Recent orders
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
magnetism
electricity as well as electromagnetism. The study of abnormalities in these properties forms useful information regarding subsurface materials
using various geology and physics concepts in order to reveal details of the study matter with the accuracy of scientific perspectives. These techniques aim at availing as much information as possible on materials below the surface of the earth using indirect assessments without necessarily performing excavation or drilling to reach on the particular study material (Soupios and Toth 22). Among the most sensitive details unraveled by geophysical investigation techniques include
the properties of earth internal materials at various depths below the surface of the earth. The physical characteristics of materials below the surface of the earth as well as their distribution and quantity form part of the detail that geophysicists devote their time to reveal. Despite the difficulties and challenges that rough terrains and depth related complications faced in such assignments