Triple
T19555367
| Position | Surface form | Disambiguated ID | Type / Status |
|---|---|---|---|
| Subject | Etna |
E489293
|
entity |
| Predicate | partOfRiverSystem |
P1009
|
FINISHED |
| Object | Randsfjorden basin |
—
|
NE NERFINISHED |
How this triple was built (3 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: Randsfjorden basin | Statement: [Etna, partOfRiverSystem, Randsfjorden basin]
NED1
Entity disambiguation (via context triple)
gpt-5-mini-2025-08-07
Target entity: Randsfjorden basin Context triple: [Etna, partOfRiverSystem, Randsfjorden basin]
-
A.
Nordfjord basin
The Nordfjord basin is a glacially carved valley and fjord system in western Norway, known for its deep waters, surrounding mountains, and numerous lakes and glaciers.
-
B.
Ofotfjord basin
The Ofotfjord basin is a geological and hydrological region in northern Norway centered around the Ofotfjord, encompassing its surrounding valleys, rivers, and catchment areas.
-
C.
Tysfjorden inner basin
Tysfjorden inner basin is the innermost, sheltered part of the Tysfjord fjord system in northern Norway, characterized by deep waters and steep surrounding terrain.
-
D.
Lofoten Basin
The Lofoten Basin is a deep oceanic depression in the Norwegian Sea known for its intense eddy activity and role in regional water mass circulation.
-
E.
Rana Fjord basin
The Rana Fjord basin is a marine basin in northern Norway that forms the receiving area for the waters of Ranfjorden and its surrounding drainage system.
- 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: Randsfjorden basin Target entity description: The Randsfjorden basin is a Norwegian watershed centered on Lake Randsfjorden, collecting water from surrounding rivers and streams into one of Eastern Norway’s major inland lake systems.
-
A.
Nordfjord basin
The Nordfjord basin is a glacially carved valley and fjord system in western Norway, known for its deep waters, surrounding mountains, and numerous lakes and glaciers.
-
B.
Ofotfjord basin
The Ofotfjord basin is a geological and hydrological region in northern Norway centered around the Ofotfjord, encompassing its surrounding valleys, rivers, and catchment areas.
-
C.
Tysfjorden inner basin
Tysfjorden inner basin is the innermost, sheltered part of the Tysfjord fjord system in northern Norway, characterized by deep waters and steep surrounding terrain.
-
D.
Lofoten Basin
The Lofoten Basin is a deep oceanic depression in the Norwegian Sea known for its intense eddy activity and role in regional water mass circulation.
-
E.
Rana Fjord basin
The Rana Fjord basin is a marine basin in northern Norway that forms the receiving area for the waters of Ranfjorden and its surrounding drainage system.
- F. None of above. chosen
Provenance (2 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_69d8e8dc5d8c8190a6d7bd8864f43ca0 |
completed | April 10, 2026, 12:11 p.m. |
| NER | Named-entity recognition | batch_69e63d335f888190abfc5ba974d3c65e |
completed | April 20, 2026, 2:50 p.m. |
Created at: April 10, 2026, 1:42 p.m.