STATE GEOLOGIS 



red, calcareous, highly shattered, breaking 

 into cuneiform fragments, with conchoidal Burfao 



changing locally to C 5 ft 



C. Li; highly ferruginous, brecciated iu pla 



ilea of chert. Passes upward into I'.i it. 

 B. Limestone, quite arenaceous, brecciated, shattered, 

 with thin layers which are Band} ib : the' 



whole exterior of some of the bli ■ red with a 



thick, sting of the same material ; up] 



surface undulating, but smoothed as if by aque 



iperior layers were deposited,. . . 2 ft. 

 compact, crystalline, Bilicious, bluish g 

 with some crystals oi dog-tooth spar. E . . 3 ft. 



turn l>. is the parting lay. en the upper and 



rtiona of the formation. The chat 



fly uniform at all the outcrops on th< Bouth and 

 il basin. 

 At the quarry of C. Roberts, S. E. \. ft . | s* 11, Spring 

 tion similar to the pre, 



:ily cala . breaking with 



cunoidal fractui 

 ft Li:: ; crystalline, thick-bedded, 



aing small crystal-lined 



r> ft 



with irr< i 



an I ae 2 ft, 



I, bluish 2 ft. 



This formation outcrsps on i 



the township of Bellevue, Eaton county. From the 



. the following 

 strata was made cut: 



< .. 1. thick-bedded 3 ft. 



P. I. ':..- 31 • ■ . ; ■ l< iw, silici' Q 2 ft. 



ititute oi ,; it. 



It filled with a cesspit hophylloid, 6 in. 



G. L;: ataining . and a 



large coiled shell | not s« i 



B. Lin contain* 

 ing g#< 'des. 



cumty, do actual outcrop of this 



