The vertical electric soundings (VES) technique has been effectively used for several purposes related to investigations of surface soils and shallow sediments. These include detection of subsurface lithology, structures, stratification, and dipping layers; evaluation of physical properties that govern fluid flow and electric-current conduction; delineation of aquifers: assessment of engineering-site properties (such as pore-water saturation and clay content); and mapping various environmental problems (such as saline-water intrusion, groundwater contamination, and leachate transport through porous media). In this study, Schlumherger VES-measurements, along with borehole and experimental data, were employ,ed to image laminations, layering, and lithology, of surface soils and subsurface aeration and saturated zones of glacial sediments; and to model the electric resistivity anti hydraulic conductivity variations with depth and lithology. It is shown that the VES-technique can provide a substantial improvement in the resolution of thin laminations within thick lavers and can also provide a good assessment of the hydraulic conductivity, water flux, and water movement. Numerous references, dealing with a wide range of VES-applications for several purposes, were reviewed and cited in this study.