544 



GEOLOGY OF OHIO. 



In the following wood cat A is a section on the north of the road 

 leading from Nashville to Loadonville, from the conglomerate to the 

 bottom of the Lozier quarry. B is a section in the first ravine south of 

 the road and nearly due west of Nashville : 



Vertical scale, 1 iucli to 72 feet. 

 A BJ 



Conglom- 

 erate. 



Waverly, 

 170 feet. 



10. 



11. 



12. 



FT. IK. 



1. Earth. 



2. Sand-rock 36 



3. Coal 2 



4. Not exposed 63 



5. Blue limestone 4 ' 



6. Coal — two benches 3 6 



7. Not exposed 45 



8. Coal. 



9. Notexposed 18 



10. Coal — iron ore vein. 



11. Black shale 27 



12. Coal No. 1. 



13. Waverly. 



We have here a Waverly hill capped with the conglomerate, and rising 

 at least one hundred and ninety-eight feet above the Old Swamp, in which 

 €oal No. 1 was deposited, and certainly five coal seams, and their includ- 

 ing rocks, below this conglomerate. 



The dotted lines in the section indicate the probable junction of the 

 coal beds with the old Waverly hill, and illustrate facts observed in other 



