The district Dangs of western India, marks the extension of Western Ghats in Gujarat state. It is characterized by less transmissible basaltic lithology of Deccan Volcanic Province (DVP), rugged trappean highlands and moderate to very steeply sloping surfaces. Despite receiving high average annual rainfall (2000 mm) the terrain framework produces high runoff than infiltration (recharge), leading to groundwater crisis. In such terrains, where lithology is homogenous, the natural groundwater recharge is significantly influenced by geomorphic indicators (landforms, drainage characteristics and slope). Therefore, identification of groundwater recharge potential (here after referred as GWRPOT) is crucial for the sustainable development of groundwater resource. In the present study GWRPOT is identified on the basis of geomorphic indicators (Gi) in sub-watersheds of Khapri, district Dangs of DVP. To generate the database on geomorphic indicators the IRS-LISS-III (24 m) satellite data, Survey of India topographic maps (1:50,000), and SRTM-DEM are used. The ranks are assigned to geomorphic indicators of each sub-watershed by considering their aerial coverage, influence on GWRPOT and field studies. The summation of average ranks of each geomorphic indicator viz., landform (Gc), drainage characteristics (Dc) and slope (Sc) is used to compute Gi value. On the basis of Gi, the GWRPOT is identified and categorized as very poor (SW-5), poor (SW-3, SW-2, SW-10), moderate (SW-7, SW-4), good (SW-11), very good (SW-1, SW-8, SW-9) and excellent (SW-6). These results are validated with seasonal groundwater level fluctuations in 33 dug-wells, which shows positive correlation between Gi and groundwater fluctuation (R2 = 0.77). Further, the sub-watershed prioritization is carried out to highlight the need of improving the GWRPOT and thereby sustainability.