Idaho batholith
E633967
The Idaho batholith is a massive granitic intrusive rock complex in central Idaho that formed during Late Cretaceous magmatism and is one of the largest batholiths in North America.
All labels observed (1)
| Label | Occurrences |
|---|---|
| Idaho batholith canonical | 1 |
How this entity was disambiguated
This entity first appeared as the object of triple T6962107 — resolving that mention is where its identity was fixed. The disambiguator weighed these candidate entities and picked the highlighted one (or “None”, minting a new entity). This is how homonymy is resolved: the same surface form can point to different entities.
Target entity: Idaho batholith Context triple: [Sierra Nevada batholith, relatedTo, Idaho batholith]
-
A.
Sierra Nevada batholith
The Sierra Nevada batholith is a massive granitic rock formation underlying much of California’s Sierra Nevada range, formed by ancient magma intrusions during Mesozoic subduction along the western edge of North America.
-
B.
Peninsular Ranges Batholith
The Peninsular Ranges Batholith is a vast Mesozoic granitic intrusive complex underlying much of the Peninsular Ranges of Southern California and northern Baja California, formed during subduction-related magmatism along the western margin of North America.
-
C.
Cascade Range volcanic province
The Cascade Range volcanic province is a major volcanic region in western North America characterized by a chain of active and dormant stratovolcanoes and extensive volcanic deposits formed by the subduction of the Juan de Fuca Plate beneath the North American Plate.
-
D.
Cornubian Batholith
The Cornubian Batholith is a large granitic rock mass underlying much of southwest England, notable for its role in shaping the region’s geology and mineral resources.
-
E.
Coast Range Ophiolite
The Coast Range Ophiolite is a Jurassic-aged slice of ancient oceanic crust and upper mantle exposed in California’s Coast Ranges, representing part of the former Farallon Plate.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
Target entity: Idaho batholith Target entity description: The Idaho batholith is a massive granitic intrusive rock complex in central Idaho that formed during Late Cretaceous magmatism and is one of the largest batholiths in North America.
-
A.
Sierra Nevada batholith
The Sierra Nevada batholith is a massive granitic rock formation underlying much of California’s Sierra Nevada range, formed by ancient magma intrusions during Mesozoic subduction along the western edge of North America.
-
B.
Peninsular Ranges Batholith
The Peninsular Ranges Batholith is a vast Mesozoic granitic intrusive complex underlying much of the Peninsular Ranges of Southern California and northern Baja California, formed during subduction-related magmatism along the western margin of North America.
-
C.
Cascade Range volcanic province
The Cascade Range volcanic province is a major volcanic region in western North America characterized by a chain of active and dormant stratovolcanoes and extensive volcanic deposits formed by the subduction of the Juan de Fuca Plate beneath the North American Plate.
-
D.
Cornubian Batholith
The Cornubian Batholith is a large granitic rock mass underlying much of southwest England, notable for its role in shaping the region’s geology and mineral resources.
-
E.
Coast Range Ophiolite
The Coast Range Ophiolite is a Jurassic-aged slice of ancient oceanic crust and upper mantle exposed in California’s Coast Ranges, representing part of the former Farallon Plate.
- F. None of above. chosen
Statements (44)
| Predicate | Object |
|---|---|
| instanceOf |
batholith
ⓘ
geologic formation ⓘ granitic intrusive complex ⓘ |
| approximateAgeRange | 98–53 million years ago ⓘ |
| boundedBy |
Bitterroot Mountains to the north
ⓘ
Snake River Plain to the south NERFINISHED ⓘ |
| composition | felsic to intermediate ⓘ |
| continent | North America ⓘ |
| coolingHistory | slowly cooled at mid-crustal depths ⓘ |
| country |
United States of America
ⓘ
surface form:
United States
|
| economicSignificance | associated with some mineralization in central Idaho ⓘ |
| emplacementStyle | multiple pluton emplacement ⓘ |
| exposedIn |
Bitterroot Range
NERFINISHED
ⓘ
Salmon River Mountains NERFINISHED ⓘ Sawtooth Range NERFINISHED ⓘ |
| formedDuring | Late Cretaceous NERFINISHED ⓘ |
| geologicAge | Mesozoic NERFINISHED ⓘ |
| geologicSetting | continental arc ⓘ |
| hasSubunit |
Atlanta lobe
ⓘ
Bitterroot lobe NERFINISHED ⓘ Challis intrusive rocks (overlapping younger suite) ⓘ |
| hostTo | Challis volcanic field (nearby and related magmatism) NERFINISHED ⓘ |
| importance |
key feature in studies of Cordilleran magmatism
ⓘ
major control on topography of central Idaho ⓘ |
| intrusiveBodyType | plutonic complex ⓘ |
| largestBatholithRanking | one of the largest batholiths in North America ⓘ |
| lithologyVariation | more mafic margins and more felsic interior ⓘ |
| locatedIn |
Idaho
ⓘ
central Idaho ⓘ |
| mineralogy |
biotite
ⓘ
feldspar ⓘ hornblende ⓘ quartz ⓘ |
| orogeny |
Laramide orogeny
NERFINISHED
ⓘ
Sevier orogeny NERFINISHED ⓘ |
| partOf | North American Cordillera NERFINISHED ⓘ |
| relatedTo |
Bitterroot lobe of the Idaho batholith
ⓘ
Sierra Nevada batholith ⓘ |
| researchUse | used to study crustal evolution of western North America ⓘ |
| rockType |
granite
ⓘ
granodiorite ⓘ |
| structuralFeature | cut by numerous faults and shear zones ⓘ |
| tectonicSetting | subduction-related magmatic arc ⓘ |
| weatheringStyle | forms rugged, granitic landscapes ⓘ |
How these facts were elicited
The pipeline generated the facts above by prompting gpt-5.1 with this entity's name + description and the instruction below.
You are a knowledge base construction expert. Given a subject entity and a description of it, return factual statements that you know for the subject as a JSON list of dictionaries(triples), where keys must be "subject", "predicate" and "object". The number of facts may be very high, between 25 to 50 or more, for very popular subjects. For less popular subjects, the number of facts can be very low, like 5 or 10. # Requirements - If you don't know the subject at all, return an empty list. - If the subject is not a named entity, return an empty list. - Include at least one triple where predicate is "instanceOf". - Do not get too wordy. - Separate several objects into multiple triples with one object.
Subject: Idaho batholith Description of subject: The Idaho batholith is a massive granitic intrusive rock complex in central Idaho that formed during Late Cretaceous magmatism and is one of the largest batholiths in North America.
Referenced by (1)
Full triples — surface form annotated when it differs from this entity's canonical label.