Chobe National Park
Whether arriving by air or road, the first glimpse of the river – deep and dazzling in the sandy terrain – is always breathtaking. It appears as a swathe of brilliant, peacock blue ribbon, winding its way through the tiny town of Kasane, and ensuing wilderness – the Chobe National Park.
Undoubtedly one of Africa’s most beautiful rivers, the Chobe supports a diversity and concentration of wildlife unparalled anywhere else in the country.
Established in 1968, the park covers approximately 11 7 00 sq kms, encompassing floodplains, swamps and woodland. The Chobe River forms its northern boundary. There are four distinct geographical areas in the park: the Chobe Riverfront, the Ngwezumba pans, Savuté and Linyanti.
The most accessible and frequently visited of Botswana’s big game country, the Chobe Riverfront is most famous for its large herds of elephants and cape Buffalo, which during the dry winter months converge upon the river to drink.
During this season, on an afternoon game drive, you may see hundreds of elephants at one time. You may be surrounded by elephants, as the main Serondella road becomes impassable and scores of family herds cross the main road to make their way to the river to drink, bathe and play.
Driving the loops that hug the river’s edge, you may see up to 15 different species of animals on any one game drive, including waterbuck, lechwe, puku (this is the only part of Botswana where they can be seen), giraffe, kudu, roan and sable, impala, warthog, bushbuck, monkeys and baboons, along with the accompanying predators lion, leopard, hyena and jackal.
Take a river cruise – and you’ll experience the park, and the animals, from another vantage point. Here you’ll get up close and personal with hippo, crocodile and a mind-boggling array of water birds.
Over 460 bird species have been recorded in the park, making it one of Africa’s premier venues for bird Safaris. Common species to be seen include the Sacred ibis, Egyptian Geese, the ubiquitous cormorants and darters, Spur-winged Geese, pel’s Fishing Owl, carmine Bee-eaters, most members of the kingfisher family, all the rollers, the unmistakable Fish Eagle, the Martial Eagle, and many members of the stork family.
The Chobe River rises in the northern Angolan highlands, travels enormous distances before it reaches Botswana at Ngoma. Like the Okavango and Zambezi rivers, the Chobe’s course is affected by fault lines that are extensions of the Great Rift Valley. These three mighty rivers carry more water than all other rivers in Southern Africa.
The Ngwezumba pans lie approximately 70 kms south of the Chobe River and comprise a large complex of clay pans, surrounded by mophane woodlands and grassland plains.
During the rainy season, the pans fill with water, then attracting wildlife that move away from the permanent water sources of the Linyanti and Chobe Rivers.
During the dry winter months, gameviewing at the permanent waters of the Linyanti can be excellent.
The area that falls within the Chobe National Park, which has a public campsite, is sandwiched between photographic concessions to the west and hunting concessions to the east.
Truly at the interior of the park, Savuté boasts most of the chobe species, except for water-loving antelope. It is best known for its predators,particularly lion, cheetah and hyena, of which there are large resident populations.
The Savuté channel flows from the Linyanti River for about 100 kilometres, carrying water away from the river and releasing it into a vast swampland called the Savuté Marsh, and further south onto the Mababe Depression, which is also fed by the Ngwezumba River from the northeast. The Mababe – immense and flat and fringed by thickets of trees – was once part of the Makgadikgadi super-lake. When filled with water, it becomes the venue for thousands of migratory birds and animals, particularly large herds of zebra.
Geographically, Savuté is an area of many curiosities. One of its greatest mysteries is the Savuté channel itself, which has over the past 100 year inexplicably dried up and recommenced its flow several times. This irregular water flow explains the numerous dead trees that line the channel, for they have germinated and grown when the channel was dry and drowned when the channel flowed again.