I907.] CRANDALL— SAN FRANCISCO PENINSULA. 55 



the same time. The cracks in the hills southwest of the Chinese 

 cemetery are almost in a direct line with the fault and may indicate 

 a slight movement. The fact that these cracks are not continuous, 

 so that they may be easily traced through Wood's Gulch to the 

 ocean, leads to the belief that they are merely due to the settling 

 or to the beginning of large landslides on the hill tops. 



Movements of the adjoining Blocks. — The southwest side of 

 the main fault line seems to be almost entirely free from cracks and 

 fissures, though there are many and large landslides. The general 

 evidence is that the intensity on this southwest side of the fissure 

 zone was about the same as it was on the northeast side. 



