Himalayan orogeny
E41167
The Himalayan orogeny is the major mountain-building event resulting from the collision of the Indian and Eurasian tectonic plates, responsible for creating the Himalayan mountain range and the Tibetan Plateau.
All labels observed (8)
How this entity was disambiguated
This entity first appeared as the object of triple T318644 — 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: Himalayan orogeny Context triple: [Indo-Australian Plate, associatedWith, Himalayan orogeny]
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A.
Alpine-Himalayan orogenic belt
The Alpine-Himalayan orogenic belt is a vast, tectonically active mountain-building zone stretching from southern Europe through the Middle East to Southeast Asia, encompassing major ranges such as the Alps and the Himalayas.
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B.
Appalachian orogeny
The Appalachian orogeny was a series of ancient mountain-building events that formed the Appalachian Mountains through the collision of tectonic plates during the Paleozoic Era.
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C.
Caledonian orogeny
The Caledonian orogeny was a major Paleozoic mountain-building event that formed ranges across what are now Scandinavia, Scotland, Ireland, Greenland, and parts of North America as ancient continents collided.
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D.
Transhimalaya
The Transhimalaya is a high, remote mountain range running parallel to the main Himalayas, primarily across Tibet and parts of India and Nepal, known for its arid plateaus and rugged peaks.
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E.
Tibetan Plateau
The Tibetan Plateau is a vast high-altitude region in Central Asia, often called the "Roof of the World," known for its extreme elevation, unique climate, and crucial role in influencing Asian weather and river systems.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
Target entity: Himalayan orogeny Target entity description: The Himalayan orogeny is the major mountain-building event resulting from the collision of the Indian and Eurasian tectonic plates, responsible for creating the Himalayan mountain range and the Tibetan Plateau.
-
A.
Alpine-Himalayan orogenic belt
The Alpine-Himalayan orogenic belt is a vast, tectonically active mountain-building zone stretching from southern Europe through the Middle East to Southeast Asia, encompassing major ranges such as the Alps and the Himalayas.
-
B.
Appalachian orogeny
The Appalachian orogeny was a series of ancient mountain-building events that formed the Appalachian Mountains through the collision of tectonic plates during the Paleozoic Era.
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C.
Caledonian orogeny
The Caledonian orogeny was a major Paleozoic mountain-building event that formed ranges across what are now Scandinavia, Scotland, Ireland, Greenland, and parts of North America as ancient continents collided.
-
D.
Transhimalaya
The Transhimalaya is a high, remote mountain range running parallel to the main Himalayas, primarily across Tibet and parts of India and Nepal, known for its arid plateaus and rugged peaks.
-
E.
Tibetan Plateau
The Tibetan Plateau is a vast high-altitude region in Central Asia, often called the "Roof of the World," known for its extreme elevation, unique climate, and crucial role in influencing Asian weather and river systems.
- F. None of above. chosen
Statements (51)
| Predicate | Object |
|---|---|
| instanceOf |
Cenozoic orogeny
ⓘ
geological process ⓘ mountain-building event ⓘ orogeny ⓘ |
| affects |
Eurasian Plate
ⓘ
Indo-Australian Plate ⓘ
surface form:
Indian Plate
|
| cause |
formation of the Himalayan mountain range
ⓘ
formation of the Hindu Kush region ⓘ formation of the Karakoram Range ⓘ high elevation of Mount Everest region ⓘ uplift of the Tibetan Plateau ⓘ |
| characterizedBy |
continental collision tectonics
ⓘ
high rates of uplift ⓘ large-scale thrust systems ⓘ major strike-slip faults ⓘ rapid erosion ⓘ |
| endTime | ongoing ⓘ |
| hasCause |
closure of the Tethys Ocean
ⓘ
collision of the Indian Plate with the Eurasian Plate ⓘ northward movement of the Indian Plate ⓘ subduction of oceanic lithosphere between India and Eurasia ⓘ |
| hasEffectOn |
Asian monsoon system
ⓘ
regional climate of South Asia ⓘ sedimentation in the Bengal Fan ⓘ |
| locatedIn | Asia ⓘ |
| partOf | Alpine orogeny ⓘ |
| produces |
Greater Himalayas
ⓘ
surface form:
Greater Himalaya
Indus-Tsangpo Suture Zone ⓘ Lesser Himalayas ⓘ
surface form:
Lesser Himalaya
Main Boundary Thrust zone ⓘ Main Central Thrust zone ⓘ Lesser Himalayas ⓘ
surface form:
Sub-Himalaya
|
| relatedTo |
Alpine-Himalayan orogenic belt
ⓘ
Himalayan orogeny self-linksurface differs ⓘ
surface form:
India–Asia collision
Tethyan Himalaya ⓘ |
| resultsIn |
Indo-Gangetic Plain
ⓘ
surface form:
Indo-Gangetic foreland basin
continental-continental collision zone ⓘ crustal shortening ⓘ development of foreland basins ⓘ exhumation of high-grade metamorphic rocks ⓘ fold-and-thrust belt formation ⓘ high seismicity in the Himalayan region ⓘ large-scale thrust faulting ⓘ ongoing uplift of the Himalayas ⓘ thickening of continental crust ⓘ |
| startTime |
Eocene
ⓘ
Paleogene ⓘ approximately 55 million years ago ⓘ |
| studiedIn |
plate tectonics
ⓘ
structural geology ⓘ tectonophysics ⓘ |
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: Himalayan orogeny Description of subject: The Himalayan orogeny is the major mountain-building event resulting from the collision of the Indian and Eurasian tectonic plates, responsible for creating the Himalayan mountain range and the Tibetan Plateau.
Referenced by (20)
Full triples — surface form annotated when it differs from this entity's canonical label.