New Britain subduction zone

E1024251

The New Britain subduction zone is a highly active convergent plate boundary north of New Britain Island in Papua New Guinea, known for intense seismicity and volcanism along the Bismarck Sea region.

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Statements (46)

Predicate Object
instanceOf convergent plate boundary
subduction zone
associatedWith Bismarck Sea NERFINISHED
New Britain Trench NERFINISHED
causes crustal deformation in New Britain region
uplift of volcanic islands
characterizedBy active volcanism
arc volcanism
frequent large earthquakes
intense seismicity
forms New Britain volcanic arc NERFINISHED
geologicalAge Cenozoic
hasAssociatedStructure back-arc region
forearc region
volcanic arc
hasFeature deep-focus earthquakes
intermediate-depth earthquakes
shallow megathrust interface
hasGeodynamicRole accommodates convergence between Pacific and Australian plates
hasHazard megathrust earthquakes
tsunamis
volcanic eruptions
hasMorphologicalExpression oceanic trench
hasProcess subduction of oceanic lithosphere
hasRelativeMotionType convergence GENERATED
hasRisk regional tsunami hazard for Papua New Guinea coasts
strong ground shaking in New Britain and surrounding islands
hasSeismicityLevel high
hasTectonicSetting oceanic-oceanic convergence
hasVolcanicActivityLevel high
locatedIn Bismarck Sea region NERFINISHED
Melanesia
Papua New Guinea NERFINISHED
South Pacific Ocean NERFINISHED
locatedNorthOf New Britain Island NERFINISHED
near Bismarck Archipelago NERFINISHED
New Britain Island NERFINISHED
New Ireland NERFINISHED
partOf Pacific Ring of Fire
Southwest Pacific plate boundary zone NERFINISHED
studiedInDiscipline plate tectonics
seismology
volcanology
tectonicallyLinkedTo Australian Plate NERFINISHED
Bismarck microplate NERFINISHED
Pacific Plate NERFINISHED

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

Garua Harbour volcanic complex tectonicSetting New Britain subduction zone