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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.
As a result of this, the Blue Nile was known as far as its exit from the Ethiopian foothills and the White Nile as far as the mouth of the Sobat River. Three expeditions under a Turkish officer, Selim Bimbashi, were made between 1839 and 1842, and two got to the point about 30 kilometres (20 miles) beyond the present port of Juba , where the ...
Gish Abay is best known as the source of the Abay, or Blue Nile, also known as Felege Ghion in Ge'ez, the liturgical language of Ethiopia.In scientific logic based on river basin, the source of Abay (the blue Nile) is Lake Tana. it is basically because the water volume that inters in to lake Tana from Gilgel Abay, Picolo Abay is only one third of the water volume that leaves Lake Tana at the ...
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 biosphere reserve comprises Lake Tana, the largest lake in Ethiopia, the main source of the Blue Nile, which provides important ecosystem services. The area is a hotspot of biodiversity, internationally known as an Important Bird Area and is of global importance for agricultural genetic diversity. The area is characterized by an enormous ...
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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]