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Wadi El Natrun

Wadi El Natrun is a depression in northern Egypt that is located 23 m (75 ft) below sea level and 38 m (125 ft) below the Nile River level. The valley contains several alkaline lakes, natron-rich salt deposits, salt marshes and freshwater marshes.

Geography
Wadi al-Natrun is the common name for a desert valley located west of the Nile Delta, along the El Tahrir markaz, which is about 10 km west of the entrance to Sadat City on the Cairo-Alexandria Desert Road, and about 50 km from Khattabah on the Nile (Rashid Branch), and it falls below the level of the plateau surface surrounding it about 50 meters. The length of this depression ranges between 5, 55 and 60 km, while its average width is 10 km, and its deepest point reaches 24 meters below sea level. The depression is the smallest depression in the Egyptian Western Desert, with an area of about 500 km2. Therefore, it is true that it is a depression and not a valley, because the region is a closed depression that has a beginning and an end, and it has no source, estuary or tributaries, so the launch of the word "Wadi" on the depression is not topographically correct. The Wadi contains 12 lakes, the total surface area of which is 10 km square and their average depth is only 2 m. The color of these lakes is reddish blue because its water is saturated with the Natron salt. ==History==
History
Fossil discoveries Fossils dating to the Pliocene era (5.3-2.6 million years ago) have been discovered in the Wadi El Natrun region, including the long-snouted crocodile Euthecodon, softshell turtles, the camel Paracamelus, the three toed hipparionine equine Cormohipparion, the primitive hippopotamus Archaeopotamus andrewsi, antelope including reedbuck (Renunca) and Alcelaphinae, and the elephant-relative Deinotherium. Ancient history Natron valley is first attested in the story of the Eloquent Peasant, and it is mentioned among the list of seven oases in the Temple of Edfu. In Ptolemaic times it constituted part of the Nitrite nome (). It was also known in Coptic as Mountain of Salt () The importance of the Natrun valley dates back to the Pharaonic era, as the ancient Egyptians and the Libyans fought many battles there. And this ended up with the Egyptians overcoming them and annexed the eastern side of the desert, which still belongs to Egypt. Then, Wadi al-Natrun became an administrative part of the country in the Pharaonic era, but there is no information about its history during their reign, and the latest writings on the wars between the Libu and the Egyptians indicate that the last of them was in 1170 BC during the reign of Ramesses III. As for the religious significance of Wadi al-Natrun, there are many discoveries that indicate that this area was considered sacred as early as year 2000 BCE at the very least. Among these discoveries is a bust of black granite dating back to the era of the Seventeenth Dynasty of the Pharaohs, and there is also a granite gate and stones from the lintel of a door bearing cartridges for King Amenemhat I, in a place called the backbone. Economic history The alkali lakes of the Natron Valley provided the Ancient Egyptians with the sodium bicarbonate used in mummification and in Egyptian faience, and later by the Romans as a flux for glass making. The Wadi El Natrun was likely one of the most important centers of primary glass production in Roman Egypt, supplying the provinces of the Roman Empire with raw glass material. Excavations revealed remains of large rectangular melting furnaces. After a tank furnace had cooled down completely, its vaulted roof was dismantled, and the resulting glass block was extracted and dispatched for further processing. This design form was probably chosen to facilitate the transport of the produced raw glass blocks to secondary workshops, which themselves might not had direct access to the necessary raw materials. Ouest Embiez 1, an early 3rd-century shipwreck discovered off the southern coast of Gallia, was carrying cargo of raw glass in blocks of different sizes, totaling around 15 to 18 tonnes, which appears to confirm the export of raw glass from the eastern provinces to some extent. The Egyptian Salt and Soda Company Railway was built at the end of the 19th century as a 33 miles (54 km) long narrow gauge railway with a gauge of 750 mm, which attracted the first tourists to the wadi. Monastic history The desolate region became one of Christianity's most sacred areas. The Desert Fathers and cenobitic monastic communities used the desert's solitude and privations to develop self-discipline (asceticism). Hermit monks believed that desert life would teach them to eschew the things of this world and follow God's call. Between the 4th and 7th century AD, hundreds of thousands of people from the world over joined the hundreds of Christian monasteries in the Nitrian Desert, centered on Nitria, Kellia and Scetis (Wadi El Natrun). Saint Macarius of Egypt first came to Scetis (Wadi El Natrun) around 330 AD where he established a solitary monastic site. His reputation attracted a loose band of anchorites, hermits and monks who settled nearby in individual cells. Many of them came from nearby Nitria and Kellia where they had previous experience in solitary desert living; thus the earliest cenobitic communities were a loose consolidation of like-minded monks. By the end of the fourth century, four distinct communities had developed: Baramus, Macarius, Bishoi and John Kolobos. At first these communities were groupings of cells centered on a communal church and facilities, but enclosed walls and watchtowers developed over time and in response to raids from desert nomads. causing many notable Desert Fathers to leave the region, such as Abba Anoub. As the Jesuit historian and Professor Willian J. Harmless said, "Scetis’s destruction marked a turning point in the history of early Christian monasticism. The site would be resettled a few years later, and in fact would suffer other raids, notably in 434, 444, and 570." Saint-Exupéry's plane crash The environs of Wadi Natrun have been identified as the likely site of where the plane of French aviator Antoine de Saint-Exupéry crashed on December 30, 1935. After miraculously surviving the crash, he and his plane's mechanic nearly died of thirst before being rescued by a nomad. Saint-Exupéry documented his experience in his book Wind, Sand and Stars. The event is thought to have inspired his most famous work, The Little Prince. ==Gallery==
Gallery
Image:Bischoy Kloster BW 10.jpg|Monastery of Saint Pishoy, Scetes, Egypt Image:Bischoy Kloster BW 1.jpg|Monastery of Saint Pishoy, Scetes, Egypt Image:Bischoy Kloster BW 9.jpg|Monastery of Saint Pishoy, Scetes, Egypt Image:Macarius Kloster BW 1.jpg|Monastery of Saint Macarius the Great, Scetes, Egypt File:Frescos from the Wadi Natrun monastery1.jpg|Frescos at the Syrian Monastery, Scetes, Egypt File:Frescos from the Wadi Natrun monastery2.jpg|Frescos at the Syrian Monastery, Scetes, Egypt File:Naba' El-Hamra Lake-2.JPG|Naba' El-Hamra Lake ==See also==
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