Seafloor topographic map of area adjactent to New Britain Trench.
Approximate surface projection on Pacific Ocean of New Britain Trench (blue).
The New Britain Trench (also known as Bougainville-New Britain Trench or New Britain-Solomon Trench)[1] has formed due to subduction of the floor of the Solomon Sea and has some of the highest current seismic activity in the world.[2]
The trench was discovered by the German research vessel SMS Planet, in 1910.[3]
^Marine Gazetteer:New Britain Trench
^Gallo et al. 2015, p. 120.
^GEBCO:New Britain Trench
and 26 Related for: New Britain Trench information
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George II", British Museum, retrieved 26 August 2011 Archive at the Wayback Machine (archived 29 April 2011) Trench, pp. 211–212. Trench, pp. 206–209...
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curved form, a chain of active or recently extinct volcanoes, a deep-sea trench, and a large negative Bouguer anomaly on the convex side of the volcanic...
has been isolated from sediments from a deep of 4700 meter from the NewBritainTrench. Parker, Charles Thomas; Garrity, George M (26 November 2018). Parker...
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Plate is the Solomon Sea Plate which is subducting under NewBritain at the NewBritainTrench and a likely still active Trobriand Plate which has fault...
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