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It displays abundant, well developed, large scale, cross-stratification and is the remains of a deflated Pleistocene seif dune created in response to the palaeo-Shamal winds (Kirkham, 1998a).
Marawah, Al Dabb'iya and Abu Dhabi Island), Al Aryam has clearly also been extended southwards by leeward accretion towards the mainland as Shamal-driven waves have driven sand southeast along the margins of the old seif dune remnants and beyond.
I'll wager this million-dollar baby has more in mind, given Hamas' encroachment of the seif dunes. The NARSS web URL to surface sediments is part encoded WAR_projectsportlet.