![]() Raw data obtained from data acquisition was analyzed using RES2DINV software. ![]() Data acquisition configuration was based on long and short arrangement, schlumberger array and 2.5 m of equal electrode spacing interval. Two spread lines of electrical resistivity imaging were performed on the slope crest using ABEM SAS 4000 equipment. As a result, this study introduced geophysical tools for slope seepage mapping based on electrical resistivity method. Conventional engineering tools to detect or mapped the seepage on slope experienced those problems involving large and high elevation of slope design. In the past, slope seepage mapping suffer from several limitation due to cost, time and data coverage. Problematic slope due to seepage phenomenon will influenced the slope strength thus promoting to its failure. Abstract The stability of slope may influenced by several factors such as its geomaterial properties, geometry and environmental factors.
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