This park contains wildlife such as giraffe, elephant, white rhinoceros, Cape buffalo, spotted hyena, brown hyena, honey badger, meerkat, yellow mongoose, warthog, cheetah, caracal, Cape wild dog, black-backed jackal, bat-eared fox, cape fox, leopard, lion, wildebeest, zebra, eland, sable antelope, gemsbok, springbok, steenbok, impala, greater kudu, aardvark, cape ground squirrel, cape hare, cape porcupine, chacma baboon, red hartebeest and ostrich. The land is mostly flat, and gently undulating covered with bush and grasses covering the sand dunes, and areas of larger trees. Many of the river valleys are fossilized with salt pans. Four fossilized rivers meander through the reserve including Deception Valley which began to form around 16,000 years ago
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The Cuando River is a river in south-central Africa flowing through Angola and Namibia's Caprivi Strip and into the Linyanti Swamp on the northern border of Botswana. Below the swamp, the river is called the Linyanti River and, farther east, the Chobe River, before it flows into the Zambezi River.
The Cuando system is noted for its wildlife and for most of its length the land either side is protected as game reserves or wildlife management areas. Some of these suffered poaching during wars and conflict in Namibia and Angola, but with peace restored in those countries they have the chance of returning to their former state.
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Khwai is a village on the north bank of the Khwai River in the North-West District of Botswana. The river is the northern boundary of the Moremi Game Reserve, and the village is just outside the north gate of the reserve, which is on the eastern side of the Okavango Delta.
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The Okavango Delta in Botswana is a swampy inland delta formed where the Okavango River reaches a tectonic trough in the central part of the endorheic basin of the Kalahari. All the water reaching the delta is ultimately evaporated and transpired and does not flow into any sea or ocean.
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The Makgadikgadi Pan, a salt pan situated in the middle of the dry savanna of north-eastern Botswana, is one of the largest salt flats in the world. The pan is all that remains of the formerly enormous Lake Makgadikgadi, which once covered an area larger than Switzerland, but dried up tens of thousands of years ago
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Savute, a remote and wild corner of Chobe National Park,
stretches from the park’s northern boundaries to the Linyanti
River. The area’s main feature is the mysterious Savute
Channel, which flows and dries up seemingly unrelated to
the rainfall. Dry and arid for almost 30 years, animals in
the area were sustained by artificial waterholes. With the
Savute Channel flowing again in recent years, the region has
undergone a startling transformation, reverting to its natural
lush and marshy state. Large numbers of wildlife have been
attracted to this rejuvenated wilderness haven.
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