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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.
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).
Its surface area ranges from 3,000 to 3,500 square kilometres (1,200 to 1,400 square miles), depending on season and rainfall. The lake level has been regulated since the construction of the control weir where the lake discharges into the Blue Nile. This controls the flow to the Blue Nile Falls (Tis Abbai) and hydro-power station.
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Balagas River - Baro River - Bashilo River - Beles River - Bilate River - Birbir River - Blue Nile - Borkana River. Cheleleka River. Dabus River - Dawa River - Dechatu River - Dembi River - Denchya River - Didessa River - Dinder River - Doha River - Dukem River. Erer River. Fafen River
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. Flowing first in a northwesterly direction to where the ...
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 Blue Nile Basin is a major geological structure in the northwestern Ethiopian Plateau formed in the Mesozoic Era during a period of crustal extension associated with the break-up of Gondwana, and filled with sedimentary deposits. The modern Blue Nile river cuts across part of the sedimentary basin. [1]