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 27 Related for: New Britain Trench information
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seamounts being in the zone, and with the New BritainTrench marking the current subduction boundary. The trench is up to 9,046 m (29,678 ft) deep. To the...
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...
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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more than 7,260 m (23,820 ft) stopped short of the bottom of the NewBritainTrench when problems with the vertical thrusters led Cameron to return to...
"Isostatic anomaly characteristics and tectonism of the NewBritainTrench and neighboring Papua New Guinea". Geodesy and Geodynamics. 9 (5): 404–410. doi:10...
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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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difficult to trace southeast of New Ireland. To the southeast, the NewBritainTrench links to the Solomon Islands Trench along which the Solomon Sea Plate...
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