Rutovu

Source of the " Great River Nile "                       
To visit this source, discovered in 1934 by the German explorer Burckhard Waldecker, one first has to travel to the commune of Rutovu, perched at the summit of Mount Kikizi, (2,145 meters). Starting out as a tiny trickle of water, the stream will change its name successively to Kasenyi, Kasumo, Kigira, Ruvyironza, Ruvubu, Kagera, Lake Victoria, Victoria Nile, Lake Kyoga, and Lake Albert, before finally becoming the mighty Nile, traveling for 6,700 km and almost tickling the feet of Egypt’s famous pyramids on its way to meet the Mediterranean. A symbolic pyramid has been build at Rutovu.
After Rutovu, a short visit is paid to Muhweza hot springs and the "German Falls," in the Mosso area.

Nile Controvercy
Since Europeans began exploring Africa, controversy has dogged the hunt for the remotest source of the Nile. Beginning in the mid-1800s, Lake Victoria was largely accepted as the source of the White Nile. But generations of explorers continued to push farther into the heart of Africa to discover tributaries of Lake Victoria that would qualify as the Nile’s “true” source. The cartographers at National Geographic Society have generally accepted two sources, one in Rwanda and one in Burundi, but the search and the controversy has continued right up to the present. In March 2006, a trio of explorers announced they had followed the Nile to its remotest point using Global Positioning System (GPS) devices, and that the river originated in a muddy pool deep in the nearly impenetrable Nyungwe Forest in Rwanda.


More Information

The Nile River                     
Introduction
The Nile river has been providing life to the vast Nile basin for hundreds of thousands of years. It is a great river which deserves our deepest respect.
The Nile River is the longest river in the world. From its major source, Lake Victoria in east central Africa, the White Nile flows generally north through Uganda and into Sudan where it meets the Blue Nile at Khartoum, which rises in the Ethiopian highlands. From the confluence of the White and Blue Nile, the river continues to flow northwards into Egypt and on to the Mediterranean Sea. From Lake Victoria to the Mediterranean Sea the length of the Nile is 5584 km (3470 mi). From its remotest headstream, the Ruvyironza River in Burundi, the river is 6671 km (4145 mi) long. The river basin has an area of more than 3,349,000 sq km (1,293,049 sq mi).

The White Nile
The Ruvyironza, regarded as the ultimate source of the Nile, is one of the upper branches of the Kagera River. The Kagera follows the boundary of Rwanda northward, turns where the borders of Rwanda, Uganda and Tanzania meet, and drains into Lake Victoria. On leaving Lake Victoria at the site of the now-submerged Owen Falls, the Nile rushes for 483 km (300 mi) over rapids and cataracts, at first northwest and then west, until it enters Lake Albert. The section between the two lakes is called the Victoria Nile. The river leaves the northern end of Lake Albert as the Albert Nile, flows through northern Uganda, and at the Sudan border becomes the Bahr al Jabal. At its junction with the Bahr al Ghazal, the river becomes the Bahr al Abyad, or the White Nile. Various tributaries flow through the Bahr al Ghazal district. At Khartoum the White Nile is joined by the Blue Nile, or Bahr al Azraq. These are so named because of the colour of the water.

The Blue Nile
The Blue Nile (in Arabic the Al Bahr al-Azraq), 1529 km (950 mi) long, gathers its volume mainly from Lake T’ana, in the Ethiopian Highlands; it is known here as the Abbai. The Blue Nile rises at a spring site upstream of Lake Tana in Ethiopia, 2,150 m (7,054 ft) above sea level. The river flows west then north until it eventually meets the White Nile at Khartoum. A length of 800 km/500 mi is navigable during high water times. Some 80% of Sudan's electricity is provided by hydroelectric schemes at Roseires and Sennar, and these dams provide irrigation water for over 10,000 sq km/3,860 sq mi of the Gezira Plain.

The Main Nile
From Khartoum the Nile flows northeast. 322 km (200 mi) below Khartoum it is joined by the ‘Atbarah River. The black sediment brought down by the 'Atbarah and Blue Nile Rivers used to settle in the Nile delta making it very fertile. This process historically occurred during the annual flooding of the Nile in the summer months. However, the opening of the Aswan High Dam in the early 1970s allowed for control of the flooding and reduced sediment deposits in the river as these now settle in Lake Nasser. During its course from the confluence of the ‘Atbarah through the Nubian Desert, the river makes two deep bends. From Khartoum to Aswan there are six cataracts. The Nile is navigable to the second cataract, a distance of 1,545 km (960 mi). The delta of the Nile is 190 km (120 mi) wide. The water level behind the Aswan Dam fell from 170 m (558 ft) in 1979 to 150 m (492 ft) in 1988, threatening Egypt's hydroelectric power generation.

Summary Fact File about the Nile River.
Length: (From White Nile Source to Mouth) 6695km (4184 miles).
Name: The Nile gets its name from the Greek word "Nelios", meaning River Valley.
Sources: The White Nile: Lake Victoria, Uganda. The Blue Nile: Lake Tana, Ethiopia.
Countries: The Nile and its tributaries flow though nine countries. The White Nile flows though Uganda, Sudan, and Egypt. The Blue Nile starts in Ethiopia. Zaire, Kenya, Tanzanian, Rwanda, and Burundi all have tributaries, which flow into the Nile or into lake Victoria Nyanes.
Cities: The major cities that are located on the edge of the Nile and White Nile are: Cairo, Gondokoro, Khartoum, Aswan, Thebes/Luxor, Karnak, and the town of Alexandria lies near the Rozeta branch.
Major Dams: The major dams on the Nile are Roseires Dam, Sennar Dam, Aswan High Dam, and Owen Falls Dam.
Flow Rate: The Nile River's average discharge is about 300 million cubic metres per day.

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