Field notes, Indiana and Kentucky, 1910

[illegible] 50-58 59 69-113- 134- 137-139+ 242-154 [illegible]

12 cores per sample, 0-6 inches, more samples 6-18 inches, less samples. 0-6 inches exceptional percent. Mmty Fischer 31 W. 8th St, Flat 4, Fernel Dray Strer Syracuse 6-7 PM. Sawed in Race St, between Canal & 12th St. Braham Edgar, at Agricultural exp. Station Chemical Aid, engaged especially in soil analysis. Leo, F. Berckman. Chemical Aid of Rg Geo. Survey, Terrell, Joe Hittel at Hamlin, turns the country mill,

Der Stolley, Die Conchilien und Saurier-Geschichte Schleswig-Holsteins und ihre Beschreibung für Anna, 1895, Kiel u. Leipzig. Philidopsis cincinnatiensis Hall, scituncata Hall. Philhedra = Robbin 1889. Philhedra (?) = Columbiana Makott, Proc. USN m., 1888. p. 441. trout moneta, Hall. N.V. VI u. VIII. Pl IV.H. fig 21, 22, setigera, Hall, Laelia Hall, scaliora Hall, multipunctata Willyi zweizibis ? scabiosa, jurcarinata) Schm. aemignea Hall setifera Hal Tag. L. cetera Hall & Clarke jucschella " " cornuthista L-demi. muleyi', Cramoida ulrida aurora 1) Rätzel's Akademies der Wissenschaften in St Peters- burg. Cill. Vickers + Schmidt. 2) Muckewitz in Peru. 3) Tölzgenwist in Irland. 4) Berl. Inst. f. K. n. Leipzig, Cill. Nussbaumer + Rothan. 5) Palaeontologische Mus. Breslau, C. F. Roemer, 14) Paz. Revue, Tübingen. mit Grimbs attached: Grania, vitaceus to, Free: Philidops, alne grimbs Attached, a Ced. ant. luga than Ced. post. - Philhedra, acd. and small than Ced. post. Cramella.

Bauxite. Hays, U.S.G.S. 21st Ann. Rept. pt 3, 1901, p. 435. Roseleur. Handbuch der Galvan. plastik, 1900, p. 235. Useful Arts Revm. Richards J.W. Aluminium, 1890, Useful Arts. Minet. p. 255. Aluminium. 1905. Useful Arts. Henty Aluminium. 1895. Smith Inst. Ann Rept 1889 1889. p. 721 Brearley. Analysis of Steel workers Materials. 1902, p. 353.

Birdenville, Bed 2 Zaphrentis aquivalva Camaroplana muthensis Pecten oblongus Pentamerites folios Gyroptera Muckropta Prismofora serrulata. Beds 4,6,9. Cheta forma Burygo a + Branchiferia, Bed 10. Fossil form in Cement ine. Birdenville, Rather rare. Archimedes confertus Bed 1. Most common Archimedes smallmanni Archimedes lateralis Archimedes muckmanni begin to St Genevieve Falsamia triforma Bed 2 Pterocrinus middle Colpitals Pterocrinus acutus Middle Pterocrinus depressus middle. Pterocrinus acutus Middle Birdenville is most from lifera Archimedes Terebriformis is very common.

Birdsville. Camarsphria wortheni, Ind., 11th Ann. Pentremite pyriformis. abundant, Sandstone of Birdsville are mini laminated while those of Cypress are more massive. Shales in Birderville but not with Cypress. Send me with the boring beds of limestone = Birdsville, with my thin layer of Limestone in Egisto Cypress. Birdsville limestone was weathered to rusty brown yellow. Fossils loose in trip, { Semi lithographic limestone now, from both a deeper Birdsville = C, Membrane - "ligny" plated chest, interfolded shales. Shell so, blue the chesters } Derbya crassa, Spinifera vesicosa larger in fresh but thin in Birdsville. Zaphrentus spirulosa in Birdsville = 2x in Osara VIII,10. Tribune Agassizocinus conicus abundant. Tribe met rare. Birderville. Productus fine ridges, silicified. Pentremite pyriformis, Tribe, recced Birdenville abundant Productus crna Less rare in Tribune More rare i. Birdsville. Lysipora rara Lysipora ranosculum. VIII, 20. Lysipora lehara = smaller species. Pentremite gordoni, Common in Tribune: Eolite 2 specimens with Archimede.

Cypress a d 17 Rene m Cypress? at etc. common name Bindsville, Tribune Centrumia grandm, cabana At once an plant impression, Worby fites yoper dendendron a are. Zaphrentis spinulosa, small form, larger in Bindsville which see. CleiThrysus subannellata Tribune's indouille cabana Freedmite

Ghara Meroblastus glaber albara Tribune? Wafim Fretelinta, aber. S. p. in ferina in Merroolana, XII, 9de 3 pds. in a T. Anos seven also - Bindonville, VIII NO, 35. 3 pds. for in Meddencens - half as large again, Bindonville, 5ed end of this section, 5 sided Pentheomite Arms Cornua R me elsewhere. Sphyr a m mordana

Rosiclara calcareous, Fresh green to gray, Weathered reddish & red porous. Distinctly lamini- nated, lies in bundles at all angles. Very common. Ram's Horn Freesonia Platyorina littoralis, twisted column, Freesonia Cytolasma quinque- septatum Cytolasma myosum Lithodion luminidto Michelina subanosa Most common. Oolite never with Archimede. Oolite very common here.

St Louis Frederick's limestone weather for less readily, St Louis weather more readily, Henry Shuck Ford St Louis. St Louis Very Rare Spirorbis intricatus Archaeocidaris with one lower. Orthoceras comus, lower Melinites multiporus Lower Lithothamnium caudatum, everywhere. Lithothamnium proliforunm Lower, everywhere. An Archaeocidaris but smaller in Birdsville, not specified Michelina much larger. Syringopora commun. Mt Sand debahus Trick at that heavy platy Frederick's chest more platy than St Louis chest = rounded nodules Ordo more frequent.

Spengler Believed not to be there, Parthenite considers Spengler? St. Louis? Friedmua Pugmax Grosseri Spenger St. Louis Friedmau Cleothyrus binata Spenger St. Louis Paculus Pugnap montatus Spengler Friedmua Ahena Semimula trinuclea Spenser Friedmu Ectynotria vera vermiculana Ic evergtheni semimula ont-gua drata evergtheni Spengler to Bordenville chama Dra'huwe Bordenville Blad Fin? Chama Friedmu

Tullahoma Almost complete absence of frassles. Chest highly plicated below in trichina. Dark colored shells with red rids in chiefly limestone micas, Spirifera spirata Rare in Ontario comm. in Birdenville; Spirifer macdougali Larger in Labyrinth than Birdville.

Mead Breckinridge Grayson sketch Hart {Greene Taylor Ladair Warren Edmonson sketch Trigg. Lynn Caldwell Griffenden Huntington Christian, Wall map.

Meade 40 ft sandstone 15 ft limestone Cmendia, lowest limestone 10 ft. Paynesville the limestone larger of preceding section is absent. Chester SS. & normally 25-40 ft. Coarse gray limestone II. 5° Only in large flat area region. at Paynesville, Dead Arable Arable on west; and Copet, Richards on south is green shale with several cherry coral. Section: III. Sandstone, shaly above, 350-40°, II Limestone 5° Green shale + coral, 1° I. Sandstone 25-40°, IV. c. Dark gray with peatstone pebbles b. marly shales a. crystalline limestone 25 ft. In shales seen only Petus Hill at Huff around Paynesville. A mile E y Cm India Mile west of Thompsons stre. On all cases with plenty fossils.

V. Light yellow SS, 60-75o 3 metres, slaty. Cojos Peter Hill at Gno- tim. Also Plateau from Payne's ville to + Legrand Rhodoba, also N to Concordia. VI. Bluffs & J of Concridia. Yellow from lifermol - 3o Oolitic l, pentamites Archimedes 6° Yellow phosphorimed l. 6'' Gray siliceous l. 3o Coarse crystalline gray l. 4° Hard dark gray coarse l. 3° Total 20o Reduced to 10° at Adam Creek, VII. Slaty SS, very creek to Thompson mss at NE, Fossil Sigillaria. VIII Yellowish oolitic, A couple of miles E of Concridia Also SW of Morleyville IX, Yellowish SS, 65° VIII Liptitic l. 20o VII, Slaty SS + Sigillaria, VI. Bi'mest me, (one red & one gray) 20o. V. Light yellow SS. 60-75° IV. a. Dark gray l. with Pentamites b. Marb'd also with plenty of fossils Pentamites Archimedes to. a. Angular lime l. 25° III, Standard me shely above 25o-40° II Lignitic ms 5° Green shale & Coral 1° I. Sandstone 25°-40°,

"Section E of Pangbourne" SS --- 450 ---- 450 Dark grey argillaceous l. with pentamerites 50 Shale, Archimedes ++ 150 + ultra Crystalline l. 250 Sandstone 350 Dellmorth l. 150 SS.- Green shale + coral -100 Grey limestone 100 Impure friable l. 350 Cretic in bed of branch 30 Fossils. Archimedes intermedius swellgrani meckanni Atyris trunclua dist ans liventa argosi= anthlamella Amistrupa sylvia Fistulbyra Fluentilla Olypura cestriensis Productus fastigata elegans cestriensis 15 ft shaley above section occurs in deep cavines in part of time 110 ft below summit of plateau, connected with Dead Horse Hollow. Kinderlens 300 limestone. Pentamerites symphysus Meade albinus Reticula rara Spirifera lucidus setigera Spiriferina hana rara spinnra Stenypora polymorpha cestrinensis Saccophyysia longibrigaei Spiriths Terebratula formna tubigida Zaphrentis opimalipara. Fine sections at Kings landing + at Concordia.

Thompson's store 150° 45° Green shales Whirl. 75° Grey limestone. 30° Big Clifty SS. 60° Cement with chert. 90° Lotic l. 75° firmstone. Whirl Fossils Head of Day Creek valley 1 mi West of Thompson's store store & 1 mi N of Bennett's store Archimedes intermedius Athysis trinuclea Cypr. parictya Fistulifera excellens Terebratella Phyline Productus fastigatus Clathriscus Pentamerites gardini jayii Morris pentalamel arnold colvin. Spirifera Ardyi. Spiriferina transversa Spirifera polymorpha Zachanthus spinulifera, at wells slate quarry, Meade Peter's Hill at Guston, SS 50° Gray sand l. 15° Crystalline Lode 3° SS 12° L. feathery foot fragments 2° Rough l 10° Fine grained l 2° 4 mi west mi & sandy 5° Fossils Montz shale 10° Big Clifty SS 50° firmed at Guston 40° Indian Hill E of Grahampton, SS 50 ft,

(illegible) in (illegible) to grassy at top of Mr & Mrs Chater's SS within for flagging 1. Saffyell nr SS - 10-150' Big cliffs 3 S. orland & under land to flagging at me Sandy, Section: Sandysholes 100 Massive SS 150' Smytholes 100 Ely very dark crystalline l 100 Mrs Blue crystalline l 100 Quarryd S of Smythole Mr. John Wimpss farm - 600 twice St Louis trip, 8 hrs at Chester, Crystal anthr. Anderson, east of Rosetta, east of Barclay ville. Back y Pierce Big cliffs SS farms fairly good farms, on low flat mylands. Moderate crops of stucco grain & root mdths,

1 lb. Limestone 10"-35" Heavy reddish blue and gray limestone, very fossil- iferous in places, occasionally orthoc. Grunwald Pentremite Lower Archimedes Perdretre Lower Penremite. Archimedes remains. Hill N of Condon's home Limestone between Hill's and Cowley's Mills on Smith Creek 100 ft above creek. Rims under drainage between Frank's Mill & Mc Danelle's, On ways between North Fork & Calamazoo & North Fork & Merrill's Creek. At crossing of Hardingsburg & Burras pike over Int Run= at Int Run Church, at Hardinging at E. 109 ft below surface, at gas well. Hardinsbury Webster Road crosses Durrigee at 665 crosses D creek at 712. Hardings creek just beyond new school house 4 miles from Hardinsburg on Stephens post road; where creek turns at right angle = 260 thick. Fm Shet Branch creek in S side of xxx Sinking creek just below xxx Little Falls, top 10° above low water at stephens pnt, xxx Archimedes fossils well shown Cedar Grove landing at base of hill. Limestone Cliff on SS at well on bank creek mouth.

No 2 Sandstone Under Breckenridge SS. 202600 - 1500 thin bedded to crasse and crassine, or as I malk cras bedded. Stephen joint. 20-250 on No 1 limestone one, on Union Star grad joint and J Barnett Artis. Forms surface north of Preston Flats, First reg in Breckanridge Just N of Hardinsburg on stephen joint road, aling Hardins creek. Section here = Sandy shales - 10 \ No 3 Massive SS 22} Marlgy shales 20} Limestone orbito 25} No 2 LS Syft SS, with mark shale 38} No 2 SS Hardins creek. Stiles Still falls at Hardins burg + Mottings road and one clear Creek to Clear Creek church, Section line = Top of hill No 3 SS - 20 Limestone (Cross) grits old to Element, shilt, t red sand - 40 Heavy SS - 79 Dark grey L. (No 1) Bed of clear creek. SS ridge on Grand Grafield just at top of SS, Asphalt Mine of Breckenridge 2 mil SW of Grifield is in this SS, Hardins burg to McDannells after crossing bridge over North Fork. Section line = SS 30 Shale Thicknes 2} No 5 SS Thin SS 14} Limestone (No 4) - 17 Covered space 750 SS (No 3) 210 L (No 2) 48 SS (No 2) 32 Cannel 10 03rd of creek.

No 2 limestone, High porphyros, Pentemrite & Achmader. Road from Mr D annells to Winchells Ford shows well in hills on each side of small creek just east of Mc Dannells runing under SS No 3, until the D annells is built, cant survey again between their bridge across Ant Fork, Just below Falls of Pumph, Head of Doddrige at Aplbiers, Tig Hill. SS No 3 - 25 Pentemrite - 24 Shales 31 Buffel 5 Anthracite 10 White Pentemrite L 5 Blue L 5 L & Chest 1.5 SS No 2 35 creek, No 2 L Stephens first in 10 me. they read! 15.0 SS - 10.0 Thin SS } 5 Black shale = Chester coal field 5 Covered 10 limestone 1.0 Marb, shale 10 Covered 2.0 limestone 11 Red & green sand 15 SS No 2 A 10 Old SS 2 Black shale 35 L w/ red to Anarry, 40 Red & Green Marl 5 SS 25 shale 25 SS 10 L No 2 L/M in water. Marb of No 2 show up around Union Star, in Mead Co Anarry at Audion. Farm of Mr Chas Thirkins on ridge between Jordon & Bull creeks, Upper meul 40 under L. 30 above RR in Burling Green Road out of Glenn fort. Under Black shale & No 3 SS.

No 3 SS. High ridge E of Minni Star, Slope N at Minni Star Old ridge from Stephens- just in Harding bury and, spring at New Picket Church Rich house SS at head of Short pinch creek, Best SS spile Hardingsburg SE to Harrod & benton farm. Tar Springs are at line 7 SS No 3, Fine water resort. Wheat Creek, above No 3 SS Below No 5 SS, Small area, No 4 L iron, No 4 SS No 3 L Hinesville and W of Clermont, High hill, 25- S No 5 R 10-40 Marl Buffalo Mullen Way 15 limestone, excavated L 20 S No 4 10 Bray Mill 20 limestone } 50 shale No 3 L 5 marl 3 limestone 10 Thin 20, 30-150. Massive 22. R fine stratified bouldry rock Conglomeratic, Similar section Clermont to Mettigny.

No 5 SS. West & SW of Clermont st into the hills, Falls & Roughs, 500 SS 10 shale 1-3 Cral 30 SS shale 40 Limestone S Green Mual Buffel Shunerton Shunton Mual No 5 SS 60 SS 45 Grey mark, Crumeteld [illegible] 12 Burnt an 15 Crumal 5 SS 5 Limestone 3 shale 10 Limestone 5 shale 5 Limestone [illegible] in water No 4 SS No 4 L. No 32. No 3 Abrev SS Highs Mountain ans, No 2 L No 5 Limestone, along Fordsville Road 1 mile east of county line, also near face S and Knots SE of Glendale.

Graves Cr. School Lime Spring, 1 mi S of Gygnite Rd. Trowil leaves Leagrange near foot of Huff's factory, Mayfield and Boaz. BOARDS (Cedar fragments, Red oak + Black jack have shining up since forming Lignite. Best at their land. Gladley Land = Whitts whit. Pant Oak + Hickory islands. Dr. Atkinson's Land, Granfishing. Clark Valley Flats. S of Radneek; S of Adams' mill in valley, and S on hill 3/4 mile in valley, the sandstone sls along 2 ocean front centers. Graves Cr. Lignite beds in Vanvity Canthus Cr., a little North of Mayfield, in O. White's + O.A. Ormondwell farms. Best at Whitts 3 ft above water of Creek. Lignite part fully broken leaves, etc., and Centers Creek project area, Black Clay, La Grange Group: Leaf impressions in clay at Boaz on CO+SW Rd. in N of county, 150-200 ft gravel Quaternary drift appears SS of Lynville + Bellevue and Horvatine + chest fragments, round gravels, pebbles at gravel bed. Best seen deep aquifer cut by CO+SW Rd., 1/4 mi N of Boaz etc. Profile clays at here contain leaf impressions. Big Inlet = 75 ft above water valley with stream Mayfield - above on county gravel. Burning Coal & Lignite in Ountman Creek, abutting Mayfield, 6-80 feet in upper parts White pipe Clays abundant near Boaz.

tube factory at Hootz station on L+NR R. S of Louinville (w of Smith Park) on road to Brooks. Louinville. Oklahoma. 5 miles to Okalon. Barkes.

Linyester Cr. Johnson Cr. Lythart 100-175 L, 144-177 I (73-165 S 120-150 II 65-115 L 60 III Binhomville) 37-75 S 50-80 IV 315-430 { 40-125 L 68 V 102-250 S 72-100 VI Tribune 170-150 L 156 VII Cypress SS 60-150 S 150-250 VIII Chana 121 Bizzell Bluff Ron'daine 4 " " Fredma 56 " "

Clarksville silty loam Soil 6" light yellow brown silty loam chert (20-50%)? Subsoil 30" chert (20-50%) Residual country limestone + granites. Philadelphia, loam Soil 6-15" fine loamy silt loam light gray orange, lime Subsoil 30+ red sandy clay Mixture of Lafayette sandy clays w/ d. Clay? Domestic settlers. Surface drainage poor. Rolling land. Good for peaches Cotton? silt loam Soil 8" silt loam light gray Subsoil yellow compact silt loam silty clay reddish yellow or red. Residual origin Barnesville Flat w/ detritus droughty, not dry for tobacco, strawberries Cautious for cotton? clay loam Soil 8" silty loam reddish brown Subsoil 30" silty clay loam red & heavy Residual Loamy under- lating. Stony fertile Best farm land. Tobacco beans, yield, but not best leaf.

La Grange. Orality in Saluda had 2 mi S by La Grange on the Gallatin rd. quite a large quarry in the form of sinks. Craft's livery stable - Mobile, Tenn. 1km very Shipy & then 2 1/2 miles west. 4 mi chpt & bend forced to SW. [illegible] force + plenty of small chert 4 ft upper bed prod clay 5 ft 9 in fairly solid white beryl cl. 6 in basal loamy (on road directly) 2 ft Chert 8 1/2 ft hard maroon Saluda 47 1/2 ft soft Saluda chalk 43 ft cherty feldspathic subquadrated top, Tetrachite layer 52 ft clay shale chalk 2 ft 6 in heavy limestone 46 ft [illegible] Corner & upper Gwynne Hill 8 ft, lined me [illegible] 31 ft stream level. Walden meeting of bull & about 5 feet of face of Louisville directly above. [illegible]

La Grange Grassy in Saluda bed 2 mi's E of La Grange on the Bolleville road, just a large quarry in this locality of silt. Crab's livery stable. - Miler's town 12 m s w. Slip & then 2' m'so mud = 4 m's ch'd & bend faced to SW. Sandy face + plenty, of mineral chert 4 ft Mpyzn Bogood clays 5 ft 9 m's fairly solid Mpyzn Bogood l, 6 in basalt layers. On road directy 2ft Chertm 8 ft hard massive Saluda 47 1/2 ft soft Saluda chalk 43 ft ch'ch from top, but my subquadrata at top. Petrachin layer 32 ft clay pink chalky, 2 ft 6 in heavy blued m 46 ft. Franis Corners & upjn Lollyfawn Blm over this 8 ft. Kinrel are layers 31-77 Thrum level Waldron meeting a hill + about 5 feet of face of Lowerville directly above. 0.23+/- 6' Proposed MMS [illegible]

52 5 miles Alford start to Bedford. 4½ miles to Alder. Aldham Landley & Johnson. Aldham is opposite Bethelhem about 6mi = 4 mi to Jennings store = 2 to 5 miles to Salpham. Bedford. 53 At John Magan's 4½ miles South of Bedford there is a good exposure up to the Upper Oxford Clay & Agar to the lower Saluda at least. Upper Oxford clay. 5¾ Bedford limestone. 5½½ indurated Lower Oxford clay 20ft 14 ft soft whitish Lower Oxford clay Oral Niagara Clinton not distinguished separ ately. Saluda bed well exposed. Mt Pleasant ¾ mile east of Mt Pleasant) 42ft Lateral limestone Oxford Saluda Versailles. Slightly farther next ½ mi east of Mt Pleasant, where road into Johnson Farm turns off North there is a glacial gravelite boulder 2 ft in diameter. Spring in Bedford. Well maybe 1 mile from Millburn comes at base of Oxford limestone.

Peter Hill Clinton Fitzgerald Pangerville 300-400 yds below farm. Mr. Clark's land. William Hendriky, call up. W H Rhodes at Chandler. try to find out about fossil. Mine solid sandstone 10ft shaly sandstone 20ft shaly clay 10ft No 1 limestone 10ft, clay Peter Hill East side, giving up. fossiliferous clay - 16 1/2 ft Disintegrated limestone 2 1/2 ft limestone and fossiliferous shaly, 23 ft Unknown interval, Scanty of limestone to top of hill. Section N of Sample RR station. More. 40 ft limestone shelly, 58 ft clay, near top and bottom shaly over middle. Better partly exposed near middle. 10 ft limestone, 26 ft clay marl. 34 ft limestone sandy clay marl.

East y Hardin Springs 63° { Brown massive sandstone. 230° { Marl fossiliferous at bottom Collected. 34° { Very white limestone, oolitic 22° { Clay and Rickly fossiliferous collected. 36° { Fossiliforms. Fossils collected { Limestone some of it fine grained Rough creek. West y Clown Creek Church No 3 Sandstone, No 2 Marl No 2 Limestone Fossils Collected. No 2 Marl No 2 Sandstone, No 1 Marl No 1 Limestone Productus cinnam. at top.

"2½ mi., W of Richards mill, 103ft. My position with Amaker party NNE 38ftS and out mrs. I do not see. #4 ft. from terms (collected) bison? 87 ft. From stone Orthornus Craniensis 4 car. W of Bumble Green, alme clay clay impurity off north. near farm the Bradley, firs. By Clifts 2 and out mrs is 100ft above Paddern Tinkers m on the lowest one layer quarried at the D.J. Sweeney Quarry & Monument Parkman. Directly west of 1289, SW of Sharpsville, chint in bed base. ½ mi's Belfast led. 10 ft clay, surficials, considerable joint jumble. 7ft6 in thin limestone + clay inter. banded, some of the clay jumbles. Platystrigelia collected. 1095- 1010 65 4230 13 15 1/2 = 5 ½ ft.

Spirifer reidyi? lei'dyi. small. bifurcatal The distinguishing feature of this form is the intercalation of one plication on each side of the 2 forming the median axis of the fold, and of 1 additional plications on each side of the fold, or that part of the lateral slopes which is nearest the fold. Also, one additional plication on the lateral slope, next to the one bordering the sinus. These features apparently are not possessed by Sp. lei'dyi. Since the types of Sp. bifurcata do not show intercalated plications, our specimens can scarcely be identified with the latter. Most if our specimens are distinctly smaller than Sp. lei'dyi. Listed by Ulrich from Spirifer to Birds ville. Similar specimens with less prominent plications seen in Freedonia Spiriferina spinosa? norwoodi? Our specimens have the surface ornamentation of Sp. spinosa (Hall & Clarke, 35) in a general way, but the spines are much shorter, almost granular, and are confined chiefly to the ridges, being usually absent in the lower part of the grooves. In specimens as large as that figured by Hall & Clarke, the number of plications on each side of the sinus usually equals 5. Our specimens may agree with Sp. nor-woodi, but usually are not rounded at the ends of the hinge line. The number of plications on each side of the sinus is 6, and this number sometimes occurs also on each side of the fold. The plications are stronger and narrower, due to the greater depths of the intermediate grooves. Found in Chera. {Paynesville. {Ey Banks Spgs. Burling Green Listed by Ulrich under Sp. ex Norwoodi from {Trihome or Birds ville {Chera {Freedonia {Spotsylvania. Sp. spinosa is listed by Ulrich from the Trihome + Birds ville, and our specimens are much less spiny.

Bone. 1697. Clay, 3 mi N of Burlington [illegible] [illegible] and light blue colored. Kent on. 1581. Silicious Grit, 1st toll gate, 2 mi from Crompt on the Lexington turnpike. Shale. 1582. Same, used for molding 2 cord. 1583. Clay. Cincinnati Group, same locality, just below the pits above. 1584. Clay pit at bridge yard, Head of Pribbell street, 9th section. Crompton 1585. Marly shale, Junction of Ohio and Licking rivers, 12 ft above low water mark. Cincinnati Group, 1586. Marly shale. Fine shales between impure limestone, Whit hall, 5 ft above low water marks. No fossils,

Campbell Cr. 1322. Sand, Mulding, Columbia Trace, ½ mi NE of Newport Reservoir. 1323. Sand beneath Berkeley, Columba corner of Harris' St. Newport. 1324. Virgin sand. Old wood, farm. Gen. G. B. Dodge. Flat woods. Waters of Phillips Creek, 1½ mi SE from Grant's Lick. 1325. 1315. Mont shale, Cincinnati Gr. ¼ mi from Newport. Alexandria turnpike, upper blue clay, dark gray soft shale. 1316. Mud from siliceous sand- stone, of Dr Kinin. 10 ft from surface. G alluvial soil. 8½ ft colored friable fine sand. 1317. Clay shale. Newport Reser- voir. 340 ft above Ohio, 6-12 ft from surface. Clay mixed with a few limestone layers. 1318. Newport Reservoir, upper blue clay, 320 ft. 1319. Bride Clay 3 ft above ledge with red shale. Newport. 1320. Sand clay 3 ft from surface. Not Volcanic Red, ½ mi from Alexandria turnpike. 1321. Ferruginous clay and of mud, 1 mi NE of Grant's Creek. N head waters of Phillips Creek.

Linderwenda, at Pomana in Byggara Northern Shaw State Silurian Associated with Gen. Strata F R Carpenter Reed. Mrs G L Elles. Sparta: 40 ft NNE to top of Cygnet aug 1 mi E of Sparta the Cygnet aug dips eastward and up to this point its dip was west. At Sparta the top of Cygn aug came to 12 ft below RR station, 82 102 184. No true base 82.5 above bend in Elburn Ave State where it is joined by 1st strike trace. 98 ft mine down to river bed 4/4 more clear to RR. Grand Central 490 430 2m water 60 50 10 ft above Cygneti 82.5 ft. 98 1.4 194.5 69

Principles at Glencoe, Illinois + etc. No type + & den contract part of cut only mark post 28 from Cinci noti. 3rd with plane mania 1 3/4pm way Garcia = 27 3/4pm from D Electrolysis electrolyte common himent in hot type, 220 Volts 110000 ohms 5/20A 1/2vr supply. Garcia. 220Vht 1100ohms 1/5A 50r 140 Volt supply + cords have failed Arise from = 755 Watt. 1/3 of 755 Watt line failed. 1500 Volts used in electric cutters at times without success, Amperes Volts Frequency of all Time Resistance of Arm Direction in body Psychophysiological Role of animal, Sleepers occupied sports of learning, Chloroform restored. How very susceptible Very little "+" Breathing + Heart action stopped, and cerebral pressure increased, + Animal Head raised to decrease cerebral pressure. But not type. Artificial breathing 18-20 per min. Breath not stopped by electrothermy. Whistling noise when successful. Rough brushing of soles of feet + No alcohol. Repeat up for hours. Physician, Injection of camphor. Luminal fragment-m. Heart Massage. Last record. Second application of electric current; [illegible] Pressure of the magnifiers. Some E & F side a where conditions to be carried on further read, associated depth. Electrolysis electrolyte common. Palmo, sensibility common + Stomachic nerve impulses not at days. Finds the Principles of Dietetics Robert Hutchison. Edwin Arnold, London.

72 Barren River section. Glasgow to Scottsville road, 1/2 mile E of bridge across Barren R. Top section in J F Harts land. 43 ft loose chert fragments in soil along hill top, with fossils, including spirifers. But it is not certain for certainty within this belongs to the Harrodsburg limestone, at least no Rhynch- orrella dulin was found. 42 ft, shaly argillaceous rock, with few stelloids and crinoid beads near top. This is the upper part of the Keokuk formation and resembles it closely. 30 ft thin shaly argillaceous lime- stone. This is evidently merely the calcareous phase of the upper Keokuke, if it is the representative of the New- Orleans clay series I do not have the proof. This part of the section is best exposed 1/2 mile east of the Bridge, at the Big Bluff on George McKimery land, although it was exposed also in the W met on farm. 6 ft cheesy white limestone, ex- poded on both farms, best at the big Bluff. At some localities its lower part of the vulgury section is less solid clearly this pure solid lime- tone section appear 11/2 thick. 73 55 ft Black Chattanooga slate, thin fissile on G W McKimery farm at big bluff. 8 ft. Devonian limest are, blue gray and the dark, with pieces of fossils except one layer about 2 ft from the top which containing crinoid stems; Nothing else recognizable. This layer is solid to lime- at me. Only seen in George McKimery farm. Hurst farm. Stock farm Black slate Big Bluff on Farm. Black slate Woods cutting Gate Gate Bridge

74 Petroleum, Ky. Visited Sarver's farm, M'gheim, at NW corner of Indian Cem. every half, 1/2 mi. East of Bridge across Drammers creek, S with side of creek. Base of New Ordinance. crust was limestone. Phosphatic nodules scarce 4 inches deep. Black shale

76 P4 Pleasant! George Jerry Delaney Swickton, Betne Walnut Bmlder ledge about 4 feet above the water. 2-3 foot Dark ladye. Only one ledge of bluder lidge that was worth quarrying, about 6 in thick, it is as good as ledges below About 3 n 4 foot ledges bellow the bluder ledge, one 12-14 inches, two or three from 3-6 in thick. Never seen another the larger ledges. Black quarries Used for building stone, about west of Southern bridge on by way. Occasionally from bluder ledge, 5 inths & dykes. Hill sometimes worked before the beach quarries w/ &' w/ clined a railroad. Beach quarries next long after, two miles after; 77 hills & Hyde park on Madison road. Takes Madison & Hyde Park car, P.J. Delaney, 1768 & McWillie's North 3379 R. W.H. Mrs Cox first quarried, Wayne, Armacoost & bulking quarrys, opened up in in 1867. Last quarry in 1887, Ernest Armacoost forty yrs old. Heavy building Turtle back came bellow the boulder ledge Better mine below.

78 New Richmond eden Fulton layer 4 1/2 ft with a few nodules. Cypridina, Dromideus 11ft below top. Alt. 15 1/2 limestone. Clay or limestone. AT A. Stephomena magp villensis half a dozen specimens in a small circle - This Stephomena magy villensis formed about above the 123 foot mark, a distance of 50 ft. = 73ft below O. cornville Rafinesquina nasatae clay layers. Belleveire lynx = 22 37 Fairmount -552 down to Steph magy, 28/64 s.s.magnitella G9:70 1/7 down to culvert simpl. magnitella 22 Mt Hope 17.5 Dalmanella multisecta common, Calyptraa verdispon. 14 Pleist. fucoidata loose. 79 Berygium. Rafinesquina nasata in lower Cornwall over the Lynx beds. zone. Mt Auburn. Top of bluff arcte Mt Auburn 22 ft, accurate includes lynx = (0-33 ft is bare of cliff) 0-46 ft to bed at turn road Coryville 69ft 0-59 1/2 ft to yellow rim 0-74 ft to earl J. fence A culvert 0-91 ft to culvert 0-108.5 ft to Dal. multisecta com. Small Calyptraa, v. disca. 0- 128 ft to Pledwillii f. vivens to Bronx. Bettel 930 160 770 above 444 326 87/52 fldm. 137/22/159 39 ft Tr face of Mt Auburn? 28 28ft to Grey clay wth Steph. annulata 22 ft bare of lalote to Steph. magy. 87 ft time of Mt Auburn & Steph. magnitella, White oak: Dalman. multisecta Cypridina Calyptrae normal Pleisoclymbe virida.

90 6 mi S of Brooksville on road to Mt Olivet, Mt bridge. Trinellous + Plectambonites above. 34.5 Limestone = Nicholas, from 315 to 38 ft. ft above bridge across Camp Creek, drop from Augusta to Brookstone 42 ft 7 mi. S of Brooksville at bridge across W Fork on Mt Olivet road Mt bridge Dalmunella eriacrata not comm. 15ft Bryograms at several levels Plectambonites abound out at top. 72 ft interval Large Dalmunellas 66 ft Interval, Bridge level. 20 ft Interval W Fork level. 475 ft at Mt Olivet highway Bethel 42 519 at Elm Grove 137 380, top of side, 240 140 = base of bedro. no sign of Niche has beds here. What does this mean? 65 ft from line of massive straths, andgyr's limestone times to made 12 miles E of Terpendixy, Stropho. wavy villanari. Hamilton school house 2 miles NNE from Brooksville. At Oakville 3 1/2 miles N, capstone road turns off at any bridge? At Lee's Caste 4 1/2 miles NE along limestone free of straths- but wall- 66 ft below top of that The limit now are full of water in caverns from 50-60 ft down. From creek's ear Dinner was Del, Dalmunella directly beneath,

82 East P. East East P. Clover clover Bantam Poplar Poplar NW Bethe 83

84 Fate? n white river Cat Park from Providence. Phelutlis neglecta ph'catella! found w'th 16 17 place of luxury dinner one with Lemmatis simple, wrapril- lissus. Dolie anulla multirecta is Canon on incorrect hatch. Later this luxury limit Stopho decagrella an slint the stophs. magrithemis is not found in these Dolie anulla lids. Hence within Phelutlis forms in upper to down upper older here can sort by dexter- suriled from not stops, a mediin large Phly suggesting beyond was found away w'th Phelutlis but not well exposed. 250 ft to basey heangl with St. maypr. 87 ft to culvert 33 ft above RR bridge. 320 ft total above RR bridge. 60 altmt 380 ft above river shore, Danis quarry Crs & O. New Appondell Park license on Front Str. Newport 6-11' pma 340' 320' 85 Country Club upper end of Reservoir, Pleasant Hill Middle of Newport Reservoir Amh ends in St Marys Point. E.g here is least Ph neglecta part of here tractions turns sharply Northward and Dolie anulla recta is abundant.

Screenings = 1/2 in + less. steam roller + crusher. Proper drainage, Rolling of earth foundation. Macadam turn stone screenings for binder. Consolidation with steam roller. 7 [illegible] 18" 5" [illegible] 2:1 2:1 1/2:12 2 2 11 Minimum longitudinal grade = 1/2 % Butters of 2 1/2% should be faced with rubble stone and under- drained with tile. Middle rows run less than 15 ft between ditches, better 22 ft or more. Side slopes not over 1/2:12 so that cars will not follow out Drag & Wheel scrapers instead of Wagons where hauling does not exceed 200 feet. Stewart grader a common grade machine for leveling up. On the best earth road only 1/2% as great a load can be carried as on a good macadam road. A slight 8 % grade is all right as economy. 2 to 3 % is better if it can be secured cheaply since this is angle of repose of wagon and truck tires can turn down road. Ditches wide enough for drag or wheel scrapers.

88 Gravel roads. Gravel should be screened as to secure free dirt- bottoms. At new embankments elevators, rotary screen bines, small dump cars. The binder + steam roller make it possible to use more run 2½ in. long. I more rocks generally than 1½ in. screen are likely to be after than 2½ in. screen, the former should be used for break larger & catch partly. 3 screens = ½ in. + two, 20% screenings necessary to act as binders. Surface tension draws the binding, dust is necessary for this binding along with water capillary action. 89 Sprinkling is necessary for binding. 3'' [illegible] 1¾ 1½'' 3½'' 8 ft. 17½'' bines for ready handling while and special binding. Sprinkling of screenings. 1 washing x 15 w/ with rotary screen $ 1000 Portable bins 200 1 15 H D Perseus 200 1 20 H P Roller 600 12 wheel scraper 600 12 large steam dumpers 2100 2 steam graders 700 2 steam drills 500 1 15 H D drill for drills 400 water steam pipes 300 2 sprinkling wagons 500 1 19 ton steam dolly 2300 Total $ 6900

90 Strips up to 3 1/4" need. Provide turn outs HO ft by every 320 ft, 16ft wide, 9ft muscular fence, when in the road. Blenda Clay Blanks. 91 Tip of cedar at east end of expense. Zygophrea crassimarginata large from star bar of wet type about 4 ft above base. Perigee round lobes like small Platysa Halia. Calyptrona of smooth grains The 4 ft above base strips narrow plane convex and not magnified, associated with Cyclomena very deep spine characteristic of wet type now 13 ft above base. 8 ft wire a diminutive large. Strips narrow plane convex with rather long central valve maybe a magniliminum type, Platysaphla rather larger than ordinary Leophlasis: Cyclotus ella with zephlication.

92 Benjamin Bald Point Up to 60½ ft above lowest good section, 2 multirecta is abundant. at 60½ ft up Str. magnillica crura- mans is in 62 ft in 1¾ ft limestone; Then there is a little slant and thin limestone up to 66 ft, contain- ing the recta cruralis. This makes a 5½ ft St.magnillium secti- on at least and must be called the base of the Fairmanian; Dalmanella multirecta occur at the top in moderate abundance. The limestone is coarse and cross bedded. None of this lime- stone with St.magnillium multirecta could very coarse occurs 1¼ ft higher up - 7 ft magnillica crura, Stained limestone area, a large specimen of magrilliu- m was found 5 ft further up: 72½ ft above lowest section, for 84½ ft thin bedded lime stone and up to seam. 106 ft up is bottom of vertical fall, Strich sinuata in large patches below this, child part large come from below 106; 113 ft up is probable horizon of St.reptil. cruralis. 133½- top of trail at first gut. 93 Belloni 22 ft, Fairmanian 11 ft to face of cliff, 2½ ft interval. Str. sinuata horzontal. 83½ft 7 ft interval. Two steep falls, 5 3¾ ft interval, 7 ft St.magnillicum Bellone 31 ft interval - Str. sinuata 46 ft interval, 7 ft St.magnillicum 83½ 23 60 56 10 4½ 1½

94 S Lebanon 0-22 ft up Olect. Phlebotrisa cym. mm, equally brown tips, 27 1/2 zyg. cin cinnamatum, cinnam, 39 1/2 Phlorttis c rarer than intimedia. 41 1/2 Phloritis crarer than intimedia. 51 1/2 Rather more clay than ex- pected in Belleme.= probably top of Fairmont.) 62 1/2 Clay less. Plenty of Refines= girlgiant bence but not high up, also some lag. Platrat infus. at base, very few secting in Dalamea near jagoa than multi- secta. 62 1/2-74 ft limestone abundant lay little. Refines genus abund ant with a few sarents, 74 to 86 ft to top of section with Rg, abund ant but their only clay here. 86 to 88 1/2 ft tip of section Mine clay, 95 struma leded above, 72 ft J Corryville, not Auburn, Top of section not Auburn 20 ft. Corryville 72-74 ft. Belleme 23 1/2 ft. Fairmont 62 1/2 ft. 50 ft{ 8 ft base J Corryville. 23 1/2 ft Belleme. 22 1/2 ft top y Fairmont 40 ft Fairmont!

91 Washing. Sun, March 31 Staphylococci, Pteraea reticulata, Microsporum (thin) name not felt. Plural reflex not very distinct. Pterinea abundant large, Platyophrys Staphylococcus. Electrometo Wine force crosses streams A Blue elements Zuberella glazfelma. Pteraea papillata, Rhinoceros common. Rulomitus fur. Rhinocynum typical. Electrophys outline, large. B Angull Laminae Microspori (thin) cover application, strong, somewhat does a real alveota. Zuberella calvata will long be under. Protanm Patellosa distinct. Oscena densa - large typical 12 m. Stylo reticulata common Angul. & Clay intermixed, not richly, Symbiophora, but in B. Standart conjugata common. One Microspori Dinojellida, exude, 40 m. 92 a common. of distributed larger local ant, up streams for washing, a distinct larger layer 2 m is abundant, not Platella ca., but not so generic as some of the minute- water specimens. 4 m. 14 m. ed L with Rhinocynum 12 m. 7 slightly slender looking ii grows. abundant large common, with faint depression the black. Protocephal not at large com rather small 32 m residential in alveata subglobosa, common, tuta annulata, large, papillata 14 m. laminiforme large, common water full. 24 m.

Weibung

91 Washing. 2nd. March 1911 Strepht. retusa, Perhaps retusum. Mod. depress [illegible] magne.ice felta. Physul capax, with granular Pleuroca decuman. large. Platysiphula. Streph. plamumbone. [illegible] ambustus Wine fence crosses stream. A) Blue clamor moss, Labeclum fragilaria. Vistaria papillata Rafinesque decuman Rafinesque form. (Rafinesquima? Tryptophend? Large? utline. large?) B) Angula laminae Modvolgensi (III). [illegible] plicatum, strong. Keratides a real abrecta. Nebulella decumana with long hair and deep. Peri area Papillate distinct. Occurence decuman large typical. 12 in. (Strept retusa common Angl l. & clay interstices, not wildly if worth for him, but with Claudowina crugulate common. [illegible] Modvolgensi dimo julicata. made? 40 m. 92 4 in. Strepti retusa common, clay with Rafinesquima large local in upper part, up stream 20 in 1st bridge below washing. ( (Rafinesque? some distant clay) Phy. capax abundant, not parallel to., but not so graceful as some of the 47 date- water specimens. 4 in clay 1966 (Clair betted l. with Rafinesquima [24'] at top last chiefly sandy lovery and piney growths. (Streph. plamumbone large common. Nebulella with faint definition around the lake. Phylocladus capax not at very red water. Streptiloma rather coarse 2 in C) Nebulella residatals? not abrecta D. ventris? or [illegible] distincta, common, with reticulata (Streph plamumbone large. Peridien papillata 14 in (Strepti. pl amumbone large common Small with fall 24 in ``` ```json { "text": "91\nWashing. 2nd. March 1911\nStrepht. retusa, Perhaps retusum.\nMod. depress [illegible] magne.ice felta.\nPhysul capax, with granular Pleuroca\ndecuman. large. Platysiphula.\nStreph. plamumbone. [illegible] ambustus\n\nWine fence crosses stream.\nA)\nBlue clamor moss,\nLabeclum fragilaria. Vistaria papillata\nRafinesque decuman Rafinesque form.\n(Rafinesquima? Tryptophend? Large?\nutline. large?)\nB)\nAngula laminae\nModvolgensi (III). [illegible] plicatum,\nstrong. Keratides a real abrecta.\nNebulella decumana with long hair and deep.\nPeri area Papillate distinct.\nOccurence decuman large typical. 12 in.\n(Strept retusa common\nAngl l. & clay interstices, not wildly\nif worth for him, but with Claudowina\ncrugulate common. [illegible] Modvolgensi\ndimo julicata. made? 40 m.\n92\n4 in.\nStrepti retusa common,\nclay with Rafinesquima large local\nin upper part, up stream\n20 in\n1st bridge below washing.\n( (Rafinesque? some distant clay)\nPhy. capax abundant, not\nparallel to., but\nnot so graceful as\nsome of the 47 date-\nwater specimens.\n4 in\nclay\n1966\n(Clair betted l. with Rafinesquima [24']\nat top last chiefly sandy lovery\nand piney growths.\n(Streph. plamumbone large common.\nNebulella with faint definition\naround the lake.\nPhylocladus capax not at very\nred water.\nStreptiloma rather coarse 2 in\nC)\nNebulella residatals? not abrecta\nD. ventris? or [illegible] distincta, common,\nwith reticulata\n(Streph plamumbone large.\nPeridien papillata\n14 in\n(Strepti. pl amumbone large common\nSmall with fall\n24 in"} ``` <think>由于您没有指定JSON格式，我将提供一个简单的文本输出。如果您需要特定的JSON格式，请告诉我。以下是根据图像中的内容转录的文本：```json { "text": "91\nWashing. 2nd. March 1911\nStrepht. retusa, Perhaps retusum.\nMod. depress [illegible] magne.ice felta.\nPhysul capax, with granular Pleuroca\ndecuman. large. Platysiphula.\nStreph. plamumbone. [illegible] ambustus\n\nWine fence crosses stream.\nA)\nBlue clamor moss,\nLabeclum fragilaria. Vistaria papillata\nRafinesque decuman Rafinesque form.\n(Rafinesquima? Tryptophend? Large?\nutline. large?)\nB)\nAngula laminae\nModvolgensi (III). [illegible] plicatum,\nstrong. Keratides a real abrecta.\nNebulella decumana with long hair and deep.\nPeri area Papillate distinct.\nOccurence decuman large typical. 12 in.\n(Strept retusa common\nAngl l. & clay interstices, not wildly\nif worth for him, but with Claudowina\ncrugulate common. [illegible] Modvolgensi\ndimo julicata. made? 40 m.\n92\n4 in.\nStrepti retusa common,\nclay with Rafinesquima large local\nin upper part, up stream\n20 in\n1st bridge below washing.\n( (Rafinesque? some distant clay)\nPhy. capax abundant, not\nparallel to., but\nnot so graceful as\nsome of the 47 date-\nwater specimens.\n4 in\nclay\n1966\n(Clair betted l. with Rafinesquima [24']\nat top last chiefly sandy lovery\nand piney growths.\n(Streph. plamumbone large common.\nNebulella with faint definition\naround the lake.\nPhylocladus capax not at very\nred water.\nStreptiloma rather coarse 2 in\nC)\nNebulella residatals? not abrecta\nD. ventris? or [illegible] distincta, common,\nwith reticulata\n(Streph plamumbone large.\nPeridien papillata\n14 in\n(Strepti. pl amumbone large common\nSmall with fall\n24 in" } ```

2½t clay, 9 m clay rate. D Plect, aurica crinum. Dim sulz gradate. Skeynch. oafas + geometrie + for opper adim palacellam. Steph drep andrum 16 h. F Parcerius Plect. abundant Din silu madats. Strefc. dref andrum. Strefc. plauruntzera. 2½ h. Dimuthi zuzgradati Strepft. plaurum lura Pectane papillato Stepft. divf or din. 20 m so next page. 98 Dinuthi zuzgradate crinum. Stepft. plaurum lura Pectane discussa latza Strefc. dref andrum. Stepft. relistat. 28 m. Plect, crinum. Dui setze a late crinum. Skeynch. oafas + paracelluria. 5 exultant listentella de calipis 9 m plantz of betutella bot nut vel crinum. Avratyfe rec dendatli tot al cota. Rode bre drepft mit lura truge. Plect Wanydoville Of landtke 18 h Stepft. plauruntzera lata. It e asimal Plect. oafas. Nil zho/fasi blach b/thero at tot of page, shut Wildy + arped. 48 m. Dimuthi gradato. Stepft. plaurum lura Plectane papillae crinum. Strefc. divf or din. 24 h. 99

100 5 sample of nummulina 60 m. Stratificated chalk from 12 h. Gyptalana crumma, Straph. planulata large, Plan. vers atllerae, 12 m.) (Gypsum gypsum) 102 m. (Lead common & some layers, X Helvetella mira ejecta crumma, Total range of fauna, 24 m.) No of Content 254, A loose bandage around knee from Litybey. diam. 2.5 m., pipelock 1.5 m. near margin of shell, 5 chambers in 10 m. length. 101 Art gypsum. 42 m. Gypsum crumma. Dalm. pygmae LAR. Plays and allitera. Straph. planulata large. Strap, drifk sanden. Patagae jetfilled. Helvetella obsidens 16 h. G (Straph petreae miral) 4 Large from common, 10 m. N. Slyper, drift sanden crumma, Helvet. crumma. Platyspirifer magus veltyph. Strapled drill on L door 12 h. Hospal same as found Crucidellae large, Platyspirifer veltyph. Abyssella occidentalis. 42 m. Gypsum crumma, Dalm. pygmae art ade, Gyptalana crumma. 12 h. 8 h. 36 m. Interal. Laminated iron limestone. 12 h. Int alveol. 30 m. Content 251. Laby in creek 30 m. 9 intervale 6 m. Art. modulare i. 66 m. Orde de.

102 Balloon set 8 in, massive mottled l. 24' / ? exprmer 6 in massive l. with vertical worm trmps) 17 in, weathering thin bedded h'ms mr frostb. 18 in dec, thin bedded & changing together and other very qvarious. 62 in, 'thin bedded slabs of lay ark, in frostb, 54 in dec not well expressed - clay with large nodular clay rock masses. A 72 inches clay rock with Tetradium at all levels, abundant & in lona 18 m. and between 3 and 5 ft. /5 steps vagans, flat hyzypus Strange new 1/3 from top, Bryozoylia Veravilles from, Rhynocapax and rolls 134in diam see next page. B 18 in, Tetradium larger, in upper 6 in the underlying 12 inches is the limestone with brgszons thick. Both from the 'massive' layers. G, for clm. C 18in Caladoccia Lindorn Spnse new Tetradium rare at base Clay Column navi obrolata qvartalam F4th. 'modern' large Colmmra wrich deto 14 in frm 103 shifty columns large columnar to at various levels, from base, at least ? steps level. ere 1 3/4 in diam, in 15/16 in diam, from many of above in is 1 3/8 in,

Ophelia

192 Balltown section 8 m, ? measure disturbed 24 m, /r-expr 6 in measure l, with vertical ?mm strings, 17m, ?enthamy thinbedded breccia? ?mr fossils? 18 inches thick bedded thin layering to settle and other way around. 62 m, ?thin bedded shale clay incl, ?fossils? 54m do not well expressed = clay with large nodular clay rocks in masses. A /72 inches clay shale with Tetradium at all levels, abundant in lower 18 m and between 3 and 5 1/2" /?strip? ragana? flat hypran?, Spongy new ?s from tip, Bryozoella ?veracilla? form, Bryz. capax and other's ?Ptyidum see next figure. B 18 m. Tetradium larger, for upper limit, the underlying 12 m is the limestone with Bryozans with ?s from the "massive layer", ?, Arm-den? C 18m, Calabocia ?in? dym. Sponge new? Tetradium rare at base. For Column marks alveolata ?gla?calma?, Ephh of ?Ardeni'? Large Crinnoraw beds to 14 m feet 103 gray dam, chatty 33" /S thin clay incl, large Chrimm? calculated at various levels, from tip to base, at least ?? specimens seen. ?creek level? sandstone, 1 3/4 in diam, siphonula 15/16 in diameter ?in from margin of shell, ? chambers in 1 3/8 in,

104 loc C, N side of stream Ballsville Ballstown N wth 105 Batzburg quarry in D. (The Batzburg quarry is 16 feet deep, chiefly in shaly layers) my local part seem 1ft. [illegible] hypsarium medium 1ft with large lime brought to top of mottled l; 3ft Glenister terrariae medium (punctata?) Dendrodon, Dendodonta, with areas as well, little l, sedm. 5 1/2 ft [illegible] White muller, Platystelella heteridella, Shep. divaricans, Sheph. vagans, hypsarium minimus pretty common 13ft not well exposed. 5 1/4 ft Jane olbia mottled l, jactipunctata Dendodonta + 2ft Bryngaram canna collected; 5 3/4 ft. Mississippian l, a mottled series; Papen 2 1/4 ft not well exposed. 5 1/2 ft more massive mottled l. Dendodonta = [illegible] jactipunctata 29 ft fly shale led down to creek near base of Dendrodian layer A. - 17ft rylie bedded mottled l, fossil well distinct, 1/4 2m 1 massive l, 2 1/2 ft to base 1 second massive l, 1 1/2 ft Dendrodium massiventum, 2 ft clay + clay arch, columnaria albertian layers

106 East of Bullstem, km. Numerous hypozoeae and broad short striped Calamodiscus dialatus. The shale layers will exp[?]red 1/2 further up the creek, eastward. Helbertella occidentalis distinct. Main Caradocian zone, similar to the massive ink below, Byzonophyllum? a) Massive layer in the Caradocian at tip. b) c) Striped retorta. Perisphinctes dennisianus. L. bondoni; Helbertella occidentalis, as regards striation but without depression toward beaks. Calopercia zygonodetae? Nudistrophe? Spruce new. 107 Tittler. 1/2 ft massive order, 12 1/2 ft shale bed, 5 ft top of massive layer. 1/2 ft. less massive, unmarked rock. 4 ft massive Caradocian rock. The hypozoeae and short Calamodiscus make up the lower effect of this part of section. Orthoceras humilis

108 Put together section at Batesville 5ft White water fossils large worm borrows. 11ft Muddy bed, hardier layers 17\frac{1}{2} Mottled bed 3 (Pterines, Tetrachonites) softer beds 1\frac{1}{2} massive L -> 2 Bryozones collected 3 massive L. 2\frac{1}{2} 8ft shale beds 4\frac{1}{2}ft hard exposed phygostoma? 6ft Othadimnus Tetrad, massite, Columaria \frac{1}{2} massive 1\frac{1}{2} Calceifera sponge 2\frac{3}{4} Columaria 109 Dromalites from tunneling ledge out side of creek, about 43m. - L boulders with Tetradimus fam. 1ft coarse grits beds L, 1ft 6 in. Micraster my. L, 1ft 9in. Micaster arg. L, 3ft 9in. clay thin bedded rock, 2 x 4x regular shale bed, 5ft 6 in. thin bedded L., but not the shale bed. 5ft 6 in. limestone one, but not 2 in. thick layers, but not the above bed. 3ft 6in. thin bedded L., but not seen hard as shale bed. 2\frac{1}{4} 6in. the deer lies larger 5ft 6in. Creek level, creek level [illegible] - crassus leamhill bone 15ft above creek 0-4ft above creek is Phycophora S. rock. retortus? Sternum denudata large striated glass animals? Peristals? parapoda? Dim. ostracodacta, 5 strips varying from Albertella? to double strip of Pteridium, very clear. Stripes diamond shaped Phymat just too close

110 1/2 mi. N of Emerysburg bridge, on E side of stream. 16 1/2 ft Silicarsch, small gas winfrds, small calcareous small chondrite, flintish 1ft ardi with top if falls > 4 ft 6 in. clay with Petralgium lenses, long, a brown half 1ft 6 in. sand exposed, partly clay, 6 in. L. melt. Petradium fen. 2 ft 6 in. Salmia, clay rock. 6 in. Nethistella crumena, 5/ft on will exposed: 4 in. large burrow mass. 2ft L with Nethistella > 8 ft m. under growth layer a with like strc shale rock but not continuous 4 in. decay arch, 1ft con. not exposed. 4 in. like shale rock above, 3ft bit not exposed. > 3 ft Hard rock with clay below. 24 ft m. total, lowest fall from creek level. Calyxina Nethistella: black Nethistella occa manis when old. 1/2 mi. N Albert Mussel shell at lower en of series and ends at 2nd road intersection. East of Emerysburg bridge, 1/4 mi. 111 4 ft like shale bed, 1ft massive, 1-2ft massive 5 1/2 ft Lm. with some huge Ostracium 2'2ft Ostracium abundant scatter! 2 ft Lr massive L. layers. 6 in. Shaly clay rock, Ostracium fen 2 ft. clayschi? Achistella crumena

112 Wesley? 9. Married L. S... [illegible] 104. U.... [illegible] [illegible] 2 m ... 2 p ... [illegible] -> 1/7 ... 3rd day & ... day [illegible] [illegible] [illegible] [illegible]

10 2

112 Wishing! S. Written & written writing {1/9, thin red lines...} {around...} {...} 2 w... 2/11 B) -> 1st Saturday in every day 5. [3rd] day + ... 1st [illegible] 4th Lakes of...

142 1. Small anticline in waste of river. 2. A small stream comes out rapidly from beneath and takes about 1 ft above low water level, resident, and underground streams. 3. Water drops then mud at river level then drying pan head. 4. Heavy flowing spring = underground stream 60 ft above low water in river. 5. For several hundred yards the water comes out of rock near river level then drying pan bend necks 30 6. At 3.30, stream on left, Mox Run 7. At 4.00 PM. 8. At 4.30 PM. Cold spring and direct south of it surface stream rather large plunges down steep cliff. Probably from same general area source since we are in gullied in the ridge. See sink in the cliff directly above, and turned Briggerville. 9. At 5 PM. Near [illegible] came down from ridgeline on west. Probably from same general source of the map. 143 10. At 5.30 PM. Farmer will take a short distance down stream water whiles down from cliff, 10 1/2 Underground stream empties here 11. At 5.45 PM. 12. Heavy stream, underground ? 13. NA Bruna Vista immediately SE cleared. The Cundsville bed is well exposed. One top of the highbridge is a chert layer 2 inches thick, at 866 USGS, 14. Cherty top of high bridge 2 inches chert, with Cundsville exposed 10 ft long away to 15 ft above. 15. Cherty top of high bridge, 1 in. chert, with remains of Cundsville directly above, near 950 USGS. 16. Top of highbridge and face of Cundsville at 865, just NW U.S.G.S. 820 marked, located on stone fence. The chert layer at top of high bridge is not actually exposed, but the other two are seen within 2 feet of each other vertically. 17. At top of hill along road side, in West is Hekelville forest + Dalmanella Cherty layer on East side, is Plain sandstone base and chert = ? [illegible], near 990 USGS.

144 18. Near [illegible] the ground cont[ain] round cherty, a granitz[ing] concret[ions] like there from Knoxville. Before reaching kind of road, there is a coarse grained limestone like Souther At end of road towards North, there is heavy mixed limest[one with] masure- m[atter] things like High Bridge Detachd. payments common. Since unknown Farther along the same road is stuff that looks later 2 and Marly, a few quartz concretions, there in the horizon showing up. This [illegible] show up beyond point where road turns NE. About 100 yards north of this point in field next to road, there is a white dyke. Apparently the rock east of this dyke is a rough brecciated limestone. This white dyke runs approximately N + S. On its eastern side, where the road turns off NE, at the point already mentioned and from there to the present when the road makes its east turn toward the North, [illegible] house, Black Slate is exposed tilted strongly southward. East of the point where the road start North for the house is Saluda like sandy clay rock, not quartzed but Psenic. Saluda. No joints, appearing. Farther east[erly] sand exposure: probably limestone? actually, with Platy shingles [illegible]. Large and 145 [illegible] concretions... Going from the sink near SE of the house southward along the street on running end of the nearest fault, [illegible] with Platy [illegible] in agreement with below the argillaceous clay rock un- twining the same [illegible] (Ol. f[orming]) and show this is the argill. Spalling clay rock with but fossils. Going southward along the stream east of the main fault, there is a steep western slope, extending eastwards as far as the first main ridge east of the stream, at the top of this ridge, southward, Black slate is exposed. Apparently, I did not go to see it. but judged from the distance. 19. Farther south near the point I have marked 19, straight east of a fence on the eastern side of the [illegible], there is a sudden eastward dip for about 30 ft west of the stream, and then the Black slate suddenly appears, appear- ently east of a fault. Is there a sub-parallel structure at the southern end of this sheet between the fault and the first ridge east? Going from 19 NE up the north S [illegible] marginal line or edge [illegible] SE of the fence, along the path east of the wire fence.

146 The bend of material directly west of the fence consists of an argillaceous sand which I assume to be the Red Sandstone. This forms the main fault. Directly west of the fault there is grey, cross limestone which I assume to be Lexington but I did not lower. Assume a fault directly west of the fault. 20 Before reaching 20, when the creek east of the main fault approaches the county road running east from the fork, the ark slope east. Then the Black slate is seen dipping NE. Below this, eastward, the over profiles form Ozander Saluda slants up, either limited or dipping gently west. A short distance SW of 20, directly east of the first house south of the junction of the depressed county road with the fork there is a quarry, ready seen from the road junction. The Huttella tricalis is about and 4 feet or within face of the quarry. The underlying ark is in thin black, is very irregularly bedded, and thus rests on 3 feet or fine grained limestone with gypsum occurring, which resembles the High Bridge Ark in general appearance. Ark great ahead and Huttella is against the High Bridge age of the under lying material. 21. Huttella tricalis has crystalline lime at the are. 22. Ozander Saluda dipping westward. 23. Fairmount bed, good but low exposure on N side of road. Large flat S lithofina. By gypsum. Huttella occidentalis or depressus thick, Platy strophia. Jura dense. Strophomena on argillaceous. Cancellaria florida. Cyclomena tale spire. Lithofina and corruptions... hills today. 24. Large depression, like a horse sink in Fairmount horizon. Another smaller sink seems farther SE. 25. Top of profiles was Fairmount bed. Flat limestone. Most indeterminate C. Huttella tricalis + occidentalis overlaid by thin chalky impure limestone. Late layers. 26. Quarry in Fairmount, 25 ft high. Strophomena on bluish C. Cancellaria C. Platy prudence. Otervina without anterior tooth. Posterior part not exposed. No late layer exposed too low.

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

148 37 On the west side of the bridge the Lycophyta roots again on the high bridge, in both cases no trace of the Cynodonte is seen. 38. Large sinker left by Lynxgta and a series of small ones on right. 39. Myer Fairmount, Oithonrhynchula taya, Heterella occidentalis Common; Oithorhynchula typical, Plat.junderna not common. Platyctophic small from common, 815 ft if bridge level is 804 as shown on the bridge, but I notice the new map say 824, look up pencil map. 40. Rock resembling Talc layers for about 20 ft above road level. Plat.junderna rare at base, 41. Upper Fairmount Heterella occidentalis, Plat.junderna, Cithonrhynchula on hillside north of road. 42. Talc layers slaying eastward gently 28. Plat. large, Heterospongia very flat. Probably above Talc horizon since the latter is exposed SW down the old p'ike valley, 149 43. Cynsilaceae no bluen l. Plat.junderna, Heterella occ. dentata; Heterospngia rarin. 9/3 at Overland by hard subtle blue l 40ft below. NSG.S., leptand ghemtridali's. Platychitesma dentata! Platy Thridi'a & ctypha general cyllulin, Heterella occidentalis. Platyctophic junderna occularis high up than the dentata + leptana! Overland by clayey silt, Overland by clay+ thin layers of hard shaly clindy silt, The level at the junderna when the bridge is 953 U.S.G.S. 44. U.S.G.S at 911m and in 10 ft above Platyc- thropic cynxis is very abundant. This brings our solid blue limestone and is overlaid by thin bedded shaly layers. Our anthelmia valley, stills higher. 45. Same abundant Platyctophic junderna larger with recent 935 and not of the last as high as 955 U.S.G.S.

150 Stand. 46. Mayville, Plat. panderi rarest common in an argil. limestone. Quarry is about 10 ft deep, 970 ft. U.S.G.S. reading [illegible] using barometer. and therefore subject to error. 47. Arg. Placene rock, apparently with Plat. panderi but no good fossil. 48. At 894 about, U.S.G.S. Plat. panderi Dalmarella accidentalis + one Weberill, sinmata. Apparently also are Prasopna. Regarded as Mayville. 49. Fairmount quarry, Stephomena mayorillensis abundant, 50 Fairmont, Stephomena mayorillensis abundant! 51. On summit S of 51, is Devonian chert, with Plat. lyracmired w/chert at base as though the Devonian lime had rested directly on the Upper Mayville. North of 51, is typical Eden with Plat. and [illegible] common. Dalmarella common out in a few layers, rare elsewh. Stephomena Halli rather rare, Prasopna sinata abundant. Eden section about 50 ft. Fault between Eden + Mayville perhapsly E+W, in dir. generally S.W. 151 52. Eden with 2 specimens of Primu- clens, also Plct. crummites ? Dalmarella, Rather numerous limonites, on both sides of the road. 53. Top High Bridge in the Vanuxemia in chert at top, also Orthni large specimens. Must be the lower Mayville bed. Above this is the basal part of the Carbon will not well exposed. At 885 i top of High Bridge, U.S.G.S. 54. High Bridge top occurs at a same level = 885 U.S.G.S., in woods along its road before reading 54. The lime vein at 54 is much more nearly but this main vein is slightly runs a little east of north, but not straight, a little zinc bleas is associated with the limete. The High Bridge + Lexington run west of the river. The counter rock east of this vein was not exposed at time of visit. 55. Lexington l. quarry, w/ith Ptychostraea megnivalve rare Webastella boralis my mi. Pras op.nk, two sp., about 10 ft below top of ball = 950 U.S.G.S. 56. High Bridge at least 4s ft above week, not examined. Lexington at mu

152-56, continued (Bridge land 831) U.S.G.S. Bare I Cynada Valle = 242 ft. 57. A series of sink in Lexington l. create underground stream. Damilla. 58 Lexington l. at Cave Spring, = outlet of underground stream. 59 Winchester with abundant Peramphora and other branching hyogranus but no Rhynchopoda or Cyclumae noticed. 60 Perryville bed laid by lower Winchester without any fossils I could recognize except a Pterotellid which looked somewhat like the Triadics. 61. Perryville bed at creek level, 861 U.S.G.S. 62-63. Limestones rather Micrum. 64. Rhynchotrema abundant and Pterotella linealis few. 66. Pleistodontes series. Eden Dolincavella multistrata. Omnidens Bygogypara Stelligera & cunnucula.) 65 Peramphora = Winchester on top of hill? 67. Eden Damarella, Pterotella multistrata. 68. Gramond 20, 69. Paramonad Stephanomera subjugabilis abundant May be west Middle. 70. Stepbonemera margariferous & Constellaria abundant = Mint Valley on East side. 153 71. I made summit of hill, Derma chest common. Highest exposures contain Ophrys - Amphileus lynx. = Ponderosa. Apparent Der rests in May'sville Top of Mayville about 1000 U.S.G.S. 72. Shaly 20, apparently upper Dana or Mt Sthe. Apparently fern stump forming at least on Danquella & Pleasanton Apparently from Pterotellus. 73. From 72 to 73 No Gramond as shifty shaly but large limestone towards top. 74. Going up hill toward 74 the same that Saward is, with heavy limestones upward the top. 75-76. Eden with Dolincavella & Ophrys Lynx. Over this dip SW under the Barrand? 76. The clay exposures fully forming and going NW down the lines are assumed to be Eden. 77. S with east I limes - hard rock with considerable masses of gypsum which is. New limes 6 Pounds 10½ lbs bridge with wood mayo. Further down the way time reading creek & Lexington l with Nebulata brodia.

(154) 78. Heterella tricolor common. 79. Heterella tricolor? Physichthysma 80 after reaching last house m left, Pussy willow bed is exposed at 80 is seen hard limestone with concretional masses, assume to be Minchite. Eden beds have slipped down hill. 81. A great Eden section could be walked out SE along the road, and up the rimmo hills. The basal part of the Eden is very sandy and like this bedded sand. The middle and upper parts have much reddish limestone with a Heterella + Plectan knuts, This basal sand and Eden is surprising and possibly has been overlooked for last 4 days trip. (9) One mile N of Roland. Leptaena? Heteropsis in upper Lynx beds. Blue shale with gastropods. Shale with that fossils (10-15?) 15ft clayey. Plat. lynx. 3/4 mi SW of Mitchellburg, and 1/2 to 3/4 mi East of Gumbo White- horse, 1 mile of Sanford C McCarty. Black shale Der.l - 9 1/2' Ordovician Mud. 3/4 mi: East of last - Bd Edward, rest of lane Der. l = 6 3/4' Hard siliceous cherta? - 5' Strong dips junction J Mill Creek + Scratchy lane. At Joshua Whitworth, NE of lane Der. l -- 13' Ord. -- mudying -> Fossil Ord. - further down hill.

82. Platipanderia, Holotella, abundant Lophospira lorenzi in considera ble sections finegrained, dark col- ored limestone, Mayorville upper, 83. Platipanderia marginaceus limestone, Mayorville upper, up to 950 level, 84. Platipanderia, Holotella, Byssoidea, Heteroserpens byssogans numerous, in blue rubble lime- stone. The Platipanderia is abu- dant and many have the shelled living line probably W.T. Auburn, 85. Sandy shale. Probably Richmond, down as far as creek level, up for 50 ft w drill side, about, [illegible] 86. Dermin shell abundant, including Phillipastrea. In stream bottoms ark lithologi- cally like that at Columnaria lorenzi, 87. Black shale will be found, with great quantities of Dermin shell forms. 88. Thin edge of black shale with Dermina limestone below and Derminire above to grade. The Derminian ident- ity rests here in the Chert, 89. Thin bedded rock (Richmond?) thus far, 90. Fossils abundant, especially byssogans + Platystrophia = lum. Richmond? Blueish clay and weathering as on to expose rather numerous fossils, giving there good Septaria & Ordovi- cian red limestone like those at loc. 82. 91. Fossils numerous, in shale ? Platipanderia (One dark colored limestone, without considerable interval, = 20 ft?) Lagone with Platipanderia, One colored limestone like loc. 82.

92 clay shale n shaly rock. \t\t1/4 ft clay w/ frpy grams = ? \t\t1/8 ft, limonite, thin n' friable crum, { Fossiliferous clay rock 1/2 ft. Plat. pandersea fairly common. 2ft. Intervals. fossils in clay rock. 5 ft. depthrema in place. Q retural 1 ft, fossils in shaly rock, D over colored limonite n. 5 1/2 ft, clay shale rock. 17 ft. } 93 Trip # D over colored, limited out at three of Mayville to 946 U.S.G.S. This gives 40 ft of section of To road corner. Old lower Richmond contains 1 shaly clay rock. 94 D over colored li->Mayville, since leaving the pike, 95 D'm colored and argillaceous limonite -> Mayville. Fossils few. 96. Argillaceous limonite n->May- village Plenty of it in creek, 971 Top of brick. \angle R 3 5/8 ft shaly li. Lower Richmond. 8-\times\t1ft with Plat. pandersea at top, rubble. 1 1/4 ft rubble. w/it, sepiaea at +2. 5 1/4 D over, section, shaly below 50 ft shaly limestone very white, 98 = Continuation of 97. \circled{114} \circled{79} 3 5/8 ft - highest point of hill. = 2nd brick 7 1/4 top of heavy arg. l, with rubble below. - 1ft. Heavy arg. l. bed, 27 1/4 ft. \angle R limonite, shaly li. <R Second visit. 43, 10ft Thin shale rock; Her erupfunga at top. 10 ft not exposed. 2 ft. ? leptaea, Pty dentata exposed. S-5 1/4 D over colored l. gardenersds 16 ft. shale rock. \qquad int anthum 6 ft - shaly rock. Plat. pandersea abundant 7 ft & blue arg. l. partly over colored, (Plat.) phidera The Plat. jandersea larger with abundant limonite is seen up to 8 ft above lager s. and abund ant brgyrams run 2 1/4 ft farther up. Several large globular Crasopra recorded once in road bed about m level with horizon between first new brownish rulying layers limonite. They perfectly well not came from here, and their actual location is unknown.

Lancaster. 99. The Amherst fossil part belongs above this level. Chin shale, tofts of till. 10 ft Mt Auburn plat fenderosa corn 19 ft grad come to top of massive l, ready above others. According to calculation in the Textor modernism should come in at 21° + 29: 50 + 920 = 970 ft U.S.G.S. and thus 84 ft at this locality plat. fenderosa is abundant up to 965 ft U.S.G.S. and from this point down 12 ft (955) U.S.G.S. The rock looks like Mt Auburn limestone. The heavy limestone lines come in at level of fence. North- ward; many of the plat fenderosa are of andmensis type. (10) massive blue limestone, Maysville. (101) 24 ft. Bryozoa abundant. Richmond beds. S plat. fenderosa tarand lay, 6½ ft septaria, Rhynch. dentata. base < 944 U.S.G.S. 4 ft. solid limestone, 16½ ft shale rock, 8 ft plat. fenderosa abundant mt Auburn 18. Massive l. < 916 U.S.G.S. Creek level. 102. S way S on this road from Gilbert Creek, tht Auburn is soon exposed, the plat gray shale + solid limestone beds are referred to a granite of a strike. Then come the Amherst, Yorkeana and 4 miles above here, whether coming in with it range up to 2 ft above the base. Plat. fenderosa occurs regularly. This is preceded by the top of firm dlay with numerous bryozoa at time from Bridgwood. Several loose Columbian's rocks partially landed down from hill side. The face of the Amherst fossils limestone, 920 ft U.S.G.S. righting along road about ½ mile east as clearly as the instrument permits. With 40 ft above Bridgwood line the rock is steady and no Colum- brian mark is found in it.

103.) Boshen Church. 11FTS. Plat: predominates toward N.E. Exploring Amberine beds, taken about (950-18) = 932 ft USGS judging from contour lines only, probably 27½ft Base of Mt Amburns side Plat dominated horizon, Dist. since: 1074 stream bottom. 104. Plat: predominates Mt Amburn face at about 860 ft USGS judging from contour lines only, Of the top of ridge is 938 USGS then the top of the Amberine face of this clay layer at line of Bricken under at 901 USGS 57th up finally copying MS map, At the next road corner near the mark is 916 USGS or that at 938 probably is correct. 105. 894ft USGS = face of Amberine. Rhy. dentata. Most of the section down to creek practically in sandstone, My. ? limestone, N.F. Formation down to creek level. Only Mt Amburn+ This would place the top of the Mt Amburn at about 874. The Mt Amburn is exposed but was not measured. The trace of the Mt Amburn Plat beds should be at about 866. The underlying section was not measured but probably is new land and Between #94/10 old numbers, N.F. Rockland, the creek is at 849 ft. U.S.G.S. The exposure in the bank cliffs and northward along the road includes only shale rock. 10. The cliff at 10 C consists of layer of clay rock, 3 ft exposed, containing Hard Detritus present in front 6 in., and Plat: predominates is present in largest large contain by Agitana. This places the base of the Amberine bed at 848 ft U.S.G.S. The old exposure at 10, west of the road, is formed by the top of the Amberine. North of the house N.F. 10, the hard limestone below the Amberine is exposed up to 7 ft above the creek. The trace of the Amberine may be several feet further up.

9) Residual blocks of developed Pendergra Come not definite, but Anheim, 974: argilla, clay, plat pendergra abundant. 51: after argill rocks plat pendergra, 52 ft cotten land. arg, cl, with plat pendergra. 106, A pressure anticline wrt. fracture at top, Mrs N 5 E. This pressure ridge crosses the Aurora east of the RR. 107. East of RR, Leptaena in lim part of Anheim, at track level, And cut up to Columnaria langer; measured clay & loose shell over fields It exposes NEY Rhenland. 108 15 ft 2 intervals to top of Hill. 2 ft residual with few Columnaria & by 64 ft Columnaria lager down to top of Anheim bed, as far as I could judge from experiences down creek. This drive must take into account the Southward dip, which in this distance is con siderable. The first place is 200 steps, Columnaria vocana Rock, when Columnaria's this field did not nearly extend toward top where it is harder. Southward the Columnaria's having drawn up first 3 hours. The mysterious Reifmann crump cos up on north endy, 109. From the creek up to grad corner grad road at 109, The base of the Platy, pendergra NW Anheim is 103 feet below the road crump. This = 950 - 103 = 847 The estimated number may be neara 860 while the measurements will trick along the road for at least 24 miles. 110 In town (Lancaster) is exposure of shale, about 5 feet thick, over with by from lifeless Anheim, below which is drive colored [illegible] Argheim base = 100. 111. Road level in say between two Lm's 360s sizes or "hills": Intervals 5-4 ft. basal part light blue fall J hugg, ans - layer of Riche mined. Upper part = shale, clay, by to Richmond. But in this is widely possible for us gone = Anheim with plat. pendergra are rather common and with me from Leptaena. Below this a drive colored lime stone. Below this is shale creek. The NW Anheim is not exposed here.

112. Farm hrs 45 down to bridge str Coryville is represented by fine grained and argillaceous limestone with very few fossils, from the base of the section the rock is more shaly.- Gate Massive argile, limestone 5\frac{1}{2} ft. Natural unknown. (16\frac{1}{2}ft shale bed.) Bridge level 828 U.S.G.S. 2673 4 ft. Dintural Note 5\frac{1}{2} ft. Shale layers + harder beds. 1\frac{1}{2}ft. Fossils fair. 5\frac{1}{2}ft Orthologychula abundants <817 U.S.G.S 15 ft. Intermix Covered here. River level, 113. A good argillaceous limestone exposure about 11 feet below road level at road angle. Top at 885 U.S.G.S., No fossil zone visible 109. Road corner 957 partially. U.S.G.S. 56 ft including Anilcium at base. Leptaena's. new base 1901 U.S.G.S 5 ft drive eroded limestone. 878> 7ft shale bed. \frac{1}{2}ft partly exposed but Coryville, Pl. Ponderosa 16\frac{1}{2}ft arg. & Coryville down part filled 5\frac{1}{2}ft shales Gate? Creek. 114. Church level top of hill Grant am 27\frac{1}{2} ft interval. Base of Milky fossiliferous section with Plati. ponderosa, not known below Underland & Lang Coryville sections. Base of Mt. Adams estimated at 965 judging from cut on line = rather a lesser number. 115. Quarry W Grant, clay spalling rock regarded as Lower half of Ordovician. 116. Road level. 18 ft natural. Leptaena 3ft drive eroded <945 U.S.G.S. 7\frac{1}{2}ft argillaceous shale (thinning) 6 ft butt Anilium Pl. ponderosa Coryville arg limestone 982 - 172 - 903 - 18 = 745

117. Fossils horizon from creek level up 5 feet. This is bounded by a shale section, horizon unknown. Southward, up the hill, is strong tilled rock dipping S to E, 118 Road corner. 10 ft S natural 5 ft. Ruddy fossiliferous plat ponderum. I am limited now with Plat. ponderum. Inner side drove cleaned, below indicates that the underlying fomy rock is not Antrim. 119. Top of hill 22 ft Natural Base exposed next Antrim (Thelater is about 5 ft thick and is overlaid by shale) Plenty of Corynille my. I have called D. beneath and on the hill. The lower part, at the creek, is shaly, for a considerable section. One Ruddy bed evidently does not reach this far west. Shale. Rather exposed 10 ft next Antrim. First exposed 50 ft Corynille. 22 ft shaly < Creek end 10 ft shaly. Beneath? I seen. 120. chest nodules and quartz jiddle. given along road sides. Presently they are found older in the rock. Did not take time to look this matter up. 121. Orthorynchula horizon, 122. Orthorynchula horizon, N of home, south of clay pate due at my road, 123. 74 ft Not exposed to top of hill 1070 ft 25 ft shale sand. Date layer <900 about 3 richly fossiliferous. 18 ½ ft massive rock. Orthorynchula. <884 u365 124. S.W. Spoonmoore's farm land, west of store at Hubble (981 corner) About 16 ft below level of church. Der christ is large quantity to follow. The Plough ditch. Gradually in place. The exposures are west of 2nd Church N of 981 road corners, and SW of a house about ½ mile W road,

125. Exposed from near top of hill (within 20 feet) and here are found [illegible] limestone in the Platts Formation. Near at 125 are some richly forested forests dangers. 126. Highest land carries loose red sandstone along road, with full sections of Marysville limestones as far as locality 28 and thence eastward as far as the east terrace. 127 From Standford to 127 frequently formations of argillaceous rock resembling Richmond. At 127, a small outlying Chinta, on a few yards across, beyond which bottomland is Richmond again. It lay a mile W of Med Creek church. The Black slate comes in and embraces J M as the church. Mr Formby is planted by the Chinta m, only lithologic re- sentlance. 128. At this locality there is some surety the rock whose lithology closely resembles the Chinta. Richmond beds exposed near eastward, but no formations of Marysville seen east- ward for quite a considerable dis- tance. 129. At this locality there is abundant Richmond rock along the railroad and thence eastward along the road up the hill, along the creek, part of 129, leaving Marysville rock with Old Pt. Fmndi, are exposed, dipping slightly down creek southward, and last strongly eastward. One proba- bly is but a local dip, but it will cause the strata to rise rapidly southward. Between these two beds the Antrim should show up but is not seen. On another dip evidently will carry the Marysville bed or creek level with 200 ft N of the bridge. From locality 129, go south one mile and take road east to May wood, along this road the rocks - Richmond, dip strongly west. During from May wood south a mile like that I said before, lithologically like Chinta shows up at angle in road 1/5 mile south of May wood, midmost Richmond and Welles it. Several parallel rock depressions occur in the Richmond and half a mile south of Maywood,

A short distance farther south, south of the home of Mill Roberts, there is a fault crossing the road, cutting clean the Black Shale on the north side. On is a live trace of shaly math rock which may be Devonian shale. Within a very short distance the old Cret Archard road is struck. From this old road eastward, there is a school house at the point where the Crab Archard road turns off sharply southward. Another road, or lane, passes down the gate at the school and follows down the creek eastward, cutting but Richmond seems far away this road. Going eastward down the creek in black loam strata, and just W of the bridge a little over a mile east of May wood, the blue clay above the Rich- mond is exposed with the Flat, under as of the upper Archim immediately beneath. The Richmont may be at least 8 ft above the creek East of the bridge. Fault runs N 40 E, On Nov 12th, fault is Richmond rock. On S side is apparently top of Archim with Flat under and with shale rock above. This is much to my former view as Leptana was found. On second examination I take it that the Archim here is now laid by shaly Richmont and is underlaid by shaly bed, Flat, underneath clay muds called Archim. No Leptana was seen. This locality is where roads fork, one mile direct East of May wood. South of locality 129, on top of hill, is the rock which I would rather classify like the Clinton. It possess that large exposure. So called Clinton = 77 ft above RR and same dis- tance above Maupville top suggesting that it's not Clinton.

130. Mr to this point I am standing with Richmond shale and then bended + opening clay rock his clay, at 130 [illegible] occurs in lower part of Amheim, Further west the Olsz sandstone in the upper part of the Amheim comes in And above this is the Richly passing forms blue clay forming the base of the Richmond my: rooms plenty. The rock was rapidly by used road, but is well laid. base of Shaly Richmond's. The left hand dip should be noted, Further west, the rock must be nearly horizontal. The Osedo- dimin showing along the leftest part of the road. Then Richmond rises up again westward. The Amheim exposure evidently is restricted to a small area along the creek at 130. 131 at 131 sudden th Black shale comes in. Probably due to faulting. 132. Chert with Am[illegible] vulmata, evidently from Denl, formally situated. The same chert wit Am [illegible] vulmata + orecis also at the bridge eastward. The same chert is exposed a-little time at the road junction. No 133. These two localities are at about the same elevation and the midley- his Richlund exposed at several localities in daylight but ups below the Devonian line it me within faulting, and the Den. Black shale which diminishes from 131 to old lines to 51 and thence westward almost as far as 132 ted ups above the Devonian line. I me situated with no faulting. 133. Den. chert with orecis. 134. Den. chert, loose location, A clayey stuff with sponge flat? B, den colored limestone, Flint Am[illegible] shale rock. A. This spring I have seen several times at back of Richmond & Strick, east + north east of Portland. B. No [illegible] seen. assumed to be Amheim at top owing to shale rock below. 25' above me to grade down turned in to a much wider mass I den colored rock from eastward, which the Amheim part appears to be- come through. 27 ft interval between clay at top with sponge flat need shale bed below. The upper 5 feet of this interval + clay stuff. The lower 23 = den colored lime, at me chiefly.

135. Australia formation in Der. Clay, rock, an argillaceous rock which may be Upper Magorville; whether any Redclim and Lelysps in here I don't know; judging from section 135, only the face of the Redclim bed could be two. 136. Apparently soft of Upper Magorville rock with top of Plate Layer at the base. If this be not the correct in terpretation then I don't know the rock; apparently no Redclima here. Our chief feature is the large quantity of argillaceous rock, spelling, and the small quan- tity of diversified limestone in the Corryville section. Our shale rock apparently rises with the stream from 136 almost as far as 233 old number. 233 Old number. Creamery. {Stratella} Der. clay scattled. Plate's quartz of? One Praefpna, 11ft internal. Shallow arg. rock with Praefpa 4 ft. Yasty comm. 25 1/2 ft. Lateral arg. rock similar. 21 ft direct incl'd. with Old. Penrose at top and also turn. Clay, rock to a great fault master the Black Shale drop in south side of this hills. Fault runs N45 E about, with the clay, rock or downy section in the Creek on North side, and the Der. bed with faults on S side; well! Our chief shale work in the Der. limestone on S side. On inside the Desertion in the limestone is represented only by clay, or top of hill, loose & scattered. The Permian represented here is the Duffin Ledge, estimated at 5 ft thick. The Black Shale dips south and line. Our small line runs across creek but not off the road junction about 100 yards and same distance S of foot home in the creek, giving's from road corner. 130. Second trip. The Pleasant View in the direct line immediately beneath the Lejeana horizon, see section 135 also, which probably represents about the same thing. About 35 feet of Redclim and over- lies the soft free-liferous Redclim and shale at this locality.

One mile S of 233, where road Turns West th and Tumeroville, Coming down the hill at the turn of the road, the Black shale is mudded and by Devonian chert in red soil, and then by a sandy clay resembling the Riclum clay. This may be Mayville lime rock, judging from sections NE of there. I assume it to be Mayville. Half a mile west of this last locality, where a road from the south curves in, Plat: Tenderosa occurs in the creek bed. This evidently is May- ville. The overlying part of the section also is presumed to be Mayville. The thin laddled stuff starting in about half way to Turnersville is assumed to be the Tote. layers. It is important to note that the Conryville here does not consist of grey-coloured limestone but of augillaceous lime- stone which lithologically resembles the Riclum clay. This might to have come migrating geographically. Devonian chert is common almost as far as Turnersville. 137. Creek N of them. Black Shale plenty, SE of this locality. Black shale was exposed on hill, over Den. limestone. E to my west and dip here, if not a fault: then the Den lime- stone-chert continues to 133 etc. 138. A cistern backed house exposed argill, cl = Conryville probably, 44ft down is shale rubble with stroph. maysvillenian. Between there should occur the orth Mayv- childa limestone but it was not seen. Exposure not sufficient to determine as yet whether the shale rises sharply since 137 or whither there is a fault here. 139. Below entrance to lime quarry smith is stroph. maysvillenian and some foot of white probably is Fort Hope, and this continues to be exposed westward as far as Hanging Park. 140. Up to this point the stone fences contain stroph. maysvillenian; some exposures seen Directly west of house are good exposures with stroph. maysvillenian, between pike and creek. There exposures continue west to fork of pike. 141. Exposures with stroph. maysvillenian.

142. Bridgy fransiferous l. but with Sleigh, mayhewellii scarce. A very full spiried Cyclenema, with weak lung; Indivd. Stridgls in all relations except last, and the last carries my transverse stratms. Cuttings rolling, transi. Osthroctina grt above, at about 955 or 960 US BS, 143. Den chat & land is high enuff to reach upper Coryville but no actual specimens of the latter. 144. Den chud abundant + Phillipsia area giga var apfillaceous l. + Yphlerian Borden's Olistosthric spec, uncertain. Probably Upper Coryville. 145 Black shale. 146. M J Mullrogerille Duffin layer over grey D'eronian apparently, as seen from bridge. 147. One same flat debris as at 134, now lying the same large concreted, skeletm, now giving the same shale section. On a one color l. l contains flat punderosa + Petromopagia, 148 Duffin exposures at about 995 US & S. with Black shale & iron red. 149. SW 149 is Duffin layer over gray Der.l. with enals. Hereis Duffin layer 3reg l. with anals, 3 ft concreted l, 8ft sandy weathered stuff full of flat punderosa, and some Petrolite but not a rich inorganic horizon, only a few are found. 150. SJ Junction City ( Dermian Brvst me Lee old number 220 Internal about 10 ft or less, 5 ft Argill Rock No fossils, 3 ft Panzyra Ommum at top large bryozoa at base, collected. Same at S E y Junction. N Brd of creek, level. 151 Duffin layer over grey limestone-Dermian, No Ordovician 152 Der.l. at top y hill. See old No 219? Internal, Dove colored l. = upper Coryville Plant Ordvicial, fat punderosa comm & creek

153. Near road level is Stroph, may villenes, near house level is now fossil form only but we with Rhynelena seen although this should have occurred now up of stratifying herein a Lyme Maestria to the Hyzanm showed up near top & similar species appear to have occurred at creek level at 152. 154. Exchangiana billi. > Rhynella sp. 22ft unknown. <R 7½ft Stall Cyclomena came out 142 but not Cerithygnaluela, my name was 58 ft with Stropho mayvillenes' 5½ ft in turn bridge level, } Unknown 15 ft acre level) along the lane a morning, a long distance south we found one tip of hill quite now drift away have taken No. 2 Black shale exposed still a with mud at 60ft interval with grit climbing argill. & with chert nodules. R> 155. Shaly Ordovician, foreign unknown, = Dalelagan grit down hill the Stropho mayvillenes, i well represented in field stone fence. Duffryn luga well exposed south of mile, strike N fault qy, slightly westy E & W but this is uncertain. with chert 156. Harrowburg chert fragments over Banks km't me. 157 Black shale, First exposure grt up down creek. 158. Dir. 1 with Antvercelia undmata to First exp now grt downstream, Battle face. 159. Clinitm.. First exp now

160 [illegible] 5\ ft, hard, argill., rock. No prints by left thing, that look like worm burrows, that branch and twist through rock. Internal large straight account for all the Richmond necessary. 10\ft thin bedded argill., and shale, may be from Richmond. No prints. 162 5\ ft massive cherty rock, black shale, 8\ft bedded Den. limestone-- 7\1/2 ft chalky stuff 2\ft, dark colored cl. 2\ft, chalky stuff with Dracophora communis, 8\ft chalky stuff, 10\ft Planktoniferous Bryozones. Septaenaria obliqua, dentata, D. 5\ft intercal. chalk rock at top of Devonian contains Phillips's notation, The sandy rock above the Den. limestone may be Devonian also but this is uncertain. Not any rate, it does not appear to belong to the known Richmond. 161. Septaenaria obliqua found 2\ft 163 Dr. colored limestone in creek bed from 161 to 163, 164 D'er. clast, 35\ft. internal. Dracophora comm. past, i am inclined to, Septaenaria communis. 27\ft Internal chiefly dark colored limestone of me. Some Dracophora at top. 13\ft dark colored cl. 27\ft creek bed Section NE of opening. Up creek - from the Hall school house about 40 miles, The locality is on Smith Gossan creek, about half way between Will branch and the road to Aliceton which starts off further down the creek. 165 Rollings is about 2\mi up North Fork from NNE withy Smith Gosse Back: 5 yds due. Devonian cl. 30\ft internal, Septaenaria communis. 33\ft dark colored cl. 50\ft in. basal argill. rock, creek level, Up this Fork eastward, the lower part of the preceding sections well exposed. It is the lower Grinnell chalked. Notice that with the white layer is plainly on display

166. 1/2 mi up branch - Medlock branch, Der. L 22 ft natural desiring, circular loose. 70 ft natural Level plane of Dand Brewer 7ft nat. gravel Shale bed in brick Farm house to Carzy county: 1/2 mile more. From north of Medlock branch to Rollington - 2 mi. And to Fland and - 2 miles. 167. Duffin Layer = 10 ft. Chaly Der. L 1 ft exposed Sandy layers at face of Devo man, not exposed will emerge for measurements. Shaly Ordovician li horizon exhed on. Possibly same dth above 168. In Amherst < R 6/7 Shaly layers 1ft hard fossils connect me. 7 2 ft arg. with fossil ferns 5 1/2 fissile remains at flat under seat top 1ft Leaflet slabs above 14" arg. & all time in. 4 1/2 ft interval. with sand. Duffin amt not measured 9ft Chaly Der. L. called sandy layers 6 ft massive arg. dth unknown R> according to section 168, the first ceding sect ms 167, reca consist of Shaly Ordovician immediately over the Amherst, 169. Last Ordovician. 170. First Black Shale South of Parksville I found Ypthrth in Polygonal form = 51 Yrs. I deal place to ngasme St Louis - Black Shale section. Milledgeville. Half a mile NN part where Black Shale beds turn to slightly East toward Morganville, also as noted by Wirt to William Sover the land line just below reading William Sear, Departs a Shaly Ordovician Rock age uncertain. Dermaian about 6 constant of usual layer thin Just beyond thier point where its Black shale picks turning East through Bridewell's Providence and, Plate joiner at C. Recently upper Fairman with Date layer above. a thin Morganville.

A.- A little over one mile west of Huntsmville is [illegible] the lens & Ortho[?]chula [illegible] Fairmount. At a large valley where a bunch of Hanging Oaks oversees the forks. B. A short dist now beyond fork's of pike 1/4 mi west of Huntsville in the southern branch, I found Conglomerate strata, Derranian limestone, 10ft direct & l with 'folds' for a bed 56 ft dist exposed 10 ft argill. l, & 1/2 Platform direct = upper Fairmount? (At least it's above the Ortho[ rhynchula horizon at the bridge now my Huntsville, creek level line. The Derranian limestone has been present at all exposures along the western boundary of Fairmont from Wineland to this point west of Huntsm- villle. C. Where road turns south 1-3/4 mi W of Huntsville, Der. limestone, 6ft directred & Shale langes, see section 224 old run in. About half a mile beyond the unity boundary where a road turns off south) Black Shale is exposed; A tiny distance of flat land up to this point (since C), limestone is under laid by the Derranian lime- stone, At the RR cut directly S into Wineland, the Der. shist writes the residual drive ordered from it was at the top of the Onsgvillle section.

O .90 1.55 3,85 5,40 .18 .72 .54 2 .90 1.55 -- 5.40 .18 .72 .54 7 1.05 1.70 -- 5,55 .21 .84 .63 12 1.20 1.85 -- 5,70 .24 .96 .72 17 1.45 2.10 -- 5,95 .29 1.16 .87 22 1.80 2.45 -- 6,30 .36 1.34 1.08 27 1.82 2.47 -- 6,32 .36 1.44 1.08 32 1.90 2.55 -- 6.40 .38 1.52 1.14 37 2.10 2.75 -- 6.60 .42 1.68 1.26 42 2.20 2.85 -- 6.70 .44 1.76 1.32 47 2.25 2.90 -- 6,75 .45 1.86 1.35 52 2.30 2.95 -- 6,80 .46 1.84 1.38 57 2.35 -- 3.00 6,85 .47 1.88 1.41 7<60 -- 3.22 7.07 64 2.57 3.30 3.85 7.15 .51 2.04 1.53 69 2.65 3.47 -- 7.32 .53 2.12 1.59 74 2.82 3.65 -- 7.50 .56 2.24 1.68 79 3.00 3.95 -- 7.80 .60 2.40 1.80 84 3.30 3.60 -- 7.45 .66 2.64 1.98 89 2.95 3.45 -- 7,30 .59 2.36 1.77 94 2.80 3.45 -- 7.30 .56 2.24 1.68 99 2.80 2.77 -- 6,62 .56 2.24 1.68 104 2.12 -- 2.25 6,10 .43 1.72 1.29 109 1.60 -- 2.10 5,95 .32 1.28 .96 114 1.45 -- 1.85 5.70 .29 1.16 .87 119 1.20 -- 1.55 5.40 .24 .96 .72 124 .90 -- 1.25 5.10 .18 .72 .54 4<128 .60 -- 1.15 5,00 .12 .48 .36 133 .50 -- .75 4,60 .10 .40 .30 138 .10 -- .55 4.40 .02 .08 .66 143 dry -- .55 4.44 dry dry dry 12<144< dry

171. Cauderill at 875 as well as can be made out from residual material and for entire lines. Grand Switch. At creek 1 mi NW Grand Switch & thin bedded with layers, from top on, Partially the not thin bed, since the sample is confined to massive, but it may be the strip are of the same. No diagnostic fossils noticed. Stephensona in upper Lewis verno between line and half way from Creek to Gran del Switch. 179 old number! Hardly long a mile NW Grand Switch at the forks of the road, the stream bed exposes clay rock, spalling into small fragments, with Plate ponderosa &, 13 feet above this level is the design fully Brachypora and modular masses, same as Sy Raneland at Rileys. Permian limestone occurs a short dis- tance at or the level, both NW of creek presently rest more than 10 or 15 ft higher. Black shale stone, About 1 mi SW Grand Switch where road crosses Creek, going west, and thus passes, Dec 6, only 4 & 2/3 mi a distance exposed. 25 ft interval. Lugia + Brachypora + ms Aulac Canny. Still more down stream the drove entered limestone comes in at least 16 ft below the Brachypora layer. Pass the mine. At North Fork nothing known than Middle Compeller Shale led below Near Lawrence, drove entered L. Black shale 5 1/2 ft Devt. 66 ft interval spalling arg, silt) shale, modular arch No Diastromageny Lough exposed. 3 3/4 ft thin bedded rock fossils few Argillite rock with Cornwell brando + celticeras. E. Near same time 3rd Wells, 1 mi along road from North Fork up North rising toward SE / 185? 6 ft Devonian L. Spalling arg, silt, 33 ft (shaley layers, modulus + Brachypora c. 18 1/2 ft arg exposures Liptanana c. type of first section & thick the entered L.

E A gaging stream from last locality. Olati, Ponderosa comes in my left bank as further east, also and two forms of Olati cap rock with 4 feet or more on fold. The formations appear to rise up stream. F. Canning black shale divide northward into the great valley. Halfway between Maria B. Rollings and Alfred Deacons. Dermoid, 3 3/4 ft shaly rock, 2 ft Praerpetia cardules. 4 ft shale bed partly exposed. 4 ft not exposed. 6 ft turgans abundant; Richmond? Olati Ponderosa c. 6 ft Leptaena. Base of Leptaena zone next looked for. G. Mormon Church going S into Jones Fork, 4 1/2 ft Der. c. + corals + spir. ?m carage with turgans and 31 ft argillite, rock higher half massive, lower half shaly. H. Smith & Lenney Carl Rey, where road across divide joins Jones Fork road, 4 1/2 ft Der. T. Black shale. 3 2 1/2 ft shaly arg., rock, some recrystallized. 14 ft. Not well exposed here. 6 ft arth. Pl. pseudoparact rothus level; Rhy. dentata (?) not above Leptaena. Leptaena rather rare, in Lower Pliat. for derma horizon. — My Henry J. T. Hogan, 1 mi Ey S with of James Fork, On Jones Fork to left. The line splits as into N & S about 2 miles E of Broadsville, from summit of Jones Fork to the rocky Wallaway rock is 2 1/4 mile east. See next page. 5 3/4 ft Dermoid c. Cylindrospira abbreviata within 6 in of top of Cretaceous section here. 81 ft interval. Leptaena c. Rhy. dentata true form. This is one of the best sections for Cylindrospira - Leptaena interval, or account for its steepness.

Same place, My J.T. Morgan 5 ½ ft Dermal limestone 66 ft interval shaly beds, Plasmona modulos. 10 ft interval shaly with fossils base. 5 ½ pluto plant, Platy femdina 12 ft Lefraena common, + Phydendata 12 ½ ft dredged, with lamellibranch at top and Platy ferdina fairly common in general place new bedrock base (+ Pterophora in lower half) 8 ft one critical, J. Moses Fiske. J.W. Isaacs, Pleasant View Farm S mile of Ridley's on Waller's Crag shale bed R < 1 ft 10m, modulos + Plasmona. 1 ½ ft Platystrigina, collected near common. 2 ½ ft not exposed well, only footprints 6 ½ ft rich fossils from Platy ferdina, 5 ½ ft Lefraena rare except at base, where it is only moderate in numbers. 9 ft clay and after? fossils few? dagrock. Lamellibranchs: Large hand lamellibranchs, Plasmona + Cancellariini, plentiful? in shell. limestone large hand lamellibranchs 2 tangled work, fossils few? more critical + Platy femdina. The left remained is exposed in the creek and from here to the Pen- nsylvania grade bed the exposure one well shown also in the creek beds, a magnificent expe- rience of the shale bed is seen upstream. Black shale. 4 ft Dermal limestone, the Wenonam mountain, 6 ½ ft interval. 5 ½ ft Columnaria 64 ft above bed. R < Plasmona modulos, many disarticulated and free for natural divisions ments: Continuing preceding section. Dermal limestone 8 ½ ft. intervals. S < 11 ft Cdl. Alveolaris common 8 ½ ft interval. (Maherville). 1 ½ ft. Strophidoma vagans, Platystrigina? 6 m Columnaria + Petrodium. 6 in Cylindrospira, + Platystrigina 14 ft. Columnaridae? - VS run further North: Derm limestone absent 18 ft interval S < Columnaria in creek Note absence of Dermal limestone where Richmond is thickest.

"Frank Langdon 1/2 mi SE of Bravel Switch, Black Shale. 4ft Duffin Layer 5ft grey silt, L. Dermin. 3 1/2 ft black shale, 5 1/2 ft fossil rich, mudsols in lower part. Lepidocena trip. Exact location of mudsols not determined, but about 6 ft above end of grey bed. One mile up Little Smith Fork, about the hill that I am, near the Black Shale school, is large exposure of shale with few fossils = Lohn Coryville, fissility in gliding top of Duffin Layer, over- laid by dark colored. 50 ft dark colored L. top mudsols, 30 ft shale rich, creek bed. S of Mrs. Nan Purdon, where lane strikes Little S Fork, 2 miles E of mouth Black Shale. 2 1/2 ft Duffin Layer. 5 1/2 Dark grey L., shell, plenty mudsols 20 ft shale bed. N dark silt / Lepidocena and C. mumon -98 ft 2 ft sandy clay. 7 1/2 ft byssocyclus C. & Plat. fendeliana. 1 ft Lepidocena. 3 1/2 Fossil fauna. 5 ft NA well exposed <79 1/2 ft Tiny dark colored limestone, 25 ft dark colored L. <54 1/2 ft 62 1/2 ft shale bed - Coryville + possibly part of Duffin but I o hard to put in that unit + shelly -8 creek bed. =126 ft from creek to Dermin. =29 1/2 ft from Lepidocena to Dermin. 126 794? 920 ft N S & S, partially, Impossible to find stream in gap with confidence. 172. Piedim out church 1/4 mi E of last, Derichot, crabs + Anistrocacia 15ft. Lepidocena Lovers. 77 ft. gate on hill road } 164 ft, 25 ft not exposed } 8 ft Byssocyclus, Pleurva large small Adella silicula crass., Plat. fendeliana 15 ft. Same sorts more common now but not same outcrops.

173. [illegible] 174. The same rich frondiferous, hnizens can be traced eastward, almost to Hanington. At 174 only the top of this horizon is seen, over land by chalk hills. 175. Lepidicera runs across here into Fakel and. Black shale 6ft. Devonian limestone. 7 1/2 ft not exposed. 4 ft light green soft clay, modules. 6 ft Spalling clay. 3 1/2 ft softer clay stuff, fossils few. Lepidocera, one but distorted. 3 1/2 ft frondiferous layers. Top of Devonian L. 40 ft Devonian L. 22 ft not well exposed here. Probably shale thin? creek level. 176. Adam. S impsons store. Black shale. 3 1/2 ft Duffin Cages. 7 1/2 in Ber. limestone. Section at Duffins end, as the lower part of the Devonian [illegible] 17 1/4 m, massive rock looks like 13ft bi.. Spalling clay arch, 6 in. Devonian crinums, Lepidocera + Rhodocelata. 2 ft limestone. 19 1/4 ft Top of heavy l. layer with large branching trygonos? not exposed creek level. 177. Breey Devil, reaches creek level; and retains type same as at 176. 178. Black Slate line reaches creek level. Smith in road to Smith's whup, road leaving a short distance up creek path 174. Here the Black Shale is by add 50 feet thick. Limestone three full yrs modules 1-3 inches in length. Conifers Gaporvady? Road along creek leading S into Smith's Fork, empties 2 mi E of Adam Black shale Devonian L. 20 1/2 ft interval de next page. 2ft Platyenda. Volatropengia Probably Umbilin but not Septata found, Interval not exposed. D one colred l, Shale bed.

over mi E & Powers P.O. J. F. Allstott's store Gunny pit is dreared L. 18 ft top part S and shale bed 16 1/2 ft drre cored, L. Possibly today. 49 1/2 ft shale bed. 33 ft richly fossil, dre cored, nodules, Same as at Piedmont church in Little Smith Forks Helotella sigmata. Lamelli frondus in upper part Plat. Ponderosa. Heteropterygia, 32 This lower Enryville Fairmount? M. Cuthill of Shrewsbury crulla or Steph. mayswillensis is found, The store is 7 ami East of mouth of Rock Branch, 3 1/2 mi West of Tallistany. One mile West of Powers is Picketry and Baptist church. Here he strike the Liberty road, gotny smaller along Holles Branch. Black shale 3 ft Dre limestone 11 1/2 ft S falling arg. rock. 2 1/2 ft Shaley arg. rock. 5 1/2 ft Spalling arg. and. 5 1/2 ft Bayprana crumma, Plat pmdara Larena in by Juric crummor Lambrum Probably the Cathedral bed or Upper arm found. 12 ft Dre cored, L. Plat. Ponderosa near top. Stephanus fordoni; 5 ft S ore and hard argill. layers running shady layers, 39 1/2 ft Drein shale bed. Whole section Plat. Shales. 5 ft Thicker shaley arg. rock. 27 1/2 ft Byprany dumaria, 7 3/2 above Callopera with Sharp mayas S all around the specimen (F) Plat. Ponderosa. Helotella sigmata crumma blue limestone nodules. 3 ft partly exposed. 14 ft. down to lowest party crack. Fine walls here with Steph. mayswillensis but where does the rock come from. Centriforums as. I adder, with granary jumble 1/2 inch. 4 ft 6 in. ? Plidrodicty a orilliate trace, in print of theme of Ar- 9 ft Plat. Ponderosa to Thur Reeves 5 1/2 ft crumma. 7 1/2 yrs rock layers with sharp. mayas willsensis. Where did it come from? Fossil very abundant in places. 3 ft Main Smith Forks

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

1/4 mi NE of Ellisburg, S, turned left, Nafely. one mile Black shale, 2 1/2 ft Duffin large, 3 1/2 ft cherty Der. partly exposed, 30 1/2 ft covered, 13 1/2 ft drove colored l. 34 1/2 ft, creek level. --- 1 1/2 mi E of Ellisburg, R, 1/8 mi E of John Ellis. Black shale, 1 1/2 ft Duffin large, 3 1/2 ft cherty Der. 7 1/2 ft shale led, 2 ft drove colored, 7 ft shale led, chiefly, covered, Bridge in forks, shale bed above bridge. --- 5 of Jackson. Steeles Run east to Liberty = Clifton's Co. 3 1/2 mi W J < Overro, modules, 40 ft Black shale exact measure R Derriman sheet. 35 1/2 Not exposed 15th margin shale bed 1 1/2 drove colored l. pet'd. 13 1/7 cutters al. chiefly shale + clay, creek flat underneath, 3 ft argill. dirt rock, possible ? Septerna horizon, 1 1/2 ft argill.rock. A S < 1 ft 20. 96 1/2 ft typical Permite but no grades. 30 ft harda arg., fine det min. 33 ft Sple Loma Permite Shale, 33 ft limetile. R 25 1/2 red cherty argil. Hardsburg? 33 1/2 cherty chiefly some limeston. 5 1/2 ft cherty sly 11 1/2 limeston. 16 1/2 ft l. + limest met interbedded, 2 1/2 ft cherty l. 3 ft limeston, 2 1/4 limestone chiefly, 2 ft limeston, 2 ft limet, cherty. 3 ft limeston. 1 1/2 ft 20. 1 ft shale Permite S < --- A 2 1/4 drove colored l. silty light blue clay + rock. 6 mi. l. Brazen or C. 7 1/2 ft about light arg. iron Orange silt slate 12 ft cherty drove colored l. = conspicuous larger of other sections. > long interval with nothing forming probably shale bed Large shale section 9ft { Brazos ma like form at left of exposed upper Permite, gigger above 2 mi long Flat underneath.

Dam Steel's gap branch as far as Jackson, into the upper Farm munt is bylined but no drag walls fossils seen. At Trinity Huff the wulzing large shale bed comes down to creek level. About 1 mile eastward, the wulzing dwe crossed b. comes down to pipe level. Anti-cline at Rockyford 13 apt's at Church. 5 am mill 300 yds W., p. varying. at 2 am mill 4 1/2 mi W. Ranch and Ioni E by Rush Branch the dwe 1 D we crossed b. comes down to about 6 feet above creek. Rush Branch is 1mi W. y Marion-Carly Cr. line. 7 mi from Rush Branch to Bradfordville. Arr'd Tracy's at D.S.C.H. Batemans' home half a mile west of Bradfordville on the road to Merriamac. Chunnas's ranch. Section 12, mi W. by Rush Branch 5 to Merriamac. Platy dolomite. 15 1/2 ft. below Dev. limestone phosporus are dark colored bl. Do not know how far it has days dropped - along the road. Rapid Southward rise. Thickness unknown, owing to any exposure of shale bed, nodules irregular. 3 1/4 ft. fossiliferous l., a few agam. 3 ft. shale bed 3 1/4 ft. fossiliferous arg. siltstone limestone. 1 ft. Septaria b. 2 ft. dolomite crossed b. with Batemans' c.c.s. 3 1/2 ft. argillite, w/Shell fossils found.

Top of ridge North endy Runch 334 Chert Leds, just by Piedmont Church Road off Runch Branch, leaves Runch B'ch at nr., goes NE up creeks. Rocks are almy m'tl creek all the way. Septana opened about half way to top of Water Chert leads roughly but short 33 feet 4 with a X near chest of Steele; This section very steep section has 179. Amrad from junction C.T. to Ercalty 68 on the Danville Stone and pike = Dev. chert at topy hills, 180. Dor. chert, an argill rock with plat pondera, Partally upper Maysville. yoc, 81, On this upper level there are large limestone horizons later widely seath and cast suggest that revert to the materials may be ss. farm gate (Partially considerable so, 38 1/2 ft. intervals with some exception, 85 1/2 ft total, down to T 11 1/2 ft reddish cl. at various intervals, & many the layers 5 ins thick. Plact and rutes C.C. Dalea multirzeta a rare 5 1/2 ft. Fine grained arg. hard rock? and, intubbed with frondiforus lags. Rafinergumna c Tricmlens Plact and rutes cc Calymene bryozoans, c Dalea multiseta 5 1/2 ft. Thin "sandy" and thus red fossil rocks, Plact and rutes C, CC, Tricmlens Zygozprine wardenta, Dal. multise eta, r. Pentaculites, oropris chalky, and fine vertical shales, Rafinergumna 5 1/2 ft. Percentage of "sandy" layers larger Dal. multiseta rarh rare, bryozoans Tricmlens Rafinergumna 2 ft red l. layers very 3 1/2 ft sandy layers) Plact and rutes: Dal. multiseta boson. 5 1/2 ft. Some red l. but "sandy" layers predominati Rafinergumna Zygozprina c. Dal.multiseta, mimum.

4 ft Chiff & muddy rock. 1 1/2 ft reddish limestone, Dal. multireds small, and emuindiviolals3/4in.inwidth. =R Rafinesquina. Zygnatha. 1 1/2mfd calcarla. Filimstrata Byssomychia. With scars. Bryograms No Plectanulmites seen, 5 1/2 ft Several black red. d. layers i chiefly sandy layers, gelliferds redder common. Dalms, multired & common rem tips Rafinesquina Calymene Mr. Plectanulmites seen. 3 1/4 ft chiefly sandy layers Rafinesquina. Large, also numerous small flat speci- mens. Cyclomera, spine not fd. Disjunctive needles. Byssomychia byssurana. Dalmarella very fine striae = emaculata: same as Middle &der firm, 5 1/2 ft! chiefly sandy strata. Fossils few. Rafinesquina. Calymene. Zygnatha 5 1/2 ft chiefly sandy layers. Fossils few. Rafinesquina Lmn 2 ft thick in part. 5 1/2 ft chiefly & sandy layers, Fossils few. Zygnospira. Intello pygidium. S Rafinesquina. 5 1/2 ft. Sandy layers. Fossils few. Rafinesquina. Calymene: 1 1/4 red. l. at base. 5 1/2 ft. Sandy layers. Fossils few. one Dalmarella. Rafinesquina. No Plectambr mites, 3 ft. Sandy ink, Fossils few, Refidescuina. T all low interiors in small, strony 1 1/4ft No specimens. West tip <Ymmele. Crane geaained Rafinesquina. Possibly top of Lynthurae. 20 ft Mr Experiences. 7 1/4 ft thin & sandy rock. 1 1/2 ft Massive Gd and later kind. Blue rocks like Perigrille, with Nebrusella hantifurcation's common. St. 181. G armb agudstone, one or mill, exact base not known.

182, excellent cazo of pressure holders with top and 1st m remaining parallels and un- turned. - Lexington on l. 11ft midt fossils in, Dolmanella etc. Rhyne there several Graeana few. 2 3/4 ft more from layers candy l, 11 1/2 ft sandglimbed mes. Rather few fossils creck. like Barand a little 183. Ify built + smth slp'ed sm'll with Dornian crels Not unspen'sia & quite a mm in y Rhyne from a t Hebertilla franklyt mass of lexing'tm. The Lexington is also a shut dis- tance below, 184. Barites rich with large masses of zinc. Afg. Hayden farm. from some little north of E. The south wall is cliken' sided vertically. The south crushing ledge is Lexing'tm with Rhyneby glena feet from Sept'ence + Dornian r. The south wall appears to be the same creek but I am not certain. Possibly only a slip of 10 to 30 feet.. 185 - NY vicinity city, Duffin cts. 6 3/4 ft Duffin layer. 5 ft Chesty falls. 7 in. 2 1/2 ft. grey arg. dimest mes. wt. 2 ft 3 in. Comp'd native little chest. 2 ft 3 in.) ? Ordovician. Plain ponderosa. ? ? middle 186 - Massive Barandss. overlaying much larger section of thin bedded shaly Barand ss. Fronds absent except Rhyne genera in very thin calcareous lazes. 187. Eden red. ls + 's sand' layers Dal. multidecta, Plect ambrutes. Pyssomyclus reda, 188 From last locality the aden extends half way from 187 to 188. At 188, 100 yds south of the culvert over the creek, the Barite vein from 184 shows up again. It also shows up just of the grad at 184. The vein runs slightly N of E. St does not fill on the creek. Possibly the Caputhiana has dropped in. The South Side a very slight rise again. One shearing strike we in the folds of the vein above.

189. [illegible], candy shale &den. Firstall Draped a little. No Cynthia and seen unless it is on south side of vein, no cynthya rock in ditch. D notful if seen at all. 190. Grand os, chiefly shale. 191. St. Stephenana majoriilenis - Fam- munt. 192. Dermon chet, 5mg Smith ward dip of upper part of Duffin laya, 193. At hme, base of Linierta, wit Black shale dnn the road northward & south ward. 194 South z Parksenville, top of hms. Lithothamn cylindrical form. Lithothamn irregularal grove 29 ft 5 St. Louis, base part with Spinifer & Productus crinoid. 11 ft 5 Spagan, full of fossils W <1315 U.S.G.S, 25 ft brnnish with chet - Ruckstone. 2½ Massive Kurbstone. 16½ covered 10½ ft brownish Kurkstone fully acc to some 8½ ft Massice Ruckstone in 2 of ferdes small. 22 ft Rucktone with grey laminiah, 107½ K norotched, or chet 195 30ft belon level of Sparger. Rhupido- mella dubia fauna is found. in thin bedded chart [illegible] connect us. The chert limestone has its base 25 feet before the Spenger, former ditch above a very massive Rucktone section. North ½ section 194 this thickness was 25 feet but our acc and was taken of stray on their dips where one must infer 5 ft thin chert l. mentioned above. Massive Sandstone alone. 13½ Rong ex part belon 5 ft limestone, Very cherty below 40¼ massive Burkstone. 38½ ft less massive Burkstone. 90½ & after Burkstone. 196 seek at base of 2 sects rms. No exposures for long distance. 197 Linierta clay T not seen. 198. Linierta clay to mouth of creeks Black shale at first appears dnn North Parka, hence north of Parksenville hand must be about at level of top of B Rankte Shale 199 Linuth clay at base of Ruckstone R> Top of ridge. 32½ chert head Hanados hms. low but flat, 38½ No exposures, Rubble like waterbeds. 77 ft Rucktone, good in upper half. 47 ft after Kurb tone 44 ft Should Kurkstone ? Linneton clay at road corners.

Cath[red]ral church. 30 ft S natural. 14 ill[ustration] cylindrical 20 ft with orbitic shell. R) 200. Nothing certain except [illegible] large [illegible] since 199, at this last locality - 200 - Phillips mella and other Hardedsburg [illegible] one found. 201. Whitish bed, 5 ft fully fossil, grey sandy appearing. 33 ft up is St Louis with Syrin appena & Archaeocidaris spp[erif]. 17 ft up with St Louis L. [illegible] limestone. 2 ft. Very abundant and quartz pebbles 1-1 1/2 in diameter. Tips of sections. 202. Massive L, like Spengler[?] ft about, apparently, judging from blocks along the road, with athurton like material di- rectly beneath. [illegible] oinoid, at road junction. 203. Limostone & Syrin? 9 in the underclay at least or dy with fossils [illegible] 204. Sipy Kurt, large Cymploma, blocks remaining. 41 ft internal, with surface crow by cyl. blocks. 6 ft sand, yellowish brown + some white. 16 1/2 ft out exposed. One loose St Louis block at top. 1435 NSGS according to [illegible], 15 ft natural & St Louis chert and zone shale beneath. Tips of massive L, such as we like the Atherton clayey ma- terial. This massive L is pretty Atherton bed and just the Spengler perfect. 205. The arch appearing size 2 with ward. The other the L exposed by reaching the [illegible], and this in nothing but HARDdsburg about is seen. Further south, the road gets down to the good forming limestones. 206 Bed of [illegible] limestone at junc- tion with road across ford, 207 Tipy Black Slate & 3 feet above creek crossing 208 Black shale at 1600 ft NSGS.

209. Black Shale top at about 1100 U.S.G.S. judging from Cmt four lines 210. Black Shale top somewhere over 1070. Probably close to this number. 211. Black Shale top somewhere over 1100, probably very close, since it at least reaches this level, but is found when pipe crosses creek, westward, south of RR. 212. Eden at South base of hill. Dalm and g abundant. 213. Eden, Dalmarella northwards + Dinys (cleus) 214. Eden Dalmarella, Drima cleus. 215 Rock resembling Birdsong. What is Peryville, as cynthiana? 15 ft partly coarse grained & regarded 4 ft Dinthis ulrichi C. Internal mass. 4ft. Perryville bed. No fossils Top of Paris bed with Rhychnisteria + Debatella 1-2 dept erosion, part of top miles fine grained. 216. one f Perryville bed. finely, with Ostracium + thin fossils R 12 ft fine grained firmst one, weather 25 ft practically with out fossils. Grey, medium grained, l. Several (Rhychnostoma, R = Ruffle C. cutania, Rhychnostoma & and H. frankfultensis (rare. H Murrina C. Murrayana (several. 217 (5 1/2 ft massive l., fully hygroso, {Dalmarella not multistrata} 6 1/2 ft Shale, sandy, fryogranu 8 1/2 ft massive rock. 14 ft. Dinthis C.C. 1ft 2 in Stephana vicina C, Rhyndor truna, TRhyndthemacss. stephanus 6 in kilina. 9 in Rhynchostoma. Hbf. frankfultensis 4 in Stenmatoceras Olatystrophy 3 1/2 ft Perryville bed. creek bed, 48. Dinthis ulrichi 5 not exact just measured 5 ft Perryville, I never seen. creek, 219 Sandas so. 220 Steph mayrillensis Olaty pindyna. Parksville.

221. Alum Shale, S & J Pervilled abundant Regarded as Aethium 222. Top of Black shale about 1100 USGS judging from country levels. 86. Pervilled bed exposed outside by rock containing B. transpat. aestis. This contribute proof at 217, that Pervilled bed belong tr the Lexington limestone. 223. Harrodsburg shales to top of bluff. 224. From 223 to 224 only Harrod sburg is shown at top of bluffs, from about 1300 up. At 224 there is a little patch of Aethium limestone, 4 feet thick with Per- villed lying upon. 225. St Louis L. in place, at very crest of bluff = 3 ft. Rockcastle conglomerate fossils, 226. The Aethium bed is well exposed along the road, near the road junction, Near 1270. {11'2" Aethium bed, chiefly massive limestone but with layer interstratified exposed. Rock may be clayey, 4'8" Aethium bed, chiefly clay, same L, {11ft B & R's ledge, massive limestone. 7'11" Clay 6 ft B and R's bury ledge L. 6'6" Chester A and R's bury L. 15'1" Harrodsburg lower half weather sandy. 2'1" Chester massice, 16'1" Harrodsburg, very massive. 20'1" Ordovician ns, Harrodsburg. 42'1" Harrodsburg 16'1ft. London road in front of station. Harrodsburg L, there has good fossils for collecting, not skipped. Top of Black shale is about 8 ft below or RR level, 227. Face of Linnetta ledge 1020 a comatate USGS. 228 - Blue grey sand ST Gmina L 15'1" sort of sandy L weather- ing 228. Maybe St Gmina. 1250 {15 ft Aethium limestone, USGS it under lying L. Rockcastle conglomerate fossils are abundant. 76-77. E den thickness up to blance limestone at top, in above cliff sandy layers 4'6" 1/2 ft Secotan Ledge. Top of bed not seen Seden. Probably. 38'1" ftb with Dalmanella at top 19'1" chiefly sandy shale 22'1" E den with coral L, chiefly do

one and a fine lime mud. 5+2 ft. Taken, chiefly clay m't hygroz. {3 ft. limestone Pentall Cynthiana, 8½ ft. Missour l. fully hygrozo, 2 ft + % of exposed {with nodules in mass 9 ft {fine grained: Cynthiana 7½ ft Limestone Christ bed perfectly 4 ft Overgravel beds. 49½ft. Paristeed Middle Yore partly on the neck. Eastward the rock rises rapidly so that the Casyville is not seen even at the highest point of the hill North of the road, as far as the pike. There is a peculiar Boulder place as in the Cynthian beds along the Abingdon river, near the creek crossing. 56 - Bridge level 831 USGS Base of Curdsville = 842 ft.1 229. - J.T. Sandidge Barite vein: I had a very little zone at Smith and Runs N+ S with practically Then layer Lexington m. The rock has the zone cm tilted larger in it as east of 76-77 on the way to the creek crossing. This can tilted layer how deeper 4 feet in the west side of of ocins. 900 - 950 USGS 230 SAM and sandstone. 231. Hardscrub. {Cynthiana "Thompson-like 4 ft. {red l. m't Dalan and multiacta clay shale 12 ft Fine grained arg. L. + small more 6½ ft. Limestone + clay shale. {12 ft Limestone, weathering badly. Full of Pelica open up thin hygrozo, Cynthiana type, 7 ft. argillaceous rocks with scattered nodular masses of size of fist, Zygospina Lingula. Dalanville thin and rare. {2 ft. Steph. vicaria Rhapalochitonia, 1½ ft Large stromatolites mm. 2 ft Same grained art. Helurella franklinensis; Did not see certain, Pergrillite bed. The Perryville bed evidently dips for a long distance NW from the cut. 232. Gray Smith and along the RR the Cynthian and Limestones are underlaid by the Cynthiana and slate argillaceo and limestone one. 233. Smith J The road crossing, the stratum with Steph. vicaria is exposed. Overlaid by another layer Cynthiana. ½ John m't rather a coarse till. Large Zygospina near First Dalanville

234, From 233 the arch rises into the railroad. At first the whole from Cynthian argillaceous limestone, cm. paralithic few fossils exposed. Then for a very long distance, the upper slightly fossiliferous Cynthian is full of layers and is seen for a long stretch. at the highest bend, at 234, the broad green laminated mixed with clay and lagers is seen, full of pyrgoma in some of the clay lagers. 235. Sandstone, just above RR trestle, 236, Tetradiem, Rhyndotierne, Hebertella frankfortensis. = must not be geodiscus. = Rock taken from Perrysville bed. 237. From rock = ? Oars? 238 Praespora stimulator 239 Placopora stipularis 240 Prasepina + Rhyndotierne, 241 Hebertella frankfortensis 242 Hebertella + Dalmanella. 243. Prasopna 244, Hebertella, Rhyndotierne hayniava Lophospira medialis. Vanmensia Hactivina saleri. 245. Richly fossiliferous zone taken from typical Perrysville bed. Fine grained... 3 same as 236 and 244 3 fine grains Clitomerites Mine family exposed, not studied. belonging to Mr of Perkin road. th clay, No fossils. th clay with pyrgoma. th rock, rock, with Galechia in loose rock. and top, fossils. Flat and medium clay mixed with fossils. fossils and rock, Massive. Shale at several layers, shale. granular fine silt, rock, fossil fro fossilized layers. and fine grained sand in shale bed. internal not measured. fossils along and out. W. along the RR ichnia and shale bed. the road heading from the turned to the fossil localit Galechia horizon is red, also the overlying Rich Clymania are + stratigela our county road in the fields, stream along the road. This section should be studied and measured,

Ballett um

234. From 233 the rock rises into the railroad. At first the whole Eria cynthia an general coarse limestone, one paratively fine fossils appear. Then for a very long distance, the upper night fossil ferns cynthia and full of frygaria are seen in a long stretch. At the highest land, at 234, the hard beds lowest me mixed with clay sand layers is seen, full of frygaro in some of the clay layers 235. Strephocina, just at RR level. 236. Tetracium, Rhynchotremum. Hebdella family for ensis. H mustna. Ovaciscus, = Rock taken three Perryville bed. 237. Iron rock = Oars? 238. Orasphera simplicata 239. Pterophora simplex. 240. Orasphera + Rhynchotremum, 241. Hebdella frankpeterseni 242. Hebdella + Dolomnella 243. Orasphera 244. Hebdella, Rhynchotremum hagniana Lophospira medialis. Vancouveria Hadrinura Salteri. 245. Richly fossiliferous same film in the typical Perryville ht. Fine grained... Same as 236 and 244 Clitambites 3 ft fine spear dolomite. More family for one of the Pergus Gap 246. Fine exposure, not studied. 247. N of Ophelia 4mi NW Pichum and R 2ft thin clay, no fossils. 2 mi thin clay in th boggy area. 1 ft white rock, S half. 2½ ft clay shale, with Galechya in lower 6 in hard rock. Round top. Weathering casts flat of indium. 6 ft 6 in, clay shale with fossils. 4 mi fossiliferous arglshale, massive. 3 mi clay shale 1½ mi S and injured layers, 7 mi clay shale 12 in fine grained fine l. rock, fossils. 3 mi shale 6 mi S and injured layers. 4 mi large fine grained with 1½m shale 6 in hard fine grained rock. 5 ft regular shale bed. Base, 9 internal not measured. Flat pendulum along and out W. along the RR R> Inner Pichum and shale bed. 248. Along the road leading from the pike eastward to the fossil local by 247 the Galechya horizon is well exposed, also the varying rock in red, Clithambites + Streptolana, vagans over south road in the fields, but not seen along the road. This section should be studied and measured.

Merritts ferry, <clint in ft. 32ft bluish clay, 29ft sandy l., softer. from common bryophylt not identifiable or cfpt/identifiable accidental?, no depression, m. Platystrophis 5 1/2ft. harder sandy l. ledges, 6 in. hard & sandy l. 26ft interval. sandy l., softer. Tetradiium, Latechia, Crummania varia. 1ft Platystrophia {identella... 16 ft interval, Milt cordifrons Same locality, clint m. 9 1/4ft. measured vertically. 1 7/8ft sandy l. wa {Tetradiium 4 9/4ft shale bed: tb 3ft freshy moss, 5<1/2ft. Hard l., layers, lamellithana, 1/2ft shale layer in front, 2ft covered. Lamnerata minima. Down the river 100 yds. S<14ft massive l. 6ft shale bed 6in Latechia crumma. 1ft shaly clay. 8 ft. Platystrophis dentata 2 1/2 ft covered < river [illegible] Ferry, Perried section, nt m exposure, light blue clay vanish clay bryophylia. Om. In sandy l. + bryograms, Holardia rder sandy l. sandy, softer l. m. 12 specimens. dim c. Latechia C. crummania shallowers sandy layer + bryop., tells without error. Platystrophis chaly rock. Town Redmond slit blue clay, clay bed. Latechia crumm. aly clay at ponduga s. ptera silu fridali at mse. lnychotoma dentata 14ft above me. and from graded, gastora layer. mmed. By river below clint of Red river.

Merritts

Merritts ferry, 2el into J Red River Clintm ft. 32ft blueish clay, 25ft sandy l. soft n. forbits common byrggrace t not identifiable as refi / schistile accidentals no depress'm. Platyphyllia 5½ ft. harder sandy l. ledges, l in. hard sandy l. 26 ft interval, sandy l. after. Tetradianum, Labechia, Columnaria varia. 1ft Platyptilbia {1/Intella. 16 ft interval, mild sand 3-5 pts Same loc at 5, clint m; 91ft measured vertically. 1½t hard loam {Tetradianum 4.9 ft shale led. tb 3 ft pretty mins. S<12ft Hard l. layers, lamellihand, 1½ ft shale layer in part. 2 ft covered. lawnwater sign's. Down the river 100 yds 5<1ft massive l. 6ft shale led 6 in Labechia comm. 1 ft shaly clay. 8 1/4 ft Platyptilbia, rhinotidic 2½ ft covered < river Merritts Ferry, Rerived section, Clintm exposures. 27 ft Light blue clay 5 ft brownish clay [Platyptilbia. Om. 25ft soft sandy l. + byrggrana, Neteida 6 ft harder sandy l. 26 ft, sandy, softer l. grena, 12 specimens. 1ft Tetradianum, Labechia C, Columnaria 3 ft free'd flowers sandy layer + byrgg, Neteidea without germ. Platyptilbia; 45 ft shaly rock. Lower Redmund 1 ft. Light blue clay. S<1ft massive l. 6 ft shale led. ½2 ft Labechia comm. 1 ft shaly clay. 8 ft Platyptilbia, C. Septalona rhinotidali et base. Plynechthoma dentata 14t above line. ½ ft Hard fine grained gastorn first layer. 2 ft Covered. by river below south of Red River.

College Hill, East of 1 mile. (T believed to be equivalent) Colmunaria lignum at Merritts, Chinon. 38 ft. Light colored clay 20ft well bedded rock. Good going up. Good exposure at hand of T>28 ft [well] bedded shale to 1 first 22 ft shaly clay rock. 44 ft No exposure. Light clay with flat sponge. 7 ft. clay rock. 2 ft clay rock. Harder, Plat. Fenderas, 2 ft clay rocks softer. 1 ft glimmering layer, fine grained, 1 1/2 ft gasteropod thin fine grained, 11 ft shale. 7 1/2 ft clay rock. 2 1/2 ft clay rock Plat. Fenderas, 5 1/2 ft Hard arg. shale with Plat. Fenderas rather common. Here no Fentana was found. 18 ft Myosmyrille dark colored. Flat layers rather few. Barkwipeds common at top. River level. Ridgway Reservoir hill section 250 E of Reservoir: 4 yds. Ridgway light clay rock, Base Ridgway 2 ft spalling clay rock 4 ft hard blue limestone fossils. 1/2 ft very dark shaly rock. 2 ft hard dense limestone, 2 ft thin layers pink exposed 1 ft very dense blue limestone. 11 ft shale bed, lower half 6 layers as well as shaly, upper half is fine sandy. 3 in. half c. Plat. Fenderas. 11ft 3 in. fossiliferous clay rock, 17 1/2 ft top of recent part E of reservoir at point bar there just along joke. Rather as well a coarse c. 5 1/2 ft purely exp new form. Half animal m to above, 3ft dense exposed c. road leads off N. 257. Warren Mints local 5 Bridge 54, Clearmonts c and Dalmont in multisection, down tr. 10 ft stone RR. A short dis- tance later, a more argilla- cious rock lines in with Pofim equinic c., and a few Platys- stratinia. This lime rock appears argillaceous and thin- bedded. 252 Middlecentation, bridge 52 Same myriacoccus arches as at 251 ha

with thorough limestone interbeds Also Plectostylaria rate. Most ward this as pillaceous section continues to expose Cephraspisina in great abundance, a few eliminated. Herbertella rather coarse than fine grained; and Plectostylaria. 253 Bridge 49 Road - public - since then 254 Bridge 46, a junior road crosses here also gradually. 255- Bridge 47. Cephraspisina very common, Plectostylaria, Conuloceras juveniscus. 256 East J. Hayden Bridge 43 JP not seen. 15 1/2 ft Hindea Cystithana. 17 ft Softie argill., bedded Cysth. 6 ft granular massive l. RR level. A short distance West of Hayden is a fault with Eden projected to RR level, fall westward and is sandy fossiliferous rather Cysthiana. 257 Clay Miller mile. West 1/4 line gyprotes are much alike. Cyan the ones two Jor west, ye 39. at O'ajakit 1/2 mi. E of g Valley Wine Lexington top above RR level, cina serrata) 4 1/2 ft helm interbedd gray, top of Lexing- Tan. ss. 6. Staph. M agenillana; my house. My says - group in western road. 9 mje house on NE chula layer of Tale layer, gassy from here visit I most post-came zona planum? me, perhaps? = Striptasma vagans ogm forms, between flutes like 5y int, 2 1/2 ft shale. 1 1/2 x Mte massive clay rock 46 1/2 ft shale, from Richmond. 1ft White clay at very Birdsmouth post 2ft nodular clay rock with C. chelina at base and also 6in firm top Plateja grandiera = 1ft down, 2ft clay rock, 3mll l. with Plateja grandiera,

with thin rough limestone interbedded, also Plectogyridula rare. Westward this argillaceous section continues to expose Representing in great abundance, a few eliminated. Helbertella rather cruiser than fusiformness; and Oletostephus. 253 Bridge 49 Road - public - cross - bar. 254 Bridge 46, a jerry road crosses here china gravelly. 255 Bridge 47, Ophites gracilis very common, Plectogyridula. Ometellaria femininus. 256 East J. Hayden, Bridge 43 JP not seen. 15 ft Heller Cysthionae 17 ft SHiller argill, bedded Cysthion 6 ft granular massive l. RR level. a short distance west of Hayden is a fault with Eden projected to RR level, fall and westward by slightly fissile for some miles Cysthionaea. 257 Clay Miller mill. West of here experiences are uncertain, Cym- thus one this I can not. 258 Bridge 39. at Oafshet church, near Eberty Valley Rim, Wile Lexington hp is 13 ft above RR level. 259 { Stephanicina serral 4'ft thick Dinutilus whithi good type of Lexing- (Rhyzommatit.} tan. 260 261 GANAGOS. 262. Bridge 66. Steph. M agnillana. 263 Scar trough lenses. M nays- willemai, common in wetwood above RR track. 264 Bridge 68. G mya house on N E 265- With Rhyzomata. 266. Large exposure of Tale layers grayly from here 248 Second visit, most problematical R> Stephanoceras planum? ma, partly in place, - Stephtasma vagans 4ft { Wmthington fauna, {lone B between flute like sy set, 2 ft hard l. granular. Plectogyridit, Helbertella 2-2 ft shaly. 1 1/2 ft M n massive clay shale 46 1/2 ft shale, from Dickmound. 1ft White clay at base of Dickmounds fossils 2 ft nodular clay and with G whelk's at base and also 6 in from top Plate pendulosa - 1 ft down. 2 ft clay dark. 3 ind l. with Platejundersona,

"12 ft clay 1 ft from layer no Oages. 3 mi Pelynclothioma dentata, highest in place. [illegible] pit ke. Traded with clay in Oages, 17 ft sand hard shot a mite. Streptelasma vagana. Rather common in lower part. Peramellias flat clay, Pelynclothioma flat, like 3 ½ ft hard sandy layers wit 2 ft softer sandy clay, 2 mi hard sandy arch. R> 4 ½ ft sandy layers + Pelyncly. caten. Streptelasma vagana longis. [illegible] Interpretation. 31 ft Middle R. clunara 2 ft Massive l. 51 ½ ft Lower R. clunara. 6 ft down to dentata layer. The Amberm probably belongs at Bleak Point, S of Belda 3 miles. so. [illegible] [illegible] only in the upper 10 ft. [illegible], but begin to be it, and with a great proportion with numerous other's remain. Lower blocks similar l. 38 ½ ft Internal with immersions. 33 ft. Inter like St. Ymbsl. Fine sediment l. 22 ft same grained l. like StYmbs [illegible] in it. 25 ft whitish l in satin. 13 ft StYmbs appearing l. with 2 ft white at base, pretty dense. 20 ft St Ymbsl. fine grained. 5 ½ ft [illegible] Chats l. full of lithostromin 22 ft heavy o f series. 3 ft Massive StYmbs arch, 2 ft soft green clay in part. 5 ½ ft Massive yellowish rock chippy. 7 ft. Brownish soft clay in part. 8 ½ ft Massive yellowish rock. 6 mi. Sand grains 1/60 inch di amete. 2 ½ ft lithos na. 11 ft Yellowish rock, massive, Yorks 3 ½ ft internal - so. Spring. Massive so.

S W H Birmingham Ky, In reverse order. Pentamerites fagiiformis. Agassizirina gardini) Paleodorus Arthromedus Orthoceras chertaceous spherifer megay? Derbya exceller Chlamida small} 20 ft thick grns fine grained l. 5 me of the layer weathering slabs, = Bermingrushells 10ft Duroral Yee ss, formation. Crab net traps about 50 ft up hill, but not one met meas ned. 246-Dannelle, Ky. Valley. Othad' whi lvsse. 2 ft granular l. Vanxomwda' mpph ldy. 2 1/2 ft granular l. Vannorani'fm, 2 ft whitish granular. 2 1/2 ft grey granular, 5 ft darker, finer grained penty fossil iflems. 8 of Slevans Dalley Ky. R<10p massive l., Agassizirina 1ft rotten l. 1ft clay, 2ft 3in. In massive l. 1ft 3 in Clay 1ft 3ins in massive l. 1ft 9 in clay 1ft 9m in massive fagiiformis, l., etc. white moss fossils found in l. here. 7 1/2 ft Birdiff freshbergrna clay, 2/4 limestone + clay interbedded 1ft 9 in Massive l. 1ft 2ins limestone + clay inter bedd 1ft 3 ins massive 1ft 6 in. bit samal out exposed. 1/2ft Limestone, rather full of fossils. Top gcentimons l. 8 ft Massared. Productus clesis ensis. Pentamerite larger than ordinary P. gardini. 1ft massive. Top g recta 6 ft massive wellmink rock 1/2 ft soft clay, 1ft hard yellowish red clayss. 7 ft soft clay with several thin band 1/2 spalling yell misth rock 2ft hard rock 1 harder clay rock. 2 1/2 ft soft clay. 1/2 ft soft spalling yellowish l. 2 1/2 ft harder y. flintish l. 2 1/4 ft Soft yellowish spalling l.

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

267. Nebatella tricalis 268. Rhynchotrema c. Brazoria Nebatella parkeriana 269. Rich's foraminifera rich film the time Perryville. 270. Chert, agglomerate 31 yrs, dust on fossils 271. L'hoste in hexagonal cylindrical in chert. 272. Rapid untracory. (Arthur 273. west there is Lithothamnion cylindrical in place, in a very chert granular l. breaking amuch less chert fine granular l. 274 Spinger like Martinia in being nearly sunott - Harrod, Brass type, also 34 yrs? Perthumto considers new middle = Cummings Station 275 Large part of the very grand Mural) Section. Mr J Martelby K 5 1/2 ft fine grained chert l.,<268 273> Lithothamnion hexagonal, 5 1/2 ft fine grained l. + few Spring spore 5 1/2 ft less granular l- sweet sand rey. 4 1/2 granular l.+ little chert. 7 1/2 V top j fine grained l. 5 1/2 ft softer l, weathering shaly, 2 1/2 Hard l. 4 1/2 S & T L, weathering clay 8 1/2 massive + concreted l. Seaming to clays 2 1/2 j- s.l. laminated and bedded / upper weath- 7 1/2 fine grained l. Softer - spalling turn and face. 13 1/2 ft ? fine grained l. 4 1/2 softer shale, - shaly l. 2 1/2 Harder fine grained l. Together - Cummings Station too regards deposition but hanging 4 1/2 Massive fine grained l. thin bedded 3 1/2 weathering soft, 14 1/2 granular l.- Spencer + Pontien lto: Considerably crossbedded l. 7 2 ft in shift the clay, for some in lower half, with large red and chert c more- 1 1/2 ft indinated Perotme like rock. 6 1/2 soft blue clay. 1 1/2 ft Jellnish spalling rock. 5 ft Rather crossly granular l. with some large blade stems, Large zoophites, 3 small Sping fers = 14 Arrasbury l. 7 the Hurstome section perfect, places. Regarded as belonging to the underlying rock at least in lito indicated but I am than 6 ft circular spellowt rock, but more 10 1/2 yf Shale like yellowish l. but probably On limestone with that nodules ? the one 3 2 1/2 greenish cross clay rock pebbly 17 1/2 Chiffy soft blue clay abode. Weathered, but part of it shivery, for it a few s & balm flint masses 4 1/2 Polterino archual Perotlome few arces included in Hurstome 5 1/2 Lenticular lardner nodules 25 1/2 mine indurated Hurstome L 124 miles. 40 1/2 Spalling clay shale, hard some, Brass Section at loc 277

276. Rim'd clay top of St Ives Filled by white Chlora which near base has small shells suggesting Spinger Type. The rock is vertical near the base. 277. Fine grained bl well bedded, crowned by whitish l. 278. Great thickness of argillite l. At least 25 ft thick. 279 Lithothamnium cylindricale 280 Two feet of Spenger chalk here contains quartz granules up to 1/32 inch, but very few fossils and there are not characters; die. Recognized lith Argillaceo by comparison with Wallbridge section - 100 ft N.S.G.S. 4 ft arg clay Reddish smartly n chalk nodules, such as seen at top of Warrids dirty section, at Marcthury, 281. No trace of Spenger. 4ft 8 ft clay <- Top of reddish chalky nodule layer 3 ft interval from top of chalky layer down. 1/2 ft l. = Harwood burg. 5 1/2 ft. interval, 1ft <- Considerable chalk firmly in place. 50 ft interval in the St Ives free stone ledge about 3 ft thick near middle. Rim'd level. Lamsted. 282. 1/3 feet of freestone about 2 ft above roadman level. At a higher level, on the smit face of the tunnel cut, an upper freestone, much thicker, shows 283. One the upper freestone c.lbc 284 which is about 8 ft thick, comes down to track level. 284. Great thickness of St Ives & Tunnel 3 1/2 ft more massive l. R> 5 ft massive arg rock, some chalky 1 ft thin layers, weathering clayey, 3 1/2 ft Massive rock, Spinger Revival 9 ft massive rock, crinoidal + free life worms locally and important as in Harwood burg occasionally on upper horst side + Rhupidomella dubia, about Wallbridge rock. R> No trace of Spenger here. 285 Narrow gap over to Big Hill, 6th Sandy face of St Ives with 2 mm grains. 32 m diameter = Spenger. 8 ft Interval = yellowish rock reddish nodules very frequent as onones, same as below older Spenger sections. No trace of Harwood burg. nor massive sandstone.

286 R> 11 ft chiefly yellowish shale. 1½ ft fine grained limetone. 4½ ft Hardie above. Soft below. 6 ft Hard medium stone. Soft clay, Yelm. 7½ ft Hard dark blue. Soft below. 2½ ft Hard rock. 2 ft Soft rock. 2½ ft Hard rock. 4 ft Sm. Shell. Gravel foot clayey. 14½ ft Yellowish shale. Chert nodularities. S> {trip.} both top and bottom, Sand at at base + Pentemites small at 8 ft orth. at top w/ minuter shells 19½ ft oolitic at base = Dacenia. 3m. {-Rosicaria?} < Sandy crptlamin to 70 ft 4528? 31 ft St Grus. 4½ ft lith. shell in cylindrical conma, cornulebeads. 7 ft limethestone w/ thin few large R> T> sand limetone. 2 ft (Similar fine grained layer, lay. chiefly radiate athyrid worms in thin layers here & there.) 3 ft fine grained l. Gravelly foot. 8½ ft somewhat coarse grained l. 11 ft fine grained l. U> 17½ ft [illegible] mottled chiefly 8½ ft Silt exposed at left clay at base wht mottled w/ [mosty silt m.] 27½ ft Siltoral. No exposures. Yrse block of l. w/ th Ages exposing partly came from here but may have come from further up. 30 ft Silt oral. No exposures. T> 287. Paint Rock trip. T ate layer. 288. Orth. Rhynch. layer, covered by Tatalayer + Crugyville rock. 289. Sandy Grwn Richmond. White fossiliferous clay. Anheim from top + Septa area. Yrme Anheime sandy shale. Dne colored l. = Hspite Cargyville. (Yrme Crugyville rock Old. P indiana.) = [illegible] all over middle rock Anheim Septa area 60 ft above creek level. 290. Dwe colored l. about 10 ft above road. Yrme argill. nubble l = Yrme Cargyville. Tate layer in creek. 291. NW of J. M. Campbell. Anheim base at road level + Septa area rhynchid abs + Rhynchostroma dentatum. 1½ ft m [illegible] domed l. Regular from Anheim shale bed,

292. Smith & Jerry Russell. LaBachia, Almond. 5 from farms 2 ft [illegible] 5 1/2 in thin limestones, yellow and flat-pendarosa 5 ft fine calc'd [illegible] fossiliferous. 13 1/4 from Amberlin shale via creek > upper fine calc'd Cozynille down the creek. 293. Limestone thin bedded, in farm Cozynille & Park layer 294. Almon Springs My geometric [illegible] Farmers marshes in [illegible] Devil. This horizon finally divides between typical Duffin layer of Black Shale since the 15 black shale is immediately above and the Duffin layer is not color at same depth though. Of great thickness at gradual angle westward. The highest red line is fine calc'd Cozynille fully from at same horizon, under many flat pendarosa. 226/ R > Assumed to be Altherton. 11 ft [illegible] full of fenestellerides, assumed to be Altherton. 5 1/2 ft Syringportia + [illegible] Style. May be H-encrusted. 6 1/2 ft shell very faintly common at 6 ft covered. Partially joint, [partially narrow layer] 5 1/2 ft chiefly L-T-F (join per forlunk) [illegible] 11ft [illegible] dubia & Springa Berthoud Altamod his chalk exact + Chujid- [illegible] turned me 26 ft Bes of strong hard white or 5 1/2 ft in darkened burnt me. 22 ft soft. elongay Kuchetme, Still collecting and all be done. 22 ft Kuchetme wildly fossiliferous 20 ft internal, Kuchetme, and leaves little stream and gas rapidly up hill. [illegible] R7 5 ft of Altherton 20 ft chiefly L = Altherton Rock

228) SE of Mitchell's bay, Typical St Louis Lacer 9er 11 ft C. stony & muffle with fossils S= 2nd ft ly 9ft L affined Wb's commns 6½" wethly way onp 2 ft l, with O spencer [illegible] 14-½ (Blind) L or natures Age 15, ft. Internal not expressed. 16½ ft towards base. 20½ ft shelly nodules of Kuebetain. 295. [Dimotus Wb] cinnam [Strphm vicina] at 7p. Rhyndetruma (Helvetella cinnamensis) All in 4 ft Whitcher's rock at 900 ft level USGS, S about 296. Same 4 fossils in 4½t section immediately above by now Perryville bed. at 880 USGS! 297. Large Rhyndetruma forming supposed to be Orthocynula Helvetella panlyformis apparently at base of front. Spires Perry ville whereth. Lyme mud, etc. & Vannxennia arenm. 298 - 928 yf above sea = top of rock with Strphm vicina, Dimentus also Wb cinnamensis, Rhyndetruma. Onno corrects rating identification of 297 as lovely profile forms Perryville. Stratocerrum with the Strphmnera layers.. 299. Helvetella lrealis and con- siderable Wb cinnamensis, near top of Hill, seen situated with Dimentus canna and some O macrum Dysgn vacuaria. It is Paris lid on elsewhere an appears to is at base of the Perryville front. - form, bed - at top yhill by Quick's 300. Lignite and bed in the Piltongen shale d and followed above by 2 run by Elen, put some L. at top in The Eden. 301 Faulcema. Helvetella plank fossils 302. Rhyndetruma. Helvetella payke fossils. Vannxennia + Terradactin in saccharidate, at base of zone iferous Perryville as in trial 299. The simply saccharidic layers is about 13 ft thick, but O macrum occur 1½ down. Also Galalua, and The lava rock is saccharidic breccy and ont ainos Vannxennia thus raising the saccharidicae layer to 4½ in the denser locality. saccha ridda layers run about 6-7mns

bringing the tractor at least 6 ft but it should be minimum, hard that I'm concerned. it varies locally. Below the ridge from Liferow Saccharal d, from what so many forms weather not, there are at least 4 or 5 similar stone hut with comparatively few fruits, including the same large Danneella as the lowerlying rock also Schicker at top. Top of section about 970 HSCS judging from unit lines, 303 Saccharin dale entailing in its a few Nanny cave in decider growing doubted with the large Dalmanella varsoveri? Also smaller specimens rather comes without valves and flat shells pretty same species as the large D. varsoveri' specimens. 304 Riffel, + Oracaria. Obliquation. Deltetella from plication as that part al frankly at least but same species. Also the calc form, zygospira. somewhat open para crissid bases. Raffled one anticlinal Dalmanella fertiles. 305 Proceropra, Deltetella, Dal- ananella c., = fertiles. 306 Yogana + Much 'sided from forms Dalmarella fertils. Normans richly from Muzzas longus with sides with the frosted forms by named Oakes. Larger Endrias 4 in wide. Siphuncle 1/2 in wide. Chambers: 10 in 3 inches. Siphuncle 1 miles half enter shell and the septa turn up there = Cirumma. Bathingmmo? Dormicles apparently. We less m head collected for pits, 307 Repetition of organ a section about 5 1/2 ft thick, normal in 4 richly fruits per zone at base of tribuna full of Dal- ananella fertiles. The top of the underlying rock is hardly will together with Dalmanella fertiles. Of this I was making the trip 13 feet or so exposed. The typical Candonille led veins at 308 after a long stretch along the northward lateral at least 6 ft bringing the top of its Candonille 19 or 20 feet below. The base of the typical Organa as well as I can make out! 308 Candonille. 8ft exposed line, orith? near top with deep burging size Vermicaria unknown part of the locality.

309. Fossiliferous Cardenville under land by about 5 ft of well bedded, sandy looking lime- stone with few fossils, and 5 ft more massive bedded limestone cut at base at 310. 310. Chert at foot of Cardenville - 4 inches thick, 311. Cardenville slates with Ostrus, Dinotella and Dinithus? looking up, I mean these card crowns as the Ostrus, 312. Cardenville base, White clay about 2 fts. + ft of high Bridge, 313. Cardsville bed. 314. Highest point in road - ends ville. Since then below the 850 mark, took up cut on line with lens, 315 High Bridge. 316 Cardenville. Ostrus, Pleurothrin Dinithus, Rhynchothrina scaring Ostrea, Dalmanella, 317 Gorgona in place. 30 ft: 2 verticals, a little fossiliferous Cardenville 15 ft intercal, calced! 7 ft intercal High Bridge. Pras oxera falsi views with plenty of Dalma cella directly over the Gorgona South of 317 there is a rather strong Northward dip where a south ward dip was expected. 318. Mostly Osuna Vista is a strong eastward dip where a westward dip was expected, 319- Cardenville chert abundant at about 90 ft as far as can be determined from the cut on line 6th, below the top of the hill west of the pond. This would give 884 ft for the Cardville clust. 320. Wilmore bed with probably the Cardenville bed beneath. The latter not well exposed, 321. Top of High Bridge with probably its Cardsville occupying 6 ft below road level - front of dam, the home level is a little less than 900, probably 880, and the top of the High Bridge maybe about 870. All of that is crossing from cut on line. 322. Rednose quartz an interesting. Stephania maxima f. t. 4 to 1 (807- <Stephanoceras small normal> (809-835) Ophiceras Dalmanella? species? Ostracods populating, many fossils -809 -815 separated in chert m with nuth at 821: ? Dinithus with a scattered bunches of cells. Not certainly determined in Ost adium, at 833 -833 = High Bridge. 865 ft in SGS accurate at highest level entering at the road corner with High Bridge still exposed

323 Columnaria in 2"m about 6 ft below the right front of new horizon, there for about 800 ft NS GS, a coneate. This is the first Rocky Columnaria in the High Bridge. The Fly mark below brings home at a distance. If it is represented by three layered layers of L, without pearls. 324, Chart layer at top of High Bridge, 5 ft below road between two lines, and 70 ft below tip of hill towards south. 9/12 + 17 = 929 - 70 = 860 ft in a coneate height of tip of High Bridge. 325 Chart layer at top of High Bridge from house along road to where road turns directly next, ford about 850 finding from center lines. 326, Chart layer at tip of High Bridge about 860 finding from center lines. 16A - Bathymora agreement in Kentucky quarable area, a plate marked them faded, but not measured. 327. Tip of Buckhorn Kentucky mouth ford at 719 ft US GS, a coneate with Bayprong to be same ford as at 16A West of Winncells part of Dry river, and Dannelle fork. 328. Numerous large limestone rocks for last half mile. Also half mile NNE of Winncells, where I forgot to record them. 329. Tip of High Bridge, or at least center line below house level before going Down east road to Reservoir at Dannelle reservoir 16 ft down. To low for water supply of Dannelle. Blasted ditches to 2 ft water holes in success in my area to keep up water supply recently, and therefore next week will be in new dam for trip to see if we are right. Water would hold back 3/4 mi., Go on next to passed dam or many springs have formed up from the dam and one or two where water only comes where than 1 ft above the dam. Some not high able to get into the place where this makes 22 cafes, from about that iron, only the Ladder below. 330 High Bridge forl. with steep dips southward, which does not climb up quite to the valley south with forks like a funnel time show no evidence here. 331. Tip of High Bridge 10 feet above the road there. 332. Top of High Bridge is part of lined, so then off about here with High Bridge in North & Seventy m south. Apparently a strong and long spit road and dip along the road. Fork of somepart forms 152 9 ft distant with scuttleless scattered over the limestone. Limestone was done 9 ft distant, Winncells. Probably in front of fine lime ores here. 11 ft arg. lined me like drive entered rock but water holes on ground

5 ft interval, uncertain, Typical dove crinid lme 2 tme The preceding section is very firm or some agreement the limits of the extremes being uncertain. But it is certain that the strata formers regarded as not Amherst in reality are Archelm with [illegible] Moe over the Devonian An limestone comes in within 5 ft of the tip of the section as here described, if not directly at top. The large fragman crusted Amherst in former trips, comes in in the 11 yard limestone section at top of the Craigville, Lebanon, Ky 154 Near Sulphum Well, Lebanon. Tetradium 9m belw Devonian l. Columnaria racca 1-2 ft below D. l. Col. racca, 3, 2-2 ft below Devonian. Columnaria rather common between 1 and 2-2 ft below Dev. l. 6 in my ink with radial Beatrix common, like a carrot with frad end down. 159 Dan they hill S of Sulphum Well, Nodule layers. 9 ft from top = Amherst. Rhy. dent at a + Lejet also lme, 7 feet lower. This shows that from Magnenville Nichle was Amherst. here at least 159 most likely globular plat, but not fender. 2 ft width front, clay rich with 6 in mfrml forms, clay soft, soft. 32 in. Plat. fenderma. 24 in. rich modl + plat. fenderma. 30 inches fransiform l. Lejetman's place. 7ft. 2 ft strong, rich. Regular dove crinid l. Shake layer of Magnenville, 4 ft my ink. 1 ft Nodule layers and undulating front arch. Maynovale, 2 ft width from l. limestone this R> All preceding and 5-6 y Lebanon three major settlement. 333 Serge Luckett, about 2 mile of Lebanon - Bradfodville junc. Plat. fenderma abundant, as far as next water. 334. Base of Date layers, Devon l. 160. 49 ft Shelly from Magnenville. nodule in relation to the soft clay 16-2 ft internal, Lejetalma loose, just above argillaceous ark, softer, which whiles typical dove crinid l. The Devonian is first about the 49 ft of from Magnenville.

5 ft along bridge .2 + .8 depth, add +2 .6 when that is impracticable, = mean. subsurface. With wheel of meter just below water, multiply this by .9 = mean. meter can be placed below the weight. For mean velocity divide Total D discharge by Total Area. Use hand mark on bridge and move away from bridge. In case of freshets use 10 ft or 15 ft interval to get across section quick. Find angle of water to bridge. Corrections must be made with bridge vertical, Rising or rising stage is greater than in falling stage. New York Standard Watch Co. Forbnscher. Locks. Wolf Cr. Culley Cr. Rosena Kindle, Straw and Bigtim Cubbery.

"Steph munea retusa Walsburg, Liberty to J Maynesville Ballot run to J Libby N of Lancaster and p.109. Libty Old Bm Cunden trip Whitevale Steph munea plamumina Walsburg, Liberty to J Maynesville Ballot run to J Libby N of Lancaster, Jul b. 109. L. f. Steph munea halli Lr 32. Middle Eden Lr 51 Middle Edn Steph. mayonilliana' Elder man Bondett kurb R. Lr 23 Lancaster, tip. Fairmont Lr 26. Primont & Lancaster. Fairm. Lr 34 b Lr 49. Fairmont Lr 50 ". Lr 69 Lr 70

♣ ♠ ♥ ♦ Grando, When jacks are trump 20 out of hands just picking up the skat 16 of taking up Skat 12 if turning is changed to grando. 12 11 10 9 Solo. 8 7 6 5 Turnney Nulla. 20 played out of hand 20 when taking up Skat but lose 40 Nulla quart played out of hand make 40 and lose 40 with skat. make 40 and lose 80 J - 2 A - 11 10 - 10 K - 4 Q - 3 9 8 One black J/10 12 14 16 Two blacks,. Denz 3 2 skat 4 3 The cards you discard count for you 5 game Schneider make 61 Schwarz make 91 - 1 extra make 120, - 2 extra If you announce Schneider before playing it you get 1 extra pt. Schwarz. 2 extra

L. L. Hardber, Arachidae, Ky. Strophomena zinnata pp. 79, 92. Bald Point ? ini? west of Glencl nr., 31 ft below Billers = 46 ft above St. mayrillensis Great base of Fairm cnt. Leptaena Maiday, Liberty nmltace Mayersville area top Bed B in Camden tri sec Whitewater bld Jrc 43, S y Lancaster Strophomena sulcata Wesburg, 9 ft above shale bed and 11 ftn Whittled bed in Saluda Bed B, in Camden tri p/Whitecnt. Strophomena planicurveta 1 3/4 mi NW of Verond h = 27 3/4 miles from Cincinnati, above. Bld. neglecta of Mt Hope? 11 ft above Allandale sta. Wlr, 101 yd west station. 13 ft above base of section at Clay Blanco nwst of Slendale, p. 91. Jrc 34. Lancasterly. Strophomena mayrillensis Euri E of Allandale Sta where road crosses B.R., associated with Pleidactites neglecta, Dolomites multiradiata Strophomella profundiorenlata = Mt Hope. Bald Point? ini? west of Strongton hp = 97 ft below top of Faison cnt in bed nr Billers base. = — at base of Faison cnt - 7 ft thick 65 ft from base of massive Stroph. mayrillensis; limestone to road 1 mile East of Lontyburg. Nrmalns Dolomellites and other rmmie dictals limestone. see Glencl nr., page 79. 4 amt in actinol, 2 m out of Bewtsonville, page 81. Lat Crrk 4 1/2 mi out. 55 to 66 ft below top of road, being limstone just of St mayrillensis 38 ft above abov str at Forter. Ky? see page 84. Dolman elle multiradiata common in middle bldw.

Oct 25. Billed, No. 913. 5 half times. East of Brazo field, limer; East of Brassfield, nearer; Brassfield L. Wj Paula Plum creeke, Der. Brassfield, Lexington, Ky. Treasure's check No 551 for $4.00 on the account of Jan 3rd. 1 zinc etching — $0.75 2 zinc etchings — $3.25 $ 4.00 Jan 5. — No. 2047. $17.00 3 H. Tmes. fossils 2 massive silurian fossils. plate brachiopods plate Favosites plate Lyellia ordinary. Oct 4 Billed, Sept 28— No. 618. $1.75 1 H.-Tme Vicw. Man standing by fence, Loulbergnd creeks. Sept 22 - No 538 $4.25 Sept 27 Billed 4 Half Times, views. Lexington pierceplain. Der. Wj Clay City. Orrine. Testle springs. Indian Field. Clinton.

Engs. What we owe. May 31 - $37.20 4 plates of fossils, Cin. Gr. June 30 - $220.10 17 plates of fossils Cin. Gr. (Sep 18 $ 1.25 book store) Sep 30 - $ 14.25 4 half times. See 538 here Oct 31 - 18.95 5 half times See 913 here. Nov. 29 - 10.66 Nov. 29 (Oct) 1.75 1 half time. see 618 here. Dec. 30 - 72.84 Jan 31 - 21.00 See No + 2047 here March 30 - 36. April 3. - 11.50 $4.00 = $17.00 [illegible] (Feb 20 cash, 1.25) Oct 25 $ 257.30 C.J.N. Nov. 3. $ 18.95 A.F.F. Dec. 2 $ 34.95 C.J.N. Dec 12. Engs, Cred. 4.00 = credit, Dec. 14 $ 14.00 mtenanc. Jan 19 $ 62.50 C.J.N. Jan 26 $ 4.00 C.J.N. Apr 20 $ 47.50 C.J.N. C.J.N. still owes $ 17.00. 71\frac{1}{2} Holmes at Burnside runs gasoline launch.

(Mo Ju (Su Sa 11 - 35 1 11 - 35 1 11 - 35 1 44. 11-40 2 37, 5½ 44 Amheim Mt Auburn 20 Caynville 60 Belleme 20 Fairmount 80 Mt Hope 50 11 - 29 11 - 35 20 11-30 25 My account to Mrs Thacher Dr Austin Dr Weller Prof Whitfield John Edward. Fre brother. A & Co. George Dan's 36-40 yrs

91-D by Ariel S[?][?]. F. C. Fales Danville, Ky. High Lord Til Co.< Chicago Veneer Co. Brown Ferguson 1/2 Serje D mss chinkes and brand Mac used Captr Massee Stormydrat offces Velieu to 27pp. & a range. a, c, Lane. other sheet 164 L. 165 L. followny 171. E. L. F. L. H. LR N J T Higam - LR. J W Dzaaco L J L S[?]re Borden L Xanning Read Brod? L 2ce 1-? Next h ay L presento LR 248 New Ephedra R 289 L 291 L R 292 L Lebranc old once, 152 L see 3-? S dythall 159 Z R 160 L