Abstract
The rock lithology of the potential hydrothermal area has been studied using Electrical Resistivity Tomography (ERT) in Pungguk Pedaro Village, Bingin Kuning District, Lebong Regency. Field data acquisition uses a stretch length of 480 meters with the MAE X612-EM Geoelectric tool that forms a straight line. ERT method, using Res2dinvx64 software. This study aims to determine the subsurface conditions of the potential hydrothermal area and the characteristics of the rocks that make up the hydrothermal area. The results of this study can be concluded that Pungguk Pedaro Village is dominated by Clay, Sandstone, Sandy Gravel, Andesite, Basalt, and Granite rocks. Line 1 has no potential for hydrothermal distribution because there has been a mixture of hydrothermal water with mountain water, so only groundwater is obtained on this line.
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