Groundwater is critical to the socioeconomic development of any region. Infiltration of
surface water into the ground is influenced by a variety of factors such as soil pores, folds, fractures,
faults, and joints, all of which contribute to groundwater recharge. Groundwater is an important
source of freshwater in the drought-prone Pudukkottai district of Tamil Nadu, India. Therefore,
the search for groundwater potential zones (GWPZs) is critical. The present study focuses on the
investigation of potential groundwater zones using geospatial techniques. Geology, land use and
land cover, geomorphology, soil, drainage density, lineament, and groundwater levels were obtained
from state and non-state associations. ArcGIS version 10.8 was used to create all thematic layers and
classified grids. The intensive use of groundwater in arid and semiarid regions is becoming a problem
for the public to meet their freshwater needs. The condition of arid and semi-arid regions due to
intensive groundwater extraction has become one of the most important environmental problems for
the public. In this study, a powerful groundwater potential mapping technique was developed using
integrated remote sensing data from GIS-AHP. Using AHP techniques, thematic layers for geology,
geomorphology, and soil followed by drainage, drainage density and lineament, lineament density,
slope, water level, and lithological parameters were created, classified, weighted, and integrated into
a GIS environment. According to the results of the study, it is estimated that 14% of the groundwater
potential in the study area is good, 49% is moderate and 36% is poor. A groundwater level map
was used to verify the groundwater potential. In addition, the model was validated with a singlelayer
sensitivity analysis, which showed that geology was the most influential layer and water
level was the least influential thematic layer. The low-potential areas identified on the groundwater
potential map can be used for further study to identify ideal locations for artificial recharge. In
low potential areas, the groundwater potential map can be used to find ideal locations for artificial
recharge. The water table in the area must be raised by artificial recharge structures such as infiltration
basins, recharge pits, and agricultural ponds. Artificial recharge structures such as infiltration basins,
recharge pits, and agricultural ponds can be used for groundwater development in the low potential
zones. The GWPZ map was successfully validated with three proxy data, such as the number of
wells, groundwater level, and well density, obtained from well inventory information. The results of
this study will improve our understanding of the geographic analysis of groundwater potential and
help policy makers in this drought-prone area to create more sustainable water supply systems.