About 1km E of Parros is a clay rock with Plat, fenedera and Prasspera. This rock drives a quarry up stream east- ward; the rock is not very prominent now. Horizon unknown, In all I learn this could be the rock at the very top of the so called Parros unit as exposed in the Hills hand section. NE 1/4 NE 1/4 S,T, Hancock, 2 mi's east of Piversyky & 1.5 mi W of Ellisburg, It is not exposed. Mr Timetta exposes 38.5 ft Black shale, cut out. 50 ft Oolral not exposed, at my face an hydropam fragm which may belong to Armheim Or diagnostic fossils 13 ft one colored. Plat, fenedera, Moberling ludden, 4 ft massive arg. rock, 18 ft shale bed, 22 ft Oolral. Oiler, about 5 ft Oolral, creek level. Denb's claim hi hill side but not exposed. Judging from exposures along creek only shale bed exposed here. Further down stream, halfway between Parros & Ellisburg. The outc bying rock with Prasspera in view den NW of school at Ellisburg. R/6 mi. Prasspera large & abundant 5 ft one colored l. 5.5 shale bed. 11.4t. shale above, one colored belw. pm 15 ft. one colored l, 58ft Oolral, creek level 5<2 ft light colored blue, soft clay, 2ft Rithm sand in cross section, evidence from constant injected as anomaly is spelling clay rock which 7 ft Plat. fenedera excellent but not 2ft. Plat. fenedera R/ Prasspera c.c.r. The Armheim has thinned out to nothing. Black shale 2 in pt Duffin layer, 24tft Chex. Dev. limestone, possibly the 4 1yt little exposed. 8 < light blue soft clay with nodules I see sections in Little Ca Smith valley. This places all of these sections in the Mayville practically. Same Slip members This section should be used for Cumberland river.