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Terrestrial erosion and marine transgressions left a cover of continental and shallow marine sedimentary rocks on the shelf. The shelf extends from the boundaries with the Arabian Shield in the west and south to margins of the Arabian Plate in the east, north and northwest: the Oman mountains and the Gulf of Oman, the Gulf–Euphrates sedimentary basin, the Zagros–Taurus mountain zone, and the Mediterranean Sea coast. The Dead Sea– Jordan rift zone dissects the shelf near its western margin as an approximately south–north directed major geosuture, extending from the Gulf of Aqaba to the Amiq depression.

The western margin of the closed basin zone is formed by the eastern slope of the Hermon–Antilebanon–Jebel ez Zaouiye mountains. Groundwater flow in the Antilebanon mountains, including Mount Hermon, comprises several separate systems with discharge in partly very large springs, from which perennial rivers rise, such as the Aouaj and Barada rivers in the Damascus basin. Some deep groundwater movement appears to be directed from the closed basins to topographically lower discharge areas of the Orontes, Euphrates and Yarmouk–Jordan–Dead Sea drainage systems.

5 Morphology The morphologic relief and erosional cycles are of major importance for the formation of detrital sediments. The morphology of the source areas of sediments is formed by tectonic and erosional forces and the resulting morphology of these source areas dominantly controls the nature of the deposited material. 2 Stratigraphic Distribution of Main Aquifers The distribution of aquifers with major economic importance on the Arabian Plate is closely related to the paleogeographic and tectonic-structural development of the plate, which controlled the history of erosional–depositional phases.

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