Pleistocene evolution of the Nile Valley in northern Upper Egypt |
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| Institution: | 1. Dept. Earth Science & Engineering, Imperial College London, Prince Consort Road, SW7 2BP, UK;2. Royal Observatory of Belgium, Av. Circulaire 3, 1180, Uccle, Brussels, Belgium;3. Renard Centre of Marine Geology, Ghent University, Krijgslaan 281 S8, B-9000 Ghent, Belgium;4. Université de Lille, UMR CNRS 8187 LOG, 59 655 Villeneuve d''Ascq, France |
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| Abstract: | In the El Minia district of northern Upper Egypt, the Pleistocene deposits of the Nile Valley include (?)Early Pleistocene conglomerates of the Armant Formation and (?)Middle Pleistocene sands of the Qena Formation. These sediments are exposed along both sides of the valley in terraces at different heights, unconformably overlying Eocene limestones. Field observations suggest that the conglomerate facies of the Armant Formation was deposited in proximal and mid-alluvial fans. The sands of the Qena Formation are differentiated into two facies: a cross-bedded sandstone, representative of alluvial fan—braided stream environments, and a facies of sand interbedded with mud that may have been deposited by a meandering river. The heavy minerals of the Armant Formation are markedly different from those of the Qena Formation, suggesting derivation from different sources. Surface textures of quartz grains from the Qena sands, observed by SEM, exhibit chemical features, attributed to a fluviatile origin. Sand from the Armant Formation is characterized by mechanical and chemical surface textural features that suggest original aeolian derivation followed by later fluvial sedimentation. |
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