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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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saddle-billed Stork
The saddle-billed stork or saddlebill (''Ephippiorhynchus senegalensis'') is a large wading bird in the stork family, Ciconiidae. It is a widespread species which is a resident breeder in sub-Saharan Africa from Sudan, Ethiopia and Kenya south to South Africa, and in The Gambia, Senegal, Côte d'Ivoire and Chad in west Africa. It is considered endangered in South Africa. It is a close relative of the widespread Asian and Australian black-necked stork, the only other member of the genus ''Ephippiorhynchus''. Description This is a huge bird that regularly attains a height of , a length of and a wingspan. While heights published have been in the aforementioned narrow range, reportedly adult saddle-billed storks in captivity can attain a height of up to . The male of the species is larger and heavier than the female, with a range of , with a mean mass of . The female is usually between , with a mean mass of . Among the large storks, the saddle-billed broadly overlap in size with ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Miombo
The Miombo woodland is a tropical and subtropical grasslands, savannas, and shrublands biome (in the World Wide Fund for Nature scheme) located primarily in Central Africa. It includes four woodland savanna ecoregions (listed below) characterized by the dominant presence of ''Brachystegia'' and ''Julbernardia'' species 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. The woodland gets its name from ''miombo'' (plural, singular ''muombo''), the Bemba word for ''Brachystegia'' species. Other Bantu languages of the region, such as Swahili and Shona, have related if not identical words, such as Swahili ''miyombo'' (singular ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bangweulu Swamp
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, Zambia, 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 River, Chambeshi, Luapula River, Luapula, Lukulu, and Lulimala rivers. The nonprofit conservation organization African Parks manages a area of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chambeshi River
The Chambeshi (or Chambezi) River of northeastern Zambia is the most remote 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 rainy season in May, the river delivers a flood which recharges the wetlands and 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, 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 bridged by the Kasama–Mpika road and the Tazara Railway, the perman ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lukanga Swamp
Lukanga Swamp is a major wetland in the Central Province of Zambia, about 50 km west of Kabwe.Terracarta/International Travel Maps, Vancouver Canada: "Zambia, 2nd edition", 2000 Its permanently swampy area consists of a roughly circular area with a diameter of 40 to 50 km covering 1850 km2, plus roughly 250 km2 in the mouths of and along rivers discharging into it such as the Lukanga River from the north-east, plus another 500 km2 either side of the Kafue River to the west and north-west, making 2600 km2 in total.Google Earth accessed 2007. It contains many lagoons such as Lake Chiposhye and Lake Suye but few large channels, and its average depth is only 1.5 m. River connections and floodplains The permanent swamp is surrounded by a seasonally-inundated |
Kafue Flats
The Kafue Flats (locally called Butwa) are a vast area of swamp, open lagoon and seasonally inundated flood-plain on the Kafue River in the Southern, Central and Lusaka provinces of Zambia. They are a shallow flood plain 240 km long and about 50 km wide,Google Earth accessed 1 September 2014. flooded to a depth of less than a meter in the rainy season (deeper in some lagoons and permanently swampy areas), and drying out to a clayey black soil in the dry season. Geography The Kafue Flats stretch for approximately 240 km east to west along the from below the Itezhi-Tezhi gap, site of the |
Barotse Floodplain
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 name recognises the floodplain as spawning the culture and way of life of the Lozi people, "Rotse" being a variant of ''Lozi'', and "Ba" meaning "people". They became a powerful kingdom in Central/Southern Africa under their king or litunga Lewanika, whose realm extended up to 300 km from the plain and was called Barotseland. Topography and area The region is a flat plateau at an elevation of about 1000 m tilting very slightly to the south. The Zambezi and its headwaters rise on the higher ground to the north, which enjoys good rainfall (1400 mm annually) in a rainy season from October to May. A flood moves down the river reaching a flat region, formed from Kalahari sands, about five hundred kilometres acro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Chilwa
Lake Chilwa is the second-largest lake in Malawi after Lake Malawi. It is in eastern Zomba District, near the border with Mozambique. Approximately 60 km long and 40 km wide, the lake is surrounded by extensive wetlands. There is an island in the middle of the lake called Chisi Island. The lake has no outlet, and the level of water is greatly affected by seasonal rains and summer evaporation. In 1968, the lake disappeared during exceptionally dry weather. When David Livingstone visited the lake in 1859, he reported that its southern boundary reached as far as the Mulanje Massif, which would have made the lake at least longer than it is today. The Danish International Development Agency, in cooperation with the Government of Malawi has been working to ensure preservation of the lake and its wetlands. The Lake Chilwa Basin Climate Change Adaption Programme (LCBCCAP) has been introduced to conserve the sensitive area, which is not only an important wetland for local fauna, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Kitangiri
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ice ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
