631 some of same kind of as. No. Chaly. Plt. Pseudana stromm upka and wth Plat. pseudanadae, Apt. rick, lower half scaling 12 ft vertical with Plat. jermcnesa 14ft thick bedded, 5ft fissile fen, more argillaceom with phymacula lufcent. 3 3 ft sinteral, wppr farrunnt 4 1/2 Detraction & Lutechia 7 ft interval River level From the stony lens in the river below 631 the rock appear to rise slightly down stream but ve is practically horizontal. At the head in the river a mile and a half above Beano Creek a sort of sandy rock some 2 less cross bedded, rises slowly down stream. It resembles the rock underlying the top of the Author's included beds at 631. But there are practically no fossils here. A party of this so-called sandstone looks quite massive. Further down stream the sand rock dips down stream and a prodigious ark comes in above. The profile essentially linsignial, further.