Upper Yerrakalava river basin, a part of the Kolleru-Upptuteru catchment lies between Krishna and Godavari river delta is experiencing fall in groundwater levels in recent years. It was identified that groundwater fall is more in sandstone terrain than in khondalitic terrain. To improve the groundwater levels, a study on multi layer analysis was conducted to identify the recharge sites. This included the rainfall and groundwater level analysis, preparation and integration of spatial maps like drainage, lithology, structures, geomorphology and land use/land cover. The final integrated layer was prepared by using weighted aggregation method and was classified into areas of high to low recharge using standard deviation as classification parameter. Remote sensing and GIS techniques were used in preparation of the thematic maps. Geologically, the area had three major rock types namely sandstones, khondalites and granite gneisses. Geomorphologically, 80% of the area was occupied by pediment deeply weathered and pediment moderately weathered material. Crop land and cropland mixed with plantation covered 59% of the area. Rainfall registered an increasing trend in most of the area. The final integrated layer had the recharge areas of very good (2.07%), good (7.15%), moderate (22.8%), poor (56.53%) and very poor (11.44%). Very good recharge locations were identified where fractures were available with good drainage in sandstone terrain, pediplain deeply weathered and double cropped lands. Very poor recharge locations were identified where no fractures and no drainage, steep slopes in khondalitic terrain occupied with forested lands.