164: Ulrich — Chattanoogan Series with Special Reference 



nitely correlated with Neodevonian formations in New York 

 while the upper three were correlated in a similarly generalized 

 manner with the Ivinderhookian. That the last of the Chatta- 

 noogan deposits is older than the Louisiana limestone is 

 inferred primarily from the fact that the Sunbury is recognized 

 in the upper part of the Chattanooga shale of central Tennes- 

 see ; and secondarily from the helief that the thin bed of black 







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