Java Trench

E41169

The Java Trench is a deep oceanic trench in the eastern Indian Ocean formed by the subduction of the Indo-Australian Plate beneath the Sunda Plate, making it one of the world’s deepest and most seismically active marine regions.

Jump to: Statements Referenced by

Statements (42)

Predicate Object
instanceOf oceanic trench
subduction zone
alsoKnownAs Sunda Trench
surface form: Java–Sunda Trench

Sunda Trench
associatedWith megathrust earthquakes
tsunamis in the Indian Ocean
characteristic frequent earthquakes
high seismic activity
tsunamigenic earthquakes
countryBorder Indonesia
extendsAlong south of Java
south of Sumatra
formedBy subduction of the Indo-Australian Plate beneath the Sunda Plate
geologicalAge Cenozoic
geologicalProcess oceanic lithosphere subduction
hazardZoneFor Indonesia
influences Indian Ocean tsunami risk
knownFor significant seismic hazard
steep bathymetric gradients
liesWithin Southeast Asia
surface form: Southeast Asia maritime region
locatedIn eastern Indian Ocean
locatedOffCoastOf Java
Sumatra
maximumDepth about 7,200 metres
over 23,000 feet
over 7 kilometres
near Sunda Strait
ocean Indian Ocean
oneOf deepest oceanic trenches in the world
oriented roughly northwest–southeast
overridingPlate Sunda Plate
partOf Alpine-Himalayan orogenic belt
surface form: Alpide Belt

Indian Ocean
plateBoundaryBetween Indo-Australian Plate
Sunda Plate
region Sunda Arc
relatedTo volcanic activity in the Sunda Arc
seafloorFeatureType deep-sea trench
subductingPlate Indo-Australian Plate
subductionType oceanic–continental subduction
tectonicProvince Sunda subduction system
tectonicSetting convergent plate boundary

Referenced by (5)

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

Sunda Trench alsoKnownAs Java Trench
Sunda Plate associatedWith Java Trench
Indian Ocean hasDeepestPoint Java Trench