Ground-penetrating radar is a non-invasive geophysical method employing electromagnetic pulses to image and characterize subsurface structures by analyzing reflected signals. It investigates the dielectric properties and conductivity variations within the ground, detecting features such as buried objects, stratigraphic layers, and anomalies. This technique is significant for its application in diverse fields requiring detailed subsurface information without excavation, including archaeology, civil engineering, environmental studies, and geological surveys.