Satellite altimetry was used to identify and characterize Pacific intr
aplate seamounts. The gravimetric amplitudes of seamounts appear to be
related to the age difference between the sea floor and seamounts; by
inverting this relation, pseudo ages can be obtained for undated seam
ounts, These pseudo ages imply that excursions in seamount volcanism g
enerally correlate with times of formation of large oceanic plateaus.