Robertson Karoo Robertson Karoo Robertson Karoo is a semi-arid vegetation type, restricted to sections of the Breede River Valley, Western Cape Province, South Africa. It is a subtype of Succulent Karoo (geographically an extension of the "Little Karoo") and is characterised by the dominance of succulent plant species, and by several endemic plants and animals. This vegetation type occurs in several large patches within the Breede River Valley, in the Western Cape Province of South Africa. It occurs in the area between Worcester in the north-west, Ashton in the east, and the Riviersonderend mountains in the south. Robertson Karoo typically consists of
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