Abstract
The research aims to reveal the analysis of the hydrological characteristics of the northern mountain Bekhair Basin within the Sulaymaniyah belt, and its area is estimated (264.22 km2). Its rocky and sedimentary formations date back to the triple and quadruple periods of sandstone, limestone and gypsum rocks located astronomically between two latitudes. (37o01’00”-37o08’00”) north And longitudes (42o20’00”-42o50’00”) east, while administratively in Dohuk Governorate it extends from Dohuk to Zakho, along the village of Fishkhabur at the Iraqi-Turkish border, and lies within the semi-arid climate that is characterized by high temperatures and its average during the month of July (34, 33.7) centigrade respectively for the two stations of Dohuk - Zakho and the annual rainfall amounted to (512.7, 559) mm respectively The hydrological characteristics of the basins were studied showing the possibility of generating water flow in the study area, in addition to the possibility of constructing additional dams to store water and benefit from it for the daily uses of shepherds and drinking Animals in the Chided period.
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