8 Clinton with Plectambonites sericea. Plinospira frondosa typical. Orthis (Palmarucella) elegantula. (Strophe). Orthothetes sufflame. - flat but raised at beak. Orthis flabellites Farmites favosus. 21 ft. Ozford clay 8 in. basal ozford, or chert, reddish in mm. siliceous. 2 1/2 ft. Clinton. salmon brown. coarse grained and rough irregular bedded. No chert. Upper 4 inches with whitish stretches. This may be the clerty part southwards. [= N. of Flagde Fork. 29 Cont. from page 1. 30 Cont. from page 3. The basal ozford clay is purplish. All exposed as at Hago Spring. 2 ft. basal Niagara. 3-4 in. of reddish siliceous rock. 21 in. salmon brown, coarse + irregularly bedded. [= 1 mi. N. of Mount Washington) 31 Cont. from page 4. oxford limestone. 20 ft ozford clay. Purple below, indicated above. 44 in. basal ozford Niagara No chert 24 in. Transition red silt with Farmites favosus. 22-48 in. salmon brown typ. Clinton. Halysites Orthothetes with flat valve and raised beak. Orthis flabellites. Plinospira frondosa typ. Doljellum Daytonense, large specimens. Very R rough bedded clinton with sandy patches. 9 32 Cont. from page 6 Lannel S of Asa Lutes brine. 2 ft. clayey 3 1/2 ft. ozford limestone 22 ft ozford clay purple at base. 2 1/2 ft. basal Niagara. light grey clayey rock. 10 in. hard stone. Whitish where not weathered. Traces of chert at top. 15 in. Thin bedded whitish rock. 20 in. granular blue clinton. A few hundred feet N of Asa Lutes brine the Clinton is salmon colored, 20 inches thick, and contains Orthis flabellites.