8 



KEW TOKK STAT£ MtTSEUM 



daries are rendered very conspicuous by their strong escarpment. Over 

 this lies the Pentamerus (Coeymans*) limestone, characteristically devel- 

 oped, and thereon a well defined mass of Catskill shaly (New Scot- 

 land') limestone. The latter is overlaid by the Becraft' limestone. To 

 these four formations Davis assigned the following thicknesses: 



Manlius limestone 20-30 feet 



Coeymans limestone 40-50 feet 



New Scotland beds 50-60 feet 



Becraft limestone 40-50 feet 



^The requirements of uniformity in stratigraphic nomenclature are compelling 

 the relinquishment of 6uch of the early division names in the New York series as 

 do not indicate localities of exposure. In order to save to the state of New York 

 its preeminent title to the names of these divisions and in the farther hope of per^ 

 petnating an equable grouping of the stratigraphic units of the New York series, the 

 writer, in conjunction with Charles Schuchert, has recently {Science. Dec. 8, 1899, 

 American gedogiM. Feb. 1900) proposed the arrangement of the formations given 

 in the following table. This proposition has been carefully considered and is the 

 result of mature deliberation. 



ITEW YOEK SERIES 



BBA OK STSTXH 



PE&IOD OR GEOUP 



AOK OR STAGE 



Cambric 



or 

 Taconie 



Champlainic* 



(Lower Silurian and 

 Ordovician) 



Georgian 



Acadian 



Potsdamian 



' Canadian** 

 (Paleochamplainic) 



Mohawkian* 

 (Mesochamplainic) 



Cincinnatian'* 

 (Neochamplainic) 



Georgia slates 



Potsdam sandstone and limestone 



f Beekmantown limestone*' 

 I Chazy limestone 



f Lowville limestone** 

 i Black river limestone 

 [ Trenton limestone 



f Utica shale 



< Lorraine beds*' 



[ Richmond beds (Ohio and Indiana) 



