Kalahari Meerkat Project Northern Cape, South Africa, close to the border to Botswana, the project is jointly funded by Cambridge University and the Kalahari Research Trust. The project was founded in the early nineties by researchers (Prof. Tim Clutton-Brock) at Cambridge University. It was originally based on the Kgalagadi Transfrontier Park, but in 1993 moved to the Kuruman River Reserve, an area spanning approximately twenty square miles of semi-arid area of the Kalahari Desert on either side of the mostly dry Kuruman River. The reserve consists primarily of sparsely vegetated fossil dunes that flatten out near the river, which is usually dry. The
Kalahari Craton Archaean-Palaeoproterozoic core of the craton is called the Proto-Kalahari Craton. This core plus accreted Mesoproterozoic crust and dispersed non-African fragments compose the Kalahari Craton. Before the Pan-African Orogeny, the Kalahari Craton was much larger than it is today, but its sutures and therefore its extent are difficult to locate due to later overprinting. The Kaapvaal Craton, Zimbabwe Craton, and Limpopo Belt are made of Archaean terranes and contain crust at least 3.2 and are underlain by a thick () layer of buoyant mantle that is producing garnets and diamonds. During the Palaeoproterozoic the northwest margin of the Archaean core grew