well records. In Scioto County, however, the member is locally 

 well developed. The following section measured on the land of 

 William Tripp, Section 14, Bloom Township, shows its relation to 

 the Sciotoville clay below and to the Bear Run coal above. 1 



Ft. In 



Coal blossom, Bear Run 6 



Clay shales, dark 3 6 



Shales, gray, and parts covered 28 



Sandstones, flaggy and medium bedded 13 



Coal outcrop, Quakertown, seen to the south 1 8 



Shales and covered 33 



Sandstones 7 



Coal, Anthony 2 



Clay, flint, dark, Sciotoville 6 



Jackson County. With the exception of Summit County, this 

 is the only county from which fossils were obtained, all of them being 

 from Coal Township. Specimens are very rare, and all belong to 

 the fresh or brackish water pelecypod, Naiadites elongata Dawson. 

 Collections were made from the Wilson rr.ine, northeastern part of 

 Section 32; from the Twin-Ada rr.ine, central part of Section 35; and 

 from the Grace mine, just east of Davisville in the northeastern rart 

 of Section 10. The following section was measured in the nine and 

 in the hollow east of the latter place: 2 



Limestone 1 Lower 



Shale, dark \ Mercer 



Limestone. . 



Ft. In. 



11 



1 10 



1 



Covered 9 



Coal, cannel, Lower Mercer 



Covered 1 6 



Top of shaft 



Covered ' 97 



Coal, Quakertown 3 



Summit County. No other fossils were found on the Quaker- 

 town coal horizon except in the extreme eastern part of Summit 

 County where Lingula carbonaria Shumard is present in great abun- 

 dance in the fossiliferous shales associated with a thin coal bed at 

 Mogadore Station, five miles east of Akron. 



Summary 

 The fossils collected from the Quakertown or No. 2 coal horizon 



are: 



Lingula carbonaria Shumard 

 Naiadites elongata Dawson 



iStout, W., Geol. Surv, Ohio, Fourth Ser., Bull. 20, p. 551, 1916. 

 2 idem, p. 146. 



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