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Chambeshi
The Chambeshi (or Chambezi) River of northeastern Zambia is the most remote River source, headstream of the Congo River (in length) and therefore it is considered the source of the Congo River. (However, by volume of water, the Lualaba River provides a greater streamflow to the Congo.) The Chambeshi rises as a stream in the mountains of northeast Zambia near Lake Tanganyika at an elevation of above sea level. It flows for 480 km into the Bangweulu Wetlands, which are part of Lake Bangweulu. By the end of the Wet season, rainy season in May, the river delivers a flood which recharges the wetlands and Zambezian flooded grasslands, inundates the Zambesian grasslands to the southeast. The water then flows out of the wetlands as the Luapula River. For more than 100 km of its length as it flows to the east of Kasama, Zambia, Kasama, the river consists of a maze of channels in wetlands about 2 km wide, in a floodplain up to 25 km wide. Further downstream, where it is ...
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Lake Bangweulu
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.Camerapix: ''Spectrum Guide to Zambia.'' Camerapix International Publishing, Nairobi, 1996. 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.Halls, A.J. (ed.), 1997. "Wetlands, Biodiversity and the Ramsar Convention: The Role of the Convention on Wetlands in the Conservation and Wise Use of Biodiversity". Ramsar Convention Bureau, Gland, Switzerland With a long axis of 75 km and a width of up to 40 km, Lake Bangweulu's permanent open ...
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Congo River
The Congo River ( kg, Nzâdi Kôngo, french: Fleuve Congo, pt, Rio Congo), formerly also known as the Zaire River, is the second longest river in Africa, shorter only than the Nile, as well as the second largest river in the world by discharge volume, following only the Amazon. It is also the world's deepest recorded river, with measured depths around . The Congo- Lualaba- Chambeshi River system has an overall length of , which makes it the world's ninth- longest river. The Chambeshi is a tributary of the Lualaba River, and ''Lualaba'' is the name of the Congo River upstream of Boyoma Falls, extending for . Measured along with the Lualaba, the main tributary, the Congo River has a total length of . It is the only major river to cross the Equator twice. The Congo Basin has a total area of about , or 13% of the entire African landmass. Name The name ''Congo/Kongo'' originates from the Kingdom of Kongo once located on the southern bank of the river. The kingdom in turn was name ...
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Luapula River
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 (wholly in Zambia) to Lake Mweru (shared between the two countries) and gives its name to the Luapula Province of Zambia.Terracarta/International Travel Maps, Vancouver Canada: "Zambia, 2nd edition", 2000 Source and upper Luapula The Luapula drains Lake Bangweulu and its swamps into which flows the Chambeshi River, the source of the Congo. There is no single clear channel connecting the two rivers and the lake, but a mass of shifting channels, lagoons and swamps, as the explorer David Livingstone found to his cost. (He died exploring the area, and one of his last acts was to question Chief Chitambo about the course of the Luapula.)Blaikie, William Garden (1880): ''The Personal Life Of David Livingstone''Project Gutenberg Ebook #13262 release date: August 23, 2004.D ...
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Kasama, Zambia
Kasama is a city in the Northern Province of Zambia. It serves as the provincial capital and the headquarters of Kasama District. Location It is situated on the central-southern African plateau, approximately , by road, north-east of Lusaka, the capital and largest city in Zambia. Kasama is located on the M1 road (old Great North Road) from Mpika in the south to Mbala and Mpulungu, at the tip of Lake Tanganyika, in the north. Population The city population grew considerably in the 1970s and 1980s after construction of the TAZARA Railway through the city, and the tarring of the Great North Road, Zambia. Its population, according to Encyclopedia Britannica, was 74,243 in 2000 and had increased to 113,779 in 2010. History In 1898/1899, a crisis over the succession of the Chitimukulu led to Bishop Joseph 'Moto Moto' Dupont gaining the agreement of Bemba chiefs to the British colonial Administrator of North-Eastern Rhodesia, Robert Codrington taking control of the are ...
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Bangweulu Wetlands
The Bangweulu Wetlands is a wetland ecosystem adjacent to Lake Bangweulu in north-eastern Zambia. The area has been designated as one of the world's most important wetlands by the Ramsar Convention and an "Important Bird Area" by BirdLife International. African Parks began managing Bangweulu in partnership with Zambia's Department of National Parks and Wildlife with the establishment of the Bangweulu Wetland Management Board in 2008. Overview The Bangweulu Wetlands ecosystem was first described in the 1940s. Bangweulu, which means "where the water sky meets the sky", is located mostly within Zambia's Northern Province and recognized by the Ramsar Convention as one of the world's most important wetlands. The region has floodplains, seasonally flooded grasslands, woodlands, and permanent swamps fed by the Chambeshi, Luapula, Lukulu, and Lulimala rivers. The nonprofit conservation organization African Parks manages a area of the greater Bangweulu ecosystem. Flora and fauna The ec ...
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TAZARA Railway
The Tazara Railway, also called the Uhuru Railway or the Tanzam Railway, is a railway in East Africa linking the port of Dar es Salaam in east Tanzania with the town of Kapiri Mposhi in Zambia's Central Province. The single-track railway is long and is operated by the Tanzania-Zambia Railway Authority (TAZARA). The governments of Tanzania, Zambia, and the People's Republic of China built the railway to eliminate landlocked Zambia's economic dependence on Rhodesia and South Africa, both of which were ruled by white-minority governments.Thomas W. Robinson and David L. Shambaugh. ''Chinese Foreign Policy: theory and practice'', 1994. Page 287. The railway provided the only route for bulk trade from Zambia's Copperbelt to reach the sea without having to transit white-ruled territories. The spirit of Pan-African socialism among the leaders of Tanzania and Zambia and the symbolism of China's support for newly independent African countries gave rise to Tazara's designation as the ...
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Zambia
Zambia (), officially the Republic of Zambia, is a landlocked country at the crossroads of Central Africa, Central, Southern Africa, Southern and East Africa, although it is typically referred to as being in Southern Africa at its most central point. Its neighbours are the Democratic Republic of the Congo to the north, Tanzania to the northeast, Malawi to the east, Mozambique to the southeast, Zimbabwe and Botswana to the south, Namibia to the southwest, and Angola to the west. The capital city of Zambia is Lusaka, located in the south-central part of Zambia. The nation's population of around 19.5 million is concentrated mainly around Lusaka in the south and the Copperbelt Province to the north, the core economic hubs of the country. Originally inhabited by Khoisan peoples, the region was affected by the Bantu expansion of the thirteenth century. Following the arrival of European exploration of Africa, European explorers in the eighteenth century, the British colonised the r ...
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Congo Basin
The Congo Basin (french: Bassin du Congo) is the sedimentary basin of the Congo River. The Congo Basin is located in Central Africa, in a region known as west equatorial Africa. The Congo Basin region is sometimes known simply as the Congo. It contains some of the largest tropical rainforests in the world and is an important source of water used in agriculture and energy generation. The rainforest in the Congo Basin is the largest rainforest in Africa and second only to the Amazon rainforest in size, with 300 million hectares compared to the 800 million hectares in the Amazon. Because of its size and diversity, many experts have characterized the basin's forest as important for mitigating climate change because of its role as a carbon sink. However, deforestation and degradation of the ecology by the impacts of climate change may increase stress on the forest ecosystem, in turn making the hydrology of the basin more variable. A 2012 study found that the variability in precipita ...
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Lualaba River
The Lualaba River flows entirely within the eastern Democratic Republic of the Congo. It provides the greatest streamflow to the Congo River, while the source of the Congo is recognized as the Chambeshi. The Lualaba is long. Its headwaters are in the country's far southeastern corner near Musofi and Lubumbashi in Katanga Province, next to the Zambian Copperbelt. Course The source of the Lualaba River is on the Katanga plateau, at an elevation of above sea level. The river flows northward to end near Kisangani, where the name Congo River officially begins. From the Katanga plateau it drops, with waterfalls and rapids marking the descent, to the Manika plateau. As it descends through the upper Upemba Depression (Kamalondo Trough), in . Near Nzilo Falls it is dammed for hydroelectric power at the Nzilo Dam. At Bukama in Haut-Lomami District the river becomes navigable for about through a series of marshy lakes in the lower Upemba Depression, including Lake Upemba and Lake Kisale ...
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Zambezian Flooded Grasslands
The Zambezian flooded grasslands is an ecoregion of southern and eastern Africa that is rich in wildlife. Setting The Zambezian flooded grasslands can be found on seasonally- or permanently-flooded lowlands in the basin of the Zambezi and neighboring river basins. These enclaves lie in the Zambezian region, a broad belt of seasonally-dry miombo and mopane savannas and woodlands that extend east and west across Africa, from northern Botswana, Namibia, and Angola in the west to Tanzania and Mozambique in the east. Large enclaves of flooded grassland include: * Kilombero Valley and Mkata Plain in southern Tanzania * Malagarasi-Muyovozi floodplain and Ugalla River floodplain in western Tanzania * Wembere River- Lake Kitangiri floodplain in Tanzania * The Okavango Delta in Botswana * around Lake Chilwa in Malawi * The Barotse Floodplain, Kafue Flats, Busanga Swamp, and Lukanga Swamp in the Zambezi basin of Zambia. * The upper Chambeshi River, Bangweulu Swamp, the Luapula River de ...
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Lake Tanganyika
Lake Tanganyika () is an African Great Lake. It is the second-oldest freshwater lake in the world, the second-largest by volume, and the second-deepest, in all cases after Lake Baikal in Siberia. It is the world's longest freshwater lake. The lake is shared among four countries—Tanzania, the Democratic Republic of the Congo (DRC), Burundi, and Zambia, with Tanzania (46%) and DRC (40%) possessing the majority of the lake. It drains into the Congo River system and ultimately into the Atlantic Ocean. Etymology "Tanganika" was the name of the lake that Henry Morton Stanley encountered when he was at Ujiji in 1876. The name first originated from the Bembe language when they arrived in South Kivu around the 7th century, they discovered the lake and started calling it “êtanga ‘ya’ni’â” which means “a big river” in their Bantu language. Stanley found also other names for the lake among different ethnic groups, like the Kimana, the Yemba and the Msaga. An alt ...
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Mountain
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ...
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