234, From 233 the arch rises into the railroad. At first the whole from Cynthian argillaceous limestone, cm. paralithic few fossils exposed. Then for a very long distance, the upper slightly fossiliferous Cynthian is full of layers and is seen for a long stretch. at the highest bend, at 234, the broad green laminated mixed with clay and lagers is seen, full of pyrgoma in some of the clay lagers. 235. Sandstone, just above RR trestle, 236, Tetradiem, Rhyndotierne, Hebertella frankfortensis. = must not be geodiscus. = Rock taken from Perrysville bed. 237. From rock = ? Oars? 238 Praespora stimulator 239 Placopora stipularis 240 Prasepina + Rhyndotierne, 241 Hebertella frankfortensis 242 Hebertella + Dalmanella. 243. Prasopna 244, Hebertella, Rhyndotierne hayniava Lophospira medialis. Vanmensia Hactivina saleri. 245. Richly fossiliferous zone taken from typical Perrysville bed. Fine grained... 3 same as 236 and 244 3 fine grains Clitomerites Mine family exposed, not studied. belonging to Mr of Perkin road. th clay, No fossils. th clay with pyrgoma. th rock, rock, with Galechia in loose rock. and top, fossils. Flat and medium clay mixed with fossils. fossils and rock, Massive. Shale at several layers, shale. granular fine silt, rock, fossil fro fossilized layers. and fine grained sand in shale bed. internal not measured. fossils along and out. W. along the RR ichnia and shale bed. the road heading from the turned to the fossil localit Galechia horizon is red, also the overlying Rich Clymania are + stratigela our county road in the fields, stream along the road. This section should be studied and measured,