The occurrence of potentially hazardous geologic events such as landslides,
rock falls, earthquakes, floods, and debris flows can be predicted using t
wo fundamentally different approaches: deterministic and probabilistic, The
most significant difference between the two approaches to geologic hazard
assessment is whether a process is envisioned to be the result of an exact
causal relationship or if some element of random behavior is assumed to be
part of the system, Although the assumption of random behavior may seem sel
f-defeating, it can provide a useful tool for the solution of important pro
blems as long as the randomness can be quantified using statistical models,
Each of these two methods can be approached either rationally (using model
s derived from accepted physical or chemical principles) or empirically (by
studying the occurrence of events without explicit regard to their driving
mechanism). The complexity of the geologic process commonly dictates which
approach is used for a particular problem, ranging from rational determini
stic models for relatively simple systems such as small landslides to empir
ical probabilistic models for complicated processes such as floods and eart
hquakes. Examples of each type of model are discussed throughout the paper,
primarily within the context of slope stability and the recurrence of extr
eme events such as floods.