To me all of these upper measures of E are equivalent to the eastern Clinton. This is seen in the Bryozoa, Ostracoda, Stricklan- dinia, Pentamerus Almyus, Leptocrea hemispherica and the Brachyprion. It is however not the highest Clinton as seen at Niagara Falls and Rochester. The faunas of the two regions are however a common one and had one source, and are quite distinct from the Ohio or called Clinton. Bolt as hard as one will great faunas can not be gathered. The fossils are hard to get because of or much limestone and then the fossil zones are limited to a few feet and then great thickness of lime- stone almost barren or a scattered few fossils of those already seen... Then for when fossils are common they are very oft either the same species. In the upper part for instance Atrypa reticularis and cutular hygra are the common species. In the Stricklandinia beds there is al-