Although far-field body waves and surface waves are widely recognized,
the improvements in broadband networks now allow the measurement of '
'near-field'' deformation of large earthquakes at great distances. Nea
r-field motions have been recognized previously only in theory and in
close-in recordings of earthquakes. We show examples from two recent e
vents. For the large deep event on June 9, 1994 in Bolivia, there is a
clear offset after the arrival of the P wave that has the amplitude e
xpected for the near-field term. In the shallow September 2, 1992 Nica
ragua earthquake, the very long-period motion observed between the P a
nd S waves has roughly the amplitude expected from near-field terms. S
uch near-field terms are insensitive to earth structure, but supply in
formation on long-period source processes, and their observation begin
s to close the gap between long-period seismology and geodesy.