Quadrille Ruled Form. John C Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 Aug 5, 1908 5 250 brook 400 brook 5.51.5 Eld. 51.5 13' <- 200 yds. horizontal: 1" = 20 ft vertical 1" = 10 ft The point in S.W. 5.51.5 is composed of a thick galbee mass trending N 55°E and mills on the opposite point N.E. of the latter Run Burnet Creeks West of this is a series of sediments which may be traced for a distance of 305 ft. normal to the strike, until near the brook occur some light gray amygdoloidal diabases; the adyaz dip. 62° (35°-40°) 37° giving a thickness of over 160 ft for the shales exposed. These are massive bedded, striking N. 52° 10° W. dip East. 190 feet east of the top of the trap flow occur some 6 feet of highly fossiliferous sediments which are exposed at K below high Lodi Foreels very abundant? includs Plectambonites (Caye) common Leptrena rhomboidalis " Strophomena sp. occasional Strophellla g profunda " Leptostrphia sp rare Chonetes cornutus occasional Dalmanella (varae) common 5.51.5 A 28 26 24 22 20 18 16 14 12 10 8 6 4 2