Coast Mountains orogeny
E1364293
UNEXPLORED
The Coast Mountains orogeny is a major mountain-building event that formed much of the Coast Mountains along the western margin of North America through prolonged subduction, magmatism, and crustal deformation.
All labels observed (1)
| Label | Occurrences |
|---|---|
| Coast Mountains orogeny canonical | 1 |
How this entity was disambiguated
This entity first appeared as the object of triple T19206969 — 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.
NED1
Entity disambiguation (via context triple)
gpt-5-mini-2025-08-07
Target entity: Coast Mountains orogeny Context triple: [Mount Callaghan, orogeny, Coast Mountains orogeny]
-
A.
Cascadian orogeny
The Cascadian orogeny is the long-lasting mountain-building episode responsible for forming the Cascade Range through subduction-related tectonic activity along western North America.
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B.
St. Elias orogeny
The St. Elias orogeny is a mountain-building event responsible for the rapid uplift and complex tectonic deformation of the Saint Elias Mountains in the coastal region of Alaska and Yukon.
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C.
Cordilleran orogeny
The Cordilleran orogeny was a long-lasting mountain-building event along western North America that created much of the modern Cordillera, including ranges such as the Rockies and the Peninsular Ranges.
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D.
Coast Ranges orogeny
The Coast Ranges orogeny is a mountain-building episode that formed much of California’s Coast Ranges through complex interactions along the western margin of the North American Plate.
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E.
Pinwarian orogeny
The Pinwarian orogeny was a Precambrian mountain-building event recorded in the Canadian Shield that predates and helped set the tectonic framework for the later Grenville orogeny.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
NED2
Entity disambiguation (via description)
gpt-5-mini-2025-08-07
Target entity: Coast Mountains orogeny Target entity description: The Coast Mountains orogeny is a major mountain-building event that formed much of the Coast Mountains along the western margin of North America through prolonged subduction, magmatism, and crustal deformation.
-
A.
Cascadian orogeny
The Cascadian orogeny is the long-lasting mountain-building episode responsible for forming the Cascade Range through subduction-related tectonic activity along western North America.
-
B.
St. Elias orogeny
The St. Elias orogeny is a mountain-building event responsible for the rapid uplift and complex tectonic deformation of the Saint Elias Mountains in the coastal region of Alaska and Yukon.
-
C.
Cordilleran orogeny
The Cordilleran orogeny was a long-lasting mountain-building event along western North America that created much of the modern Cordillera, including ranges such as the Rockies and the Peninsular Ranges.
-
D.
Coast Ranges orogeny
The Coast Ranges orogeny is a mountain-building episode that formed much of California’s Coast Ranges through complex interactions along the western margin of the North American Plate.
-
E.
Pinwarian orogeny
The Pinwarian orogeny was a Precambrian mountain-building event recorded in the Canadian Shield that predates and helped set the tectonic framework for the later Grenville orogeny.
- F. None of above. chosen
Referenced by (1)
Full triples — surface form annotated when it differs from this entity's canonical label.