Triple
T1036376
| Position | Surface form | Disambiguated ID | Type / Status |
|---|---|---|---|
| Subject | James Hutton |
E22371
|
entity |
| Predicate | studied |
P778
|
FINISHED |
| Object |
Siccar Point unconformity
The Siccar Point unconformity is a famous geological site in Scotland where dramatically tilted older rocks are overlain by younger strata, providing key evidence for deep geological time and helping to establish modern geology.
|
E122990
|
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: Siccar Point unconformity | Statement: [James Hutton, studied, Siccar Point unconformity]
NED1
Entity disambiguation (via context triple)
gpt-5-mini-2025-08-07
Target entity: Siccar Point unconformity Context triple: [James Hutton, studied, Siccar Point unconformity]
-
A.
Hutton's Unconformity at Lochranza
Hutton's Unconformity at Lochranza is a famous geological site on the Isle of Arran where James Hutton found key evidence for deep geological time and the foundations of modern geology.
-
B.
Caledonian fault system
The Caledonian fault system is a major ancient tectonic fracture network formed during the Caledonian orogeny that helped shape the geological structure of parts of Scotland and other regions in the North Atlantic.
-
C.
Highland Boundary Fault
The Highland Boundary Fault is a major geological fault line in Scotland that marks the boundary between the Highlands and the Central Lowlands, separating distinct rock formations and landscapes.
-
D.
Old Red Sandstone
Old Red Sandstone is a thick sequence of Devonian-age sedimentary rocks, notable for its red coloration and widespread occurrence across parts of Scotland and other regions of the North Atlantic.
-
E.
Southern Uplands Fault
The Southern Uplands Fault is a major geological fault line in Scotland that marks the boundary between the Central Lowlands and the Southern Uplands, playing a key role in the region’s tectonic and landscape history.
- 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: Siccar Point unconformity Triple: [James Hutton, studied, Siccar Point unconformity]
Generated description
The Siccar Point unconformity is a famous geological site in Scotland where dramatically tilted older rocks are overlain by younger strata, providing key evidence for deep geological time and helping to establish modern geology.
NED2
Entity disambiguation (via description)
gpt-5-mini-2025-08-07
Target entity: Siccar Point unconformity Target entity description: The Siccar Point unconformity is a famous geological site in Scotland where dramatically tilted older rocks are overlain by younger strata, providing key evidence for deep geological time and helping to establish modern geology.
-
A.
Hutton's Unconformity at Lochranza
Hutton's Unconformity at Lochranza is a famous geological site on the Isle of Arran where James Hutton found key evidence for deep geological time and the foundations of modern geology.
-
B.
Caledonian fault system
The Caledonian fault system is a major ancient tectonic fracture network formed during the Caledonian orogeny that helped shape the geological structure of parts of Scotland and other regions in the North Atlantic.
-
C.
Highland Boundary Fault
The Highland Boundary Fault is a major geological fault line in Scotland that marks the boundary between the Highlands and the Central Lowlands, separating distinct rock formations and landscapes.
-
D.
Old Red Sandstone
Old Red Sandstone is a thick sequence of Devonian-age sedimentary rocks, notable for its red coloration and widespread occurrence across parts of Scotland and other regions of the North Atlantic.
-
E.
Southern Uplands Fault
The Southern Uplands Fault is a major geological fault line in Scotland that marks the boundary between the Central Lowlands and the Southern Uplands, playing a key role in the region’s tectonic and landscape history.
- 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_69a493d848848190aed4011b34b2e8d3 |
completed | March 1, 2026, 7:30 p.m. |
| NER | Named-entity recognition | batch_69a4b82a1014819085bfc077e24c9742 |
completed | March 1, 2026, 10:05 p.m. |
| NED1 | Entity disambiguation (via context triple) | batch_69ac42990be88190aeda5ec08fce5288 |
completed | March 7, 2026, 3:22 p.m. |
| NEDg | Description generation | batch_69ac430384ec8190a307c895bb12a122 |
completed | March 7, 2026, 3:23 p.m. |
| NED2 | Entity disambiguation (via description) | batch_69ac437b62bc8190abfb721c570b4768 |
completed | March 7, 2026, 3:25 p.m. |
Created at: March 1, 2026, 7:41 p.m.