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The Aswan Dam, or Aswan High Dam, is one of the world's largest embankment dams, which was built across the Nile in Aswan, Egypt, between 1960 and 1970. When it was completed, it was the tallest earthen dam in the world, surpassing the Chatuge Dam in the United States. [ 2 ]
The Aswan Low Dam or Old Aswan Dam is a gravity masonry buttress dam on the Nile River in Aswan, Egypt. The dam was built by the British at the former first cataract of the Nile, and is located about 1000 km up-river and 690 km (direct distance) south-southeast of Cairo. When initially constructed between 1899 and 1902, nothing of its scale had ...
Until 1974, the ruins of temples and an ancient Egyptian city were located here. They were damaged by several decades of seasonal submergence of the lake holding back the old Aswan Dam. [2] [3] With the commissioning of the Aswan High Dam in 1970, there was a threat of permanent flooding of the area. [4]
The Philae temple complex (/ ˈ f aɪ l iː /; Ancient Greek: Φιλαί or Φιλή and Πιλάχ, Arabic: فيلة Egyptian Arabic:, Egyptian: p3-jw-rķ' or 'pA-jw-rq; Coptic: ⲡⲓⲗⲁⲕ, ⲡⲓⲗⲁⲕϩ, [1] [2] Coptic pronunciation: [ˈpilɑk, ˈpilɑkh]) is an island-based temple complex in the reservoir of the Aswan Low Dam, downstream of the Aswan Dam and Lake Nasser, Egypt.
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Qasr Ibrim is the only major archaeological site in Lower Nubia to have survived the Aswan Dam floods. [ 2 ] [ 3 ] Both prior to and after the floods, it has remained a major site for archaeological investigations.
Philae flooded by the Aswan Low Dam in 1906. In 1902, the Aswan Low Dam was completed on the Nile River by the British. This threatened to submerge many ancient landmarks, including the temple complex of Philae. The height of the dam was raised twice, from 1907 to 1912 and from 1929 to 1934, and the island of Philae was nearly
The Cataracts of the Nile are shallow lengths (or whitewater rapids) of the Nile river, between Khartoum and Aswan, where the surface of the water is broken by many small boulders and stones jutting out of the river bed, as well as many rocky islets. In some places, these stretches are punctuated by whitewater, while at others the water flow is ...