Though among the most famous earthquakes in modern times, San Francisc
o (18 April 1906) has almost always been presented as nothing more tha
n a great human disaster. While certainly that, we should regard it al
so as having had unusual significance in the development of seismology
. Because the full extent of the San Andreas fault was thereafter reco
gnized, and the association between faulting and earthquakes confirmed
, we may consider the San Francisco earthquake of 1906 to be the first
in which modern understanding of seismic causality prevailed.