Kafue National Park is the largest national park in Zambia, covering an area of about 22,400 km2 (similar in size to Wales or Massachusetts). It is one of the largest parks in Africa and is home to 152 different species of mammals. The park is named for the Kafue River. It stretches over three provinces: North Western, Central and Southern. The main access is via the Lusaka–Mongu Road from Lusaka to Mongu which crosses the park north of its centre. Seasonal dirt roads also link from Kalomo and Namwala in the south and south-east, and Kasempa in the north. History Kafue National Park was established in the 1950s by Norman Carr, an influential British-Rhodesian conservationist. Establishment may have been possible after the British colonial government moved the traditional owners of the area, the Nkoya people of (King) Mwene Kabulwebulwe, from their traditional hunting grounds into the Mumbwa District to the east in 1924. Dissatisfaction with the pace of development in Central Province and a lack of benefit from tourism in the park have led to calls from Nkoya leaders to establish a new province in the area which they have proposed to call Kafue Province. Geology and climate The country is generally flat or gently undulating apart from some small, steep porphyritic granite hills between Chonga and Ngoma and occasional sandstone and granite hills around Ngoma rising to . The southwestern part of the Hook granite massif underlies the central part of the park, including schist, gneiss, granite-gneiss and granite. On the edge of the granite massif there are slates, quartzites and limestones from the Katanga sediments of the inner Lufilian Arc. To the north and south of the massif the soil covers Karroo sediments of shales, siltstones, concreted gravels and various types of laterite. In the northern end of the park the flood plains have clay soils, but otherwise the soils are strongly leached sandy to loamy soils with low fertility. In most of the drainage of the Nanzila river, and in some of the lands around the Nkala, Musa and Lwansanza rivers, there are dark grey alkaline clays. Otherwise, the park is covered by well-drained and relatively infertile pale or orange Kalahari sands mixed with some silt and clay. The main tributaries to the Kafue river in this park are the Lufupa and Lunga rivers in the north, the Luansanza (or Lwansanza) in the centre and the Musa