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 an isometrically projected, generated hodograph, and means for plotting representations 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.l and X.sub.n of seaid 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.