benefits of the aswan high dam in egypt
Aswan Dam The Aswan Dam, or more specifically since the 1960s, the Aswan High Dam, is an embankment dam built across the Nile in Aswan, Egypt, between 1960 and 1970. Its significance largely eclipsed the previous Aswan Low Dam initially completed in 1902 downstream. Based on the success of the Low Dam, then at its maximum utilization, construction of the High Dam became a key objective of the government following the Egyptian Revolution of 1952; with its ability to control flooding better, provide increased water storage for irrigation and generate hydroelectricity the dam was seen as pivotal to Egypt's planned industrialization. Like the earlier implementation, the High Dam has had a significant effect on the economy and culture of Egypt.
Water scarcity in Africa Africa's susceptibility to potential water-induced conflict can be separated into four regions: the Nile, Niger, Zambezi, and Volta basins.[14] Running through Egypt, Ethiopia, and Sudan, the Nile's water has the potential to spark conflict and unrest.[14] In the region of the Niger, the river basin extends from Guinea through Mali and down to Nigeria. Especially for Mali – one of the world's poorest countries – the river is vital for food, water and transportation, and its over usage is contributing to an increasingly polluted and unusable water source.[14] In southern Africa, the Zambezi river basin is one of the world's most over-used river systems, and so Zambia and Zimbabwe compete fiercely over it. Additionally, in 2000, Zimbabwe caused the region to experience the worst flooding in recent history when the country opened the Kariba Dam gates.[14] Finally, within the Volta river basin, Ghana is dependent on its hydroelectric output, but plagued by regular droughts which effect the production of electricity from the Akosombo Dam and limit Ghana's ability to sustain economic growth. Paired with the constraints this also puts on Ghana's ability to provide power for the area, this could potentially contribute to regional instability.[14]