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temperature and density that are a consequence of convection Also, by mapping seismic anisotropy both vertically and laterally it is possible to obtain estimates of the direction of mantle ow The rst three-dimensional seismic velocity models for the mantle derived by the tomographic technique were published in the early 1980s (Woodhouse & Dziewonski, 1984) Since then there have been great improvements in data quality, geographic coverage, and processing techniques, and the resolution of subsequent models has greatly improved However, many of the essential features of the velocity variations were apparent in the earliest models Plate 121 (between pp 244 and 245) shows the variations in the shear wave velocity at 12 depths in the mantle according to model S16B30 of Masters et al (1996).

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It is immediately apparent that the greatest variations occur near the top and bottom of the mantle, presumably within or in the vicinity of the thermal boundary layers Within the top 200 km the perturbations are very closely related to surface tectonic features Ocean ridges, the rifts of northeast Africa, and the active backarc basins of the western Paci c are all underlain by anomalously low velocity mantle Continental areas in general, and shield areas in particular, are underlain by the highest velocities, and older oceanic crust by relatively high velocities These variations essentially re ect the different thermal gradients and hence the thickness of the lithosphere in these areas (Section 1131) Between 200 and 400 km most of these generalizations still apply but the velocity contrasts are lower.

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A notable exception is the mantle beneath the backarc basins where the slow velocities at shallower depths have been replaced by near zero anomalies In the transition zone (eg 530 km) the variations are in general quite small and the correlation with surface features has largely broken down Again an exception is the mantle beneath the backarc basins of the western Paci c, which, at this depth, is characterized by high velocities presumably associated with cold subducted lithosphere In the lower mantle (depths greater than 660 km) the variations in shear wave velocity are generally quite small (less than 15%), but a persistent feature is a ring of higher than average velocities beneath the rim of the Paci c This becomes particularly marked in the lowest 400 km of the mantle (eg depths of 2500 and 2750 km).