31 4) South of Mt Washington, along Whitaker's creek, along Bardest and pike. Salmom brook Clinton. 3 1/2 ft. Hard bedded Madison. 8 ft. { Poor massive Madison above. Sandy clay below owing to weathering 1 1/2 ft full of fossils. 3 in. limestone. 23 1/2 ft Concretinany rubble limestone full of fossils. Calcite! at top = Steph. sulcata + Orthus occidentalis, with scarcely distinct dorsal zinnos. 4 1/2 ft Concretinany rubble limestone, at base with Beatricia undulata + Neterispon- gia at top is Steptolaema rusticum. 12 ft covered, Probably like rock beneath. 41 ft. Massive Madison Limer. Quite massive until near base when it became argillaceous rock. 5 ft. Soft clay rock. 2 ft 8 in. Clayey limestone with Costel- laria perminero? One large Orthus lynx with sub-quadrate form. = The bed at base of Flyods Fork section. 2 ft 6 in. Hard limestone with fossils. 19 1/2 ft. Clay rock limestone full of fossils. One strong Orthus lynx = sub-quadrate form. Hard limestone. Top 4 in. = flat. Below = crossbedded. Beautifully exposed by weathering. Cross bedding due to wave action, forming crescentic sweeps. Waves from the West. Almost 20 ft clay. Shale runs N 40 W. (5) Sweep of Waves from S.W. Photo 5. Clinton. Photo 6,7. Waves 20 ft Waves. a very dark blue sandy layer of lime- stone contains Orthus lynx more ab- brudantly {1/2 ft. More, crossbedded sandy limestone Coarse dark blue limestone with Orthus lynx abundant down to level of creek at Jasper's store, a short distance N. of where the road towards Grinnell's Ford turns off westward. Base of Orthus lynx bed not seen here. 2 ft total Grinnel's Ford to Jasper's store = 4 mi. Saville " " " " = 3/4 " Gar rock " " " " = 2 " Grinnell's Ford to Lick Skillet = S 4 mi. Shepherdsville " " " " = W 3 mi.