Meiji Seamount

E130107

Meiji Seamount is a large, ancient underwater volcano located at the northern end of the Hawaiian–Emperor seamount chain in the North Pacific Ocean.

All labels observed (1)

Label Occurrences
Meiji Seamount canonical 3

How this entity was disambiguated

Statements (47)

Predicate Object
instanceOf guyot ⓘ
seamount ⓘ
submarine volcano ⓘ
age approximately 80 million years ⓘ
approximateLatitude ~53°N ⓘ
approximateLongitude ~165°E ⓘ
baseDepth over 5000 meters below sea level ⓘ
chain Emperor seamounts ⓘ
linked to: Emperor Seamounts

Hawaiian–Emperor seamount chain ⓘ
chainPosition oldest large volcano in the Hawaiian–Emperor seamount chain ⓘ
country international waters ⓘ
crustType oceanic crust ⓘ
discoveredBy bathymetric surveys of the North Pacific ⓘ
distanceFromHawaii over 2000 kilometers northwest of the Hawaiian Islands ⓘ
eroded yes ⓘ
erosionalHistory summit planed off by wave erosion before subsidence ⓘ
erosionProcess marine erosion ⓘ
featureType flat-topped seamount ⓘ
underwater volcano ⓘ
formedAs shield volcano ⓘ
formedBy Hawaiian hotspot ⓘ
geologicalAge Late Cretaceous ⓘ
geologicProvince northwestern Hawaiian–Emperor seamount province ⓘ
hasFlatSummit yes ⓘ
hasScientificInterest high ⓘ
hotspotTrackRole records early part of Hawaiian hotspot track ⓘ
lastEruption Cretaceous period ⓘ
locatedAtEndOf northern end of the Hawaiian–Emperor seamount chain ⓘ
locatedIn Hawaiian–Emperor seamount chain ⓘ
North Pacific Ocean ⓘ
movementHistory transported northwestward by Pacific Plate motion ⓘ
namedAfter Emperor Meiji of Japan ⓘ
linked to: Emperor Meiji
namedFor Meiji period of Japan ⓘ
linked to: Meiji era
ocean Pacific Ocean ⓘ
partOf Hawaiian–Emperor seamount chain ⓘ
region northwestern Pacific Ocean ⓘ
shape broad, flat-topped guyot ⓘ
significance records motion of the Pacific Plate over the Hawaiian hotspot ⓘ
studiedIn marine geology ⓘ
plate tectonics ⓘ
subsidenceProcess thermal subsidence of oceanic lithosphere ⓘ
summitDepth approximately 2000 meters below sea level ⓘ
summitEnvironment deep-sea environment ⓘ
tectonicPlate Pacific Plate ⓘ
usedFor reconstructing Pacific Plate motion ⓘ
volcanicActivityStatus extinct ⓘ
volcanicOrigin hotspot volcanism ⓘ

How these facts were elicited

Referenced by (3)

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