Cascadian orogeny
E111529
The Cascadian orogeny is the long-lasting mountain-building episode responsible for forming the Cascade Range through subduction-related tectonic activity along western North America.
All labels observed (1)
| Label | Occurrences |
|---|---|
| Cascadian orogeny canonical | 1 |
How this entity was disambiguated
This entity first appeared as the object of triple T926047 — 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: Cascadian orogeny Context triple: [Cascade Range, orogeny, Cascadian orogeny]
-
A.
Acadian orogeny
The Acadian orogeny was a major Middle Paleozoic mountain-building event that significantly shaped the northern Appalachian Mountains through the collision of ancient landmasses.
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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.
Taconic orogeny
The Taconic orogeny was an early Paleozoic mountain-building event along the eastern margin of ancient North America that contributed significantly to the formation of the Appalachian Mountains.
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D.
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.
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E.
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.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
Target entity: Cascadian orogeny Target entity description: The Cascadian orogeny is the long-lasting mountain-building episode responsible for forming the Cascade Range through subduction-related tectonic activity along western North America.
-
A.
Acadian orogeny
The Acadian orogeny was a major Middle Paleozoic mountain-building event that significantly shaped the northern Appalachian Mountains through the collision of ancient landmasses.
-
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.
Taconic orogeny
The Taconic orogeny was an early Paleozoic mountain-building event along the eastern margin of ancient North America that contributed significantly to the formation of the Appalachian Mountains.
-
D.
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.
-
E.
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.
- F. None of above. chosen
Statements (47)
| Predicate | Object |
|---|---|
| instanceOf |
geological event
ⓘ
mountain-building episode ⓘ orogeny ⓘ |
| affects |
Canada
ⓘ
Cascade Range ⓘ Pacific Northwest ⓘ
surface form:
Pacific Northwest region
United States of America ⓘ
surface form:
United States
|
| associatedWith |
Cascadia Subduction Zone
ⓘ
surface form:
Cascadia megathrust
Cascadia Subduction Zone ⓘ
surface form:
Cascadia subduction earthquakes
|
| cause |
subduction of oceanic plates beneath North America
ⓘ
subduction of the Explorer Plate ⓘ subduction of the Farallon Plate (in the past) ⓘ subduction of the Gorda Plate ⓘ subduction of the Juan de Fuca Plate ⓘ |
| drives | arc volcanism from northern California to British Columbia ⓘ |
| endTime | ongoing ⓘ |
| geologicalProvince |
Cascade Range
ⓘ
North American Cordillera ⓘ
surface form:
Pacific Northwest Cordillera
|
| hasDuration | long-lasting ⓘ |
| hasEffect |
formation of the Cascade Range
ⓘ
uplift of the Cascade Range ⓘ volcanism in the Cascade Range ⓘ |
| involves |
accretion of oceanic terranes
ⓘ
magmatic arc development ⓘ oceanic-continental plate convergence ⓘ |
| locatedIn | western North America ⓘ |
| namedAfter |
Cascadia
ⓘ
surface form:
Cascadia region
|
| orogenyType |
continental-margin orogeny
ⓘ
subduction-related orogeny ⓘ |
| partOf | Cordilleran orogeny ⓘ |
| produces |
andesitic to dacitic volcanism
ⓘ
continental arc magmatism ⓘ plutonic intrusions beneath the Cascade Range ⓘ |
| relatedTo |
Cascade Volcanic Arc
ⓘ
surface form:
Cascade volcanic arc
Cascadia Subduction Zone ⓘ
surface form:
Cascadia subduction zone
Explorer Plate ⓘ Gorda Plate ⓘ Juan de Fuca Plate ⓘ North American Plate ⓘ |
| resultsIn |
crustal deformation in the Pacific Northwest
ⓘ
faulting and folding in western North America ⓘ regional metamorphism in the Cascade region ⓘ topographic relief of the Cascade Range ⓘ |
| startTime |
Cenozoic
ⓘ
surface form:
Cenozoic era
late Mesozoic to early Cenozoic (approximate) ⓘ |
| tectonicProcess | subduction ⓘ |
| tectonicSetting | convergent plate margin ⓘ |
How these facts were elicited
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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: Cascadian orogeny Description of subject: The Cascadian orogeny is the long-lasting mountain-building episode responsible for forming the Cascade Range through subduction-related tectonic activity along western North America.
Referenced by (1)
Full triples — surface form annotated when it differs from this entity's canonical label.