GEOLOGY AND PALEONTOLOGY OP THE SCHOHARIE VALLEY 



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Fig-. 208 Section at the north end of the fifth Binnewater, Ulster co. (After Darton) 

 HR=Hudson river shales, S=Shawangunk:, Cl^Hig-h Falls shale and Binnewater sand- 

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

 and Coeymans, LS=N^ew Scotland beds, US=Becraft and Port Ewen, CGr=Oriskany and 

 Esopus 



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

 (After Darton) H=Hudson river shales, S=:Shawang-unk, M=Hig'h Falls shale, C=Bin- 

 newater sandstone, LC=Rosendale cement,— Cobleskill, UC=Rondout cement, T= 

 Manlius, P=Coeymans, LS=New Scotland 



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

 of thrust plane (upper) and present chai'acter after thrust and erosion (lower). 



