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Fig. 9 | Bulletin of the National Research Centre

Fig. 9

From: Flash floods mitigation and assessment of groundwater possibilities using remote sensing and GIS applications: Sharm El Sheikh, South Sinai, Egypt

Fig. 9

a Elevation layer showing shows a wide variations in the values ranging due to the structural setting which cause the basement uplift as a horst block. b Slope layer clarifies the lowland that includes fans and coastal plain are characterized by gentle slope (0°-8°) while the basement terrains and the isolated hills have steep slope (> 35°)

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