Measured By M.K. Elias, 1932; NEVA LIMESTONE FORMATION,Limestone--fossiliferous,Mudstone--splittery, softer toward top, crinoid joints,Shale--calcareous, splittery, numerous Triticites ventricosus about one foot from top and numerous Ambocoelia planocovexa 1.5 to 2 feet below top,Limestone,Shale--gray,Limestone,Shale--gray, Spirifer and small Chonetes near the base,Mudstone--splittery, same fossils as above,Limestone--fossiliferous,Shale--gray,Limestone to mudstone--splittery,Shale--gray,Mudstone--light gray, somewhat cavernous and banded, microfossils (ostracodes?) near top,Mudstone--light gray, massive,Shale--gray, to fissile dark gray,Limestone--dark gray, somewhat earthy, Juresania and Myalina,Limestone--dark gray, fossiliferous,Limestone--dark [...]
