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Wadi Muqaddam
Geography Wadi Muqaddam is a dry water course some 320 km extending from beyond Omdurman north to the great bend of the Nile near Korti. It gives its name to the geological Wadi Milk Formation. Delimiting the Bayuda Desert to the west it still flows during rainy seasons. Some scholars assume ''Wadi Muqaddam'' as a former channel of the White Nile.D. Q. Fuller and L. Smith, ''The Prehistory of the Bayuda: New Evidence from the Wadi Muqaddam'' In: Kendall, T, (ed.) Nubian Studies 1998. Proceedings of the Ninth Conference of the International Society of Nubian Studies, August 21–26, 1998. (pp. 265-281). Department of African-American Studies, Northeastern University, Boston. Archaeology Mesolithic pottery and lithics (stone tools and their manufacturing debris) from the Holocene and the Middle Stone Age have been found in ''Wadi Muqaddam''. In the north of the wadi there is the archaeological site of Al-Meragh. References {{coord missing, Sudan Muqaddam ( ar, مقدم) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Omdurman
Omdurman (standard ar, أم درمان ''Umm Durmān'') is a city in Sudan. It is the most populated city in the country, and thus also in the State of Khartoum. Omdurman lies on the west bank of the River Nile, opposite and northwest of the capital city of Khartoum. Etymology The name Omdurman (''Umm Durmān'') literally translates as "Mother of Durmān", but who she was or might have been is not known. History After the siege of Khartoum, followed by the building there of the tomb of the Mahdi after his death from typhus, the city grew rapidly. However, in the Battle of Omdurman in 1898 (which actually took place in the nearby village of Kerreri), Lord Kitchener decisively defeated the Mahdist forces. The following year British forces defeated Abdallahi ibn Muhammad, the Khalifa, as the Battle of Umm Diwaykarat; ensuring British control over the Sudan. In September 1898, the British army of twenty thousand well drilled men equipped with the latest arms, Maxim guns a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nile
The Nile, , Bohairic , lg, Kiira , Nobiin language, Nobiin: Áman Dawū is a major north-flowing river in northeastern Africa. It flows into the Mediterranean Sea. The Nile is the longest river in Africa and has historically been considered the List of rivers by length, longest river in the world, though this has been contested by research suggesting that the Amazon River is slightly longer.Amazon Longer Than Nile River, Scientists Say Of the world's major rivers, the Nile is one of the smallest, as measured by annual flow in cubic metres of water. About long, its drainage basin covers eleven countries: the Democratic Republic of the Congo, Tanzania, Burundi, Rwanda, Uganda, Kenya, Ethiopia, Erit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Korti
Korti or Kurti is a town in northern-central Sudan. In the Meroitic period the city appeared as Cadetum, Cadata or Coetum in Roman sources. The town lies about from Khartoum, on the south side of the Nile at the terminus of the Wadi Muqaddam. It is also known for being the centre location for the Shaigiya tribe. History In 1881, the Mahdist uprising led to Britain sending in an army in August 1884 under Garnet Wolseley in the so-called Nile Expedition to relieve General Gordon. Korti became a rallying point for British troops. In January 1885 a fort was built by British troops on the north side of the Nile, right in front of Korti. From here, the advance on the Nile and through the desert could take place simultaneously. In the fighting in the Bayuda Desert between ''Kurti'' and Metemmeh (on the Nile opposite Shendi) the Madhist Sudanese suffered a defeat in the Battle of Abu Klea soon after the base at Korti was built. See also * List of cities in Sudan This is a lis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wadi Milk Formation
The Wadi Milk Formation is a geological formation in Sudan whose strata date back to the Late Cretaceous. Originally, the formation was thought to be Albian to Cenomanian, later research has provided dating to the Campanian to Maastrichtian. Dinosaur remains are among the fossils that have been recovered from the formation.Weishampel, David B; et al. (2004). "Dinosaur distribution (Late Cretaceous, Africa)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 604-605. . It stretches from the lower Wadi Al-Malik across the Wadi Muqaddam into the Bayuda Desert.Oliver W.M.Rauhut, A Dinosaur Fauna from the Late Cretaceous (Cenomanian) of Northern Sudan. In: Palaeontologie africaine,35,61-84(1999) Vertebrate paleofauna Ornithischians Saurischians See also * List of dinosaur-bearing rock formations This list of dinosaur-bearing rock formations is a list of geologic formations in which din ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bayuda Desert
The Bayuda Desert, located at , is in the eastern region of the Sahara Desert, spanning approximately 100,000 km2 of northeast Sudan north of Omdurman and south of Korti, embraced by the great bend of the Nile in the north, east and south and limited by the Wadi Muqaddam in the west. The north to south aligned Wadi Abu Dom divides the Bayuda Desert into the eastern Bayuda Volcanic Field and the western ochre-coloured sand-sheets scattered with rocky outcrop. Gold mining occurs today from October to March, as labourers work auriferous quartz found in wadis and shallow mines. These workings are usually in areas previously worked during the New Kingdom of Egypt and the Early Arab Period. In July 2020, it was found that gold hunters had used heavy machinery at the Jabal Maragha archaeological site in the Bayuda Desert, destroying it by digging a huge trench. The gold diggers were arrested and their equipment seized, but they were later released without charges. The Bayuda D ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
White Nile
The White Nile ( ar, النيل الأبيض ') is a river in Africa, one of the two main tributaries of the Nile, the other being the Blue Nile. The name comes from the clay sediment carried in the water that changes the water to a pale color. In the strict meaning, "White Nile" refers to the river formed at Lake No, at the confluence of the Bahr al Jabal and Bahr el Ghazal Rivers. In the wider sense, "White Nile" refers to all the stretches of river draining from Lake Victoria through to the merger with the Blue Nile; the "Victoria Nile" from Lake Victoria via Lake Kyoga to Lake Albert, then the "Albert Nile" to the South Sudan border, and then the "Mountain Nile" or "Bahr-al-Jabal" down to Lake No. "White Nile" may sometimes include the headwaters of Lake Victoria, the most remote of which being from the Blue Nile. The 19th-century search by Europeans for the source of the Nile was mainly focused on the White Nile, which disappeared into the depths of what was then known ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mesolithic
The Mesolithic (Greek: μέσος, ''mesos'' 'middle' + λίθος, ''lithos'' 'stone') or Middle Stone Age is the Old World archaeological period between the Upper Paleolithic and the Neolithic. The term Epipaleolithic is often used synonymously, especially for outside northern Europe, and for the corresponding period in the Levant and Caucasus. The Mesolithic has different time spans in different parts of Eurasia. It refers to the final period of hunter-gatherer cultures in Europe and Western Asia, between the end of the Last Glacial Maximum and the Neolithic Revolution. In Europe it spans roughly 15,000 to 5,000 BP; in Southwest Asia (the Epipalaeolithic Near East) roughly 20,000 to 10,000 BP. The term is less used of areas farther east, and not at all beyond Eurasia and North Africa. The type of culture associated with the Mesolithic varies between areas, but it is associated with a decline in the group hunting of large animals in favour of a broader hunter-g ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Holocene
The Holocene ( ) is the current geological epoch. It began approximately 11,650 cal years Before Present (), after the Last Glacial Period, which concluded with the Holocene glacial retreat. The Holocene and the preceding Pleistocene together form the Quaternary period. The Holocene has been identified with the current warm period, known as MIS 1. It is considered by some to be an interglacial period within the Pleistocene Epoch, called the Flandrian interglacial.Oxford University Press – Why Geography Matters: More Than Ever (book) – "Holocene Humanity" section https://books.google.com/books?id=7P0_sWIcBNsC The Holocene corresponds with the rapid proliferation, growth and impacts of the human species worldwide, including all of its written history, technological revolutions, development of major civilizations, and overall significant transition towards urban living in the present. The human impact on modern-era Earth and its ecosystems may be considered of global si ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Middle Stone Age
The Middle Stone Age (or MSA) was a period of African prehistory between the Early Stone Age and the Late Stone Age. It is generally considered to have begun around 280,000 years ago and ended around 50–25,000 years ago. The beginnings of particular MSA stone tools have their origins as far back as 550–500,000 years ago and as such some researchers consider this to be the beginnings of the MSA. The MSA is often mistakenly understood to be synonymous with the Middle Paleolithic of Europe, especially due to their roughly contemporaneous time span, however, the Middle Paleolithic of Europe represents an entirely different hominin population, ''Homo neanderthalensis'', than the MSA of Africa, which did not have Neanderthal populations. Additionally, current archaeological research in Africa has yielded much evidence to suggest that modern human behavior and cognition was beginning to develop much earlier in Africa during the MSA than it was in Europe during the Middle Paleoli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Al-Meragh
Al-Meragh is an archaeological site in Sudan. It is situated in the Wadi Muqaddam approximately north of Omdurman in the Bayuda, an area that today is largely desert. A buried Napatan settlement was discovered at al-Meragh in 1999-2000. The site consists of two houses with stone pillars and stone door frames. Both buildings are oriented in the same way, which assumes a uniform plan. It appears that the place was inhabited by only one or two generations and was then destroyed by fire, apparently by nomads. The function of this settlement may have involved an administrative center as Nubians Nubians () (Nobiin: ''Nobī,'' ) are an ethnic group indigenous to the region which is now northern Sudan and southern Egypt. They originate from the early inhabitants of the central Nile valley, believed to be one of the earliest cradles of c ... colonized in this area. Further reading * Timothy Kendall: ''Evidence for a Napatan occupation of the Wadi Muqaddam: excavations at al-Meragh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wadis Of Sudan
Wadi ( ar, وَادِي, wādī), alternatively ''wād'' ( ar, وَاد), North African Arabic Oued, is the Arabic term traditionally referring to a valley. In some instances, it may refer to a wet (ephemeral) riverbed that contains water only when heavy rain occurs. Etymology The term ' is very widely found in Arabic toponyms. Some Spanish toponyms are derived from Andalusian Arabic where ' was used to mean a permanent river, for example: Guadalcanal from ''wādī al-qanāl'' ( ar, وَادِي الْقَنَال, "river of refreshment stalls"), Guadalajara from ''wādī al-ḥijārah'' ( ar, وَادِي الْحِجَارَة, "river of stones"), or Guadalquivir, from ''al-wādī al-kabīr'' ( ar, اَلْوَادِي الْكَبِير, "the great river"). General morphology and processes Wadis are located on gently sloping, nearly flat parts of deserts; commonly they begin on the distal portions of alluvial fans and extend to inland sabkhas or dry lakes. In basin and ran ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
