Abstract
Mandli Basin was located in the Iraq-Iran border East of Diyala government. Thearea of basin its abut (491 km2). The basin was covered by recent deposits from theQuaternary age and the greater part of basin was located in the Mesopotamianvalley. The basin was completed study hydromorphomatric and themorphomatricanalysis was explain three stream order. The identical bifurcation 4.43and stream frequency 0.45 and the mass of basin were not good and discharge itsbad. As while as the basin was by far from the roundess and the basin shape wasnearby elongation and the relief was indicated .Quantity of Surface Run off in thebasin 50.8mm that is 19,24% from the precipitation and 7.1% from the precipitationto basin was infiltration to nutrition the ground water
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