GEOLOGY AND PALEONTOLOGY OP THE SCHOHARIE VALLEY 315 



Fig-. 206 Section at the north end of the fifth Binne water, Ulster co. (After Darton) 

 HR=Hudson river shales, S=Shawangunk, Cl=High Falls shale and Binnewater sand- 

 stone, C— cement beds (tiosendale and Rondout, with Cobleskill between), P— Manlius 

 and Coeymans, LS=New Scotland beds, US=Becraft and Port Ewen, CG=Oriskany and 

 Esopus 



Fig. 207 Section of the cement district 1 mile south of Whiteport station, Ulster co. 

 (After Darton) H— Hudson river shales, S=Shawangunk, M=High Falls shale, C=Bin- 

 ne water sandstone, LC=R,osendale cement,— Cobleskill, UC=Rondout cement, T= 

 Manlius, P=Coeymans, LS=New Scotland 



Fig. 208 Section of North hill, Kingston, showing strata as originally folded, positio: 

 of thrust plane (upper) an<* present character after thrust and erosion (lower*. 



n 



