Cascadian orogeny

E111529

The Cascadian orogeny is the long-lasting mountain-building episode responsible for forming the Cascade Range through subduction-related tectonic activity along western North America.

All labels observed (1)

Label Occurrences
Cascadian orogeny canonical 1

How this entity was disambiguated

Statements (47)

Predicate Object
instanceOf geological event
mountain-building episode
orogeny
affects Canada
Cascade Range
Pacific Northwest
surface form: Pacific Northwest region

United States of America
surface form: United States
associatedWith Cascadia Subduction Zone
surface form: Cascadia megathrust

Cascadia Subduction Zone
surface form: Cascadia subduction earthquakes
cause subduction of oceanic plates beneath North America
subduction of the Explorer Plate
subduction of the Farallon Plate (in the past)
subduction of the Gorda Plate
subduction of the Juan de Fuca Plate
drives arc volcanism from northern California to British Columbia
endTime ongoing
geologicalProvince Cascade Range
North American Cordillera
surface form: Pacific Northwest Cordillera
hasDuration long-lasting
hasEffect formation of the Cascade Range
uplift of the Cascade Range
volcanism in the Cascade Range
involves accretion of oceanic terranes
magmatic arc development
oceanic-continental plate convergence
locatedIn western North America
namedAfter Cascadia
surface form: Cascadia region
orogenyType continental-margin orogeny
subduction-related orogeny
partOf Cordilleran orogeny
produces andesitic to dacitic volcanism
continental arc magmatism
plutonic intrusions beneath the Cascade Range
relatedTo Cascade Volcanic Arc
surface form: Cascade volcanic arc

Cascadia Subduction Zone
surface form: Cascadia subduction zone

Explorer Plate
Gorda Plate
Juan de Fuca Plate
North American Plate
resultsIn crustal deformation in the Pacific Northwest
faulting and folding in western North America
regional metamorphism in the Cascade region
topographic relief of the Cascade Range
startTime Cenozoic
surface form: Cenozoic era

late Mesozoic to early Cenozoic (approximate)
tectonicProcess subduction
tectonicSetting convergent plate margin

How these facts were elicited

Referenced by (1)

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

Cascade Range orogeny Cascadian orogeny