Hydro-Geological Context of Mikkes Springs and Different Variations of their Flows (Morocco)
محورهای موضوعی : Mineralogy
K. Belhassan
1
(UFR: Geology Applied to Hydro-Geological Researches. Faculty of Sciences Dhar Mehraz
B.P. 1796 Fez Atlas. 30 003. Fez. Morocco.)
کلید واژه: Morocco, Mikkes, Sais phreatic aquifer, Sais confined aquifer, Tabular aquifer, springs, Flow, hydro-geological context,
چکیده مقاله :
The Mikkes basin is located at the north center of Morocco. It comprises three different zones which represent diversified geologies which shelter a phreatic and confined aquifer in the Sais basin and a shallow aquifer in the Tabular Middle Atlas. The springs in the Sais phreatic aquifer have suffered a maximum depletion. The springs with a deep or mixed origin are known as low flow variation springs. Actually, the variations of the fall of spring’s flows could be linked to a different hydro-geological context of these springs.
The Mikkes basin is located at the north center of Morocco. It comprises three different zones which represent diversified geologies which shelter a phreatic and confined aquifer in the Sais basin and a shallow aquifer in the Tabular Middle Atlas. The springs in the Sais phreatic aquifer have suffered a maximum depletion. The springs with a deep or mixed origin are known as low flow variation springs. Actually, the variations of the fall of spring’s flows could be linked to a different hydro-geological context of these springs.
