250 xi:\v ^(>KK siwi-i: museum 



Feet Inches 



S 1 1" o \) li o () (1 11 1 a V a r i s t r i a t a , also 

 S t V () ]» li () 11 (' 1 I a |) u 11 (• I u 1 i f 1' a, I? t o r- 

 i li (' a 1 (' x I i 1 i s and occasioiiallv T ii - 

 c i 11 11 1 11 s 111 11 t a 1) i 1 i s and Teutaeiilites. 

 The limestone lenses contain C a in a r o t o e - 

 (• li i a s (' 111 i |» 1 i (• a 1 a vdv 10 



g4 Fine lime sandrock with numerous criuoid joints 



wliich weather in relief 10 



g 3 Shale with mud lenses, the latter with C a m a - 



r t o e (• li i a s e in i ]) 1 i c a t a var 6 



<i' 2 Lime sandi-ocks and lime miidrocks, alternatin<>\ 

 thin bedded, mostly dark gray in color. Fos- 

 sils most common are O a m a r o t o e c h i a 

 semiplicata var., in the mudrocks and 

 crinoid joints in the sandrocks. Other species 

 are S t r o p h e o d o n t a v a r i s t r i a t a , 

 S p i r i f e r v a n u x e m i and var. a m a - 

 rotoechia ventricosa, Fenes- 

 t e 1 1 a sp., D a 1 m a n i t e s sp. To base of 

 quarry 5 6 



g 1 Thin bedded gray lime mudrocks, somewhat are- 

 naceous in the upper part, with occasional 

 crinoid joints and with S t r o p h e o d o n t a 

 V a r i s t r i a t a and occasional S p i r i f e r 

 vanuxemi 4 8 



Total transition beds 13 2 



Manlius 



f 13 Lime nnidrock with S p i r i f e r v a n u x e m i 



in abundance (ui)per part of bed) 8 



f 13 Lower part, to f 5. Mostly coveiTd, exposures 



are found at intervals 20 



f 4 (approximately). Ledges of a dark lime niud- 

 ]•()( k ai-c (|uarried in the field half way between 

 N'loiiian's and llie Syndicate quarries. The 

 r<K'k has a ringing sound when struck wiH^ o 



