Tongue of the Ocean margins

E659342

Tongue of the Ocean margins are the steep submarine slopes and transition zones that border the deep Tongue of the Ocean basin within the Bahamian archipelago.

Try in SPARQL Jump to: Statements Referenced by

Statements (44)

Predicate Object
instanceOf continental margin analogue
marine geomorphological feature
submarine slope
adjacentTo deep Tongue of the Ocean basin
shallow Bahamian banks
associatedWith carbonate slope failures
contourite deposits
mass-transport deposits
submarine canyons
turbidite systems
border Great Bahama Bank NERFINISHED
Little Bahama Bank NERFINISHED
Tongue of the Ocean basin NERFINISHED
characterizedBy sharp bathymetric gradients
steep submarine slopes
transition from shallow carbonate platform to deep basin
composedOf carbonate sediments
platform-derived debris
environmentType marine environment
slope environment
formedBy carbonate platform margin progradation
erosional processes
fault-controlled subsidence
geologicalAge Cenozoic
hasBathymetry steep slope from hundreds to thousands of meters water depth
hasFunction boundary between shallow-water banks and deep basin
sediment transfer pathway from platform to basin
hasRelevanceTo carbonate platform evolution models
petroleum system analysis in carbonate margins
submarine slope stability studies
influencedBy gravity-driven sediment transport
ocean currents
sea-level fluctuations
locatedIn Atlantic Ocean
Bahamian archipelago NERFINISHED
Tongue of the Ocean NERFINISHED
overlie older carbonate platform strata
partOf Bahamas platform NERFINISHED
studiedFor carbonate slope processes
oceanographic circulation effects on slope sedimentation
sequence stratigraphy of carbonate margins
submarine landslide hazards
tectonicSetting intra-platform basin setting
passive margin setting

Referenced by (1)

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

Bahamas Platform underlies Tongue of the Ocean margins