Kwilu River

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Kwilu River
Crossing kwilu river.jpg
May, 2003 - Villagers crossing the Kwilu river
Kasai River Catchment OSM.png
The Kwilu River in the Kasai catchment (center)
Location
Countries
Physical characteristics
Mouth 
 • coordinates
3°23′07″S 17°23′04″E / 3.385251°S 17.384491°E / -3.385251; 17.384491Coordinates: 3°23′07″S 17°23′04″E / 3.385251°S 17.384491°E / -3.385251; 17.384491
Length965 km (600 mi)
Basin features
River systemKasaï River

The Kwilu River (or Quilo River) is a major river that originates in Angola and flows north through Bandundu Province in the Democratic Republic of the Congo (DRC) to the city of Bandundu, where it joins the Kwango River just before this stream enters the Kasai River. In the DRC the river flows past the towns of Gungu, Kikwit, Bulungu, Bagata, Rutherfordia and Bandundu.[1] Lusanga, formerly Leverville, lies at the location where the Kwenge River joins the Kwilu, between Kikwit and Bulungu.[2]

Characteristics[]

It is a meandering river. Near its mouth it is 950 meter wide. The bed material is sand.[3] The river is about 965 kilometres (600 mi) long. In the wet season the flooded area covers 1,550 square kilometres (600 sq mi). The headwaters of the river rise at elevations between 1,000 metres (3,300 ft) and 1,800 metres (5,900 ft) in the Angolan highlands. They drop steeply to the flat central Congo Basin at between 500 metres (1,600 ft) and 300 metres (980 ft) above sea level. A 2011 survey found 113 species of fish in 21 families and eight orders.[4]

Same name rivers in South west DRC and north west Angola[]

Just south of the city of Kwilu Ngongo two other rivers name Kwilu are merging together at coordinate point 5°34'52"S 14°37'43"E

References[]

  1. ^ Blaes 2008.
  2. ^ C.J. Warrington (May 1972). "M'Bwa na Basenji" (PDF). The Basenji. Retrieved 2012-02-02.
  3. ^ Hanibal Lemma, and colleagues (2019). "Bedload transport measurements in the Gilgel Abay River, Lake Tana Basin, Ethiopia (Table 7)". Journal of Hydrology. 577: 123968. doi:10.1016/j.jhydrol.2019.123968.
  4. ^ Munene & Stiassny 2011.

Sources[]


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