New Hebrides Trench

E200325

The New Hebrides Trench is a deep oceanic trench formed by subduction along the convergent plate boundary near the New Hebrides island arc in the southwest Pacific.

All labels observed (1)

Label Occurrences
New Hebrides Trench canonical 2

How this entity was disambiguated

Statements (45)

Predicate Object
instanceOf oceanic trench
subduction zone feature
associatedWith New Hebrides island arc
Vanuatu island arc
linked to: New Hebrides

accretionary prism development
earthquakes
sediment subduction
seismic activity
volcanism in New Hebrides arc
formedBy subduction
geologicalAge Cenozoic
hasEnvironmentalCondition absence of sunlight
high hydrostatic pressure
low temperature deep-sea environment
hasFeature deep forearc basin
steep trench walls
hasGeodynamicRole consumption of oceanic lithosphere
hasMorphology narrow, elongated depression
hasNameOrigin New Hebrides (former name of Vanuatu)
linked to: New Hebrides
hasProcess oceanic plate subduction
isAdjacentTo New Hebrides back-arc basin
isBoundaryBetween Australian Plate
Pacific Plate region
linked to: Pacific Plate
isImportantFor hazard assessment in Vanuatu region
understanding convergent margin dynamics
isPartOf Southwest Pacific subduction systems
isTypeOf deep-sea trench
liesEastOf Australia
liesWestOf Fiji Basin
locatedIn Pacific Ocean
Southwest Pacific Ocean
locatedOffCoastOf New Caledonia region
linked to: New Caledonia

Vanuatu
maximumDepth over 7 km
over 7000 m
oceanRegion Coral Sea region
linked to: Coral Sea

southwestern Pacific basin
partOf New Hebrides island arc system
Pacific Ring of Fire
relatedTo subduction earthquakes
tsunami generation potential
studiedInField marine geology
plate tectonics
seismology
tectonicSetting convergent plate boundary

How these facts were elicited

Referenced by (2)

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

southwest Pacific Ocean contains New Hebrides Trench
Santa Cruz Islands hasNearbyTrench New Hebrides Trench