“…The result has indicated that the clayey sand, the gravelly, and sandy soils are the major constituents of the site in Landmark University farm with resistivity ranging from 152 Ωm to 3045 Ωm ( Table 1 ). The average thickness of the weathered layer may not support groundwater yield [ 32 ]. Therefore, the fractured zone with massive sand body at depth ˃37 m is delineated as an aquiferous zone at the farm site.…”