Introduction
The variation of geology, soils and rainfall over the CWCBR has produced a region with great bio diversity. The soils in particular, with a gradual transition from calcareous sands to acid soils, and a juxtaposition of these soils with those of the shales and granites have a marked influence on vegetation. The result is a rich flora with over 1500 species within the CWCBR.
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Vegetation An analysis of the floras of the BR indicates several centres of floral diversity and concentration and species diversity. |
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History Prior to European settlers moving into the West Coast area, hunter-gatherers inhabited the region. They were followed by the Khoi herders who grazed sheep and cattle in the region for at least 2 000 years. These nomadic herders practiced burning of the veld to stimulate regrowth for grazing purposes.
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West Coast Fossil Park The fossil occurrences at Langebaanweg are among the most extensive of the Late Tertiary period. At this site a set of circumstances have made it possible to discover and recover a veritable treasure trove of fossils. |
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West Coast National Park The West Coast National Park, which constitutes the Northern Core Area first received official statutory conservation status on 14 December 1984 when the Langebaan Lagoon; the Admiralty Zone (a strip of land of ±38m along the high water mark); portions of Sixteen-Mile beach; and certain farms adjacent to the Lagoon were proclaimed the Langebaan Nature Area. |
