Cocos Ridge

E51834

Cocos Ridge is a prominent submarine volcanic ridge in the eastern Pacific Ocean formed by hotspot-related volcanism on the Cocos Plate.

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Statements (46)

Predicate Object
instanceOf oceanic plateau
submarine volcanic ridge
adjacentTo Middle America Trench
ageRange Miocene to present volcanism
associatedWith Central American Volcanic Arc
surface form: Central American volcanic arc

seamount chains
boundedBy Middle America Trench
countryOffshoreFrom Costa Rica
Nicaragua NERFINISHED
Panama
crustType thickened oceanic crust
elevationRelativeToSeafloor up to several kilometers above surrounding basins
extendsTowards Central America
formedBy hotspot volcanism
formedDuring Cenozoic
geologicalHazardImpact modification of tsunami and earthquake behavior along Central America
geologicalProcess intraplate volcanism
hasFeature flattened volcanic edifices
sediment-covered volcanic basement
hasMorphology broad elevated ridge
influences regional plate buoyancy
seismicity in Central America
subduction geometry beneath Central America
uplift of Costa Rican margin
isExampleOf hotspot track on an oceanic plate
subducting aseismic ridge
isPartOf Cocos Plate large igneous province
locatedIn eastern Pacific Ocean
locatedOnTectonicPlate Cocos Plate
namedAfter Cocos Plate
ocean Pacific Ocean
origin hotspot-related oceanic plateau
region offshore Central America
relatedTo Galápagos hotspot
Galápagos plume track
researchInterest plate–mantle interaction
ridge subduction processes
separates Cocos Basin
Guatemala Basin
surface form: Panama Basin
studiedBy marine geology
marine geophysics
seismology
subductsBeneath Caribbean Plate
Central American margin
tectonicSetting subducting oceanic ridge
trends northeast–southwest

Referenced by (2)

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

Cocos Plate hasFeature Cocos Ridge
Cocos Island volcanicArcOrBelt Cocos Ridge