SHULIE TO SPICER COVE (0). FLETCHER. 531 



Ft. In. 



2. Greenish-gray, dark-bluish-gray and reddish argilla- 



ceous shale, the dark portions full of fossil plants 12 6 



3. Gray and ru5ty fine sandstone, full of broken plants 



and having a one-inch lenticular layer of coal, 

 sometimes in the bed- ling, sometimes in the joints 9 



4. Greenish and bluish-gTay pea-and-nut conglomerate 11 



5. Gray and cream-colored pebbly sandstone, fin sand- 



stone and conglomerate, a large proportion of 

 which is conglomerate. It passes on the strike into 

 Indian-red conglomerate, resembling that of Polly 

 Brook and the Morang River, and soon it all 

 turns to Indian-red. Many of the pebbles are as 

 large as a cocoanut. Where coal-pipes are seen 

 the rock is rusty and gray. Dip S. 21° E.< 15° . . 90 



6. Gray fine flaggy sandstone with a nine-inch len- 



ticuLir layer of greenish-gTay argillace ms shale. . 6 6 



7. Ked argillaceous shale or marl. These beds are all 



lenticular and thin out 5 



8. Mottled red and green argillaceous shale 2 



9. Greenish and gray coarse grit and nut-and-egg con- 



glomerate 45 



10. Red argillaceous shale with greenish layers, cut out 



to form a fine cave behind a bluff 2 6 



11. Red, rubbly, more coherent flag 11 



12. Reddish sandstone with greenish blotches 10 



13. Gray and greenish, fine, massive sandstone with 



broken plants 4 10 



14. Gray and rusty fine sandstone, the upper surface of 



W'hich is spottel with prostrate plants 3 



15. Rusty-gray pea-and-nut conglomerate with layers of 



sandstone, th3 latter being blackened with carbon- 

 ized plants. Veins of coal lie at various angles to 

 the bedding, seldom exceeding half an inch in 

 thickness. The gray sandstone is in very irregular 



Proc. & Traxs. N. S. Inst, Scj., Vol. XI. Trans.— II 



