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Kafue River
The long Kafue River is the longest river lying wholly within Zambia. Its water is used for irrigation and for generating Hydroelectricity, hydroelectric power. It is the largest tributary of the Zambezi, and of Zambia's principal rivers, it is the most central and the most Urban area, urban. More than 50% of Demographics of Zambia, Zambia's population live in the Kafue River Basin and of these around 65% are urban. It has a mean flow rate of through its lower half, with high seasonal variations. The river discharges per year into the Zambezi River. Course Sources The Kafue River rises at an elevation of on the relatively flat plateau just south the border between Zambia and the Democratic Republic of the Congo north-west of Chingola in the Copperbelt Province. The source of the Kafue River is in the North-Western Province, Zambia, North-western Province of Zambia. The area is Miombo woodland on the Congo-Zambezi watershed, with many branching dambos lying lower th ...
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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. It is typically referred to being in South-Central Africa or Southern Africa. It is bordered to the north by the Democratic Republic of the Congo, Tanzania to the north-east, 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 population 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 European colonization of Africa, European colonisers in the 18th century, the British colonised the region into the British protectorates of Barotziland–North-Western Rho ...
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Plateau
In geology and physical geography, a plateau (; ; : plateaus or plateaux), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wider ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, plate tectonics movements, and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. They may be formed by upwelling of volcanic magma or extrusion of lava. The underlining mechanism in forming p ...
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Irrigation
Irrigation (also referred to as watering of plants) is the practice of applying controlled amounts of water to land to help grow crops, landscape plants, and lawns. Irrigation has been a key aspect of agriculture for over 5,000 years and has been developed by many cultures around the world. Irrigation helps to grow crops, maintain landscapes, and revegetation, revegetate disturbed soils in dry areas and during times of below-average rainfall. In addition to these uses, irrigation is also employed to protect crops from frost, suppress weed growth in grain fields, and prevent soil consolidation. It is also used to cool livestock, reduce dust, dispose of sewage, and support mining operations. Drainage, which involves the removal of surface and sub-surface water from a given location, is often studied in conjunction with irrigation. There are several methods of irrigation that differ in how water is supplied to plants. Surface irrigation, also known as gravity irrigation, is the olde ...
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National Monuments Of Zambia
This article gives lists of the National Monuments and other historic sites of Zambia, with a one- or two-line description providing links to details given on other pages. National Heritage Conservation Commission The Institution mandated by Cap 173 of the Laws of Zambia to manage and Conserve Zambia's outstanding Cultural and Natural Heritage resources is the National Heritage Conservation Commission (NHCC) which has its headquarters in Lusaka. According to ICOMOS (see references), the NHCC's profile report, it lists over 4000 heritage sites in Zambia, including: * historic/architectural/buildings (over 384 sites) * historic sites (over 180 sites) * anthropological sites (over 189 sites) * engineering industrial structures (over 62 sites) * archaeological sites (over 2000 sites) * geomorphological sites, geophysical sites, palaeontological, ecology and other sites. However, only about 35% of the country's land area has been adequately surveyed for cultural heritage and, due to a ...
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Mufulira
Mufulira is a town in the Copperbelt Province of Zambia. Mufulira means "Place of Abundance and Peace". The town developed around the Mufulira Copper Mine in the 1930s. The town also serves as the administrative capital of Mufulira District. Geography Location Mufulira is located approximately southwest of the town of Mokambo, at the international border with the Democratic Republic of the Congo. A tarmac highway to the south-west (the M4 Road (Zambia), M4 road) connects Mufulira to Kitwe, away. The city of Ndola, the commercial and transport hub of the Copperbelt, lies approximately , by road, southeast of Mufulira. A shorter, less well-maintained road (the M4 Road (Zambia), M4 road) exists and measures . Mufulira is connected to the Mokambo Border and eventually the Luapula Province of Zambia by the Congo Pedicle road. The section from Mufulira to Mokambo is designated as the M5 Road (Copperbelt), M5 road while the route through the Congo Pedicle to the Chembe Border is na ...
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Chililabombwe
Chililabombwe (formerly named Bancroft) is a small town in Copperbelt Province, Zambia. It is located near the Democratic Republic of the Congo border. The name Chililabombwe means 'place of the croaking frog' in the local language of Lamba. The town has a population of 87 000 based on census data from 2010, making it one of the largest towns in the Copperbelt. The town is on the T3 road, 26 km north of the neighbouring town of Chingola, and approximately 10 km south of the large border market of Kasumbalesa. It has also produced national heroes like the late soccer star Eston Mulenga and many others. The town's main economic activity is copper mining. Chililabombwe town also has small communities like Konkola. Konkola town is the home of Konkola Copper Mine. Politics The current mayor is Lucky Sichone supported by the deputy mayor, Getrude Witola. The town is represented in the National Assembly by the Chililabombwe constituency and the current Member of Par ...
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Copperbelt
The Copperbelt () is a natural region in Central Africa which sits on the border region between northern Zambia and the south eastern Democratic Republic of Congo. It is known for copper mining and is the second largest global reserve of copper, about the size of the Copper mining in Chile#Geology, Chilean reserve. Traditionally, the term ''Copperbelt'' includes the mining regions of Zambia's Copperbelt Province (notably the towns of Ndola, Kitwe, Chingola, Luanshya, and Mufulira in particular) and the Congo's Haut-Katanga Province, Haut-Katanga and Lualaba Province, Lualaba provinces (notably Lubumbashi, Kolwezi, and Likasi). It arises because of the Katanga Supergroup, a Neoproterozoic sequence of geological formations. In some contexts the term ''Copperbelt'' may exclude the Congo entirely. Zambia's Copperbelt became a province soon after independence in 1964, when it was named "Western province". President Kenneth Kaunda changed the name to its present-day "Copperbelt provin ...
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Floodplain
A floodplain or flood plain or bottomlands is an area of land adjacent to a river. Floodplains stretch from the banks of a river channel to the base of the enclosing valley, and experience flooding during periods of high Discharge (hydrology), discharge.Goudie, A. S., 2004, ''Encyclopedia of Geomorphology'', vol. 1. Routledge, New York. The soils usually consist of clays, silts, sands, and gravels deposited during floods. Because of regular flooding, floodplains frequently have high soil fertility since nutrients are deposited with the flood waters. This can encourage farming; some important agricultural regions, such as the Nile and Mississippi Basin, Mississippi Drainage basin, river basins, heavily exploit floodplains. Agricultural and urban regions have developed near or on floodplains to take advantage of the rich soil and freshwater. However, the Flood risk, risk of inundation has led to increasing efforts to Flood control, control flooding. Formation Most floodplai ...
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Topography
Topography is the study of the forms and features of land surfaces. The topography of an area may refer to the landforms and features themselves, or a description or depiction in maps. Topography is a field of geoscience and planetary science and is concerned with local detail in general, including not only relief, but also natural, artificial, and cultural features such as roads, land boundaries, and buildings. In the United States, topography often means specifically relief, even though the USGS topographic maps record not just elevation contours, but also roads, populated places, structures, land boundaries, and so on. Topography in a narrow sense involves the recording of relief or terrain, the three-dimensional quality of the surface, and the identification of specific landforms; this is also known as geomorphometry. In modern usage, this involves generation of elevation data in digital form ( DEM). It is often considered to include the graphic representation of t ...
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Dambos
A dambo is a class of complex shallow wetlands in central, southern and eastern Africa, particularly in Zambia, Malawi and Zimbabwe. They are generally found in higher rainfall flat plateau areas and have river-like branching forms which in themselves are not very large but combined add up to a large area. Dambos have been estimated to comprise 12.5% of the area of Zambia. Similar African words include ''mbuga'' (commonly used in East Africa), ''matoro'' (Mashonaland), ''vlei'' (South Africa), ''fadama'' (Nigeria), and ''bolis'' (Sierra Leone); the French ''bas-fond'' and German ''SpĂĽltal'' have also been suggested as referring to similar grassy wetlands.Andrew S. Goudie, "The Geomorphology of the Seasonal Tropics" in William M. Adams, ''et al.'' (editors), ''The Physical geography of Africa'' (Oxford: University Press, 1996), p. 152 Characteristics Dambos are characterised by grasses, rushes and sedges, contrasting with surrounding woodland such as miombo woodland. They may be sub ...
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Woodland
A woodland () is, in the broad sense, land covered with woody plants (trees and shrubs), or in a narrow sense, synonymous with wood (or in the U.S., the '' plurale tantum'' woods), a low-density forest forming open habitats with plenty of sunlight and limited shade (see differences between British, American and Australian English explained below). Some savannas may also be woodlands, such as ''savanna woodland'', where trees and shrubs form a light canopy. Woodlands may support an understory of shrubs and herbaceous plants including grasses. Woodland may form a transition to shrubland under drier conditions or during early stages of primary or secondary succession. Higher-density areas of trees with a largely closed canopy that provides extensive and nearly continuous shade are often referred to as forests. Extensive efforts by conservationist groups have been made to preserve woodlands from urbanization and agriculture. For example, the woodlands of Northwest Indiana ha ...
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Miombo
Miombo woodland is a tropical and subtropical grasslands, savannas, and shrublands biome (in the World Wide Fund for Nature scheme) located in central and southern tropical Africa. It includes three woodland savanna ecoregions (listed below) characterized by the dominant presence of '' Brachystegia'' and '' Julbernardia'' genera of trees, and has a range of climates ranging from humid to semi-arid, and tropical to subtropical or even temperate. The trees characteristically shed their leaves for a short period in the dry season to reduce water loss and produce a flush of new leaves just before the onset of the wet season with rich gold and red colours masking the underlying chlorophyll, reminiscent of autumn colours in the temperate zone. Miombo woodlands extend across south-central Africa, running from Angola in the west to Tanzania in the east, including parts of Democratic Republic of the Congo, Malawi, Mozambique, Zambia, and Zimbabwe. They are bounded on the north by the humid ...
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