On coming down the Mt. and near the station (Cuyahoga Springs) the grad beneath a house, crosses (a part of Brown Ridge) the apex of a low arch dipping under to the Ch-E. At the apex are shown for fifty feet of heavy bedded Massanutten sandstone followed by a few feet of thin beds and then some heavy beds. A short distance towards the station and still in the same formation, from some Leperditia which may be the Orictina L. cae- corona (These seem to be lower than the Clinton of Buffuto Shelf section). Just a little to the Ch-E of the station along the railroad there is a cut which first appears to be in the Richwoods (our air fossils here) then after an interruption come in heavy beds of crippled sandstone and lime, but gone above I solid limestone filled with crinoid stems and segments. Some of these are 3 feet in diameter and one of Ostracions. Saw also Rhyn- choceras transversum, P. onutilus, but nothing else though the rock is rounded and crinoidal (one this appears to be this Cragans design for both the System's matter.) Before these beds is a silicious