Field notes, Ohio, undated, 2 volumes

Foerste, Aug. F (Aug. Frederic),1862-1936

Unknown

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Geology

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Please return to Aug F. Foerste 348 Richard St Dayton, Ohio FROM THE MILLER STATIONERY CO. 25 East Third St. DAYTON, O. 2847

Walton Dornbusch 135 N. St James St. Waukegan, Ill. In Bill's creek in reach of Whitefish river, 6 mi. N of Belar - 12 ft shales. 2 mi S of Squaw Ot. = drift covered. N of Escanata - sections lower. Largest sections = opp. Escanaba Landsperm 4 mi E of Light house T 38, R. 21, Sect. 8. net imp. = 6 ft. arenaceous shales, Chaetetes Platystaphnia Dalmarella Raphnequinus Light house at S end of peninsula E of Little Bay de Noguette Rocks outcrop from here for 10 miles N. in cliffs 15-50 ft. 60 ft = total section. 3 ft. = uppermost beds, light colored siliceous flint nodules cc. fractured shells of same kinds as those below. 57 ft = blue argill. c. x Streptelasma reticulum fer Orstocaria riclin in densis 12. Tetradium lounacuse 12. Platystaphnia Pele et ortuis plicatella Dalmarella testudiqua Defertella residentilis Raphnequinia capax fer Raphnechinoma small op. Zygophra urdesta Raphinesquina alternata Straphnelina cimata Strephnelma Byss mycliis x Meridiopsisun di'clais x Pterinea denissa x Cyrtodonta x Perbelus gigas

Electricity 22 *26 Ster, 27 Ster, 27 Aster, 21 St. *37 Ster, 39, 31 A 17, 15, 13, 12 Ster., 14, 16 Ster. Emmeline C Case Chair. of Michigan Bal. Ann Arbor. Charles W Cork Chair. of North. William D Hitts. Chair of Mich. Sed Min. Walter P Hunt Chair of Chem., Minn. Edmund Illanes Chair. of Mich. Minn. Ed L Osbourn Chair of Work. Frank Everett Ann Arbor. Lucius L Houghland Houghton. Wattles W Jefferson, Mich. St. Normal, [illegible] A & Seaman Mich Coll of Mines Houghton Drummond Island. Dividing old-Sili. line - From Vieux Bat hearth in Portage passing Bay, SE to centre of Six greates Bay. Principal vein crops between Six great's Bay and Reynolds Bay. dip SE. streptelasma necticum Colium maria alb data Calopocia burqulosis strumator cistam buer mona Ort area vitreata Rhynechotroma capax zygospira ardesta Capines spinis alternate Platy atr plena Plectnthus plicatella Robert ella a ident dis Strophomona Modilopsi modi lavis Dartclus gigas.

Trenton, at Loc 4. Section 17 of T 41 R 23, 6 5 4 3 2 1 7 8 9 10 11 12 18 [17] 16 15 14 13 19 20 21 22 23 24 30 29 28 27 26 25 31 32 33 34 35-36 Comarocystites punctatus. Strephomena Plectotus jectinella Orthis triceraria Platy strophia Fygraphia recurvata Rhynchotrema plena Crania Pholidops. Jatillus gigas Illaeus americanus Chiermus Calymone Othrops callicephalus Eucrinus Streptelasma Stromatocium.

530, Hartfrd Ave, SW on 2 minn av, Miss Margaret Campbell Milwaukee Danner College Lake 2593. Ogan Coll. Chicago Acad. of Sciences. Delafield, Anispira madrunidea 1111 Alverites irregulanda. 1112 Multicilifera ramma 1099 " pulchella 1097 multitu forcucata 1153 rectangulana 1103 sulpulchella 1100 Fitzhulpia oridissima 1080 lens 1081 jamesii 1092 pulchella 1098 Cassellaria pulstrella, 1088, Delafield. Plemapna granulata. 1087, Plutistylpha hypnata, 975- (Rlyneclerthoma copax, 960) Dm Ridge Replner zurna nitens 1015 Plect ambunite, avicena, 997, Calymene cenaria Robert Benham C. J. Kreibiel Co. Broadway + Reading Road, Cincinnati, O. 100 reprints extra. Leo Gnew 2314 Murray Ave Pgh Pa Sheney 1798 R.

Somrigtm N 15 W strua. Harphnuma wide, acute angles. Rafinesquina Strephomena hismenis? Strephomena mutans? Rafinesquina large, moderately curved Mordilopsis of concentric Phladomorpha philadiformis Ptminea demissa 2 in. long, Dakwanella ingra large. zygophin zebra like Ctagya and Platyshelvia elates, slender Herbille of presidentalis Pyramychia Strephomena neglecta Cranida L. P. Barrett, 30 years old. Andren Rheinwelder 5 ft church 31\frac{1}{2} ft fossils? & chalk black. 9 16 min sine + } B stratum < 2 min. Grouse Hall Church Swed. Luth. < 8 min. And. Rheinwelder, 3/4 mile to the S of stratum at me. 5\frac{1}{2} ft, of cream colored l, with Ptminea, Pyramychia & Phosphina Cymophalip, chats a little Amberlych 11 ft of fossiliforms gray clay & rattle l, w/ white- water ? ichr. 2 ft of clay rock with Phladomorpha. 6ft. fossiliforms? gray the clay & rattle l. as in 10 ft layer above. Straphomena sulcata 7 in down 1 ft Rhembystra quadrata of 10 ft Strephomena small length ? yrs at Norwegian church above, \frac{1}{2} mi S of stratum A specimen suggesting Dinathis subjeu denta, at next landingS, came from 1 ft below top of 16 ft Znr. Another, large cracked at landing near Norwegian church.

And. Rheinfeld Nympha Church Stington Rd. Brad, Farmers Dock, schree, No.2 = 2 1/4 mi S of Stratton. scow Skauge Brothers = 1 3/4 mi by nd schroll Store. m Wai de jorad Finn line & bluff for 1m's 1m' sandy beach, Dinuthis antguadrata 1ft film the upper cream colned cherty and occurs at last cliff out crop gring S. = first out crop NE of Farmers Dock. NE of Farmer's Bluff. J pile. Chert L. 14y's. Fossil O. 16 ft clayey with Wht Mintersta clay bank 2 yd cloud Dumps at 24 cm- in ch 5 ft. down to shale, Almygrad E & Stratton corner. Cherty L. grey, weathering firm + cream colned. D deranella jupre Primula deniara Platynophia clarkovillensis Simpsonina much elongated laterally Calymene sp. Pygmycheia magnitabulum Reibella occidens Strophalosoma austromum 21/2 by rather strongly curved. Streptomena stylacta Dinuthis antguadrata Cgt rodonta almygrad Relictroma bruckei Hormotoma Lophospira bicincta archiacella Proctus like but long + narrow. Modiolopsis magnitabumari? Conularia cf. folosa Cyrtodonta Rotund of old lighter fossiliferous Base of ditch, just below cherty L. layer. Lichenorisma intercalata Dinuthis antguadrata

e *2 *3 Sk ang Bass. Myjun Mytilus like carnelli & and. Hornwort mud Gymnopine Plecotrea Ostrea Platys phle Hebetula boodensis Stephomena neglecta Bysamy clw in and bullmers Stepheloma errord, me 3\2 x eng, Base & harder, weathering wth. beach. 13 Sk ang Brythia 4 mi sq stratta. from Stephelasma muticomm. med. Plumatostyga quadrate D'almanella jugosa Platy sphle d whosillmers Hebetula occidenta Hebetula abrecta? Reptine pinnal laterally elongate Reptine frusta, larger, curved, Reptine spines, large, nearly flat Stephomena neglecta, stephenmella at ally elongate Stephemina lanuiceros Stephemina formell and aus 2g grappina globose from Stephelasma aurifex Stephemina vetusta Oterma dermisca Cath. rerua dist ant septa

E *2 *3 Toftum farm road to beach, Julius Brandt + Claus Petersen Bore Cherty, as at Stratton, in 10th. Kemi N of Stratton 57 ft interval, 5 ft very crasdy granular, 21 ft clay shale with sm-? underated clay layers, lunch, 1 mi NW strat on Cass road, many old trees Fossils ?? of next stratum? once. ? Strphomenus sulcata. Dinohthi us gradata, Ostrac quells lutica cc. Cass road Smith Berg 12 min N of Stratton. 6 4 mi from Stratton to Lighthouse. Bacazata + Lake Superior Rd Wells 3.45 Hescomahi 800 3.30 17 Kingsley 853 .217.2 32 Channing Hallwood 1/2 mi, Eversen. Gerscho? Winnebag, Wb am pm om 7.05 6.20 10.40 Madison 5.30 3.10 7.35 pm am am. Mrs Creivy Bird Service, corals. Sardes on old railway early Michigan. State Geol Survey. Neenah Duniv. Delain? Madison Park Inn ? B Junct 107 Washington 75 Elkhorn 75 Foss 41-25 Winneago Wd Nicollet 1.75 Weed 1.05 New Campfield new Vandalia to Stroma 1.00 Revere .75 Mojest. 75 Longlynn 75 New Winsell 75 Allen 75 & olda West .95

Sardes on Collection Orthus futilis, extremely fine striae, scarcely visible with a lens. x Orthus perradi, dorsal valve tends to be more convex than the ventral. x Orthus emacrata, slims, fasciculate grapey y flications distinct outline. Orthus terea, very convex at back of ventral valve; very short hinge- line; faint small striae [illegible] x Orthus ignota has double plication at back, sinuos in front, resemble weeki. x Orthus copulenta, alternating plica- tions as they come in convex brachial valve, x Orthus argata, medium plications, plications come in symmetri- cally on two sides y media plication, Chas B Cleavy Mar. Ago. 2022 Park Ave, Chicago Ave Car. n 6th St. Sardes on Collection 1 Plect ant no [illegible] small, convex, get size with age. 2. Plect. plication strongly convex, especially at midr. 3. Plect. recedens, quadranigulara, and long tends to have a flat backy 2 plicae 4 Plect. Oaxea broader or flatter. 5 Plect. services Brickyard, Twin City! Near Pi [illegible] Lake Minneapolis - St Paul street car transfer Wabasha + West St Paul, to Charles Heights gor to end of line, in county line. Or straight W until road bends, then to R down the ravine. New Palad. 4 street

Minnesota. Spirorbis vitrea, N. Rhynchosia feda Escharina limnata. Rhynchotya ? feda. Schuchart collected Rhynchomella neenah from San Ridge Wisconsin. 32 strath Brthig. Miscellaneous Vol 1, 1883. No new species, of no value to me whatever. Vol 2, 1878. No new species even in Keenah, About 1/2m SE of town quarried to depth of a few feet. Spirula gradata O. fectinella Nemipermtes americanus Rhynchomella neenah, Helicostoma planulata Cranularia ? tentacum? Dentulus ? varus? Menasha 2 jars, N 5 of Mr Arnt Recylacrita ovuli? S. monesi; Streptelasma conviculum O. utto fectinula Ortho durganiis, Ortho tricenuata Stylopemena ? curvata? Rhynchomella neenah Duck creek at outlet of Duck creek Planorapyth Glyptocystites O. fectinelle Streptomena ? incruceta Rhynchomella coprea Dalumonta calypstula

Front Flintville, in river bed, Hermite Americanus Rhynchonella neoral Platymetrodon wrightiatus Strophomena incrassata, Miscellany. Cincinnati Oran Ridge O. subquadrate Strophomena auricostata Strophomachus Rhynchonella cupax Rhynchonella minor affinis Rhynchonella palamestera Green Bay Whitneys Bluff, 65 feet exposed, Mr Jones mentioned. Green Bay, S of Little Sturgeon Bay, 15 feet exposed,

Vol. IV. Out- volume of value to me Polyclinella palandella a Min. Am. Rep. 3 mr. Mich 1877, p. 73, Delafied + Sam Bridge Mt Figured frm D lafield. Polyclinella neenah. Oentr at Neenah, Menasha, Centra, Oajim, Wata lor, Jlmesville, B elsvi, G leen sheio at Oshkosh Neenah, Menasha, Plushille An Dan River at Delafied. 19 mrct 20m Bridge 20-22 Figured frm D. Lafield. 3 trophima bingii, m Figured frm Delafield. Strophomena micrstate & spred from Delafied. Strophomon specimen novae, figued frm Delafeld. 5 Weststrophonus Cardinals Figured from D lafield. State Geol. & surg Map, 1911, 30 cts. Superint indenty Public Projects, Bull. 29, 2nd Series No 3, Waukesha Co. (Delafield) 1914, 5 cts. Ed. IV m. Savage, T. E., 611 W Nevada. ? instructa bvir. Galena + Apple River, The Strophomenidae of the Kristianic Region. Oly H. F. t. dahl. Widenskapselskapets Skrifter. 1. Nat.-Vittour. Klasse 1915. No 12. Kristiania, in Commission at Jacet Dybwad. 1916.

Forster 46 Oxford Ave. Buy, Agent, Buy Buy Mrs. Clara, Married Florence*, Daughter Marj Lutz Emburger, 450, 4th St., Near Borderland. Mrs Anderson, Mrs. App. Dayton Vier Sch Barn 133 Rothernd 6.00 4' 4" x 17 in. tread 4 7' x 30 in. Cohn 492 Hill Street Library, Main 2268 Business Office, Wes Dury 537 R[illegible]way Ave Canada - Memoin 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18E 19 20E 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 58 59 60 61 62 63 64 65 66 67 68 69 70 71 72 73 74 75 76 77 78 79 80 81 82 83 84 85 86 87 88 89 90 91 92 93 94 95 96 97 98 99 100

Change of address. [illegible] 2/3 3/3 Am. Min. Journal. Am. Inst. Scientist Forey Bulletin Science Sat. Evening Post World's Work: Doubleday Page & Co. New York 11-13 W 32nd St. Journ. of Geology Outlook National Geographic Mag. [illegible] Am. Journal of Science Bull. Biological Survey, Bulletins Bureau Divining Public Documents Look up Refines gruei Kingi. Whitfield Wisconsin 4. 1882. pl 12. fig. 15-16 27 Hendlev. upper: 3bimert mc, Hirmant 2 ay'llacem volint me. 1 Limart me, luma = Bala Christ me.

electrical conductivity is proportional to thermal conductivity K/q = constant The continuity will determine the electrical flow also determine the thermal flow Migration of electrons in both cases of conductivities 12.48 + Swridge Donald And Schrauths Robert 39 + Bizer Erwin ? 23 A) + Brown Albert 23 A Brown Edith 23 A + Ferguson Robert 14 (Shannon Edgar 12) (Riley 71 73 Park 35) Ltz. 78 83 79 36 74 84 88 Rochle Walter 15 Smith Harold 23 Race Albert And. Chance Fred. 14 Rike Fred 15 Leptocera rhomboides small + Diaphorostena miagarensis + Dalsmanites Sinulimus + Spinifer miagarensis novist. Spindle with implications within Metellus + Plate trophob Daytonensis 3 n field + one by Proterozoic cornutus Cladozona reticulata Diemancatus Spinifer acuta Clypeus reticulatus -+ Cyrtoceras myrice, Kemper, Amphicoelia costata Kemper Mareiprimum praematum Kemper Partikim v-ceras rebeclus Johnson Syngolito Springfield op. Johnson might photograph for transverse connections. Calliovrissumit plate Johnson, Platyceras angulata, Johnson, Holozetis cenostrate. n.op Johnson Phynchitesa conneata? - n.op Palamita

58 measured 40 miles. Real 1 7,9 2 7,8 3 8,1 10 8,5 11 8 12 7,6 13 6,9 14 6,8 15 6,6 16 6 17 5 18 4,2 19 3,6 20 3,2 21 3,1 22 2,9 23 2,7 24 2,6 25 2,6 26 2,9 27 3,7 28 4,4 29 5,7 30 6,9 31 7,5 32 8,7 33 8,7 34 8,5 35 8,7 1 graduated wire to 2 3 4 7,5 5 7,5 6 7,5 7 8,2 8 9,2 9 11, 10 11 12 13 11 14 15 16 9,5 17 9 18 8,5 19 8,3 20 8,0 21 7,3 22 6,5 23 5,6 24 4,7 25 4,1 26 3,3 27 3,0 28 3,0 29 3,0 30 2,9 31 2,6 32 2,6 33 2,5 1 2,8 2 2,9 3 3,5 4 4,3 5 5,0 6 6,4 7 6,5 8 6,6 9 7,3 10 7,9 11 9, 12 9,2 13 9,5 14 9,8 15 9,5 16 9,3 17 9, 18 9,1 19 9,2 20 9,5 21 9,9 22 10,0 23 10,5 24 10,8 25 11 26 10,7 27 10,2 Cincinnati. 28 9,5 29 9,6 30 9,3 31 9,2 32 8,9 33 8,8 34 8,9 35 8,9 1 9 2 3 9,2 4 8,9 5 8,3 6 8,1 7 7,1 8 6,3 9 5,4 Change 3,9 10 4,9-7,9 11 7,6 12 6,9 13 6,2 14 5,5 15 4,8 16 4,3 17 3,8 18 3,7 19 3,7 20 3,6 21 3,2 22 3,0 23 2,8 24 2,5 25 2,5 26 2,5 27 2,4 28 2,4 29 2,9 30 3,6 31 4,4 32 5,4 33 6,4 34 7,1 35 7,7 36 8,6 37 8,9 38 9,3 39 9,5 measured from West to East. 28 2,5) 185 (7.4 33 17,2 h. 35 108 39 7,4 135 5-2 3) 270, 90 in 37,0 (90) max length drawing 37) 90 (2,5 74 160 148 -

Teaching Physics, Marin Macmillan 1915 5s.net. Dr Charles A Mercer Principles of Rational Educat Mental Culture Enterprise, 329 High Street. Very idlect land Una Stjellest terrain is that of Inn Pernia. Warc marks. Area too wide for shore ripples. So many horizons in Blanford each of which suggests some change in level permitting some new migration. Instead of changes very few then perfectly sure on grey, H. botelle his melpha 3 ni res. Dinther outquadict a. Rhychothreme dentate, Stiple more ant musc, etc. Anthinella Wave marks of same age only should be compared. Waremarks in successive strata, change i direction suggests change in condition similar to those accompanying changes of fauna. Wavemarks compare with Kinde's illustrations, Are dr coarse-grained limestones originate? Since nuds.

Worm marks. Some of the pebbles practically never were moved. Others partially once let down, by hunkering up & moderately cleaned, when fine stuff was washed out & coarse grained material remained behind. Wind could not have settled at once on pebbles since time must have elapsed sufficient for growth of Crabs & Rhizids otherwise, A shoreline crack draws away laterally, a wind crack spalls off upward at edges also. To what extent do wave marks tend to indicate the trend of the shore line, or do they indicate wind direction? In a shallow epicontinental sea, it should be wind direction. Wimbleton Shore Road bridge Measured from S. to N. 35 0-8.2 1-8.5 2-8.3 3-8.2 4-7.7 5-6.9 6-6.1 7-5 8-4.2 9-3.6 10-2.7 11-2.5 12-2.8 13-3.2 14-3.5 15-3.9 16-4.5 17-4.8 18-5.3 19-5.6 20-6 21-6.2 22-6.3 23-6 24-5.9 25-5.9 26-6.3 27-6.8 28-7.2 29-8.1 30-8.4 31-8.5 32-8.5 33-8 34-7.3 35-6.8 1-6 2-4.9 3-4.1 4-3.0 5-2.7 6-2.7 7-3.3 8-3.5 9-4 10-4.6 11-5 12-5.4 13-6 14-6.2 15-6 16-6.0 17-5.9 18-6 19-5.9 20-6.3 21-6.9 22-7.3 23-7.6 24-8 25-8.4 26-8.5 27-6.3 28-7.5 29-7.2 30-6.5 31-5.4 32-4.1 33-3.1 34-2.5 35-2.7 1-2.5 2-3.3 3-3.8 4-4.8 5-4.7 6-5.3 7-5.15 8-5.8 9-6 10-6.1 11-6.1 12-5.9 13-5.6 14-5.9 15-6.3 16-6.7 17-7.1 18-7.5 19-7.7 20-7.5 21-7.5 22-7.4 23-6.8 24-6 25-5 26-4.4 27-4 28-3 29-2.5 30-2.5 31-3 32-3.7 33-4.3 34-4.7 35-5.1 1-5.3 2-5.4 3-5.5 4-5.7 5-5.8 6-6 7-6 8-5.7 9-5.6 10-5.9 11-6.3 12-6.6 13-7.3 14-7.3 15-7.3

Windcatcher above bridge - end. 16 - 7.1 17 - 6.7 18 - 6 19 - 5.1 20 - 4.4 21 - 3.7 22 - 2.8 23 - 2.5 X - 1 - 2.7 2 - 3.2 3 - 3.9 4 - 4.7 5 - 5.1 - 6 - 5.6 7 - 6.1 8 - 6.13 9 - 6.5 10 - 6.5 11 - 6.4 12 - 6.4 13 - 6.13 14 - 6.4 15 - 6.5 16 - 6.9 17 - 7.6 18 - 7.8 19 - 8.1 20 - 8.1 21 - 7.7 22 - 7 23 - 6.3 24 - 5.5 25 - 4.5 26 - 3.5 27 - 2.8 28 - 2.5 X 29 - 2.4 30 - 2.8 31 - 3.4 32 - 3.9 33 - 4.5 34 - 4.9 35 - 5.2 1 - 5.7 2 - 6.3 3 - 6.3 4 - 6.7 5 - 6.0 cc 6 - 6. 7 - 6.1 8 - 6.5 9 - 7.1 10 - 7.5 11 - 7.6 12 - 8.1 13 - 8 14 - 7.7 15 - 7 16 - 6 17 - 5.1 18 - 4.3 19 - 3.7 20 - 3 X 21 3.2 22 - 3.6 23 - 4 . 24 - 4.5~ 25 - 5 26 - 5.6 27 - 5.9 28 - 6.5 29 - 6.5 30 - 6.5~ 228 Fossils etc. Sleepe grudge more frequent: Striplaminhus Str retusa Plugs, cafex H. occidentalis Str vulcenta Rel. alternata vly abundant hygram ee. Fossil or den in temple hut not in S side Bridge slope. Relative intensity & periods. Analysis of wave wanted, 2 component waves. Large boulder in this layer, earlier strained. One very large boulder polished - grooved by me = 4.7 ft N + S long by 3 in thick, and must have been about 45 in. wide also. In the end only & surrounding rock the wave marks also are deepest in S side as at bridge. From 3 to 4 in of coarse li underlay this large pebble. Along middle in N + S direction, it is level with the surrounding rock, but at SE edge it rises 2 in over above the 2 area, being in trough of wave. Warp here have approximately N + S trends. 17.3 in = 5 steps 34.6 in = 12steps Distances: Round bridge, 280 steps 807 ft 800 35 steps, pebble jolney 101 ft 100 2 extreme 35 steps. 101 ft 100 hence 130 steps. 375/ft 375 large pebble. 37

wave marks Great abundance of fine-grained Oolitic pebbles. Relatively few distance washed pebbles. Pebble edges rounded both as well as above, along edges, hence have been moved, This is true even of the very large pebble 45 inches across, In case of the small Portara pebbles, the coarse grained stuff which should have engulfed the pebbles was washed away clean, and this is the only reason for the pebbles not churning up. Wave marks after the washed down to underlying layers through the coarse glauconite layer. 35 25 60 18 Clarkeville Yron in anhydrite, 3 str. calcareous finely commin. Cyclamine Ruby ratite rate, 2-4 m layer. Ripples weak. Interval 1 1/2 ft. Diminthis only in 2: th., one spec. Interval 1/2 ft. Strongly rippled marked layer, N35E. With -8.8 1 -8.4 2 -8.7 3 -8.9 4 -8.9 5 -8.3 6 -7.7 7 -7.2 8 -5.8 7 -6.0 10 -5.2 11 -4.4 12 -3.8 13 -3.1 14 -2.8 15 -2.6 16 -2.6x 17 -2.8 18 -3.3 19 -3.7 20 -4.4 21 -5.3 22 -6.0 23 -6.7 24 -7.1 25 -7.4 26 -7.5 27 -7.7 28 -7.8 29 -8.0 30 -8.1 31 -8.1 32 -8.1 31 32 33 34 35 1 2 3 4 5 6 7 product from 5 each. 9 10 11 12 13 14 -6.0 15 -5.9 16 -5.9 17 -5.6 18 -5.11 19 -5.0 20 -4.5 21 -4.0 22 -3.4 23 -3.2 24 -2.6 25 -2.6 26 -2.7 27 -2.9 28 -3.4 29 -4.0 30 -4.7 31 -5.3 32 -5.9 33 -6.3 34 -6.6 35 1 2 3 4 5 6 7 8 -7.3 9 -7.1 10 -6.8 11 -6.8 12 -6.2 13 -5.5 14 -4.95 15 -3.7 16 2.7 17 - X 18 19 Note: 'kings' is written vertically on the far right edge.

41 East 20 -3.6 21 -3.0 22 -2.7 23 -2.6x 24 -3.4 25 -4.8 26 -5.3 27 -5.9 28 -6.5 29 -7.1 30 -7.6 31 -8.3 32 -8.5 33 -8.15 34 -8.16 35 -8.8 1 2 3 4 5 6 7 8 8.8 9 -8.6 10, -8.4 11 -9.9 12 -7.2 13 -6.4 14 -5.6 15 -5.0 16 -4.6 17 -3.6 18 -3.0 19 -2.7 20 -2.7x 21 -2.9 22 -3.2 23 -3.9 24 -4.9 25 -5.6 26 -6.7 27 -7.2 28 -7.7 29 -8.4 30 -8.4 31 -8.9 32 -8.6 33- South Trip 34 - 35- North Trip 1. 2. 3. 4- 6.9 5 -7.0 1-6.7 7- 6.4 8 -6.1 9 -5.8 10 -5.2 11 -4.8 12 -4.1 13 -3.4 14 -2.9 15 -2.6X 16 -2.6 17 -2.7 18 -2.8 19 -3.4 20 -3.8 21 -4.4 22 -5.2 23 -5.9 24 -6.4 25 -6.4 26 -6.9 27 -7.2 28 -7.4 29 -7.8 30 - 8.1 31 -8. 32 - 33 -8.5 34 -8.3 35 -8.1 1- 7.6 2 -6.6 3 -6.1 4 -5.1 5 -4.2 6 -3.6 7 3.0 8 -2.7 9 -2.15 10 -2.4X 11 -2.9 12 -3.4 13 -4.0 14 -4.3 15 -5.0 16 -5.6 17 -6.2 18 -6.6 19 -7.1 20 -7.3 21 -7.6 22 -7.9 23 -8.0 24 -8.2 25 -8.1 26 -8.3 27 -8.1 28-8.2 29-8.1 30 -7.9 31 -8.0 32 -7.9 33 -7.2 34 -6.5 35 -6.0 1 -5.3 2 -4.1 3 -3.5 4 -3.0 5 -2.6 6 -2.6 X 7-3.3 8 -3.9 9 -4.2 10 -4.6 11 -5.2 12 -5.1 13 -5.9 14 -6.3 15 -6.3 16 -6.3 17,-6.6 18 -6.8 19 -6.9 20 -6.6 21 -6.4 22 -6.2 23 -6.0 24-5.9 25 5.4 26 -4.8 27 -4.6 28 -4.2 East Only well defined Ripples whittle d present trip 2 / Ripples in canyons in their rippled range. One large kettle on E side of crest of ridges F=3 1/2 x 3 miles in length. Ridges and smaller I'm not sure. Gravelly Rippling ground with few. Second / Stone-line depression Rippling ridge rare. No species of Mucuna noticed on these plants of ridges, standing firm and steady looking from East and E. to West current, X 1/ Note, Scuttle depression whiting center, West

Peckhami 2/3 mm. total. 43 Spongophyllum giganteum; Etheridge, Rec. Sed. Surv. NSW, fn 1898-1900 Publ., 1901, p. 158 published in 1899. Circumferential zone largely vesicular; the vesicles large. 5 pta 7 intermediate zone from 45-50, with un marked divisions into primary & secondary, intra- costal dissepiments; Central area tabulate, tubulae very close together, as a rule, largely vesicular, the vesicles small, looks much like Spongyphyll- um, except that tubulae are described as vesicular, Whole Cryathophyllum Mitchelli. Der. Etheridge. D dem. Vol. 2, p. 172. Resembles very Bolmiense, Blainville. 1892, Laudaleia(?) bipartita, Eth. D dem. vol. 1 p. 22 1889. Resembles my Spongophyllum demgophyllodes very closely. Spongophyllum and Cryptophyllum are closely allied to this species. Published during or shortly after 1889 privately,

Cyathiphyllum approximans Frederick Chapman Paleontologist to National Museum Melbourne Rec. Geol Surv. N.Vict. Vol III, 1914, is said to resemble C. mitchelli and but is from Gippsland Silurian Scott & Jeffrey. On fresh Plants from time of Waverly Shale J Bentinck, Royal Soc. London. Proc. Trans. ser B, vol 205, pp 315-373, 13 pls, 5 figs 1914 E.G. Pittman, Government Geol. Sydney, Prof. E.W. Skeats, Univ Melbourne W.G. Wollnough. Lect. Geology. Univ. Sydney. Prof. O. Marshall. Univ. Otago Dunedin, New Zealand Serb. J Gas District. A.J. Shearby. Silurian, Austral. Ass. Adv. Sci'4m 1911. P.M. 1912, p. 106, Address, Yan., N.S.W.

Amphibichas tentamen Carlisle, Pa. Lichas halli. Front. Amphibichas leavis interie view of top by system & thena 47 Lichas crosimarginate North Graine, Columbia Term. Curlypt. Lideas I studied both shells further from medial groove.

49 Storm Point N 1/2 Fair Haven 3 mi. 2 ft dolomitic O, thin bedded Springfield 1/2 ft Pottsaucus cc wt top half, less chalky 8 1/2 ft limestone, thin bedded, 2 1/2 ft cherty limestone, thin bedded, <-1090 ft U.S. G.S. rocks dip N here, but possible in different directions farther N. NW 1/4 Fair Haven 1/2 mi. lying the clay shale. Rehobella + Rafflesquina over Ridgwood limestone with then are at least 6 ft of heavy bedded About 15 ft thin bergy Transfield. 1053 37 1016 Richmond ark 2 ft thick, underlaid by a very white graniform feet below the road corner 1053, and in SW from quarry the face of Clinton is seen 37 There is a total y about 13 ft of Clinton. - 7 1/2 ft extra Clint in farther SW, my belief, 6 ft Clint in = local. From Fair Haven SE 1/2 mi., then E 1/2 mi. Concludes cc, with Silica mica retinate at creek level below bridge, at 975 USGS. = Limestone, sand and by some clayey stuff.

From Fair Haven, 2 mi E, then 2/3 mi S and east 1/8 mile to farm house. Brassfield at 10:05 USGS. Neklem shows up in creek along road northward at 997 = creek bend. M.J Brassfield at 10:33 former trip. Brassfield not exposed this trip. Muttenville, 6 pressure km W, bridge on pike. 965 USGS = top of clays which are jammed full of fossils. Nekeloc, + Rafinesquina, hyrzams. From Sugar Valley 3/4 mi S, 1/3 mi E, 1/3 mi E. Pentameros apparently at 10:27 USGS. Actual exposures in creek did look like rock immediately below Pen-tameros at Ridley Point, N of Fair Haven, and the Pentameros occurs immediately above apparently. Pentamerus found loose (in blocks) at top of actual exposure. Magle Barre Church 4 mi SE of Eaton. On R + S road, 1/2 mi each way: white l. over Brassfield about Brassfield at two point immediate S J crossroads, about 955 USGS. West end of West Elkton. 6 1/2 ft of whitish limestone layers one to three inches thick, inter-bedded with whitish clay, the clay predominate at base = Cent Orchard clay shale. 1 ft. Several white l., like that above, in layers 2 to 3 in deep thick = Daytal equivalent. The rock is very finely grained, white and chalky, and does not look like Daytal. No fossils seen. Brassfield top with calcite nodules. Rock rather roughly bedded. 10 ft opened. Original thickness may have been greater. A quarter of a mile W by Kenworthy school; the top of The Brassfield at 10:20 USGS is overlaid by local Niagaran fine-grained limestone. Half a mile W by Kenworthy School, 10 feet of Brassfield is exposed. Total unknown. Half a mile S of Bakes School. Brassfield up to 1040 at road corner (1042). Base of Brassfield probably at 1030 USGS.

Eat m. 1 1/2 mi SE, then down Rocky Rim 1/3 mi to quarry. Whitish cl. = 9 inel. cl. Not much 5 ft whitish clay shale = Oxford extended 9 ft. Dayon limed me, some of it quite typical, other parts often. Brassfield. Total thickness could be measured here. Bantas Fork Overlying arch 10 ft. Lower 1 ft = bedded lime Crimsonal (J.Olympus) Redbank? Whitish cl. Christy cl. = 1ft. Then folded after limit me 2 ft 5 ft n clay ark, 1 ft. Plm whitish limed me 1 1/2 ft. Clay shales indicated clay arch= Oxford, 4 ft exposed. Probably about 5 ft thick. Base 965 NSGS, Base of Brassfield calculated at 942 NSGS. From Brennersville Inn s and SE to creek 976. Oxford clay level. Top of Dayton cl., at 968 quarried Dayton cl. 10 feet thick measured. Brassfield top at 958 NSGS. Brassfield time calculated at 945 NSGS, 1/4 mi E y Brennersville Martin House quarry. Dayton cl. quarried. Base of Brassfield - about 950 NSGS. Brassfield 16 ft actually measured. Prices Creek. Brassfield measured: 16 ft. Brassfield time: 948 NSGS, exact Quarry E y RR track. 1/2 mi's J 939 J limit of Eatm. Lewisburg Paint Gr, 965 = top of Brassfield; Brassfield: 17 ft measured. Brassfield time: 948 ft NSGS, E y Lewisburg, E y Paint creek 1/4 mi, SE 1/4 mile to road from 943. Brassfield up there? Base of Brassfield at 945, exact. Lewisburg quarry, Land, about 8 ft. (1 1/2 ft clay + argillaceous indicated ark) 2 ft clay 10 ft Dayton. Brassfield top at 940. NSGS, exact. Base at about 923 calculated. Camden 2 mi W 1 mi's. NW of road line Spring. Brassfield 1015-1020. See Fig? Top run with me seen. Also at Road corner up to at least 1027 NSGS, Big Cave School Corner. NE y Cnr: white limed clc lying along quarry 1035-1040 NSGS.

Big Cave School, 3 mi NW 1/2 mile clay with indurated shale. Thick bedded fossiliferous daylight limestone 3 1/4 miles, while I TJ of Branfield - 1040 NCS Branfield or least 1974 Chick, But not exposed Road corner 1053. May extend up to 1050 at least Big Cave School, 1 mi S, then to four house. Branfield up to house level and thirteen limit up to 1042. At least 975 rock shown of below this land. Big Cave School, 1 mi N, 1 1/2 mi W, Springs SE of road corner 1027. Branfield base = 1027, W of Union road, Flynn Mfg factory joke, 2 1/2 ft less well bedded limestone. 5 1/4 ft white clay, well bedded - Pentamurus Pentamurus or in base of quarry. East J Union road at school, SW J corner 983, 2 1/2 ft less well bedded shale. 2 1/2 ft Hematite bedded rock + Pentamurus 2 1/2 ft, Thinner bedded L = Springfield also. West J Union road 2 mi, Mfg factory joke 1 3/4 mi, - large quarry. 4 ft crosser bedded rock, with Pentamurus in layered layers. Looks more like Cedarville rock. Orthos hyprita. Lepidoceras North american fossil may be top of Springfield shale, 11 ft well bedded Springfield with Pentamurus or 2 ft below top. 1/4 mi due westy quarry. Clinton face = 930 us GS. Clinton top - 940 cliff along N + E road 2 mi E of quarry.

quarry 3/4 mi N of Fairview School House Tmi E of Amity + 1/2 mi S wth. 2 ft cherty rock. 3 1/2 ft' Rather massive bedded luttles. 6+ ft Well bedded rock. resembling Springfield. As far as I can tell, the entire section, including the cherty rock at the top, may be Springfield. Some fragments cut coming from between like the Kitchenaria of the Red and the 1st & the Sphrodex relics rorwingeri) may come from immediately underlying Cedarville here At road corner 961, north of quarry, 4y mi. 6-thin bedded which doesn't seem to be the same as that at face of quarry last described. NW of Amity = quarry. 6 ft rock resembling Springfield at the lower quarry is more thinly bedded, which doesn't also resemble the Springfield Bearing 2 mi W of Drexel, 4 mi NW of Stop 5. More coarsely bedded L but no Cedarville fauna seen. - about 5 feet. 8 ft Well bedded L. Springfield with bent ammonites within 2 feet of base. Basal side of quarry, with arthur's labellites Pterocrinus gemmifrons stephencrinus scordium, & small crabs which may be? ?Heloplacoma ? ?3a? brachiopod signata? but the specimens are too poor to identify even approximately. East of Taylor crossing (Union City line) 1/2 mile, on road straight east to 6 mile house. N E of Brasfield = 915 US GS. Considerable Brasfield exposure here along side. Glacial striae S80E, Considerable exposure of Brasfield also east of C Road 936 going from the hill, cells below beneath. One mile E of Taylor crossing. W of 944 Brasfield topo = 922 US GS Glacial striae - S 80E about.

a little over 4 mi N of Six Mile Arm where lane goes S to farm home Brosefield exposed about 5 feet above entrance to lane and also formerly gneissed here in S side of road. Bme - 9.60 ftns & s. Englewood. Brassfield up to strike level 1/2 mi S 1 point where National Pike cross section D 5 miles field wth Pentamerus 2 1/2 ft above C 5 1/2 ft Tentaculites typical B 3 ft Fairly well bedded Cephalonia Lared {Lared c. 1 3/4 ft} will bedded {Lared b. 2 ft} < Atrypa reticularis, {indicated clay rock 1 1/2 ft} {Blue clay shale 3 ft.} Dagtmel, 8 ft wth 5 ft thinbedded Brassfield Transition, 10 inches. Brassfield 2 2 ft. Drypea (as per elijarta schumbe) elle, like Birker dam form: large B Atrypa like Birker dam form. B Striatophora cral protosordials, B With flatellite B Platyspharia lignata, C Platyspharia lignata D Atrypa reticularis B Platyspharia lignata, C Blackjawm Like Lilty form. Interior of actual valve well marked + showing fine radiating striations Exterior, Could not collect but well preserved. C Pentamerus in typical mottled Tentaculites rich in upper 6 inches. C with flatellite to, C Large Striat form 5 1/2" in diameter with natural cross long indined rockin. The upper part of the Dayton limestone for a few layers 1-5 ft tends to be thin bedded with layers 2 in deep with weathering clays between the layers = along the seams, horizontally. Which + after the age Laurel. Farm Pleasant Hill west beyond cemetery 1/4 mi. Try 1 actual Brassfield layer here along road = 8.70 ftns & s An old abandoned quarry occurs N Wth of the road about 3 mile. = Brassfield with flaggera lone struck eastward, toward the cemetery.

jackson quarry, 2 mi S of Crompton Euphemia bed. Schuchertella suifloma naturalize Whitfieldella nutdurate cc at tp. Strephella l.? to pant ammus duran. Brachypora like Riley form. Septaria thm ret data? Dalmantios Spinifer radiators Camarotoechia neglecta Platysiphonaria A aytrm annos for Athya anitherd anus The funnel-shaped twisted Lichenal Carycerimus sp. Cenocrasma valinthus New York Favosites small but cells large pores Dimor gusidli Laphroetma maganoso 2 mts. Journal of Geology. American J. of Science Torrey Bull. Ottawa Naturalist. National Geographic Mag. Science NEA 61 jackson quarry. 5 ft.+ Pentamurus at tp = Springfield but much bedded < Pant ammus cc. 8 1/4 ft Springfield well bedded < Pentamurus terrizon cc. 3 ft. Typical Springfield, 3/4 ft. More like bedded rock + Pentamurus cc [Euphemia typical folded = 6 1/2 ft. a little fractured] More less well bedded Euphemia = 2 1/2 ft. Lardell = 3 ft. (Ces good bedded clay rocks) 5 1/4 clay bryozo Daytn in 8 ft. P to Springfield tp opened up thru = 860 N S & S, No genuine Ce d ammus seen here. Rule quarry, S end of Crompton. Pike, Intervals about 12 ft not measured Thin bedded but not like Springfield, 8 3/4 ft. Massive blotchy l. 6 ft blotchy l. typical. Pentamurus ct various levels from top to bottom, 8 1/2 ft. Looks like trans ition rock at jackson quarry, below the typical Euphemia, but Pentamurus occurs 3 1/2 ft above base. 12 ft interval. < Base Gtymry = hard l. Crete level, 873 N S & S.

West Milton, West Ogiva - National park Indicated with S 80 E. 20 ft interval, 2 1/2 ft harder limestone than beneath. 3 1/2 ft softer cement, weathering clay. 4 1/2 ft whiter limestone Daym. 30 ft Brassfield, measured exact. South end of Ogiva, West Ridley River Step 48 - in chalk, Casparis Stone Co = Old Staller Stone quarry, 10 to 15 ft soft Ogiva indicated clay, 12-13 ft. Daym l. 853 ft USGS, tip of Brassfield. 22 ft Brassfield 5 ft of Belfast beneath - Ogira overlaid by scale corresponding to Laurel and this is real area by some Cephemia stuff but experience not good for measurements. The 2 ft of Brassfield above the Belfast part is sandy looking, The Belfast has much blue argillaceous as an actual through it and weathers to pieces; Below Belfast is soft blue clay of Eelhom member. Base of Belfast = 826 USGS. South end of Ogiva, bridge. Large granite with N & S Y bridge, Tip of Brassfield = about 855 USGS. 1/2 mi S E of Carstman NE of road crossing. 22 ft Brassfield = 22 ft actually measured, <870 x 84.8= line exact. 2 1/2 ft pseudo - Belfast see Ogiva section. From Carstman 1 mi S E, then 2 1/2 mi S = 1/2 mi S of corner 919. Brassfield, probably near top, at 910 USGS. 1/3 mi further S - Brassfield at 910 USGS 1/3 mi S note, NE of road corner 887, Brassfield base at 890, further exposed on former visit. From Carlesville 1 mi NW, then N along tracks. Brassfield with capped plate c at top of formation. Brassfield exposed as low as 886 Brassfield Daym in contact at 884 USGS Brassfield base estimated at 862 USGS about.

From Charlesville 1 mi W, then 2 mi N to NE side of abandoned house on side of road, = at abandoned quarry. Top of Springfield exposure: 925 ft. Springfield & ft exposed in quarries. Base of Springfield exposure: 917 ft NS& S. Thickness of Springfield Member: Not clear here mulletted and with Pont anemones. Looks like typical Springfield. From Charlesville 2 mi W, then N to quarry, 4 ft thin bedded l. < about 920 ft. 2ft 9 in, chestnut varnish beds- thin bedded. 3 ft 3 in, coarse bedded Pseudosiphonia < Pont anemones. 14 inches like pseudophemia- Paulmer? 10 ft well bedded l. < about 900 ft. About 21 ft of rock exposed Compare best with Judger Falls section. Judger Falls section: 3 Springfield with Pont anemones 5½ ft Emphemia typical ? 2¼ ft Pseudosiphonia 4¾ ft I would well bedded. As good. 65 At Charlesville, Brassfield is exposed at least up to 882 ft NS& S. Base of Brassfield in gully NE of station at 857 ft exact. True thickness of Brassfield - about 25 ft. Pauldr Belfant reported for about 2 ft below the Brassfield. One's Pauldr Belfant is in dominion. From Charlesville 1 mi S along rd to, Brassfield exposed at least as far up as 883 and the sandstone down behind the barn for at least 10 feet. The top part of exposure is believed to be within 5 feet of top of Brassfield or still closer to the top, - outside at top. From Offuscate City 2 mi S. Brassfield forms top of hill ridge & NE road cross and the top evidently reaches 900 NS& S, about 25 ft of Brassfield exposed here. Half a mile S in road from 919 Eastward, at corner of land, top of Brassfield rises to 904 NS& S. Glacial strike as indicated on map.

Nearly ½ mi's of road E from 919, near the house, top of Brassfield rises to at least 911 U.S.G. One mile S of road corner 919, and dear ½ mi SE of Ginghamsburg, the road falls going southward. Along the east branch, going south, Brassfield rises to at least 20 ft above the fork of the road = about 905 ft., not very exact since I do not know levely road forks. From Vandalia 1½ mi E, then 1 mi N to small stream. Top of Brassfield E of road = 905 U.S.G. Dayton here represented by about 7 feet of whitish thin bedded stuff, very thin bedded toward top and weathering spalling. Above this is 2 ft. of sparkling argillaceous indurated sand which may represent the base line. Of not, this 2 ft part is merely the top of the Dayton section. Sunderland Falls. Top of Brassfield = 906 exact. Brassfield at least 22 ft thick Road level. 7 ft interval. 920? 7 ft fairly well bedded L = Laurel? 3 or 4 ft argillaceous indurated sand, good, 7 or 8 ft of Dayton, some cracked at base, partly exposed toward top < 905? At least 15 ft. of Brassfield, none seen. -drawn sketch. 30-50 + North of Chambersburg 3 mi., E ½ mi. Top of actual exposure of Brassfield = 900 ft. but there is no actual contact with the Dayton line, nor on any of an exposure to be reasonably come of this day near the top of the Brassfield. From West Charleston N 3/4 mi., then W 3/4 mi. to Mt. Pleasant Cemetery. Top of Brassfield = 900 U.S.G. at least 18 ft. of Brassfield exposed at quarry. Top of probably 2-2½ ft or a little more. Base of Brassfield estimated at 850 about 3 Glacial till S 80 E 200 yds N school at end of West Charleston 2 chemic bank exposed 4 ft deep road level in telegraph post hole at 970

Bransfield exposed a little over half a mile West of center West Charleston, North A W Heyman at Atlas Cement Co. Planet m. 1 mi W to line flow. came leading N to lower. Bransfield 27 1/2 ft., th at 900 nsgs. Base exposed at old fall telom house, 873 NSGS appear ently. From Planet m. 1 mi S then 2 mi. Directly NE of road circa 915; Top of Brassfield exposure 900 ns gs exact. It may seem a little higher, but not much since the crystal plates with the [illegible] charac thetics of The Cadesville exposure is found here also. Also the Jadeian columns, at least 20 ft of Bransfield exposed line. From Planet m. 2 1/2 mi S, 1/2 mile then 4 mi NE, directly E of house. Large Bransfield exposure. West of Slimps Lime Kiln 2 mi Top of Brassfield. 905 NSGS exact. Slimp Lime Kiln quarry, Cedarville white limestone calcite. Platy was on a glance tall crystal crystal springfield from plastered, B Mandella like plain and red of Springfield. Half a mile S of Slimps Lime kiln. Bransfield exposed in road quite just S of lower lane, at 920 NSGS This is considerably higher than all of the exposures southward, and until northward near top. 4 1/5 mi S of Slimps Lime Kiln just NW of house. Bransfield up to top of hill which line reaches 910 NSGS, exposure continue north of house down to about 895 ns gs. One mi S of Slimps Lime Kiln new quarry opened NW by road opening 864, showing basal contact of Bransfield with lssender Belle font at 881 exact. Bransfield exposure 21 1/2 ft thick. While I did not find any actual spectral rocks here, numerous plates resembling the crystal plates at Cadesville occur here also as far as known latter.

Groups Lime Kiln, 1½ mi S, a little over 4 mi E, N to homey, then NE up shale gully, 22 ft above brice level = top of Brass field exposures = 922 ft = contact w/ Dayltm here at me. = ¼ mi NW by 955 on Brandt pike, From Andler Falls 4 mi S, 3½ mi E. Brassfield outcrops 10th road E of brice. On same road, just E of mine, road turns off S mile. Half a mile South on this road the Brassfield (Lyme joint?) is exposed near 880 ft. Three quarters of a mile farther S, ½ mi S of Corner 902, top of Brass- field is near 900 ft level. On National pike, about half way between Brassfield exposures (1 mi E of Tanglewood) and road corner 972 is rock which looks like jendo euphemia of Andler Falls section, near 935 ft. SW corner 972, about ½ mile, went old house now removed. Brassfield top = about 940 ac- cording to map. Apparently too high judging from other sections The Dayltm limestone once was married here. Chiefly thin and with clay between, except in lower 1 ft of section. Overal Dayltm section at least 1 ft thick. This is like the southern phase of the Dayltm seen NE & SE of Tandalia for miles. From road corner 972, 1½ mile east of Tanglewood, SE 1 mile, then east ⅓ mile to old mill. Brassfield - top of exposure at 910. Base probably somewhere near 895 - but neither top nor both my contacts are actually exposed. east of Speaker from ½ to ¾ mi. joint lutes strike Magazine ridge, looks like Dayltm. Rock is thickly jointed also on going down the hill eastward. West from Chambersburg 1½ mi. Then SW from corner 937. Dayltm limestone in vertical section of 15 ft, but slopes 8 miles = 10 ft perhaps. Thin bedded E. in clay between. Next page,

beads large cc, also Dufplein atn 2 in der Brass field with erinoid with Gyalophyllum lambe. 3ft Very whitish Brassfield resembling Dayland Typical Brassfield sparmular, tc. Cedarnille gr asly 1/2 mi West of RR station Road level x 4 gr ass. = 2 ft up, 20 ft = Brichy front for new Cedarnille. 16 1/2 ft < level front house, Water almost all drained out of quarry. Call reports described to me. Lichen pezoidinum printed axial like Brachyferin me a little more convex than mens uranis. Ret all corinus Barr andella-like species. Defet acanlum fridalis - small size 3/8 inch long, Spirifer moderately plicated longitudinal striae. Cyploceras moderately curved longitudinal striae rather fine, crossing annulations sharp and more distant. Orthoceras with more distant lugs; tendined strong striae used <915 with close but rather faint transverse striae. Gyalophyllid large + strongly flattened to my largest Steptoceras signiata. Fenestella archimedes-like from I multi Okamprose multi-fida but of medium size. Could just be celerity and I plus, all branches close together. Cyclonema sharp striae, high spine. Lithomaria - funnel-like. Ophaps my new species. Platyceras tall like figured Niagaran from. Not rare. Fenestella merrata Part amurus rare + in g medium size, It is the vertically fluted Cerithi-ceros that has the restricted top. Farnites small-celled species. Crawns (of one) Brangeri Halyn to xxno rare. Mytilus. Dolomunity Springfield type trilobita figured by me, Half a mile W of Cedarnille quarry then N to creek. We've bedded Cedarnille. 11 1/2 ft Springfield c. especially in th Conchania at base. 4 ft argillaceous + soft weathering = Ozford? 73

Chylen Below 2nd camp (Wiley camp) short dist. First camp is [illegible]. all following expressions are in Third camp = Bryan Park. Daytn L. 3 1/2 ft strata exposed. From [illegible] in 6 in, layer for 1ft, upper joint, for 2 feet, in 2-3 inch layers, with 2ft in intermediate layers. Resembling Daytn MEOSEY Vanuelia. Further W 4 ft J Daytn L. is exposed. Further W is 4 ft Daytn L. with Streptelasma large like those from Caprengix is ?) Further W is another gully. This is in chief part J Bryan Park. situate here. 5 1/2 ft Daytn L, 5 1/4 ft exposed, upper part thin headed. 4 1/2 ft whitish limestone, weathering brownish. Looks like Daytn but I am not certain. 3-4 inch layers, 1ft like that above but clay layers, about 3 inches thick, included in 2 ft like that above. My fossils. Fossils to come here for first time There are Bransfield fossils. 16 1/2 ft Bransfield exposed. Springfield, East Mills quarry. Springfields 15ft thicker. finest me quarries, Delamuelle springfeldensis Cimmeratocella neglecta. Whitfieldella ? short, rounded, Spirifera, many plications, 2 or 3 in fold strong growth variations (see this a Spiriferina?) Flaty cars on a massive crucible, tal. Certhureus strong rising annulations with lower vertical ridges as figured by McCheaney at end of Walden left 2 inches wide center .8 annulations in 3/4 inches. 7 vertical thirce or ridge in 2 1/6 inch width. Frgy 1 1/4 min N, on E+W strad east of road other fossils. Bransfield exposed at 945, but nothing higher known. Half a mile NE East locality NE of road, Bransfield exposed from 942 to 950 at least. Northing up in forthin seen,

Dunnsville. Brainfield base = 26 ft above road crossing at station on West Electric, Egrem. quarry S of West Electric St. Brainfield Base = 882 NGS. From Dunnsville village 3/4 mile then 1 1/2 miles to Jackson creek. Brainfield top at 925 and base estimated at 970, NGS. The top of Brainfield is difficult to distine guish from the Dayton since only the top layer is granular here and below the rock is finer grained. The only way I can tell is fairly exposed. The bottom 24 inches of the Dayton is rotten and not thick bedded. C & W'd drift immediately above. Dunnsville village S 1/5 mile. Top of Brainfield near 920. Dunnsville village at bend of road, south 1/2 mile. Large Brainfield exposure much disturbed - synagural fold and depressions. Lowest exp. sures about .890 as mean as (can be estimated) Snyderville, N.J. Railroad. Top of Brainfield '895. Base calculated at 870 a little bs. Brainfield also along RR track east by RR crossing. S W of Snyderville 1/2 mile, n road to corner 982. Springfield section at 950 and below with gradual strike S 45 E, Egrem village, 1 mi E, south 1/4 mile, Springfield & walking Cedarville appear as two quarries. Egrem village. Wells in village go so to 16 ft through gravel to get water, therefore no Brainfield here. Byram 1 mi E 1 mi SE. More Dinnercinos Platystrophiia reverenda many ples Cations on fold. Cysted bedded shales. Clothogena phaeo chint menas Strong drift south in smiths mead. Byram 1 mi E, 1/5 mi SW, 1 1/2 mi E, south east of road corner. Top of Brainfield = 970 - 975 Dinnercinos. Smith last trench 1/4 mi', Top of Brainfield at least 1/4 to 965 Dinnercinos good.

Bypm 3 1/2 mi due east, 1/3 mi EY corner 994, Top of Brassfield about 970 Tractin corner EY 988. 1 2/5 mi NEy Goes station. Spring Weld with Pentamerus. 8 1/2 ft Amphermus, typical < 950 11 ft interval. Junction crossing. Top of Brassfield estimated at 917 SE corner Yellow Spring where grad goes E down hill between 3/4 miles to creek and. Brassfield top 5 ft below road corner, somewhere between 900 and 910 as near as can be estimated. Clayton, Wiley Park = 3/5 mi SE of village, where road turns Ws Road corner. 980 27 ft Cedar mill canyon. 56 ft J. Island; 13 ft Brassfield rock. No very Crinoidal parts. Mistypne 1 mi NE at Croiled Dimerocrinus atumcrab, cystid plate with ectostichmmb. Dimerocrinus Brassfield top at 940 Vanceburg. Murro exposed about 20 sq. miles down river from depot Street. Rock much pressure brecciated, and cherty, About 5 1/2 ft exposed but looks thicker since it stands parallel to river bank and dips inward river. Three laminated layers, a small rag unlayerly deposition which maybe alga, Today unknown Spherospira. Thin shale films intervene between some of the laminates. The Murro out crops gently north of Salt Lick creek, at the down river end of Vanceburg, It continues down the arm from this creek still striking parallel to the stream and dipping at least 10 de grees toward the river. Have some of the Murro Conyers have a "sm cracked

This rock angle or headland 1 mile below them - Big Bank and Deep Water. M curve = 15 ft exposed, and no question why a cement durable thickness is left below water level. Vanceburg ferry landing, M curve 17 ft thick line, nearly horizontal. Going up stream, the brecciated appearance is common again, especially in certain layers, while in the bedded rocks lack the brecciation. Why? Large chert masses, like concrete, about 3 x 4 x 3 ft in different diameters, some in place & one from loose. These large concrete massy masses are especi ally abundant at my first on about 8 feet below the top of the M curve. A quarter of a mile up stream from the ferry landing there is a continuous chert layer in the M curve, from 2 to 3 feet thick, about 4½ feet below the top of the M curve. Could the growth of these cherts have been the cause of the brecciation? Going up stream, the top of the M curve slowly approaches river level, at the upper landing for boats at the upper end of Vanceburg the top of the M curve is 15 ft above river level. Apparently different sets from the top of the M curve at different places. Three quarters up stream meeting three fourths down stream. No exposure up river from this land- ing in the river edge beyond ½ mile. Sandy Springs, opposite Vanceburg, along river road to Gilpin Run. No exposures, just NW of Gilpin Run Bench Mark, 579 ft above sea. Bench Mark, Black shale is exposed as low as 575 US GS. This is not the face of the Black shale. Little Sulphur Creek, crossing. Sully crossing. Black shale < 540 US GS. 6½ ft blue clay shale with thin black shale at couple levels. 1 inch very lithuminous lens - tree trunk 4 inches 1½ ft black shale interbedded in blue clay shale 2 ft blue clay shale. < 530 Sulphur Creek, just S of road crossing, Top of M curve = 495 exact. Strike almost N+S, Dip rather steep easter at least 10 degrees. A short distance up the creek, at school, the thick greenish clay shale section

near the crest of the Olive Black Shale is exposed, where the black shale entering large concretary masses three feet in diameter, about 15ft above its base, and also about 35 feet above its base, our their level measured. The Clent Rugby appears to be at 520 so near as can be guessed from the contour lines. 3/4 mi SE of Wykoff creek. road level. 37 feet interval. +91 USGS < 26ft above low water in 'Electricity' Brecciated West Union with Ormond Stones, Cladophora, small celled Farnito or Lily bed type, small ascentured Concretes like that already collected by me from Wells Over area. 1/2 mi SE of Wykoff creek. West Union apparently, about 545 is top of exposure along road. Rock not identified with certainty but appears too sandy for Marine. Analysis rock not seen. 2/5 mi SE of Wykoff creek. < 550 almost. Brecciated West Union with small celled Concretes + Stromatoloid masses. 1/8 mi SE of Wykoff creek. Top of West Union as far as exposed, 17 ft above road level = near 560. Immediately NE of Wykoff creek crossing, Rock which I called West Union 22ft thick, and overlaid something sandy (must be "mud" of Beetham area. NW of house immediately out of gate, with creek crossing 570 about 46 feet of West Union with top exposed. Shale Point SE end of Vance Bridge 10ft + S mudding shale. Top not seen. 16 1/2 Berea {34 ft Bedford shale} 107+20ft 2 ampt me. {53 ft Bedford shale,} 292 Top of Ohio shale 2-1/2 ft above R & level Lower part of Olive Black Shale 50 ft below R & Level Top of black mud here = 18 ft. Low water in Clent River.

South J Carr's station. m'th'd going to Martine. Black shale, but not the base. No expense for considerable interval. 5 ½ ft harder argillaceous rock, 20 ft shaly stuff, weathering soft, 16 ½ ft Massive L. thin shale, first cliff forming. 22ft chiefly massive trumitl. intruded with a little shale. Grey chalk and white sand layers 1-2 inches thick interbedded. Martins Lirca by some chitin? atypa petularis Chonetes murrae artica Bryozoa trilimata, quadri? Ostrea brisa, Crab chalk and flints for a long distance in taly, but original horizon for half within 30 ft of tops. Can't varied fauna requiring much collecting. Martins - North Novy 2 2R 5 ½ ft hard limestone (weathering) 5 ½ ft clay argillaceous rock 8ft hard iron-studded L. 4 ½ ft pure white limestone. 30 ft granular & t from feldspar only? 12 ½ ft silty flintiferous 11ft West Kinnin. B ase as far as Kennon. 28 ft in terrace, supposed to be Crutcher's Highest horizon. I get out back yard exposures and here full of characteristic fossils. J P J Scott. 6 ½ ft Chlor shale 1 ¾ ft Binnish phyllaceous rock. 13 ft White chalk shale 14ft hard rock like Dorrien boggs 14 ft argillaceous rock. 22 ½ ft Black shale, chlor. > R. District No 4 School house. Quicks Run. 65 ½ 79 11 9 11ft greenish shale - Glentany? C ¾ ft white L. fully concrete margalimestones 68 ft upper half weathering soft & sandy (Lower half massive limestone) 2ft full fl pebbles as at Martins. 9 ft met ma'm, 2 andy limed m. The Glentany is overlaid by Black shale further up. Hill N of Grad about 200 yds E J School, about 6 mn from Conelurg.

North of Amick's Run is 3½ mi from Vanceburg. Martins is 10 miles from Vanceburg. Where road turns off to Carr is 8 miles from Vanceburg. Rome sheet crossing = 60 ft above present river level = 525-60 = 465=river level at present. Low water is about 2 or 3 feet lower. Run, 3½ mi N, then up East Fork ¾ mi on Norrisdy Creek; opposite house on SE side. West Union in situ. First seen in Creek bed but where West Union it comes in is unknown. 675 shut. 1 mile up East Fork, several hundred yards NE of last house on Norrisdy creek, up stream climb in map. Black shale at 730 but Clinton age not exposed here. SW of last house in SE side, East Fork a little down creek from last house West Union up to 712. or 12 ft above The level of the house here meantime. Top of Clintonage + Black shale contact at. 735 ft. Clintonage face at 725 or below. 87 House ½ mi up East Fork, on Norrisdy creek. West Union base & outcrops extend exposed opposite house on SE side, creek about 14 feet above house line = 674 ft approx. but union estimated at 50 ft at least partly should be much thicker, owing to eastward dip of strike line. Pantony, up west branch of Stut creek a little over 1 mile, Since gained West Union at 640 about. Came way up west branch of Stut creek 1¼ mi. My house in Whiteforkal 8 ft Clintonage greenish shale <753 25 ft in total. <728 38½ ft. West Union top. House 1½ mi from Pantonyville up west branch. If I have gained whited creek which way be Monroe, about 20 put below house where road turns off NW from creek up hill. Top of Monroe? Here = 745 about. Pantonyville, up south branch Blue Creek was exactly 1 mile. West Union in creek bed at 620 about. Massive West Union at 640 at 1¼ mi N of Pantony.

Read corner 660, 1/4 mi NE Punt Turn up Blue creek road branch. Above this everything is uncertain. Ride extends up to 1002, at least. West Union, schistoidal appearance; up to 993 of act. Discard for next measurement in mapping. From Road Corner 660 measured northward along the road. 1/4 mi West Union up to 685. Hillsboro sandstone 2 ft. Invert Black shale = 717 about. Silent augy, 1 c considerable thickness but not measured nor its exact place in levels determined, 2 mi. NE Puntarmville, at West y ridge. 65 ft below crest (1115) is barely showing apparently but the exposure is very fair. On N side of ridge the Silurian shale base is shown in contact with Berea sandstone 50 ft below 1115 or 1065 USGS, Blue Creek, 1 mi W y, NE road co mer 666. Top of whitish apt l. crumbling as though it would make suml= 659 USGS exam 89 Blue Creek, 3/4 mi W y, where road starts across creek at road corner 65-3. Thin bedded shist met in creek at 645, Blue Creek. No Silent augy exposed. Black slate lies down to creek level. Russell Fork (Wny River) 3/4 mi SE y junction with Waggoner Run road (790) opposite second house on White road, 687 face of massive West Union exposure cat each end out all. Russell Fork, opposite 1st house on White y road. SE y Waggoner road junction. excellent West Union-Black Limestone junction at about 690 to 695. Waggoner + Russell creek junction W of River? 1 ft thick. Top of West Union 825 West side of intercp is faults and on East side of fault is upper mud. NE of Waggoner-Russell Road Junction. Top of measure? 810 about. Measure? 4 ft? May equal 15 ft. Can't distinguish River in th certainty,

Further N of Magorner Riffle end, is Hillstor sandstone. 1ft thick, in purplish but my hand blurs it. Hillstor sandstone width is at least 10 ft of Elliot away, Hillstor as level as about 870, This is a throw of at least 45 ft at the fault mentioned in preceding page. Road junction 808, 3/4 mi SWY Dulip. At first house SE W road, SW W road junction = West Union real top = 820 as near as can be deter- mined from contour lines. From same road junction 806 north 1/4 mi, in hollow, West Union real top at about 820. From same road corner 808, south 7/8 mile, S of Middle Beach. Top of West Union trail = 810 at mt. From road junction with Black Rim road (840 it seems) Top of trail Union trail up to 835, English West Union top good. Magorner road junction here is exposed between 840 and 845, but nearly crushed by faulting S with Chester West road junction (840 approx) Ie end, east of place where road is suggested as running but mean two houses. Top of West Union with Dalgites mix us = 862 apparently as well as can be determined from contour lines. At steep Sandy road S, from top trail, - Wards, so. 20 ft. This Wards may have slipped down the hill and then may be our fault of large portion town. Wards = once West Union! One mile up Black Riffle road corner 571, at second house south of road running up south is main fork of Black Rim is top of Daffy at 610 as near as can be determined from contour lines. N E W road corner 571, turn off N E from Black Rim road 82 West Union trail 16 ft. Offprint seen <860> West Union me 66 ft to west bridge road or at Richard 185 ft. <794> Top of Daffy m 49 ft above junction 571 = 620. Lower part of West Union resembles Wards see former section on this page. 620 185 86 571

Day in about 4ft thick. Several nipple marked L layers with much clay between, the latter faded minimating - Total 11ft. 1 4/7 c, like Day m. 2 3/4 ft chuffy clay. 1 1/4 min'n'dal. 2 3/4 ft chuffy clay. 1 1/4 'min'dall 11 1/4 ft chuffy clay + 4/5 ferruginous limestone 7 2/7 incl continuous c. But real not measured. Top of Belfast is at about 563, therefore Bransfield is about 52 feet thick. Top of [illegible] hill 1/2 mi SWy Me & gozney school, Waid of Bondary valley 10 2/7 incl. Incl'd by Sladeholi. Residual red mineral. 16 3/4 ft interval. Top of Large West Union L exposure 164 in total. West Union - G at Archard cmt. 930? - 180 = 850 for base of this section 800 - 616 = 184 for that chalk estimate Top of Day m = 46 ft above when ferruginous start off NW toward little house up hill. 670 + 46 = 616 last measured. German church section up Town Sister Road, 1st street part I built 27 2/7 in total, 10 3/7 street part I road, 18 2/7 ft interval Lowest actual Blackshale exposure 28 2/7 in total. German church. 11 2/7 ft interval. 1 junction section Minnie? 17 2/7 White L like that at top of Waggyma Waggy Road junction yealdes, clearly by I West Union section at 46 3/7 in total, with c, at top like that level 1 2nd house NW side J road 22 2/7 Masonic West Union. 2 2/7 Whitefieldella cc Diaphoritesma. 5 2/7 ft West union. Actual exposure. --- At first little bank NW of Germany church the people had fitted limestone at top, I section recurs 11 3/4 ft close level at German church. --- The same dampish rock recurs in lowest sag J road beyond second little kerb, at approximately 925. Black slate on the 3rd bank. At house 3/8 son NW of Germany church Top of clinton gy stuff about 20 ft below top of hill will black shale at least 10 ft lower,

Neshitt school. about 950 My section of school under 2 ft thick. Purple shal l, at top of section. 32 ft in turnel. Marl soft, much crushed. 11ft white l., Frimerella 2 small speds. 42ft natural chiefly white l. 77 ft of massive West Wm's. Maple frt on Orchard contact at large but nearly dry fall. Actual black shale in fault N of Neshitt school, about 950-965 Beyond 2 houses in windy creek, 1/2 mi N of my Yick school. 2 mi E of Rm alms Black shale 22 ft clean argy chiefly. < 600 about. 22 ft in turnel West Wm's. creek level. Half way to next house on right, at about 600. West Wmuri creeks bed. strong Shanna Top white cc. Farmites small called. West of Blue Creek 13/5 miles and Turn off N up Randall's Rim, 1/2 mi N by road junction at 720, top reach in the creek, Top of West Wm & I see it cleanly at 685 foot at top of this exposure is purpled. 1 ft thick, 95 Bielmo white l. 2 ft thick, in th large gastropods common, includ my large Paroy Sharp mollus. Phaeocentruma residens, etc. The gastropod zone of W. Wm apparents. Apparently Megaloma scens here large! 33 ft internal. Redden l. zone in th Shanna top rim & Outcree. There evidently is no Marie here. Second house up Randall's Rim, definite R in Rim m my, Black shale contact. Top of West Wm at 728 exact, about 2 ft of white l. purpled fused at top, same as th at contacting large gastropod form in last section. 13/4 mi by Randall's Rim, 8 of 780 road clear. Black shale - West Wm contact at 745 exact, Wt 2 or each of me only 1/2 mi N. near home on right. Top of West Wm 782 at least. Contact not seen but must be near here.

From Cedar Mills 3 mi SW, and then 3/4 mi S to projecting tongue of land. Tp of West Union exposed repeatedly at about 780 in the road. Cremites with small and dirty root specks, as at Hillstown Small celled Favosites. 1/2 mi N of 943 crest, at house in tongue of land, Tp of West Union at 800 about. Small celled Favosites. Crossed by 20 ft s which greenish a light colored slent angry shales. Fired animate whole hander light colored shales continue for 5 ft quite. At house 1/4 mi's the slent angry appears to show up at correct part of road 7/8 mi N by Mill creek spike, on same road as before. Tp of West Union, as far as exposed, is at 790 about, 5/8 mi S of Mill creek road, means road as before, 1/2 of 2nd house in way down. 1-5 ft Celluarangy. 2 ft Hillsb'wn sandstone. 770 ft US G S. Tp of West Union, From mouth of Bates Run take road straight south from Mill's creek spike. Tp of West Union - 770. Tp 1/2 pt my hard L, containing in large Megalodons, large gastern ports including large Strapartlia of Hillstown area. Between 4 and 5 feet below top, I West Union a large Trimerella to chum m. Also small celled Favosites, large gastropods, West Union covered by 22 ft of clut angry. On same road S of mouth of Bates Run, 5 from Mill creek road, 1/2 mile, just N by 766 and junction, Tp of West Union - 775 accurate. Blue creek Rd, 2 mi W then 1/2 mi SW. Tp of West Union at 705. Clent angry. Cladofna, Helyites nexus, the large strapartlia like shell found at Hill- town. Other large gastropods, evidently the large gastropod family of Hilltown. Mill creek road, west of mouth of Middle creek 3 mile, Tp of junction West Union - clut angry contact at 745 about, - east of first house and I word UNION on map,

Mill Creek road 4 mi E of junction Bates Run, 20 ft of St Matthew's level. West Unin exposed between road level (~724) and 744 dep'ty. Favonite b'l'aster from Plymley. Heta cuneata, st. mathypula etc, Road going S from WJ with J Bates Run, near house 3/4 mi S of Mill Creek road. West Unin mines to 780 according to the contour lines. 1 1/2 mi's at Ellis Run crossing, excell West Unin - Offensine' at 695 down to creek level, South of Ellis Run 4 mi, tip of West Unin mines at least up in 765, with black shale debris over it. at Hamilton School corner, the tip of the West Unin is below 780 since clentangy shows up here. It probably is near 770. West of Hamilton school road junction 3/4 mi E of 776 road corner, West Unin clentangy junction = 792 exact. Crossroad 3/4 mi S W J Lynx. West Unin at all high points in road thus far since last break described. That means at least to 800 and probably 810 ft. Ellis Run school, 40 mi NE. Tip of West Unin at 873 as near as can be told from contour lines alone. Ellis Run school, 4 mi SW road junction 870. Clentangy - West Unin contact at 882 exact. Large gastropoda. G. W. i'phara? excellent internal casts of M. murella. Lynx, 3/5 mi W, 1/2 mi S 1/2 mi W road. Clentangy - West Unin contact at about 870, Lynx, 1/2 mi W at 8415 corner, store. Highest stratumiferous West Unin at 840. Tip of gastropod layer estimated at 845. Clentangy seen about 850, Large gastropoda horizon with good specimens, hard white l, 2 ft thick containing numerous stromata? or 'os' + small called Favonite. Also small convex Trimerella like that from Germany church but 1 mile

From Lynx 3/5 mi W then N to humer, Oletrangy = 22 ft greenish shale. Oletrangy - West Min on North at at about 845. Gastropods in very hard white limestone. Buzz and Rust Rock road from Brink creek side, Lowest West Min seen actually was 110 ft above humer, 760+110= 870 ft. Highest Catbschard seen actually at sharp bend in road = about 810 ft. One end not between the Brink Rock & West Min probably is near 820 I think. From Wrightsville top of hill at 989cm. Here West Min = 125 ft thick up to this corner. One mile east of this 989 cm, at hill E of 954 the West Min is exposed up to 960, 3/4 mi SE of 954 the Hills hor ss is exposed at 960. SE of 925, Hills hor ss is seen at 970. 3/4 mi S E of 954 the furze hill ridge forming top of West Min is seen at 970 about. The next full E end aims Black Slate at 980 NW of Nashim School, 101 West Min in, east bed of turn, SE by minumment at corner 981, top of highest exposure of West Min = 987 exact, and no stratum above this line, or abundant fossils, but Chas. Space. Rock is highly mineralized in some layers directly S and SW of min- ument in open fields, at about 960 to 970, with Schmidtelle, Brachyura, Ostia reticularis, Septaria, Dolomiale, Dolomite, Calymere, Spirifer with radiate striations and fairly stiff folds, paddle shaped spines of? Ormond Leda. I don't know to what genus they belong. Also the spirifer with moderate fold g small size figured from West Min bed. Correlates with our all species, Oligodonta to Emmata. Base of West Min at least as low as 920. This gives a minimum thickness of 987 - 920 = 67 ft. One hp locality is 1/2 mile east of latter locality, making allowance for eastward dip the maximum thickness of West Min at West Min in is 67 + 8 = 75 ft. Could not be over 82 ft.

The Lynn expressive veins at beginning of Bearly Fork road. Here the double pored plates of a cepid occur in the Lynn Whisfieldella horizon. Like the double pores of the Tetragysts of the Ceyrood beds. Also Delman as at Martins, Bogdyspm and Martins. Spirifer radiate striate no folds except median fold & sinnes, Common Species. Phynchistia conneata, Leptaena, Hmold antra, Spirifera magensis like that at Danville, Large Staphimella as seen Birhus dam, large Philipimella (amargiacardinella), Camantracite with 3 plications in airums neglecta type, Otyga vitulans. A large Hmerland pygocidum at least 2 inches wide. Clathrypna pseudra, good specimen but cells poor of cast only. Spirifer magarensis type. Excrimura pygid Diaphanostoma magnafalunus, small st source specimens. Spirifera antle lode of Jeddide where its straight not curved. Conulits large. Ceramus magarensis. 4ft below the heavy Belfast (1#) layer is a thin layer exactly like the Belfast, containing Fungula and graptolites. femissing Cedar Mills. Draft out type 550 Brassfield, upper, Ontarian Gathiphyllum Lankei, Olitzophyle Draftmensi, Left side D shumwell &, Philotrja parallel sides. Phthyfera East y CedarMills. B suff zestria With Mu'm 1ft rather hard, whitish. 25 ft soft weathering marl containing Halysite, Dimorphyridec, Favrite. 32 ft weathering shale. 2ft permimus massive limest m. 45 ft massive limestone. Ct wt lrichard 3/4mi E y Cedar Mills. Olentangy base - west New tp, same where near 780. with yard C MeI 792 Olentangy West Mu'm cut out at 760 exact. Olentangy 22 ft thick. 2 mi E y Cedar Mills, at 743 grad CMei. Arg hard 1ft dark limestone occurs near base of Olentangy, but is mudaid by Black shale. Base of Olentangy estimated here at 740 but was not seen. Olentangy continues to show above rock level as far as Deep Run.

From Hunt Hollow NW to White Oak school, 1/4 mi NW of White Oak school, belonging to Honey depression in SE side, and tip of West Main in NW sided hollow, Contact at 739. Tip of West Main in the Stonemats? wilds cc, and a few gasteroids. The tip is [illegible], but not. Stonemats reaches as just stated, immediately N of 733 road junction then, the tip of West Main is at 739. This probably to the contact foliation although no clear Glentany was seen above there. North higher section. Before reaching first house NW 733 on next side of road, the tip of West Main is seen at 760 about or 755. N of road junction 765 the trace Glentany runs as far as 755 at least. S of first house N of 765, at 765 about, the tip of West Main is seen with actual contact with Glentany above. East of road corner 1/2 mile NW of 765. West Main Glentany contact at 770. West Main tip is whitish land, At first house N of road crossing there is a strong east dip of the West Main N of road corner 775, New tip of West Main is at 775+15 = 790 exact. The Glentany shows up clear and up the other road, 1/8 mi SE of Scout Ridge, Glentany - West Main contact near 845-30 = 815 Scout Ridge is estimated at 865. Black Shale and Glentany exposed NP go low as 865-40 = 825 ft. But trace not seen here. Probably dropped at base. See next section. West of Scout Ridge. Glentany - West Main contact good at 820+28 = 848 exact. Farrellt 1/4 mi E, 1/8 mi SE, N of Glenne. Tip of West Main at 825 about, Glentany exposed 1697 lighter, 1/4 mi N of 867, at first house NW road Tip of West Main 860-30 = 830 exact. Tip of West Main - very hard white limestone as in southern Adams Co with large stromatoporoids, small celled Farmeria, the large West Main stroma hollows, large Thamnella, large Megalinos, large gastropods at 830, but Main tip at 825 about

Turn E at 830, 1/2 mile to 819, then just SE 1/2 house Glenangy remns as Corner 820. 3/4 mi E y 830 Corner, is 826 Corn. Here Glenangy seems down to 796 at least. Along another road, SW of 826 Corner, top of very white + hard West Union is at 798 ex act. Section N of Cedar Mills 164. More massive l + strata parallel. R 33 ft chuffy gray but with l. int bedded, with stratification & arnite clay. B 55 ft m mass R. Base of West Union, 680 about. 35 ft. < 645 about. Cedar School. 1/4 mile N. West Union exposed by toll. The Wupa exposures at West Union with crystallal beds, then, along my new sandy beds, probably comes fenced to part R of Cedar Mills section. & to the Wupa heart y B. From Scrut Ridge N to 849 corner, then SE. West Union exposed up to top of land here = 860. This probably breaks in at the top of the West Union line, Scrub Ridge 1/8 mi, then E y 845 Top of West Union, darker junction = 834 with Glenangy immediately above. 1/4 mi E y 845 Corner, white hard top of West Union green 830 & 835 I think. Glenangy above. Diedly in front of house 1/4 mi E of 845, along Road is much hard white l, with large str ups on rolls of Hillston type. Highlignite carbonates small cells, Farnite. At the house this white rock appears now laid banded rock, whitish, with not fossils up to 830 Scrub Ridge is mi N to 845, then exactly 1/2 mi E to corner 807. Top of limestone at 787 with Glenangy above. One injfer 10 feet of this lowest mi is formed in thin laminiae, but not far now can think to be of Monroe age. E y 807 1/2 mi, where road turns NE Glenangy < 785 2 ft very white hard rock. 24 ft. Massive l in good layers Stratified w & c.

807. East 3/8 mile, at south end of his Turn in road, Clent argy limestone at 800- 755 exact as far as can be judged from contour lines. At hill above the letter r in Turkey the limestone is seen at this road mile, at 750 about. Top of limb of line not exposed here. At road center 735, above y in Turkey, Clent argy limestone contact at 735 + 1/8 = 753 exact. At road center 712, 1 mile west of Mineral Spring road, Clent argy limestone contact at 712 + 8 exact = 720 exact. Pink color laminated. Probably marble. No fossils. Down 35 ft from here to mile of last locality. West of Mineral Spring Road 3/4 mi Clent argy limestone (dunare?) Contact at 720 or a little below, Mineral Springs hotel, 1/2 mi then W of creek. Black shale down to creek level, Along Turkey Creek just, 1/2 mi W of Mineral Spring Road, Black shale down to road level which has gone down to 680 ft. On face the Clent argy should be still lower but is not exposed. West Minm Dike. Beverly Fork. Wjper West Verm, interbedded crinoidal layers in so far as West Verm, East rimmed. Crinoid head. 5 joints radius, Silmuchistella about but broad - form Crinum also in Lawn West Verm, has crinum at West Verm after injection by S joints and a slightly the last more of my calculated occurrence. S that I am small, Peteforia, Forestella. This type crinoidal horizon dominates 30 ft below the top of the West Verm exposed at least and 1 West Verm. This is about 45 feet above base of West Verm here. Lower West Verm, at West Verm Beachyptin with ventral valve depressed slightly certainly, Gyrolapis. Eucema pycidiom Petopora Amplata. Diaphorina a jura's brood. Ridged fossil bed with from laminae. Delament it is between 18 + 20 ft down line of quarry 109

Beetles 8,20am (35) [illegible] 4,25 pm ? 10,05 am stop anywhere east 8.30 PM stop anywhere east Beetles, Linn road until led in gravelly 1/2 mile W of turn. Blacyleptus Crematogaster Dalmanites typical Billings from Dalmarea Elle Whitefeldella Rhyphocheta connecta Spinipalmarium, short bridge Sclerostella case Hillerton Brachyferm very fine thin depressed materially Camponotus neglecta Diaphoristana infugmens Platycerus anagyrus Hornhambros head. Neburella. At the top of the gravelly the centralised ridge cuts across the flat central ledge aspendage seen in upper beds at West Vm III Beetles SW 1/4 mi, then 13mi E, then S 3/4 mi, then E from 843, 1/2 mile, Green Clay from Clentangy shale first seen at 890, with black shale further up the hill. No stratum more km. From corner 843 a little over a mile & then spinulae smithi. Black shale time at 8181/2, from Gutter lines, 7ft thick when 3 ft hard white b. Black shale 5ft thinbedded li apparently with Lepidodina 6 ft. limestone layers like that below <800 10 ft interval. li in layers as far as seen coal abundant. The contact between Marse and Kent White not determined with exactness. 1/2 mile NE of whether last road turned off still, where house is on N side of road, at sharp angle in road. Clentangy well expressed. 825 exact 2ft Thiel with Lepidodinae. 141 very hard white b. or fossils. Course to nearly massive Carboniferous. Feel off in layers. On closer examination this hard layer is seen to be made up of thin layers even as far as the carbonaceous are concerned, which may be due to concretions my growth on altering the thin layers bridge.

1/4 mile E of last locality where line turns off R. Elktr ugly - Monore contact at 800 exact. B Oara Pmd, 1/3 mi N to corner 719. Elkt an gy Monore contact at 714 exact. From corner 719 about 2 mi SW, Elktr ugly - Monore approxmtg at 760 as near as c an be told from cont mt lines, From corner 719 about 1/2 mi SW, to the road turns south, Elkt an gy - Monore contact at 745 exact, judging from cont mt line From corner 719 nearly 1 mi SW + just bfore reaching Elktrl at road junction. No limit lne seen but only shale trace in road. From corner 719, about 1 mi SW and to another road junction, at school. Then westward angling a cross creeke to 750+70=790 ft Elkt an gy Monore contacts Rocks dip steep east here at 772 corner Blackshale turns up, then east, in east side of creek Elktr ugly appears to rise steeply west ward. At Minnual Spring a well went down 132 ft with no getting through the (Elkt?) Black Shale. From Minnual Spring about 1 mi NW across the bridge, on its east side.<1080. 30 ft Redynd ss. 94 ft. Bedfordshale+ thin sandstne (Elktr) Black Shale. There is a strong east slope line for striking exposed clefts spot of Monro other 1080, strong edge road, at least so far as first hill top. =1200. Returning from Minnual Spring, I came around as before NW, as far as 772, then west 3 mi to road & creek, then SW about 1/2 mi where went out 800 crossroad twice. Elkt an gy Monore contact at 809 as exact as c an be determined from cont mt lines Only upper 2ft of it we broke the lmonorated like the Helmarre. Are lower part is massive whitish, I am not any looking but may be Monore. I can not tell it apart from the West Minr Stramat formoid layers

being W a line is marked on map in grid quad. Alent angy - More contact at 820 about. 3/4 mi massive rock b/t below Alent angy. Here I found glens with although rock was a rock eroded and ornamented during. Rock remains massive from to creek level N me of the rock can be identified with certainty as West Union. At 926, the high gradient along the road, the top of the black shale + base of the Bedford shale appear to be exposed, but the Bedford shale may have slumped. 3/4 mi E of corner 827. Alent angy - More contact at 870 as near as can be judged from contour lines. 1/2 ami E of corner 827, at highest road level = about 875, very hard white l. with Monomville small tuff: Ogenosity low, and numerous large gast eruptions. = top of Chinotone line and in depths West Union with Alent angy immediately above. Steam Furnace School 1mi W to 845 corner then 3/4 mi S E Alent angy - West Union contact at 900-25 = 875, judging from contour lines. Steam Furnace School south to corner 804, 1/2 mile south of 804 lane leads off east. Highest West Union road creek seen at about 840, Fig 9 West Union unknown. Steam Furnace school south to corners 804 and 846, Highest west Union seen just N of 846 at about 870. Fig unkown 870 or 880 Steam Furnace south to 846 corner, then south 1/8 mile and North up lane east 1 jukes. West Union at angle where road turns east up to 880. Top unknown. Then north east anything 1/2 mile to corner. Bedford bridge thickness is assumed to be 910. Given part of Alent angy at least as low as 910-50 = 860, with base of Alentangy unknown. Continue on road NE, E, and SE to lone house NE of road crossing in valley.

Cleet angry - West Min'm contact seen at 820 +15 = 835 judging from contn'd lines. Steam Furnace School 1 7/8 mi South of 826 Cmn. 3/8 mi SE of 826 Cleet angry as far as low as 890 - 10 = 880, B are unknown. at highest I and 3/8 mi SE of 826 Cmn. Highest Cleet angry = about 895 - = 890 with 15 ft of Cleet angry below and some Cleet angry calculated at 890 - 25 = 865 or 730 about. From road corner 826 SE 3/4 mi West Min'm at 860 full of large stratay deposits & small celled ferrites. From 826 road corner SE 1 mile, at house on N side of road, West Min'm at least up to line level at 850. Op I West Min'm unknown. 2/4 mi SE of Steam Furnace School, cmnt of corner 745, up road. 745 + 52 = 797 = Cleet angry - Min'm Min're with superdition at top. Total thickness possibly 18 ft. I had station 40 mi W and then 10 mi SW to bridge. Cleet angry - Min're contact at 627 exact at Jaybird RR station the level is 629 and the Cleet angry - Min're contact is about 631 line. Jaybird Sta, 5/8 mi NW to road junc- tion 645 Min're at least as high as 655 but no contact with Cleet angry seen. Jaybird sta, 5/8 mi NW then SE of 645 Cmn 1/4 mi. Highest Min're exposed = 640. Op unknown. From last locality 3/4 mi SE to lane to a house. SW in lane about RR track track. Min're exposed to 10 ft above creek - 610 + 10 = about 620, at the 2 lanes 5/8 mi further SE my mind is exposed along the creek. Pebbles E to Buena Flat School, SE to cedar Fork, Rem E from fork roads = 1 mi N of Beam Pond. Cleet angry - Min're contact = 700 ft as near as can be told from contour lines.

No exposures along road going down east side of Pine Gap. Opposite letter S in Scitra First Monree I exposure going east along Scitra Bank road is at first house on Smiths creek road, about 1/2 mi SE corner 683. Monree at 670. Partially near top of Monree but Clentcangy contacts not seen here. Opposite letter O in Scitra. Highest Monree seen 1 1/4 mi NW corner 645 at Scitra Branch creek bridge, is seen at 660. Probably near top of Monree. 1 3/4 mi SW Scitra Branch creekpike up Poted Hollow bycellent Clentcangy - Monree contact at about 695 quite a contact. Top of Monree wind contacted by pressure also pressure dissociated locally, as clearly as at Vanceburg. Peebles, m old State road, to fork with Pine Gap road, 2 mi NE of Peebles. Top of Monree at 850, at least 40 ft of Monree exposed, Base not determined. System is at top bottom. 1/4 mi W of Bachm Flat school across On highest land is Monree at 810, top of Monree unknown since the rocky ridge is eroded. Exposure in room at least 20 ft lowa still lower looks not exposed. Bachm Flat School, 1/2 mi SE, at road angle. Highest limit me exposed at 760. Higher points eroded. From last road angle NE's mi. Rock dips NNW distinctly. at 760 about. No exposures between last locality and house 1/2 mi NW of Cedar Fork bridge on S sidey road. Monree top at 735 about. Cracking Clentcangy not exposed. Therefore top of Monree is assumed. Up the next rise I land and eastward there is no work exposure nuite near Cedar Fork Bridge. This suggest to me that the high rock exposures from 3/4 mi W of Bachm Flat school east to Cedar Fork bridge all are on the top of the Monree with Clentcangy and Chir Blam shale at duced to red clay. Black Hollow School, 1/2 mi SE, just beyond house on N side of road. Clentcangy - Monree contact at 680 exact,

Black Hollow School corner. Excellent Alentany-Minore contact at 706 exact, apparently guppy from contour lines. Black Hollow School 1/2 mi N. Qu Hillton R in Franklin is Black Shale down to bottom. Black shale continues as far as road corner 3/4 mi NE of Black Hollow school. Black Hollow school, 1/8 mi N, at corner 706. Alentany-Minore contact at 706 exact. Peebles S 1/4 mile E 1/8 mi. then E of corner & E7 a short distance, Trimerella + gastropods. somewhere near 830 or 835. The underlying earth may have been black shale but I am not certain. Small Conchidina straparules mingled ones. 3/8 mi E of corner 827, Alentany-West Minor contact at 840. No sign of Minore here. 1/8 mi E of corner 827. Only baby near top of Minore at 795 about, but no sharp contact seen. From 827 corner, 3/8 mi E, then 1/4 mi N and 1/4 mi E, to terrace. Top of Minore exposure left to 820 approx only, but no contact with Alentani gy reefs. High kind, 1/2 mi SW at road junction to Black Pond & Mineral Sq go. First appearance of Minore top going down stream, at 6:30 about as far as can be told from contour lines. Peebles, center 1/4 mile. then 2/8 mi east on road to Pine Gap. First house in wide yard. West Minor up to 830 at least. Small cellar Creek, + Farm lots. Holgates above, SW road junction. Old State Road NE of Peebles, 1/2 mi N of #1 corner. Alentany-Minore contact at 850 about. The higher land in immediately west is underlain by Black shale, but only for a short distance west. Minore thick ness still considerable. 1/8 mi NW of 811 corner. Alentany-Minore contact at 841. With Alentany & Black shale N but fault eastward will appear. From 811 corner N 1/2 mi to #76 corner, at next corner's mi beyond is excellent Alentany. Minore contact at 782 about,

From last locality (2 mi N of 786 corner) go SE to second home on Waldey road a distance of 3/8 mi. Ellent angy - M more contact at 790. Black shale fills all the coal westward, Bacon Flat school. 1/2 mile 1/4 mi before reaching 1st home in left lane. Simarella, Halys to nexus, Large Ho'elabor Straparollus, Straparollus, nidagarensis, Minumula, West Union at farm gate by creek crossing, near 860. I think a rather indefinite. The same small Con chlidian as that found SE of Peebles about 1 1/4 mi, a slight dist- ance east of corner 827. There only he more fossil streaks then. Bacon Flat School, 7/8 mi NE yoach, 9 in all this distance there is not one crops. Here there appears as to be thin M more section over a thick West Union stuff not crop as far down as the creek, No clear evidenc y Ellent angy n Black shale here. Bacon Flat School Then 1/2 mi NE to road junction. Near highest elevation = 725 with lowest Ellen- tangy about 730. which is close enough in absence of actual contact From this point E on Black Hollers road, East end and some farm, by M more at 720 mth only from days ride above. 1/2 mi Ey last locality, near home on cart side y week crossing excellent Ellentangy - M more contact at 705 about. 1/2 mi Ey corner 743, at home, Ellent angy - M more contact at 760 at 760 continue line to angle of land a little farther SE, Ellentangy M more contact at 755. From 743 corner small short distance. Ellen crops M more contact at 758 rising southward distinctly. From 743 ninth, just before reaching next road corner. Ellent angy - M more contact at 755 apparently. Front Grove, 1/2 mi E to road corner typ. y M more at 760 or at least that high n higher. Ellent angy not seen, but should be near. Front Grove 2 mi E m east side by Sci'otr Branch Creek, Eg, y M more near 720, Further east is road corner 706. 1/2 mi N of 706 = Ellent angy - M more contact at 720 fairly exact according to Cartan lines.

Ellensburg Monrose contact at about same level just before reaching next road. On Bainbridge sheet Monrose is well exposed at bridge & mi's of Pleasant Valley School, also along road as far as the school. - At Pleasant Valley school: Monrose up to 735. with dependent crumbles. Ellensburg contact not seen here but must be near. Large spherical concretions in red bed here. Pleasant Valley School. White Black Shale Bluff 7/8 mi N of school down to creek level with quartz, Truant Grove, 3/4 mi SW to cemetery Then 5/8 mi East. Here is highest Monrose with Dependentia at 840. perhaps in top of Monrose. From here top of Monrose slopes along the top of road almost as far as next road corner and west. Truant Grove 1mi E, then 3/4 mi N Monrose up to 790, only from one above this level. 1 mi farther N. the Ellensburg-Monrose contact runs at about the same level. Now it can be seen that the Ellensbur gy at into with several feet, possibly 2 ft., of black shale overlaid by a much greater thickness of blue clay. 3/4 mi farther N. at road crossing, Only SE 1/4 mi. Ellensburg Monrose contact at 770, as near as can be told from contour lines. SE nearly 1/2 mi, at road junction. Ellensburg Monrose contact near 750 as near as can be judged from contour lines. On Bainbridge sheet. Smiley Crummo School. Then a with nearly a mile, in stream south of road going west. Here top of Monrose is seen at about 800 with Ellensburg along road only a short distance above. On Peetles sheet. From Truant Grove 1 mi E, then 3/4 mi N & 1/2 mi W. Monrose top at 800 as near as can be made out from contour lines. 1/4 mi W. This Monrose ridge over rock which looks like Marble. 1/2 mi W of road corner, outward from last locality, beyond lines. Marble at least as high as 830. at top are loose blocks of white limestone containing small pyrenostylos. Large Halysites very Megasteropsids of large size seen in Monrose,

Peebles - Sinking Springy Juke. B[illegible]edge sleet. At road angle I met N'y Southern edge of sleet. West Wm'm well alt up to 845 at least. At bottom of hill before reaching 769 corner, Inner West Wm'm quarry is defined N' side of Juke. Here fossils are white & calcified to SE of Sinking Springy. Sh my dir't N. Continuing N from 769 corner, West Wm'm gives way to West Wm'm sand to top of hill = 825 at least. No room for higher strata here. Crooke creek bridge. Inner West Wm'm down to creek level. Small bend N of Crooked creek. E'y side. 14 ft of z'cald M ark - much fractured locally. 3 interval 30 feet partly exposed. Typha Lillie bed in Strobilogramma linden with Cyath. phyllum radwicz, strobi[illegible]a digginitata, small called 'farnites'. Stratigina, Willehm Lyellia cc. 1 ft solid laminated jelly beds which we either met locally. 2 1/2 weathering shaly. I rate few 5 2 1/2 ft interval. All inner West Wm'm. Crooked creek at bridge. Base part of West Wm'm not exposed here. A little farther north on west side of Juke is a quarry where we found cannarite calcite nodules. Left some Branchysperm large in the front end of pedicle were depressed gently along medium parts so at West Wm'm, cannulites lay, all in one layer. See section below:- 1 ft very travelliferous Carboniferous bed. 2 0 ft interval. 1/2 ft hard dolomitic foreign. 8 ft interval. Weathering like cc. 3 ft finish shale & indurated rock. 2 ft soft t. 1/2 ft weathering shaly, 1 1/2 ft solid limestone. 1/2 ft clay shale. 5' solid limestone. The crinoidal layers found at the top of the section SE of West Wm'm other appears to occur in the preceding section a short distance below the Cyathophyllum radwicz bed. I went Grave 3/4 mile SW to cemetery at road crossing. Ellent angry. Mudire contact at 885 ft. Not actually identified as mudire.

to east Grove NW 1 mile, to bridge hangs over Crooked creek. All west of this as far as bridge, but at bridge the top of the Great Arch and clay is seen. Crooked creek itself crossed further west. My Crooked creek bridge ½ mile, just beyond Come turning off west. On N E side of ridge, beyond farm, Minerve exposed with strike N W to road and dip N E. Only about 12 ft dip here actually exposed here. North + NW y Cant expose the ridge is formed by Black slate underlain by Clinton argy on southern side. At next house northwest below lettered in Andrews, this is Minerve which continues as far west as Andrews school & corner 773, dipping southwest a north west road all the way. Beyond it at a third house. At first house S y road westy 773 corner is Minerve still. At second house S y road westy 773 corner Clay Black shale shows up in soil south of the house about 20 feet. This underlies house also firstably, west of the next house, on N side of road, is Clinton argy on N side of road; Further W, beyond small dry swm indicated only by contour line in creek, is Minerve. Further W, is plenty of Little Black shale No outcrops west of Straight Stream cutting in from N as far as first road turning off N, beyond house. Turn N th the Brady way.) 2 ½ mi NW by strike, west y road, (Clinton argy - Minerve contact at about 760-20 = 740 fairly exact. at road angle 3/8 mi NW by strike, west y road. Clinton argy-Minerve contact is about 765-50 = 715, indicating dip t north west, here. At lane leading west toward 3 repeat W and the near slope of about 25 ft from road level. To expose along road until cut y road at some 840 ft but at NE of Surveyor's mound line is reached. New Great Arch end shows up on Sma west thin dip facing nearly 60 degrees east. Lack y contact about 820. Northward down hill, Great Archard shows of below the same form west Min'm

South East of Church at next comer is Cliver Black shale, this black shale is exposed also N of church corner. From house N of church, going up the road, While on E side of road, white clay on left. From middle part of rise hill is Cliver black shale on both sides of road, presumably dipping NW. House rooms at top of hill on W side of road. No exposure here but cherty rock occurs where road turns off to east. Rock dips strongly W. That is very thin strips x 2 chains wide. Dissected to be Lower West Union. Further up down the hill along upper third of hill above, is sand rock with small celled foraminifera, East of the road junction the Lower West Union rock ascends the hill and at the same time slopes northward. At some 5 feet below the level the strong bend of the road northward, there is a white clay, as yet unexamined. Just before reaching strong bend in road towards east, white clay film from west which shows up, fronting strong bend in road to mi where road descends the hill, there is Lower West Union dipping strongly NNW, undulated at lower part of built by White Clay arch formation partially. Hill runs N of roads along edge of this hill bounding the road occurs white creek chalk and clay at scheme SE and runs back limbering, very slightly lower West Union. Then runs rises eastward along long hill slope exposing Bellport near base with Bransfield debris begin up and Cincinnati rocks seen top but not actually in site, Some Cincinnati rocks show up on that part of road which as Cline's hill SE in direction. When road runs E there are no opposes until bend of road is reached where it turns at right angle northward. Here very strongly tilted Cincinnati rocks near, Road turns NNE, then ENE. Cincinnati debris occurs at bend,

Next, road turns NNE again, then ENE. A little Cincinnati delvis runs in the road. House on S side of road, NE y house by rm, just before end of road toward ESE, Cincinnati rubs debris at several intermediate points. Where road begins to go strong, from hill is first Cincinmate rnb, then jumble clay, farther dwn road and quite farther dwn is Bossfield, a little furn are also, a little lower is Crab Oak and white clay. Still lower is from West Union plain tically vertical with strike about N 80 E. The road goes more directly south and turns one east. In a short distance the exposures are from West Union, then for a much larger distance they are marble. About 300 yards west of the point where the road turns N in order to give the spike there is exposed the Delvis Black shale. Andrew school NW y Grant Grove WTr 773 corner. Then up hill. Marble for considerable distance sides up hill. At first west of hill is marble and thus marble continues to se and east, a short distance S of house on left of road. From this house northward to bend of road is from West Union. Then E to bend of road. Then NNE down hill where rock is from West Union to road junction with house toward NE side of junction. West of this house is white Crab Oak and clay, and farther west in the sun bed Bossfield. Limestone are common. Some that are dark green. A short distance before reaching the house and end of lane, a dry wealth. The sun is indicated by the cut on line. Bossfield is exposed SE of this limestone crossing in a low elevation in this valley. There, from of this Bossfield is dipple marked on large scale. One layer one layer is included here in the debris. The iron ore bed is well exposed west of this dry water stream dipping strongly eastward. The bed about 2 ft thick. The dry stream goes only about 2 feet below this red bed. The bed rises to, point where road turns NW to house,

A fault plane seems to intersect just East of house, going N to S, and on North side of this fault seems to be some partly West North West of this house is stream junction. On eastern branch at this junction is Brassfield and Brassfield shows up on the southern side of the hill land between this junction stream junction or of the Farm the course the Clints extending including the Iron ore, continue west ward on N side of stream, and on again East bank of western forks. Here * Cathayron clint merges, Birdshy, *Lancetata with parallel sides. * Defile area, Iron ore, occur in Brassfield limestone. Along the Eastern side of this western fork the Brassfield dips southward and somewhat easterly so that it would go under the hill land on the South side of the stream south of the junction of the two forks. The Dayton limestone seems to form the top of the section as exposed along this ridge between the two forks. It is not known what lies N of the western forks, and this system fork might be due to fault lines. Look up. Return to road junction a little over 1 mile NNE from Andrews school. Go E. Probably Crab Orchard clay on North bottom. Then NE, probably, also Crab Orchard clay in North bottom and on south side of valley. Before reaching point where road turns about due west N, blue black shale is exposed on S side of road and also on N side of road further up hill. Here the black shale dips steeply West or that at road angle where road turns to right N there is Monroe with black shale westward, the plane of joint act dipping steeply west. Road turns straight north. Monroe Road turns ENE. Monroe at road corner. Stone on north side of road. Monroe in road very poorly exposed along road. 1 white east is little limestone all along the road. The road turns to right N again. East of this road are great areas covered with blue black shale also pretty well mixed with Bedford drift. Along the road southward is white clay, probably Clinton argy. Stone further N, as far as road angle, is blue's black shale.

The road turns straight east, then NE. No good outcrop. Brassfield extends along road from 820 corner south as far as first fence in W side of this new road, alter in road angle SW to 820 corner. NE corner 820 is rally, then muddy, then highest land with no exposure. A low hill NE, no exposure for any distance. Half way to the school is white clay, age uncertain, but probably Cretaceous. At the C manor point it is similar White clay, possibly Crat Lichard, London 1 mi NE, while Sinking Spring road a Baker orch road crosses. Middle Fork rock strikes NNW and dips NE, bringing up West Main mtf. It dips NE. Then NE to house on little projection. In first little stream valley NE corner is Brassfield at outcrop, dipping SW south. The next stream valley appears to be mapped by Crat Lichard, overlaid at top ridge by West Main dipping south down the ridge, and still Steeple eastward. Eastward a very short lane leads N to farm. Where Baker orch road takes W bend by Baker creek, decorated white band &: mud rock is exposed. This undulating immediately eastward by that part of the banded mottled stone examined West Main which undulated the Holsphraguna clay zone, but not Holsphraguna clay appears me same line. Dip = W steep. At corner 689 outcrop also shows up, if road, overlaid by Lower Red Main as that the Lower Whitefieldella bed occurs at 700 about, dipping SW southward. Immediately E of 659 corner the road turns NNE. Here from West Main is shown above the road level while Crat Lichard is seen beneath, south of the road. House on farm S side of roads on hill side NE of this house, west of a faintly long valley, is Brassfield ditch, including Holsphraguna & Magna. This strikes departingly north east bringing it below this dry stream level within 200 feet of Baker road. At house on farm and in road bed NE Brassfield dipping E as though a low anticlinal ran through here north eastward. NE corner & fence a lone cincein from the SE. Further on is low flat valley and NE this valley the little projection is made up of mud rock.

Just beyond this the road bends straight east. Here Clent argy clay is overlaid by Black shale. Clent argy shins up at Honey Hill east ward. Next a house is seen in N sidey road. Here Clent argy is overlaid by Black shale and further north the top of West Wmin is seen. Road goes NE and passes Dane on west side. Black shale underlaid Clent argy all the way up the hill to the cabin by the road in Up, Also Black shale E coming down the hill as far as road coming in from Dr. Marl rock occurs in creek bed just cast of road junction, NE as far as house in hill crest south y road, my marl is exposed except a very small patch of Clent argy. This marl looks on though once it had been thin bed like Wmin, but this is uncertain. East y lurnee. Black shale shins up on far as base of hill. Followed by marl rock as far east as next house in N side of road. Easty lurnee the marl shins up to foot y hill, E y Baker Fork bridge is lime West Wmin. This continues E to first house in N sidey road. Further E the ground probably is underlaid by black shale but no actual exposures are seen until little stream in next lurnee in N sidey road. No exposure east ward until the jpike is reached. Along Sinking Springs- Grant Grove jpike Black shale in E 2 ide y jpike from Allamo Cr line 3 mi's where laine turns off W. Here, is led y creek and in hill most y creek to W horse dipping cast ward and at least 20 degrees. Black shale above in hill. West ward up, hill is Black shale about halfway to bendy road, the second half of this strd is marl apparently of Wmin origin. Then road turns south. The ridge presently is under laid by West Wmin. Then road turns E, SE of lurnee is rock identified as West Wmin. Past off house along old lane on map marl from Wminre is exposed in drop to point where road turns south up a stream hollow. Here marl dips druggy west ward and is Gore West Wmin. On next side of creek direct E & W y bend of road The formations Orssofield strikes on Summit Large Dayton & Others also run. Follows stream down to entrance into Baker creek. Here, up a hill side run, my Richmond Achis occurs, but in great abundance. This run is located at point where Baker Run makes a strong west bend just south of mouth of little branch just of me describes.

On east side of mouth of this branch at edge of hill land is ferny pinus B s associates dipping north. Also bone Dragm l. blanks with small tubed springs near as at John Shrop's. All of ridge like S & SE glennoe when horse stayed (about 3/4 mi S E y point) while Stuckley springs- fromt Gleno juke crosses Adam's Cr line) consists of marl and then West Nine mile km. to creek level westward while lane ends in map, and thence SW and S y thence as far as creek in each case. Beckles. W y t mm 1/4 mi at large grassy, Shrips smells magical or dival. = try hida. C roundt redm large like Stricklandi form's horse another ahead, Allaermb Amerianus head. Beckles to Plum Run (quarry) 10 3/4. Plum Run quarry. 44' Clairang will opened Water Marine 16 1/2 O. Construction small ce. Liner Marine 27 1/2 West Marine mails Halyton m 141 Half a mile west of the Plum Run quarry, along the railroad east of a crossing the railroad on the N. side of the track, the rock near track level contains Pentamites along with nighstone at at Alletron, and very common. At the height of land cut by the railroad, 3/4 mi W of Plum Creek (Basic Products) quarry, is large meal exp mine. No sign of Pentamites here. 1 1/2 mi W of Plum Creek quarry, the railroad is crossed by a farm lane. The rock expost line seems to be within West Nine m. a little farther W, the rock in the stream crossed by the railroad was not examined but probably is the same as the West Nine m

143 47-72 [illegible] 868 - Springfield -0 866 864 - Wrtled 2 Yellow and dense 855 -> sharp c/n change 11 Blurish 847 - Blurish fine grained 19 841 - Blursh fine graner 26 More glittering Specks in light third arch 1 838 - Glittering specks 25 832 - Dayton mill 34 831 - Brassfield ? 36 8½ Enphemia 11 Bedded euphemis 14 Laurel base 18 @ good base 26 Dayton base Blansfield by

Brassfield Smith, p. 134, 103, Dayton Smith 140 . 74) Crabtree and Martinsham. p. 84) Osgaard 145

Lanrel Bisler Fossils at Pueblo quarry 140, 130, 127, 110, 109, 102, 93, Martin's Rest, 85 upper part at West Union, 109, 106 Holley p. 126, Stenmatopora p. 121, 116, 107, 106, 99, 98, 96, 94, 83, 82, Trimerella Megaloma Fossils. p. 141, 125, 122, 120, 114, 107, 105, 104, 99, 99 bis, 97, 97 bis, 95, 95bis, 94, Trimerella 94 97 99 105, 120, 122 Megaloma 95 97 105 Strophalos papyr. 96 97 97 bis 105 107, 122, Phanerthema recidens 95 Pect antrum 95, 141. Swirphora 99 Monomrella 99 114 122 Pyramstylos 114 125; Cinclidium 122;

Enjohemia p, 60, 58, 57?, Springfield p, 64, 61, 55, 50, 49, Cederville Springfield zw mry. do 55, 72 73) Slumpó Gimejalu, p. 69. 56,

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Do not stuff your husband - Husband your stuff (Ford Cussack) Buy thrift stamps, Stamp out the Hun. Contributors to the War Chest have a right to feel chatty, every time you lick a thrift stamp you help to lick the Hun. Red - Blair Black Shale Green - West Union Yellow - Crat Archard Blue - Alderson Orange - Brassfield. Dr. Arthur Gitzon, Pay Ottawa Net $200 Pane Ruedemann oldest son. officers training Camp Chilli's the, Ruedeman mm. Second cm. 1st Leint. Medical Corps Redner girl, 4 trip altogether in draft. Keystone Lantern slides. C H Newell . 93 Bing Ave, Ottawa mo2. $ 29. 30 covers expenses to June 23 mty.

1902 Cuphemia p 57 Hudson Falls Cephemia p 58 Cephenmia Jacksonsury p 60 Springfield at Springfield. p 75

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W TEMPLE TABLET VIRTUS SERIES LABOR POCKET NOTES.

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Clinton Cr. V Charlesville+ Adams Cr. Brown Cr. Waller Cr. X Ft Ancient X [illegible] X Benqunte Hollow near Clarksville Butler Cr. V NM Middletown Clemont. Hamilton Millgrove ? Millanchy, Burlle. Fleming, X East of Wyoming Batt X Amargossee. Lewis Cr. V

NE of Versailles 735 10 ft mollusca 5 1/2 pt Bryozoa collected mollusca 5 1/2 pt monted L. Leporidae 5 1/2 pt express form 5 1/2 pt L, matkred to small bottle, collecta byzgra 1 1/2 pt monted L. + Tetradium & Stromatolites 6 ft mollusca 11 9/0 shale bed [illegible] 12 ft massive including Tetradium Base of massive Tetradium.

"Tetradium, 12 ft Massive including Tetradium Base of massive Tetradium, with Calapocia just bdm., 21 ft interval. [illegible] viruta at this base may sue before Tetradium Strophi, Opposite base of written expen 11 ft. St. glauca, 5 1/2 ft with Plectanm in place 3 ft up, Plectanmites c. St. glauca 5 1/2 ft interval. in round side ditto, St. glauca, and another Dine out quadrata block over Dinotlia subquadrata in block twice thick large with Plectanmites 16 1/2 ft interval. 4ft Tetradium viruculjeta in place at top Middle of byroad internally. 5 ft interval 1/2 ft Phychistron dentatum in place 9 ft interval. Will collected by grass, with Constellaria in lower 4 ft. [illegible] Staphylea neglecta & Tetradium viruculjeta at my base.

1 ft interval Culvert some pike up. 6 1/2 ft interval Rest sect'n any hand on War distances of miles Physochitine dulcamara long Stroph. plumbina cupularia 2 1/4 ft interval, Ft Ancient bridge across creek westward, 5 1/4 Ft Ancient 1ft above the bridge above named is Stroph. solcata virity. Plect andmites ee about 2 ft below lowly bridge.

38\u00bd 17\u00bd 26 44\u00bd

Wreithung S. A. thaly, streptilasma strigillana sulecata, Rhy: caprae, jostae, Nebulilla Platystigma Otenqua demissa Lichenomimus tuber culatus in upper part of merentua mottled l. li are more directly seen O. andalusium bed, but little Tetradinium, Orthoceras, Pterinus demissa + Byssocyclus bural found here in O. andalusium bed, upper O. andalusium level at Versailles also large + small hyggrams found at upper strata; Cyrturus with close septae, Versailles layer annulated Orthoceras with ribbed Millerio species Tetradinium as at same as at Versailles, Byssocyclus Dartelno. Nebulilla, Sargeciana Hygrma Shale bed.

Shale bed. 13½ 5½ ft Harder mottled l, with strac vdot at top. 4½ ft interval softer mottle. ← Lichenocrinus in tabulatus C., 3½ ft interval, ← Starharmena sulcata. ½ ft interval, softer. ¾ ft Tetradiina 1¼ ft Softer mottled 1 ft massive mottled l's 1 ft Tetradiina c. upper hard at very milled, 1½ ft weathering back, soft. Hard in cut, 2 ft Mottled l. + Byssomychla's. 6½ ft Shale bed. Base not seen. 745 (9½ ft interval. Not expressed. Tf I may say ⅘ side of RR.) 13½ ft (I) now base of shale bed as expressed, Bellerophininae Ostracoda with, Ostraea, Lichenocrinus, Acharnacula Basal of Delegriata bed & variegated. 3½ ft interval, Stroph. reticulata, Ostraea, Lichenoclinus, Ostracoda with Tetradiina. Fine grained at top. Artificers as collected..

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Adams Cr, Upper [illegible] to reflect=13\frac{1}{2} Blanchester, Total not known here. 20? Clarksville 12 ft. 10 Ft Ancient 12 ft. 10 encordswi, 5 ft Dweneel 35 ft. Flatbyne

Marchy 1 - 16 out Creek Rd.

Wednesday 1, - 16 int Creek bed. 17½ ft til nr mile post Cin 36,=Nmy post 1ft. Straph numma, plgummtua_+ el myata. Perisjara,? or tenura Debuttella larye 12s in wide. Rafinesa grana large flat. Plati clarkes williams? Leptaea zyg. urdecta? Hlychlothenma dentata, Striptelasma histivnum. long? 8taph numera retusta. Wednesday 2, - 16 int 37½ ft,N of Cin. 36 mile post. Creek bed. 3ft. Mint fossils listed at Ep Leptaea, c. Platy strilbia, clarkes williams? or el vicerna. Debuttella larye, Rafinesa grana. Striptelasma virpandrum Crustellaria florida, No Striphemina seen

Weisburg 3.-16 cut 20m 23½ft NE of Melopnt Cir 36. 5¼ft sech. Friesella. strigosa nova mutans, strigosa neglecta? bidentata valv. strigilifera planimbrana, Saphrena, Platystrophin, Longa Weberstella. Stylitesana oblongum, (Schnitella neculpta c) (Phy. palacullra c.) Weisburg 4.-16 cut 35ft tulnr Cir 36 feet. Dreigolar teddes, - Uros tedded "litt" Dalmatella gynaec Platystrophia elastellum c. Programma occ Weisburg 5.-16 cut 40ft tulnr Cir. 36 feet.

Wesding 5 - 16 unt 40 ft telma Crin 36 feet. Leptaea cc, Olatj. [illegible] c. Refinea guisna c convex Wesding 6 - 16 unt 20 ft telma Crde 8/7, Dalmarella c Olatj. [illegible] c. Refineguina. Plerica dennissa lage. Zyg. urdosta Crdei 35 ft telma. Crin 36 feet.

West end 1 cut 14 | Cut 35 first at E 246 [illegible] bote end

West end I cut 14 | Cut 35 feet at E 246 signal pt, 44 ft above signal pt 246 stroph, neglecta, praecursor, strophy. mutans. H. in calcif., strophy. dichondra, all lone at 44 ft above 246 pt. but believed to have dropped chiefly from 6 ft farther up. 18'2 ft above signal pt 246 is zone of Clark ville bed. Plant fossils considerable 2, carboniferous rudgate 2. ft ancient much more clay

Cut 12 section Anomalidonta alata. Cyelena fluctuans, in gritty (andy) L. not in Moderat top, w/t Shemendy's Long Rafinesque box slates; Bare cut 13 sighted 12 ft interval, This clay w/ D almonella. P? Andrew 2ft Noderbed. Andren bed. 12 ft interval gritty app. L R N level cut 12 Cut 13.

Art. 13. Byssomyelua gigartea, rot unt angulae ostae -- -- but ~~~ i 3¾ li lng. O E Mica de mibus large. Dabrunella cc mrhlopsi ozzaiilnesi; Strofhmen peculiar in tertio,

Cut 15, East end, in creek bed Dalm. juncea cc. 0-5 above creek under E ridge, cut 15 clay, with Dalmarella cc, inclining from westwardly drops rapidly east ward,

Cut 16. Olet ambrota cc. Little stream from south Ortaria papulata, Strept. hosp. nudum Streph. planumina Yegitalia cc Rhy. pulamellna - Upper w.e.attn bridge here. -Ledy c 36, 5ft 6in Cut 16 west end, Olet ambrota 10'2 ft down from RR to left side Rhy. [illegible] cc silver.

Antiracaria 4 in tray, 11 ft - 25/2 calx Perg clay perch. 1 1/2 ft. stryp. dispandium. Sturvelina + planulina. Ptyg. palamellae, 2 in. entgradata 1 ft. Palamellae. Nett. viz nepeta, D. in. aquacalata 1 ft. Total val 5 ft Ptyg. palamellae Din. entgradata. stryp. planulina stryp. dispandium Nettella micropita base: 6 1/2 ft above tb 1 innot Plecl an tritis or lagr. y last two sections, 2 23 1/2 23 1/2 5 1/2 8 1/2 ----- 12 Washg,

Washing, 3rd insculpta int uval 12 ft 2nd + Main insculpta exact int uval 23 1/2 ft} Blandester let H. insculpta. int uval 25 1/2 ft, Clarksville. Insect A. flammea or int uval 26 ft, St Orient, Arbuthnot

Mroo Hill Stz, 100 y ds. My min fence across my. Hillside S of creek SW of station. 5 ft from Oayu Plectambum Tecoo. 1 ½ ft interval. Rhy, c opax c. 2 ½ ft interval. depression. rather convex fracture valve mud day Left area CC, + Dalin small 3 in wide 1 ½ ft interrupt. 5y 7 ft. Miss en AFA at top of Blam heat 16 ½ ft interval. 276 m. Left area cc. Crustella? polystrumlla? Platystich. clarksonilleni Tremata. Strujet, are span dum. Plicina collected. min fence across creek SW of station 9 m. interval. Stych. neglecta c. Tremenatis. nutta 3m interval Plid clarksoneileni. Crustellana stych. planum hum. rotusta, angulata

"Lepidocena ce. Crustellaria polystrnulla Platystriph. clarkesvilleni Tremata. Striped, drifpan drum. Plethieran collected. Wire fence across creek stry stat 9 in. interval. Striph. neglecta c, Oremata mutans 3 in. interval Plat clarksvilleni Crustellaria striped. pl annulima, retrota, neglecta Striped diaphanum 3 in. interval. Small drop at RR bridge immediately E-J station. 1ft Several Strip. mutans One Striped. neglecta 3 in. Striph. vitrata. neglecta, mutans. Wire fence 10 in. deep. striped. pl annulima. Helmlite. R of magnina 3 in. crosshilled not approaching westward but dipping east. producing faint wave ridges N SSE. 9 in. interval (= 9 in.) Arthra, drop. Refinesginnace. Platystriphlice c. Ozymyran cc. 1ft 6in. Interval Refinesginnace Platstigh Cravia Lachia. 5-Striped Arama drop Andron ce. Attachment Specimen. 3 in. interval w'tt Straptelrama at lac 6 in. interval. Highest Dal. jusra typical, 2/30. Striped arama,

Mares Will 5 7, 2. 9 m., interval Staptdazina c. my fence. c 40 m RR, long stretch stone bottom from miles N 65 west! 2 m high 24 m apart. 5 m. arresteddu longei 17 m. Zytana, c. Dalmanella jingra, c Dorpsostylos, ce. 6 m natural flat rock, well. 6 m interval, Dalmanella ccara. celomera flectrosum typical motus millepunctata. Dimer derm ca 3 m. hgt. Lepidaea, c. 20 m. natural Lepdama c, Dalmanella jingra cc Platyostaphria ce. 6 m interval c Staptdlazma c. Plagsta Jdeur c. D jingra c. 6 m Platystrophus c. 10 m. Platy Strophica spurstigleranae Nascia Prof, brachyptus, Slight wave marked, 12 m. Dalmanella c Plagstrophe c miltelle. Staptdlazma derdel celomera me. formal belux celomera belix tile,

12 in Dalimella c, Pletzstrophia c Schrubella. Simplilasma general Cylmena me. Samuel Dohy Gelmuna Liby tale, 3/4t. Ref. Droxlytis. 9m mt under. Ref. droxlytic & Dalm. j'mna c, Pletzstrophia? 7pm. Singl. Gelmumma c. Cylmena Liby annul. = 12 ft 1 in. Dalm crossballed from of Blanchester + is first Simple man seen s'ving dark, aber Simpli tilasma, general, Gremat. Zwilllepenclata, Dalmella c, Pletzstrophia c. 12m. Lepstaena catup Strophimma Gelmumma, Walter Reath's house. 3m: S'ing wam marks N 70 W. 10m apart 3i light. 12 in interval. 3m. Lepstaena cc. 12m. Lepstrem. 6m Gremat. zwilleppendata, strong more planumma c 16ft 1 in. Dalm crossballed y Blanchester. Will Speizhausshaus.

mme's Hill Sta 3 2 ft estimated interval = 9 mi, strip, plain me, fern, Dalmarella c. Plect an [illegible] c. Strip Dazma fern. 6 in Bryge saki creek bottom strip, salt bar - 1944.4 mi [illegible] Benj F Shelding Rich bruce's g RR, 1 ft i Dalmarella c Plect an l [illegible]s Plect an trite s Plat stripho. P tinea sui ligh. - 22/4 mi Lohn Blan 12 mi. party more marked logs Dalmarella cccc 3 1/2 ft estimated! 3 in limestone recently quarried ft to wooden keel road. Dalmarella c 3 ft interval 1 1/2 ft. Dalmarella, 1 1/2 ft. road crossing F.W.O. Danger. (100 ft E of Gii., 39 mi m RR) 3 ft estimated Anomalodonts Gigantea several High bank in Wilde.

1/2 ft road crossing TWO. (100 ft E of Gr., 39 bnt m RR) Danger. 3 ft estimated. Angiulardata. zigzants several High tank m N side. express become scarce here, short sighting on same ground, (8 strip neglect zone = 5ft about at railroad ex promehue) 33 ft - one / strip neglect to side, ↑/highest str. neglect. 19½ ft str > struct + neuranotely ↓ Wrijm 18 ft interval, Dolbying on ccg. Str. sulcata. 6 in intervals. Strapli. sulcata in dry stream bed, N y Creek, immediateq N y wire fence 200 yds N of wide limze.

A Moore's Hill Sta. (Blanchetua 22'7") Djy Lebertella immaculata 19ft 9 in interval 1ft 9 in. Stz. neglecta, retiveta, nutans 10 in. Interval 3 in. Crustedd base & Blanchetu 10 in interval Rafinesquime, Oleti c. 4 1ft 8 in interval Craww Laelia 1-6 4 in Streptelasma at base. 8 in interval highest Dalu, jupza typica 4 10 in. single area c. c 4s & RR, 9 wire fence. 5 in. Cross heddled, wave marked 5 2ft Leptaena c., Djupra c, 7 in. Flat side w neck, 7 in. Leptanac, D. jupza scorte, Cyclimma plucticann, ?remotus, 2ft 6 in. Leptenia c. Dalmanella jigza c. 7 in. < Streptelasma c, 7 in. < Oleti crmnn 1ft 3 in Opith Petra CreaD. 1ft 6 in. Dalu Damella c. < Cyclimma ?libra 4ft 6 in. Raye, Lox styhi. 1ft 2 in. Dalu jigza c. No planktonoma 19 ft 10 in. (10in str. jel nemumina, 1ft 6 in. Leptaeaa c et wp.) 4 in. String wane musho, N7D W.

1ft 3 w. Opitha [illegible] c[?], 1ft 6 w. Dalmarella c. < Cyclumma libra 4ft 6 w. Raje lox styta. 1ft 2 w. Dalmajura c. 10w str. Jel mummia, 1ft 6 w. Leptaeon, c et typ , 4 w. Strig rame [illegible], N70w, 1ft 6 w. interval, 4 w. Leptaea c. 1ft 6 w. Leptalon, 9 w. Oreamhos str[?]launus Hune y mll Speizhais, 5 ft. interval, 3 w. L & tr. jlannum ma feor Dalmarella c. Pleit antmita c strig et [illegible] fer/red e. 1ft interval, - Strig sulcata c. i Hunk arj. l. Pletantwto

1914 Copied Verraielles erecta, Stroph. neglecta, 44½ Vervaiella bienepta (varna) just above 30 ft Dalmanella jigrza, rather scarce. Plativeraillensis typical. Septacena Fairy numerous lid ayes, 30 ft above creek, Type Dal. jigrza typical. Leptacena, Rhyg. platamellina streptelasma, cylmenathicus, in situ? Rhyg. platamella, St. plammulma. 27 ft {Rhyg. ped gunellas, St. plasmulma, St rept clarma} 25 ft above creek low projecting ledge, 22 ft above creek, stroph., plannulma n. s. (1) 21½ streptelasma in situ. 20½ ft above creek. Leptacena in situ, Common + air dmit about 1/4 in 6. 19 ft. (=14½ft above bridge level. Leptacena common in situ, 17½ ft above creek Leptalma in s.tn! 9 ft Pascedus clarmini large loose, 8 ft 6 in. Stroph. Sulcata 8 ft 3 in. Stroph. plannulma in sitm. 7 ft, stroph. sulcata in situ 4 ft. platantmto c.c. Bridge Level = 6 ft exact above Ozelen in creek bottom, 60 H to tin y Cumming's West end up creek to jizzo to Caprol,

60 H section of Cummings. Westward up creek to jilze to top. From 32 to 33 ft above shale bed, Strath relations widen midway is over me... with rocky fracture mis lays), called White water immediately above, grading up from Saluda which is present for us at top. 60 D Not good for lower party section. 17.5 39 1/2 17 1/2 21 1/2

NW Canaan 2mi Equestrian Liberty in the 9, almy E+ word Wave marks N60 E trend, 30m apart 3 inches high, well marked Strephi planum mac. Physchitium cyprean palauellum Cystocarp velatum, A. mutica antiparadict, Sepiaceous, D. mutica antiprodictal, Platanthera cc, About 3 ft in total, Hebryella macgysie few but clear, 8ft 3in in total, Septanea cc 5th. pl antruma Partura papillata 2ft 3in in total, Partara n.dum medians typical dam. 4ft in total 34 Septaneae large, Septanea cc. 2ft in total Strephi neglecta good, 16½ ft Septaneae Cantillaria not prominent montana Cantillaria just at smalla stipt. dijfounded Hebryella nodatalsis, 15=17hm. 3ftandin 4½ 2½ 3½ft. interse. 1914 Cyprean 10½ ft dam. 14½ ft dam.

3 1/2 ft interval. 1 ft ring angilacea di strigila c. str. fel minuta d, 23 ft dm. 3 ft interval 1/2 ft streptelasma laye. -> 26 1/2 ft dm. streptelasma leptaena c. all night. 2 1/2 ft internal leptaena, c streptelasma 29 1/2 dm, 3 ft interval leptaena 22 1/2 dm, 5 ft internal -> 27 1/2 dm. 3 m streptelasma. rare strigla, zulecata c, 3 m leptaena, catazyga c, 1 ft streptelasma c. str 27 1/2 dm 1 ft interval. streptelasma c leptaena. strigla. plennima, -> 32 1/2 dm. 5 ft 40 1/2 ft 3 ft 2 minnella c, pleo audita c streptelasma!

9 mi. (on steep slant) -> 41\frac{3}{4} ft. 5\frac{1}{2} ft. interval 2\frac{1}{2} ft interval Platypus c Didimella c. "Large Bysanycla c Pterinus large c. Acmalodonta, 25 ft interval 4V exposure The lower twenty section is better exposed along Indian Kendrick creek in section m10. from bridge to Barbosa. while northwesterly beyond road leading west to Michigan pikes [illegible] 1914 copied This area at Madison, \frac{1}{2} ft. typical clay shale. Varying from silt to day. clay

11\frac{1}{2}ft strata at Madison \quad \begin{cases} \text{1}\frac{1}{2}\text{ft}\underline{varing} from bluish to gray, \\ 4\text{in. Clinton}, \end{cases} \begin{cases} \text{1 ft upper half Clinton} \\ \text{1 ft lower half washed with Madison} \end{cases} 1\text{ft }6\text{ in., with Lepidocicera crecigera at my base.}\underline{ \quad \begin{cases} 3\text{in. dark shales}\\ mythalay strata cerium, fresh spiral lamellae} \end{cases}} 1\text{ft }3\text{ in., Spld. with Clidocera + dark}\underline{ \quad 6\text{in. soft blue top Strumatocerium}} 18\text{ ft Massive quartzite (revotted)} \\ 6\text{ ft inclined to be massive}\\ \begin{cases} \text{especially in lower }\frac{2}{3}\\ 9\text{ft Massive strk with thin laminae},\\ 9\frac{1}{2}\text{ft interval, soft stuff} \end{cases} \begin{cases} \text{cerium at top, but } \\ \text{main zone here}\\ 11\frac{1}{2}\text{ft. Columnaria creodata}}\end{cases} \quad \begin{cases} 1\text{ft Columnaria}\\ \text{interval}\\ 4\frac{1}{2}\text{ft interval } \\ 1\text{ft Columnaria}\\ 4\frac{1}{2}\text{ft interval} \\ \text{culvert} \end{cases} 71\frac{1}{2}\text{ ft} \\ 128\frac{1}{2}\text{ Catagga beds in place, 76 ft below Columnaria zone}

RR at Madison, 1½ ft Christ, [illegible] 2 ft 4 in Ordinance [illegible] 43¾ in interval, interval with Loph. hammelii at top. 7½ ft trend of culvert, £ 7 fall, wet weather. ½ Colmanaria lesser zone here, large zone winding RR, 4 ft interval, 1¼ ft Colmanaria major zone here. 14 ft. 37 ¾ ft limbedded with thin blue lid age [illegible] calcareous dip and run. Septic area forbale length at 5 end of deep box limest larger exposed for Cymati? 6 ft mineral 5 end 9 deep Saluda cut N end 9 short pile my north box at 72½ ft interval. (130 ft below) [illegible] Abundant madimeria; at N side of culvert. [illegible] 3 in interval Top of culvert cement at highest level, 38 ft interval. Archaica up to top. Din. retroza in wtn at 4th zone hammelii zone Helostella scalygderensis typic. narrow with deep fractural depressura 1914 Copied Hanging Rock Brady, ½ ft interval, 2 ft interval, Base 1 Very hard Saluda 4 ft rather massive 3 in blue l. fossil.

"Hanging Rock Bradi" 1/2 ft Chadr'mm 1 1/2 ft Saluda 2 ft in terral. 1/2ft Columnaria 4 ft in terval) 1/2 ft Columnaria c. 2 8 ft in terral, Din, subgradata in w'th. 34 1/2 ft in terral.) RX Long wall. Nend of fence at culvert, 23 1/2 ft in terral. Stwath plummbrac. in sully. 4 1/2 ft. in terval. RA thank Gm W'tm, side a farust bull, First yard from exp more below culvert . y.p. Krebs PUNKS 3 ft Striph. sulcata at run ins levels, (9 3/2 ft belw Columnaria.) 18 ft inteval. Dune of heavy loestnes. (11 1/2 ft belw Columnaria layer)

Nemicystites stellatus in same Refiner prima as Apelacrinus pilleus. Cystactea granulatus border is wide at midist point, spread absolutely flat and thinly against supporting Refinergging. Alternating this membranous border these plates are minutely parallel, and further back there are granules, rather distant. membranous border. in this case there are 3 Cystaetes in the same specimen. An hygroma. Apelacrinus given me by John Bammells found at St. Petrocrinus dyeri bridge above J.ocrinus intrassus, at 2mm bridge as Anmalocystites salamwides.

above I venimus intrassus, At same bridge as Animalogytsts Salawrides. Aplacinarus, near school house was at top of hill at Cincinnati west Highland Park turn; Chrs W Mykoff. lived Jpnite. John Damnell,

Hanging Brook Road, 1914 copied C. [illegible] at a, lower sep. 2 4/2 ft interval. Din. subgrandata, Rhy. capax, [illegible] planumma, Str. retusta 3 ft interval, 1/2 ft Din. subgrandata, Rhy. capax, RX) [illegible] planumma 4 ft interval, Nr expressed, {at this horizon = Base of hard layers, Stripl. planumma, Streptelasma RZ [Plect ambra to small, c. 3 ft [Leptaenace. Rhy. capax Streptelasme [Helvotella inculta, one specimen at base] 1 1/2 ft 2 1/2 ft Stripl. planumma, at various 3 1/2 ft interval, Ostrea papillata 2 1/2 ft interval Leptaenace 3 ii. Streptelasma das. [illegible] ```)

2 1/2 ft stroph. Jd ammitma, at various in- 3 1/2 ft interval, or two papillata. 2 ft internal leptaeanae 3 h . Strong glasma large. 1 1/4 3 1/2 internal. Strips. Jd brrmmbrma c. 1 1/4 9 m. Strph., jd ammitma at intervals. 2 ft interval. Striph. Jd ammitma 2 ft 3 h, interval 1/2 ft Strong glasma large, singh. Jd ammitma 5 ft internal. Add on p 32 1/2 ft RY N end of culvert below RX. Should be 34 1/2 ft film RX according to direct measure- ment 2 3 1/2 ft interval, 5 m. Jd ammitma c. RA, internal 4 1/2 ft RX Diminished and sp. a dentu more common 5 ft interval. Fine Plate. various leaves. Dinillias subgracilenta rare. 1 1/4 ft interval, RZ Plectam bristles at top. 1 1/2 ft solid l. layers projecting. 2 ft leptaeanae m, whitish any. I, retreating Helvella maculata. 2 1/4 ft RY N end of culvert. 1914 carried

1914 Copied RA, thank you man. Strelitzia sulcata. Bleed ant mites cc, Str. Sulcata. Strip - jel minimum juglans. 3/17 interval, Strel. Sulcata. Streplaria c, Strel. Sulcata. (D.) Jugns C at vari nos 12 1/2 ft in intervals. 2 1/2 ft D. jugosa cc, 2/17, light me plenty + rattan bean, 14 heavy limt me, Wros sub normal 1914 interval. No exposures 14 Cland mte madizoneensis ccc, level, 48 1/2 ft interval. R. M'jicea ginkha cc. Diplorella, Defect remn Dimorphus retroza line 1ft wither Evidently practically in place. N 50 E for some cut on RR Half way between bed W and Wind E going north up hill.

Madizin. Caudised. Inver Columnaris Dinuthi striquadrata 27½ ft blw Colum 7½ interval, Net 10 Pleis antwortes 37½ ft blw Columnariz (Heterella in aqua) 41 ft blw Columnari three eggs in Saluda art 51½ ft blw-Columnaris N end of Ns bottom 62½ ft blw-Columnari Catayya leadi 76 ft blw Columnari Strph. planulata 86 ft blw Columnariz Strph. sulcata 93½ ft blw Columnariz Neargl. lare, 111½ ft blw Columnariz ctordanta madimms 130½ ft blw Columnariz First gull 161½ ft blw Columnari Dinuthi Retroza 178 ft blw Columnari Dulmurella jugo base 130 blw Colun Dinuthi retusa 171 belw Columnaris Man. Verrille, Canada 25 37 57 93½ 41 52t 37½ 28½ 58. 52¾ 41

(William Bairman) Robert Schreiber Mr Carthy creek 3 ft. H. miricupta wth. 8 ft H. riscalpta rita at species 5½ft vizcalpta, strptelaeura plannima, 5½ riscalpta, plannima - 115 cafax, palanderse lorne. 5½ ft, D nonuptle Leptona ) lone Plannima, cafax 5½ 13. riscalpta. Strplannimae c. lone p.lon calpta leptaea, Rhy,pulmilla 5½ft str. plannima, all lone Divalina retrose emeat 95ft {Plect animita lone Leptaeua, H.miricupta dune. 5½ ft str. plannima. {Leptalma, Daluanella fer 5½ft Strph. plannima c, ← 82 S strph. plannima lorne. 5½ft Dalmaciellae, Leptaeu lone. 5½ ft Dalmanella c, ←71 (5½ft inter val Dalmariellee str.plannima lone) Dalmariella cc 8½ft interval Leptaeua c. lorne)lone 13 ft, Dalmanella cc. Millng creek. Heavy L. wth. Dalmarella cc.(44) 29 ft interval Trudulasarg, rde, abundant. 44 {15 ft interel retrosea c, Pipe creek. Nend spectum 7, alng words road leading up and angle drill.

27 ft interval Tridacna arg, rox, abundant. 15 ft interval, retusa c. Pipe creek, Nendy rectway, along woods road leading up hill. S. retusa lone, angle hill. Boundary Hill RR cut is on Indian Boundary, Dalmarella here. repetition repeated, Blanchata 23 1/2 Clarksville 25 1/2 Ft Ancient 26 75 total McCarthy creek H. virgulta virga 128 - 33 D. retusa lone 95 - 20 75 - 35 44 - 35 84 total Nick Sengfeld H. virgulta Distance 38

Senfeld locality 15 ft H. viridipta c. 12 ft Calibrari 11 ft Leptalana Dolinmella Platystripluri Senfeld Old lense creek branch toward s. 8 ft Dolmanella c, Platystripluric, Middlages & Plumin radiate strue. 5 1/2 ft Dolnamellac, Platystriplic. Nebertallec. 6 in., thru l., Dlu. net near 4 minuta 6 in., Hard, c., Road leads up side creek s. 6 in., Slap, sulcata, Leptalana, thru l. 2 1/4 interval. Ophistoptera amerdensis, me 5 1/3 74 Dolmanella c. Platystripluri Platystriplic 3 ft Annulipalma alata c., arg. arde nesci 5 1/2 Plumin loma fow. Dolmanella Road crossing 3 1/2 ft Leptalana c., Dolmanella coc 13 ft A, interval. Road running over creek 13 ft interval, Dolmanellac, 2 ft Massive irregular c, Dolmanellac, 37 1/2 interval. F.T. Hewitt beds 2 ft after low. 2 ft morden ambden t.d.

Road crossing over creek 13ft interval. Dalmarella c. 2ft Massive irregular cl. Dalmarella c. 37 1/2 ft interval. FT current beds. 2 ft after clay. 2 ft nodular. Arnhem top. St Peters, S 1 mile. 3 1/4 Blue clay 10 1/2ft N. biscayta ccc. n. alternectora, 13ft interval. Str. mutans. Str neglecta. 5 1/2ft Orthotheca crinoides; First bridge. 3 1/2 ft Road leads SSW up hill. 6ft D. pigma c. Leptaena. 11ft interval. D. pigma c. Olatzytheki's cyl.fluctuans M'hirdrae, Leptaeana, Orthoceras. Fino. 2 ft Road crossing 12 ft interval. Crinulace at base. Large flat area in creek trbr. 5 1/2 ft Leptaena c. Dalmarella c. Str. planulata; Orth alata, Haoren semissa 3u leaf. Ref. laxiflora c. Cyclomena fluctuans 2ft. Leptaena c. Dalmarella c. Road crossing. 7 1/2 ft Leptaeana c. Ref. laxitylic c Dalmancellac cc. Road crossing.

3½ FT Hempfield fence on dwn side of road crossing. 1½ FT Dalmarella cc, Platysticula. Ovith. alata. Rcf. in Agas (Plectan. hirtus) 5½ FT 2 interval. Dalmarella 1 FT Massival. Dalmarella cc. 10½ FT. Dalmarella cc. 1½ FT massival. 4 FT interval. 5½ FT road crossing. Dalmarella cc. Heavy clay beds. 8½ FT, Dalmarella cc. mntg clay 3 FT Dalmarella cc. mntg clay Road crossing. 13 FT. Dalmarella in massival. 20 FT up out cross road crossing fence. St Peters condensed. 10½ FT. I nesculpta

St Peters undersea 10 1/2 ft D nuculpa 13 ft interval. str, neetamsi str, neglecta. 23 1/2 40 ft Leptaeana, 5 1/2 ft Str, plamlnac. 69 9 1/2 ft Leptaena 78 1/2 5 ft opith. plina atata 83 1/2 <pleidamintes, 17 ft interval 100 1/2 1 1/2 ft Massnel, 102 34 ft D ulanella C, 136 Sangfield undersea 1 ft min. neglecta. 27 ft interval 27 11 ft Leptaeana. 38 13 1/2 ft interval X 51 1/2 1 str. letrina 53 1 1/2 ft Str, nelecta, Leptaena, 7 1/2 ft interval 60 1/2 3 ft Str plamlnma fern 63 1/2 3 1/2 ft Leptaeana 67 65 ft St holintre Anheim. 132

Easty Dunlapville. S. Iron Creek. 71½ ft 66 ft. 60²/₄ft Lefdaem brrre 54¾up. Lefdaem brrre 49³⁄₂ft D.)'hprza ccc. 44¼ft up. 38²⁄₄ ft.up. 33½ft up. 27½ ft up. 22 ½ ft up 16 ½ ft up st. anlye du lrrre. st. sulcatalone, Lefdaem brrr. an. alata brrr. Lefdaem brrr. Same place as last on

same place as last in Silver Creek 50-60 (Lepidena) love. (50?) Stroph. sulcata normal and not 1 ft 3 in. interval. D. jugosa Cec. Lepidana i nite (49) 12 ft interval. S'tr. barata love (37) 2 ft interval. 2 in. setosa love, (27½ neglecta love) 35 ft interval. {21½ sulcata Lepidena}.

N.D. Collinville, this 4½ mi. My ford bridge - 1 mi. My thr 10½ ft up 2nd dim change from coarse gritty arg. siltstone to fine biddled clay shales above 54½ ft up above same D.in retusac. 25¾ft up, pure river clay with graptolites. 6½ ft up - Cyclonema fluctuosa 4½ ft interval, Plat. lgy & Septaria at same levels; N.W. 5 7 jacksoning 12 mi. 16 ½ ft Bridge Siltwood 89 mi.

5/7 Jacksonty 12m. 16 1/2 ft Bridge 14ft. Sttela arenacea Rad vssm = Lane, 196m interval wave in cltes N 5 E strong 2ft apart 3 1/2 ft inteval Plect anmites cc. Wave marks N 90 E, grvte stry, margining doni creeke into ripple marke. 2 1/4 interval Plectanmites cc. 1/2 ft interval. Ripple marks N 6 5 W. strong as first 11 ft intervals. Plectanmites to nut studa. Wave marks N 35 W, faint stry, 3 ft interva. Leptaena, Oeiverus small cc, wave marks N 40 E, faint stry. 1/2ft Retivella visculgetae massive de 3 1/2 ft shuffy clay Retivitella visculteta c. 1 ft interval. Shuffy clay, N. visculgeta 2 ft interval. cly. solid layer 3 1/2 ft interval. Lept aena cc. 14ft Leptaena & Ste. planum bno. c Wave marks N 80 E. 14ft Retinices germen disturbed St. Vistota I 2 ft - teral clay,

War marks N20E change to No. in short distance & both will marks 1 3/4 in turrall 2 1/4 {Str. reflectr, cc, Str, mut ans cc, Str. whita - 4 1/2 Str; Sol quabine Str reflectr in opp half. 2 1/4 dayg Mrdirtypes' 4 1/4 Leptaea at various leds Dalmella c, 2 1/4 mg. l, Dalmella c. XXXX Former retromza sucaba at this beginning. No expenses for quite a distance. Todd's Fork. Xerxes pike Glacial deposit. Top of Niagara shall not please

T odde Fnk. X errie j uke Glacial depost. T o f M ayne shale not plenti of arg, b i nter bedded Maynesh 7ft 9 in. Clay shale w ith few l and s i n courses 3 in th e courses at base of Mayneshale = 9 in Dayton st me. heavy courses. 6 ft 9 in.

4ft li Het. [illegible] flaminna Jed wellin 3 ft in Terraslayes flat Tetradim at top. Small Calyordruta circular planing 5 ft on level. 3 in, more nigbual, N100W, 1 1/2, plaminna, Rother prime 14T -> {Distinct layer, catminelytrista} sto {fluminna,

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Clarksville St my Hill no. 21 in. l. layers prediminating, 480 H. miscellita. plamwellia, plamintine, 24 in. clay shale. 459. 6 in. l. calcy? name marks N 85 W, in top [435] 18 in againt, 2 in lay. H. miscellita, plamintine, overdat plamwellia, Whitella. 6 in clay, 429 1 in. l. H. miscellita? pl ammbina 423 14 in. clay with several Ostracium (vay flat) at top 422 1 in. N. miscellita here. 408 20 in clay. 407 4 in. l. wave marked, N 65 E plamintine 397 clerudata are at top 383 51 in. Not expeled. Overth cliffy clay 4 in. l. wave marked, N 55 W, 332 Smjed int another, 9 in. sandy l. plamintmae 328 Whitella, overdata. ```</think>{'text': 'Clarksville St my Hill no. 21 in. l. layers prediminating, 480 H. miscellita. plamwellia, plamintine, 24 in. clay shale. 459. 6 in. l. calcy? name marks N 85 W, in top [435] 18 in againt, 2 in lay. H. miscellita, plamintine, overdat plamwellia, Whitella. 6 in clay, 429 1 in. l. H. miscellita? pl ammbina 423 14 in. clay with several Ostracium (vay flat) at top 422 1 in. N. miscellita here. 408 20 in clay. 407 4 in. l. wave marked, N 65 E plamintine 397 clerudata are at top 383 51 in. Not expeled. Overth cliffy clay 4 in. l. wave marked, N 55 W, 332 Smjed int another, 9 in. sandy l. plamintmae 328 Whitella, overdata. '} ```json {

9 in clay, plannima, Rebutilla occidentalis. Strigilazina Refineguina. 3 in l. Rafinezgmina. 319 10 in clay 316 3 in mudle l., Refinergmina, 306 4 in. Rejinegzmina distributed layers, 303 5th instar? Strigilazima, neglecta, c. Platystrobus contabellensis, 8 in clay 299 6 in l., Refinezgmina 291 5 m. Hylust Septaena seen in 285 Planclister this trip, Strigilazina Plannima, Rhy. dentata several. 20 in clay, 280 2 in l., Refineguina. Platystropheus, 260 4 in clay 258 6 in l. Septaena, 254 Refinezgmina. Platystropheus, 24 in not exposed. 248 2 in l., Strombus c. neglecta. 224 plannima, 10 in interal, l. o l. 222 2 in l. Strneglecta. 212 guitans, plannima,

5 in. l + cl., silt, plancton, 218 4 in. l., Sil. plancton, 16 in. clay, Thm. l., layers 12 in. chiefly clay. 2 in. l. 173 5 in. Repines grum disturbed Platystomina clarksoniana 171 6 in. clay 166 5 in. l., Repines grum, Dal. j'ayre, Platystomina 160 24 in. clay 156 6 in. l + l., Dalmarella j'ayre. Lamellibranchs c. 30 individuals (125) 12 in. clay 124 4 in. l., Dalmarella c. Lamellibranchs, Leptaea, Periophagus (113) 18 in. cl. 109 4 in. l., Di'jypnae c. Leptaea 97 8 in. clay, 2 l., Repines grum, 87 1 in. very thin l. 79 36 in. clay, Lamellibranchs (28) N45E, Wave marks,

1 mi., very [illegible], 74 36 in clay, Camelliachno. N45E, wave marks, 30 ft. apart, 3 in high. 11 in. l. + clay Dal. jujoca, Refinesquinia, Debutella occidentalis. 18 in. clay. 3 mi. l. wave marks. N+5, It. miculpta, Loma, Plammbina. 10 mi. l. + clay, plammbine. 1 mi. plammbine, Septaena, 20 in. rubble l. plammbine Septaena, D. jujoca, Platystrophia, 15 in. rubble l+clay, Septaena, plammbine Platystrophila, Debutella occidentalis, D. jujoca. 2 mi. l. 12 mi. d. + l. plammbina, D. jujoca, 10mi rubble l. D. jujoca, plammbine, Strelcarnea, 1 mi. Olectranmites ce., j'ugra, plammbine.

2ii. clay, 18m, rubble & Plecta from ts C. D. jngr.. striptlam plamhma, 5i'ds. very single bedded. 8ii. clay, 1k'.d. plamhna, 18i', rubble. long flat stretchy water up stream from culvert cemented or slope toward creek, A W Heyman Er J M A Smith

A W Heyman E J M A Smith Big 4 RR Station Sandusky Club Samples at South Lebanon. Notes for South Lebanon firm. Special Notes Cincinnati formation. Thicknesse & L. Avery.

S m Rm Limestone layer. 3 1/2 ft whitish clay. 10 ft to top y massive coal, or top 1 sample (8ft to walk.) 2 1/2 ft massive l, or top 1 sample 9 in., white var dense clay like Dublin layer 14 1/2 ft l & clay, 15 inches l; 2 other coarse grained, 5 ft, indurated clay. 11 ft. to top y Sample 2, put a fine lay 16 ft. to top y sample 1, Small branch design, 2 ft. B mider layer. 5 1/2 ft,

Strophula plannum ranges thru Charlesville, Absent lower 17 ftg Blanchester, Comes in again 1ft belm-mutano, thru upper Blanchester. Leptelna Comes in 3 ft belmv top J Charles ville To th y Charles ville. From 4 to 9 ft alvebene J Blanched From 21 to 24 // -- " // -- Blo Acantmiles 6 to 8 ft belao top y Charles ville, None in Blanchester, Rhynclatroma. cofea Comes in with upper vis cultor

Dalmarella End 4 ft blue intans. Smith Lebanon

Smith Lebanon 104 ft up, Rhy. nasuta, 98½ ft up, [illegible] zygaena nasuta, 93 ft up, dividing two streams, 88 ft up to 1 cent' em in no experience, 77 ft - 71y 11ft y l very abundant 66 ft up, Dalim and/or formen tentius C. 51½ ft up, Dros. &/a Dalim and/or foramen tentius E. 54½ ft up, Yrme l, w/tt. Dalim and/or foramen tentius, plectinella plicatella, 36 ft up, Bare 2 stretch filled with large blocks 20½ ft up, Wain marked l., N 70 E. 17½ ft up, Plat, str, pleur jendena, Pl. plicatella, 14½ ft up, Plect altus plicatella cc. cyclamund,

M. Leptaena cc. brongn. Leptaeana rare. Platystropha, yugrii stript de planis, Actinella cc. plannumma cc) yugria c. 36 in. clay + rubble l. with 2 grne fossils <Leptaena m ntm first. Nr Plectammites stript lazunly, Platystropha planumma, Dysgreate Nr new presented Hebrwella recently whitewater clay and ruble 48 in. chiefly clay + thin layers of clay and rubble Heberville, (9 1/6 in long pipe, Small Rhynchotrema pedanellus, Plectrammites grne again, 14 in. planummae. Dalmanella c. plannumma not cc & triptilaren, yugria cc, Plectrammites cc, 6 in n'tural planumma salten fnu. yugria cc, Plectramites cc, Syge 12m interral Heberville residentls. Cyelmina. yugria cc. planumma. 12 in n'tural, Plectrammites seems to disappear as Hebrwella residentels. strophanae st, layer with St. planumme cc, 19 m interral. chiefly clay striulcate & Nr Plectrammites N. Base of Heysman secto in my prof. St. planumma, ust common. Plectramites cc yugria cc spiral pla striated w bundles, 6 in m'tural st. planumma

17 m' interval. Plect antimates seems to disappear as Habitella videntalis, striplasma 2 layers with Str. plannum rae cc. 19 m' interval slightly clay. Striulcata w/ No Plect antmatmes N. Base of Weyman section very hard. Str. planum rae, not common, Plect antimates, or Juppra cc spirula pla stranded in bundles. 6 m' interval Str. planum rae juppra cc. striplasma 10m' interval striplasma cc. Striplo. plannum rae rare but 1 1/4 m' wide Plect antmites, 3/4 m' wide. Tremati millefermat ctc, 9 m' interval Habitella videntalis, Plect antmites - Plesma dewssa, Platytriplur clarksvillewrd. c Stripplasma rustiann B1/2m' long, 7 m' interval. Stripplasma rare + small, 2 m' long. Plectantmitos cc. juppra cc. 6 m' interval. 4m' interval Spirula rucula. strangocernium flat Calymene cc 5y8m' clay,

P 4h. Leptaeon Streptelasma, Plasmotma, Debutello Rupinesgura Olaty Strphiw 20m. chiefly cleg, Olatystplhia e. 7m. interval. 40m. interval. streph. vestita, juyza raro. 8h. neglecta, c., mutans, co. plasmotma 16+1/2 1941, 6m. interval 5m. interna Strenglecta, Olatystplhia e. Streptelasma, Debutello. - plasmotma. neglecta, mutans 7 m. plasmotma c., disturbed legs Plann loma. 16m. interval. 12m. interna Olaty Strphla c. Rupinesgura in edge, 6m. rough bedded, b. disturbed + 8m. internal. 6m. limit me. o Leptaeoa ce. 32m. interval. Robbee swan cleg., leptaea fer, 18h. Dalmata styza raro.

Refinegmina in edge. 6 m rough lidded, b disturbed + 8m interval. 6 mi: limit me. 0) Leptema cc. 32 mi interval. Profines sur les Lays, leptama fem 1/8 in. Dalmada jugza rara. in la via. Leptama, c. M radipeni vrsavilleana; 12mi, interval. 8mi interval. jugza. Profinesgmina crasa stupid asina small cc, jugza. 10 mi interval Cylinema liliy, platylopid "Antimeta" long blur arante fem, supersor live, Mrd Lepsos vrsavilleana 24 jw clay. Tetradium in siti : Waremako N 22 E, strong jugza c, Platystri fohn. Nebrilella, recidentalis, cc, Leptama 2, 24 mi interval. Nts Waremako, Nr Plect ambulos 1/4mi wide Leptema ear line. Platystrophx, lays. stripi milcata, c natm evgne c H, misculita, kara, plasmeme jugza, 12 mi interval, Mrdibpni vrsavilleana jugza. M. Leptama cc. luviza, plasmeme, cc

R 40 mi, Schiff very white clay Nauticella residuata, large, Jutlandellra planbrina. 6 mi, 17 mi. interval clay red 10 mi, clay red 14 mi. Nizacypa., Julanellra, 1 mi. interval Nauticella residuata, nizacypa, julanelle planbr 7 mi. Nizacypa, 3 mi. interval Mordostyga nizacypena, Jutandella, nizacypa., planbrina, cr 6 mi. nizacypa, 8 mi. Jutandella, planbrina planbrina, Jutandella) 15' mi. Q 3 mi, Sank frink to helm Jutandellra typka Pb, Cupers Large fort widgr A nixacypa ca. planbrina cc.

6 m. vz antp. 8 m. putamella plumbae plumbae, putamellae, 15 m 9 3 m. Wane marks N & S Same frnts as helon putamellotype Pls, cufys large font wide A virulpts ca. plumbra ce. 12m natural R. capax. small, H. vz antyda., c. plumbna e, 16 1/2 ft 196 15 m. natural, Wane marks N+S, 18 m. natural, wane marks Uaredita cc. plambm. 45 m. natural, 108-12 Wane marks stary N 45 W. 3 m. e. Partana papillata. 9 m. stryph. plambrna c. Refine grinta, c. leptura c 12m natural, 3 m. Stryph, notusta, c. Refine spary 5 m. Platystripha striptclaena large 5 m. clay P.

S. including Dinotherium subquadratum More rocky from Lofoten C. 90 in whitish clay + thin limestone Paranellina planulata, 164. Interval, Strophelasma duplicatum Heterella prudens 12 m' chuffel, Plectambonites 24 in cliffy very white clay R.

24th cliffing white clay R. 58/7

Blanchiert Chart Railroad level = 59 1/4 ft. 12 1/2 ft. interval. Pike level at pointy exit = -46 3/4 ft. 15 ft. 14x strph. mutans in situ. also neglected. 5 ft 7 in. lateral. (strph. mutans, neglecta, velusta, etc.) 14x 2 1/2 ft. interval. Strph. mutans from Refino quina tree right. Septen. 1 1/2 ft.

5\n1/4. (Staph, mutans neglecta, velusta long) 2 1/2 A. intercal. Staph, mutans long Refines grina tre rhytis Septemba 1 1/2 A. 2 1/4. (Septemna, mutans, neglecta) velustr) all tosse) (mutans + neglecta long) 2 1/4. intercal 2 1/4. Septena c, in situ. at two level, neglecta, retusta mutans are loose Septemna c, blummae co., BrAma schunndenes 5 A. literal. (Disjunct neglecta + retusta + mutans) 2 1/4 intercal. Ded. j'ayza, cc, Staph neglecta, 2 1/4 intercal. {in both side, Cutaggyga. Dim. retrusa, staph. subcata, 2 1/4 intercal. l mi. Staphi sulcata. Dimeritus retrosa. Catagyza trada; staphi sulcata. 6 mi intercal. Crista. lica cullita, 1 1/4 A mi. hlotisckelay + c. Septemna j'ayza cc. jel nunmae co. Platthjntin. Nistella nundentalis Lange. Dolmumellae. jel annaiae.

Point Pleasant opp. Mento 9 mi heavy clay. Layer top 1 section examined. 3 4 1/2 ft interval. Endorithus? 7 1/2 ft interval. Endonitus 6 ft interval. Endolithus 14 ft interval with Fullin forming lamp post, wave markers, clay 9 ft thick clay. With Endoliths in situ at top. 2 1/2 ft clay. Endoliths strike true. 3 ft Endoliths flush true. 6 1/2 ft Endoliths flush true. 6 1/2 ft interval, 2 1/4. Boulders bed 1.0 ft interval. 5 1/2 ft interval, Wave marked clay. 13 ft. Road level. [BR] These slates came from the lower 1 ft.

"R These slates came from the lower 1 ft of New Richmond Arothen cwm path cross gully, 88-10 2½ ft. 9 in. heavy layer. 9 ft 6 in. interval, heavy wave marked l. layer. 4 ft. cwm path crossing gully. 19 ft. cwm path crossing gully, 3½ ft. Plentideps Bronze Block, 13¼ in. interval. Opposite joined across the bare gully 12½ ft interval. 9 in. l. & mylaminate, with Leiodontus cc. in situ. 6 ft 9 in. interval. 4 inches l. layer with Leiodontus in situ. 11½ ft interval, 5 ft 3 in. Fault w/ Terrasenta oblique. Opp. cwm path with Leiodontus at top.

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Colonel Army Men - Mrs and Mr - Ruth Delegate, 4:30 PM. Thursday. Churn, three, expelled Rothko Grand,

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