Integrating conventional and remote sensing with DC resistivity datasets to map groundwater potential areas using the analytical hierarchy process method, North Wadi Diit, Egypt.

The second geological layer, corresponding to the fourth geoelectrical layer, exhibits resistivity values ranging from 253.8 Ω m (VES-05) to 295.5 Ω m (VES-06) along the first profile, with a decreasing trend toward the southeast, as evidenced by lower values of 12.92 Ω m and 41.45 Ω m at VES-02 and VES-03, respectively.

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