Glarus thrust (geological feature)
E936987
The Glarus thrust is a famous Alpine geological structure in eastern Switzerland where older rock layers have been thrust over much younger ones, serving as a classic example of large-scale thrust faulting.
All labels observed (1)
| Label | Occurrences |
|---|---|
| Glarus thrust (geological feature) canonical | 1 |
How this entity was disambiguated
This entity first appeared as the object of triple T11605918 — 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: Glarus thrust (geological feature) Context triple: [Glarus, contains, Glarus thrust (geological feature)]
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A.
Keystone Thrust Fault
The Keystone Thrust Fault is a prominent geological feature near Las Vegas where older limestone rock has been pushed up and over younger sandstone, creating dramatic cliffs and colorful rock formations visible in Red Rock Canyon.
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B.
Vienna Basin transfer zone
The Vienna Basin transfer zone is a major geological structure in Central Europe that accommodates tectonic movement between the Eastern Alps and Western Carpathians, influencing regional basin formation and seismicity.
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C.
San Gorgonio Pass thrust fault system
The San Gorgonio Pass thrust fault system is a complex network of active thrust faults in Southern California that accommodates significant crustal deformation and influences regional seismic hazard.
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D.
Glocknerkees glacier
Glocknerkees glacier is a prominent alpine glacier on Austria’s Grossglockner massif, known for its dramatic high-mountain ice scenery and accessibility to climbers and hikers.
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E.
Calder Graben
Calder Graben is a structural depression within Western Australia’s Bonaparte Basin, known as a hydrocarbon-bearing sub-basin formed by extensional tectonics.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
Target entity: Glarus thrust (geological feature) Target entity description: The Glarus thrust is a famous Alpine geological structure in eastern Switzerland where older rock layers have been thrust over much younger ones, serving as a classic example of large-scale thrust faulting.
-
A.
Keystone Thrust Fault
The Keystone Thrust Fault is a prominent geological feature near Las Vegas where older limestone rock has been pushed up and over younger sandstone, creating dramatic cliffs and colorful rock formations visible in Red Rock Canyon.
-
B.
Vienna Basin transfer zone
The Vienna Basin transfer zone is a major geological structure in Central Europe that accommodates tectonic movement between the Eastern Alps and Western Carpathians, influencing regional basin formation and seismicity.
-
C.
San Gorgonio Pass thrust fault system
The San Gorgonio Pass thrust fault system is a complex network of active thrust faults in Southern California that accommodates significant crustal deformation and influences regional seismic hazard.
-
D.
Glocknerkees glacier
Glocknerkees glacier is a prominent alpine glacier on Austria’s Grossglockner massif, known for its dramatic high-mountain ice scenery and accessibility to climbers and hikers.
-
E.
Calder Graben
Calder Graben is a structural depression within Western Australia’s Bonaparte Basin, known as a hydrocarbon-bearing sub-basin formed by extensional tectonics.
- F. None of above. chosen
Statements (47)
| Predicate | Object |
|---|---|
| instanceOf |
World Heritage Site component
ⓘ
geological structure ⓘ tectonic boundary ⓘ thrust fault ⓘ |
| composedOf |
Mesozoic dolomites
ⓘ
Mesozoic limestones ⓘ Mesozoic shales ⓘ Permian Verrucano rocks ⓘ |
| country | Switzerland ⓘ |
| exposedAs | distinct contact surface between rock units ⓘ |
| formedDuring | Alpine orogeny NERFINISHED ⓘ |
| hasGeologicalAge |
Cenozoic
NERFINISHED
ⓘ
Mesozoic NERFINISHED ⓘ Paleozoic NERFINISHED ⓘ |
| hasLength | approximately 35 km ⓘ |
| hasMaximumDisplacement | several kilometers GENERATED ⓘ |
| hasScientificSignificance |
classic example of large-scale thrust faulting
ⓘ
important for development of modern geology ⓘ key evidence for nappe theory ⓘ |
| hasStratigraphicRelationship | older rocks above younger rocks ⓘ |
| hasUNESCOWorldHeritageStatus | yes ⓘ |
| includedIn | UNESCO World Heritage List NERFINISHED ⓘ |
| locatedIn |
Swiss Alps
NERFINISHED
ⓘ
canton of Glarus NERFINISHED ⓘ canton of Graubünden ⓘ canton of St. Gallen NERFINISHED ⓘ eastern Switzerland NERFINISHED ⓘ |
| orientation | roughly northwest–southeast ⓘ |
| overlies | younger sedimentary rocks ⓘ |
| overthrusts |
Eocene–Oligocene sediments
ⓘ
Tertiary flysch ⓘ younger rock layers ⓘ |
| partOf |
Glarus Alps
NERFINISHED
ⓘ
Tectonic Arena Sardona NERFINISHED ⓘ |
| recognizedAs | type locality for major thrust faults ⓘ |
| studiedBy |
Albert Heim
NERFINISHED
ⓘ
Arnold Escher von der Linth NERFINISHED ⓘ Hans Conrad Escher von der Linth NERFINISHED ⓘ |
| UNESCOCriteria | criterion (viii) ⓘ |
| UNESCOInscriptionYear | 2008 ⓘ |
| usedFor |
field training for structural geology
ⓘ
geological education ⓘ |
| visibleAt |
Lochsite near Glarus
ⓘ
Piz Dolf NERFINISHED ⓘ Piz Segnas NERFINISHED ⓘ Segnes Pass NERFINISHED ⓘ Tschingelhörner NERFINISHED ⓘ |
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: Glarus thrust (geological feature) Description of subject: The Glarus thrust is a famous Alpine geological structure in eastern Switzerland where older rock layers have been thrust over much younger ones, serving as a classic example of large-scale thrust faulting.
Referenced by (1)
Full triples — surface form annotated when it differs from this entity's canonical label.