The Upper Pliocene- Pleistocene Nile sediments cropping out in the areas around El Salamony and El Sawamha Sharq constitute two terraces including five facies: Flood plain, talus and lacustrine facies in the upper terrace skirting the Eocene scarp and fluviatile (channels and flood plain) facies in the lower terrace near the cultivated land. Distribution and facies changes exhibited by these ...
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