Mount Sabinyo
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Mount Sabinyo
Mount Sabyinyo ("Sabyinyo" is derived from the Kinyarwanda word "Iryinyo", meaning "tooth"; also "Sabyinyo, Sabyinio") is an extinct volcano in eastern Africa in the Virunga Mountains. Mount Sabyinyo is the oldest volcano of the range. It is north-east of Lake Kivu, one of the African Great Lakes, and west of Lake Bunyonyi in Uganda. The summit of the mountain, at , marks the intersection of the borders of the Democratic Republic of the Congo (DRC), Rwanda, and Uganda, and holds religious significance for local tribes. It also is within the adjoining national parks established by these countries: Virunga National Park in the DRC, the Volcanoes National Park in Rwanda, and Mgahinga Gorilla National Park in Uganda. The slopes of Mount Sabyinyo are a habitat for the critically endangered mountain gorilla. The mountain carries the local nickname "Old Man's Teeth," because its serrated summit resembles worn teeth in a gum line (in contrast to the perfect conical summits of the adjacent ...
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Democratic Republic Of The Congo
The Democratic Republic of the Congo (DRC), also known as the DR Congo, Congo-Kinshasa, or simply the Congo (the last ambiguously also referring to the neighbouring Republic of the Congo), is a country in Central Africa. By land area, it is the List of African countries by area, second-largest country in Africa and the List of countries and dependencies by area, 11th-largest in the world. With a population of around 112 million, the DR Congo is the most populous nominally List of countries and territories where French is an official language, Francophone country in the world. Belgian French, French is the official and most widely spoken language, though there are Languages of the Democratic Republic of the Congo, over 200 indigenous languages. The national capital and largest city is Kinshasa, which is also the economic center. The country is bordered by the Republic of the Congo, the Cabinda Province, Cabinda exclave of Angola, and the South Atlantic Ocean to the west; the Cen ...
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Volcanoes Of Africa
A volcano is commonly defined as a vent or fissure in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and because most of Earth's plate boundaries are underwater, most volcanoes are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes resulting from divergent tectonic activity are usually non-explosive whereas those resulting from convergent tectonic activity cause violent eruptions."Mid-ocean ridge tectonics, volcanism and geomorphology." Geology 26, no. 455 (2001): 458. https://macdonald.faculty.geol.ucsb.edu/papers/Macdonald%20Mid-Ocean%20Ridge%20Tectonics.pdf Volcanoes can also form where there is stretching an ...
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Kisoro District
Kisoro District is a Districts of Uganda, district in the Western Region, Uganda, Western Region of Uganda. The town of Kisoro is the site of the district headquarters. Education Kisoro Municipality includes Metropolitan International University, a secular, private educational institution. Location Kisoro District is bordered by Kanungu District to the north, Kabale District to the east, Rwanda to the south, and the Democratic Republic of the Congo to the west. The town of Kisoro is approximately , by road, west of Kabale, the largest town in the Kigezi, sub-region. Population In 1991, the national population census estimated the district population at 186,870. The population was estimated at 220,300 during the 2002 national census. In 2012, the population was estimated at 254,300. The national population census on 27 August 2014, enumerated the district's population at 281,705 people. Religion As of September 2002, the religious affiliations of the district residents broke ...
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Democratic Republic Of The Congo–Uganda Border
Democrat, Democrats, or Democratic may refer to: Politics *A proponent of democracy, or democratic government; a form of government involving rule by the people. *A member of a Democratic Party: **Democratic Party (Cyprus) (DCY) **Democratic Party (Hong Kong) (DPHK) **Democratic Party (Italy) (PD) ** Democratic Party (Japan) (DP) **Democratic Party (United States) (D) **Democratic Progressive Party (DPP) ** Democratic Party’s (South Korea, 2015) **Democratic Party (Indonesia) (PD) **Democratic Party (other), for a full list *A member of a Democrat Party (other) *A member of a Democracy Party (other) *Australian Democrats, a political party *Democrats (Brazil), a political party *Democrats (Chile), a political party * Democrats (Croatia), a political party *Democrats (Gothenburg political party), in the city of Gothenburg, Sweden *Democrats (Greece), a political party *Democrats (Greenland), a political party * Democrats (Slovakia), a political party *De ...
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Democratic Republic Of The Congo–Rwanda Border
The border between the countries of Rwanda and the Democratic Republic of the Congo is 221 kilometers long. Crossing Lake Kivu in its entirety through the Virunga Mountains down to Mount Karisimbi, it divides the cities of Goma/Gisenyi and Bukavu/Cyangugu Cyangugu (formerly Shangugu) is a city and capital of the Rusizi District in Western Province, Rwanda. The city lies at the southern end of Lake Kivu, and is contiguous with Bukavu, Democratic Republic of the Congo, but separated from it by the .... There was a brief border clash between the two countries in 2012, which resulted in a few soldiers being killed. Additional alleged cross-border shellings happened during a period of heightened tensions between the two countries. See also * Democratic Republic of the Congo–Rwanda relations References {{DEFAULTSORT:Democratic Republic of the Congo-Rwanda border ...
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Border Tripoints
Borders are generally defined as geographical boundaries, imposed either by features such as oceans and terrain, or by political entities such as governments, sovereign states, federated states, and other subnational entities. Political borders can be established through warfare, colonization, or mutual agreements between the political entities that reside in those areas. Some borders—such as most states' internal administrative borders, or inter-state borders within the Schengen Area—are open and completely unguarded. Most external political borders are partially or fully controlled, and may be crossed legally only at designated border checkpoints; adjacent border zones may also be controlled. For the purposes of border control, airports and seaports are also classed as borders. Most countries have some form of border control to regulate or limit the movement of people, animals, and goods into and out of the country. Under international law, each country is general ...
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Three-thousanders
Three-thousanders are mountains with a height of between , but less than above sea level. Similar terms are commonly used for mountains of other height brackets e. g. four-thousanders or eight-thousanders. In Britain, the term refers to mountains above . Climatological significance In temperate latitudes three-thousanders play an important role, because even in summer they lie below the zero degree line for weeks. Thus the chains of three-thousanders always form important climatic divides and support glaciation - in the Alps the contour is roughly the general limit of the "nival step"; only a few glaciated mountains are under (the Dachstein, the easternmost glaciated mountain in the Alps, is, at , not a three-thousander). In the Mediterranean, however, the three-thousanders remain free of ice and, in the tropics, they are almost insignificant from a climatic perspective; here the snow line lies at around to , and in the dry continental areas (Trans-Himalayas, Andes) it m ...
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Stratovolcanoes Of The Democratic Republic Of The Congo
A stratovolcano, also known as a composite volcano, is a typically conical volcano built up by many alternating layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and explosive eruptions. Some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and solidifies before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high to intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less viscous mafic magma. Extensive felsic lava flows are uncommon, but can travel as far as 8 km (5 mi). The term ''composite volcano'' is used because strata are usually mixed and uneven instead of neat layers. They are among the most common types of volcanoes; more than 700 stratovolcanoes have erupted lava during the Holocene Epoch (the last 11,700 years), and many older, now ...
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Stratovolcanoes Of Uganda
A stratovolcano, also known as a composite volcano, is a typically Volcanic cone, conical volcano built up by many alternating layers (Stratum, strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and explosive eruptions. Some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and solidifies before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high to intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less viscous mafic magma. Extensive felsic lava flows are uncommon, but can travel as far as 8 km (5 mi). The term ''composite volcano'' is used because strata are usually mixed and uneven instead of neat layers. They are among the most common types of volcanoes; more than 700 stratovolcanoes have erupted lava during the Holocene Epoch (the last 11,700 year ...
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Stratovolcanoes Of Rwanda
A stratovolcano, also known as a composite volcano, is a typically conical volcano built up by many alternating layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and explosive eruptions. Some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and solidifies before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high to intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less viscous mafic magma. Extensive felsic lava flows are uncommon, but can travel as far as 8 km (5 mi). The term ''composite volcano'' is used because strata are usually mixed and uneven instead of neat layers. They are among the most common types of volcanoes; more than 700 stratovolcanoes have erupted lava during the Holocene Epoch (the last 11,700 years), and many older, now ...
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