followed by a solid li some about 15 foot thick, until the upper 7 foot more weathering into shale. Then a Stromato- poroid bed about 3 foot thick followed by nodules the bedded hard li for about 20 feet. Then another long bedded disseminated blue li for 20 going helus into decidedly nodular li for about 60 foot thick hany T. gysracanthus, Homocospira organum and Chneles jersugensis in great abundance. The section is the broken by a loose ocilley papers, Chneles jersugensis zone is several foot thick and occurs about 15 foot above the base. See Whick's detailed section. West on B s O R P of the Loros Leap may be seen contact between the Manlius City limestone and the Uppermost Puerto series (Valeria). The beds are slightly discordant. CPIHly thin bedded li with C. gersugani by the great abundance Corniced li with C. geracuni 2 foot disconance Kirk has taken pictures of the contact. This discordance while distinct after probably has no marked time value. It certainly means that at this time the Manlius - Coeymans sea was deeper over that of the