Romanche transform fault

E270105

The Romanche transform fault is a major east–west striking fracture zone and transform fault in the equatorial Atlantic Ocean that offsets the Mid-Atlantic Ridge and hosts one of the deepest points in the Atlantic.

All labels observed (1)

Label Occurrences
Romanche transform fault canonical 1

How this entity was disambiguated

Statements (30)

Predicate Object
instanceOf geologic structure
oceanic fracture zone
transform fault
bathymetricExpression deep oceanic trench
displacementType strike-slip
featureType fracture zone
transform plate boundary
geologicalProcess sea-floor spreading accommodation
hasGeologicalAge Mesozoic–Cenozoic activity
hasMaximumDepth over 24000 ft
over 7600 m
hasPart Romanche Trench
hosts one of the deepest points in the Atlantic Ocean
isInRegion equatorial Atlantic
isMajorStructureIn Central Atlantic Ocean floor
surface form: Atlantic Ocean floor
isPartOf Mid-Atlantic Ridge
surface form: Mid-Atlantic Ridge system
isStudiedInDiscipline marine geology
plate tectonics
locatedIn equatorial Atlantic Ocean
namedAfter Romanche (French survey vessel)
ocean Atlantic Ocean
offsets Mid-Atlantic Ridge
orientation approximately east–west
plateBoundaryBetween African Plate
South American Plate
relativeLocation near the Equator
separates northern Mid-Atlantic Ridge segment
southern Mid-Atlantic Ridge segment
strikes east–west
tectonicSetting mid-ocean ridge system

How these facts were elicited

Referenced by (1)

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

Romanche Trench liesOn Romanche transform fault