SHULIE TO SPICER COVE (6). — FLETCHER. 523 



The direction of the line of fault is iST. 53° W., with do^\Ti- 

 throw to the southwest ward. At the last reefs, 225 yards west 

 of the mouth of Sand Brook, the dip is S. 61° E. <15° to 22° 

 near the landwash and X. 77° E. <10° farther seaward. 



Ignoring faults, the strata ^vest of Sand River appear to 

 overlie those on the east side and may represent some of those 

 between Sand Cove and Shulie. And unless there is a fault, the 

 uppermost teds of the Pudsey Point section must be near, or 

 repeat the lowest strata of Hetty Point. It may ther-eiore be 

 possible from the measurements to srhtw the entire section from 

 Shulie to Spicer Cove. 



On the west side of Sand River the first rocks exposed dip 

 iST. 80^^-83° E.< 21°, and their section is as follows: 



Section VI. 



WEST OF SAND EIVER^ 



In descending order. 



Ft. In. 



1. Gray fine sandstone with layers of dark-gray argil- 



laceous shale; coal-pipes. Dip jST. 82° E. <21°. 

 At water-levx'l 250 yards southwest of the end of 

 the road to the beach 10 



2. Gray, coarse, pebbly gi'it with layers of gray sand- 



stone, full of carbonized plants 11 



3. Red and green mottled argillaceous shales 10 



4. Light gray fine sandstone 7 



5. Dark bluish-gray argillaceous shale, lenticular 



6. Light-gray and greenish-gray fine sandstone, in thick 



irregularly jointed beds, with a few pebbly patches 

 of grit, coarser at the bottom; for the most part 

 very ma-sive 49 



7. Greenish argillaceous shde. Dip S. 15° E. <9° . . . 9 



A fault, the direction of which is S. 5° W. and 

 the dip apparently S. 85° E.<85°, seems to pro- 



