one mile along here a fault with Romney on one side and Martinsburg on the other. Nothing of the latter is to be seen here any the road all is Hamilton, then higher up the road much comes in Moscoanuttles the Ortany are again and about 1/2 mile farther E. beyond a spray crossing the road the Char- terbury. Just quite in the highest beds I saw Trinucleus concentricus, Syng- -pire modesta, Plectambonites sericeus, Rafines- quina alternata (small sp.), Dalmanella testu dinaria. This seems to indicate Utica – & a – These fossils occur Ostreophengula living below these productive beds the Martinsburg beds are sandy shale. Solid not go down to the mountain base on the E side. In the Hamilton near Astrocrada, Stylosina fisurella?apidruptus carinatus, Michelinia (by cells about 4 across & smaller) one outside.) Phacops and a Dalmanites with a denticulate head shield. Further of