DAL GEOLOGY OF OHIO. 
In the following wood cut A is a section on the north of the road 
feading from Nashville to Loudonville, 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 inch to 72 feet. 
A BI 
Conglom- Ae We 1. 
erate. } 
3% 
Waverly, 
170 feet. 4, 
5 D. 
do 
8, 
9, 
10. 
11. 
12. 
13. 
1. Earth. 
OFA eH ALG C5 X81 6) (Cra er PU I eH a aan See im UV NUR Dita, AUN fe nuk ess Fae 8 ios 36 0 
SSSA abd oe is hang Mel Whe oe he Nat Vee i ae Dh MeL gl es eee Ue ape oe Q 0 
4; NOtGXposed 6 ae a ee Ses eae einai at eete sclepae seein nie mene terevasiots 63 0 
Fe BTS MES CONS see ee ee eB aR ce pe ca tere 4 0 
Oo RCS Oai1 TWO DEMCIIOS es wre ers ea ea Pr ete atten es ein nT esp een 3 6 
4 SNOtIERPOSed i2acs Seow cas co Bee a ia ele te oe ere ere 45 0 
8. Coal. 
Oe NOTES POSE. hee a co We are Re kT Ae ee Te ae eyed atetete 18 0 
10. Coal—iron ore vein. 
PL Black shale cee ee ces ae oN ate ae TR a hh 0 
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 
‘Coal 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 
