Charlie-Gibbs Fracture Zone

E3192

The Charlie-Gibbs Fracture Zone is a major deep-sea transform fault system in the North Atlantic Ocean that offsets and disrupts the continuity of the Mid-Atlantic Ridge.


Statements (41)
Predicate Object
instanceOf oceanic fracture zone
tectonic feature
transform fault system
disruptsContinuityOf Mid-Atlantic Ridge
geologicalProcess seafloor spreading
transform faulting
hasDepthCharacteristic abyssal depths
hasEnvironment deep-sea
hasFeature deep-sea topography
fracture zone valleys
transform faults
hasGeologicalAge Mesozoic to Cenozoic oceanic crust context
hasMorphology elongate, linear seafloor structure
steep escarpments and deep troughs
hasRelativeLocation between North America and Europe
north of the Azores region
hasRoleIn accommodating differential motion along the Mid-Atlantic Ridge
segmenting the spreading center of the Mid-Atlantic Ridge
hasScientificInterest oceanic crustal structure
plate kinematics
influences pattern of ridge segmentation in the Mid-Atlantic
regional bathymetry of the North Atlantic
isImportantFor understanding segmentation of mid-ocean ridges
understanding transform plate boundaries
isMappedOn bathymetric charts of the North Atlantic
isSubjectOf marine geophysical studies
plate tectonics research
isTraversedBy ocean currents of the North Atlantic
isTypeOf mid-ocean ridge fracture zone
liesOn oceanic crust of the North Atlantic plate boundary region
locatedIn North Atlantic Ocean
namedAfter RRS Charles Darwin and USNS Gibbs (commemorative naming origin)
oceanBasin Atlantic Ocean
offsets Mid-Atlantic Ridge
partOf Mid-Atlantic Ridge system
separates segments of the Mid-Atlantic Ridge
studiedUsing bathymetric mapping
magnetic anomaly data
seismic reflection and refraction surveys
tectonicSetting divergent plate boundary
oceanic lithosphere

Referenced by (3)
Subject (surface form when different) Predicate
RRS Charles Darwin
USNS Gibbs
associatedWith
Mid-Atlantic Ridge
segmentIncludes

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