Seismic refraction data from oceans and continents have been examined to see whether they are related in any systematic way to geological structures or provinces. A series of broadly defined provinces, related in general to topography, has been established, and the seismic compressional velocities determined by refraction measurements have been plotted as a function of depth. As might be
... [Show full abstract] expected, the narrowest range of seismic properties is found in the ocean basins and beneath the stable, low-lying Precambrian shields, while the greatest variability is found under the young orogenic belts. If one accepts that ancient and more recent orogenic activities are controlled by the same mechanism, then there is an indication that material in the velocity range 7.2–7.7 km/sec may be of a transient nature and may appear and then disappear during the orogenic history of a given region. The data also suggest that oceanic crust might be converted to continental crust, but do not support the reverse process.