Abstract
This research work aims to recognize the contact between Ajeel and Shari ground water basins on the South west limb of the Northern hemrien Anticline, depending on the hydraulic Conditions and Pumping test which carried out on three Wells in the Study area.
 According to the result, it is found that the Transmissivity(T) = 1177.605 m2/day, hydraulic conductivity (K)= 52.754 m/day, and Storage coefficient (Sc)= 0.00053, East the contact.
 While west of the contact T= 717.10 m2/day, K= 24.34 m/day, and Sc = 0.0001 .
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