9 Quadrille Ruled Form. John C Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 In northern 1.35.2 there begins back of the house a gray glyphy tuff (rhyolite) which bends E. Eastward across the trail & after crossing the railroad tracks bends abruptly to the east for a hundred yards and reappears forming the little 80 ft. knoll S.W. of the RR. Station this Rhyolite tuff glyphy in depths, 50 ft. broad on outcrop, and where it bends to the east -- underlaid by some nor 15- ft. of gray shale striking N. 8 8 W. & dipping north at an angle of 150. sl 1352 A These gray shales (silty) contain an occasional Grammopora lamelli Branch. There as near the Garnet Point (not shale species N. 77 Lbsc. collected these gray shales are correlated within as gray band in the Pembroke gmple or else as the top of the Garnet Point member. 1.35.2 A In the upper 80' where RR crosses Wilson Stream occurs a white firm ft of fine grained light gray dense sediment striking N. 50 W dipping 70 N.E. The rock resembles the Wilson Stream formation led of Schuyerville, but largely over 1.30.4 A