In accurately determining shape and elastic parameters of an earth formation to identify ore, marker rocks, economic minerals or the like, using a refraction exploration field system including a series of detectors, positioned along a line of survey at inline positions X.sub.1, X.sub.2, . . . X.sub.n and at least one seismic source located adjacent to said detectors for producing a seismic wave for travel through said formation, means for distinguishing arrival times of refracted shear waves from compressional waves by means of two-dimensional, generated hodographs, and means for plotting a series of said distinguished refracted travel time values versus horizontal offset coordinate annotated by sourcepoint-profile number and refraction arrival direction indicated by sourcepoint offset positions at one of a forward and trailing inline position X.sub.1 and X.sub.n of said detectors, slope of said travel time values versus offset being indicative of apparent P-wave and/or S-wave velocities, said sourcepoint offset positions being alignable along an imaginary line of ascertainable slope.