one and a fine lime mud. 5+2 ft. Taken, chiefly clay m't hygroz. {3 ft. limestone Pentall Cynthiana, 8½ ft. Missour l. fully hygrozo, 2 ft + % of exposed {with nodules in mass 9 ft {fine grained: Cynthiana 7½ ft Limestone Christ bed perfectly 4 ft Overgravel beds. 49½ft. Paristeed Middle Yore partly on the neck. Eastward the rock rises rapidly so that the Casyville is not seen even at the highest point of the hill North of the road, as far as the pike. There is a peculiar Boulder place as in the Cynthian beds along the Abingdon river, near the creek crossing. 56 - Bridge level 831 USGS Base of Curdsville = 842 ft.1 229. - J.T. Sandidge Barite vein: I had a very little zone at Smith and Runs N+ S with practically Then layer Lexington m. The rock has the zone cm tilted larger in it as east of 76-77 on the way to the creek crossing. This can tilted layer how deeper 4 feet in the west side of of ocins. 900 - 950 USGS 230 SAM and sandstone. 231. Hardscrub. {Cynthiana "Thompson-like 4 ft. {red l. m't Dalan and multiacta clay shale 12 ft Fine grained arg. L. + small more 6½ ft. Limestone + clay shale. {12 ft Limestone, weathering badly. Full of Pelica open up thin hygrozo, Cynthiana type, 7 ft. argillaceous rocks with scattered nodular masses of size of fist, Zygospina Lingula. Dalanville thin and rare. {2 ft. Steph. vicaria Rhapalochitonia, 1½ ft Large stromatolites mm. 2 ft Same grained art. Helurella franklinensis; Did not see certain, Pergrillite bed. The Perryville bed evidently dips for a long distance NW from the cut. 232. Gray Smith and along the RR the Cynthian and Limestones are underlaid by the Cynthiana and slate argillaceo and limestone one. 233. Smith J The road crossing, the stratum with Steph. vicaria is exposed. Overlaid by another layer Cynthiana. ½ John m't rather a coarse till. Large Zygospina near First Dalanville