5 ft interval, uncertain, Typical dove crinid lme 2 tme The preceding section is very firm or some agreement the limits of the extremes being uncertain. But it is certain that the strata formers regarded as not Amherst in reality are Archelm with [illegible] Moe over the Devonian An limestone comes in within 5 ft of the tip of the section as here described, if not directly at top. The large fragman crusted Amherst in former trips, comes in in the 11 yard limestone section at top of the Craigville, Lebanon, Ky 154 Near Sulphum Well, Lebanon. Tetradium 9m belw Devonian l. Columnaria racca 1-2 ft below D. l. Col. racca, 3, 2-2 ft below Devonian. Columnaria rather common between 1 and 2-2 ft below Dev. l. 6 in my ink with radial Beatrix common, like a carrot with frad end down. 159 Dan they hill S of Sulphum Well, Nodule layers. 9 ft from top = Amherst. Rhy. dent at a + Lejet also lme, 7 feet lower. This shows that from Magnenville Nichle was Amherst. here at least 159 most likely globular plat, but not fender. 2 ft width front, clay rich with 6 in mfrml forms, clay soft, soft. 32 in. Plat. fenderma. 24 in. rich modl + plat. fenderma. 30 inches fransiform l. Lejetman's place. 7ft. 2 ft strong, rich. Regular dove crinid l. Shake layer of Magnenville, 4 ft my ink. 1 ft Nodule layers and undulating front arch. Maynovale, 2 ft width from l. limestone this R> All preceding and 5-6 y Lebanon three major settlement. 333 Serge Luckett, about 2 mile of Lebanon - Bradfodville junc. Plat. fenderma abundant, as far as next water. 334. Base of Date layers, Devon l. 160. 49 ft Shelly from Magnenville. nodule in relation to the soft clay 16-2 ft internal, Lejetalma loose, just above argillaceous ark, softer, which whiles typical dove crinid l. The Devonian is first about the 49 ft of from Magnenville.