Zambezi

Zambezi
Physical characteristics
Mouth	Indian Ocean
Length	2,574 km (1,599 mi)

(also spelled Zambesi) is the fourth-longest river in Africa, and the largest flowing into the Indian Ocean. The area of its basin is 1,390,000  km² (537,000 miles²), slightly less than half that of the Nile. The 2,574 km- (1,600 mile-) long river has its source in Zambia and flows through Angola, along the borders of Namibia, Botswana, Zambia, and Zimbabwe, to Mozambique, where it empties into the Indian Ocean.

The Zambezi's most spectacular feature is Victoria Falls, the world's largest waterfalls. Other notable falls include the Chavuma Falls at the border between Zambia and Angola, and Ngonye Falls, near Sioma in Western Zambia. Over its entire course, the Zambezi is spanned by only five bridges: at Chinyingi, Katima Mulilo, Victoria Falls, Chirundu and Tete.

There are two main sources of hydroelectric power on the river. These are the Kariba Dam, which provides power to Zambia and Zimbabwe and the Cahora Bassa Dam in Mozambique which provides power to South Africa. There is also a smaller power station at Victoria Falls.

The river rises in a black marshy bog in north-western Zambia, in undulating forested hills about 1,500 metres (4,900 ft) above sea level. Eastward of the source the watershed between the Congo and Zambezi basins is a well-marked belt of high ground, falling abruptly north and south, and running nearly east-west between 11 and 12° S. This distinctly cuts off the basin of the Lualaba (the main branch of the upper Congo) from that of the Zambezi. In the neighbourhood of the source the watershed is not as clearly defined, but the two river systems do not connect.

The upper river

After flowing to the south-west for about 240 km (150 miles), the river turns south, and is joined by many tributaries. A few miles above Kakengi, the river widens from 100 to 350 metres (330 to 1,150 ft), and below Kakengi are a number of rapids ending in the Chavuma Falls, where the river flows through a rocky fissure. The first of its large tributaries to enter the Zambezi is the Kabompo River in the north-western province of Zambia. A little farther south is the confluence with the Lungwebungu River. The savanna through which the river has flowed gives way to a more open bush valley, studded with Borassus palm trees. Dense vegetation is confined to narrow strips of matted forest which skirt the first few hundred metres of the sources of the Zambezi and its tributaries during the first 160 km (100 miles) or so.

Zambezi River in North Western Zambia

From 1500 metres (4,900 ft) at the source, the river drops to about 1100 metres (3,600 ft) at Kakengi, 350 km (220 miles) downstream. From this point until the Victoria Falls, the level of the basin is very uniform, dropping only by another 180 metres (590 ft). Thirty kilometers (19 miles) below the confluence of the Lungwebungu the country becomes flat, and in the rainy season is largely covered by floods. Eighty kilometers (50 miles) further down, the Luanginga, which with its tributaries drains a large area to the west, joins the Zambezi. A few kilometres higher up on the east the main stream is joined in the rainy season by overflow of the Luampa/Luena system.

A short distance downstream of the confluence with the Luanginga is Lealui, one of the capitals of the Lozi people who populate the semi-autonomous Zambian region of Barotseland. The chief of the Lozi has two compounds, the other being at Limulunga. Limulunga is on high ground and serves as the capital during the rainy season. The annual move from Lealui to Limulunga is a major event, celebrated as one of Zambia's best known festivals, the Kuomboka.

After Lealui, the river turns to the south-east. From the east it continues to receive numerous small streams, but on the west is without tributaries for 240 km (150 miles), when the Cuando River joins it. Before this, the Ngonye Falls and subsequent rapids interrupt navigation. South of Ngonye Falls, the river briefly borders Namibia's Caprivi Strip. The strip projects from the main body of Namibia, and results from the colonial era: it was added to German South-West Africa expressly to give Germany access to the Zambezi.

Below the junction of the Cuando and the Zambezi the river bends almost due east. Here, the river is very broad and shallow, and flows fairly slowly, but as it flows eastward towards the border of the great central plateau of Africa it reaches a chasm into which the Victoria Falls plunge.

The middle Zambezi

Victoria Falls, the end of the upper Zambezi and beginning of the middle Zambezi

The Victoria Falls are considered the boundary between the upper and middle Zambezi. Below them the river continues to flow due east for about 200 km (120 miles), cutting through perpendicular walls of basalt 20 to 60 metres (65 to 200 ft) apart in hills 200 to 250 metres (650 to 820 ft) high. The river flows swiftly through the gorge, the current being continually interrupted by reefs. Beyond the gorge are a succession of rapids which end 240 km (150 miles) below Victoria Falls. Over this distance, the river drops 250 metres (820 ft).

At this point, the river enters Lake Kariba, created in 1959 following the completion of the Kariba Dam. The lake is one of the largest man-made lakes in the world, and the hydroelectric power-generating facilities at the dam provide electricity to much of Zambia and Zimbabwe.

The Luangwa and the Kafue are the two largest left-hand tributaries of the Zambezi. The Kafue joins the main river in a quiet deep stream about 180 metres (590 ft) wide. From this point the northward bend of the Zambezi is checked and the stream continues due east. At the confluence of the Luangwa (15°37′ S) it enters Mozambique.

The middle Zambezi ends when the river enters Lake Cahora Bassa (also spelled Cabora Bassa). Formerly the site of dangerous rapids known as Kebrabassa, the lake was created in 1974 by the construction of the Cahora Bassa Dam.

The lower river

The lower Zambezi's 650 km (400 miles) from Cahora Bassa to the Indian Ocean is navigable, although the river is shallow in many places during the dry season. This shallowness arises as the river enters a broad valley and spreads out over a large area. Only at one point, the Lupata Gorge, 320 km (200 miles) from its mouth, is the river confined between high hills. Here it is scarcely 200 metres wide. Elsewhere it is from 5 to 8 km (3 to 5 miles) wide, flowing gently in many streams. The river bed is sandy, and the banks are low and reed-fringed. At places, however, and especially in the rainy season, the streams unite into one broad fast-flowing river.

The Zambezi's delta

About 160 km (100 miles) from the sea the Zambezi receives the drainage of Lake Malawi through the Shire River. On approaching the Indian Ocean, the river splits up into a number of branches and forms a wide delta. Each of the four principal mouths, Milambe, Kongone, Luabo and Timbwe, is obstructed by a sand bar. A more northerly branch, called the Chinde mouth, has a minimum depth at low water of 2 metres at the entrance and 4 metres further in, and is the branch used for navigation. 100 km (60 miles) further north is a river called the Quelimane, after the town at its mouth. This stream, which is silting up, receives the overflow of the Zambezi in the rainy season. The delta of the Zambezi is today about half as broad as it was before the construction of the Kariba and Cahora Bassa dams controlled the seasonal variations in the flow rate of the river.

The region drained by the Zambezi is a vast broken-edged plateau 900–1200 metres high, composed in the remote interior of metamorphic beds and fringed with the igneous rocks of the Victoria Falls. At Shupanga, on the lower Zambezi, thin strata of grey and yellow sandstones, with an occasional band of limestone, crop out on the bed of the river in the dry season, and these persist beyond Tete, where they are associated with extensive seams of coal. Coal is also found in the district just below the Victoria Falls. Gold-bearing rocks occur in several places.

Zambezi Basin

NASA false-colour image of the upper Zambezi and Barotse (Balozi) floodplain in extreme flood in 2003, water shows as dark areas. Blue numbers are rivers: 1 Zambezi source, 2 Zambezi at Chavuma Falls, 3 at start of Barotse Floodplain, 4 at end of the floodplain at the Kalongola Ferry, 5 at Ngonye Falls. Tributaries: 6 Chifumage, 7 Luena, 8 Lungwebungu, 9 Kabompo, 10 Luampa, 11 Luanguinga, 12 Lui, 13 Cuando. Towns (white numbers): 14 Mwinilunga, 15 Cazombo, 16 Zambezi, 17 Lukulu, 18 Limulunga, 19 Lealui, 20 Mongu, 21 Senanga, 22 Sioma. Credit: Jacques Descloitres, MODIS Rapid Response Team, NASA/GSFC.

The north of the Zambezi basin has mean annual rainfall of 1100 to 1400 mm which declines towards the south, reaching about half that figure in the south-west. The rain falls in a 4 to 6 month rainy season when the Inter-Tropical Convergence Zone moves over the basin from the north. Evaporation rates are high (1600mm−2300 mm) and much water is lost this way in swamps and floodplains, especially in the south-west of the basin.

Tributaries, their basin areas, discharge rates, and region drained

Upper Zambezi: 507200 km², discharges 1044 m³/s at Victoria Falls, comprising:

Northern Highlands catchment, 222,570 km², 850 m³/s at Lukulu:

• Chifumage River: Angolan central plateau
• Luena River: Angolan central plateau
• Kabompo River: 72,200 km², NW highlands of Zambia
• Lungwebungu River: 47,400 km², Angolan central plateau

Central Plains catchment, 284,630 km², 196 m³/s (Victoria Falls – Lukulu):

• Luanguingu River: 34,600 km², Angolan central plateau
• Luampa River: 20,500 km², eastern side of Zambezi
• Cuando /Linyanti/Chobe River: 133,200 km², Angolan S plateau & Caprivi

Middle Zambezi cumulatively 1,050,000 km², 2442 m³/s, measured at Cahora Bassa Gorge

(Middle section by itself: 542,800 km², discharges 1398 m³/s (C. Bassa – Victoria Falls)

Gwembe Catchment, 156,600 km², 232 m³/s (Kariba Gorge – Vic Falls):

• Gwayi River: 54,610 km², NW Zimbabwe
• Sengwa River: 25,000 km², North-central Zimbabwe
• Sanyati River: 43,500 km², North-central Zimbabwe

Kariba Gorge to C. Bassa catchment, 386200 km², 1166 m³/s (C. Bassa – Kariba Gorge):

• Kafue River: 154,200 km², 285 m³/s, West-central Zambia & Copperbelt
• Luangwa River: 151,400 km², 547 m³/s, Luangwa Rift Valley & plateau NW of it
• Panhane River: 23,897 km², North-central Zimbabwe plateau

Lower Zambezi cumulatively, 1,378,000 km², 3424 m³/s, measured at Marromeu

(Lower section by itself: 328,000 km², 982 m³/s (Marromeu – C. Bassa))

• Luia River: 28,000 km², Moravia-Angonia plateau, N of Zambezi
• Luenha River/Mazoe River: 54,144 km², 152 m³/s, Manica plateau, NE Zimbabwe
• Shire River , 154,000 km², 539 m³/s, Lake Malawi basin

Zambezi Delta, 12,000 km²

TOTAL ZAMBEZI RIVER BASIN: 1,390,000 km², 3424 m³/s discharged into delta

Source: Beilfuss & Dos Santos (2001)

The Okavango basin is not included in the figures because it only occasionally overflows to any extent into the Zambezi.

Due to the rainfall distribution, northern tributaries contribute much more water than southern ones, for example: the Northern Highlands catchment of the upper Zambezi contributes 25%, Kafue 8%, Luangwa and Shire Rivers 16% each, total 65% of Zambezi discharge. The large Cuando basin in the south-west on the other hand contributes only about 2 m³/s because most is lost through evaporation in its swamp systems.

The 1940s and 1950s were particularly wet decades in the basin. Since 1975, it has been drier, the average discharge being only 70% of that for the years 1930 to 1958.

Floods

Before the dams were built, the lower Zambezi experienced a small flood surge early in the dry season as rain in the Gwembe catchment and north-eastern Zimbabwe rushed through while rain in the Upper Zambezi, Kafue, and Lake Malawi basins, and Luangwa to a lesser extent, is held back by swamps and floodplains. The discharge of these systems contributed to a much larger flood in March or April, with a mean monthly maximum for April of 6700 m³/s at the delta. The record flood was more than three times as big, 22,500 m³/s being recorded in 1958. By contrast the discharge at the end of the dry season averaged just 500 m³/s.

The dams at Kariba, Cahora Bassa and Itezhi-Tezhi on the Kafue have changed that pattern completely. Downstream of the dams, the mean monthly minimum—maximum was 500 m³/s—6000 m³/s, now it is 1000 m³/s—3900 m³/s. Medium-level floods especially, of the kind to which the ecology of the lower Zambezi was adapted, happen less often and have a shorter duration. As with the Itezhi-Tezhi Dam's deleterious effects on the Kafue Flats, this has the following effects:

• fish, bird and other wildlife feeding and breeding patterns disrupted
• less grassland after flooding for grazing wildlife and cattle
• traditional farming and fishing patterns disrupted.

The dams have not removed flooding in the lower Zambezi completely. They can't control extreme floods, they have just made medium-level floods less frequent. When heavy rain in the lower Zambezi combines with good runoff upstream, massive floods still happen, except they are more destructive because the absence of regular medium floods lures people to settle and farm former floodplains, so that when the flood does occur, it causes more damage. This is what happened in the floods of 1997.

Geological changes to the course of the Zambezi

More than two million years ago, the Upper Zambezi river used to flow south through what is now the Makgadikgadi Pan to the Limpopo River. The land around the pan experienced tectonic uplift (perhaps as part of the African superswell) and a large lake formed, and extended east.

Meanwhile, 1000 km east, a western tributary of the Shire River in the Great Rift Valley's southern extension through Malawi eroded a deep valley on its western escarpment. At the rate of a few centimetres per year, this river, the Middle Zambezi, started cutting back the bed of its river towards the west, aided by grabens (rift valleys) forming along its course in an east-west axis. As it did so it captured a number of south-flowing rivers such as the Luangwa and Kafue.

Eventually the large lake trapped at Makgadikgadi (or a tributary of it) was captured by the Middle Zambezi cutting back towards it, and emptied eastwards. The Upper Zambezi was captured as well. The Middle Zambezi was about 300 m lower than the Upper Zambezi, and a high waterfall formed at the edge of the basalt plateau across which the upper river flows. This was the first Victoria Falls, somewhere down the Batoka Gorge near where Lake Kariba is now. For details of how the falls cuts back its bed to form the gorge, see the article on Victoria Falls.

Exploration of the river

Satellite image showing Victoria Falls and subsequent series of zigzagging gorges

The Zambezi region was known to medieval geographers as the Empire of Monomotapa, and the course of the river, as well as the position of Lakes Ngami and Nyasa, were given broadly accurately in early maps. These were probably constructed from Arab information.

The first European to visit the upper Zambezi was David Livingstone in his exploration from Bechuanaland between 1851 and 1853. Two or three years later he descended the Zambezi to its mouth and in the course of this journey discovered the Victoria Falls. During 1858–60, accompanied by John Kirk, Livingstone ascended the river by the Kongone mouth as far as the Falls, and also traced the course of its tributary the Shire and reached Lake Malawi.

For the next 35 years very little exploration of the river took place, but in 1889 the Chinde channel north of the main mouths of the river was discovered. Two expeditions led by Major A. St Hill Gibbons in 1895 to 1896 and 1898 to 1900 continued the work of exploration begun by Livingstone in the upper basin and central course of the river. Portuguese explorer Serpa Pinto examined some of the western tributaries of the river and made measurements of the Victoria Falls in 1878.

Wildlife

The river supports large populations of many animals. Hippopotamuses are abundant along most of the calm stretches of the river, and many crocodiles are also present. Monitor lizards are found in many places. Bird life is abundant, with species including heron, pelican, egret and African Fish Eagle present in large numbers. Riverine woodland also supports many large animals, such as buffalo, zebras, giraffes and elephants. However, below Kariba and Cahora Bassa dams, the cessation of annual flooding has seen the area of this habitat greatly reduced and a corresponding reduction in the populations of the large mammals.

The Zambezi also supports several hundred species of fish, some of which are endemic to the river. Important species include cichlids which are fished heavily for food, as well as catfish, tigerfish, yellowfish and other large species. The bull shark is sometimes known as the Zambezi Shark after the river but is found around the world. It normally inhabits coastal waters but has been found far inland in many large rivers including the Zambezi. It is an aggressive shark which has been responsible for several attacks on humans.

Economy

The river and its floodplain near Mongu in Zambia

The population of the Zambezi river valley is estimated to be about 32 million. About 80% of the population of the valley is dependent on agriculture, and the upper river's flood plains provide good agricultural land.

Communities by the river fish extensively from it, and many people travel from far afield to fish. Some Zambian towns on roads leading to the river levy unofficial 'fish taxes' on people taking Zambezi fish to other parts of the country. As well as fishing for food, game fishing is a significant activity on some parts of the river. Between Mongu and Livingstone, several safari lodges cater for tourists who want to fish for exotic species, and many also catch fish to sell to aquaria.

The river valley is rich in mineral deposits and fossil fuels, and coal mining is important in places. The dams along its length also provide employment for many people near them, in maintaining the hydroelectric power stations and the dams themselves. Several parts of the river are also very popular tourist destinations. Victoria Falls receives over 1.5 million visitors annually, while Mana Pools and Lake Kariba also draw substantial tourist numbers.

Transport

Victoria Falls Bridge. 1975 photo.

The river is frequently interrupted by rapids and so has never been an important long-distance transport route. David Livingstone's Zambezi Expedition attempted to open up the river to navigation by paddle steamer, but was defeated by the Cahora Bassa rapids. Along some stretches, it is often more convenient to travel by canoe along the river rather than on the unimproved roads which are often in very poor condition due to being regularly submerged in flood waters, and many small villages along the banks of the river are only accessible by boat. In the 1930s and 40s a paddle barge service operated on the stretch between the Katombora Rapids, about 50 km upstream from Livingstone, and the rapids just upstream from Katima Mulilo. However, depending on the water level, boats could be paddled through — Lozi paddlers, a dozen or more in a boat, could deal with most of them — or they could be pulled along the shore or carried around the rapids, and teams of oxen pulled barges 5 km over land around the Ngonye Falls.

There are only five major road or rail bridges across the river (ignoring any near its source where it's just a rivulet) and at many locations pontoons ferry people and vehicles across the river. Victoria Falls Bridge was the first to be built, and was completed in April 1905. It was initially intended as a link in Cecil Rhodes' scheme to build a railway from Cape Town to Cairo. The bridge is 250 m (820 ft) across, with a main arch spanning 150 m (490 ft), and the top of the bridge is 125 m (410 ft) above the low-water level of the river.

Later bridges were constructed at Chirundu in Zambia (Otto Beit Bridge, 1939, and the second Chirundu Bridge, 2002), at Tete in Mozambique (1960s) and at Katima Mulilo in Namibia. The bridge of that name, opened in 2004, crosses the river from Sesheke in Zambia so completing the TransCaprivi Highway and connecting Lusaka in Zambia with Walvis Bay on the Namibian coast.

The Chinyingi suspension bridge near the town of Zambezi is a 300 m long footbridge built as a community project.

Ecology

Lake Cahora Bassa in Mozambique, one of the river's major sources of hydroelectric energy

Sewage effluent is a major cause of water pollution around urban areas, as inadequate water treatment facilities in all the major cities of the region force them to release untreated sewage into the river. This has resulted in eutrophication of the river water and has facilitated the spread of diseases of poor hygiene such as cholera, typhus and dysentery.

The construction of two major dams regulating the flow of the river has had a major effect on wildlife and human populations in the lower Zambezi region. When the Cahora Bassa Dam was constructed in 1973, its managers allowed it to fill in a single flood season, going against recommendations to fill over at least two years. The drastic reduction in the flow of the river led to a 40% reduction in the coverage of mangroves, greatly increased erosion of the coastal region and a 60% reduction in the catch of prawns off the mouth due to the reduction in emplacement of silt and associate nutrients. Wetland ecosystems downstream of the dam shrank considerably.

Major towns

Along much of the river's length, the population is sparse, but important towns and cities along its course include the following:

• Katima Mulilo (Namibia)
• Mongu, Lukulu, Livingstone, & Sesheke (Zambia)
• Victoria Falls & Kariba (Zimbabwe)
• Songo & Tete (Mozambique)

References

General references

• Bento C.M., Beilfuss R. (2003), Wattled Cranes, Waterbirds, and Wetland Conservation in the Zambezi Delta, Mozambique, report for the Biodiversity Foundation for Africa for the IUCN - Regional Office for Southern Africa: Zambezi Basin Wetlands Conservation and Resource Utilisation Project.
• Bourgeois S., Kocher T., Schelander P. (2003), Case study: Zambezi river basin, ETH Seminar: Science and Politics of International Freshwater Management 2003/04
• Davies B.R., Beilfuss R., Thoms M.C. (2000), "Cahora Bassa retrospective, 1974–1997: effects of flow regulation on the Lower Zambezi River," Verh. Internat. Verein. Limnologie, 27, 1–9
• Dunham KM (1994), The effect of drought on the large mammal populations of Zambezi riverine woodlands, Journal of Zoology, v. 234, p. 489–526
• Wynn S. (2002), "The Zambezi River - Wilderness and Tourism", International Journal of Wilderness, 8, 34.
• H. C. N. Ridley: “Early History of Road Transport in Northern Rhodesia”, The Northern Rhodesia Journal, Vol 2 No 5 (1954) — Re Zambezi River Transport Service at Katombora.

This article incorporates text from a publication now in the public domain: Chisholm, Hugh, ed. (1911). Encyclopædia Britannica (11th ed.). Cambridge University Press. {{cite encyclopedia}}: Missing or empty |title= (help)

External links

• Information and a map of the Zambezi's watershed
• Map of the Zambezi River basin at Water Resources eAtlas
• Zambezi River Authority
• The Zambezi Society
• Map of Africa's river basins
• Bibliography on Water Resources and International Law See Zambezi River. Peace Palace Library