Bou Regreg
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| Bou Regreg | |
|---|---|
| Lua error in package.lua at line 80: module 'Module:InfoboxImage/data' not found. Valley of the Bou Regreg near Rabat, Morocco | |
| Lua error in package.lua at line 80: module 'Module:InfoboxImage/data' not found. Course of the Bou Regreg [2] | |
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| Native name | Template:Native name checker |
| Location | |
| Country | Morocco |
| Physical characteristics | |
| Mouth | |
• location | Atlantic Ocean |
• elevation | Template:Infobox river/calcunit |
| Length | Template:Infobox river/calcunit |
Basin size | Template:Infobox river/calcunit |
| • minimum | Template:Infobox river/calcunit |
| • average | Template:Infobox river/calcunit |
| • maximum | Template:Infobox river/calcunit |
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The Bou Regreg (Template:Langx) is a river located in western Morocco which discharges into the Atlantic Ocean between the cities of Rabat and Salé. The estuary of this river is termed Wadi Sala.[1]
The river is 240 kilometres long, with a tidal estuary of approximately 24 kilometres extending upriver. Its average discharge is 23 m3/s and can reach 1500 m3/s during periods of flooding. The river originates in the Middle Atlas mountains at an altitude of 1627 meters on the level of Jbel Mtourzgane (province of Khemisset) and of Grou (province of Khénifra) and descends to its mouth at the Atlantic Ocean, separating the cities of Rabat to the south and Salé to the north.
Water quality
Water quality issues of the Bou Regreg include tidal saltwater intrusion, excessive runoff of nitrates from agricultural land uses and mercury contamination thought to arise from use of certain pesticides within the drainage basin.[2]
History
The Phoenicians and the Carthaginians, who founded several colonies in Morocco, inhabited the banks of the Bou Regreg approximately two kilometers from its mouth at the ancient site of Chellah. This archaeological site contains the ruins of a Roman town known as Sala Colonia and referred to as Sala by Ptolemy. Chellah was a significant ancient port city with remains including the Decumanus Maximus, or principal roadway, as well as those of a forum, a monumental fountain, a triumphal arch, and other Roman ruins.[3]
See also
References
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- ^ Voyages and travels, Hakluyt Society, page 280 (1962)
- ^ Page Module:Citation/CS1/styles.css has no content."Tarik Bahaj, Geochemical Characteristics of the Continental Waters Downstream from the Bou Regreg Basin and the Temara Plain, Morocco, October 30, 2007". Archived from the original on October 20, 2014. Retrieved November 25, 2007.
- ^ C. Michael Hogan, Chellah, The Megalithic Portal, ed. A. Burnham, 2007 [1]
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