Taconic volcanic arc

E413461

The Taconic volcanic arc was an ancient chain of volcanoes active along the eastern margin of ancestral North America during the Ordovician period, whose collision and accretion played a key role in building the early Appalachian Mountains.

All labels observed (1)

Label Occurrences
Taconic volcanic arc canonical 1

How this entity was disambiguated

Statements (46)

Predicate Object
instanceOf paleovolcanic arc ⓘ
volcanic arc ⓘ
approximateAgeMa 490–440 ⓘ
associatedWith arc-related plutonism in the Appalachian region ⓘ
high-pressure metamorphism in accretionary complexes ⓘ
subduction of Iapetus Ocean lithosphere ⓘ
collisionWith Laurentian continental margin ⓘ
contributedTo Appalachian Mountains ⓘ
geodynamicEnvironment migrating magmatic arc ⓘ
oceanic island arc ⓘ
geologicalPeriod Ordovician ⓘ
linked to: Ordovician Period
hasRockTypes metamorphosed volcanic rocks ⓘ
plutonic rocks ⓘ
volcanic rocks ⓘ
influenced foreland basin development along eastern Laurentia ⓘ
locatedOn eastern margin of Laurentia ⓘ
eastern margin of ancestral North America ⓘ
orogeny Taconic orogeny ⓘ
partOf Taconic orogeny ⓘ
precedes Acadian orogeny ⓘ
Alleghanian orogeny ⓘ
linked to: Appalachian orogeny
presentIn New England region ⓘ
New York region ⓘ
Newfoundland region ⓘ
Quebec region ⓘ
preservedAs arc-derived sedimentary sequences ⓘ
metavolcanic rocks ⓘ
produced andesitic volcanic rocks ⓘ
basaltic volcanic rocks ⓘ
volcanic island arc rocks ⓘ
volcaniclastic sediments ⓘ
relatedTectonicEvent thrusting and stacking of Appalachian terranes ⓘ
relatedTo closure of the Iapetus Ocean ⓘ
roleIn early construction of Appalachian Mountains ⓘ
significance key to understanding early Appalachian mountain building ⓘ
records early Paleozoic convergent margin magmatism along Laurentia ⓘ
studiedInDiscipline paleogeography ⓘ
stratigraphy ⓘ
tectonics ⓘ
successor later Appalachian orogenic events ⓘ
tectonicProcess accretion to Laurentia ⓘ
arc–continent collision ⓘ
tectonicSetting convergent plate margin ⓘ
timeSpan Early Ordovician ⓘ
Late Ordovician ⓘ
Middle Ordovician ⓘ

How these facts were elicited

Referenced by (1)

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

Taconic orogeny → associatedWith → Taconic volcanic arc ⓘ