“…The 1D VES data were acquired using the OYO McOhm Resistivity Meter and the Dipole-Dipole electrode configuration was used to site the thirty (30) points, in total, spread across eight communities in the district (i.e., Akantansu, Kenyasi By-Pass, Obenkrom, Yakuba Village, Kofi Manukrom, Nfahu-Nfaka, Panaba, Yaw Wusukrom, and Kokofu ). The VES data were thoroughly reviewed and then re-processed for analyses following standard procedures observed in previous studies (Ewusi and Kuma, 2009;Ratnakumari et al, 2012;Aning et al, 2019;Raji and Abdulkadir, 2020;Abdulrazzaq et al, 2020;) Abdulrazzaq et al, 2020;) The drilling records for the 16 borehole logs and their corresponding 1D VES data points were organized into parameters such as observed aquifer zone (screen position), depth to bedrock, well status, and predicted aquifers zone. The stratigraphic and lithological descriptions obtained from the boreholes logs were laterite, clay, phyllite, granite, and metamorphosed lava.…”