Triple

T12300261
Position Surface form Disambiguated ID Type / Status
Subject Racha Mountains E293199 entity
Predicate geologicalContext P4015 FINISHED
Object Caucasus orogeny
The Caucasus orogeny is the mountain-building event responsible for forming the Caucasus region through the collision of tectonic plates between the Black and Caspian Seas.
 E975601 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: Caucasus orogeny | Statement: [Racha Mountains, geologicalContext, Caucasus orogeny]
NED1 Entity disambiguation (via context triple) gpt-5-mini-2025-08-07 
Target entity: Caucasus orogeny
Context triple: [Racha Mountains, geologicalContext, Caucasus orogeny]
  • A. 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.
  • B. Baikal orogeny
    Baikal orogeny is an ancient mountain-building event that shaped parts of Siberia and Central Asia during the late Precambrian to early Paleozoic eras.
  • C. Karelian orogeny
    The Karelian orogeny was an ancient Paleoproterozoic mountain-building event that shaped much of the bedrock and geological structure of the Fennoscandian Shield in northern Europe.
  • D. 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.
  • E. Cadomian orogeny
    The Cadomian orogeny was a late Neoproterozoic mountain-building event that shaped parts of what are now western Europe, contributing to the assembly of the supercontinent Pannotia.
  • 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: Caucasus orogeny
Triple: [Racha Mountains, geologicalContext, Caucasus orogeny]
Generated description
The Caucasus orogeny is the mountain-building event responsible for forming the Caucasus region through the collision of tectonic plates between the Black and Caspian Seas.
NED2 Entity disambiguation (via description) gpt-5-mini-2025-08-07 
Target entity: Caucasus orogeny
Target entity description: The Caucasus orogeny is the mountain-building event responsible for forming the Caucasus region through the collision of tectonic plates between the Black and Caspian Seas.
  • A. 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.
  • B. Baikal orogeny
    Baikal orogeny is an ancient mountain-building event that shaped parts of Siberia and Central Asia during the late Precambrian to early Paleozoic eras.
  • C. Karelian orogeny
    The Karelian orogeny was an ancient Paleoproterozoic mountain-building event that shaped much of the bedrock and geological structure of the Fennoscandian Shield in northern Europe.
  • D. 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.
  • E. Cadomian orogeny
    The Cadomian orogeny was a late Neoproterozoic mountain-building event that shaped parts of what are now western Europe, contributing to the assembly of the supercontinent Pannotia.
  • 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_69d6ab6a2b50819082f6aedd32ed608a completed April 8, 2026, 7:24 p.m.
NER Named-entity recognition batch_69d93edb59908190bcef9d0cdc11081f completed April 10, 2026, 6:18 p.m.
NED1 Entity disambiguation (via context triple) batch_69f61e7d757881908ac6af2b70a6dafe completed May 2, 2026, 3:55 p.m.
NEDg Description generation batch_69f61f5cc5608190a67a888eb5136ada completed May 2, 2026, 3:59 p.m.
NED2 Entity disambiguation (via description) batch_69f62009766c8190985fafe9ba53ae7b completed May 2, 2026, 4:02 p.m.
Created at: April 8, 2026, 9:53 p.m.