North Atlantic seabed

E750617

The North Atlantic seabed is the deep ocean floor in the North Atlantic Ocean, known for its cold, high-pressure environment and for hosting famous shipwrecks such as the RMS Titanic.

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Statements (51)

Predicate Object
instanceOf marine geographic region
seabed
borderedBy eastern coast of North America
western coast of Europe
western coast of North Africa
contains RMS Lusitania wreck site NERFINISHED
RMS Titanic wreck site NERFINISHED
SS Andrea Doria wreck site
numerous World War I shipwrecks
numerous World War II shipwrecks
transatlantic cable routes
hasAverageTemperature near 0 to 4 degrees Celsius
hasClimate cold
hasDepthRange from continental shelf edge to over 6000 meters
hasDepthZone abyssal zone
bathyal zone
hadal zone
hasEcosystem deep-sea benthic community
hasEnvironment deep ocean
hasFeature Mid-Atlantic Ridge NERFINISHED
abyssal plain
continental rise
continental slope
fracture zone
mid-ocean ridge
seamount
sediment-covered basin
submarine canyon
hasHazard cable damage risk from turbidity currents
submarine landslides
hasPressure tens to hundreds of atmospheres
hasProcess plate tectonics
seafloor spreading at Mid-Atlantic Ridge
sediment deposition
hasProperty aphotic zone
high hydrostatic pressure
low light levels
low temperature
hasResourcePotential hydrocarbon deposits in some margins
polymetallic nodules
inhabitedBy benthic invertebrates
chemosynthetic microorganisms
deep-sea fish
locatedIn North Atlantic Ocean NERFINISHED
partOf Atlantic Ocean floor
regulatedBy United Nations Convention on the Law of the Sea NERFINISHED
studiedBy marine biologists
marine geologists
physical oceanographers
usedFor scientific oceanographic research
submarine telecommunications cables

Referenced by (1)

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

Return to Titanic narrativeLocation North Atlantic seabed