Earth and Environment Atlas

How The Planet Works
Sign In
Text size
100%
Theme
Geological Formation

Wadi El Natrun

Structural and Tectonic Formations

Wadi El Natrun is a depression in northern Egypt that lies about 23 meters below sea level and 38 meters below the level of the Nile River. It contains alkaline lakes, marshes and deposits of natron, a naturally occurring salt. Known historically as Scetis, the valley was one of three early Christian monastic centers in the Nitrian Desert and is still home to ancient monasteries that remain in active use. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

Connections

Caused By

Erosion, Processes

Wikidata P31 formation-type mapped to formative process Erosion via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Wadi El Natrun

In Discipline

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Wadi El Natrun
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Wadi El Natrun
Sources
Wadi El Natrun (Wikipedia)
Lead section
Quote, Lead section
Wadi El Natrun (Arabic: وادي النطرون, lit. 'Valley of Natron'; Coptic: Ϣⲓϩⲏⲧ, romanized: Šihēt, lit. 'measure of the heart') 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.
View the Source
Wikidata: Wadi El Natrun
Wikidata Q1074945, class allow-list match (w-wdresolver-0926)View the Source
Comments (0)
No comments yet. Be the first to share a thought.
Reader Challenges (0)
No disputes yet. Spotted an error or a better source? Open the first one.