compressional wave velocities possessed by particular subsurface study matter forms the information basis for determination of the effective features of the material under study. The geophysics principle employed in seismic surveys is the ability to capture and characterize acoustic echoes emanating from stratified subsurface material to account for the different wave features and determine the nature of material and conditions below the surface of the earth (Castañeda and Brunkal 3). Compressional wave velocity measurements under seismic surveys imply that the wave strength and its penetration to the underlying material can only give depth dependent accuracy. According to the geotechnical problem considered by the study

the depth level that the material lays can determine the kind of seismic study to engage. Apparently