Water transport and the many navigable inland waterways in Zambia have a long tradition of practical use except in parts of the south. Since draught animals such as oxen were not heavily used, water transport was usually the only alternative to going on foot until the 19th century. The history and current importance of Zambian waterways, as well as the types of indigenous boats used, provide information on this important aspect of Zambian economy.
The techniques of making temporary boats or rafts by weaving together bundles of buoyant reeds were known to African people living near the many rivers, lakes, lagoons and swamps of what is now Zambia. [1] The coming of the Iron Age introduced tools such as the adze which facilitates the construction of dugout canoes, especially from African teak ( Pterocarpus angolensis or 'mulombwa' in Chibemba, 'mulombe' in Chilozi, 'mukwa' in Chishona) which has a long life even when constantly immersed. The dugout then took over as the principal means of fishing and travel by boat, whether paddled in deeper water, or punted in shallow water like makoros in neighbouring Botswana.
When explorer David Livingstone, the first European to see Lake Bangweulu arrived on the western shore of that lake in 1868, he was conveyed across it efficiently in a dugout canoe 45 feet long and 4 feet wide (about 14 m by 1.2 m), paddled by six men. The people of the lake and its wetlands, which cover a completely flat area of more than 10,000 km2 in flood, have the ability to navigate unaided across open water or through mazes of swamp channels despite having no landmarks to guide them most of the time. [2]
There is an account of the Shila people in the Luapula swamps in the 19th century hunting hippos with great skill by throwing harpoons at them from dugout canoes, despite being in great danger from these huge aggressive animals’ ability to overturn a canoe and virtually bite its paddlers in half, and they are responsible for many human deaths in Zambia. [3]
Several dugout canoes may be lashed together and a timber platform built over them to carry heavy loads, and many early pontoon ferries were made in this way, such as the first ferry over the Luangwa River in 1929, which could carry a 1.5 ton truck. Paddled by a dozen men, the crossing used to take four to six hours, not because of the great width of the river but the need to go a long way upstream before the crossing, when the current would sweep the pontoon several kilometres downstream. [4]
There are both permanent and seasonal fishing communities to which the only access is by boat or canoe, such as in Bangweulu and Mweru Wantipa in particular, but also along many rivers and lake shores. To such communities canoes and boats are a way of life. A colonial administrator in the 1920s saw a dugout canoe crossing Lake Tanganyika (35 km wide) which is large enough to have waves of around 1 m. Though such a feat was commonplace, he was astonished to discover that the three paddlers were all blind, and the boat was being steered by a small child to the store at Mpulungu so they could buy supplies. [5]
Before the coming of the Europeans from 1860 onwards, the Lozi people of Barotseland were building Nalikwanda royal barges made from teak planks fixed with iron nails (extensive Rhodesian Teak forests grew in the east of Barotseland). As seen in the Kuomboka ceremony these reached huge sizes, requiring a hundred paddlers or more. Although there has been speculation that the Lozi learnt this method of boat building from Arab or Portuguese traders, the Lozi did not allow such traders to enter their territory, and the traders certainly did not haul boats overland to central Africa with them. There is no evidence to suppose that the Lozi plank boat is anything other than an indigenous technology. [1]
For about three decades after the start of the colonial era as North-Western and North-Eastern Rhodesia, there was no road transport in the territory, except by ox-wagon. Even when the first railway reached the Copperbelt in 1910, there was no mechanised road transport from that single line into the surrounding areas or the rest of the country. Water transport was used by colonial officials, businesses, and the few settlers, and some Africans made their living hiring out their canoes and labour to them. [4]
The main waterways used in this way were: [4]
There is a need to develop inland waterways in Zambia but it is hampered by a lack of management know-how in the sector and a lack of port facilities. [8] Development of the road network has reduced the demand for commercial boat services where road services compete. No major urban centres have developed on any waterways and so boat transport is not used for any urban or inter-urban travel. The only centres which can be considered to have commercial boat services are, in rough order of size:
Boat operators serving the tourist trade are found in: [9]
In addition to these there are a number of tour companies and camps set up for fishing and adventure tours, especially on the upper Zambezi, mostly catering for international tourists at high prices.
Use of dugout canoes has declined somewhat except in more remote locations, due to a relative shortage of good African Teak trees, and competition from timber plank, aluminium and glass-fibre boats. The use of outboard motors remains relatively low due to the high cost of fuel and lack of maintenance services.
This article is about the Transport in Zambia.
The Zambezi is the fourth-longest river in Africa, the longest east-flowing river in Africa and the largest flowing into the Indian Ocean from Africa. Its drainage basin covers 1,390,000 km2 (540,000 sq mi), slightly less than half of the Nile's. The 2,574-kilometre-long (1,599 mi) river rises in Zambia and flows through eastern Angola, along the north-eastern border of Namibia and the northern border of Botswana, then along the border between Zambia and Zimbabwe to Mozambique, where it crosses the country to empty into the Indian Ocean.
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.
This article deals with the disputed area on the borders of the Democratic Republic of the Congo and Zambia, in Luapula Province.
Bangweulu — 'where the water sky meets the sky' — is one of the world's great wetland systems, comprising Lake Bangweulu, the Bangweulu Swamps and the Bangweulu Flats or floodplain. 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.
The Luapula River is a section of Africa's second-longest river, the Congo. It is a transnational river forming for nearly all its length part of the border between Zambia and the DR Congo. It joins Lake Bangweulu to Lake Mweru and gives its name to the Luapula Province of Zambia.
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.
Kazembe is a traditional kingdom in modern-day Zambia, and southeastern Congo. For more than 250 years, Kazembe has been an influential kingdom of the Kiluba-Chibemba, speaking the language of the Eastern Luba-Lunda people of south-central Africa. Its position on trade routes in a well-watered, relatively fertile and well-populated area of forestry, fishery and agricultural resources drew expeditions by traders and explorers who called it variously Kasembe, Cazembe and Casembe.
The Congo Pedicle is the southeast salient of the Haut-Katanga Province of the Democratic Republic of the Congo, which divides neighbouring Zambia into two lobes. In area, the pedicle is similar in size to Wales or New Jersey. 'Pedicle' is used in the sense of 'a little foot'. 'Congo Pedicle' or 'the Pedicle' is also used to refer to the Congo Pedicle road, which crosses it.
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.
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.
The Zambezian flooded grasslands is an ecoregion of southern and eastern Africa that is rich in wildlife.
Chilubi District with headquarters at Chilubi is located in Northern Province, Zambia. It covers the north-east Lake Bangweulu and Bangweulu Wetlands containing several islands including Chilubi Island, and some of the mainland northeast of the lake. As of the 2000 Zambian Census, the district had a population of 66,338 people.
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.
The Barotse Floodplain, also known as the Bulozi Plain, Lyondo or the Zambezi Floodplain, is one of Africa's great wetlands, on the Zambezi River in the Western Province of Zambia. It is a designated Ramsar site, regarded as being of high conservation value.
The following outline is provided as an overview of and topical guide to Zambia:
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.
The geological history of Zambia begins in the Proterozoic eon of the Precambrian. The igneous and metamorphic basement rocks tend to be highly metamorphosed and may have formed earlier in the Archean, but heat and pressure has destroyed evidence of earlier conditions. Major sedimentary and metamorphic groups formed in the mid-Proterozoic, followed by a series of glaciations in the Neoproterozoic and much of the Paleozoic which deposited glacial conglomerate as well as other sediments to form the Katanga Supergroup and rift-related Karoo Supergroup. Basalt eruptions blanketed the Karoo Supergroup in the Mesozoic and Zambia shifted to coal and sandstone formation. Geologically recent windblown sands from the Kalahari Desert and alluvial deposits near rivers play an important role in the modern surficial geology of Zambia. The country has extensive natural resources, particularly copper, but also cobalt, emeralds, other gemstones, uranium and coal.