different water bearing horizons within the coastal plain sands of the Calabar area in
southern Nigeria. Results show that two major water bearing horizons exist in the area:(i) an
upper zone consisting of medium-to coarse-grained sands and gravels having a mean
formation resistivity of 1500 Ω m (gravelly zone) and (ii) a lower zone consisting of fine-to
medium-grained sands with a mean formation resistivity of 320 Ω m (sandy zone). The …