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Botswana MenuHighlights
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The source of the Okavango DeltaSpurred by huge subtropical storms, the Cubango River rises in central Angola, flows through Namibia as the Kuvango River and finally enters Botswana as the Okavango River at Mohembo in the north. With it comes some 11 billion cubic metres of water each year which drains away through a maze of lagoons, channels and islands before disappearing into the Kalahari wastes of the south. This is the Okavango Delta, some 15000 square kilometres of wetland with a special diversity of fauna and flora. The Okavango River is funnelled through parallel faults of the Panhandle as a deep and fast-flowing river before being confronted by another perpendicular fault with a sudden increase in gradient. This slows the flow of water considerably as it spreads into relatively shallow sediment with a fall of only 62 metres over approximately 250 kilometres. The Okavango's seasonal floodsAn important feature of the Okavango is the seasonal flooding which commences in mid-summer in the north and ends about six months later in the south. This results in a cyclical motion of water rising in the north as it recedes in the south during summer, and a rising in the south as it drops in the north during winter. The nature of the annual floods is gentle with floodplains and islands disappearing under water and then reappearing in an ever-changing landscape at the end of each season - this is particularly pronounced in the central Okavango. The flood zonesThe Delta can be reasonably well divided between a permanently flooded zone in the north and a seasonally flooded zone in the south.
MoremiThe Moremi Game Reserve and its surrounds is the focal point for safaris in the Okavango and includes habitats from both the permanently and seasonally flooded zones. With the exception of the eastern "tongue" of Moremi, access into the Okavango Delta is by aircraft. |
Botswana MenuHighlights
| Last updated 10 June, 2000 |
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