Triple

T18365576
Position Surface form Disambiguated ID Type / Status
Subject Pyrenean foothills karst system E440035 entity
Predicate associatedWith P37 FINISHED
Object Pyrenean orogeny
The Pyrenean orogeny was the major mountain-building event that created the Pyrenees through the collision of the Iberian and Eurasian tectonic plates during the Late Cretaceous to early Cenozoic.
E1320852 NE FINISHED

How this triple was built (4 steps)

Every LLM step that produced this triple, in pipeline order — named-entity classification, the disambiguation choices (the exact options shown, with the pick highlighted), and the generated description. The batch + timestamp of each is in the Provenance table below.

NER Named-entity recognition gpt-5-mini
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: Pyrenean orogeny | Statement: [Pyrenean foothills karst system, associatedWith, Pyrenean orogeny]
NED1 Entity disambiguation (via context triple) gpt-5-mini-2025-08-07
Target entity: Pyrenean orogeny
Context triple: [Pyrenean foothills karst system, associatedWith, Pyrenean orogeny]
  • A. Variscan orogeny
    The Variscan orogeny was a major late Paleozoic mountain-building event in Europe, broadly contemporaneous with the Appalachian orogeny, that resulted from the collision of continental plates during the assembly of the supercontinent Pangaea.
  • B. Carpathian orogeny
    The Carpathian orogeny is the mountain-building event responsible for forming the Carpathian Mountains through the collision and deformation of tectonic plates in Central and Eastern Europe.
  • C. Apennine orogeny
    The Apennine orogeny is the mountain-building event responsible for forming Italy’s Apennine Mountains through the collision and complex interaction of the African and Eurasian tectonic plates.
  • D. Pindus orogeny
    The Pindus orogeny is a mountain-building event that formed much of the Pindus mountain range in Greece through the collision and deformation of tectonic plates during the Mesozoic–Cenozoic eras.
  • E. Zagros orogeny
    The Zagros orogeny is the mountain-building event that formed the Zagros Mountains through the collision of the Arabian and Eurasian plates along the former Tethys Ocean margin.
  • F. None of above. chosen
  • G. Unsure - the case is ambiguous/there is not enough information to decide.
NEDg Description generation gpt-5.1
Instruction
Generate a one-sentence description of the target entity. 
You are given a context triple in the form (subject, predicate, object), where the object is the target entity. 
# Instructions
Use the triple to infer relevant information about the entity. Describe the entity based on what is most defining, well-known. 
Avoid repeating the information from the triple, unless really essential.
# Response Format
Return only the sentence: "Description: [one-sentence description of the target entity]"
Input
Entity: Pyrenean orogeny
Triple: [Pyrenean foothills karst system, associatedWith, Pyrenean orogeny]
Generated description
The Pyrenean orogeny was the major mountain-building event that created the Pyrenees through the collision of the Iberian and Eurasian tectonic plates during the Late Cretaceous to early Cenozoic.
NED2 Entity disambiguation (via description) gpt-5-mini-2025-08-07
Target entity: Pyrenean orogeny
Target entity description: The Pyrenean orogeny was the major mountain-building event that created the Pyrenees through the collision of the Iberian and Eurasian tectonic plates during the Late Cretaceous to early Cenozoic.
  • A. Variscan orogeny
    The Variscan orogeny was a major late Paleozoic mountain-building event in Europe, broadly contemporaneous with the Appalachian orogeny, that resulted from the collision of continental plates during the assembly of the supercontinent Pangaea.
  • B. Carpathian orogeny
    The Carpathian orogeny is the mountain-building event responsible for forming the Carpathian Mountains through the collision and deformation of tectonic plates in Central and Eastern Europe.
  • C. Apennine orogeny
    The Apennine orogeny is the mountain-building event responsible for forming Italy’s Apennine Mountains through the collision and complex interaction of the African and Eurasian tectonic plates.
  • D. Pindus orogeny
    The Pindus orogeny is a mountain-building event that formed much of the Pindus mountain range in Greece through the collision and deformation of tectonic plates during the Mesozoic–Cenozoic eras.
  • E. Zagros orogeny
    The Zagros orogeny is the mountain-building event that formed the Zagros Mountains through the collision of the Arabian and Eurasian plates along the former Tethys Ocean margin.
  • F. None of above. chosen

Provenance (5 batches)

The batch behind each pipeline step, in order, with when it ran. Timestamps are batch-level — stages were processed in waves, so the object chain (NER → NED1 → NEDg → NED2) reads in order, but predicate / elicitation batches can sit in a different wave.

Step Stage Batch ID Status When
creating Elicitation batch_69d8b918221c8190a9f7b563d64ac677 completed April 10, 2026, 8:47 a.m.
NER Named-entity recognition batch_69e5174d31608190851a5bab6878c203 completed April 19, 2026, 5:56 p.m.
NED1 Entity disambiguation (via context triple) batch_6a03d7748558819093969d121d385126 completed May 13, 2026, 1:44 a.m.
NEDg Description generation batch_6a03d8512d4c8190b113f7ed1f8a044c completed May 13, 2026, 1:48 a.m.
NED2 Entity disambiguation (via description) batch_6a03d8d863cc819098b46d5d26db05cd completed May 13, 2026, 1:50 a.m.
Created at: April 10, 2026, 10:38 a.m.