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Southern Highlands, Tanzania
The Southern Highlands is a highland region in southwestern Tanzania, at the northern end of Lake Malawi. The highlands include portions of Mbeya, Njombe, Rukwa, Ruvuma, and Songwe regions, bordering Malawi, Mozambique, and Zambia. Mbeya is the largest city in the highlands. Geography The highlands comprise a group of plateaus and volcanic mountains, including the Mbeya Mountains, Poroto Mountains, Kipengere Range, Mount Rungwe, Kitulo Plateau, Umalila Mountains, and Matengo Highlands. The Ufipa Plateau extends northwest, between Lake Tanganyika and Lake Rukwa. The eastern and western branches of the East African Rift converge in the highlands, and the Western Rift continues south as the valley of Lake Malawi. To the northeast, the Makambako Gap separates the Southern Highlands from the Eastern Arc Mountains. Mt. Rungwe (2,960 metres), and Mtorwe (2961 m) in the Kipengere Range, are the highest peaks in the highlands. Other peaks include Chaluhangi (2933 m) and Ishinga (2688 m) i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Livingstone Forest
Kitulo National Park is a protected area of montane grassland and montane forest on the Kitulo Plateau in the southern highlands of Tanzania. The park is at an elevation of between the peaks of the Kipengere and Poroto mountains and covers an area of , The Ndumbi forest is also home to a 100-meter waterfall. References External links Kitulo National Park, Tanzania National Parks website {{authority control Geography of Njombe Region Geography of Mbeya Region National parks of Tanzania Protected areas established in 2005 Southern Highlands, Tanzania Southern Rift montane forest–grassland mosaic Tourist attractions in the Njombe Region Tourist attractions in the Mbeya Region 2005 establishments in Tanzania ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Umalila Mountains
The Umalila Mountains are a mountain range in southern Tanzania, on the border with Malawi. The Umalila Mountains are part of Tanzania's Southern Highlands. The mountains are named for the Malila people. Geography The Umalila Mountains lie northwest of Lake Malawi, and trend roughly northwest-southeast. They form part of the western edge of the East African Rift. The Kyela Plain lies to the east and northeast of the mountains in the rift valley.Racaud, Sylvain, and Francois Bart (2017). "Rural-Urban Dynamics in the East African Mountains" Mkuki na Nyota Publishers, 2017 The volcanic Poroto Mountains and Mount Rungwe lie to the northeast across the Kiwira River. The town of Mbeya lies to the north, and plateaus to the west. The Songwe River drains the western and southern slopes of the mountains, and separate the Umalila Mountains from the Misuku Hills in neighboring Malawi. The Kiwira River drains the eastern slopes. Both rivers empty into Lake Malawi. Climate The mountains h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ruhuhu River
The Ruhuhu River is a river in Ruvuma Region, Tanzania. Geography The source of the Ruhuhu is on the eastern slope of the Kipengere Range (Livingstone Mountains) in Tanzania, where it first flows southeast and then turns west to Lake Nyasa Lake Malawi, also known as Lake Nyasa in Tanzania and Lago Niassa in Mozambique, is an African Great Lake and the southernmost lake in the East African Rift system, located between Malawi, Mozambique and Tanzania. It is the fifth largest fres ... (Lake Malawi). It is over long, of which the last is a single deep gorge. The river's mouth is just south of Manda. Catchment area At over (between depending on the data source), the Ruhuhu River Basin is the largest of the Malawiese River Basins and the largest in Tanzania. As the longest river flowing into Lake Malawi, by convention it is the headwaters of the Shire, which drains the lake. The Ruhuhu carries water all year round. Hydrometry The discharge of the Ruhuhu was measured in m³ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kiwira River
Kiwira River is a river located in Rungwe District and Kyela District of Mbeya Region, Tanzania. Course It rises in the Poroto Mountains southeast of Mbeya and receives several streams originating on the slopes of Mount Rungwe, including the Marogala, Sinini, Kipoke, Kilasi and Mulagala. Kijungu Falls is on the upper course of the river. It then flows southeast and empties into the northern end of Lake Malawi near the town of Kyela. The lower course flows through the Kyela Plain, which sits northwest of Lake Malawi in the valley of the East African Rift. The Kyela Plain is cultivated intensively with rice and other crops. Daraja la Mungu Daraja la Mungu ( sw, "Bridge of God") is a natural bridge A natural arch, natural bridge, or (less commonly) rock arch is a natural landform where an arch has formed with an opening underneath. Natural arches commonly form where inland cliffs, coastal cliffs, fins or stacks are subject to erosion f ... that spans the Kiwira River at , r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Songwe River
The Songwe River is a river that forms the international boundary between Malawi and Songwe Region, Tanzania. The songwe region in Tanzania is named after the river. The Songwe's headwaters are where the borders of Malawi, Tanzania, and Zambia meet. It flows southeast to empty into Lake Nyasa. The middle course separates Malawi's Misuku Hills from the Umalila Mountains in Songwe Region Tanzania. The lower course flows through the Kyela Plain, a fertile lowland lying northwest of Lake Malawi the valley of the 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 .... The Kyela Plain is cultivated intensively with rice and other crops.Racaud, Sylvain, and Francois Bart (2017). ''Rural-Urban Dynamics in the East African Mountains''. Mkuki na Nyota Publishers, 2017. E ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rufiji River
The Rufiji River lies entirely within Tanzania. It is also the largest and longest river in the country. The river is formed by the confluence of the Kilombero and Luwegu rivers. It is approximately long, with its source in southwestern Tanzania and its mouth on the Indian Ocean opposite Mafia Island across the Mafia Channel, in Pwani Region. Its principal tributary is the Great Ruaha River. It is navigable for approximately . The Rufiji river is approximately south of Dar es Salaam. The river's delta contains the largest mangrove forest in eastern Africa. History A branch of ancient sea routes led down the East African coast called "Azania" by the Greeks and Romans in the 1st century CE as described in the Periplus of the Erythraean Sea (and, very probably, zh, 澤散, Zesan in the 3rd century by the Chinese), at least as far as the port known to the Romans as Rhapta, which was probably located in the delta of the Rufiji River in modern Tanzania. During the First World War ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Ruaha River
The Great Ruaha River is a river in south-central Tanzania that flows through the Usangu wetlands and the Ruaha National Park east into the Rufiji River. It traverses and marks the borders between Iringa Region, Dodoma Region and Morogoro Region. The Great Ruaha river has a basin catchment area of . The population of the basin is mainly sustained by irrigation and water-related livelihoods such as fishing and livestock keeping. Size Great Ruaha is about long, its tributary basin has a catchment area of and the mean annual discharge is per second. The Great Ruaha River supplies 22 percent of the total flow of the Rufiji catchment system. Thirty-eight species of fish have been identified in the Great Ruaha River. The river's headwaters are in the Kipengere Range In west Njombe Region. From there the Great Ruaha River descends to the Usangu plains, an important region for irrigated agriculture and livestock in Tanzania. The river eventually reaches the Mtera Dam and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Ngozi
Lake Ngozi (or Lake Ngosi) is the second largest crater lake in Africa. It can be found near Tukuyu Tukuyu, known as Neu Langenburg during the German colonial rule, is a small hillside town that lies about south of the city of Mbeya, at an elevation of around in the highland Rungwe District of southern Tanzania, East Africa. Tukuyu town ..., a small town in the highland Rungwe District, Mbeya Region, of southern Tanzania in East Africa. It is part of the Poroto Mountains and the northern rim of the caldera is the highest point in the range. The caldera mostly composed from trachytic and phonolitic lavas. Ngozi is a Holocene caldera that generated the Kitulo pumice 12,000 years ago during a Plinian eruption, most likely in the same eruption that generated the caldera. Other eruption deposits are the Ngozi Tuff (less than thousand years ago) and the Ituwa Surge base surge deposits of uncertain age, but intermediary to the Kitulo pumice and Ngozi Tuff. The younges ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Ngozi, Tanzania (2464101174)
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] |
Eastern Arc Mountains
The Eastern Arc Mountains is a chain of mountains found in Kenya and Tanzania. The chain runs from northeast to southwest, with the Taita Hills being in Kenya and the other ranges being in Tanzania. They are delimited on the southwest by the fault complex represented by the Makambako Gap that separates them from the Kipengere Range. To the northeast, they are delimited by more recent volcanism represented by Mount Kilimanjaro. The chain is considered a Tentative World Heritage Site. Mountain ranges The Eastern Arc Mountains forms a roughly crescent-shaped arc and consists of: # Taita Hills # North and South Pare Mountains # East and West Usambara Mountains # Nguru Mountains # Ukaguru Mountains # Uluguru Mountains # Uvidunda Mountains # Rubeho Mountains # Malundwe Mountain # Udzungwa Mountains # Mahenge Mountains Geology These mountain ranges are the oldest in East Africa, and though physically separated from each other, share a similar geomorphology and ecology. They wer ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 kilometer ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Rukwa
Lake Rukwa is an endorheic lake located the Rukwa Valley of Rukwa Region, Songwe Region and Katavi Region in southwestern Tanzania. The lake is the third largest inland body of water in the country. Geography The alkaline Lake Rukwa lies midway between Lake Tanganyika and Lake Malawi at an elevation of about , in a parallel branch of the rift system. Almost half of the lake lies in Uwanda Game Reserve. Hydrology The lake has seen large fluctuations in its size over the years, due to varying inflow of streams. Currently it is about long and averages about wide, making it about in size. In 1929 it was only about long, but in 1939 it was about long and wide. During the early rifting of this part of Africa, the basin of Lake Rukwa may at times have been part of a much larger basin which also included the basins of Lake Tanganyika with Lake Malawi; ancient shorelines suggest a final date of overflow into Lake Tanganyika of 33,000BP. For overflow to occur again, the lake's ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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