Then 8 of my thin bedded shale on each side with the centre zone dense li, that has been found into a usual clay. This is my 5-p. The balance of my 3 sections follows which are did not examine. Three John Hopkins students are doing this Messrs Hopkins, Price and Croll. My 5a Points of 95' is one of the nodular characters and mostly with the Merlins. The bed grain in Chald Jorae rectilimata is either in the top of the bed or just above it. The coral also occurs so far down just past the corroid strip down to the Michesta grain, Stomatofore common and the Chald Jorae. If the bed until the griters abundance is not added then my 5a is 90 feet thick. The 95 feet only takes in the bed with the coral. The contact between the basal Manlius (95' bed) and the upper small Tolonaway here has the same character as in the Keays quadris, Belns are the then regular bedded Tolonaway beds and above at once the Hurst cathy beds with mine fossils. Along the Drinolates grade beyond the stone cave at the top of the brown clay pit are seen the Skirper ranges and beds with the large Ruderspira Rensselaria Swantzi