Geoelectric resistivity method is one of a branch of geophysics method that is able detect an electric current in the earth subsurface. One of the application of geoelectric resistivity method is able to identify the quifer layer in subsurface.This research used the resistivity geoelectric method Schlumberger configuration. Study of investigation was located at Pasir Parupuk Tabing Padang. The investigations are conducted two sessions there are longitudinal direction and tranversal direction. Both directions have 600 m length. The investigation result shows that the area study have a good groundwater potential indicated by an aquifer having the character of sallow water table and unconfined aquifer. The aquifer potential lies at depth of about 55 – 125 meter.
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