14. 39 A. E of William McBurdor's house, at End of glen or valley, entering boun- dary creek. 2\/2 mi. from Carson Springs Sta. Clinton. ->9 ft below Clinton is highest Spange. 18ft sandy decayed Madison. Mst Spanges are found now at the top of the fossiliferous expo- sure. If the base of the banded Madison is 15 feet below the Clinton, thetopofthebandedMadisionis probably still beneath the spange layer. The thickness of the richly fossilif- ous Richmond section was not measured. It equals about 5 feet as near as I can remember. One stray Columnaria was found, pre- sumably C. abecata but no record was made. Further along the track Columnaria halli occurs 17 feet below top of richly fossil. Richmond section. 9feetCornith on theC.halli layer where C. halli occurs in association with Tetradinium minimus, Platano 23 B Samuels. 9ft{1/2clayinsoil. 71/2 ft. massive with Calcites of Clinton. 5ft weathering to clay. 1/2 ft. thin limestone. 4 ft Madison like rock. 40 At bridge 5, E. of Hobbs. 1mi. N. of Carson Spgs. E.ofbridge. Black Shale coarsely crinoid Corniferous. 2 feet seen. 11/2 ft. Louisville 18 feet = 2nd measuremen {TopofWaldronaboutinRRlevel. about 7 feet of Waldron shale. oolitic top of Laurel with orthoethes subplanus Spirifer endora Multifieldella nitida. W.ofbridge.16ftLouisville.forsmdol.l. TopofWaldronis4feetbelowRR level. In Waldron = Rhyn. concata. spiriferendona.sp.radiata.Orthophyllum. 41 At bridge 4, east of Hobbs, the middle of Waldron is at track level. 42 Small Pentana. olivigerous in Louisville, 5 ft above railroad Hobbs station. BaseofWaldronis5ftaboveRR. oolitic layer{Topaboutmidwayatupretail 35ft Laurel down to shale in Laurel. See Burdston section. The exposed out 18mi. Blue clay shale 3 fossils in white lay Limestone = Lower Laurel? 2ft seen. Therore Halich. Dizza of well. Chapelze Station. Bullitt Cr. Chapelze In Waldron shale - Rhynch. concata, Spirif. endora, Spirifer radiola, Orthophyllum.