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It merged with the Metsweding District, which was a consequence of the Gauteng Global City Region Strategy to reduce the number of municipalities in Gauteng to at least four by The City of Tshwane is the single-largest metropolitan municipality in the country, comprising seven regions, wards and councillors. Pretoria is the capital of South Africa.
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An overview of the geology of the Transvaal Sequence and Bushveld Complex, South Africa
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Various types of veld may be discerned, depending upon local characteristics such as elevation, cultivation, and climate. Thus, there is a high veld, a middle veld, a low veld, a bush veld, a thorn veld, and a grass veld. The boundary between these different varieties of veld is frequently vague, and all of them are usually referred to with the general term veld by the local inhabitants.
For convenience, its major regions—Highveld, Middleveld, and Lowveld—are distinguished on the basis of elevation. The Highveld comprises most of the high-plateau country of Southern Africa. Except in Lesotho , where it extends well above 8, feet 2, metres and even above 11, feet 3, metres in places, all of it lies between 4, and 6, feet 1, and 1, metres above sea level.
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The rich biodiversity includes floral species such as Aloe peglerae and Frithia pulchra , and faunal species such as the forest shrew Myosorex varius , sable antelope Hippotragus niger and bird species representing The area is characterized by remarkable scenic beauty and unique natural features. The area faces high levels of unemployment and poverty. The main economic activities are agriculture, mining, urban development and tourism. The reserve includes a variety of landscapes including slopes, cliffs, crests, kloofs, rivers, wetlands and valleys.
Although the area covers a diverse geological area, it consists mainly of the Magaliesberg mountain complex comprising two geological formations: the Transvaal System and the Bushveld Igneous Complex.
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Both Transvaal and Bushveld rocks are extensively mineralized, the former containing large deposits of iron, manganese, asbestos, andalusite, gold, fluorine, lead, zinc and tin ores, and the latter some of the World’s major occurrences of PGE, chromium and vanadium ores. Transvaal sedimentation began with thin, predominantly clastic sedimentary rocks Black Reef-Vryburg Formations which grade up into a thick package of carbonate rocks and BIF Chuniespoort-Ghaap-Taupone Groups.
These lithologies reflect a carbonate-BIF platform sequence which covered much of the Kaapvaal craton, in reaction to thermal subsidence above Ventersdorp-aged rift-related fault systems. An erosional hiatus was followed by deposition of the clastic sedimentary rocks and volcanics of the Pretoria-Postmasburg-Segwagwa Groups within the three basins, under largely closed-basin conditions. An uppermost predominantly volcanic succession Rooiberg Group-Loskop Formation is restricted to the Transvaal basin.
A common continental rift setting is thought to have controlled Pretoria Group sedimentation, Rooiberg volcanism and the intrusion of the mafic rocks of the Rustenburg Layered Suite of the Bushveld Complex. The dipping sheets of the Rustenburg magmas cut across the upper Pretoria Group stratigraphy and lifted up the Rooiberg lithologies to form the roof to the complex. Subsequent granitic rocks of the Lebowa and Rashoop Suites of the Bushveld Complex intruded both upper Rustenburg rocks and the Rooiberg felsites.
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The Magaliesberg Biosphere Reserve is located in South Africa between the cities of Pretoria The area is characterized by remarkable scenic beauty and unique natural features. of Humankind World Heritage site which encompasses cultural heritage and sites of archaeological interest dating back 4 million years.
In the article below, journalist Lucille Davie traces the fascinating history of various South African War battles in the Magaliesberg. The piece was originally published on the City of Joburg’s website on 10 December Click here to view more of Davie’s work. Boer strategy in the Battle of Nooitgedacht left the British hopelessly outmanoeuvred, in one of many battles fought for control of the Magaliesberg in the Anglo-Boer or South Africa War of The beauty of the Magaliesberg belies the fact that it was the scene of 10 fierce battles between the two forces.
In the Battle of Nooitgedacht the Boers gave the British a thorough hiding but in the end it was to no avail – the sheer force of numbers of the British finally forced the Boers out of the Magaliesberg. These battles provided the Boers with excellent training in the guerrilla tactics that helped them win many battles against a better-armed and larger force.