Cocos Ridge seamounts

E885776

The Cocos Ridge seamounts are a chain of submarine volcanic mountains in the eastern Pacific Ocean formed by hotspot-related volcanism along the Galápagos plume track.

Try in SPARQL Jump to: Surface forms Statements Referenced by

All labels observed (1)

Label Occurrences
Cocos Ridge seamounts canonical 1

Statements (32)

Predicate Object
instanceOf seamount chain
submarine volcanic mountains
agePattern generally younger toward the Galápagos hotspot
associatedWith hotspot track bathymetric high
oceanic crust thickening
composition basaltic rocks
discoveredBy marine geophysical surveys
formedBy Galápagos hotspot NERFINISHED
hotspot volcanism
formedDuring Cenozoic NERFINISHED
geologicalSetting intraplate volcanism
influences seafloor topography of Cocos Plate
locatedIn eastern Pacific Ocean NERFINISHED
locatedOn Cocos Plate NERFINISHED
morphology elongate ridge with aligned seamounts
ocean Pacific Ocean
originatesFrom Galápagos plume track
partOf Cocos Ridge NERFINISHED
process oceanic plate motion over stationary hotspot
relatedTo Carnegie Ridge NERFINISHED
Cocos Island NERFINISHED
Galápagos Islands NERFINISHED
researchField marine geology
plate tectonics
volcanology
studyMethod dredge sampling
marine seismic reflection
multibeam bathymetry
radiometric dating of basalts
tectonicPlateContext Cocos Plate NERFINISHED
Nazca Plate NERFINISHED
volcanicProvince Galápagos hotspot track

Referenced by (1)

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

Galápagos plume track hasPart Cocos Ridge seamounts