Karoo historical Karoo described in South African atlases and guide books (compare the map on the right with the map at the beginning of the article). The Succulent Karoo biome runs along the West Coast, from approximately Lamberts Bay northwards to over 200 km into southern Namibia. It starts in the south just north of the Sandveld geographical region, about 250 km north of Cape Town, and continues through Namaqualand, the Richtersveld, immediately south of the Orange River, and on into the Namaqualand or Namaland region of southern Namibia. None of these regions is ever referred to, either geographically or locally,
Karoo National Park Karoo paleontologically famous. Their fossils have been found all over the Karoo. Some of these fossils are on display in the Park, though none of them have been found there. About 60 million years after the Beaufort sediments had been laid down and topped with a thick layer of desert sands, there was an outpouring of lava on to Southern Africa on a titanic scale. The entire area was covered within a very short space of time with a 1.5 km thick layer of lava, the remnants of which form the Drakensberg. In addition to flooding the African surface with