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Semuliki National Park
Semuliki National Park is a national park in Bwamba County, a remote part of the Bundibugyo District in the Western Region of Uganda that was established in October 1993. It encompasses of East Africa's only lowland tropical rainforest. It is one of the richest areas of floral and faunal biodiversity in Africa, with bird and butterfly species being especially diverse. The park is managed by the Uganda Wildlife Authority. Location Semuliki National Park lies on Uganda's border with the Democratic Republic of the Congo. The Rwenzori Mountains are to the south-east of the park, while Lake Albert is to the park's north. The park lies within the Albertine Rift, the western arm of the East African Rift. The park is located on a flat to gently undulating landform that ranges from above sea level. The park experiences an average rainfall of , with peaks in rainfall from March to May and from September to December. Many areas of the park experience flooding during the wet season. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bundibugyo District
Bundibugyo District is a district in the Western Region of Uganda, bordering the Democratic Republic of the Congo (DRC). The town of Bundibugyo is where both the district headquarters and the Bwamba Kingdom seat ( Obudhingiya Bwa Bwamba) are located. Before July 2010, the districts of Ntoroko and Bundibugyo were one. These districts are the only two in Uganda that lie west of the Rwenzori mountains. Bundibugyo (With Ntoroko) was first named Semuliki district on separating it from the Greator Kabarole district alongside Rwenzori district (Kasese) in 1974. Location Via Karugutu Bundibugyo District is bordered by Ntoroko District to the northeast, Kabarole District to the east, Bunyangabu District to the southeast, Kasese District to the south and the D.R.C to the west and north. The district headquarters at Bundibugyo are located approximately , by road, west of Fort Portal city the capital of Rwenzori Sub-region. This is about , north of Kasese town but no motorable roads l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sea Level
Mean sea level (MSL, often shortened to sea level) is an average surface level of one or more among Earth's coastal bodies of water from which heights such as elevation may be measured. The global MSL is a type of vertical datuma standardised geodetic datumthat is used, for example, as a chart datum in cartography and marine navigation, or, in aviation, as the standard sea level at which atmospheric pressure is measured to calibrate altitude and, consequently, aircraft flight levels. A common and relatively straightforward mean sea-level standard is instead the midpoint between a mean low and mean high tide at a particular location. Sea levels can be affected by many factors and are known to have varied greatly over geological time scales. Current sea level rise is mainly caused by human-induced climate change. When temperatures rise, Glacier, mountain glaciers and the Ice sheet, polar ice caps melt, increasing the amount of water in water bodies. Because most of human settlem ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
DR Congo
The Democratic Republic of the Congo (french: République démocratique du Congo (RDC), colloquially "La RDC" ), informally Congo-Kinshasa, DR Congo, the DRC, the DROC, or the Congo, and formerly and also colloquially Zaire, is a country in Central Africa. It is bordered to the northwest by the Republic of the Congo, to the north by the Central African Republic, to the northeast by South Sudan, to the east by Uganda, Rwanda, and Burundi, and by Tanzania (across Lake Tanganyika), to the south and southeast by Zambia, to the southwest by Angola, and to the west by the South Atlantic Ocean and the Cabinda exclave of Angola. By area, it is the second-largest country in Africa and the 11th-largest in the world. With a population of around 108 million, the Democratic Republic of the Congo is the most populous officially Francophone country in the world. The national capital and largest city is Kinshasa, which is also the nation's economic center. Centered on the Congo Bas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Virunga National Park
, iucn_category = II , iucn_ref = , location = Democratic Republic of the Congo , map = Democratic Republic of the Congo , relief = 1 , coordinates = , area = , established = , nearest_city = Goma , photo =Virunga National Park-107997.jpg , photo_caption = , governing_body = Institut Congolais pour la Conservation de la Nature , website = , administrator =Emmanuel de Merode , embedded1 = , embedded2 = , visitation_num = , visitation_year = Virunga National Park is a national park in the Albertine Rift Valley in the eastern part of the Democratic Republic of the Congo. It was created in 1925. In elevation, it ranges from in the Semliki River valley to in the Rwenzori Mountains. From north to south it extends approximately , largely along the international borders with Uganda and Rwanda in the east. It covers an area of . Two active volcanoes are located in the park, Mount Nyiragongo and Nyamuragira. They have significantly shaped the national park's dive ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Queen Elizabeth National Park
Queen Elizabeth National Park is a national park in Uganda. Location Queen Elizabeth National Park (QENP) is in the Western Region of Uganda, spanning the districts of Kasese, Kamwenge, Rubirizi, and Rukungiri. The park is approximately by road south-west of Kampala, Uganda's capital and largest city. The city of Kasese lies to the northeast of the park, while the town of Rubirizi is to the southeast. The park adjoins Kyambura Game Reserve to the east, which itself adjoins the Kigezi Game Reserve (including the Maramagambo Forest) and thus the Kibale National Park to the northeast. The Virunga National Park in the Democratic Republic of the Congo lies across the border to the west. Together, these protected places completely encircle Lake Edward. The Rwenzori Mountains National Park in Uganda lies not far to the northwest. Confusingly, during the 1970s and 1980s, Western conservationists usually referred to the park as Rwenzori National Park. History In 1921, a rinderpest ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kibale National Park
Kibale Forest National Park is a national park in western Uganda, protecting moist evergreen rainforest. It is in size and ranges between and in elevation. Despite encompassing primarily moist evergreen forest, it contains a diverse array of landscapes.McGrew, William, ''et al''. ''Great Ape Societies''. Cambridge University Press, 1996. Print. Kibale is one of the last remaining expanses to contain both lowland and montane forests. In eastern Africa, it sustains the last significant expanse of pre-montane forest. The park was gazetted in 1932 and formally established in 1993 to protect a large area of forest previously managed as a logged forest reserve. The park forms a continuous forest with Queen Elizabeth National Park. This adjoining of the parks creates a wildlife corridor. It is an important ecotourism and safari destination, well-known for its population of habituated chimpanzees and twelve other species of primates. It is also the location of the Makerere University ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bwindi Impenetrable National Park
The Bwindi Impenetrable National Park (BINP) is in southwestern Uganda. The park is part of the Bwindi Impenetrable Forest and is situated along the Democratic Republic of the Congo (DRC) border next to the Virunga National Park and on the edge of the Albertine Rift. Composed of of both montane and lowland forest, it is accessible only on foot. BINP is a United Nations Educational, Scientific and Cultural Organization-designated World Heritage Site. Species diversity is a feature of the park. It provides habitat for 120 species of mammals, 348 species of birds, 220 species of butterflies, 27 species of frogs, chameleons, geckos, and many endangered species. Floristically, the park is among the most diverse forests in East Africa, with more than 1,000 flowering plant species, including 163 species of trees and 104 species of ferns. The northern (low elevation) sector has many species of Guineo-Congolian flora, including two endangered species, the brown mahogany and ''Brazzeia lo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Colonial Uganda
The Protectorate of Uganda was a protectorate of the British Empire from 1894 to 1962. In 1893 the Imperial British East Africa Company transferred its administration rights of territory consisting mainly of the Kingdom of Buganda to the British government. In 1894 the Uganda Protectorate was established, and the territory was extended beyond the borders of Buganda to an area that roughly corresponds to that of present-day Uganda. Background In the mid-1880s, the Kingdom of Uganda was divided between four religious factions - Adherents of Uganda's Native Religion, Catholics, Protestants and Muslims - each vying for political control.Griffiths, Tudor. “Bishop Alfred Tucker and the Establishment of a British Protectorate in Uganda 1890-94.” Journal of Religion in Africa, vol. 31, no. 1, 2001, pp. 92–114. JSTOR, www.jstor.org/stable/1581815. In 1888, Mwanga II was ousted in a coup led by the Muslim faction, who installed Kalema as leader. The following year, a Protestan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salt Lick
A mineral lick (also known as a salt lick) is a place where animals can go to lick essential mineral nutrients from a deposit of salts and other minerals. Mineral licks can be naturally occurring or artificial (such as blocks of salt that farmers place in pastures for livestock to lick). Natural licks are common, and they provide essential elements such as phosphorus and the biometals (sodium, calcium, iron, zinc, and trace elements) required in the springtime for bone, muscle and other growth in deer and other wildlife, such as moose, elephants, tapirs, cattle, woodchucks, domestic sheep, fox squirrels, mountain goats and porcupines. Such licks are especially important in ecosystems with poor general availability of nutrients. Harsh weather exposes salty mineral deposits that draw animals from miles away for a taste of needed nutrients. It is thought that certain fauna can detect calcium in salt licks. Overview Many animals regularly visit mineral licks to consume clay, supp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geyser
A geyser (, ) is a spring characterized by an intermittent discharge of water ejected turbulently and accompanied by steam. As a fairly rare phenomenon, the formation of geysers is due to particular hydrogeological conditions that exist only in a few places on Earth. Generally all geyser field sites are located near active volcanic areas, and the geyser effect is due to the proximity of magma. Generally, surface water works its way down to an average depth of around where it contacts hot rocks. The resultant boiling of the pressurized water results in the geyser effect of hot water and steam spraying out of the geyser's surface vent (a hydrothermal explosion). A geyser's eruptive activity may change or cease due to ongoing mineral deposition within the geyser plumbing, exchange of functions with nearby hot springs, earthquake influences, and human intervention. Like many other natural phenomena, geysers are not unique to Earth. Jet-like eruptions, often referred to as cryoge ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Swamp
A swamp is a forested wetland.Keddy, P.A. 2010. Wetland Ecology: Principles and Conservation (2nd edition). Cambridge University Press, Cambridge, UK. 497 p. Swamps are considered to be transition zones because both land and water play a role in creating this environment. Swamps vary in size and are located all around the world. The water of a swamp may be fresh water, brackish water, or seawater. Freshwater swamps form along large rivers or lakes where they are critically dependent upon rainwater and seasonal flooding to maintain natural water level fluctuations.Hughes, F.M.R. (ed.). 2003. The Flooded Forest: Guidance for policy makers and river managers in Europe on the restoration of floodplain forests. FLOBAR2, Department of Geography, University of Cambridge, Cambridge, UK. 96 p. Saltwater swamps are found along tropical and subtropical coastlines. Some swamps have hammock (ecology), hammocks, or dry-land protrusions, covered by aquatic vegetation, or vegetation that tolerates ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hot Spring
A hot spring, hydrothermal spring, or geothermal spring is a spring produced by the emergence of geothermally heated groundwater onto the surface of the Earth. The groundwater is heated either by shallow bodies of magma (molten rock) or by circulation through faults to hot rock deep in the Earth's crust. In either case, the ultimate source of the heat is radioactive decay of naturally occurring radioactive elements in the Earth's mantle, the layer beneath the crust. Hot spring water often contains large amounts of dissolved minerals. The chemistry of hot springs ranges from acid sulfate springs with a pH as low as 0.8, to alkaline chloride springs saturated with silica, to bicarbonate springs saturated with carbon dioxide and carbonate minerals. Some springs also contain abundant dissolved iron. The minerals brought to the surface in hot springs often feed communities of extremophiles, microorganisms adapted to extreme conditions, and it is possible that life on Earth had its ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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