Karakoram orogeny
E280248
The Karakoram orogeny is the mountain-building event responsible for forming the high, rugged Karakoram Range in the western Himalayas through ongoing tectonic collision and uplift.
All labels observed (1)
| Label | Occurrences |
|---|---|
| Karakoram orogeny canonical | 1 |
How this entity was disambiguated
This entity first appeared as the object of triple T2582522 — 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: Karakoram orogeny Context triple: [Hispar Glacier, geologicalSetting, Karakoram orogeny]
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A.
Himalayan orogeny
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.
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B.
Alpine orogeny
The Alpine orogeny is a major mountain-building event that created the Alps and other ranges across southern Europe and parts of Asia through the collision of tectonic plates during the Cenozoic Era.
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C.
Cadomian orogeny
The Cadomian orogeny was a late Neoproterozoic mountain-building event that shaped parts of what are now western Europe, contributing to the assembly of the supercontinent Pannotia.
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D.
Grenville orogeny
The Grenville orogeny was a major Precambrian mountain-building event that helped assemble the supercontinent Rodinia and formed the ancient core of parts of North America and other continents.
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E.
Variscan orogeny
The Variscan orogeny was a major late Paleozoic mountain-building event in Europe, broadly contemporaneous with the Appalachian orogeny, that resulted from the collision of continental plates during the assembly of the supercontinent Pangaea.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
Target entity: Karakoram orogeny Target entity description: The Karakoram orogeny is the mountain-building event responsible for forming the high, rugged Karakoram Range in the western Himalayas through ongoing tectonic collision and uplift.
-
A.
Himalayan orogeny
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.
-
B.
Alpine orogeny
The Alpine orogeny is a major mountain-building event that created the Alps and other ranges across southern Europe and parts of Asia through the collision of tectonic plates during the Cenozoic Era.
-
C.
Cadomian orogeny
The Cadomian orogeny was a late Neoproterozoic mountain-building event that shaped parts of what are now western Europe, contributing to the assembly of the supercontinent Pannotia.
-
D.
Grenville orogeny
The Grenville orogeny was a major Precambrian mountain-building event that helped assemble the supercontinent Rodinia and formed the ancient core of parts of North America and other continents.
-
E.
Variscan orogeny
The Variscan orogeny was a major late Paleozoic mountain-building event in Europe, broadly contemporaneous with the Appalachian orogeny, that resulted from the collision of continental plates during the assembly of the supercontinent Pangaea.
- F. None of above. chosen
Statements (52)
| Predicate | Object |
|---|---|
| instanceOf |
geological process
ⓘ
mountain-building event ⓘ orogeny ⓘ |
| actsOn |
Eurasian continental margin
ⓘ
surface form:
Eurasian Plate margin
Karakoram terrane ⓘ |
| associatedWith |
Karakoram fault system
ⓘ
granitoid intrusions ⓘ metamorphic core complexes ⓘ normal faulting at high elevations ⓘ strike-slip faulting ⓘ thrust faulting ⓘ |
| causedBy |
India–Eurasia continental collision
ⓘ
continental collision ⓘ convergent plate boundary ⓘ tectonic compression ⓘ |
| geologicalAge |
Cenozoic
ⓘ
Neogene ⓘ Quaternary ⓘ |
| hasFeature |
deep valleys
ⓘ
extreme elevation gradients ⓘ high, rugged relief ⓘ steep slopes ⓘ |
| hasPeak |
Broad Peak
ⓘ
Gasherbrum I ⓘ Gasherbrum II ⓘ K2 ⓘ Masherbrum ⓘ |
| influences |
glaciation in the Karakoram Range
ⓘ
regional climate ⓘ river incision ⓘ sediment supply to surrounding basins ⓘ |
| isOngoing | true ⓘ |
| locatedIn |
Asia
ⓘ
China ⓘ Gilgit-Baltistan ⓘ India ⓘ Karakoram ⓘ
surface form:
Karakoram Range
Ladakh ⓘ Pakistan ⓘ Xinjiang ⓘ western Himalayas ⓘ |
| partOf |
Alpine-Himalayan orogenic belt
ⓘ
surface form:
Alpine–Himalayan orogenic belt
|
| resultsIn |
crustal shortening
ⓘ
crustal thickening ⓘ exhumation of deep crustal rocks ⓘ faulting ⓘ folding ⓘ high topography ⓘ magmatism ⓘ metamorphism ⓘ mountain uplift ⓘ |
| startTime |
Cenozoic
ⓘ
surface form:
Cenozoic era
|
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: Karakoram orogeny Description of subject: The Karakoram orogeny is the mountain-building event responsible for forming the high, rugged Karakoram Range in the western Himalayas through ongoing tectonic collision and uplift.
Referenced by (1)
Full triples — surface form annotated when it differs from this entity's canonical label.