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Mount Morrumbala
Mount Morrumbala, also known as Mount Tembe, is a mountain in Morrumbala District of Zambezia Province in central Mozambique. Mount Morrumbala rises as an isolated massif at western edge of the Morrumbala Plateau. The Morrumbala Plateau reaches over 400 meters elevation, descending gently to the north, more sharply to the south and east, and steeply towards the valley of the Shire River to the west."Perfil do Distrito de Morrumbala Província da Zambézia". Ministério da Administração Estatal, República de Moçambique, 2014/ref> The Morrumbala escarpment separates the plateau from the Shire and Zambezi River, Zambezi lowlands to the west and south. The Shire River valley is a graben, part of the African Rift Valley system. The mountain's climate is cooler and wetter than the adjacent plateau and lowlands. Moist oceanic air masses moving in from the southeast rise up the mountain slopes and cool, and the moisture in the air condenses and falls as rain, or forms low clouds a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Portuguese Language
Portuguese ( or, in full, ) is a western Romance language of the Indo-European language family, originating in the Iberian Peninsula of Europe. It is an official language of Portugal, Brazil, Cape Verde, Angola, Mozambique, Guinea-Bissau and São Tomé and Príncipe, while having co-official language status in East Timor, Equatorial Guinea, and Macau. A Portuguese-speaking person or nation is referred to as " Lusophone" (). As the result of expansion during colonial times, a cultural presence of Portuguese speakers is also found around the world. Portuguese is part of the Ibero-Romance group that evolved from several dialects of Vulgar Latin in the medieval Kingdom of Galicia and the County of Portugal, and has kept some Celtic phonology in its lexicon. With approximately 250 million native speakers and 24 million L2 (second language) speakers, Portuguese has approximately 274 million total speakers. It is usually listed as the sixth-most spoken language, the third-most sp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Morrumbala District
Morrumbala District is a district of Zambezia Province in Mozambique. The town of Morrumbala is the district headquarters. The Shire River forms the western boundary of the district, separating the district from Tete Province and Malawi. The Ruo River, a tributary of the Shire, forms the northwestern boundary. Milange District lies to the north. Mocuba District lies to the east, and Nicoadala District to the southeast. Mopeia District Mopeia District is a district of Zambezia Province in Mozambique Mozambique (), officially the Republic of Mozambique ( pt, Moçambique or , ; ny, Mozambiki; sw, Msumbiji; ts, Muzambhiki), is a country located in southeastern Africa border ... is to the south. Most of the district lies on the Morrumbala Plateau. The plateau drops steeply on its western edge, called the Morrumbala Escarpment, to the valley of the Shire River. Mount Morrumbala (1,172 m.) lies on the western edge of the plateau. Further readingDistrict profile( PDF) {{co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zambezia Province
Zambezia ( pt, Zambézia) is the second most-populous province of Mozambique, located in the central coastal region south-west of Nampula Province and north-east of Sofala Province. It has a population of 5.11 million, according to the 2017 census. The provincial capital is Quelimane. Zambezia has a total area of 103,478 km2; much of it drained by the Zambezi River. Much of the coast consists of mangrove swamps, and there is considerable forest inland. Agricultural products include rice, maize, cassava, cashews, sugarcane, soybeans, coconuts, citrus, cotton, and tea. The country's largest tea estates are at Gurúè, while Lioma is a centre of soybean production. Fishing is especially productive of shrimp, and gemstones are mined at several sites. Vasco da Gama landed at the site of Quelimane in 1498. Shortly after, the Portuguese established a permanent presence, and many moved up the Zambezi into the interior, for many years the farthest inland European presence (although ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zambezi River
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 Ri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Graben
In geology, a graben () is a depressed block of the crust of a planet or moon, bordered by parallel normal faults. Etymology ''Graben'' is a loan word from German, meaning 'ditch' or 'trench'. The word was first used in the geologic context by Eduard Suess in 1883. The plural form is either ''graben'' or ''grabens''. Formation A graben is a valley with a distinct escarpment on each side caused by the displacement of a block of land downward. Graben often occur side by side with horsts. Horst and graben structures indicate tensional forces and crustal stretching. Graben are produced from parallel normal faults, where the displacement of the hanging wall is downward, while that of the footwall is upward. The faults typically dip toward the center of the graben from both sides. Horsts are parallel blocks that remain between graben; the bounding faults of a horst typically dip away from the center line of the horst. Single or multiple graben can produce a rift valley. Half-g ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
African Rift Valley
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rain Shadow
A rain shadow is an area of significantly reduced rainfall behind a mountainous region, on the side facing away from prevailing winds, known as its leeward side. Evaporated moisture from water bodies (such as oceans and large lakes) is carried by the prevailing onshore breezes towards the drier and hotter inland areas. When encountering elevated landforms, the moist air is driven upslope towards the peak, where it expands, cools, and its moisture condenses and starts to precipitate. If the landforms are tall and wide enough, most of the humidity will be lost to precipitation over the windward side (also known as the ''rainward'' side) before ever making it past the top. As the air descends the leeward side of the landforms, it is compressed and heated, producing foehn winds that ''absorb'' moisture downslope and cast a broad "shadow" of dry climate region behind the mountain crests. This climate typically takes the form of shrub–steppe, xeric shrublands or even deserts ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southern Zanzibar-Inhambane Coastal Forest Mosaic
Southern may refer to: Businesses * China Southern Airlines, airline based in Guangzhou, China * Southern Airways, defunct US airline * Southern Air, air cargo transportation company based in Norwalk, Connecticut, US * Southern Airways Express, Memphis-based passenger air transportation company, serving eight cities in the US * Southern Company, US electricity corporation * Southern Music (now Peermusic), US record label * Southern Railway (other), various railways * Southern Records, independent British record label * Southern Studios, recording studio in London, England * Southern Television, defunct UK television company * Southern (Govia Thameslink Railway), brand used for some train services in Southern England Media * ''Southern Daily'' or ''Nanfang Daily'', the official Communist Party newspaper based in Guangdong, China * ''Southern Weekly'', a newspaper in Guangzhou, China * Heart Sussex, a radio station in Sussex, England, previously known as "Southern FM" * 8 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eastern Miombo Woodlands
The Eastern miombo woodlands (AT0706) are an ecoregion of grassland and woodland in northern Mozambique, southern Tanzania, and southeastern Malawi. Setting These species-rich savanna ecosystems cover wide areas of gentle hills and low valleys containing rivers and dambo wetlands. The region is located on the East African Plateau, extending from inland south-eastern Tanzania to cover the northern half of Mozambique, with small areas in neighbouring Malawi. They are a section of the belt of miombo woodland that crosses Africa south of the Congo rain forests and the savannas of East Africa. The ecoregion covers an area of . It is bounded by the Northern and Southern Zanzibar-Inhambane coastal forest mosaic to the east along the Indian Ocean, and by the Zambezian and mopane woodlands in the Zambezi lowlands to the southwest, and by Lake Malawi to the west. To the north and northwest, the forested Eastern Arc Mountains separate the eastern miombo woodlands from the Southern Acacia-C ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zambezian And Mopane Woodlands
The Zambezian and mopane woodlands is a tropical and subtropical grasslands, savannas, and shrublands ecoregion of southeastern Africa. The ecoregion is characterized by the mopane tree ''(Colophospermum mopane)'', and extends across portions of Botswana, Malawi, Mozambique, Namibia, South Africa, Eswatini, Zambia, and Zimbabwe, including the lower basins of the Zambezi and Limpopo rivers. The more humid Southern Zanzibar-Inhambane coastal forest mosaic and Maputaland coastal forest mosaic ecoregions lie between the Zambezian and mopane woodlands and the Indian Ocean. The Zambezian and mopane woodlands lie generally at a lower elevation, and has lower rainfall, than the neighboring miombo woodlands ecoregions, which occupy the plateaus and escarpments above the river lowlands. It is bounded to the southwest by the Drakensberg Range and Southern African Bushveld and Drakensberg montane grassland, woodland, and forest ecoregions. To the west, it transitions to the drier Zambez ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
