The limestone from this locality is extremely hard and contains 

 many fragments of fossils, which are for the most part too poorly 

 preserved to be identified. The list includes the following identifiable 

 forms : 



Crinoid segments and plates 



Fenestella sp. 



Derbya crassa (Meek and Hayden) 



Chonetes choteauensis Mather 



Pustula punctatus (Martin) 



Marginifera muricata var. missouriensis Girty 



Spirifer opimus Hall 



Composita subtilita (Hall) 



The fossils below were collected from the black shale above the 

 hard limestone on Poverty Run: 



Crinoid segments 



Orbiculoidea missouriensis (Shumard) 



Derbya crassa (Meek and Hayden) 



Chonetes choteauensis Mather 



Productus cora d'Orbigny 



Pustula nebraskensis (Owen) 



Maginifera muricata var. missouriensis Girty 



Rhipidomella pecosi (Marcou) 



Spiriferina kentuckyensis (Shumard) 



Ambocoelia planoconvexa Sh.mard var. 



Edmondia sp. 



Leda bellistriata Stevens 



Parallelodon obsoletus Meek? 



Aviculopecten pellucidus Meek and Worthen 



Aviculopecten coxanus Meek and Worthen 



Enchondria neglecta (Geinitz) 



Pleurophorus tropidophorus Meek 



Astartella concentrica (Conrad)? 



Schizostoma catilloides (Conrad) 



Pseudorthoceras knoxense (McChesney) 



In Fall Township on the land of E. G. Marshall, the Lowellville 

 (Poverty Run) limestone outcrops in the bed of a small stream which 

 flows into the Licking River at Holbein from the northeast. Col- 

 lections of fossils were made from the limestone and from a dark 

 shale at an undetermined distance above. The geologic section here 

 shows the following members: 1 



Ft. in. 



Limestone, shaly 



Limestone, hard, blue . 



Shale, calcareous 



Limestone, blue, hard . 



7 

 5 



Lower Mercer } . . 2 



4 



Coal, clay, and covered 10 6 



Sandstone, shaly 5 



Sandstone, massive 10 



Sandstone, shaly, with siliceous shales 11 



Shale, gray 3 



iStout, W., Geol. Surv. Ohio, Fourth Ser., Bull. 21, p. 62, 1918. 



25 



