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About: Omagh Thrust     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:Space113910384, within Data Space : dbpedia.demo.openlinksw.com associated with source document(s)

Type: World Heritage Sitegeo:SpatialThingyago:Abstraction100002137yago:AmorphousShape113867492yago:Attribute100024264yago:Crack109258715yago:Fault109278537yago:Location100027167yago:Object100002684yago:Opening109379111yago:PhysicalEntity100001930yago:WikicatGeologicalFaultsOfNorthernIrelandyago:YagoGeoEntityyago:YagoLegalActorGeoyago:YagoPermanentlyLocatedEntityyago:Shape100027807yago:Space113910384 New Facet based on Instances of this Class

The Omagh Thrust Fault is a geological fault in County Tyrone. It is of one of the most important structural discontinuities in Northern Ireland and an extension of the Highland Boundary Fault which runs through Scotland. The fault occurred in the Caledonian orogeny, during a late stage of this period of mountain building. Older sequences of Dalriadan metamorphic strata were moved over younger Ordovician ones with the fault as their boundary. There is access to a view of the fault at Mountfield Quarry, County Tyrone. This has been designated an Area of Special Scientific Interest.