SHULIE TO SPICER COVE (9) — FLETCHEK. 535 



Ft. In 



31. Red argillaceous shale with bands of reddish 



arenaceous shale ; layers of greenish or whitish- 

 gray calcareous, fine sandstone and of bluish-gray 

 shale -in a deep little cove 50 



32. Greenish and rusty-gray fine grained arenaceous 



shale and sandstone, with carbonized plants ; cut 

 into long blocks by irregular joints; some pebbly 

 patches occur towards the bottom, but the fine beds 

 greatly predominate. Changes in the lower part 

 into Indian-red sandstone like that of Birch Cove 68 



33. Red argillaceous shale with greenish thin bands. . , 15 



34. Indian or brick-red fine sandstone with pebbly 



patches containing laj^ers of arenaceous shale, pre- 

 cisely like the grefenish and gray varieties except 

 in color; shows the usual whitish and greenish 

 blotches of the red rocks. At the lighthouse on 

 Hetty Point, the red layers are underlaid by gray 

 or brown, and these latter replace certain beds 

 on the strike 58 



35. Greenish-gray and rusty fine sandstone with very 



few pelDbles, generally in thick beds, some patches 

 very rusty; in part conoertionary, with "bulls- 

 eyes" ; many of the beds have wavy lines. Certain 

 layers at the bottom turn into red. Almost the 

 whole thickness may l^e said to lie below high water 

 on Hetty Point and to extend to the lowest point 

 seen on the reefs 1-10 



Total thickness - 1038 9 



The beds now ri-e on the right bank of Apple River. They 

 appear to be but very little higher than the strata of the follow- 

 ing section at- Pudsey Point on the opposite side of the river, or 

 may represent a portion of the latter. 



