Aleutian Basin

E77184

The Aleutian Basin is a deep, sediment-filled oceanic basin in the western Bering Sea, bordered by the Aleutian Island arc and characterized by its complex tectonic and volcanic history.

All labels observed (2)

Label Occurrences
Aleutian Basin canonical 4
Bering Sea abyssal plain 1

How this entity was disambiguated

Statements (37)

Predicate Object
instanceOf geologic region
oceanic basin
associatedWith Aleutian Trench
Aleutian subduction zone
borderedBy Aleutian Island arc
linked to: Aleutian Arc

Aleutian Islands
Kamchatka Peninsula
countryOffshoreFrom Russia
United States
formedBy plate tectonics
geologicalAge Mesozoic-Cenozoic
hasBoundaryType continental margin
island arc margin
hasGeologicalCharacteristic complex tectonic history
deep
oceanic crust
sediment-filled
volcanic history
hasMorphology abyssal plain-like floor
hasNearbyFeature Aleutian Ridge
linked to: Aleutian Trench

Bowers Ridge
hasProcess sediment accumulation
subduction-related volcanism
hasSedimentType marine sediments
pelagic sediments
terrigenous sediments
influences Bering Sea circulation
Bering Sea sedimentation patterns
isSubjectOf geophysical surveys
marine geological research
locatedIn Bering Sea
western Bering Sea
linked to: Bering Sea
oceanRegion North Pacific
partOf North Pacific Ocean
linked to: Pacific Ocean
seafloorProvinceOf Bering Sea
tectonicSetting convergent margin
underlies western Bering Sea
linked to: Bering Sea

How these facts were elicited

Referenced by (5)

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

Bering Sea hasFeature Aleutian Basin
Navarin Canyon nearbyFeature Aleutian Basin
Bowers Ridge formsBoundaryWith Aleutian Basin
Bering Sea canyon system extendsTo Bering Sea abyssal plain
linked to: Aleutian Basin
Bowers Basin separatedFrom Aleutian Basin