Iceland continental slope

E1026846

The Iceland continental slope is the steep underwater margin off Iceland’s coast that channels dense overflow waters from the Denmark Strait into the deep North Atlantic.

All labels observed (1)

Label Occurrences
Iceland continental slope canonical 1

How this entity was disambiguated

Statements (45)

Predicate Object
instanceOf continental slope ⓘ
submarine geomorphological feature ⓘ
adjacentTo Iceland Basin ⓘ
Iceland shelf ⓘ
affects distribution of cold dense water along western subpolar North Atlantic boundary ⓘ
stratification of subpolar North Atlantic ⓘ
associatedWithCurrent Denmark Strait Overflow Water (DSOW) ⓘ
deep boundary current along Greenland–Scotland Ridge outflow path ⓘ
boundedBy Denmark Strait region to the northwest ⓘ
Iceland–Faroe Ridge region to the southeast ⓘ
channelsWaterMass dense overflow waters from Denmark Strait ⓘ
conveysWaterTo deep North Atlantic ⓘ
hasApproximateDepthRange from continental shelf break (~200–500 m) to abyssal depths (>2000 m) ⓘ
hasClimateRelevance component of high-latitude control on global thermohaline circulation ⓘ
indicator of past changes in Nordic Seas overflow strength ⓘ
hasImportance important control on structure of North Atlantic Deep Water ⓘ
key gateway for export of dense Nordic Seas waters ⓘ
hasMorphology incised by channels and gullies in places ⓘ
steep submarine slope ⓘ
hasProcess entrainment of surrounding North Atlantic waters ⓘ
gravity-driven downslope flow of dense water ⓘ
turbulent mixing of overflow waters with ambient water masses ⓘ
hasRole conduit for dense water from Nordic Seas to North Atlantic ⓘ
hasSeafloorFeature contourite deposits ⓘ
sediment drifts formed by contour currents ⓘ
submarine channels guiding overflow plumes ⓘ
hasSedimentSource downslope transport from Iceland shelf ⓘ
overflow-related contour currents ⓘ
influences deep water mass distribution in the North Atlantic ⓘ
ventilation of the deep North Atlantic ⓘ
locatedIn North Atlantic Ocean ⓘ
linked to: North Atlantic
locatedOffCoastOf Iceland ⓘ
partOf North Atlantic basin margin ⓘ
pathway of the Atlantic Meridional Overturning Circulation ⓘ
receivesOverflowFrom Denmark Strait overflow waters ⓘ
relatedTo Denmark Strait sill ⓘ
linked to: Denmark Strait

Greenland–Scotland Ridge overflow system ⓘ
Iceland Basin deep circulation ⓘ
Irminger Sea ⓘ
studiedInDiscipline marine geology ⓘ
paleoceanography ⓘ
physical oceanography ⓘ
subjectOf hydrographic surveys of Denmark Strait overflow plume ⓘ
moored current meter observations of deep boundary currents ⓘ
seismic and multibeam mapping of slope morphology ⓘ

How these facts were elicited

Referenced by (1)

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

Denmark Strait overflow pathway → flowsAlong → Iceland continental slope ⓘ