CONCLUSION
The Electrical Resistivity Method has helped in the identification of, and better understanding of, aquifer dimensions. It has been established from this study that electrical resistivity methods are suited for estimating thickness of weathered mantle and mapping of bedrock topography and fractured zones. It is therefore suggested that geophysical methods, most especially the electrical resistivity method, along with geological methods should form an integral part of groundwater exploration programs in solving complex geohydrological problems associated with ground water occurrence and resource development.