Cordilleran magmatic arc

E630492

The Cordilleran magmatic arc is a vast, long-lived chain of continental-margin volcanoes and intrusive igneous bodies that formed along the western edge of North America due to subduction-related tectonic activity.

All labels observed (1)

Label Occurrences
Cordilleran magmatic arc canonical 2

How this entity was disambiguated

Statements (49)

Predicate Object
instanceOf continental-margin volcanic arc
geologic province
magmatic arc
activityDuration long-lived
associatedMineralization gold deposits
molybdenum deposits
porphyry copper deposits
silver deposits
associatedSubductingPlate Farallon Plate
Juan de Fuca Plate
Kula Plate
associatedWith Cordilleran orogenic belt
North American Cordillera
mineral deposits
mountain building
regional metamorphism
cause subduction of oceanic plates beneath North America
continent North America
contributesTo crustal thickening of western North America
extendsThrough Alaska
Canada
Central America
Mexico
South America
United States
forms continental crustal growth features
geologicAge Cenozoic
Mesozoic
includes batholiths
dike swarms
intrusive igneous bodies
plutons
sill complexes
volcanic arcs of the North American Cordillera
volcanic edifices
lengthCharacteristic continental-scale
location western margin of North America
marginType continental margin
orientation north-south trending
orogenyType Cordilleran orogeny
researchField economic geology
igneous petrology
tectonics
rockType granitoid
igneous rock
plutonic rock
volcanic rock
tectonicProcess subduction
tectonicSetting convergent plate margin

How these facts were elicited

Referenced by (2)

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

Sierra Nevada batholith associatedWith Cordilleran magmatic arc
Sevier orogeny relatedTo Cordilleran magmatic arc