Mariana Island Arc

E22121

The Mariana Island Arc is a curved chain of volcanic islands in the western Pacific Ocean formed by the subduction of the Pacific Plate beneath the Philippine Sea Plate.


Statements (50)
Predicate Object
instanceOf island arc
tectonic feature
volcanic arc
adjacentTo Mariana Trench
associatedWith Benioff zone beneath the Mariana Trench
deep-focus earthquakes
contains Agrihan
Alamagan
Anatahan
Asuncion Island
Farallon de Pajaros
Guam
Guguan
Mariana Islands
Northern Mariana Islands
Pagan
Rota
Saipan
Sarigan
Tinian
country United States
formedBy subduction of the Pacific Plate beneath the Philippine Sea Plate
geologicalAge Cenozoic
governingTerritory Commonwealth of the Northern Mariana Islands
Guam
hasEconomicActivity fisheries
tourism
hasFeature active volcanoes
dormant volcanoes
extinct volcanoes
stratovolcanoes
submarine volcanoes
highestPoint Agrihan volcano
locatedIn Pacific Ocean
western Pacific Ocean
marginType ocean-ocean convergent margin
orientation north-south trending curve
overlies Philippine Sea Plate
overridingPlate Philippine Sea Plate
parallelTo Mariana Trench
partOf Mariana subduction system
Ring of Fire
rockType basaltic-andesitic volcanic rocks
separates Philippine Sea from the Pacific Ocean
studiedBy marine geologists
volcanologists
subductingPlate Pacific Plate
tectonicSetting convergent plate boundary
volcanicActivity frequent small to moderate eruptions
volcanismType subduction-related volcanism

Referenced by (7)
Subject (surface form when different) Predicate
Mariana volcanic arc ("Mariana Islands")
Micronesia ("Mariana Islands")
hasPart
Mariana Trench
adjacentIslandArc
Philippine Sea ("Mariana Islands")
locatedWestOf
Mariana subduction zone ("Mariana island arc")
produces
Magellan–Elcano expedition ("Mariana Islands")
visitedRegion
Sarigan ("Mariana Arc")
volcanicArc

Please wait…