kemi Smith & Alcorn Ry. road 1/2 mi's south of Daleville. chert at base, 24 ft Massive l, ffnish, finegrained and medium grained. Are large Pentemite pygiforms. 20ft about Arctic l. Archinmedes laxus; Agassizirinus C. Pentemites signifurus large C. Pre measure- ments were made along a lay out line along the railroad. The fossils are found chiefly in Upper 5 feet. For these should stop at last. 6ft granular with Martinia glaber C. 3 ft finer grained dark l, with Martinia glaber C. And some small Pentemite, me- b & pygform type but small, - eleg antulus? 2 ft othitic l. with Pentemites elegantula. 2ft Rock like St Johns giani. Apparently there is an inter- calation of rock like St Johns and J granular rock with l extremities, at least as far north as the cut N Dale- ville. Here large Pterithen its pygiformis is found. 1 mile N Daleville is a great othitic l. section 20 ft thick at base Abbreviated section, ? Stvans Valley 6ft Massive yellow rock, 20 3/4t Chiffy clay 10 ft Massive l. Agassizirinus 28 ft Clay + l. Irroriformus 24 ft Massive l. ffnish, finegrained, 20 ft about othitic l. <6ft granular l. Martinia 3 ft finegrained Martinia 2ft othitic l. Pentemites elegantula 1 miith of Burnsville . R. Arctic rock Massive < Cincinnati 168 miles 4 ft 3 in. Bended l. wed mathingully? -> 1 ft ss, agreeably, Proclaima ? 9 ft veg white Massive l.ike frosty green 10 ft Beddel l. Syringophane lithozone 3 ft Lithostrotion lepadome Cherry 2ft Polygranular. Germinalia {fifteen or so slats up to here } [1]ithrostrum cylindricus? 10 ft Chiffy granular, ffiniformis 2 ft broiler layer. pressure on bottom. 20ft St Johns' 4 ft fine grained St Johns depart at Burnsville.