Humboldt (Nazca) Seamount Chain

E256201

The Humboldt (Nazca) Seamount Chain is a linear series of submarine volcanic mountains on the Nazca Plate in the southeastern Pacific Ocean, formed by hotspot-related volcanism and trending roughly parallel to the nearby Nazca Ridge.

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All labels observed (1)

Label Occurrences
Humboldt (Nazca) Seamount Chain canonical 1

Statements (30)

Predicate Object
instanceOf seamount chain
submarine volcanic mountain chain
composedOf seamounts
submarine volcanoes
formedBy hotspot volcanism
geodynamicOrigin fixed or slowly moving mantle hotspot
geologicalAge Cenozoic
geologicalProcess volcanic construction
geologicalRelation parallel to Nazca Ridge
hasMorphology linear chain of seamounts
isBathymetricHigh true
isLinearFeature true
isSubmarine true
isUnderJurisdictionOf international waters
isVolcanic true
liesOnPlate Nazca Plate interior
locatedInOcean southeastern Pacific Ocean
locatedOnTectonicPlate Nazca Plate
namedAfter Alexander von Humboldt
nearbyFeature Nazca Ridge
orientation roughly northwest–southeast
partOf Nazca oceanic crust volcanic provinces
researchDiscipline marine geology
plate tectonics
volcanology
seafloorFeatureType oceanic volcanic chain
tectonicPlateMotionContext Nazca Plate motion over hotspot
tectonicSetting intraplate volcanism
trendRelativeToNazcaRidge roughly parallel
volcanismType oceanic hotspot volcanism

Referenced by (1)

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

Nazca Ridge isParallelTo Humboldt (Nazca) Seamount Chain