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Chupanga
Chupanga, formerly Shupanga, also known as Lacerdónia, is a village in Marromeu District, Sofala Province, Mozambique, located on the right bank of Zambezi River. It is the administrative center of one of the two postos which constitute Marromeu District. There are strata of grey and yellow sandstone, along with limestone, located nearby. The village of Shupanga was founded before the arrival of Europeans. It was visited by the Second Zambesi expedition of David Livingstone. The wife of Livingstone, Mary, died in Shupanga of malaria. Chupanga is located on Road N219, which connects it with Marromeu to the east and provide access to EN1 road to the west. It is connected by an unpaved road R1002 with Inhamitanga Inhamitanga is a town in Cheringoma District in Sofala Province of Mozambique. Transport It is served by a station on the Mozambique Railway system, where it is a junction. Inhamitanga is connected by an unpaved road R1002 with Chupanga. .... References ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
David Livingstone
David Livingstone (; 19 March 1813 – 1 May 1873) was a Scottish physician, Congregationalist, and pioneer Christian missionary with the London Missionary Society, an explorer in Africa, and one of the most popular British heroes of the late 19th-century Victorian era. David was the husband of Mary Moffat Livingstone, from the prominent 18th Century missionary family, Moffat. He had a mythic status that operated on a number of interconnected levels: Protestant missionary martyr, working-class "rags-to-riches" inspirational story, scientific investigator and explorer, imperial reformer, anti-slavery crusader, and advocate of British commercial and colonial expansion. Livingstone's fame as an explorer and his obsession with learning the sources of the Nile River was founded on the belief that if he could solve that age-old mystery, his fame would give him the influence to end the East African Arab–Swahili slave trade. "The Nile sources", he told a friend, "are valuabl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marromeu District
Marromeu District is a district of Sofala Province in Mozambique. The principal town is Marromeu. The district is located in the northeast of the province, and borders with Chinde and Mopeia Districts of Zambezia Province in the north, Cheringoma District in the south and in the west, and with Caia District in the northwest. In the southeast, the district is limited by the Indian Ocean. The area of the district is . It has a population of 119,718 as of 2007. Geography The principal river of the district is the Zambezi, which separates it from Zambezia Province. Most of the rivers in the district are left tributaries of the Zambezi, and a large part of the Zambezi Delta lies within the district. The climate of the district is tropical humid, with the average annual rainfall being . History The population of the area before Portuguese colonization consisted mostly of nomadic Phozo peoples who were frequently in war with each other. Demographics As of 2005, 46% of the population ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Second Zambesi Expedition
The Second Zambezi expedition, from 1858 to 1864, was launched by the Royal Geographical Society of Britain to explore Southeast Africa for mineral deposits and other natural resources. The expedition led to the establishment of the Central Africa Mission and was under the command of Dr. David Livingstone, who would become famous for his journeys into the interior of Africa. References *{{cite book, last=Johnston, first=Harry H., title=Livingston and the explorations of Central Africa, year=1891, publisher=G. Philip & Son Zambesi Zambesi 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 hal ... 1850s in Africa 1860s in Africa 1850s in the British Empire 1860s in the British Empire Expeditions from the United Kingdom Royal Geographical Society 1858 in Africa 1864 in Africa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Inhamitanga
Inhamitanga is a town in Cheringoma District in Sofala Province of Mozambique. Transport It is served by a station on the Mozambique Railway system, where it is a junction. Inhamitanga is connected by an unpaved road R1002 with Chupanga. See also * Transport in Mozambique * Railway stations in Mozambique Railway stations in Mozambique include: Towns served by railways (The lines do not all connect, or connect indirectly) Northern system (northernmost) (CDN) (from west to east) * Nayuchi - Malawi - border town. * Malema - way station ** R ... References Populated places in Sofala Province {{Mozambique-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sofala Province
Sofala is a province of Mozambique. It has a population of 2,259,248 (2017 census). Beira is the capital of the province, named for the ruined port of Sofala which is to the south. History Portuguese landholder and imperialist Joaquim Carlos Paiva de Andrada established a base at the river mouth at what is now Beira in 1884. Sofala Province is one of the strongholds of the RENAMO. In late 1978 RENAMO guerrillas were "ranging into Sofala Province and launching attacks along the Beira–Chimoio road and rail line, the Dondo–Inhaminga corridor". Some of the more scarcely populated areas of the province are affected by landmines; defensive rings around villages were still common in some rural areas according to mid 1990s reports by Oxfam. In March 2019, the province was severely affected by Cyclone Idai, with its capital city of Beira being largely destroyed. The flooding resulting from this storm was widespread throughout the province and the rest of Central Mozambique. De ... [...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] |
Postos Of Mozambique
The districts of Mozambique are divided into 405 ''postos''. ''Postos administrativos'' (administrative posts) are the main subdivisions of districts. This name, in use during colonial times, was abolished after independence, and was replaced by ''localidades'' (localities). However, it was re-established in 1986.Lei nº 4/86 de 25 de Julho. Administrative posts are headed by a ''Secretário'' (secretary), which before independence were called ''Chefes de Posto'' (post chief). Administrative posts can be further subdivided into localities, also headed by secretaries. Notes ''This article includes content from the Portuguese Wikipedia article Posto administrativo.'' See also * List of postos of Mozambique Here is a list of administrative posts (''postos administrativos'') of Mozambique, sorted alphabetically by province and district, based on the National Statistics Institute of Mozambique. See also *Provinces of Mozambique *Districts of Mozamb ... References Subdi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stratum
In geology and related fields, a stratum ( : strata) is a layer of rock or sediment characterized by certain lithologic properties or attributes that distinguish it from adjacent layers from which it is separated by visible surfaces known as either '' bedding surfaces'' or ''bedding planes''.Salvador, A. ed., 1994. ''International stratigraphic guide: a guide to stratigraphic classification, terminology, and procedure. 2nd ed.'' Boulder, Colorado, The Geological Society of America, Inc., 215 pp. . Prior to the publication of the International Stratigraphic Guide, older publications have defined a stratum as either being either equivalent to a single bed or composed of a number of beds; as a layer greater than 1 cm in thickness and constituting a part of a bed; or a general term that includes both ''bed'' and ''lamina''.Neuendorf, K.K.E., Mehl, Jr., J.P., and Jackson, J.A. , eds., 2005. ''Glossary of Geology'' 5th ed. Alexandria, Virginia, American Geological Institute. 779 pp. . ... [...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 related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saunders_Quarry-1.jpg "Click for more on -> Sandstone")
