SHULIE TO SFICEH COVE (4). FLETCHER. 515 



The first cliti's include only Nos. 4, 5 and ten ft. of 3. Then a 

 downthrow fault on the south sida brings red rock against the 

 gray sandstone the whole height of the cliff, the displacement 

 being probably sixty feet nearly vertical in a southeasterly direc- 

 tion. Further along, at another downtlirow, a bed, perhaps 3. 

 is seen to be twenty feet thick, while overlying come 2 and 1 

 as given in tlie section. 



Outside on tlie point, a band of sixty feet of fine gray sand- 

 stone is overlaid by red rocks and gray sandstone at another 

 fault. 



Again a thick sandstone, perhaps 5, comes on the shore 

 and is faulted. This is nearly all of fine texture, wdiereav«i 

 further along the shore there are bands of coarser material. It 

 seems possible that for all this distance the same sandstone (5) 

 runs along on the strike, broken by many little faults. 



Then comes a thickness of seventy-five feet of red rocks with 

 conglomerate bands nearly horizontal. Then a heavy gray sand- 

 stone with a band of conglomerate twenty feet thick, greenish 

 and reddish and gray, underlaid by pebbly sandstone. 



Towards Sand River the section is in ascending order, red 

 shale, sandstone of coarser texture wdth more conglomerate being 

 abundant as far as a clean cliff of sandstone, nearly all fine, 

 about 100 feet high. The highest beds at Sand River show thin 

 layers of shale. A descending section is as follows : 



Section IV. 



FROM SAND RIVER EASTWARD, 



In descending order. 



1. Red marl with green layers, broken in the bank, 

 beneath tlie first house behind the Post Oflice at 

 Sand River. Dip S. 19° W.< 20° to 44\ 

 Thickness undefined 5 



Proc. & Trans. X. S. Inst, Sct., Vol. XI. Trans.— HH 



Ft. In 



