Avalonia microcontinent

E89372

Avalonia microcontinent was a small ancient landmass that rifted from Gondwana and later collided with Laurentia and Baltica, contributing to the formation of parts of modern North America and Western Europe.

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All labels observed (3)

Statements (48)

Predicate Object
instanceOf ancient landmass
microcontinent
activeDuringPeriod Early Paleozoic
Late Neoproterozoic
alsoKnownAs Avalonia
boundedBy major Paleozoic sutures
collidedWith Baltica
Laurentia
collisionClosedOcean Iapetus Ocean
collisionEventAgeApproximate around 430–400 million years ago
containsRockAges Cambrian
Neoproterozoic
Ordovician
Silurian
contributedToFormationOf parts of Western Europe
parts of modern North America
hostedMagmatismType arc-related magmatism
calc-alkaline volcanism
importantFor reconstruction of Paleozoic plate motions
understanding formation of Appalachian–Caledonian mountain belt
involvedInOrogeny Acadian orogeny
Caledonian orogeny
Variscan orogeny
laterPartOf Euramerica
Laurussia
locatedInGeologicPast Southern Hemisphere
movementDirectionAfterRifting northward
paleogeographicAffinity peri-Gondwanan terrane
partOfSupercontinentCycle assembly of Laurussia
presentDayRemnantsFoundIn Belgium
Netherlands
New Brunswick
island of Newfoundland
surface form: Newfoundland

Nova Scotia
Poland
eastern North America
northern France
northern Germany
southern Ireland
southwestern Britain
riftedFrom Gondwana
riftEventAgeApproximate around 600–550 million years ago
separatedFrom Gondwana
surface form: Gondwana margin
studiedInDiscipline paleogeography
stratigraphy
tectonics
subductedOceanBetween Iapetus Ocean
tectonicSettingDuringRift passive margin of Gondwana

Referenced by (4)

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

Appalachian orogeny involvesPlate Avalonia microcontinent
Baltica hasTectonicHistory Avalonia microcontinent
this entity surface form: collided with Laurentia
Avalonia contains Avalonia microcontinent
this entity surface form: Avalon terrane
Gaskiers glaciation evidenceFoundIn Avalonia microcontinent
this entity surface form: Avalon terrane