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Wadi El Natrun
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Wadi El Natrun
Wadi El Natrun (Arabic: وادي النطرون, lit. 'Valley of Natron'; Coptic: Ϣⲓϩⲏⲧ, romanized: Šihēt, lit. 'measure of the hearts') 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.
In Christian literature it is usually known as Scetis (Σκήτις in Hellenistic Greek) or Skete (Σκήτη, plural Σκήτες in ecclesiastical Greek). It is one of the three early Christian monastic centers located in the Nitrian Desert of the northwestern Nile Delta. The other two monastic centers are Nitria and Kellia. Scetis, now called Wadi El Natrun, is best known today because its ancient monasteries remain in use, unlike Nitria and Kellia which have only archaeological remains. The desertified valley around Scetis in particular may be called the Desert of Scetis.
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.
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.
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 (Ancient Greek: Νιτριώτης νομός). It was also known in Coptic as Mountain of Salt (Coptic: ⲡⲧⲱⲟⲩ ⲙⲡϩⲙⲟⲩ) or Phanihosem (Coptic: ⲫⲁⲛⲓϩⲟⲥⲉⲙ, lit. 'the one (place) on the natron').
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.
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Wadi El Natrun
Wadi El Natrun (Arabic: وادي النطرون, lit. 'Valley of Natron'; Coptic: Ϣⲓϩⲏⲧ, romanized: Šihēt, lit. 'measure of the hearts') 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.
In Christian literature it is usually known as Scetis (Σκήτις in Hellenistic Greek) or Skete (Σκήτη, plural Σκήτες in ecclesiastical Greek). It is one of the three early Christian monastic centers located in the Nitrian Desert of the northwestern Nile Delta. The other two monastic centers are Nitria and Kellia. Scetis, now called Wadi El Natrun, is best known today because its ancient monasteries remain in use, unlike Nitria and Kellia which have only archaeological remains. The desertified valley around Scetis in particular may be called the Desert of Scetis.
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.
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.
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 (Ancient Greek: Νιτριώτης νομός). It was also known in Coptic as Mountain of Salt (Coptic: ⲡⲧⲱⲟⲩ ⲙⲡϩⲙⲟⲩ) or Phanihosem (Coptic: ⲫⲁⲛⲓϩⲟⲥⲉⲙ, lit. 'the one (place) on the natron').
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.
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