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The Blue Nile [note 1] is a river originating at Lake Tana in Ethiopia.It travels for approximately 1,450 km (900 mi) through Ethiopia and Sudan.Along with the White Nile, it is one of the two major tributaries of the Nile and supplies about 85.6% of the water to the Nile during the rainy season.
The Bashilo River (less often known as the Beshitta) is located in Ethiopia. Known for its canyon, which one source describes as almost as extensive as the canyon of its parent the Abay , [ 1 ] also known as the Blue Nile , the river originates just west of Kutaber in the Amhara Region .
During the dry season the natural discharge of the Blue Nile can be as low as 113 m 3 /s (4,000 cu ft/s), although upstream dams regulate the flow of the river. During the wet season, the peak flow of the Blue Nile often exceeds 5,663 m 3 /s (200,000 cu ft/s) in late August (a difference of a factor of 50).
Blue Nile Falls. The Blue Nile Falls is a waterfall on the Blue Nile river in West Gojjam, Amhara Region, Ethiopia. It is known as Tis Abay in Amharic, meaning 'great smoke'. It is situated on the upper course of the river, about 30 kilometres (19 miles) downstream from the town of Bahir Dar and Lake Tana. The falls are one of Ethiopia's best ...
The White Nile (Arabic: النيل الأبيض an-nīl al-'abyaḍ) is a river in Africa, the minor of the two main tributaries of the Nile, the larger being the Blue Nile. [4] The name "White" comes from the clay sediment carried in the water that changes the water to a pale color.
The Blue Nile is a river originating at Lake Tana in Ethiopia. With the White Nile, it is one of the two major tributaries of the Nile. The Blue Nile supplies about 80% of the water in the Nile during the rainy season.
The source is located 15 km west of Lake Tana at an elevation of 2,100 metres (6,900 ft) above sea level. The mouth of the river Beles in the Blue Nile is located about 40 km upstream of the Grand Ethiopian Renaissance dam that is under construction, and the water of the Beles will be used in the future.
The Blue Nile rift is a major geological structure in the Sudan, a rift with a NW trend that terminates on the Central African Shear Zone. [1] It was formed through crustal extension during the break-up of Gondwana .
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