166 J. J. STEVENSON — CARBONIFEROUS OF APPALACHIAN RASIN 



Feet. Inches 



7. Cedar Grove coal bed 2 5 



8. Shale, sandstone, concealed ... 165 



9. Coal bed 1 8 



10. Sandy shales 12 



11. Peerless coal bed .... 2 



12. Bluish shale 15 



13. Blacksburg coal bed 5 4 



14. Fireclay, shale, sandstone 40 



15. Coal bed and shale 4 4 



16. Shale, sandstone 15 



17. Coal bed 1 2 



18. Concealed and sandy shale , 40 



19. Silicious limestone 1 



20. Shale , . . . . 10 



21. Coal bed 2 6 



22. Sandy shale 20 



23. Eagle coal bed 3 8 



24. Shale, sandstone 20 



25. Little Eagle coal bed 1 6 



26. Shale, sandstone 55 



27. Eagle limestone 1 



28. Fossiliferous shale 5 



29. Sandstone 75 



30. Bituminous shale 2 



31. Shale 30 



32. Silicious limestone 1 



33. Shale, sandstone, and concealed 100 



The interval from the top of the Stockton coal bed, number 2, to the 

 Cedar Grove is 375 feet, but at 3 miles farther down the river it is 421 

 feet, where the Coalburg and Winnifrede coal beds are shown. The in- 

 tervals there are 



Feet 



1. Stockton coal bed 



2. Interval 90 



3. Coalburg coal bed 



4. Interval 100 



5. Winnifrede coal bed 



6. Interval 210 



7. Cedar Grove coal bed 



8. Interval 145 



9. Blacksburg coal bed , 



10. Interval 115 



11. Eagle coal bed 



The Campbells Creek limestone is not exposed at either locality, but 

 there are many exposures of it between them.* 



*I. C White : West Virginia Survey, vol. ii, pp. 371, 372, 529. 



