Baoulé River
The Baoulé River (French: Fleuve Baoulé, from Manding for "Red River") is a river in Mali in West Africa. It flows from a source west of Bamako to the Bakoy downastream of Toukoto and forms part of the Senegal watershed.[1][2]
| Baoulé River | |
|---|---|
Map of the Senegal River drainage basin | |
| Location | |
| Country | Mali |
| Physical characteristics | |
| Mouth | |
• location | Bakoy River near Toukoto |
• coordinates | 13°32′58″N 9°54′35″W / 13.54944°N 9.90972°W |
• elevation | 750 meters (2,460 ft) |
| Basin features | |
| River system | Senegal River |
In Manding languages, Baoulé signifies 'red river', Bakoye 'white river' and Bafing 'black river'.[1][2]
Geography edit
The Baoulé's source is in the hills 120 kilometers south-west of Bamako near the Guinean border. It flows in a northerly direction for more than 200 kilometers, then turns to the west, making a wide meander, then a large northerly loop. Throughout this stretch, it constitutes the northern limit of the Boucle du Baoulé National Park. The last part of the Baoule flows in a southwesterly direction. It reaches the Bakoye on the right bank, about twelve kilometers downstream from Toukoto, almost doubling its flow.
Its total length is about 500 kilometers. It is not navigable.
Flow edit
The average monthly flow, tracked over a period of 39 years (1952-1990) at a station opposite the small town of Bougouda at the Bakoy-Baoule confluence, was 64 cubic metres (2,300 cu ft) for a drainage area of approximately 65,000 square kilometres (7.0×1011 sq ft).[3]
References edit
- ^ a b (in French), Organisation pour la mise en valeur du fleuve Sénégal, archived from the original on 16 July 2013, retrieved 2 June 2012.
- ^ a b Maïga, Mahamadou (1995), Le bassin du fleuve Sénégal: de la Traite négrière au développement sous-régional autocentré (in French), L'Harmattan, p. 14 footnotes 4, 5.
- ^ Numbers calculated on the basis of measurements made on the Bakoye at Toukoto GRDC - Le Bakoye à Toukoto and OualiaGRDC - Le Bakoye à Oualia, upstream and downstream respectively of the confluence.