Lake Bangweulu | |
---|---|
Location | Luapula Province and Northern Province |
Coordinates | 11°05′S29°45′E / 11.083°S 29.750°E |
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 a freshwater lake in northern Zambia. Bangweulu is one of the world's great wetland systems, comprising Lake Bangweulu, the Bangweulu Wetlands and the Bangweulu flats or floodplain. [3] Situated in the upper Congo River basin in Zambia, the Bangweulu system covers an almost completely flat area roughly the size of Connecticut or East Anglia, at an elevation of 1,140 m straddling Zambia's Luapula Province and Northern Province. It is crucial to the economy and biodiversity of northern Zambia, and to the birdlife of a much larger region, and faces environmental stress and conservation 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 and floodplains are in flood at the end of the rainy 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 the Chambeshi (the source of the Congo River) is the largest, and is drained by the Luapula River. [3]
The lake was known to Europeans from reports by chiefs such as Kazembe and from Swahili traders, and it was sometimes referred to as 'Lake Bemba' from the name of the dominant tribe. In 1868 explorer and missionary David 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 the Livingstone 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 King Leopold II of Belgium to insist, in border negotiations between his Congo Free State and the British in Northern Rhodesia, on a land corridor reaching Bangweulu from Katanga. This resulted in the shape of the Congo Pedicle (34) which, as it turned out, does not penetrate the area enough to be of the desired value.
The first Christian missions in Bangweulu were founded in the early 1900s under the authority of Bishop Joseph Dupont of the Catholic White Fathers who was based north of Kasama.
The area of the lake is inhabited by the Bisa in Chilubi and Mpika, the Bemba in Luwingu, the Unga in Lunga, the Kabende in Samfya, the Ngumbo in Lubwe, the BenaMukulu in Chungu and affiliated tribes who all speak Chibemba. The Bemba heartland of Paramount Chief Chitimukulu lies to the north-east, around Kasama.
The lake supports a seasonal fishing 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 5305 dugout canoes, 114 plank and fibreglass boats, and only 54 outboard 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, its boma is on Chilubi Island (6), which is bordered by the swamps to the east. Luwingu District just touches the lake at Nsombo, which is the principal town at the northern end of the lake. Mpika and Kasama districts just touch the eastern and southern margins of the floodplain, and Serenje 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 with Schistosoma 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 the Chambeshi River, and drain to the south into the Luapula 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 to Kapalala Ferry on the Luapula and from there to the Copperbelt. [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 the Pook 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).
Large grassy floodplains with an area of about 3,000 km2 lie 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-endemic black lechwe. Further information on wildlife of the wetlands is found on the Bangweulu 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:
This article is about the Transport in Zambia.
Lake Mweru is a freshwater lake on the longest arm of Africa's second-longest river, the Congo. Located on the border between Zambia and Democratic Republic of the Congo, it makes up 110 kilometres (68 mi) of the total length of the Congo, lying between its Luapula River (upstream) and Luvua River (downstream) segments.
The Luapula River is a north-flowing river of central Africa, within the Congo River watershed. It rises in the wetlands of Lake Bangweulu (Zambia), which are fed by the Chambeshi River. The Luapula flows west then north, marking the border between Zambia and the Democratic Republic of the Congo before emptying into Lake Mweru. The river gives its name to Zambia's Luapula Province.
The ChambeshiRiver of northeastern Zambia is the most remote headstream of the Congo River and therefore it is considered the source of the Congo River.
Northern Province is one of Zambia's ten provinces. It covers approximately one-sixth of Zambia in land area. The provincial capital is Kasama. The province is made up of 12 districts, namely Kasama District, Chilubi District, Kaputa District, Luwingu District, Mbala District, Mporokoso District, Mpulungu District, Mungwi District, Nsama District, Lupososhi District, Lunte District and Senga Hill District. Currently, only Kasama and Mbala have attained municipal council status, while the rest are still district councils. It is widely considered to be the heartland of the Bemba, one of the largest tribes in Zambia.
Samfya is a town located in the Zambian province of Luapula. It is the centre of Samfya District. The town is located on the south-western shore of Lake Bangweulu, on the longest stretch of well-defined shore of that lake. Samfya has a few guesthouses and a number of white sandy beaches which are used for recreation, although the lake does have crocodiles.
Luapula Province is one of Zambia's ten provinces located in the northern part of the country. Luapula Province is named after the Luapula River and its capital is Mansa. As per the 2022 Zambian census, the Province had a population of 1,519,478, which accounted for 7.72 per cent of the total Zambian population.
The Bemba belong to a large group of Bantu peoples, primarily in the Northern, Luapula, Muchinga and the northern Central Province of Zambia. The Bemba entered Zambia before 1740 by crossing the Luapula River from Kola. Several other ethnic groups in the northern and Luapula regions of Zambia speak languages which are similar to Bemba, but have different origins. The Bemba people are not indigenous to Copperbelt Province; they arrived there during the 1930s due to employment opportunities in copper mining.
Kazembe is a name used for Mwata Kazembe's town in the Luapula Province of Zambia, especially on maps and in the Zambian postal service. The other name for the town is Mwansabombwe and this is the one used by its or Luba or Chibemba-speaking inhabitants. They may refer in English to "Kazembe's Village" or just "Kazembe", as traditionally a settlement is named after the chief or headman, rather than the location. The Luba-Lunda shared with many tribes the custom of moving to another village or a new site on the death of the chief. Historical references to a village or town may actually be to a different location. For instance when the explorer David Livingstone visited Mwata Kazembe in 1867 and 1868, "Casembe's town", as he wrote it, was further north at the town now called Kanyembo.
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The Congo Pedicle road crosses the Congolese territory of the Congo Pedicle and was constructed by and is maintained by Zambia to connect its Copperbelt and Luapula Provinces. Both the road and the territory may be referred to as ‘the Pedicle’. It is designated as the N36 Route on the Congolese Road Network.
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Chilubi is a settlement on an island in Lake Bangweulu and its swamps, and is headquarters of Chilubi District in the Northern Province of Zambia.
The wildlife of Zambia refers to the natural flora and fauna of Zambia. This article provides an overview, and outline of the main wildlife areas or regions, and compact lists of animals focusing on prevalence and distribution in the country rather than on taxonomy. More specialized articles on particular groups are linked from here.
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The biomes and ecoregions in the ecology of Zambia are described, listed and mapped here, following the World Wildlife Fund's classification scheme for terrestrial ecoregions, and the WWF freshwater ecoregion classification for rivers, lakes and wetlands. Zambia is in the Zambezian region of the Afrotropical biogeographic realm. Three terrestrial biomes are well represented in the country . The distribution of the biomes and ecoregions is governed mainly by the physical environment, especially climate.
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Zambia, officially known as the Republic of Zambia, is a landlocked country in Southern Africa. The neighbouring countries are the Democratic Republic of the Congo to the north, Tanzania to the north-east, Malawi to the east, Mozambique, Zimbabwe, Botswana, and Namibia to the south, and Angola to the west. The capital city is Lusaka, located in the southeast of the country. The population is concentrated mainly around the capital and the Copperbelt to the northwest.
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Samfya District is located in Luapula Province, Zambia. The headquarters is at Samfya.
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