Revealing the geomorphic parameters of neotectonics based on geological and seismic data at Wadi Beda basin, NW Gulf of Suez, Egypt

Abstract The current study used remote sensing, GIS, and seismic data to determine the geological morphometric parameters of Wadi Beda Basin area, which is located in northwestern part Gulf Suez Province. geomorphic related with development neotectonics are deduced using Shuttle Radar Topography Mission (SRTM), DEM-derived catchments, drainage networks research area. most important applied area valley floor width height ratio (Vf), stream length gradient index (Sl), transverse topographic symmetry (T), hypsometric curve integral (HI), basin shape (Bs). Based on obtained parameter results, El-Noqra Umm Athala basins exhibit moderate tectonic activity considered be at their mature stage. main Elda moderately symmetrical reflect youth However, Bs suggests that has activity, whereas strong activity. By integrating data, it possible majority (83.4%) categorized by a risk. Low-risk high-risk zones, other hand, make up 11.1% 5.5%, respectively, wadis Main controlled NW-trending faults, perturbation sites concentrated there where these faults cross E-W-trending making them areas.