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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Dale, T. N. 1879. The Fault at Rondout. Am. Jour. Sci. Ser. 3, 18: 293-95 

 Davis, W. M. 1882. The Little Mountains east of the Catskills. Appalachia, 

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305-6. 



Darton, N. H. 1894. Preliminary Report on the Geology of Ulster County, 



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

 1894. Report on the Relations of the Helderberg Limestones in Eastern 



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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Geol. 15th An. Rep't, 1 : 393^475, pi. 1-42. 

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N. Y. N. Y. State Mus. Mem. 3, p. 1-128, pi. 1-9. 

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