Kyushu–Palau Ridge system

E71827

The Kyushu–Palau Ridge system is a major underwater volcanic island arc and tectonic ridge in the Philippine Sea, formed by subduction-related processes along the western Pacific margin.

All labels observed (4)

How this entity was disambiguated

Statements (30)

Predicate Object
instanceOf geologic feature
tectonic ridge
underwater volcanic island arc
associatedWith Pacific Plate
Philippine Sea Plate
characterizedBy deep-sea ridges
submarine volcanoes
extendsFrom Kyushu region of Japan
linked to: Kyushu
extendsTo Palau region
linked to: Palau
formedBy subduction-related processes
geologicAge Cenozoic
geologicOrigin island arc volcanism
isPartOf western Pacific island arc system
liesEastOf Ryukyu Islands
liesWestOf West Philippine Basin
locatedIn Philippine Sea
western Pacific Ocean
namedAfter Kyushu
Palau
orientation roughly north–south
partOf Izu–Bonin–Mariana arc system
linked to: Izu–Bonin Arc

Philippine Sea plate margin
relatedProcess arc magmatism
oceanic crust subduction
researchField marine geology
plate tectonics
separates Parece Vela Basin
West Philippine Basin
tectonicRole fossil island arc
tectonicSetting convergent plate margin

How these facts were elicited

Referenced by (6)

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

Philippine Sea Plate hasTrench Kyushu–Palau Ridge system
Philippine Basin boundedBy Kyushu–Palau Ridge
linked to: Kyushu–Palau Ridge system
Shikoku Basin boundedBy Kyushu–Palau Ridge
linked to: Kyushu–Palau Ridge system
Shikoku Basin liesEastOf Kyushu–Palau Ridge
linked to: Kyushu–Palau Ridge system
West Philippine Basin boundedBy Palau-Kyushu Ridge
linked to: Kyushu–Palau Ridge system
Hyuga-nada segment adjacentTo Kyushu-Palau Ridge (to the south, plate interior)
linked to: Kyushu–Palau Ridge system