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White Nile

White Nile (Bahr al Jabal)
Victoria Nile, Albert Nile
River
Sudan Juba bridge.jpg
A steel Bailey bridge spans the White Nile at Juba, South Sudan
Countries Sudan, South Sudan, Rwanda, Tanzania, Uganda, Democratic Republic of the Congo
Cities Jinja, Juba, Khartoum
Source White Nile
 - coordinates 2°16′55.92″S 29°19′52.32″E / 2.2822000°S 29.3312000°E / -2.2822000; 29.3312000
Length 3,700 km (2,299 mi)
Basin 1,800,000 km2 (694,984 sq mi)
Discharge
 - average 878 m3/s (31,006 cu ft/s)

The White Nile (Arabic: النيل الأبيض‎‎ an nīl al 'abyaḍ) is a river of Africa, one of the two main tributaries of the Nile, the other being the Blue Nile.

In the strict meaning, "White Nile" refers to the river formed at Lake Victoria at the confluence of the Bahr al Jabal and Bahr el Ghazal Rivers. In the wider sense, "White Nile" refers to the rivers draining from Lake Victoria into the White Nile proper (Victoria Nile, Kyoga Nile, Albert Nile, Bahr-al-Jabal). It may also, depending on the speaker, refer to the headwaters of Lake Victoria (about 3,700 kilometres (2,300 mi) from the most remote sources down to Khartoum)

The 19th century search by Europeans for the source of the Nile was mainly focused on the White Nile, which disappeared into the depths of what was then known as "Darkest Africa". The White Nile's true source was not discovered until 1937, when the German explorer Burkhart Waldecker traced it to a stream in Rutovu at the base of Mount Kikizi.

When in flood, the Sobat River tributary carries a large amount of sediment, adding greatly to the White Nile's color.

The Kagera River, which flows into Lake Victoria near the Tanzanian town of Bukoba, is the longest feeder river for Lake Victoria, although sources do not agree on which is the longest tributary of the Kagera and hence the most distant source of the Nile itself.

The source of the Nile can be considered to be either the Ruvyironza, which emerges in Bururi Province, Burundi, near Bukirasaz or the Nyabarongo, which flows from Nyungwe Forest in Rwanda.


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