Sine-beat phenomena have been found in the 1994 Northridge earthquake recor
ds, and they are capable of producing time-history responses and damaging q
uasiresonance effects in structures. Linear, single DOF (degree of freedom)
oscillators, in lieu of nonlinear, multiple DOF systems, have been found a
dequate to discuss the failures of tall circuit breakers during the 1971 Sa
n Fernando and the 1989 Loma Prieta quakes in California. The use of sine-b
eat excitation for seismic-shaking-table tests of equipment continues to be
a conservative simulation of earthquakes.