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Atakora Mountains
The Togo Mountains is a mountain range which stretches across the central region of the West African country of Togo and across the eastern and western borders of that country into Ghana and Benin. In Ghana, the range is also known as the Akwapim Hills, and in Benin it is also known as the Atakora Mountains . Part of the range is associated with the country of Niger, where the W National Park is found.W National Park of Niger. 2009 The African wild dog, ''Lycaon pictus'', was historically found in this region but may now be extirpated from this locale.C. Michael Hogan. 2009 Geography The Togo Mountains run across the central region of Togo, ranging from the southwest to the northeast. To the northeast, the mountain range extends into Benin where it is known as the Atakora Mountains, and to the southwest it extends into Ghana where it is known as the Akwapim Hills. The average elevation of these mountains is and the highest peak in Togo is Mount Agou, with a height of . It is in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mont Sokbaro
Mont Sokbaro (also spelled as SagbaraoTchaboue, B.I. (2015) ''Tourisme et developpement socio-economique dans la commune de Bassila (Benin)''. Université d'Abomey-Calavi) is a hill that is mostly cited as the highest point of Benin, with an elevation of . This designation is contested, as SRTM readings at coordinates give an elevation of . This is a location southeast of Kotoponga. Mont Sokbaro is located on the border of the Donga Department in Benin and the Kara Region in the country of Togo, close to the source of the Mono River. It is located from the town of Bassila. The hill is part of the quartzite massif of the Atakora Mountains that continues westward into the latter country, where they are called the Togo Mountains. Some of these have higher elevations. On the Eastern side into Benin lies lower land with an average elevation of . Close by lie the villages of Tchèmbèré, Aledjo-Koura and Akaradè. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of Togo
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of Ghana
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mono River
The Mono River is the major river of eastern Togo. Approximately long, and draining a basin of about , it rises between the town of Sokodé and the border with Benin, and flows south. Along the southern portion of the river towards its mouth, it forms the international boundary between Togo and Benin. The river drains into the Bight of Benin through an extensive system of brackish water lagoons and lakes, including Lake Togo. Only the part of the river nearest its mouth is navigable. Most of the river's basin on the upper tableland is cultivated for maize, yams, rice, cotton and cassava. The river is dammed from its mouth by the Nangbeto Dam, a partnership between Benin and Togo completed in 1987. Studies have reported economic benefits from the dam, including tourism and fishing in the lake behind it. The dam's construction displaced between 7,600 and 10,000 people, however, and studies indicate that it has substantially modified the ecology of the lagoon system at the rive ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gulf Of Guinea
The Gulf of Guinea is the northeasternmost part of the tropical Atlantic Ocean from Cape Lopez in Gabon, north and west to Cape Palmas in Liberia. The intersection of the Equator and Prime Meridian (zero degrees latitude and longitude) is in the gulf. Among the many rivers that drain into the Gulf of Guinea are the Niger River, Niger and the Volta River, Volta. The coastline on the gulf includes the Bight of Benin and the Bight of Bonny. Name The origin of the name Guinea is thought to be an area in the region, although the specifics are disputed. Bovill (1995) gives a thorough description: The name "Guinea (region), Guinea" was also applied to south coast of West Africa, north of the Gulf of Guinea, which became known as "Upper Guinea", and the west coast of Southern Africa, to the east, which became known as "Lower Guinea". The name "Guinea" is still attached to the names of three countries in Africa: Guinea, Guinea-Bissau, and Equatorial Guinea, as well as New Guinea in Mel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Volta
Lake Volta, the largest artificial reservoir in the world based on surface area, is contained behind the Akosombo Dam which generates a substantial amount of Ghana's electricity. It is completely within the country of Ghana and has a surface area of . It extends from Akosombo in the south to the northern part of the country. Geography Lake Volta lies along the Prime meridian, and just six degrees of latitude north of the Equator. The lake's northernmost point is close to the town of Yapei, and its southernmost extreme is at the Akosombo Dam, downstream from Yapei. Akosombo Dam holds back both the White Volta River and the Black Volta River, which formerly converged where the middle of the reservoir now lies, to form the single Volta River. The present Volta River flows from the outlets of the dam's powerhouse and spillways to the Atlantic Ocean in southern Ghana. The main islands within the lake are Dodi, Dwarf, and Kporve. Digya National Park lies on part of the lake's weste ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Volta
The Volta River is the main river system in the West African country of Ghana. It flows south into Ghana from the Bobo-Dioulasso highlands of Burkina Faso. The main parts of the river are the Black Volta, the White Volta, and the Red Volta. In the northwest, the Black Volta forms the international borders between the Ivory Coast, Ghana, and Burkina Faso. The Volta flows southward along the Akwapim-Togoland highlands, and it empties into the Atlantic Ocean at the Gulf of Guinea at Ada Foah. It has a smaller tributary river, the Oti, which enters Ghana from Togo in the east. The Volta River has been dammed at Akosombo for the purpose of generating hydroelectricity. The reservoir named Lake Volta stretches from Akosombo Dam in the south to the northern part of the country, and is the largest man-made reservoir by area in the world. Volta was named by the Portuguese, meaning twist or turn. The country of Burkina Faso was formerly called Upper Volta, after the river. The reser ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oti River
The Oti River or Pendjari River is an international river in West Africa. It rises in Benin, forms the border between Benin and Burkina Faso, flows through Togo, and joins the Volta River in Ghana. Geography The Oti River is about long. Its headwaters are in Benin and Burkina Faso, it flows through Benin and Togo and joins the Volta River in Ghana. Tributaries on the left bank in Togo originate from the Togo Mountains to the south. One of its eastern tributaries is the Kara River, the confluence being on the Ghana–Togo border, where another tributary joins from the south, the Koumongou River. The mouth of the Oti was formerly on the Volta River, but it now flows into Lake Volta reservoir in Ghana. The river crosses the northern part of Togo in a savannah-clad valley some wide. Along the margins of the river is gallery forest which floods periodically. The dry season here lasts from about November until April, with the hot dry Harmattan wind blowing from the north. At this tim ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Agou
Mount Agou (French: ''Mont Agou'', earlier known as ''Baumannspitze'' or Baumann Peak) is the highest mountain in Togo at . It is situated to the south east of Kpalimé in the Plateaux Region of Togo. The mountain lies close to the border with Ghana; this country can be seen from the summit. Geology Mount Agou is part of an extreme western outlier of the Atakora Mountains that cross neighbouring Benin. Within the Togolese borders, this range is sometimes called the Togo Mountains. Together with these mountains, Mount Agou forms part of the Dahomeyide Orogen, an area that was uplifted in an orogenic process when the West African Craton bumped into the Benin-Nigerian Shield. The internal suture zone of this belt contains several isolated massifs that are oriented in North-South direction. Mount Agou is part of one of these massifs which, depending on the scientific classification, is either called the Lato-Agou Massif (together with nearby Lato Hill) or the Ahito-Agou Massif ( ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Houses On The Akwapim Mountain 2
A house is a single-unit residential building. It may range in complexity from a rudimentary hut to a complex structure of wood, masonry, concrete or other material, outfitted with plumbing, electrical, and heating, ventilation, and air conditioning systems.Schoenauer, Norbert (2000). ''6,000 Years of Housing'' (rev. ed.) (New York: W.W. Norton & Company). Houses use a range of different roofing systems to keep precipitation such as rain from getting into the dwelling space. Houses may have doors or locks to secure the dwelling space and protect its inhabitants and contents from burglars or other trespassers. Most conventional modern houses in Western cultures will contain one or more bedrooms and bathrooms, a kitchen or cooking area, and a living room. A house may have a separate dining room, or the eating area may be integrated into another room. Some large houses in North America have a recreation room. In traditional agriculture-oriented societies, domestic animals such ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Local Extinction
Local extinction, also known as extirpation, refers to a species (or other taxon) of plant or animal that ceases to exist in a chosen geographic area of study, though it still exists elsewhere. Local extinctions are contrasted with global extinctions. Local extinctions mark a change in the ecology of an area. In recent times, local extinction has sometimes been followed by a replacement of the species taken from other locations; wolf reintroduction is an example of this. The term "local extinction" is highly vernacular. The more proper biological term is ''extirpation''. Discussion Glaciation can lead to local extinction. This was the case during the Pleistocene glaciation event in North America. During this period, most of the native North American species of earthworm were killed in places covered by glaciation. This left them open for colonization by European earthworms brought over in soil from Europe. Species naturally become extirpated from islands over time. The number ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
