Greenland continental slope

E1024588

The Greenland continental slope is the steep underwater margin off Greenland’s coast that channels dense overflow waters from the Nordic Seas into the deep North Atlantic.

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Statements (45)

Predicate Object
instanceOf continental slope
submarine landform
adjacentTo Denmark Strait NERFINISHED
Greenland Sea NERFINISHED
Irminger Sea NERFINISHED
borders Greenland abyssal plain NERFINISHED
Greenland continental shelf NERFINISHED
composedOf glacial-marine sediments
connectedTo Iceland continental slope via Denmark Strait region
contributesTo formation of North Atlantic Deep Water
depthRange from shelf break to abyssal plain depths
extendsAlong eastern Greenland margin
southeastern Greenland margin
southwestern Greenland margin
hasClimateRelevance affects heat and freshwater redistribution
controls deep ocean ventilation in North Atlantic
hasEcologicalRole habitat for deep-sea benthic communities
pathway for nutrient transport
hasFeature channel-levee systems
sediment drifts
submarine canyons
hasFunction conduit for dense overflow waters
hasGeomorphologicalCharacteristic steep gradient
hasHydrographicCharacteristic cold and saline bottom waters
strong along-slope currents
hasProcess contour current erosion
gravity-driven downslope flow
turbidity currents
hasResearchInterest overflow plume dynamics
response to climate variability
sediment transport and deposition
influencedBy Greenland boundary current
glacial processes
sea-ice conditions
locatedIn North Atlantic Ocean NERFINISHED
locatedOffCoastOf Greenland NERFINISHED
partOf Greenland margin
North Atlantic continental margin NERFINISHED
partOfProcess Atlantic Meridional Overturning Circulation NERFINISHED
studiedInDiscipline marine geology
paleoceanography
physical oceanography
transportsWaterMass Denmark Strait overflow water
Iceland–Scotland overflow water
Nordic Seas overflow water

Referenced by (1)

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

Denmark Strait overflow pathway flowsAlong Greenland continental slope