Beaufort continental slope

E74746

The Beaufort continental slope is the steep underwater margin of the Beaufort Sea’s continental shelf that descends into the deep Canada Basin of the Arctic Ocean.

All labels observed (1)

Label Occurrences
Beaufort continental slope canonical 1

How this entity was disambiguated

Statements (42)

Predicate Object
instanceOf continental slope
submarine landform
adjacentTo Beaufort Sea
surface form: Beaufort Sea continental shelf
associatedWith Arctic sea ice cover
Beaufort Gyre
descendsInto Canada Basin
environmentType deep marine environment
polar marine environment
formsBoundaryBetween continental shelf and abyssal plain in the Beaufort Sea
hasFeature mass-transport deposits
sediment drifts
submarine canyons
hasGeologicalSetting passive continental margin
hasMorphology steep underwater margin
hasProcess sediment transport
slope failure
turbidity currents
hasRelevanceFor Arctic climate studies
hydrocarbon exploration
slope hazard assessment
subsea infrastructure stability
hasSubstrate glaciomarine sediments
marine sediments
influences deep-water circulation in the Beaufort Sea
sediment deposition in Canada Basin
isMappedBy bathymetric surveys
multibeam sonar
seismic reflection profiling
isPartOf Amerasian Basin
surface form: Amerasian Basin margins
isSubjectOf Arctic Ocean bathymetric charts
marine geological surveys in the Beaufort Sea
locatedIn Arctic Ocean
Beaufort Sea
locatedInRegion Arctic Ocean
surface form: western Arctic Ocean
locatedOffCoastOf Alaska
northern Canada
partOf Arctic Ocean seafloor
Canada Basin
separates Beaufort Sea
surface form: Beaufort Sea continental shelf

deep Canada Basin
studiedInDiscipline marine geology
oceanography

How these facts were elicited

Referenced by (1)

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

Canada Basin hasSeafloorBoundary Beaufort continental slope