Different soil types have their own distinct impact on the groundwater levels, seasonal water table fluctuations and yield of the open dug wells. The aim of this study was to evaluate the role of different soil types and their possible implications on groundwater regime in unconfined aquifers. This paper is concerned with the static groundwater levels, water table fluctuations and yield of the open dug wells in different types of soils. The results indicate: (A) Clayey soil represents 12.2 to 13.11 mbgl pre-monsoon SWL, 7.02 to 8.54 mbgl post-monsoon SWL, 4.57 to 5.18 meter water table fluctuation and yield of the dug wells between 36 m3/day to 90 m3/day in pre-monsoon respectively; (B) Fine Calcareous soil represent 7.02 to 16.16 mbgl pre-monsoon SWL, 3.66 to 9.6 mbgl post-monsoon SWL, 1.52 to 6.71 meter water table fluctuation and yield of the dug wells between 36 to 72.9 m3/day in pre-monsoon respectively; (C) Loamy soil and clayey soils (mixed) with moderate erosion (mixed) represent 4 to 18.9 mbgl pre-monsoon SWL, 3 to 12.93 mbgl post-monsoon SWL, 3 to 12.5 meter water table fluctuation and yield of the dug wells between 9 to 97.2 m3/day in pre-monsoon respectively; (D) Loamy soil represent 5.79 to 8.54 mbgl pre-monsoon SWL, 2.15 to 4.27 mbgl post-monsoon SWL, 1.52 to 6.39 meter water table fluctuation and yield of the dug wells between 33.75 to 67.5 m3/day in pre-monsoon respectively. Thus out of four types of soil zones, C- soil zone (loamy + clayey soil) represent deeper groundwater levels, probably due to deeply weathered condition. The water table fluctuation (WTF) also indicates similar results where, C-soil zone has greater WTF values as compared to A, B and D soil zones. On the other hand yield of the open dug wells, tapping unconfined aquifers has higher values in B, C and D soil zones, which indicates negligible control of soil zone on yield of the dug wells. This deviation (higher yield values) may be due to other hydrogeological characteristics of the aquifer and not influenced by soil zones.