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The Cape Flats, characterized by relatively flat surface and vegetation of thick Coastal Fynbos, represent the Late-Tertiary and Recent sands unit up to 50 m thick in places. The sandy aquifer is underlain by Precambrian and Palaeozoic rocks belonging to the Cape granite suite, the Malmesbury Formation, and the Table Mountain Group. With a long- term mean annual precipitation (MAP) of 600 mm, the management of the groundwater resource in this area becomes necessary. This book reviews the history and problems of groundwater development, and provides extensive information on the...