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Geotherms in the boundary layer undulate over the width of the convection cell in Figure 1. The ?20 km of scalloped relief for the T_? = 40 K model is potentially detectable by seismic methods. Other effects may indirectly be detectable. The flow pattern may produce mineral fabric. The time variation of temperature along a flow path of a rock is potentially detectable by xenolith studies. I obtain scaling relationships for relief, with forethought beginning with penetration of an upwardswelling into the lithosphere.