrothermal vents to supply their living needs. These environments can be seen in many continental margins around the world. Hydrothermal ecology The hydrothermal ecology of the Lau Basin is home to many endemic organisms, including the Lamellibrachia columna which shows similarity to Lamellibrachia satsuma that can be found in Japan; Neobrachylepas relica, a close relative to the Brachylepadomorpha which was extinct since the Miocene; and more. In West Mata, these organisms were not observed, pointing to the diversity of the Lau Basin's ecology. Instead, a hydrothermal environment consisting of three species of polychaete worms, two species of shrimp, three species of crabs and eelpouts was observed. During the eruption of 2008–10 it was observed that there were only large groups of opaepele shrimp on the seamount and the normal hydrothermal vent community was not present. ==Activity==

The volcano has known to be both hydrothermally and eruptively active in recent history, the most active in between its neighboring volcanoes. Both vents, Hades and Prometheus, had different eruption styles. Hades was erupting with frequent magma bursts; meanwhile, Prometheus was showing a rapid degassing eruption. These eruptions both generated broadband signals which were recorded by hydrophones that were set up in the area in 2009. Elevation changes at the flanks of the volcano were observed by hydrophones and bathymetric surveys at the area over the years, pointing out that West Mata has had many landslides at the years of the eruption. Following the main eruption, several papers suggest that in 2010–11 lava flows were recorded that covered an area of by at below sea level according to bathymetry depth differences. The same papers also note that a year later, West Mata had an eruption between 2012 and 2016 at a depth of . It was discovered the same way as the 2010–11 eruption, via bathymetry depth differences and bathymetric surveys. ==See also==