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About: Geology of the Australian Capital Territory     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:Vent109470550, within Data Space : dbpedia.org associated with source document(s)

Type: yago:WikicatVolcanoesOfTheAustralianCapitalTerritoryyago:Abstraction100002137yago:AmorphousShape113867492yago:Attribute100024264yago:Crack109258715yago:Location100027167yago:Object100002684yago:Opening109379111yago:PhysicalEntity100001930yago:YagoGeoEntityyago:YagoLegalActorGeoyago:YagoPermanentlyLocatedEntityyago:Shape100027807yago:Space113910384yago:Vent109470550 New Facet based on Instances of this Class

The geology of the Australian Capital Territory includes rocks dating from the Ordovician around 480 million years ago, whilst most rocks are from the Silurian. During the Ordovician period the region—along with most of eastern Australia—was part of the ocean floor. The area contains the Pittman Formation consisting largely of Quartz-rich sandstone, siltstone and shale; the Adaminaby Beds and the Acton Shale.