The Okavango Delta

The Okavango Delta, situated in northern Botswana, is a large alluvial fan (40,000 km2 ) lying within grabens of the southern extension of the East African Rift system (Scholtz, 1975). The Okavango Delta is situated within two major grabens, one containing the Panhandle and the other the Delta itself (McCarthy et al., 1998). The delta is located at the terminus of the Okavango River and is a terminal depository for the Okavango River system, which drains central Angola (McCarthy and Metcalfe, 1990; McCarthy, 2013). Topographic gradients on the fan are low, and at the fan the Okavango River forms a system of anastomosing channels flanked by perennial and seasonal swamps (McCarthy and Metcalfe, 1990). The river discharges about 10 km3 of water onto the fan each year, augmented by about 6 km3 of rainfall, which sustains about 2500 km2 of permanent wetland and up to 8000 km2 of seasonal wetland (McCarthy, 2006). The Okavango is a large low gradient Inland delta and is Africa’s largest endorheic delta and the third biggest alluvial fan in Arica. It is largely untransformed wetland system, with uniquely adapted biota timed with the arrival of flood water in the dry, winter season of Botswana (World Heritage Nomination Dossier, 2013).