Acadian orogeny

E89371

The Acadian orogeny was a major Middle Paleozoic mountain-building event that significantly shaped the northern Appalachian Mountains through the collision of ancient landmasses.


Statements (47)
Predicate Object
instanceOf geological event
mountain-building event
orogeny
affects Canadian Appalachians
Gaspé Peninsula
Maritime Provinces of Canada
New England region
Newfoundland
northern Appalachian Mountains
causedBy closure of the Iapetus Ocean
collision of Avalonia with Laurentia
discoveredBy 19th-century geologists studying the Appalachians
endTime Devonian period NERFINISHED
approximately 360 million years ago
follows Taconic orogeny
hasEffectOn paleogeography of eastern North America
sedimentation patterns in the Appalachian Basin
hasPart Acadian climax phase
early Acadian phase
late Acadian phase
multiple deformation phases
locatedIn eastern North America
namedAfter Acadia
occursIn Middle Paleozoic
orogenAssociatedWith Avalonia
Laurentia
microcontinents of the northern Appalachians
partOf Appalachian orogeny
precedes Alleghanian orogeny
produces gneiss
granite plutons
schist
slate
relatedTo Caledonian orogeny
resultsIn Catskill Delta complex
development of a foreland basin
folding of sedimentary rocks
plutonism
regional metamorphism
thick clastic wedge deposits
thrust faulting
uplift of the northern Appalachians
startTime Devonian period NERFINISHED
approximately 420 million years ago
studiedIn Appalachian geology
structural geology
tectonics


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