Nile - Wikipedia. Nile. River. The river in Uganda. Countries. Ethiopia,Sudan,Egypt,Uganda,Congo- Kinshasa,Kenya,Tanzania,Rwanda,Burundi,South Sudan,Eritrea. Cities. Jinja,Juba,Khartoum,Cairo. Primary source. White Nile - elevation. It is generally regarded as the longest river in the world. The White Nile is considered to be the headwaters and primary stream of the Nile itself. The Blue Nile, however, is the source of most of the water and silt. The White Nile is longer and rises in the Great Lakes region of central Africa, with the most distant source still undetermined but located in either Rwanda or Burundi. It flows north through Tanzania, Lake Victoria, Uganda and South Sudan. The Blue Nile (Amharic: . The two rivers meet just north of the Sudanese capital of Khartoum. The northern section of the river flows north almost entirely through the Sudanese desert to Egypt, then ends in a large delta and empties into the Mediterranean Sea. Egyptian civilization and Sudanese kingdoms have depended on the river since ancient times. Most of the population and cities of Egypt lie along those parts of the Nile valley north of Aswan, and nearly all the cultural and historical sites of Ancient Egypt are found along riverbanks. In the ancient Egyptian language, the Nile is called . At Khartoum the river is joined by the Blue Nile. The White Nile starts in equatorial East Africa, and the Blue Nile begins in Ethiopia. Both branches are on the western flanks of the East African Rift. The drainage basin of the Nile covers 3,2. Africa. The Kagera River, which flows into Lake Victoria near the Tanzanian town of Bukoba, is the longest feeder, although sources do not agree on which is the longest tributary of the Kagera and hence the most distant source of the Nile itself. It flows north for some 1. Lake Kyoga. The last part of the approximately 2. Masindi Port, where the river turns north, then makes a great half circle to the east and north until Karuma Falls. For the remaining part it flows merely westernly 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. After leaving Lake Albert, the river continues north through Uganda and is known as the Albert Nile. In South Sudan. The river flows into South Sudan just south of Nimule, where it is known as the Bahr al Jabal (. Just south of the town it has the confluence with the Achwa River. The largest selection of conflict free diamonds. Choose from over 100,000 certified diamonds. Free Secure Shipping. The Bahr al Ghazal, itself 7. Bahr al Jabal at a small lagoon called Lake No, after which the Nile becomes known as the Bahr al Abyad, or the White Nile, from the whitish clay suspended in its waters. 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 1. An anabranch river, the Bahr el Zeraf, flows out of the Nile's Bahr al Jabal section and rejoins the White Nile. The flow rate of the Bahr al Jabal at Mongalla, South Sudan is almost constant throughout the year and averages 1,0. After Mongalla, the Bahr Al Jabal enters the enormous swamps of the Sudd region of South Sudan. More than half of the Nile's water is lost in this swamp to evaporation and transpiration. The average flow rate of the White Nile at the tails of the swamps is about 5. 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 River. This fluctuation is due the substantial variation in the flow of the Sobat, which has a minimum flow of about 9. Trailer for the film Death on the Nile, based off of the classic Agatha Christie novel of the same name. March and a peak flow of over 6. October. It flows over six groups of cataracts, from the first at Aswan to the sixth at Sabaloka (just north of Khartoum) and then turns to flow southward before again returning to flow north. One name for this is the . 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. It joins the Nile approximately 3. Khartoum. Blue Nile. Annotated view of the Nile and Red Sea, with a dust storm. The Blue Nile flows about 1,4. Khartoum, where the Blue Nile and White Nile join to form the Nile. Ninety percent of the water and ninety- six percent of the transported sediment carried by the Nile. Featuring jewelry boxes and displays. Large stock of jewelry supplies, including boxes, trays, tools, and watch displays. Nicky Romero is Joined by Nile Rodgers for 'Future Funk' By Idris Jones February 18, 2016. Nicky Romero is one of the most recognizable names in the electronic dance music industry. Having opened up about his battle with. Despite the odd misconception that Nile's members are of Egyptian descent, none are; they do, however, have an interest in Egyptian mythology, especially Karl Sanders. In the late 1980s, prior to forming Nile, Sanders played. Nile River, the father of African rivers and the longest river in the world. It rises south of the Equator and flows northward through northeastern Africa to drain into the Mediterranean. West Nile virus (WNV) is most commonly transmitted to humans by mosquitoes. You can reduce your risk of being infected with WNV by using insect repellent and wearing protective clothing to prevent mosquito bites. Nile red (also known as Nile blue oxazone) is a lipophilic stain. It is produced by boiling a solution of Nile blue with sulfuric acid. As can be seen from the structural formulae, this process replaces an iminium group with a. Above Khartoum the Nile is also known as the White Nile, a term also used in a limited sense to describe the section between Lake No and Khartoum. At Khartoum the river is joined by the Blue Nile. The White Nile starts in. The erosion and transportation of silt only occurs during the Ethiopian rainy season in the summer, however, when rainfall is especially high on the Ethiopian Plateau; the rest of the year, the great rivers draining Ethiopia into the Nile (Sobat, Blue Nile, Tekez. During the dry season the natural discharge of the Blue Nile can be as low as 1. During the wet season the peak flow of the Blue Nile often exceeds 5,6. August (a difference of a factor of 5. Before the placement of dams on the river the yearly discharge varied by a factor of 1. Aswan. Peak flows of over 8,2. August and early September, and minimum flows of about 5. April and early May. Bahr el Ghazal and Sobat River. The Bahr al Ghazal and the Sobat River are the two most important tributaries of the White Nile in terms of discharge. The Bahr al Ghazal's drainage basin is the largest of any of the Nile's sub- basins, measuring 5. Sudd wetlands. The Sobat River, which joins the Nile a short distance below Lake No, drains about half as much land, 2. Nile. 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. History. Reconstruction of the Oikoumene (inhabited world), an ancient map based on Herodotus' description of the world, circa 4. BC. 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. Climate change at the end of the most recent ice age led to the formation of the Sahara desert, possibly as long ago as 3. BC. Eonile. 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. An Eonile canyon, now filled by surface drift, represents an ancestral Nile called the Eonile that flowed during the later Miocene (2. The Eonile transported clastic sediments to the Mediterranean; several natural gas fields have been discovered within these sediments. During the late- Miocene Messinian salinity crisis, when the Mediterranean Sea was a closed basin and evaporated to the point of being empty or nearly so, the Nile cut its course down to the new base level until it was several hundred metres below world ocean level at Aswan and 2,4. Cairo. 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. Integrated Nile. 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. Said postulated that Egypt itself supplied most of the waters of the Nile during the early part of its history. 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. The White Nile Rift System, although shallower than the Bahr el Arab rift, is about 9 kilometers (5. Geophysical exploration of the Blue Nile Rift System estimated the depth of the sediments to be 5. 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 1. The Blue Nile connected to the main Nile during the 7. The White Nile system in Bahr El Arab and White Nile Rifts remained a closed lake until the connection of the Victoria Nile to the main system some 1. Role in the founding of Egyptian civilization. A felucca traversing the Nile near Aswan. The Greek historian Herodotus wrote that . An unending source of sustenance, it provided a crucial role in the development of Egyptian 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. The Ishango bone is probably an early tally stick. It has been suggested that this shows prime numbers and multiplication, but this is disputed. In the book How Mathematics Happened: The First 5. Years, Peter Rudman argues that the development of the concept of prime numbers could only have come about after the concept of division, which he dates to after 1. BC, with prime numbers probably not being understood until about 5. BC. These animals were killed for meat, and were domesticated and used for ploughing. 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.
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