Nubians are a Nilo-Saharan 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 civilization. In the southern valley of Egypt, Nubians differ culturally and ethnically from Egyptians, although they intermarried with members of other ethnic groups, especially Arabs. They speak Nubian languages as a mother tongue, part of the Northern Eastern Sudanic languages, and Arabic as a second language.
Meroë was an ancient city on the east bank of the Nile about 6 km north-east of the Kabushiya station near Shendi, Sudan, approximately 200 km north-east of Khartoum. Near the site is a group of villages called Bagrawiyah. This city was the capital of the Kingdom of Kush for several centuries from around 590 BC, until its collapse in the 4th century AD. The Kushitic Kingdom of Meroë gave its name to the "Island of Meroë", which was the modern region of Butana, a region bounded by the Nile, the Atbarah and the Blue Nile.
The Nubian pyramids were built by the rulers of the ancient Kushite kingdoms. The area of the Nile valley known as Nubia, which lies in northern present-day Sudan, was the site of three Kushite kingdoms during antiquity. The capital of the first was at Kerma. The second was centered on Napata. The third kingdom was centered on Meroë. The pyramids are built of granite and sandstone.
Wadi Allaqi, also transliterated as Wadi Allaqui or Wadi Alalaqi, is a wadi in southern Egypt. It begins in Sudan below the Halaib Triangle, and its mouth is south of Aswan on the eastern shore of Lake Nasser.
The Battle of Abu Klea, or the Battle of Abu Tulayh took place between 16 and 18 January 1885, at Abu Klea, Sudan, between the British Desert Column and Mahdist forces encamped near Abu Klea. The Desert Column, a force of approximately 1,400 soldiers, started from Korti, Sudan on 30 December 1884; the Desert Column's mission, in a joint effort titled "The Gordon Relief Expedition", was to march across the Bayuda Desert to the aid of General Charles George Gordon at Khartoum, Sudan, who was besieged there by Mahdist forces.
Napata was a city of ancient Kush at the fourth cataract of the Nile founded by the Egyptian Amun cult for Egyptian pilgrims given by its, as suggested, Egyptian name. It is located approximately 1.5 kilometers from the east side of the river at the site of modern Karima, Sudan.
The Arabian-Nubian Shield (ANS) is an exposure of Precambrian crystalline rocks on the flanks of the Red Sea. The crystalline rocks are mostly Neoproterozoic in age. Geographically – and from north to south – the ANS includes parts of Israel, Jordan, Egypt, Saudi Arabia, Sudan, Eritrea, Ethiopia, Yemen, and Somalia. The ANS in the north is exposed as part of the Sahara Desert and Arabian Desert, and in the south in the Ethiopian Highlands, Asir province of Arabia and Yemen Highlands.
The Nile Expedition, sometimes called the Gordon Relief Expedition (1884–1885), was a British mission to relieve Major-General Charles George Gordon at Khartoum, Sudan. Gordon had been sent to Sudan to help the Egyptians withdraw their garrisons after the British decided to abandon Sudan in the face of a rebellion led by self-proclaimed Mahdi, Mahommed Ahmed. A contingent of Canadians was recruited to help the British navigate their small boats up the Nile River. The Nile Expedition was the first overseas expedition by Canadians in a British imperial conflict, although the Nile Voyageurs were civilian employees and did not wear uniforms.
Wadi Hammamat is a dry river bed in Egypt's Eastern Desert, about halfway between Al-Qusayr and Qena. It was a major mining region and trade route east from the Nile Valley in ancient times, and three thousand years of rock carvings and graffiti make it a major scientific and tourist site today.
The National Museum of Sudan or Sudan National Museum, abbreviated SNM, is a two-story building, constructed in 1955 and established as national museum in 1971.
Al-'Ain al-Sokhna is a town in the Suez Governorate, lying on the western shore of the Red Sea's Gulf of Suez. It is situated 55 kilometres (34 mi) south of Suez and approximately 120 kilometres (75 mi) east of Cairo.
Mining in Egypt has had a long history that dates back to predynastic times. Active mining began in Egypt around 3000 BCE. Egypt has substantial mineral resources, including 48 million tons of tantalite, 50 million tons of coal, and an estimated 6.7 million ounces of gold in the Eastern Desert. The total real value of minerals mined was about E£102 million (US$18.7 million) in 1986, up from E£60 million (US$11 million) in 1981. The chief minerals in terms of volume output were iron ore, phosphates, and salt. The quantities produced in 1986 were estimated at 2,048, 1,310, and 1,233 tons, respectively, compared with 2,139, 691, and 883 tons in 1981. In addition, minor amounts of asbestos (313 tons) and quartz (19 tons) were mined in 1986. Preliminary exploration in Sinai indicated the presence of zinc, tin, lead, and copper deposits. Private sector exploration and exploitation activities so far have been limited. Only recently, AngloGold Ashanti with its joint Venture Partner Thani Dubai and a Canadian listed exploration company, Alexander Nubia International have been undertaking exploration in Egypt's Eastern Desert with some success. Centamin Ltd., a mineral exploration company founded in Australia, started a massive mining project in Sukari Hill.
Nubian architecture is diverse and ancient. Permanent villages have been found in Nubia, which date from 6000 BC. These villages were roughly contemporary with the walled town of Jericho in Palestine.
Nubia is a region along the Nile river encompassing the area between the first cataract of the Nile and the confluence of the Blue and White Niles, or more strictly, Al Dabbah. It was the seat of one of the earliest civilizations of ancient Africa, the Kerma culture, which lasted from around 2500 BC until its conquest by the New Kingdom of Egypt under Pharaoh Thutmose I around 1500 BC, whose heirs ruled most of Nubia for the next 400 years. Nubia was home to several empires, most prominently the Kingdom of Kush, which conquered Egypt in the eighth century BC during the reign of Piye and ruled the country as its 25th Dynasty.
The Kingdom of Kush, also known as the Kushite Empire, or simply Kush, was an ancient kingdom in Nubia, centered along the Nile Valley in what is now northern Sudan and southern Egypt.
Jubayt or Gebeit is a small town in eastern Sudan.
The Twenty-fifth Dynasty of Egypt, also known as the Nubian Dynasty, the Kushite Empire, the Black Pharaohs, or the Napatans, after their capital Napata, was the last dynasty of the Third Intermediate Period of Egypt that occurred after the Nubian invasion.
The mining industry of Sudan is mostly driven by extraction fuel minerals, with petroleum accounting for a substantial contribution to the country's economy, until the autonomous region of Southern Sudan became an independent country in July 2011. Gold, iron ore, and base metals are mined in the Hassai Gold Mine and elsewhere. Chromite is another important mineral extracted from the Ingessana Hills. Other minerals extracted are gypsum, salt, and cement. Phosphate is found in Mount Kuoun and Mount Lauro in eastern Nuba. Reserves of zinc, lead, aluminium, cobalt, nickel in the form of block sulfides, and uranium are also established. Large reserves of iron ore have been established.
The Wadi el-Hudi is a wadi in Southern Egypt, in the Eastern Desert. Here were ancient quarries for amethyst. The Wadi el-Hudi is important in archaeology for its high number of rock inscriptions and stelae, mainly dating to the Middle Kingdom, as amethyst was especially popular in this period. The Wadi el-Hudi ends in the Nile valley a few kilometers north of Aswan and is coming there from the South-East. The ancient amethyst quarries are about 20 kilometres south-east from Aswan.
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.
