St. Elias orogeny
E1157126
UNEXPLORED
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.
All labels observed (1)
| Label | Occurrences |
|---|---|
| St. Elias orogeny canonical | 1 |
How this entity was disambiguated
This entity first appeared as the object of triple T15447259 — 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: St. Elias orogeny Context triple: [Saint Elias Mountains, orogeny, St. Elias orogeny]
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A.
Sevier orogeny
The Sevier orogeny was a major Mesozoic mountain-building event in western North America that produced extensive thrust faulting and deformation along the continental margin.
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B.
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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C.
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.
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D.
Innuitian orogeny
The Innuitian orogeny was a major mountain-building event that formed much of the Arctic Cordillera in the Canadian High Arctic during the Paleozoic era.
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E.
Damara orogeny
The Damara orogeny was a major Neoproterozoic–early Paleozoic mountain-building event in present-day Namibia associated with the assembly of the Gondwana supercontinent.
- 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: St. Elias orogeny Target entity description: 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.
-
A.
Sevier orogeny
The Sevier orogeny was a major Mesozoic mountain-building event in western North America that produced extensive thrust faulting and deformation along the continental margin.
-
B.
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.
-
C.
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.
-
D.
Innuitian orogeny
The Innuitian orogeny was a major mountain-building event that formed much of the Arctic Cordillera in the Canadian High Arctic during the Paleozoic era.
-
E.
Damara orogeny
The Damara orogeny was a major Neoproterozoic–early Paleozoic mountain-building event in present-day Namibia associated with the assembly of the Gondwana supercontinent.
- F. None of above. chosen
Referenced by (1)
Full triples — surface form annotated when it differs from this entity's canonical label.