The bedrock can interpreted using the Geolectrical method. The aim of this research was determine the resistivity and structure of bedrock in Malalak District Agam area. This research used Dipole-dipole configuration and Schlumbergerconfiguration. Both of that configuration have complementary advantages and disadvantages to each other. The data were processed and interpreted with using Smoothness-Constraint Least Square inversion. The result of this research showed that type structure of bdrock in malalak Disctrict Agam area with Dipole-dipole configuration and Schlumberger configuration. The type structure of bedrock on this research is Clay, Sandstone, Limestone, Andesite andGranitee.
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