WEST VIRGINIA GEOLOGICAL SURVEY. 621 



Feet. Inches. 



1. Bakerstown Coal, concealed in fill of 

 electric railroad 



2. Interval, concealed, grade of electric 

 railroad 11 



3. Shale, sandy, greenish, containing lime- 

 stone concretions 7 6 



4. Sandstone, fine-grained, slightly mi- 

 caceous, lenticular, hard, brown 1 6 



5. Shale, greenish, weathers in chips 6 



6. Shale, black, weathers in chips 1 



7. Shale, green and yellow, red stains, con- 

 taining limestone nodules 7 



8. Limestone nodules in shale, like the 

 above (No. 7), but containing Spirorbis 

 pusilhis in abundance, Locality 89 1 



9. Shale, yellow and green, sandy 6 



10. Sandstone, yellowish, fine grained, hard, 



top of cut 4 



11. Interval, concealed in hillside (aneroid 

 barometer measurement) 65 



12. Ames Limestone, marine fossils, Local- 

 ity 90 



The lithology of the Orlando Limestone and of the ma- 

 rine limestones has been described by Reger in a preceding 

 Chapter and is not repeated here. However, two localities, 

 one in the Ames and one in the Kanawha Black Flint, are 

 unusually fine places to collect fossils, and the sections as 

 measured by the writer are here given. Also the section of 

 the Pine Creek Limestone where fossils were collected is 

 described. 



Section, ascending, hand-level, in cut of B. & O. R. R. on 

 north side of Maxwell Run, 0.3 mile from its mouth and 

 0.6 mile northeast of Deanville, Hackers Creek District, 1050' 

 B., Locality 93 : 



