SHULIE TO SPICER COVE (6). — FLETCBEE. 525 



Ft. In. 



a mile further west. On the strike there are of 

 courste many changes. The upper part is in places 

 fine arenaceous shale and at the mouth of this 

 second brook patches of conglomerate contain 

 pebbles of gray, fine, micaceous sandstone and 

 shale almost certainly newier than Devonian. The 

 bedding is very irregular and also the lenticular 

 layers of conglomerate and greenish shale 77 



16. Red argiUaceous shale with greenish blotches 9 



17. Greenish and reddish mottled argillaceous and 



arenaceous rock 5 



IS. Gray sandstone like Xo. 15, the upper part beinii' in 

 places fine wavy arenaceous shale. Xearly all the 

 pebbles of the conglomerate are of Pre-Carbonifer- 

 ous rocks, the layers varying from six feet to two 

 inches in thickness 55 



19. Dark bluish-gray argillaceous shale, with bands of 



dark-reddish shale and lenticular layers of green- 

 ish very fine sandstone and shale ; an upright 

 Calamite with the bark converted into coal. The 

 overlvine; sandstoues are verv rustv and full of 

 broken carbonized plants 10 6 



20. Gray and rusty fine massive sandstone, jointed at 



right angles to the bedding; pebl)ly |)atches and 

 lenticular layers of dark shale 23 



21. Rusty nut-and-egg conglomerate with pebbles uu to 



three inches in diameter. Thicker in places, the 

 sandstone cutting it out 1 6 



22. Red argillaceous shale with bands of light gray and 



greenish very fine, coherent sandstone 25 



23. Light gTay very fine sandstone, with thin layers of 



red and gray argillaceous shale 15 



24. Red argillaceous shale interbedded with reddish fine 



sandstone 13 



