Kawa River (Togo)
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Kawa River (Togo)
The Kawa River is an intermittent river and tributary in the Kara Region of Togo. The river flows from the Kara River near Agbande and joins the Katassou River near Binako Binako is a village in the Bassar Bassar is a town in Bassar Prefecture, Kara Region in Togo, situated west of Kara. The town borders Tatale which is in Ghana. The town has a population of 64,888. Culture Bassar was originally a centre for .... The sands of the Kawa River have been recommended for catchment works although the river is without road access. References Rivers of Togo Kara Region {{Togo-river-stub ...
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Togo
Togo (), officially the Togolese Republic (french: République togolaise), is a country in West Africa. It is bordered by Ghana to the west, Benin to the east and Burkina Faso to the north. It extends south to the Gulf of Guinea, where its capital, Lomé, is located. It covers about with a population of approximately 8 million, and has a width of less than between Ghana and its eastern neighbor Benin. From the 11th to the 16th century, tribes entered the region from various directions. From the 16th century to the 18th century, the coastal region was a trading center for Europeans to purchase slaves, earning Togo and the surrounding region the name "The Slave Coast". In 1884, Germany declared a region including a protectorate called Togoland. After World War I, rule over Togo was transferred to France. Togo gained its independence from France in 1960. In 1967, Gnassingbé Eyadéma led a successful military coup d'état, after which he became president of an anti-communist, ...
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River Mouth
A river mouth is where a river flows into a larger body of water, such as another river, a lake/reservoir, a bay/gulf, a sea, or an ocean. At the river mouth, sediments are often deposited due to the slowing of the current reducing the carrying capacity of the water. The water from a river can enter the receiving body in a variety of different ways. The motion of a river is influenced by the relative density of the river compared to the receiving water, the rotation of the earth, and any ambient motion in the receiving water, such as tides or seiches. If the river water has a higher density than the surface of the receiving water, the river water will plunge below the surface. The river water will then either form an underflow or an interflow within the lake. However, if the river water is lighter than the receiving water, as is typically the case when fresh river water flows into the sea, the river water will float along the surface of the receiving water as an overflow. Alon ...
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Kara River
The Kara (russian: Ка́ра) is a river draining to the Arctic Kara Sea in Russia. It flows through the Pai-Khoi Range in the Polar Ural region, and forms parts of the borders between the Yamalo-Nenets Autonomous Okrug, the Nenets Autonomous Okrug and the Komi Republic. The length of the river, from the confluence of the Malaya and Bolshaya Kara to the mouth in the Baydaratskaya Bay Baydaratskaya Bay or Baydarata Bay (russian: Байдарацкая губа, Baydaratskaya guba, Tundra Nenets language, Tundra Nenets: Пэдарита, ''Pėdarita'') is a gulf in Russia, located in the southern part of the Kara Sea between t ... is . Its drainage basin area is . The settlement of Ust-Kara is near the river mouth. The name of the river is derived from Nenets word meaning " hummocked ice".V.Yu. Vize, ''Karskoye more // Morya Sovetskoy Arktiki: Ocherki po istorii issledovaniya'' (Leningrad, 1939) — pp. 180—217 References Rivers of Yamalo-Nenets Autonomous Okrug R ...
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Intermittent River
Intermittent, temporary or seasonal rivers or streams cease to flow every year or at least twice every five years.(Tzoraki et al., 2007) Such rivers drain large arid and semi-arid areas, covering approximately a third of the earth's surface. The extent of temporary rivers is increasing, as many formerly perennial rivers are becoming temporary because of increasing water demand, particularly for irrigation. Despite inconsistent water flow, intermittent rivers are considered land-forming agents in arid regions, as they are agents of significant deposition and erosion during flood events. The combination of dry crusted soils and the highly erosive energy of the rain cause sediment resuspension and transport to the coastal areas.(Tzoraki et al., 2009) They are among the aquatic habitats most altered by human activities. During the summer even under no flow conditions the point sources are still active such as the wastewater effluents, resulting in nutrients and organic pollutant ...
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Tributary
A tributary, or affluent, is a stream or river that flows into a larger stream or main stem (or parent) river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean. The Irtysh is a chief tributary of the Ob river and is also the longest tributary river in the world with a length of . The Madeira River is the largest tributary river by volume in the world with an average discharge of . A confluence, where two or more bodies of water meet, usually refers to the joining of tributaries. The opposite to a tributary is a distributary, a river or stream that branches off from and flows away from the main stream."opposite to a tributary"
PhysicalGeography.net, Michael Pidwirny & S ...
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Kara Region
Kara is one of Togo's five regions. Kara is the regional capital. Other major cities in the Kara region include Bafilo, Bassar, and Niamtougou. Kara is divided into the prefectures of Assoli, Bassar, Bimah, Dankpen, Doufelgou, Kéran, and Kozah. Kara is located north of Centrale Region and south of Savanes Region. To the west lies the Northern Region of Ghana, and to the east lie the Atakora (further north) and Donga (further south) Departments of Benin. See also *Regions of Togo References Kara Region Kara is one of Togo's five regions. Kara is the regional capital. Other major cities in the Kara region include Bafilo, Bassar, and Niamtougou. Kara is divided into the prefectures of Assoli, Bassar, Bimah, Dankpen, Doufelgou, Kéran, and ...
{{Togo-geo-stub ...
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Kara River (Togo)
The Kara River is a river of northern Togo and Benin. It rises in Benin's Donga Department and flows northwest through Kara Region in Togo, including through the town of Kara, emptying into the Oti River on the Togo-Ghana Ghana (; tw, Gaana, ee, Gana), officially the Republic of Ghana, is a country in West Africa. It abuts the Gulf of Guinea and the Atlantic Ocean to the south, sharing borders with Ivory Coast in the west, Burkina Faso in the north, and To ... border. The Kara River Valley Agricultural Development Project is underway in the river valley, protecting about 300 square kilometres. References Rivers of Benin Rivers of Togo Kara Region Benin–Togo relations {{Benin-river-stub ...
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Agbande
Agbande is a village in the Doufelgou, Doufelgou Prefecture in the Kara Region of north-eastern Togo. There is also another village in the Prefecture which have the same name. This is located at: *Agbande Maplandia world gazetteer


References

Populated places in Kara Region Doufelgou Prefecture {{KaraTG-geo-stub ...
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Binako
Binako is a village in the Bassar Bassar is a town in Bassar Prefecture, Kara Region in Togo, situated west of Kara. The town borders Tatale which is in Ghana. The town has a population of 64,888. Culture Bassar was originally a centre for iron Iron () is a chemical elemen ... Prefecture in the Kara Region of north-western Togo.Maplandia world gazetteer References Populated places in Kara Region Bassar Prefecture {{KaraTG-geo-stub ...
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Catchment
A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the ''drainage divide'', made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, "watershed" is used only in its original sense, that of a drainage divide. In a closed drainage basin, or endorheic basin, the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, a dry lake, or a point where surface water is lost underground. Drainage basins are similar but no ...
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Rivers Of Togo
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, a ...
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