Whether electromagnetic precursors to earthquakes (EQs) exist is an importa
nt question not only for EQ prediction but also for understanding the physi
cal processes of EQ generation. Slow transient geoelectric potential change
s have been observed before several recent EQs in Japan. In most cases, the
y appeared 1-19 days before the EQs, and their duration and intensity were
several minutes to 1 h and 1-2 mV/100 m. The changes appeared before five o
f all six EQs with magnitude greater than or equal to 5 that occurred withi
n 20 km of our stations during the observation period. Changes were also de
tected at greater epicentral distances (up to 75 km) before two other EQs,
including one EQ of magnitude 4.7. which was preceded by a signal simultane
ously recorded at three widely separated stations. These geoelectric potent
ial changes have been distinguished through the following criteria from a m
ultitude of other changes, which were noise of various origins. (i) The sel
ected changes were proportional in amplitude to the length of the recording
station's short (approximate to 100 m) dipoles and were simultaneously det
ected also on long (1-10 km) dipoles when the latter were in operation. (ii
) No such changes occurred during the observation period that were not foll
owed by EQs. Although the EQ precursory nature of these geoelectric potenti
al changes is admittedly unproven, it seems that the present results warran
t continued serious research into the occurrence, generation, and transmiss
ion of these signals and their possible causal relationship to EQs.