EXPLANATION OF PLATE XXXIV. 
Fault in Triassic sandstone produced by up-thrust of granite. Exposure of 
granite is seen in the middle ground at the right. On the left the Triassic strata 
are seen highly tilted and resting upon the granite. In the foreground and at the 
crest of the bluff these strata show only a slight dip in the direction of the 
monocline. 
