We explore here the following hypothetical phenomenon: the territorial dist
ribution of low-magnitude seismicity is reversed within several months prio
r to a strong earthquake in the area, surrounding its source; the diameter
of this area is on the order of 100 km. This phenomenon is investigated for
the Lesser Antilles and southern California. On that basis, we suggest a h
ypothetical earthquake prediction algorithm to be tested by advance predict
ion. Retrospective application of the algorithm and the first three years o
f advance prediction in Lesser Antilles give encouraging results. In compar
ison with well-known intermediate-term prediction algorithms M8, CN, and Me
ndocino Scenario, the SR algorithm gives smaller time-space areas of the al
arm. It has a serious disadvantage, however; the catalogue should be comple
te for a longer period of time and for smaller magnitudes, than are require
d in CN and M8. (C) 1999 Elsevier Science B.V. All rights reserved.