Suiko Seamount
E125547
Suiko Seamount is an underwater volcanic mountain in the northwestern Pacific Ocean that forms part of the long, age-progressive Hawaiian–Emperor seamount chain.
All labels observed (1)
| Label | Occurrences |
|---|---|
| Suiko Seamount canonical | 4 |
Statements (35)
| Predicate | Object |
|---|---|
| instanceOf |
seamount
ⓘ
underwater volcanic mountain ⓘ |
| formedBy |
Hawaiian hotspot
ⓘ
volcanic activity ⓘ |
| hasAge |
Cretaceous
ⓘ
approximately 65–70 million years ⓘ |
| hasBiologicalContext | deep-sea benthic habitat ⓘ |
| hasCrustalContext | oceanic crust ⓘ |
| hasDiscoveryMethod | bathymetric survey ⓘ |
| hasEruptionStatus | extinct volcano ⓘ |
| hasGeologicalCharacteristic | guyot ⓘ |
| hasImportance | key constraint on hotspot drift hypotheses ⓘ |
| hasLatitude | approximately 44 degrees north ⓘ |
| hasLongitude | approximately 170 degrees east ⓘ |
| hasMorphology |
large volcanic edifice
ⓘ
steep flanks ⓘ |
| hasNameOrigin | named after Empress Suiko of Japan ⓘ |
| hasRelationTo |
Emperor Trough
ⓘ
Hawaiian–Emperor seamount chain ⓘ
surface form:
Hawaiian Ridge
|
| hasResearchUse |
ocean drilling studies
ⓘ
paleomagnetic studies ⓘ study of Pacific Plate motion ⓘ study of hotspot motion ⓘ |
| hasSedimentCover | pelagic sediments ⓘ |
| hasSummitDepth | approximately 1400 meters below sea level ⓘ |
| hasSummitFeature | eroded volcanic surface ⓘ |
| hasSummitShape | flat-topped ⓘ |
| hasTectonicSetting | intraplate volcano ⓘ |
| isIncludedIn | Hawaiian–Emperor Bend studies ⓘ |
| isOlderThan | Midway Seamount ⓘ |
| isYoungerThan | Yomei Seamount ⓘ |
| locatedIn |
Northwestern Pacific Ocean
ⓘ
surface form:
northwestern Pacific Ocean
|
| locatedOn | Pacific Plate ⓘ |
| partOf |
Emperor seamounts
ⓘ
Hawaiian–Emperor seamount chain ⓘ |
Referenced by (4)
Full triples — surface form annotated when it differs from this entity's canonical label.