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Hydro-Geological Context of Mikkes Springs and Different Variations of their Flows (Morocco)Keywords: Morocco , Mikkes , Sais phreatic aquifer , Sais confined aquifer , Tabular aquifer , springs , flow , hydro-geological context Abstract: 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
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