Cocos–Nazca spreading center

E54044

The Cocos–Nazca spreading center is a mid-ocean ridge in the eastern Pacific where tectonic divergence forms and separates the Cocos and Nazca plates.

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Statements (45)

Predicate Object
instanceOf mid-ocean ridge
spreading center
associatedWith magmatic accretion at plate boundary
seafloor spreading
boundedBy transform faults
crustAgePattern progressively older crust away from axis
youngest crust at ridge axis
crustFormationMechanism partial melting of upper mantle
crustTypeProduced mafic oceanic crust
forms oceanic crust
geodynamicContext spreading of oceanic plates in eastern Pacific
geologicalAgeContext Cenozoic
geologicalProcess tectonic divergence
hasFeature axial rift valley
hydrothermal circulation
normal faulting
volcanic activity
hasMorphology linear volcanic ridge
heatFlow elevated
influences bathymetry of eastern Pacific seafloor
isAssociatedWith mantle upwelling beneath ridge axis
isBoundaryType constructive plate margin
isCharacterizedBy high geothermal gradient
high seismicity relative to surrounding seafloor
thin lithosphere at ridge axis
isPartOf global mid-ocean ridge system
isSiteOf mid-ocean ridge basalt eruptions
isSubmarine true
lithosphereType oceanic lithosphere
locatedIn eastern Pacific Ocean
movementType spreading apart
namedAfter Cocos Plate
Nazca Plate
ocean Pacific Ocean
partOf East Pacific Rise
surface form: Pacific mid-ocean ridge system
plateBoundaryBetween Cocos Plate
Nazca Plate
separates Cocos Plate
Nazca Plate
spreadingEnvironment oceanic-oceanic divergent boundary
tectonicPlateRegion Cocos Plate
Nazca Plate
tectonicRole accommodates relative motion between Cocos and Nazca plates
tectonicSetting divergent plate boundary
topographicExpression submarine ridge

Referenced by (1)

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

Cocos Plate createdAt Cocos–Nazca spreading center