K Kaligending Village which is geographically located between 7 ° 35 '22"South Latitude and 109 ° 41 '05" East Longitude. Villages with elevationdifferences cause differences in aquifer height. Based on the difference in heightwithin the study site, this research was conducted with a geoelectrical resistivitymethod, to determine the depth and thickness of the aquifer. An aquifer is agroundwater carrier layer that has a rock composition that can store and drainwater in significant quantities. The purpose of resistivity estimation is to investigatechanges in rock resistivity with respect to depth. This study uses the SchlumbergerConfiguration. Vertical electronic sounding (VES) method is a common methodused to measure and analyze crossing of aquifer zones with geoelectricity becausethe results are more accurate and the cost it requires is lower. Geoelectricsounding method is done by injecting direct current DC (Direct current) where apair of electrodes with other electrodes are plugged into the ground so that depthand resistivity variations can be determined based on vertical geologicalformations.