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Kipengere Range
The Kipengere Range, also known as the Livingstone Mountains, lies entirely in Njombe Region in southwest Tanzania at the northern end of Lake Nyasa. Near Lake Nyasa they are known as the Kinga Mountains. It is a plateau-like ridge of mountains running southeastwards from the basin of the Great Ruaha River in the north to that of the Ruhuhu River in the south, and forms part of the eastern escarpment of the East African Rift. The range is mostly clad in montane grasslands, renowned for their botanical diversity and displays of flowers, with montane evergreen forests mostly in stream valleys. Some sources use the names Kipengere Range or Livingstone Mountains to describe the entire range, while others distinguish the Livingstone Mountains as the southwest-facing escarpment which runs along the shore of Lake Malawi, and the Kipengere Range as the high ridge that defines the northeastern edge of the Kitulo Plateau. Geography From the town of Mbeya the range runs south-east and for ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Njombe Region
Njombe Region (''Mkoa wa Njombe'' in Swahili) is one of Tanzania's 31 administrative regions. The region covers a land area of . The region is comparable in size to the combined land area of the nation state of El Salvador. Njombe Region is bordered to the north by the Iringa Region and Mbeya Region, to the east by Morogoro Region, to the south by the Ruvuma Region and to the west by Lake Nyasa. The regional capital is the municipality of Njombe. According to the 2012 national census, the region had a population of 702,097. Etymology The name Njombe originated from a name of a tree species called ‘''Mdzombe''’ for singular and ''Mazdombe'' for plural which then dominant in one of its localities known as Mdandu. And it was in Mdandu where the Germans chose to build an administrative and defence block; the Boma. Geography The Njombe Region is situated in Tanzania's Southern Highlands Zone. It shares borders with the regions of Iringa to the north, Morogoro to the east, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Manda People
The Manda are an ethnic and linguistic group based in Ludewa District in the Iringa Region of southern Tanzania, along the eastern shore of Lake Malawi 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 fr .... In 2002 the Manda population was estimated to number 22,000. Some of these lived in Gua land and Mkwajuni, Chunya district in Mbeya region. They also found in areas where fishing activities take place like Mtera Reservoir, nyumba ya mungu, mlimba etc. Manda people originated from Ngoni References Ethnic groups in Tanzania Indigenous peoples of East Africa {{Tanzania-ethno-group-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yushania Alpina
''Oldeania alpina'', the African alpine bamboo, is a perennial bamboo of the family Poaceae and the genus '' Yushania''. It can be found growing in dense but not large stands on the mountains and volcanoes surrounding the East African Rift between the altitudes of 2,500 meters (8,200 feet) and 3,300 meters (11,000 feet). Description ;Stems and leaves: 200 – 1,950 centimeters (6 – 64 feet) tall and 5 – 12.5 centimeters (2 – 5 inches) in diameter; these grass stems get used as fencing, plumbing and other building materials. Culm sheaths (tubular coverings) are hairless or with red bristles. :Leaf sheath is covered with bristles. Leaf blades are "deciduous at the ligule"; blades 5 – 20 centimeters (2 – 8 inches) long. ;Flowers: Branched cluster of flowers in solitary spikes, which can be dense or loose and are 5–15 centimeters (2–6 inches) long. ;Roots: Short rhizomes described as pachymorph (a term which is recommended for describing rhizomes wh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Juniperus Procera
''Juniperus procera'' (known by the common English names African juniper, African pencil-cedar, East African juniper, East African-cedar, and Kenya-cedar) is a coniferous tree native to mountainous areas in Africa and the Arabian Peninsula. It is a characteristic tree of the Afromontane flora. Description ''Juniperus procera'' is a medium-sized tree reaching (rarely ) tall, with a trunk up to diameter and a broadly conical to rounded or irregular crown. The leaves are of two forms, juvenile needle-like leaves long on seedlings, and adult scale-leaves 0.5–3 mm long on older plants, arranged in decussate pairs or whorls of three. It is largely dioecious with separate male and female plants, but some individual plants produce both sexes. The cones are berry-like, 4–8 mm in diameter, blue-black with a whitish waxy bloom, and contain 2–5 seeds; they mature in 12–18 months. The male cones are 3–5 mm long, and shed their pollen in early spring.(Page archived ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geophyte
A storage organ is a part of a plant specifically modified for storage of energy (generally in the form of carbohydrates) or water. Storage organs often grow underground, where they are better protected from attack by herbivores. Plants that have an underground storage organ are called geophytes in the Raunkiær plant life-form classification system.; reprinted (1977) in ''History of ecology'' series, New York: Arno Press, Storage organs often, but not always, act as perennating organs which enable plants to survive adverse conditions (such as cold, excessive heat, lack of light or drought). Relationship to perennating organ Storage organs may act as perennating organs ('perennating' as in perennial, meaning "through the year", used in the sense of continuing beyond the year and in due course lasting for multiple years). These are used by plants to survive adverse periods in the plant's life-cycle (e.g. caused by cold, excessive heat, lack of light or drought). During these pe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rungwe Volcanic Province
Mount Rungwe is a volcanic mountain in Mbeya Region, in Tanzania's Southern Highlands. At an altitude of , it is southern Tanzania's second-highest peak. Rungwe's volcano is currently inactive. Geography Rungwe stands at the junction of the eastern and western arms of the East African Rift. It dominates the mountainous country at the north-west end of the trough that contains Lake Malawi. The Kipengere Range lies to the east, and the Poroto Mountains lie to the north. Kyejo volcano (or Kiejo) (2176 m) lies to the southeast.Global Volcanism Program, 2013. Kyejo (222170) in Volcanoes of the World, v. 4.8.2. Venzke, E (ed.). Smithsonian Institution. Downloaded 06 Sep 2019 (https://volcano.si.edu/volcano.cfm?vn=222170). https://doi.org/10.5479/si.GVP.VOTW4-2013 The Kyela Plain, which occupies the valley of the East African Rift, lies to the south, extending to Lake Malawi. The western slopes of the mountain are drained by the Kiwira River, which empties into Lake Malawi. Geology ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually relate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quartz
Quartz is a hard, crystalline mineral composed of silica ( silicon dioxide). The atoms are linked in a continuous framework of SiO4 silicon-oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall chemical formula of SiO2. Quartz is the second most abundant mineral in Earth's continental crust, behind feldspar. Quartz exists in two forms, the normal α-quartz and the high-temperature β-quartz, both of which are chiral. The transformation from α-quartz to β-quartz takes place abruptly at . Since the transformation is accompanied by a significant change in volume, it can easily induce microfracturing of ceramics or rocks passing through this temperature threshold. There are many different varieties of quartz, several of which are classified as gemstones. Since antiquity, varieties of quartz have been the most commonly used minerals in the making of jewelry and hardstone carvings, especially in Eurasia. Quartz is the mineral defini ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Precambrian
The Precambrian (or Pre-Cambrian, sometimes abbreviated pꞒ, or Cryptozoic) is the earliest part of Earth's history, set before the current Phanerozoic Eon. The Precambrian is so named because it preceded the Cambrian, the first period of the Phanerozoic Eon, which is named after Cambria, the Latinised name for Wales, where rocks from this age were first studied. The Precambrian accounts for 88% of the Earth's geologic time. The Precambrian is an informal unit of geologic time, subdivided into three eons ( Hadean, Archean, Proterozoic) of the geologic time scale. It spans from the formation of Earth about 4.6 billion years ago ( Ga) to the beginning of the Cambrian Period, about million years ago ( Ma), when hard-shelled creatures first appeared in abundance. Overview Relatively little is known about the Precambrian, despite it making up roughly seven-eighths of the Earth's history, and what is known has largely been discovered from the 1960s onwards. The Precambrian fos ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nena People
The Nena people are an African tribe first encountered in the last quarter of the 19th century in the north-east Livingstone Mountains in what is now Tanzania by two different European travellers. The Scottish explorer Joseph Thomson stumbled across them in 1879 during his journey from the East African coast to Lake Nyasa (now also known as Lake Malawi) (Thomson 1881). Eighteen years later, in 1897, they were encountered a second time by the German priest Alphonse Adams (Adams 1899). Thomson and Adams' accounts had a number of similarities, which makes it probable that they met the same group of people. However, the next European visitor could find no trace of the Nena (Fülleborn 1906): they went missing from the ethnographic record and did not feature in subsequent German and British colonial Colonial or The Colonial may refer to: * Colonial, of, relating to, or characteristic of a colony or colony (biology) Architecture * American colonial architecture * French Colonial * ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ngoni People
The Ngoni people are an ethnic group living in the present-day Southern African countries of Malawi, Mozambique, Tanzania, Zimbabwe, and Zambia. The Ngoni trace their origins to the Nguni and Zulu people of kwaZulu-Natal in South Africa. The displacement of the Ngoni people in the great scattering following the Zulu wars had repercussions in social reorganization as far north as Malawi and Zambia. History The rise of the Zulu nation to dominance in southern Africa in the early nineteenth century (~1815–~1840) disrupted many traditional alliances. Around 1817, the Mthethwa alliance, which included the Zulu clan, came into conflict with the Ndwandwe alliance, which included the Nguni people from what is now kwaZulu-Natal. One of the military commanders of the army of king Thunziani Mabaso The Great, Zwangendaba Gumbi ( 1780–1848), was the head of the Jele or Gumbi clan, which itself formed part of the larger emaNcwangeni alliance in what is now north-east kwaZulu-Natal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pangwa People
The Pangwa are a Bantu ethnolinguistic group based in the Kipengere Range on the eastern shore of Lake Malawi, in the Ludewa District of Njombe Region in southern Tanzania. In 2002 the Pangwa population was estimated to number 95,00 The Pangwa language is a member of the Bantu languages, Bantu family. Alternate names for Pangwa are Ekipangwa and Kipangwa. See also * Nena people The Nena people are an African tribe first encountered in the last quarter of the 19th century in the north-east Livingstone Mountains in what is now Tanzania by two different European travellers. The Scottish explorer Joseph Thomson stumbled a ... References Ethnic groups in Tanzania Indigenous peoples of East Africa Languages of Tanzania Northeast Bantu languages {{tanzania-ethno-group-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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