Manual The Geological Evolution of the River Nile

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For the remaining part it flows merely westerly through the Murchison Falls until it reaches the very northern shores of Lake Albert where it forms a significant river delta. The lake itself is on the border of DR Congo , but the Nile is not a border river at this point. Just south of the town it has the confluence with the Achwa River. When the Nile floods it leaves a rich silty deposit which fertilizes the soil.

The Nile no longer floods in Egypt since the completion of the Aswan Dam in More than half of the Nile's water is lost in this swamp to evaporation and transpiration. From here it soon meets with the Sobat River at Malakal. On an annual basis, the White Nile upstream of Malakal contributes about fifteen percent of the total outflow of the Nile. The course of the Nile in Sudan is distinctive. It flows over six groups of cataracts , from the sixth at Sabaloka just north of Khartoum northward to Abu Hamed. North of Cairo , the Nile splits into two branches or distributaries that feed the Mediterranean: the Rosetta Branch to the west and the Damietta to the east, forming the Nile Delta.

The Atbara flows only while there is rain in Ethiopia and dries very rapidly. During the dry period of January to June, it typically dries up north of Khartoum. In harsh and arid seasons and droughts the blue Nile dries out completely. The flow of the Blue Nile varies considerably over its yearly cycle and is the main contribution to the large natural variation of the Nile flow. Before the placement of dams on the river the yearly discharge varied by a factor of 15 at Aswan. The Bahr al Ghazal and the Sobat River are the two most important tributaries of the White Nile in terms of discharge.

The wadi passes through Gharb Darfur near the northern border with Chad and meets up with the Nile near the southern point of the Great Bend. The Nile iteru in Ancient Egyptian has been the lifeline of civilization in Egypt since the Stone Age , with most of the population and all of the cities of Egypt resting along those parts of the Nile valley lying north of Aswan.

The present Nile is at least the fifth river that has flowed north from the Ethiopian Highlands. Satellite imagery was used to identify dry watercourses in the desert to the west of the Nile. A canyon, now filled by surface drift, represents an ancestral Nile called the Eonile that flowed during the later Miocene 23—5. The Eonile transported clastic sediments to the Mediterranean; several natural gas fields have been discovered within these sediments. At some point the sediments raised the riverbed sufficiently for the river to overflow westward into a depression to create Lake Moeris.

Lake Tanganyika drained northwards into the Nile until the Virunga Volcanoes blocked its course in Rwanda. The Nile was much longer at that time, with its furthest headwaters in northern Zambia. There are two theories about the age of the integrated Nile. One is that the integrated drainage of the Nile is of young age, and that the Nile basin was formerly broken into series of separate basins, only the most northerly of which fed a river following the present course of the Nile in Egypt and Sudan. Rushdi Said postulated that Egypt itself supplied most of the waters of the Nile during the early part of its history.

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The other theory is that the drainage from Ethiopia via rivers equivalent to the Blue Nile, the Atbara and the Takazze flowed to the Mediterranean via the Egyptian Nile since well back into Tertiary times. Salama suggested that during the Paleogene and Neogene Periods 66 million to 2. This rift is possibly still active, with reported tectonic activity in its northern and southern boundaries. The Sudd swamps which form the central part of the basin may still be subsiding. Geophysical exploration of the Blue Nile Rift System estimated the depth of the sediments to be 5—9 kilometers 3.

These basins were not interconnected until their subsidence ceased, and the rate of sediment deposition was enough to fill and connect them. The Egyptian Nile connected to the Sudanese Nile, which captures the Ethiopian and Equatorial headwaters during the current stages of tectonic activity in the Eastern, Central and Sudanese Rift Systems.

The River Atbara overflowed its closed basin during the wet periods that occurred about , to , years ago. The Blue Nile connected to the main Nile during the 70,—80, years B. The Greek historian Herodotus wrote that "Egypt was the gift of the Nile". An unending source of sustenance, it provided a crucial role in the development of Egyptians civilization. Silt deposits from the Nile made the surrounding land fertile because the river overflowed its banks annually.

The Ancient Egyptians cultivated and traded wheat , flax , papyrus and other crops around the Nile. Wheat was a crucial crop in the famine-plagued Middle East. This trading system secured Egypt's diplomatic relationships with other countries, and contributed to economic stability. Far-reaching trade has been carried on along the Nile since ancient times. A tune, Hymn to the Nile , was created and sung by the ancient Egyptian peoples about the flooding of the Nile River and all of the miracles it brought to Ancient Egyptian civilization.

Water buffalo were introduced from Asia, and Assyrians introduced camels in the 7th century BC. These animals were killed for meat, and were domesticated and used for ploughing—or in the camels' case, carriage. Water was vital to both people and livestock. The Nile was also a convenient and efficient means of transportation for people and goods. The Nile was an important part of ancient Egyptian spiritual life. Hapi was the god of the annual floods, and both he and the pharaoh were thought to control the flooding.

The Nile was considered to be a causeway from life to death and the afterlife. The east was thought of as a place of birth and growth, and the west was considered the place of death, as the god Ra , the Sun, underwent birth, death, and resurrection each day as he crossed the sky. Thus, all tombs were west of the Nile, because the Egyptians believed that in order to enter the afterlife, they had to be buried on the side that symbolized death.

As the Nile was such an important factor in Egyptian life, the ancient calendar was even based on the 3 cycles of the Nile. These seasons, each consisting of four months of thirty days each, were called Akhet , Peret , and Shemu. Akhet, which means inundation, was the time of the year when the Nile flooded, leaving several layers of fertile soil behind, aiding in agricultural growth. Owing to their failure to penetrate the sudd wetlands of South Sudan , the upper reaches of the Nile remained largely unknown to the ancient Greeks and Romans.

Various expeditions failed to determine the river's source. Agatharcides records that in the time of Ptolemy II Philadelphus , a military expedition had penetrated far enough along the course of the Blue Nile to determine that the summer floods were caused by heavy seasonal rainstorms in the Ethiopian Highlands , but no European of antiquity is known to have reached Lake Tana.

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The Tabula Rogeriana depicted the source as three lakes in Europeans began to learn about the origins of the Nile in the 14th century when the Pope sent monks as emissaries to Mongolia who passed India, the middle east and Africa, and described being told of the source of the Nile in Abyssinia ancient European name for Ethiopia [54] [55] Later in the 15th and 16th centuries, travelers to Ethiopia visited Lake Tana and the source of the Blue Nile in the mountains south of the lake.

Europeans had been resident in Ethiopia since the late 15th century, and one of them may have visited the headwaters even earlier without leaving a written trace. Telles also used his account. The White Nile was even less understood. The ancients mistakenly believed that the Niger River represented the upper reaches of the White Nile. For example, Pliny the Elder wrote that the Nile had its origins "in a mountain of lower Mauretania ", flowed above ground for "many days" distance, then went underground, reappeared as a large lake in the territories of the Masaesyli , then sank again below the desert to flow underground "for a distance of 20 days' journey till it reaches the nearest Ethiopians.

Lake Victoria was first sighted by Europeans in when the British explorer John Hanning Speke reached its southern shore while traveling with Richard Francis Burton to explore central Africa and locate the great lakes. Believing he had found the source of the Nile on seeing this "vast expanse of open water" for the first time, Speke named the lake after the then Queen of the United Kingdom.

Burton, recovering from illness and resting further south on the shores of Lake Tanganyika, was outraged that Speke claimed to have proved his discovery to be the true source of the Nile when Burton regarded this as still unsettled. A very public quarrel ensued, which sparked a great deal of intense debate within the scientific community and interest by other explorers keen to either confirm or refute Speke's discovery.

British explorer and missionary David Livingstone pushed too far west and entered the Congo River system instead. It was ultimately Welsh-American explorer Henry Morton Stanley who confirmed Speke's discovery, circumnavigating Lake Victoria and reporting the great outflow at Ripon Falls on the Lake's northern shore.

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European involvement in Egypt goes back to the time of Napoleon. Laird Shipyard of Liverpool sent an iron steamer to the Nile in the s.

With the completion of the Suez Canal and the British takeover of Egypt in the s, more British river steamers followed. The Nile is the area's natural navigation channel, giving access to Khartoum and Sudan by steamer. The Siege of Khartoum was broken with purpose-built sternwheelers shipped from England and steamed up the river to retake the city.

After this came regular steam navigation of the river. With British Forces in Egypt in the First World War and the inter-war years, river steamers provided both security and sightseeing to the Pyramids and Thebes.

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Steam navigation remained integral to the two countries as late as Sudan steamer traffic was a lifeline as few railways or roads were built in that country. Most paddle steamers have been retired to shorefront service, but modern diesel tourist boats remain on the river. Macklin , Derek Anthony Welsby , D. Maddy , Michele Mackin. Adamson , B. De Cock , Rosanna M Mcevedy. The Jonglei canal — impact and opportunity William Richard Stern. Williams , D.

Adamson , H. The geological evolution of the river Nile Rushdi Said. Processes reshaping the Nile delta promontories of Egypt: pre- and post-protection Omran E. River Nile sediment. Krom , J. Stanley , Cliff , R. By clicking accept or continuing to use the site, you agree to the terms outlined in our Privacy Policy , Terms of Service , and Dataset License. Egyptian Archaeology 36, Folk R. Hemphill Publishing, Austin, p. Journal of Sedimentary Petrology 27, Ghilardi M. Surveys and Perspectives Integrating Environment and Society , Goiran J.

PhD thesis in physical geography, university of Provence Aix-Marseille 1 , p. Hassan F. Higgs R. Journal of sedimentary petrology 49, Hillier J. Krinsley D. Cambridge University Press, Cambridge, 91 p. Krom M. Geology , Science , Kuper R. Lario J. Quaternary Science Reviews 16, Lauffray J. Les Cahiers de Karnak, 5, Legrain G. Martin-Puertas C. Quaternary Research , Midant-Reynes B. Fayard, Paris, p. Petrie W. Editions Bernard Quaritch, London, 38 p. Pirazzoli P. Wiley, New York, p. Reinach A. Reimer P. Robinson C. Journal of African Earth Sciences 44, Said R. In Wendorf F.

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Sommaire - Document suivant. Plan Introduction. Geological and geomorphological settings. Archaeological context and study sites. Grain-size analyses and quartz microscopy. Magnetic susceptibility measurements. Radiocarbon dating conventional method. Surface topography within the Nile valley Coptos site and satellite image interpretation. Landscape evolution around the archaeological sites of Karnak and Coptos. Agrandir Original png, k.

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