Geography
The primary source of the Balikh River is the karstic spring of 'Ayn al-'Arus, just south of the Syro-Turkish border. Additionally, the Balikh receives water from a number of periodical streams and wadis that drain the Harran Plain to the north, as well as the plains to the west and east of the river valley. These streams are the Jullab, the Wadi Qaramogh, and the Wadi al-Kheder.
A few kilometres south of 'Ayn al-'Arus, the Balikh is joined by the channel of the Jullab. This small river rises from springs north of Şanlıurfa, but already runs dry at Harran, before it can reach the Balikh. Numerous now dried-up wells in the old city of Harran suggest, however, that the water table may have been significantly higher in the past.
The Wadi al-Kheder drains the plain to the east of the Balikh Valley, and is fed by the Wadi al-Burj and the Wadi al-Hamar, which in turn is fed by the Wadi Chuera. These wadis, as well as the Wadi Qaramogh, can transport considerable amounts of water after heavy rainfall, and large limestone blocks can be found in their lower courses.
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