
Velocity in a subterranean interval is determined graphically from Root-Mean-Square (RMS) velocities at the end point of intervals by plotting time vs. velocity squared. A straight line can be drawn through the end points and the intersection of that straight line at T.sub.1 + T.sub.2 can be read directly as the velocity of the interval. Alternately, a special template can be used with conventional plotting of time vs. velocity.











