Probabilistic seismic hazard analysis has been practically unchallenge
d since its inception three decades ago. However, information has been
accumulating which shows convincingly that PSHA is a defective proced
ure. Its greatest weakness is the dependence of the probability theory
on the Gutenberg-Richter magnitude and a recurrence relation which ca
n no longer be regarded as a power law. Remedies that rely on incorpor
ating paleoseismic information and characteristic earthquakes into the
probability calculation introduce other errors resulting from fragmen
tary data and the known non-uniformity of earthquake occurrence in spa
ce and time. The worst corrective for probability is the method develo
ped by the Electric Power Research Institute and the Lawrence Livermor
e National Laboratory that averages multiple expert opinions. Expert o
pinions cannot be averaged meaningfully because the criteria for diffe
rent models are nonequivalent. On the other hand, the deterministic pr
ocedure for earthquake hazard evaluation avoids the above defects by e
liminating the falsely precise time element in the probabilistic estim
ation. Geologic time for recurrence is used, according to accepted cri
teria such as a single movement in the past 12,000 years or multiple m
ovements in 500,000 years. For a critical project, where the consequen
ces of failure are intolerable and protection is needed against the wo
rst that can be reasonably expected to occur (the maximum credible ear
thquake), the deterministic method is strongly recommended.