The Drakensberg Group was formed approximately 182 million years ago during the early Jurassic period. Riftingtectonics in response to the breakup of the supercontinentGondwana are believed to have been the cause for the formation of the Drakensberg Group. Networks of hyperbyssal dikes and sills represent the conduits through the crust that brought basaltic and andesiticlava to the surface, and caused the formation of the extrusiveflood basalts of the Drakensberg Group. The dikes and sills are preserved throughout the Karoo Basin, and have served as a weathering barrier for much of the Karoo Supergroup rocks. The Drakensberg Group comprises minor sedimentary and is part of the greater volcanicextrusive rock sequences of the Karoo Igneous Province. In its entirety, the Karoo Igneous Province represents a vast suite of sedimentary, extrusive and intrusive rocks ranging from 200 - 130 million years in age. Past studies have shown that there are major geochemical changes in the provinces from the north and the south. The provinces of the central to southern areas are composed ofTitanium - Zirconium low tholeiitic basalt, and andesitic compositions also occur. The Drakensberg Group has been subdivided into two recognized geological formations. While both formations are composed of tholeiitic basalt, they have minor geochemical differences. The two formations are listed below :
Barkly East Formation: This formation is the only formation of the Drakensberg Group to contain sedimentary units. These sedimentary units are composed of sandstones, lapillideposits, and pyroclastic deposits. They are only found in the lower sections and are interbedded with basalts.
Lesotho Formation: Composed entirely of tholeiitic basalts. However, in some parts of Lesotho pillow lava basalts are found which means these basalts had extruded out as lava underwater into large lakes.
The Drakensberg Group lavas compose the upper levels of the entire Drakensberg mountain range. The lavas stretch out over most of Lesotho and into the northeastern Eastern Cape, the southern Free State, and eastern KwaZulu-Natal provinces of South Africa. Basalt provinces of the same low Ti-Zr chemical composition as the Drakensberg lavas are found in the Springbok Flats province in Limpopo, and other basalt sub-outcrops are found in eastern Botswana and central Namibia. These occurrences suggest that the Drakensberg Group lavas once covered a vast area over southern Africa. In addition, basalt xenoliths of the same chemical structure as the Drakensberg lavas have been found in the Northern Cape within Cretaceous-aged kimberlite pipes that intruded older rocks of the Karoo Supergroup. In the Lesotho highlands and the highest sections of the Drakensberg mountain range, only erosional remnants of the Drakensberg lavas remain.
Correlation
The Drakensberg Group is part of the greater Mesozoic-aged Karoo Igneous Province of southern Africa and the Ferrar Large Igneous Province of Antarctica. The Kirwan basalts of Antarctica particularly resemble the Drakensberg Group, because Antarctica was close to the southern Lebombo province before the break up of Gondwana. The Drakensberg basalts are geochemicallyidentical to the Springbok Flats volcanics. It was thought for some time that the Drakensberg volcanics were associated with the Parana Igneous Province of Brazil and the Etendeka Province in northern Namibia. However, these provinces have since been dated some 50 million years younger than the Karoo-Ferrar provinces.
