Triple

T19206969
Position Surface form Disambiguated ID Type / Status
Subject Mount Callaghan E480258 entity
Predicate orogeny P946 FINISHED
Object Coast Mountains orogeny — NE NERFINISHED

Named-entity recognition

Before disambiguation, gpt-5-mini classified whether the object phrase is a named entity — the step behind the object's NE type shown above.

Instruction
Given a phrase, classify it is english named entity (e.g., persons, organizations, works of art) in Latin script, or not (e.g., literals, dates, URLs, verbose phrases). For disambiguation, the statement where the phrase occurs as object is also given. Please return a JSON object with `phrase` (string, the phrase being analyzed) and `is_ne` (boolean, indicating whether the phrase is a Named Entity).
Input
Phrase: Coast Mountains orogeny | Statement: [Mount Callaghan, orogeny, Coast Mountains orogeny]

Disambiguation candidates (2 decisions)

The exact options the model was shown at each disambiguation step, with the option it chose highlighted — the evidence behind this triple's disambiguated ids.

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.
  • 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
  • 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

Provenance (2 batches)

Stage Batch ID Job type Status
creating batch_69d8e8cb8c348190b52075823911c869 elicitation completed
NER batch_69e5f99d8ad0819098ebd4ee007149f1 ner completed
Created at: April 10, 2026, 1:19 p.m.