| Lake Bangweulu | |
|---|---|
 Locals on the shore of Lake Bangweulu | |
  Lake Bangweulu  Lake Bangweulu | |
| Location | Luapula Province andNorthern Province |
| Coordinates | 11°05′S29°45′E / 11.083°S 29.750°E /-11.083; 29.750 |
| Primary inflows | Chambeshi |
| Primary outflows | Luapula River |
| Basin countries | Zambia |
| Surface area | 15,100 km2 (5,800 sq mi) |
| Water volume | 5,000 million cubic metres (4,100,000 acre⋅ft) |
| Surface elevation | 1,140 m (3,740 ft) |
| Official name | Bangweulu Swamps |
| Designated | 28 August 1991 |
| Reference no. | 531[1] |
Lake Bangweulu ('where the water sky meets the sky'[2]) is afreshwaterlake in northernZambia. Bangweulu is one of the world's greatwetland systems, comprisingLake Bangweulu, theBangweulu Wetlands and the Bangweulu flats orfloodplain.[3] Situated in the upperCongo River basin in Zambia, the Bangweulu system covers an almost completely flat area roughly the size ofConnecticut orEast Anglia, at an elevation of 1,140 m straddling Zambia'sLuapula Province andNorthern Province. It is crucial to the economy and biodiversity of northern Zambia, and to the birdlife of a much larger region, and facesenvironmental stress andconservation issues.[4]
With a long axis of 75 km and a width of up to 40 km, Lake Bangweulu's permanent open water surface is about 3,000 km2, which expands when its swamps andfloodplains are in flood at the end of therainy season in May. The combined area of the lake and wetlands reaches 15,000 km2. The lake has an average depth of only 4 m,[5][6] and a maximum depth of 10 m.[7]
The Bangweulu system is fed by about seventeen rivers of which theChambeshi (the source of the Congo River) is the largest, and is drained by theLuapula River.[3]
The lake was known to Europeans from reports by chiefs such asKazembe and fromSwahili traders, and it was sometimes referred to as 'Lake Bemba' from the name of the dominant tribe. In 1868 explorer and missionaryDavid Livingstone was the first European to see the lake at the north end of the Lake Chifunabuli section. He was taken by canoe as far as Mbabala Island. His last expedition a few years later foundered in the swamps and their maze of shifting channels as he struggled to discover the rivers draining in and out of the lake. He died in 1873 in Chief Chitambo's village on the edge of the southern flood plain, about 100 km from the lake itself.[8] The spot is marked by theLivingstone Memorial (see map). The lake was partially surveyed in 1883 by the French traveller, Victor Giraud, and first circumnavigated by Poulett Weatherley in 1896.[9]
It was a desire for the riches of Bangweulu's fisheries and game-rich floodplain which motivated KingLeopold II of Belgium to insist, in border negotiations between hisCongo Free State and theBritish inNorthern Rhodesia, on a land corridor reaching Bangweulu fromKatanga. This resulted in the shape of theCongo Pedicle(34) which, as it turned out, does not penetrate the area enough to be of the desired value.
The firstChristian missions in Bangweulu were founded in the early 1900s under the authority ofBishop Joseph Dupont of theCatholicWhite Fathers who was based north ofKasama.
The area of the lake is inhabited by the Bisa inChilubi andMpika, theBemba inLuwingu, the Unga inLunga, the Kabende inSamfya, the Ngumbo in Lubwe, the BenaMukulu in Chungu and affiliated tribes who all speakChibemba. The Bemba heartland ofParamount ChiefChitimukulu lies to the north-east, aroundKasama.
The lake supports a seasonalfishing industry and the population may increase markedly during the season. In 1989 the average annual catch was estimated at 11,900 tonnes, caught by 10,300 people using 5305dugout canoes, 114 plank and fibreglass boats, and only 54outboard motors. In 2000 the catch was 13,500 t.[10]
In early 2004 a private European natural gas company finished preliminary plans to lay a pipeline which would cut directly through the Southeast portion of the lake. Part of this plan was a proposed dam to allow for partial drainage of the required part of the lake. This plan was met with harsh opposition from the local people as well as environmental activists. After much court-wrangling and lengthy hearings on the project, the plan was disposed of by the European company as they built a detour for their pipeline in the surrounding province.[citation needed]
The largest town,Samfya lies on the south-western shore and is the principal base for road and boat transport and tourism, as well as being the administrative centre for Samfya District covering about three-quarters of the lake and swamps.Chilubi District covers most of the rest, itsboma is on Chilubi Island(6), which is bordered by the swamps to the east.Luwingu District just touches the lake atNsombo, which is the principal town at the northern end of the lake.Mpika andKasama districts just touch the eastern and southern margins of the floodplain, andSerenje District and the Congo Pedicle just reach the southern margin of the floodplain.
A notable feature of the Bangweulu system is a series of parallel sandy ridges running south-west to north-east. These are particularly striking in satellite photographs and are easily seen along the north-western shore, the Lifunge Peninsula(2), Mbalala Island(3), Chilubi Island(6), and the Kapata Peninsula(10). They divide the lake into three sections parallel to its main axis. One divides off a section called Lake Chifunabuli(1), 50 km long but only 5 km wide. Its entrance through a gap in the sand spits (at the end of Lifunge Peninsula) is only 250 m wide. Another sandy ridge, Mbabala Island, divides off a section called Lake Walilupe(4), 30 km long by 13 km wide. The main, middle section of the lake between Ifunge and Mbabala is known only as Bangweulu.[11]
There are numerous bays, inlets, smaller lakes and lagoons around Lake Bangweulu, connected by open water, narrow channels or swamps. The largest is Lake Kampolombo(9), 30 km by 5 km, south of Lake Walilupe and connected to it by a 7 km channel. The 32 km long Kapata Peninsula lies between Lake Kampolombo and the swamps; at its tip on the eastern side is the 15 km long Lake Kangwena(11).[11]
Only the western side of the lake and some of the islands have a well defined shore, with sandy beaches in places especially around Samfya, though even there, some of the bays and inlets are swampy.[5][12]
It was found that infection withSchistosoma haematobium on the western shores of Lake Bangweulu, Zambia, is higher than previously reported.[13]
The Bangweulu Swamps, larger than the lake, extend from the north-west clockwise around to the south. The main part covers an area of roughly 120 km by 75 km and they are normally not less than 9,000 km2.[5][6]
The swamps act as a check on annual flooding downstream in the Luapula by releasing water slowly through many lagoons and channels. They help prevent the Luapula valley being flooded excessively in the rainy season.
The Bangweulu swamps are fed mainly from the north-east by theChambeshi River, and drain to the south into theLuapula River. The lake is connected to these rivers, and they to each other, by a complex mass of channels through the swamps that may become choked by vegetation and change their course; there is no easy navigation between them. Floating beds of papyrus may close up the channels to a width allowing only dugout canoes to pass. Motorised vessels are hampered by their width as well as by vegetation clogging propellers. Since colonial times attempts have been made to improve navigation and alter drainage patterns by cutting channels through the swamp. In 1942, attempts were made, with limited success, to cut an outlet from Lake Walilupe to the Luapula's exit from the swamps, to allow motor boats to transport cassava and other produce from the northern area of the lake toKapalala Ferry on the Luapula and from there to theCopperbelt.[12][14]
There are numerous lagoons in the swamps, the more prominent ones are:Lake Chali (12) in the south-west,Lake Chaya (13) in the east at the mouth of the Lulingilla River in the east,Lake Wumba (14) in the north-east at the confluence of the Chambeshi and Luansenshi(20) Rivers, and thePook Lagoon (15) in the East near Nsalushi Island(25).[11]
On the northern side there are several wide swampy estuaries where rivers enter the lake or swamps, going from north-west to north-east they are: Lupososhi Estuary(16), Luena Estuary(17), Lukuto Estuary(18), Chambeshi Estuary(19) (and Luansenshi Estuary which feeds into it).[11]
On the eastern and south-eastern sides the swamps are fed by the Munikashi, Luitikila, Lumbatwa, Lukulu and Lulimala rivers.[11] The estuaries of the last three are the main dry season grazing grounds of the Black Lechwe.
In the main part of the swamps, just south of Chilubi Island, is a large area which is very shallow in the flood season and may become fairly dry at the end of the dry season, called the Lunga Bank(27).
An area of about 3,000 km2 of large grassy floodplains lies mainly south of the swamps, but also in the north-north-east, acting as an extension of the region in the wet season. The southern floodplains are famous for large herds of the near-endemicblack lechwe. Further information on wildlife of the wetlands is found on theBangweulu Wetlands page.
Water temperatures at the surface of the Bangweulu system ranged from 25.8 to 28.3 °C in November 1993 and from 23.7 to 27.1 °C in February 1994.[15] The conductivity of the Bangweulu system is unusually low and varies between 20 and 40 μS/cm.[15] Transparency of the water ranges from 0.35 to 0.60 m in most water bodies of the system, but in the Tuchingo lagoon the transparency is much larger (>1.70 m) allowing the bottom to be seen.[15]
There are numerous inhabited islands in the Bangweulu system.[11]
On the lake they are:
In the swamps:
Flood season islands: on the edge of the swamps, connected to the mainland in the dry season:
One or more of the preceding sentences incorporates text from a publication now in thepublic domain: Chisholm, Hugh, ed. (1911). "Bangweulu".Encyclopædia Britannica. Vol. 3 (11th ed.). Cambridge University Press. p. 318.
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