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Choa Mountains
The Choa Mountains (Portuguese: ''Serra Choa'') are a mountain range in Manica Province of Mozambique. The mountains lie in Báruè District, west of Catandica. The mountains are at the northern end of the Eastern Highlands. The higher Nyanga Mountains lie to the southwest. The eastern slope of the mountains rises steeply from the surrounding plateau, forming a 20km-long escarpment northwest of Catandica. Small areas of the range exceed 1500 meters elevation, and Serra Nhatoa, the highest peak, is over 1850 meters. The western slopes of the mountains are drained by the Gairezi River, which flows northwards towards the Zambezi River from its source in the Nyanga Mountains. The eastern slopes of the mountains are drained by the Nhazonia River (also known as the Nyadzonya River), a tributary of the Pungwe River. The mountains are mostly covered in miombo woodland. The eastern slopes intercept winds from the Indian Ocean, and the resulting orographic precipitation sustain lush mo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Serra Nhatoa (4329821971)
The Choa Mountains (Portuguese: ''Serra Choa'') are a mountain range in Manica Province of Mozambique. The mountains lie in Báruè District, west of Catandica. The mountains are at the northern end of the Eastern Highlands. The higher Nyanga Mountains lie to the southwest. The eastern slope of the mountains rises steeply from the surrounding plateau, forming a 20km-long escarpment northwest of Catandica. Small areas of the range exceed 1500 meters elevation, and Serra Nhatoa, the highest peak, is over 1850 meters. The western slopes of the mountains are drained by the Gairezi River, which flows northwards towards the Zambezi River from its source in the Nyanga Mountains. The eastern slopes of the mountains are drained by the Nhazonia River (also known as the Nyadzonya River), a tributary of the Pungwe River. The mountains are mostly covered in miombo woodland. The eastern slopes intercept winds from the Indian Ocean, and the resulting orographic precipitation sustain lush m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of Manica Province
Geography (from Greek: , ''geographia''. Combination of Greek words ‘Geo’ (The Earth) and ‘Graphien’ (to describe), literally "earth description") is a field of science devoted to the study of the lands, features, inhabitants, and phenomena of Earth. The first recorded use of the word γεωγραφία was as a title of a book by Greek scholar Eratosthenes (276–194 BC). Geography is an all-encompassing discipline that seeks an understanding of Earth and its human and natural complexities—not merely where objects are, but also how they have changed and come to be. While geography is specific to Earth, many concepts can be applied more broadly to other celestial bodies in the field of planetary science. One such concept, the first law of geography, proposed by Waldo Tobler, is "everything is related to everything else, but near things are more related than distant things." Geography has been called "the world discipline" and "the bridge between the human and t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eastern Zimbabwe Montane Forest-grassland Mosaic
:''"Eastern Highlands" also refers to Eastern Highlands Province in Papua New Guinea, and part of the Great Dividing Range, Australia.'' The Eastern Highlands, also known as the Manica Highlands, is a mountain range on the border of Zimbabwe and Mozambique. The Eastern Highlands extend north and south for about through Zimbabwe's Manicaland Province and Mozambique's Manica Province. The Highlands are home to the Eastern Zimbabwe montane forest-grassland mosaic ecoregion. The ecoregion includes the portion of the highlands above 1000 meters elevation, including the Inyangani Mountains, Bvumba Mountains, Chimanimani Mountains, Chipinge Uplands, and the isolated Mount Gorongosa further east in Mozambique. The Southern miombo woodlands ecoregion lies at lower elevations east and west of the highlands. The highlands have a cooler, moister climate than the surrounding lowlands, which support distinct communities of plants and animals. The ecoregion is home to several plant commun ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Protea
''Protea'' () is a genus of South African flowering plants, also called sugarbushes (Afrikaans: ''suikerbos''). Etymology The genus ''Protea'' was named in 1735 by Carl Linnaeus, possibly after the Greek god Proteus, who could change his form at will, possibly because they have such a wide variety of forms. Linnaeus's genus was formed by merging a number of genera previously published by Herman Boerhaave, although precisely which of Boerhaave's genera were included in Linnaeus's ''Protea'' varied with each of Linnaeus's publications. Taxonomy The family Proteaceae to which ''Protea'' species belong is an ancient one among angiosperms. Evidence from pollen fossils suggests Proteaceae ancestors grew in Gondwana, in the Upper Cretaceous, 75–80 million years ago. The Proteaceae are divided into two subfamilies: the Proteoideae, best represented in southern Africa, and the Grevilleoideae, concentrated in Australia and South America and the other smaller segments of Gondwana that ar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Orographic Precipitation
Orography is the study of the topographic relief of mountains, and can more broadly include hills, and any part of a region's elevated terrain. Orography (also known as ''oreography'', ''orology'' or ''oreology'') falls within the broader discipline of geomorphology. The term orography comes from the Greek: , hill, , to write. Uses Mountain ranges and elevated land masses have a major impact on global climate. For instance, the elevated areas of East Africa substantially determine the strength of the Indian monsoon.Srinivasan, J., Nanjundiah, Ravi S. and Chakraborty, Arindam (2005Impact of Orography on the Simulation of Monsoon Climate in a General Circulation Model''Indian Institute of Science'' In scientific models, such as general circulation models, orography defines the lower boundary of the model over land. When a river's tributaries or settlements by the river are listed in 'orographic sequence', they are in order from the highest (nearest the source of the river) to the l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southern Miombo Woodlands
The Southern miombo woodlands is a tropical grasslands and woodlands ecoregion extending across portions of Malawi, Mozambique, Zambia, and Zimbabwe. It is one of four miombo woodlands ecoregions that span the African continent south of the Congo forests and East African savannas. Geography The Eastern miombo woodlands covers the hills and low plateaus in the watersheds of the Zambezi and Limpopo rivers, north and south of the Zambezi, and north and east of the Limpopo. The drier Zambezian and mopane woodlands occupy the lowlands along the Zambezi and its major tributaries, including the Shire and Lugenda, and the lowlands of the Limpopo. To the north and northwest, the Eastern miombo woodlands transition to the Central Zambezian miombo woodlands. To the southwest, they transition to the Southern Africa bushveld. The Southern Zanzibar-Inhambane coastal forest mosaic bounds the ecoregion on the southeast, along the Indian Ocean coast. Zambia's capital Lusaka and Zimbabwe's ca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pungwe River
Pungwe River ( pt, Rio Púngoè, links=no or ''Rio Púnguè'') is a long river in Zimbabwe and Mozambique. It rises below Mount Nyangani in the Eastern Highlands of Zimbabwe and then flows southeasteastward through the Manica and Sofala provinces of Mozambique. The Pungwe enters the Urema Valley, the southernmost portion of the Great Rift Valley, where it forms the southern boundary of Gorongosa National Park. The Urema River joins it, and the river follows the rift valley southward. Large seasonal wetlands form around the Pungwe and Urema rivers in the rift valley section. It empties into the Mozambique Channel at Beira, forming a large estuary. It is one of the major rivers of Mozambique and often causes floods. Tributaries The principal left tributaries are, from upstream to downstream, the Nhazonia, Txatola, Vinduzi, and Nhandugue-Urema. The right tributaries are the Honde and the Muda. Pungwe basin Administratively, the Pungwe Basin covers parts of Sofala and Manica p ... [...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] |
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] |
Gairezi River
Overview The Gairezi River begins on the slope's of Zimbabwe's highest mountain, the 2,592 meter Mount Nyangani, and is located in eastern Zimbabwe. As it winds its way north from the Eastern Highlands, and for more than 60 km, it subsequently forms the border between Zimbabwe and Mozambique before joining the Mazowe and Zambezi Rivers—as well as the Luenha River, a tributary of the Zambezi—at approximately 160 km upstream. The Gaizeri River runs through Nyanga, a town in Zimbabwe's Manicaland Province Manicaland is a province in eastern Zimbabwe. After Harare Province, it is the country's second-most populous province, with a population of 2.037 million, as of the 2022 census. After Harare and Bulawayo provinces, it is Zimbabwe's third-most de .... River system Rivers of Zimbabwe {{Zimbabwe-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nyanga Mountains
Mount Nyangani (formerly Mount Inyangani) is the highest mountain in Zimbabwe at . The mountain is located within Nyanga National Park in Nyanga District, about northwest of Mutare. The summit lies atop a small outcrop of rock around above the surrounding area. The remainder of the peak is a broad moor of mainly rolling hills and plateau with an area of about 8 km2. The edges of this plateau then fall steeply to the east and west sides. The mountain vegetation is largely composed of heath around the summit plateau with evergreen forest along the wetter eastern slopes and grassland to the western side. Annual rainfall totals are high (around ) but long spells of dry weather occur during the winter period of May to August. Due to its relatively low altitude and tropical location, snow falls very rarely, last recorded in August 1935. Geology The mountain is composed of an upper sill of dolerite and sandstone, with the harder dolerite forming cliffs and ridges. The dolerite si ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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