RESuLtS And dIScuSSIon The results of faults, fracture zone and lineaments obtained from aerial photographs and geological / topographical map interpretations are indicated in Figure 1. Results obtained from resistivity imaging and self potential methods are shown in Figures 3 - 18. As can be seen from the resistivity images, a wide range of resistivities ranging from about 25 ohm.m to about 5000 ohm.m are shown on the resistivity image profiles, indicating areas of hard rocks (with a resistivity value approaching 5000 ohm.m) to areas of possible groundwater accumulations (with a resistivity of 10 – 100 ohm.m). Self-potential surveys were conducted to compliment and confirm the results obtained from resistivity images