SHULIE TO SPICER COVE (8). — FLETCHER, 529 



Ft- In. 



3. Gray sandstone, tine on top bnt becoming- pcbblv 



below. 38 feet of tkis sandstone comes to water- 

 level at the next little brook. With so mncli sand- 

 stone the measurement of some parts of the section 

 is incorrect no doubt, but the bedding is usually 

 plain 50 



4. Ecd argillaceous shale with bluish and greenish 



layers ; replaced by gray coarse pebbly sandstone. 5 



5. Gray pebbly sandstoiie. In places the layers of shale 



are thicker and contain bands of gTay fine sand- 

 stone 7 



6. Greenish and reddish argillaceous rubbly rock ; also 



replaced by gray sandstone 4 



7. Rusty-gray or cream-colored fine sandstone, passing 



into coarse sandstone and intermixed with pebbly 

 layers. In places it turns nearly all into nut-and- 

 e^g conglomerate. Lenticular layers sometimes 

 six inches thick and ten feet long, show alternate 

 bands of impure coal and pyrite. At ninety feet 

 there is a landing place. Here the rocks are 

 largely conglomerate and in certain bands this 

 assumes a reddish tint as well as in patches of the 

 finer sandstone. Some of the pebbles are of brick- 

 red sandstone, others, of greenish-gray and gray 

 micaceous sandstone, like Carboniferous. The 

 low^er part is very rusty and full of veins and 

 blotches of coal 95 



8. Greenish-rubbly argillaceous shale with red patches 



and layers 4 



9. Gray-flaggy argillaceous sandstone with a lump of 



coal near the top 5 



10. Greenish-gray and cream-colored alternations of fine 

 sandstone, pebbly sandstone, and pea-and-nut con- 

 glomerate with larger pebbles ; coal streaks and 

 pipes 22 



