3^4 



STEPHEN TABER 



tain, and with the effects of the earthquake on the district lying on 

 both sides of the fauU-Hne and extending from San Francisco Bay 

 to the Pacific Ocean. 



Map of file Stevens Cree 

 Scale of Mi/e5 



Fig I. 



The Stevens Creek fault is one of the most recent, for it cuts 

 gravel beds that were laid down as late as the Pliocene or perhaps 

 Pleistocene period. The old uplift along the Stevens Creek fault 

 is on the northeast side, and the rocks on both sides of the fault dip 



