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 ⓘ