Matandwe Forest Reserve
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Matandwe Forest Reserve
The Matundwe Range is a range of mountains in southernmost Malawi and adjacent Tete Province of Mozambique. The range is located between the Zambezi and Shire rivers just north of their confluence, and the Malawi-Mozambique border runs along the divide between the two rivers' watersheds. The Shire River Valley is a southern extension of the East African Rift. The southern end of the Matundwe Range rises as a steep escarpment along the west side of the Shire Valley lowlands, and descends more gently westwards towards the Zambezi. At the northern end of the range, the western face of the range has a steep escarpment. Malawi's Matandwe Forest Reserve covers part of northern range. The reserve was established in 1931, and covers and area of 31,053 ha. The main plant community in the reserve is open-canopy miombo woodland dominated by '' Brachystegia'' species, particularly '' B. boehmii'', along with ''Uapaca kirkiana''.Mwafongo E (2019). ABC Matandwe Forest Reserve Vegetation ...
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Malawi
Malawi (; or aláwi Tumbuka: ''Malaŵi''), officially the Republic of Malawi, is a landlocked country in Southeastern Africa that was formerly known as Nyasaland. It is bordered by Zambia to the west, Tanzania to the north and northeast, and Mozambique to the east, south and southwest. Malawi spans over and has an estimated population of 19,431,566 (as of January 2021). Malawi's capital (and largest city) is Lilongwe. Its second-largest is Blantyre, its third-largest is Mzuzu and its fourth-largest is its former capital, Zomba. The name ''Malawi'' comes from the Maravi, an old name for the Chewa people who inhabit the area. The country is nicknamed "The Warm Heart of Africa" because of the friendliness of its people. The part of Africa now known as Malawi was settled around the 10th century by migrating Bantu groups . Centuries later, in 1891, the area was colonised by the British and became a protectorate of the United Kingdom known as Nyasaland. In 1953, it became ...
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Tete Province
Tete is a Provinces of Mozambique, province of Mozambique. It has an area of 98,417 km² and a population of 2,648,941 (2017 census). Tete is the capital of the province. The Cahora Bassa Dam is situated in this province. Districts On March 21, 2013, Mozambique's Assembly of the Republic authorized the creation of 13 new districts throughout the nation. Two were added to Tete. Tete Province's districts include: *Angónia District *Cahora-Bassa District *Changara District *Chifunde District *Chiuta, Mozambique, Chiuta District *Tete, the capital city of the province *Doa District *Macanga District *Magoé District *Marávia District *Marara District *Moatize District *Mutarara District *Tsangano District *Zumbo District Demographics Tete Fossil Forest A fossil site of global significance covers almost 1500 square km of the region. Well-preserved fossil wood from the Late Permian provides an insight into the flora of the area just prior to the Permian–Triassic ext ...
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Mozambique
Mozambique (), officially the Republic of Mozambique ( pt, Moçambique or , ; ny, Mozambiki; sw, Msumbiji; ts, Muzambhiki), is a country located in southeastern Africa bordered by the Indian Ocean to the east, Tanzania to the north, Malawi and Zambia to the northwest, Zimbabwe to the west, and Eswatini and South Africa to the southwest. The sovereign state is separated from the Comoros, Mayotte and Madagascar by the Mozambique Channel to the east. The capital and largest city is Maputo. Notably Northern Mozambique lies within the monsoon trade winds of the Indian Ocean and is frequentely affected by disruptive weather. Between the 7th and 11th centuries, a series of Swahili port towns developed on that area, which contributed to the development of a distinct Swahili culture and language. In the late medieval period, these towns were frequented by traders from Somalia, Ethiopia, Egypt, Arabia, Persia, and India. The voyage of Vasco da Gama in 1498 marked the arrival of t ...
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Zambezi
The Zambezi River (also spelled Zambeze and Zambesi) 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 , slightly less than half of the Nile's. The 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. The Zambezi's most noted feature is Victoria Falls. Its other falls include the Chavuma Falls at the border between Zambia and Angola, and Ngonye Falls near Sioma in western Zambia. The two main sources of hydroelectric power on the river are the Kariba Dam, which provides power to Zambia and Zimbabwe, and the Cahora Bassa Dam in Mozambique, which provides power to Mozambique and South Africa. Additionally, two smaller power stations are along the Zambezi Riv ...
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Shire River
The Shire is the largest river in Malawi. It is the only outlet of Lake Malawi and flows into the Zambezi River in Mozambique. Its length is . The upper Shire River issues from Lake Malawi and runs approximately before it enters shallow Lake Malombe. It then drains Lake Malombe and flows south through Liwonde National Park where large concentrations of hippopotamus are common along its shores. Between the towns of Matope and Chikwawa, the middle river drops approximately through a series of falls and gorges, including Kapachira Falls. Two hydroelectric dams have been built along the Shire northwest of Blantyre. Beyond Chikwawa, the lower river turns southeast and enters the low-lying Mozambique plain. Its largest and one of its few perennial tributaries, the Ruo River, joins the Shire near the Malawian town of Chiromo. The muddy waters pass through a large stagnant area known as the Elephant Marsh before reaching the confluence with the Zambezi River south of the town of Sen ...
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East African Rift
The East African Rift (EAR) or East African Rift System (EARS) is an active continental rift zone in East Africa. The EAR began developing around the onset of the Miocene, 22–25 million years ago. In the past it was considered to be part of a larger Great Rift Valley that extended north to Asia Minor. A narrow zone, the rift is a developing divergent tectonic plate boundary where the African Plate is in the process of splitting into two tectonic plates, called the Somali Plate and the Nubian Plate, at a rate of 6-7 mm per year. The rift system consists of three microplates, the Victoria Microplate to the north, and the Rovuma and Lwandle microplates to the south. The Victoria Microplate is rotating anti-clockwise with respect to the African plate. Its rotation is caused by the configuration of mechanically weaker and stronger lithospheric regions in the EARS. Extent A series of distinct rift basins, the East African Rift System extends over thousands of kilometers. The ...
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Escarpment
An escarpment is a steep slope or long cliff that forms as a result of faulting or erosion and separates two relatively level areas having different elevations. The terms ''scarp'' and ''scarp face'' are often used interchangeably with ''escarpment''. Some sources differentiate the two terms, with ''escarpment'' referring to the margin between two landforms, and ''scarp'' referring to a cliff or a steep slope. In this usage an escarpment is a ridge which has a gentle slope on one side and a steep scarp on the other side. More loosely, the term ''scarp'' also describes a zone between a coastal lowland and a continental plateau which shows a marked, abrupt change in elevation caused by coastal erosion at the base of the plateau. Formation and description Scarps are generally formed by one of two processes: either by differential erosion of sedimentary rocks, or by movement of the Earth's crust at a geologic fault. The first process is the more common type: the escarpment is a t ...
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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 ...
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Brachystegia
''Brachystegia'' is a genus of tree of the subfamily Detarioideae that is native to tropical Africa. Trees of the genus are commonly known as miombo, and are dominant in the miombo woodlands of central and southern tropical Africa. The Zambezian region is the centre of diversity for the genus.Emmanuel N. Chidumayo and Davison J. Gumbo, eds. (2010). ''The dry forests and woodlands of Africa: managing for products and services''. Earthscan, 2010. Description Hybridisation between the species occurs and taxa show considerable variation in leaflet size, shape and number, making identification difficult. New leaves show a great range of red colours when immature, later turning to various shades of green. Species * '' Brachystegia allenii'' * '' Brachystegia angustistipulata'' * '' Brachystegia bakeriana'' * '' Brachystegia bequaertii'' * ''Brachystegia boehmii'' * '' Brachystegia bussei'' * '' Brachystegia cynometroides'' * ''Brachystegia eurycoma'' * '' Brachystegia floribunda'' * ...
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Brachystegia Boehmii
''Brachystegia boehmii'', named after the 19th-century German naturalist and collector Richard Böhm, is a flat-topped tree with spreading crown, native to eastern and southern Africa. It forms an important component of miombo woodland, and occurs in Angola, Botswana, Democratic Republic of the Congo, Malawi, Mozambique, Zimbabwe, and Zambia. Common names are machabel (Mashonaland Mashonaland is a region in northern Zimbabwe. Currently, Mashonaland is divided into four provinces, * Mashonaland West * Mashonaland Central * Mashonaland East * Harare The Zimbabwean capital of Harare, a province unto itself, lies entirely ...), mufuti ( Zimbabwe) and Prince of Wales feathers. Occurring in the altitude range 900 – 1600 m, and growing to 15 m tall, it has glabrous or pubescent young branchlets. Its long, pendulous, tufted leaves are some 35 cm long, with 15−30 pairs of leaflets, the middle pair measuring 30−65 x 7−18 mm. Upper and lower surfaces are m ...
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Uapaca Kirkiana
''Uapaca kirkiana'', the sugar plum or mahobohobo, is a species of dioecious plant in the family Phyllanthaceae. It is native to the southern Afrotropics, where it occurs in well-watered miombo woodlands. Within range it is one of the most popular wild fruits. It is rarely cultivated but trees are left when land is being cleared. Still a traditional food plant in Africa, this little-known fruit has the potential to improve nutrition, boost food security, foster rural development and support sustainable land care. In Shona, the fruit are referred to as ''mazhanje'', and in Chichewa ''masuku''. Range It occurs in the miombo woodlands of Angola, the DRCongo, Zambia, southern Burundi, Tanzania, Malawi, central and northern Mozambique, and Zimbabwe Zimbabwe (), officially the Republic of Zimbabwe, is a landlocked country located in Southeast Africa, between the Zambezi and Limpopo Rivers, bordered by South Africa to the south, Botswana to the south-west, Zambia to th ...
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