Climate and Time in Their Geological Relations
E1502923
UNEXPLORED
"Climate and Time in Their Geological Relations" is an influential 19th-century scientific work that advanced the theory that variations in Earth’s orbit drive long-term climatic and glacial cycles.
All labels observed (1)
| Label | Occurrences |
|---|---|
| Climate and Time in Their Geological Relations canonical | 1 |
How this entity was disambiguated
This entity first appeared as the object of triple T21794635 — 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.
NED1
Entity disambiguation (via context triple)
gpt-5-mini-2025-08-07
Target entity: Climate and Time in Their Geological Relations Context triple: [James Croll, notableWork, Climate and Time in Their Geological Relations]
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A.
On the Imperfection of the Geological Record
"On the Imperfection of the Geological Record" is a chapter in Charles Darwin's *On the Origin of Species* that addresses why the fossil record is incomplete and how this affects evidence for evolutionary change.
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B.
An Inquiry into the Original State and Formation of the Earth
*An Inquiry into the Original State and Formation of the Earth* is an 18th-century geological treatise by John Whitehurst that explores the Earth's structure, history, and the processes that shaped it.
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C.
The Age of the Earth
The Age of the Earth is a landmark 20th-century geology book that helped establish modern estimates of Earth’s age using radiometric dating methods.
-
D.
Illustrations of the Huttonian Theory of the Earth
Illustrations of the Huttonian Theory of the Earth is an 1802 geological treatise by John Playfair that clearly expounds and defends James Hutton’s uniformitarian theory of the Earth’s formation and processes.
-
E.
Eocene–Oligocene climate transition
The Eocene–Oligocene climate transition was a major global cooling event around 34 million years ago that marked the shift from a greenhouse to an icehouse Earth, including the formation of large Antarctic ice sheets.
- 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: Climate and Time in Their Geological Relations Target entity description: "Climate and Time in Their Geological Relations" is an influential 19th-century scientific work that advanced the theory that variations in Earth’s orbit drive long-term climatic and glacial cycles.
-
A.
On the Imperfection of the Geological Record
"On the Imperfection of the Geological Record" is a chapter in Charles Darwin's *On the Origin of Species* that addresses why the fossil record is incomplete and how this affects evidence for evolutionary change.
-
B.
An Inquiry into the Original State and Formation of the Earth
*An Inquiry into the Original State and Formation of the Earth* is an 18th-century geological treatise by John Whitehurst that explores the Earth's structure, history, and the processes that shaped it.
-
C.
The Age of the Earth
The Age of the Earth is a landmark 20th-century geology book that helped establish modern estimates of Earth’s age using radiometric dating methods.
-
D.
Illustrations of the Huttonian Theory of the Earth
Illustrations of the Huttonian Theory of the Earth is an 1802 geological treatise by John Playfair that clearly expounds and defends James Hutton’s uniformitarian theory of the Earth’s formation and processes.
-
E.
Eocene–Oligocene climate transition
The Eocene–Oligocene climate transition was a major global cooling event around 34 million years ago that marked the shift from a greenhouse to an icehouse Earth, including the formation of large Antarctic ice sheets.
- F. None of above. chosen
Referenced by (1)
Full triples — surface form annotated when it differs from this entity's canonical label.