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The basin rises in the highlands and flows in extremely arid regions, in particular the Sahara Desert. [3] Its main navigable course is through the Nile River, being the mouth section in the Mediterranean Sea (more precisely after the Nile Delta) until it surrounds the city of Aswan, in southern Egypt.
However, the riparian countries cooperate through the Nile Basin Initiative. Satellite view of the Nile near Qena in Upper Egypt. Egypt has four main groundwater aquifers: the Nile Aquifer, the Nubian Sandstone Aquifer, the Moghra Aquifer between the West of the Nile Delta and the Qattara Depression, and coastal aquifers on the North-Western ...
Congo Basin with the divide between it and the Nile Basin to the east highlighted in green. The Congo–Nile Divide or the Nile–Congo Watershed is the continental divide that separates the drainage basins of the Congo and Nile rivers. It is about 2,000 kilometres (1,200 mi) long.
The Nile is the only significant source of water in North Africa and 40% of Africa’s population lives in the Nile River Basin. [3] The Nile has two major tributaries: the White Nile and the Blue Nile. The White Nile is the longer of the two, rising in the Great Lakes Region of central Africa.
The next agreement on water use in the Nile did not come for exactly three more decades. The new 1959 Nile Agreement was signed by Egypt and Sudan, and was at this point free from political influence by the UK. However, the limitation of this agreement was that it was not more than a bilateral treaty between the two participant countries and ...
This has resulted in the development so far of 18,000 km 2 (6,900 sq mi) of irrigated land, making Sudan the second most extensive user of the Nile, after Egypt. [3] While Egypt is highly dependent on the Nile, there are factors that may lead to the necessity of conflict over the distribution of the Nile's water supply.
The Bahr al Ghazal's drainage basin is the largest of any of the Nile's sub-basins, measuring 520,000 square kilometers (200,000 sq mi) in size, but it contributes a relatively small amount of water, about 2 m 3 /s (71 cu ft/s) annually, because tremendous volumes of water are lost in the Sudd wetlands.
On January 25 and February 10, 1991, the reservoir continued to lose about 3.4 km2 per day of the lake surface, leading to a final surface area of 215 km2 and a volume of 3.3 km3. [72] This was the same time in February 1991 when multiple British bombers sent multiple missiles hitting bridges in southern and western Iraq , killing more than 100 ...