Ouachita orogeny
E92147
The Ouachita orogeny was a major Paleozoic mountain-building event that formed the Ouachita Mountains of Arkansas, Oklahoma, and adjacent regions through the collision of ancient continental plates.
All labels observed (6)
| Label | Occurrences |
|---|---|
| Ouachita orogeny canonical | 4 |
| Ouachita Fold and Thrust Belt | 1 |
| Ouachita Uplift | 1 |
| Ouachita orogen | 1 |
| Ouachita orogenic belt | 1 |
| Ouachita structural front | 1 |
How this entity was disambiguated
This entity first appeared as the object of triple T738668 — resolving that mention is where its identity was fixed. The disambiguator weighed these candidate entities and picked the highlighted one (or “None”, minting a new entity). This is how homonymy is resolved: the same surface form can point to different entities.
Target entity: Ouachita orogeny Context triple: [Appalachian orogeny, hasPart, Ouachita orogeny]
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A.
Acadian orogeny
The Acadian orogeny was a major Middle Paleozoic mountain-building event that significantly shaped the northern Appalachian Mountains through the collision of ancient landmasses.
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B.
Appalachian orogeny
The Appalachian orogeny was a series of ancient mountain-building events that formed the Appalachian Mountains through the collision of tectonic plates during the Paleozoic Era.
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C.
Taconic orogeny
The Taconic orogeny was an early Paleozoic mountain-building event along the eastern margin of ancient North America that contributed significantly to the formation of the Appalachian Mountains.
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D.
Ouachita Mountains
The Ouachita Mountains are a rugged, forested mountain range in western Arkansas and southeastern Oklahoma known for their unique east–west orientation, rich biodiversity, and outdoor recreation opportunities.
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E.
Caledonian orogeny
The Caledonian orogeny was a major Paleozoic mountain-building event that formed ranges across what are now Scandinavia, Scotland, Ireland, Greenland, and parts of North America as ancient continents collided.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
Target entity: Ouachita orogeny Target entity description: The Ouachita orogeny was a major Paleozoic mountain-building event that formed the Ouachita Mountains of Arkansas, Oklahoma, and adjacent regions through the collision of ancient continental plates.
-
A.
Acadian orogeny
The Acadian orogeny was a major Middle Paleozoic mountain-building event that significantly shaped the northern Appalachian Mountains through the collision of ancient landmasses.
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B.
Appalachian orogeny
The Appalachian orogeny was a series of ancient mountain-building events that formed the Appalachian Mountains through the collision of tectonic plates during the Paleozoic Era.
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C.
Taconic orogeny
The Taconic orogeny was an early Paleozoic mountain-building event along the eastern margin of ancient North America that contributed significantly to the formation of the Appalachian Mountains.
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D.
Ouachita Mountains
The Ouachita Mountains are a rugged, forested mountain range in western Arkansas and southeastern Oklahoma known for their unique east–west orientation, rich biodiversity, and outdoor recreation opportunities.
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E.
Caledonian orogeny
The Caledonian orogeny was a major Paleozoic mountain-building event that formed ranges across what are now Scandinavia, Scotland, Ireland, Greenland, and parts of North America as ancient continents collided.
- F. None of above. chosen
Statements (42)
| Predicate | Object |
|---|---|
| instanceOf |
Paleozoic mountain-building event
ⓘ
orogeny ⓘ |
| affected |
Arkoma Basin
ⓘ
Ouachita orogeny self-linksurface differs ⓘ
surface form:
Ouachita Fold and Thrust Belt
|
| associatedWith |
development of foreland basins
ⓘ
hydrocarbon-bearing basins in the Arkoma region ⓘ |
| cause |
closure of the Rheic Ocean
ⓘ
collision of Laurentia with Gondwana-related continental blocks ⓘ |
| chronostratigraphicRange | Late Mississippian to Early Permian ⓘ |
| continent | North America ⓘ |
| deformed |
Paleozoic deep-marine sedimentary sequences
ⓘ
turbidite deposits ⓘ |
| formed | Ouachita Mountains ⓘ |
| geologicalAge | approximately 330–280 million years ago ⓘ |
| geologicalPeriod |
Late Paleozoic
ⓘ
Mississippian ⓘ Pennsylvanian ⓘ |
| locatedIn | southern margin of Laurentia ⓘ |
| namedAfter | Ouachita Mountains ⓘ |
| occurredIn |
Arkansas
ⓘ
Oklahoma ⓘ Texas ⓘ adjacent regions of the southern United States ⓘ southeastern Oklahoma ⓘ western Arkansas ⓘ |
| orogenyType | collisional orogeny ⓘ |
| overlapsWith | Appalachian–Ouachita–Marathon orogenic system ⓘ |
| partOf | assembly of Pangea ⓘ |
| plateInvolved |
Gondwana-derived terranes
ⓘ
Laurentia ⓘ |
| precededBy | subsidence of a passive continental margin along southern Laurentia ⓘ |
| region | south-central United States ⓘ |
| relatedTo |
Appalachian orogeny
ⓘ
surface form:
Alleghanian orogeny
Appalachian orogeny ⓘ Marathon orogeny ⓘ |
| result |
crustal shortening
ⓘ
folding of sedimentary rocks ⓘ thrust faulting ⓘ uplift of the Ouachita Mountains ⓘ |
| significance | records late Paleozoic continental collision along the southern margin of North America ⓘ |
| structuralStyle | thin-skinned fold-and-thrust belt ⓘ |
| tectonicSetting | convergent plate margin ⓘ |
How these facts were elicited
The pipeline generated the facts above by prompting gpt-5.1 with this entity's name + description and the instruction below.
You are a knowledge base construction expert. Given a subject entity and a description of it, return factual statements that you know for the subject as a JSON list of dictionaries(triples), where keys must be "subject", "predicate" and "object". The number of facts may be very high, between 25 to 50 or more, for very popular subjects. For less popular subjects, the number of facts can be very low, like 5 or 10. # Requirements - If you don't know the subject at all, return an empty list. - If the subject is not a named entity, return an empty list. - Include at least one triple where predicate is "instanceOf". - Do not get too wordy. - Separate several objects into multiple triples with one object.
Subject: Ouachita orogeny Description of subject: The Ouachita orogeny was a major Paleozoic mountain-building event that formed the Ouachita Mountains of Arkansas, Oklahoma, and adjacent regions through the collision of ancient continental plates.
Referenced by (9)
Full triples — surface form annotated when it differs from this entity's canonical label.