GEOLOGY AND PALEONTOLOGY OF THE SCHOHARIE VALLEY 



247 



Transition Feet inches 

 g 2-g 7 Thin bedded lime sandrocks and lime mudrocks, 

 with shaly argillaceous beds, the whole weath- 

 ering back in a slope, with the Coeymans over- 

 hanging 5 





rs-9 





Fig. 195 Section in Becker's quarry 



g 1-g 2 Thin bedded limestones mostly weathering into 

 a sloping bank and merging into the beds be- 

 low and above. Approximately 



Total transition 12 



Manlius 



f 13 Beds similar to g 1 and not readily separable 



from them 6 



''v-^N^ 





Fig-. 196 Lenses of lime mudrock (a) n 

 lime sandrock (Z)). Manlius 



f 12 Lime sandrocks like f 10 in two beds, 2 feet 

 each, with a thin shaly parting 



f 11 Irregularly bedded thin layered lime sandrock 

 with lenses of lime mudrock [fig. 196]. The 

 main mass of lime sandrock compoised of 

 shells and shell fragments 



