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About: Bushveld Igneous Complex     Goto   Sponge   NotDistinct   Permalink

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

Type: yago:WikicatMountainRangesOfAfricayago:WikicatMountainRangesOfSouthAfricayago:GeologicalFormation109287968yago:Object100002684yago:PhysicalEntity100001930yago:Range109403734yago:YagoGeoEntityyago:YagoPermanentlyLocatedEntitymountain New Facet based on Instances of this Class

The Bushveld Igneous Complex (BIC) is the largest layered igneous intrusion within the Earth's crust. It has been tilted and eroded forming the outcrops around what appears to be the edge of a great geological basin: the Transvaal Basin. It is approximately 2 billion years old and is divided into four different limbs: the northern, southern, eastern, and western limbs. The Bushveld Complex comprises the Rustenburg Layered suite, the Lebowa Granites and the Rooiberg Felsics, that are overlain by the Karoo sediments. The site was first discovered around 1897 by Gustaaf Molengraaff.