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Wadi Al-Batin alluvial fan, which extends northeastward from Hafar Al-Batin in Saudi Arabia to cover parts of Kuwait and southwestern Iraq, represents the largest of several other non-active fans in central and south Arabia. Evidence put forward suggests that, like other comparable deposits of varying age in the Arabian Peninsula, the Al-Batin fan was deposited following downdip breaching of a scarp...
Morphostructural analysis and interpretation of the geomorphic features of the surface of Kuwait are essentially dependant on the recognition of the structural configuration of the top of the upper Eocene Dammam Formation and its influence on the overlying sediments of the Kuwait Group. The top surface of the Dammam Formation has an undulatory form representing a series of N-S to NNW-SSE trending...
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