Cascadia Subduction Zone

E15671

The Cascadia Subduction Zone is a major convergent plate boundary off the Pacific Northwest coast of North America, capable of generating powerful megathrust earthquakes and tsunamis.


Statements (54)
Predicate Object
instanceOf convergent plate boundary
megathrust fault
subduction zone
affectsRegion British Columbia
Northern California
Oregon
Pacific Northwest
Washington State
associatedWith Cascadia earthquake hazard
Cascadia tsunami hazard
Ring of Fire
averageRecurrenceInterval approximately 500 years
earthquakeType megathrust earthquake
extendsFrom Northern Vancouver Island
extendsTo Cape Mendocino
hazardType coastal subsidence
liquefaction
strong ground shaking
tsunami
knownFor potential for large megathrust earthquakes
potential for large tsunamis
lastKnownGreatEarthquakeDate January 26, 1700
lastKnownGreatEarthquakeGenerated trans-Pacific tsunami
lastKnownGreatEarthquakeMagnitude approximately 9.0
length approximately 1000 kilometers
locatedIn Pacific Ocean
locatedOffCoastOf British Columbia
North America
Northern California
Oregon
Pacific Northwest
Washington
maximumEstimatedMagnitude 9.0
paleoseismologyEvidenceFoundIn coastal marshes
offshore turbidites
plateMotionType oblique convergence
recurrenceIntervalEstimate approximately 300 to 600 years
riskTo Coastal communities of British Columbia
Coastal communities of Northern California
Coastal communities of Oregon
Coastal communities of Washington
Portland, Oregon
Seattle
Vancouver, British Columbia
Victoria, British Columbia
seismogenicZoneWidth approximately 60 to 80 kilometers
slipType thrust faulting
studiedBy Geological Survey of Canada
United States Geological Survey
tectonicPlateOverriding North American Plate
tectonicPlateSubducting Explorer Plate
Gorda Plate
Juan de Fuca Plate
tsunamiRecordedIn Japan

Referenced by (24)
Subject (surface form when different) Predicate
Blanco Fracture Zone ("Cascadia subduction zone")
Gorda Plate ("Cascadia megathrust")
North Coast Ranges ("Cascadia subduction zone region")
associatedWith
Explorer Ridge ("Cascadia subduction zone")
Mendocino Fracture Zone
near
Explorer Plate ("Cascadia subduction zone")
Juan de Fuca Plate
subductionZoneName
Explorer Plate ("Cascadia forearc")
adjacentTo
North American Plate ("Cascadia subduction zone")
boundaryFeature
Queen Charlotte Fault
connectedTo
Gorda Plate ("Cascadia subduction zone")
formsPartOf
Gorda Ridge ("Cascadia subduction zone region")
geologicalProvince
Mount Mazama ("Cascadia subduction zone")
geologicalSetting
Pacific coast of North America ("Cascadia subduction zone")
hasNotableFeature
North American plate boundary system ("Cascadia subduction zone")
hasPart
eastern Pacific Ocean ("Cascadia subduction zone")
hasSubductionZone
Blanco Fracture Zone ("Juan de Fuca–Pacific plate boundary system")
isPartOf
Canada West Coast ("Cascadia subduction zone")
locatedOnTectonicPlateBoundary
Gorda Ridge ("Cascadia megathrust region")
nearbyHazardContext
Cascadia ("Cascadia subduction zone region")
overlapsWith
Juan de Fuca Ridge ("Cascadia subduction system back-arc")
region
Gorda Plate ("Cascadia subduction zone")
subductsAt
Mount Meager massif ("Cascadia subduction zone")
tectonicSetting
Crescent City, California
tsunamiSourceRegion

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