Senegal River

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french: Fleuve Sénégal)
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, image_caption = Fishermen on the bank of the Senegal River estuary at the outskirts of Saint-Louis, Senegal
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, map_caption = Map of the Senegal River drainage basin.
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The Senegal River ( ar, نهر السنغال, Nahr as-Siniġāl, french: Fleuve Sénégal, wo, Dexug Senegaal) is a long river in West Africa; much of its length marks part of the border between Senegal and Mauritania. It has a drainage basin of , a mean flow of , and an annual discharge of . Important tributaries are the Falémé River, Karakoro River, and the Gorgol River. The river divides into two branches once it passes Kaédi The left branch, called the Doué, runs parallel to the main river to the north. After the two branches rejoin a few kilometers downstream of Podor.

In 1972 Mali, Mauritania and Senegal founded the Organisation pour la mise en valeur du fleuve Sénégal (OMVS) to manage the river basin. Guinea joined in 2005. , only very limited use was made of the river for the transportation of goods and passengers. The OMVS have looked at the feasibility of creating a navigable channel in width between the small town of Ambidédi in Mali and Saint-Louis, a distance of . It would give landlocked Mali a direct route to the Atlantic Ocean.

The aquatic fauna in the Senegal River basin is closely associated with that of the Gambia River basin, and the two are usually combined under a single ecoregion known as the Senegal-Gambia Catchments. Only three species of frogs and one fish are endemic to this ecoregion.

The river has two large dams along its course, the Manantali Dam in Mali and the Maka-Diama Dam downstream on the Mauritania-Senegal border. In between is the Félou Hydroelectric Plant, built in 1927, but replaced in 2014. The construction of the Gouina Hydroelectric Plant upstream of Felou at Gouina Falls began in 2013.

Geography

The Senegal's headwaters are the Semefé (Bakoye) and Bafing rivers which both originate in Guinea; they form a small part of the Guinea–Mali border before coming together at Bafoulabé in Mali. From there, the Senegal river flows west and then north through Talari Gorges near Galougo and over the Gouina Falls, then flows more gently past Kayes, where it receives the Kolimbiné. After flowing together with the Karakoro, it prolongs the former's course along the Mali–Mauritania border for some tens of kilometers till Bakel where it flows together with the Falémé River, which also has its source in Guinea, subsequently runs along a small part of the Guinea-Mali frontier to then trace most of the Senegal-Mali border up to Bakel. The Senegal further flows through semi-arid land in the north of Senegal, forming the border with Mauritania and into the Atlantic. In Kaedi it accepts the Gorgol from Mauritania. Flowing through Boghé it reaches Richard Toll where it is joined by the Ferlo coming from inland Senegal's Lac de Guiers. It passes through Rosso and, approaching its mouth, around the Senegalese island on which the city of Saint-Louis is located, to then turn south. It is separated from the Atlantic Ocean by a thin strip of sand called the Langue de Barbarie before it pours into the ocean itself.

The river has two large dams along its course, the multi-purpose Manantali Dam in Mali and the Maka-Diama Dam downstream on the Mauritania-Senegal border, near the outlet to the sea, preventing access of salt water upstream. In between Manantali and Maka-Diama is the Félou Hydroelectric Plant which was originally completed in 1927 and uses a weir. The power station was replaced in 2014. In 2013, construction of the Gouina Hydroelectric Plant upstream of Felou at Gouina Falls began.

The Senegal River has a drainage basin of , a mean flow of , and an annual discharge of .. Important tributaries are the Falémé River, Karakoro River, and the Gorgol River.

Downstream of Kaédi the river divides into two branches. The left branch called the Doué runs parallel to the main river to the north. After the two branches rejoin a few kilometres downstream of Pondor. The long strip of land between the two branches is called the Île á Morfil.

In 1972 Mali, Mauritania and Senegal founded the Organisation pour la mise en valeur du fleuve Sénégal (OMVS) to manage the river basin. Guinea joined in 2005.

At the present time, only very limited use is made of the river for the transport of goods and passengers. The OMVS have looked at the feasibility of creating a navigable channel in width between the small town of Ambidédi in Mali and Saint-Louis, a distance of . It would give landlocked Mali a direct route to the Atlantic Ocean.

The aquatic fauna in the Senegal River basin is closely associated with that of the Gambia River basin, and the two are usually combined under a single ecoregion known as the Senegal-Gambia Catchments. Although the species richness is moderately high, only three species of frogs and one fish are endemic to this ecoregion.

History

The existence of the Senegal River was known to the early Mediterranean civilizations. It or some other river was called ''Bambotus'' by Pliny the Elder (possibly from Phoenician "behemoth" for hippopotamus) and ''Nias'' by Claudius Ptolemy. It was visited by Hanno the Carthaginian around 450 BCE at his navigation from Carthage through the pillars of Herakles to Theon Ochema ( Mount Cameroon) in the Gulf of Guinea. There was trade from here to the Mediterranean World, until the destruction of Carthage and its west African trade net in 146 BCE.

Arab sources

In the Early Middle Ages (c. 800 CE), the Senegal River restored contact with the Mediterranean world with the establishment of the Trans-Saharan trade route between Morocco and the Ghana Empire. Arab geographers, like al-Masudi of Baghdad (957), al-Bakri of Spain (1068) and al-Idrisi of Sicily (1154), provided some of the earliest descriptions of the Senegal River. Early Arab geographers believed the upper Senegal River and the upper Niger River were connected to each other, and formed a single river flowing from east to west, which they called the "Western Nile". (In fact, some of the headwaters of the Senegal River are near the Niger River in Mali and Guinea.) It was believed to be either a western branch of the Egyptian Nile River or drawn from the same source (variously conjectured to some great internal lakes of the Mountains of the Moon, or Ptolemy's Gir (Γειρ) or the Biblical Gihon stream).

Arab geographers Abd al-Hassan Ali ibn Omar (1230), Ibn Said al-Maghribi (1274) and Abulfeda (1331), label the Senegal as the "Nile of Ghana" (Nil Gana or Nili Ganah).

As the Senegal River reached into the heart of the gold-producing Ghana Empire and later the Mali Empire, Trans-Saharan traders gave the Senegal its famous nickname as the "River of Gold". The Trans-Saharan stories about the "River of Gold" reached the ears of Sub-Alpine European merchants that frequented the ports of Morocco and the lure proved irresistible. Arab historians report at least three separate Arab maritime expeditions - the last one organized by a group of eight ''mughrarin'' ("wanderers") of Lisbon (before 1147) - that tried to sail down the Atlantic coast, possibly in an effort find the mouth of the Senegal.

Cartographic representation

Drawing from Classical legend and Arab sources, the "River of Gold" found its way into European maps in the 14th century. In the Hereford Mappa Mundi (c. 1300), there is a river labelled "Nilus Fluvius" drawn ''parallel'' to the coast of Africa, albeit without communication with Atlantic (it ends in a lake). It depicts some giant ants digging up gold dust from its sands, with the note "''Hic grandes formice auream serican r servantarenas''" ("Here great ants guard gold sands"). In the mappa mundi made by Pietro Vesconte for the c. 1320 atlas of Marino Sanuto, there is an unnamed river stemming from the African interior and opening in the Atlantic ocean. The 1351 Medici-Laurentian Atlas shows both the Egyptian Nile and the western Nile stemming from the same internal mountain range, with the note that "''Ilic coligitur aureaum''". The portolan chart of Giovanni da Carignano (1310s-20s) has the river with the label, ''iste fluuis exit de nilo ubi multum aurum repperitur''.

In the more accurately-drawn portolan charts, starting with the 1367 chart of Domenico and Francesco Pizzigano and carried on in the 1375 Catalan Atlas, the 1413 chart of the Catalan '' converso'' Mecia de Viladestes, etc. the "River of Gold" is depicted (if only speculatively), draining into the Atlantic Ocean somewhere just south of Cape Bojador. The legend of Cape Bojador as a terrifying obstacle, the 'cape of no return' to European sailors, emerged around the same time (possibly encouraged by Trans-Saharan traders who did not want to see their land route sidestepped by sea).

The river is frequently depicted with a great river island midway, the "Island of Gold", first mentioned by al-Masudi, and famously called "''Wangara''" by al-Idrisi and "''Palolus''" in the 1367 Pizzigani brothers chart. It is conjectured that this riverine "island" is in fact just the Bambuk-Buré goldfield district, which is practically surrounded on all sides by rivers - the Senegal river to the north, the Falémé River to the west, the Bakhoy to the east and the Niger

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