Prehistoric large earthquakes produced by slip on the San Andreas fault at Pallett Creek, California.

Abstract

Late Holocene marsh deposits composing a terrace about 55 km northeast of Los Angeles, California,

contain geologic evidence of many large seismic events produced by slip on the San Andreas fault since

the sixth century A .D. I excavated several trenches into the deposits in order to study this evidence. The

principal indicators of past events are (1) sandblows and other effects of liquefaction, (2) the termination

of secondary faults at distinct levels within the stratigraphic section, and (3) sedimentary deposits and

faulted relationships along the main fault. The effects upon the marsh deposits of six of the eight

prehistoric events are comparable to those of the great (Me = 8 1/4 +) 1857event, which is the youngest of

the nine events disturbing the strata and is associated with about 4 1/2 m of right lateral slip nearby. Two

large events may be smaller than this. Radiocarbon dates indicate that the events occurred in the

nineteenth,eighteenth,fifteenth, thirteenth, late twelfth, tenth, ninth, seventh,and sixth centuries A .D.

Recurrence intervals average 160 years but vary from 1/2 century to about 3 centuries. The dates may

indicate a fairly systematic pattern of occurrence of large earthquakes.