Field Notebook: New York, Pennsylvania, Ohio, Ontario 1913
Page 35
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Transcription
"The Clinton appears the here with the same and th[illegible] character as at Hamilton. Belms are the thin bedded about 8 feet, this is limestones terminated above by the heavy bed of at the Falls. limestone which here is about 6 feet thick. Contact Belms with the Oredina was not made out. Did not see any Hyattella conjuncta said to occur here (did not look hard for them). The Archeatur is here easily mistaken for the Lockport, Billings made out thicker than at Hamilton. 6 to 7 feet. Suppose there is true but half the. The Lockport here again has a basal conglomerate as at Hamilton but the opposite and sandstone was not made out. Cataract. At base in the Whilford sandstone as at Hamilton followed by the same thin bedded limestone series. Between 10 and 20 feet above the sandstone occur the free A. Hancrocorae. This is the type locality for the species.