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Abstract The Egyptian Nile, the northernmost segment of the Nile system, at Sohag area provides an excellent example for the studies of fluvial siliciclastics and mixed siliciclastic-carbonates transition. It also provides the opportunity to examine the influence of regional tectonics, local structures and paleoclimatic changes on the geomorphological evolution of drainage systems. These opportunities arise from that the present geological and geomorphological setting of this segment of the Egyptian Nile system manifest different evolutionary stages that were the result of the interplay between paleogeomorphology, tectonic and climate. |