148 29. Orthophrychula abundant - upper Farmmunt Plat. ferndrena. 30. 31. Garrard 20, 2 mile artificial ponds have been constructed for watering stock = small ferndo. 32. Limestone fully broken from dipping stratum east) under the Garrard as possibly. Down the hill westward is thinly bedded sandstone with lime stone thyme, mineralal, representing probably the Mt type. Farther out is limestone with Dalmac ella multiseeta, Plectam truite serricae, Strophomena gracilis, in ty of Middle Eden?, Pennsone. 33 Dalmanella + Plectam truite common. Eden, 34 - Striph. magonwilleris abundant 50 ft down road in front g fern between typical 33+ 34. This place n fault between 23 + 34. Possibly this is a continuation of the Bundett high fault. Or it may be at least a branch of the latter. This single magonwilleni layer is assumed to be the base of the Farmmunt because same fossil occurrence as far up as the road level. Farmmunt enidra, Platophrychula, Striph. magonillensis, abostroph., Plectam convexa apparently C crystalline, Nodarella residentalis C, Plat. ferndrena. C. in argillaceous rock dipping strongly west. 35. At pond east of house is limestone with D almanella multiseeta c numm. A barite vein is exposed with 10 ft pond, running Mt S, The rock on the east side of Barite vein is the Farmmunt. The rock with Dalmanella common is a west side g vein. The barite vein runs NTS, + contains small quantities of zinc blende, No galena was found. Farther North, High bridge L in the Bend or High bridge seen yesterday rising E g vein, and the Lexington with Rhyndation ma occurs west g same. Also a little patch east g vein. 36. Whinnite with Brazephia c numm. At 840 USG S corel, saccharine L. wit a few Braesphena ovens run fine parallel to North side High bridge. B W Severs 3/4 mi NW Middle Brante in Nidderlandville ferndo ln