Blanco Transform

E360800

The Blanco Transform is a major right-lateral transform fault segment of the plate boundary between the Juan de Fuca and Pacific Plates off the coast of the Pacific Northwest.

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All labels observed (1)

Label Occurrences
Blanco Transform canonical 1

Statements (31)

Predicate Object
instanceOf plate boundary segment
transform fault
associatedWith Cascadia subduction zone
Gorda Ridge
Juan de Fuca Ridge
connectsTo Cascadia Subduction Zone
surface form: Cascadia subduction zone

Gorda Ridge
Juan de Fuca Ridge
countryOffshoreFrom United States of America
surface form: United States
displacementType horizontal
hazardType seismic
isSubparallelTo Blanco Fracture Zone
locatedIn eastern North Pacific Ocean
surface form: northeast Pacific Ocean
marginType active continental margin
motionSense dextral
namedAfter Blanco Fracture Zone
ocean Pacific Ocean
partOf Juan de Fuca Ridge
surface form: Juan de Fuca–Pacific plate boundary
plateBoundaryBetween Juan de Fuca Plate
Pacific Plate
plateBoundaryType transform
region off the coast of Oregon
off the coast of northern California
relativeMotionType right-lateral strike-slip
seafloorFeatureType fracture zone
tectonicEnvironment oceanic-oceanic plate boundary
tectonicPlate1 Juan de Fuca Plate
tectonicPlate2 Pacific Plate
tectonicRole accommodates differential motion between Juan de Fuca and Pacific Plates
links spreading centers and subduction zone in Cascadia region
tectonicSetting offshore Pacific Northwest

Referenced by (1)

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

Blanco Fracture Zone namedAfter Blanco Transform