GEOLOGY AND PALEONTOLOGY OF THE SCHOHARIE VALLEY 249 



6 Section of syndicate quarry in the hillside behind Vroman's quarry 



Figure 197 and plate 20 

 Soil 



Coeymans Feet Inchea 



h 1 B Dark tough lime sandrock showing where wea- 

 thered innumerable Sieberella gale- 

 a t u s . These sometimes cover the weathered 

 surfaces or edges, but are difficult to separate. 

 Large fragmentary masses of Favosites 

 helderbergiae are common and not in- 

 frequently lie overturned 15 



Fig-. 197 Section of Syndicate quarry 



h 1 A Lime sandrock with large heads of Fa v o s i t e s 

 helderbergiae and Stromatopora appa- 

 rently in place 1 



Transition beds 

 g 7 Limestone bed largely made up of S t r o p h e o - 



d n t a V a r i s t r i a t a 



g 6 Crinoidal lime sandrock 



g 5 Dark gray lime mudrocks in lenslike masses em- 

 bedded in shale and separated by shaly layer 

 from g 6. The shales contain an abundance of 



