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  • Kimberley, South Africa: miners and washing gear at the Bultfontein diamond mine

    Woodburytype
  • Griqualand West, South Africa: Kimberley diamond mine.

    Woodburytype
  • Kimberley Mine

    A detail from the wallpaper used outside the Cape Town Diamond Museum in the V&A Waterfront.
  • Kimberley Mine 1886

    Plate from Williams, G. 1902. 'The Diamond Mines of South Africa: Some Account of their Rise and Development'. New York, London: Macmillan.
  • Kimberlite

    A display outside the Cape Town Diamond Museum in the V&A Waterfront
  • Kimberlite

    Kimberlite specimens, UCT Mantle Room
  • Kimberlite

    Kimberlite specimen, UCT Mantle Room
  • The Diamond Mines of South Africa: Some Account of their Rise and Development.

    “In the mines operated by the De Beers Company alone, more than eleven thousand African natives are employed below and above ground, coming from the Transvaal, Basutoland, and Bechuanaland, from districts far north of the Limpopo and the Zambesi, and from the Cape Colony on the east and the south to meet the swarms flocking from Delagoa Bay and countries along the coast of the Indian Ocean, while a few cross the continent from Damaraland and Namaqualand, and the coast washed by the Atlantic. The larger number are roughly classed as Basutos, Shanganes, M'umbanes, and Zulus, but there are many Batlapins from Bechuanaland, Amafengu, and a sprinkling of nearly every other tribe in South Africa” (Williams 1902: 412-413). ​
  • The Diamond Mines of South Africa: Some Account of their Rise and Development.

    “The initial impetus for establishing a collection of mantle materials for research purposes in South Africa was provided by Gardner Williams and his son Alpheus Williams in the late 19th and early 20th century. These two American mining engineers shared a great interest in the mining methods and geology of the South African kimberlite-hosted diamond mines they were supervising. Each wrote books on the subject and the two men assembled a collection of scientifically interesting rock samples and minerals from the mines. Subsequent to the death of Alpheus Williams, the Williams family donated this collection to the Geology Department at UCT for teaching and research purposes” (Department of Geological Sciences 2021).
  • Deductions from smooth rocks

    Extract from Bettie Higgs's reading of rocks in 'Visual Practices Across the University'. Most of the rocks in this photograph are about 360 million years old, so the grains that comprise them are substantially older. The grains came originally from a mountain range, as large as the Himalayas, whose roots can still be seen in counties Mayo and Donegal, in the northwest of Ireland. The grains were carried south by rivers and deposited in this area; the smallest grains were carried all the way to the ocean, which was far south of Cork at the time, in what is now the Atlantic Ocean south of Ireland. (There was very little rainfall at the time: the portion of land that is now Cork was 10° south of the Equator. This can be deduced from the properties of the iron in the rock.) The water in which the grains were transported was oxygenated, and the iron precipitated out as iron oxide (haematite), which cemented the grains and which accounts for the red color (Elkins 2007: 74 - 78).
  • Big Good Strong Hands...

    The 1984 film, 'The Neverending Story', features Pyornkrachzark, the Rockbiter, a large creature made of stone. The Rockbiter species are named due to their diet of rocks and earth-based materials. The Rockbiter seen in the film particularly has a liking for limestone. In the novel and the first film, the Rockbiter appears early among the messengers sent to see the Childlike Empress at the Ivory Tower during the Nothing crisis. In the first film he ultimately reappears, encountered by Atreyu. He has lost faith in himself after failing to save his travelling companions from the Nothing, and advises Atreyu to flee.
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