irregular and resclnful that I have this time called Wasen Mr Dalmanella seen / 5½ ft up to layer looks like Wassen with Kucina, last words, to, 7ft further up in Dalmarella abroad and in rather thin line of me shivers, formerly called Layer of Richmond,) Septaena Shimbriddis was found 2 ft lower in layer with plenty of Refines quinnagot on edge, By this I mean lower than Dinmitis returning. Retina layers in a same level, a bridge. Mr ends noticed at back of madism at within 4 Cobs rich crossings while the grad was good, it even in the incline down to Milton. Opposite W. this Barilli's home is a gully and at head of this gully, about two thirds is the Dinmitis returne locality! Dinmitis retoma lignum is 2 ft. 9 in. thick. Kendal's branch. Milliners, Aug 30th W. V. p. 378: Believe Black shale sediment was derived from Cincinnati platian along the black shale at top at Savage Corners and melted Coniferous forests while at the same period far Appalachian side of Cumberland channel there was sediments of a differ- it character. George H. Girty ! 1898. Carl Springs, in Guilbfort Creek 2 mi SE of Indian Fields, Clark Co. Ky, Lingula (Lingula)fordii William. circa, n. sp. Leiohyulus gradicatala Vancsen Pleurodus armatus, Blade Sprangites Harmensis, Dawson? 7 Dalmanella alba data. Strigph., Nucula quadridens Gyn Lingula 11ft mediae. Retoma — 2½ ft Septaena Shimbriddis Ref. n. edy. plus