Ryukyu Trench

E49320

The Ryukyu Trench is a deep oceanic trench in the western Pacific, running along the Ryukyu Islands south of Japan where the Philippine Sea Plate subducts beneath the Eurasian Plate.

Observed surface forms (1)

Surface form As subject As object
Ryukyu Trench region 0 1

Statements (30)

Predicate Object
instanceOf oceanic trench
subduction zone
associatedIslandArc Ryukyu Islands
surface form: Ryukyu Island Arc
causes earthquakes
tsunami hazard
countryMaritimeZone Japan exclusive economic zone
countryOffshoreFrom Japan
extendsFrom south of Kyushu
extendsTo near Taiwan
featureOf Eurasian Plate
surface form: Eurasian Plate margin

Philippine Sea Plate
surface form: Philippine Sea Plate margin
formedBy plate convergence between Philippine Sea Plate and Eurasian Plate
geologicalAge Cenozoic
geologicalProcess oceanic lithosphere subduction
locatedIn western Pacific Ocean
locatedOffCoastOf Ryukyu Islands
locatedSouthOf Japan
maximumDepth over 7000 meters
nearbySea East China Sea
Philippine Sea
ocean Pacific Ocean
overridingPlate Eurasian Plate
parallelTo Ryukyu Islands
surface form: Ryukyu Island chain
partOf Pacific Ring of Fire
region East China Sea region
Philippine Sea
surface form: Philippine Sea region
relatedTo Ryukyu Islands
surface form: Nansei-Shoto (Ryukyu) Islands
seafloorMorphology narrow and elongated trench
subductingPlate Philippine Sea Plate
tectonicSetting convergent plate boundary

Referenced by (7)

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

Okinawa Plate adjacentTo Ryukyu Trench
this entity surface form: Ryukyu Trench region
Ryukyu Arc adjacentTo Ryukyu Trench
western Pacific Ocean contains Ryukyu Trench
Philippine Sea hasOceanTrench Ryukyu Trench
Ryukyu Arc hasPart Ryukyu Trench
Philippine Sea Plate hasTrench Ryukyu Trench
Ryukyu Arc parallelTo Ryukyu Trench