REPORT OF THE STATE PALEONTOLOGIST 1902 1227 



Induced in them before the beds were flexed and broken into 

 their present attitudes. 



Finally, all the structural features, with exception of the 

 westward tilting of the White lime quarry overthrust plane 

 which has been otherwise accounted for, can be assigned to the 

 typical Appalachian orogenic movements at the close of the 

 Paleozoic era. 



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1884. The Folded Helderberg Limestones east of the Catskills. Mus. 



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N. Y. State Geol, An. Rep't 1893, p. 291-372. 

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New York. N. Y. State Geol. An. Rep't 1893, p. 393-422. 

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47th An. Rep't, p. 569-600. 

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