Irish Caledonides
E842648
The Irish Caledonides are a mountain belt in Ireland formed during the Caledonian orogeny, representing deformed and metamorphosed remnants of ancient oceanic and continental crust.
All labels observed (1)
| Label | Occurrences |
|---|---|
| Irish Caledonides canonical | 1 |
How this entity was disambiguated
This entity first appeared as the object of triple T10123373 — 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: Irish Caledonides Context triple: [Iapetus Ocean, marginPreservedIn, Irish Caledonides]
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A.
British Caledonides
The British Caledonides are an ancient mountain belt in the British Isles formed during the Caledonian orogeny, representing the deformed and metamorphosed remains of early Paleozoic ocean closure and continental collision.
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B.
Scandinavian Caledonides
The Scandinavian Caledonides are a major Paleozoic mountain belt in Scandinavia formed by the collision of ancient continental plates during the Caledonian orogeny.
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C.
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.
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D.
Dalradian Supergroup
The Dalradian Supergroup is a thick sequence of late Precambrian to early Paleozoic metamorphic sedimentary and volcanic rocks extensively exposed in the Scottish Highlands and parts of Ireland.
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E.
Grampian Terrane
The Grampian Terrane is a major geological block in Scotland characterized by ancient metamorphic and igneous rocks that form much of the Grampian Highlands.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
Target entity: Irish Caledonides Target entity description: The Irish Caledonides are a mountain belt in Ireland formed during the Caledonian orogeny, representing deformed and metamorphosed remnants of ancient oceanic and continental crust.
-
A.
British Caledonides
The British Caledonides are an ancient mountain belt in the British Isles formed during the Caledonian orogeny, representing the deformed and metamorphosed remains of early Paleozoic ocean closure and continental collision.
-
B.
Scandinavian Caledonides
The Scandinavian Caledonides are a major Paleozoic mountain belt in Scandinavia formed by the collision of ancient continental plates during the Caledonian orogeny.
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C.
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.
-
D.
Dalradian Supergroup
The Dalradian Supergroup is a thick sequence of late Precambrian to early Paleozoic metamorphic sedimentary and volcanic rocks extensively exposed in the Scottish Highlands and parts of Ireland.
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E.
Grampian Terrane
The Grampian Terrane is a major geological block in Scotland characterized by ancient metamorphic and igneous rocks that form much of the Grampian Highlands.
- F. None of above. chosen
Statements (43)
| Predicate | Object |
|---|---|
| instanceOf | mountain belt ⓘ |
| ageRange |
Ordovician
ⓘ
Silurian ⓘ |
| contains |
ancient continental crust remnants
ⓘ
ancient oceanic crust remnants ⓘ deformed crust ⓘ metamorphosed crust ⓘ |
| exposedIn |
northwest Ireland
ⓘ
western Ireland NERFINISHED ⓘ |
| extendsInto |
Greenland
NERFINISHED
ⓘ
Scandinavia NERFINISHED ⓘ Scotland NERFINISHED ⓘ |
| formedBy |
continental collision
ⓘ
crustal thickening ⓘ subduction ⓘ |
| formedDuring | Caledonian orogeny NERFINISHED ⓘ |
| geologicalAge | Paleozoic ⓘ |
| hasEconomicInterest | mineral exploration ⓘ |
| hasEvidenceFor | closure of the Iapetus Ocean ⓘ |
| hasMetamorphicGrade |
high-grade metamorphism
ⓘ
low-grade metamorphism ⓘ medium-grade metamorphism ⓘ |
| hasProcess |
faulting
ⓘ
folding ⓘ regional metamorphism ⓘ |
| hasRockType |
igneous rocks
ⓘ
metamorphic rocks ⓘ sedimentary rocks ⓘ |
| hasStructure |
fold belts
ⓘ
thrust belts ⓘ |
| isRemnantOf | ancient mountain chain ⓘ |
| locatedIn | Ireland NERFINISHED ⓘ |
| orogenyType | collisional orogeny ⓘ |
| overlainBy | younger sedimentary basins in Ireland ⓘ |
| partOf |
Caledonides
NERFINISHED
ⓘ
North Atlantic Caledonides NERFINISHED ⓘ |
| relatedTo |
Appalachian–Caledonian orogen
NERFINISHED
ⓘ
Iapetus Ocean NERFINISHED ⓘ |
| significantFor | Paleozoic tectonic evolution of Ireland ⓘ |
| studiedInDiscipline |
metamorphic petrology
ⓘ
structural geology ⓘ tectonics ⓘ |
| 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: Irish Caledonides Description of subject: The Irish Caledonides are a mountain belt in Ireland formed during the Caledonian orogeny, representing deformed and metamorphosed remnants of ancient oceanic and continental crust.
Referenced by (1)
Full triples — surface form annotated when it differs from this entity's canonical label.