An age-independent, geometric relationship is presented that links hot
spots to the seamounts which they produce, and so permits the use of u
ndated seamounts to refine the motion of tectonic plates. This techniq
ue has the potential to rigorously assess hotspot fixity and to locate
extinct hotspots. The present application of this method points to a
recent change in Pacific plate motion, and suggests a relocation of th
e Louisville hotspot to the Hollister ridge, south of the Eltanin frac
ture zone.