Field notes, eastern Kentucky, 1902

Eastern Ky 1902 Field

1902 Eastern Ky All copied. Eastern Kentucky. If found, send by mail to Drug. P. Foerste 1017 Grand Ave. Canton Ohio, 1426 K&T' 30

1) at Spring N of Mr. Willis Lawrence N of Oil Springs, Black Shale Brecciated limestone Massive 3 ft 9 in. Shaly rock 1 ft 3 in. Limestone Massive 3ft 4 in. Crumbling rock on the face tooth, The deeper unknown The Black shale is imbedded with lenticular masses of a sort of lime- stone rock for at least 8 ft from base They are boring a well NW of the house in the bottom of Lulbergard Creek. 2) Stworts Mill Between Oil Springs and Kiddville, about 2 mile across the ridge from Oil Springs. There is a fine exposure of Black shale - Coniferous juncture a few hundred yards up the Hollywood Spge

3) Carno Mill Black Shale, with interbedded clay, with near base, merging into the shale. Massive limestone 4½ feet Only refined 1 foot Massive limestone are 3½ ft. Fish teeth at very base of this limestone = 2 inch Blue clay shale 18½ ft 9 inches of solid limestone crossing the creek forming a little fall of 1 foot + 4) From Peel N. West of his house. & east side of brook on hill side, 600 feet N of road going west from Kid mill. At top of section are loose boulders with Whitfeldella large crinoid heads + large and small corals. 5½ feet partly exposed. Limestone only fairly exposed and base not certain. 7½ feet, 3 feet clay more, large & small as at end as turns top, Inner part of section nearer the road, 1 ft limestone ½ ft clay 7½ ft limestone Base of Clinton ?

5) Clintn with Halysites ctenulatus many Stepheloceras large & small, Lyellia antinlmutus. At top are several thin layers (= 1 foot?) with Whitfieldella? + Penn. Stocklandisina? Meanur thickness of oosgro clay is 38 ft but owing to slope of the rock it is probably at least 45 ft thick. B one of Devonian seen. Fish- tooth layer = about 8 inches, Wint Tooth & lower bed, Weathering not 8 inches. Marine bed (1/2 foot) 38 22 1/2 ft. drive Clinton thin s 15 1/2 ft. limestone layers. Not collected? 6 S. of J.T. Elphins along Rm. From Clinton base to top of marine continuous exposures 10 ft 6 in. 5 1/2 ft chiefly clay & some limestone, 2 inches larger limestone. 8 ft clay, soft. 4-6 in solid brown limestone 5-ft stuffy clay 2-4 inches brown limestone, 12 ft blue clay 1 ft solid brown limestone. The distinction of this layer unknown. 1 3/4 ft unknown. 3 3/4 ft. Cherty Criniforms. 3 ft Black shale base is a clay rock. Tirezille black shale above. Further south at lowest point of around the line of Clinton is clearly seen resting of clay shale, Clinton to layer with large oozoid beads = 14 1/2 feet. The layer in which the beads occur disintegrates readily as do also other layers above the middle. The lower 6 1/2 to 8 1/2 feet are more solid. The layer taken as base of Osgood is more solid, unsbedded 6 in. More limestone up to 2 feet. 6 ft blue shale mixed with small limestone and rubble. 6 inch limestone, about 33ft to top.

7.) W. of James Stonehame. 8 ft. whid Clinton. 2 ft. limestne claggy, weathring much. 3 ft. sandstone claggy, near top at least. Red just abt visible. 8 inches heavy red, massive crm bedded. Cosgrove face 85 ft. clay with some lime- stone layers especially near the face. Contact not seen, 6 ft north of crest in streaks & repduls in all parts, 5 ft brecciated layer. 80 ft from Red river to Clinton, 8, Road going East at St Johns Church 65 ft from face of Clinton m. to base of Criniferous. The 14 ft bmn (red) limestone occurs here as at 6 years tho north the chisty Criniferous. 4 ft Criniferous cherty. 3 ft brecciated layer. 9.) On road leading from 2 mi. S of Indian Fields. Clay layer soft. 22 in. limestne, Cosgrove? 8 in clay, 6 in whid limestone. 12 ft clay, 13 in. limest. several layers 22 ft covered. 14 ft whit limest., bmn. (37?) Total 15 ft from top of Derminus. Is this brown limestone one layer Derminus? 10, NE of Kidsville, In stream bed. The heavy crm-embedded layer is fully Strepelocrinus. 8 inches level and 9 thin limestne layers with large crinoid beaks. The (forgiven) bed is 3-4 feet (?) higher up. Thickness unknown. The Strepelocrinus bed has pin wave marks.

11. E of Kiddville near mouth N Fork. Feruginous bed = 1½ feet thick. Contains Streptaphyca sub. plana, about 1½ feet above Strephelasma layer. The feruginous layer is overlaid by 8 in class of limestone. This 5 feet consisting chiefly of thin rift clay with a few thin linsen, at one crosses, more frequent near top. These are overlain by 5½ feet of thin limestone with thin clay partings, thicken til never as to merge into the clay (5 feet) beneath. There thin limestone furnished the middle stone of more seemingly sections. At the top a one of these beds is about 4 inches thick + some contact. 12. About ¼ mi, N of level. Dig 18 feet in & steps East on West side of creek. Barny Christian well shown. Massive clinton 5 ft. Softer layers between 2 feet. Massive limestone ½ foot 6½ feet unknown. Very finegrained purple material mixed up in a finegrained limestone. This layer at a numerous of places contained large crinoid heads, identically well shown, also some stephelia, cross on plana and vegetations abundantly. Overlying this bed is a sandy layer with more lay crinoid beads, poorly shown, we found not exactly one inch across. Also Streptelasma 4½ in dig the clay. Above is thin clay and then the thin limestone seen in last section. This shows the formation of the (le) wood line? This part is exposed also on N side of creek, it occurs higher in the section than the dig towards West on other side of creek would warrant.

It is about 12 feet my to face of the limestone layers which are light lemon thin beddy the limest mes are 5½ feet thick. From line b to line J Devonian is 11 feet, Devonian top foot thick. According to dips the Devonian base should be 67 feet above line J Chintm. According to actual measurement it is only 37 feet above the line of Chintm. According to dips the top of the thin limestone is 29 feet down Devonian, according to actual measurement it is only 12 feet below. There is an east cliff on east side J creek but I do not know how rapid the dip is, n whether it is constant. The elevation of the thin lime stones suggests that the dip is not constant. 13. At cross roads 2½ mi. S of J of Levee. The bed which usually shows a nodular layer in southern Kentucky & allly Tennessee, here a continuous purple ph glathic bed, 1 foot to ½ feet thick. The base of the black shale is claygy rock, hard at road angle a quarter of a mile N. This basal clay rock is seen to be under laid by a little black shale. 14) Squeamore Creek. The clay hard rock in lower face of Black shale section is under coved by 5½ feet of black shale then by 4 inches hard rock then by 16 feet of Osgrowe bireault which is the red sandy rock with fine gravelly bed. The J an inch clay trimoid beads are very even- ner in bed of stream. This layer contains clay lumps all is irregularly wave marked. The overlying 12 ft. of red are equally red, a fine grained purple thin layer occurs just above.

15) West of Jeffersonville. Coniferous, 14 inches thick. The clayey rock near base of black shale section is seen farther up the road, 29 ft from face of Clint to Clinton in bed of creek. The red sandy massive layer is a foot or two feet above bed of creek. 12 feet above the creek is larger with large crinoid beads on ledge by sandy rock. This crinoidal layer is 17 feet below the base of Coniferous which corresponds with section 14. I may next from creek up to 39 ft from face of Clint, to bottom of creek. Averaging the two sections it is 33 ft. from face of creek to the base of Clinton. Since the east exposure is nearest the creek, it About 3 feet of Conif. partly exposed. 16) E side of Branch Creek Ed Comar. About 26 feet from base of Clint comes to what seems to be the base of the Clinton. Crinoid fossils exposed. 17) A little over 2 mi. SE of Mt Sterling. Blue clayey limestone, looks like a small lagoon. The cliff fossil. The 2 mile sink is exposed between here and Mt Sterling several times. 16) Continued. Clinton. Massive rock at base less than 5 feet thick. Not measured. 18) East of Slate Creek E of Spencer. Confirms. Massive layer at face 3 ft thick. Unknown = 14 inches 5 ft. full of clams. The lower massive bed is also short. 56 feet from base of Div to base of Clinton. Blue lagoon exposed just west of the Slate Creek Bridge. 19) West of State creek bridge Ed Spencer. Cardovician blue clay. 3 ft 10 in more than felded limestone. 19 in, blue clay 8 in, massive layer. 16 in, massive layer 3 ft thin limestone with the clay parting 8 in an abrasive bed 20 in thin felded limestone

11 2 ft. chiefly clay, rest well exposed. 10 in. thin limestone, 10 in. chiefly clay, 9 in. massive limestone, 6 in. clay, 5 in. massive limestone 2 ft 5 in. chiefly clay; 2 in. thin clazy limestone full of large crinoid heads 2 in. clay. 4 in. limestone, partly white needles a short distance further west - 20 ft to bridge. = 19 ft of Chint according to these measurements. The local Oxford layers from their source material in this district are always shaly and planar + Stri telazema. 82 ft. between base of Clinter & base of Conifers west f Slate Cuth. Crnp. at top 4 ft 3in. 1/4 in. like brecciated rock but without breccia 1½ ft. brecciated rock below, 1½ ft. fully chert, almost all chert at least 5 feet of rock with chert + with clazy chalk. 82 20 4 61 8 15 20) Enroad leading to Heward's Mill ½ mi. W of Spencer, Blue clay rock, Ordovician. Good section f about 40 feet. Claygy matrix. 3 ft. local massive Richmond Shry. telazema. Within bipinata large large crinoid stems. 2ft 6 in. thickest nos layers 2 in thick with clay partings about 4 in. thick. 11 in. lower half of same. Upper clay clay rich with byzovana to, per 5 ft. 6 in. chiefly clay with a few thin limestone layers 1 in. thick. The limestone is a very small part f this section. 6 inches several thin node layers with Rhynchotella cafaux. Cortus or indeters & subgrydae Orthis bipinata lower S.2. Simple mena Rafineszonia simple mena, jplanumbrana small from wt 5 mil Ordred ventral area + strong brian along an turn + lateral edge. 1½ ft. limest. Rafineszonia. Very good Strph! planumbrana 28 ft clay at top limestone with Rafineszonia, Simple sulcata 20 ft to base of Clint m. clay.

The Strophelœna in the massive limestone is large + rather com- mon & defines into Richmond age. The rock below the massive layer for about 6 ft. is consolidated clay and corresponding to the beds bar layer, The 33 feet of fine Warren lens just beneath the equivalent of the nodular layer are nearly un- iform forms, almost entirely clay. The Orbitis layers in the road to West Sterling probably be- ing in its Not. Carbon set. Strophœna Mionobridalis in same bed with other fossils 12 feet above base of Richmond and as like de- termined. Present trip: Friday night West Sterling, Thurs. .. Indian Fields Wednes ... Winchester, Saturday Dodder's Lickman Sunday Delaware, eight. Monday Clarksville night, Tuesday ..... home. Friday to Friday 4½ 2 weeks 21) ½ mi. S.W. of Harward's Mill, 0 creek level 11 feet not exposed, 6 in fine grained dol. limestone, 12 ft. fine grained limest. with clay fossils; 7 ft. clay with nut fossils. 7-½ ft. Clay rubble with Spherical + hemispherical hyzozoma petin- foliata, 25 ½ ft to base of Richmond. = 53 ft J Walker had exposed & the Not Carbon beds not seen. 22) ½ mi. S.W. of Harward's Mill, 0. Rather uniform forms sandy clay barn rock weathering to sandy clay 23 feet clay limestone weathering or as to leave out many fossils, tho kind of them better lying large with several Strophœna crenulata dentis seen the base !!! Neterogyrpina 6½ feet limestone, clayey with piece tically no fossils. 40 ft. layers practically no fossils except the petinæ determin up to base of Richmond.

Making allowance for dip the Pit chalk bed = Warren = 50 feet about ? not Arthur = 24 feet about. Sandv clay ~ 14 feet ? not Arthur = 50 feet with plenty of typical Arthurs lynx, hare of lynx beds not exposed At Warren Arthurs lynx recorded in lower part of Warren bed some distance above the base, 23) 2 mi. east & county line m road to Chertm. Ordovician blue clay. Base chalk limestone, 3 ft 7 in. 6 in, blue clay. (The local led with chalk) 12 ft solid with smaller ornoid beds. 4 in. blue clay. 3 ft irregular bedded limestone with intercalated clay sedents by washed out, 7 m. an assive l.. 2 ft. more l, some smalls ornoid beads, Wane marked layer with large crinoid heads seems in some blocks 5 ft higher up. at 93 ft above base of Chertm 19 the chalk is about out = Dec. 24. a short distance east. 9 ft 3 ins chiefly limestone, from base of Chertm up ending at the white orpid layer 11 feet thick 3 ft chiefly clay. strongly mare marked layer varying much in the cleanness from 6 to 15 inches, 12 feet clay. 2 in limestone full of large crinoid heads. 12 ft strongly ferruginous rock some red and purple. One Whitefieldella vary in tips 51/2 ft of clay, white. 51/2 ft of thin firm limestone 3 ft of thin limestone weathering to rubble. Plenty of white clay = 60 ft to by of dirty Dernian of which 2 ft are exposed. 9.3 /7 / 76

25) E of Lemonsville. Massive Chert with chert 4ft 9in Clayey thinbed Limestone weathering to clay 5 in. Three beds of limestone together equal - 8 inches. The face of the Richmond is 70 feet farther down the road, Its real thickness is 62 feet; Dip makes it appear thicker. Two specimens of Strophomena planaulma were found near the lower part of this sandy clay, 11 feet below the face of the Richmond and, in the limestone just beneath small good specimens of St. planumula and good Strop. Leptrena c deliculum are seen. The upper part of this thin shiny section beneath contains several species of gastropods, Obirandna, 24 to 23½ ft thick. The limestone section extends beneath and 11 feet lower than the 2½ ft section occurs 94½ trace in large. This is 94½ ft beneath the Chert. Not also reduced = 23½ ft below what was first called the Richmond bed. 1028 ft clayey stuff ruffy near bone No fossils and no calc. 140ft 28 feet clagy lime weathering to rubble upper half with plenty of foo, 2s's & a few Oithni hyprata not large enough for Lyres. 28+8 + 23½ = 59½ feet and no Oithis lyrux, typical & common. A short distance beneath let down far not been seen than limestone beds full of longycom some Oithni hyprata not large & Leptrena c deliculum. 26) East of West branch of Will Creek. Good clay at least 60 feet thick. The many large fossils just beneath at such level but not seen. Fish teeth layers about 3 in. thick as far as seen. Chert conforming about 5½ ft. Binnish layer with traces of speciatum = 2½ ft. Black shale. 27) E side of Blue Bank Creek. 1½ ft from limestone fully Amby. cockia umbonata. Middle & 15 in reddish limestone, massive and overlaid by 1ft cherty lime & ml.

28) At Rose Run Mining Co. Boring in several layers: full large crinoids 4 in. blue clay + 5 in. thin limestone 3 ft. ferns in some Clinton = etc. 1 ft. bluish slate including many layers. 7 1/2 ft. 2 ft shaly clay. 5 ft. thin (1/2-3 in.) layers of lime stone with 4-6 in. layers of clay between. The top layer is in places 8 in. thick. Do this ? up: the Huntfieldella bed? 29) Roran Cr. NW 1 Morris Ferry. Devonian limestone 13 in. of a grey color with some play or matter within on upper surface. Nothing else exposed). On further examining in, this Spindrift layer appears to occur in the lower part of the Black shale + the Clinton ferns is entirely absent. On the N side of the hill, North- ward, a similar rock appears. The lime surface is red, ferny-moss has a bluish-tinted appearance and may have had red tints in it, but this is uncertain. The fact that this then follows an irregular course of cause the first one to be on top. 30) Road to Farmville. Wavy Clinton layer (trending) waves NW 1/2 W, Northward up the hill the exposed shale section exceeds 70 feet. I forgot seen. 31) apparently its layers overlying the wavy Clinton layers. 32) Do wavy Clinton layer is seen here? trend NW 65 W. Thin limestone layers separated by greater thickness of 1-1/2 ft shaly clay etc. Like it did at Rose Run Mine. At least 5 feet seen here. 33) at Mill on Fox Creek Two miles below Farmville. 6 in. greenish clay, with brown under one. 1 1/2 ft clay 1/2 foot hard limestone. 1 ft 4 in clay 8 in. thin limestone 10 in. shelly wavy layers, 1 1/2 ft blue clay; 1 ft. limestone full large crinoids locus, not found here.

16 in ferruginous limestone, red ore, 4 in light brown limestone, 2 ft thin bedded limestone & clay. The clay much fer. dominating. Vanceburg. At each end of town the Wavely limestone rests on Black Shale & near it contains fine grained sand stone layers rather in abundance and differs in this respect from the thin soft clays of the Central Riv in dry wavely. The flags used for that joining are evidently Wavely flags and are fully Springfield like those found in Fleming Cnty and thus probably extend only referred to the base of the Black Shale. Just below the Court House on the river bank there is fine grained sand which may be the fine grained sand in some localities seen at the face of the Black Shale. It is at least 6 feet thick. Bare not exposed with a little high. If a fault crosses through here then the way to come then explanation for this rock. One mile west of town where the river comes a little stream the Black Shale is exposed down to creek level at least.

East side of Quick's Run. Quick's Run Blacksmith Shop 2 mi. up from Rome. A. 17 ft thin Redded, dark the dark many seams weathering is a sort of dark fine shale. B. Overlying it is more solid limer stone irregularly bedded 14 feet C Over this the limest one is more sandy in appearance = 40 feet to top of exposures. In A + B, small min'd beds and stems are associated with very small narrow stems ---- lay jointed, There is a spring below the level of the road at slope. West of Quick's Run the relation between this rock and The Black Shale may be determined. About 1/2 mi. up river from Rome 24 feet of the massive rock are exposed. At the top it looks successed but does not clearly resemble the Perm- nian. It is overland by the Black shale series in the lower party while are several feet of greenish shiny clay. At angle of hill S W of Carr's Sta. 27. On west side of Road. Black shale, at least 30 feet seen, Sandy limestone 75 ft. measured, lagged whitish clay 100 ft. base not seen. Just E up river from Concord Ky, Artus [illegible] = B and am type. Artus [illegible]. 2 pl. at mos. Leptaena rhomboidalis, Streptelasma calycula the little disagreement well shown. found in loose pieces over Ordovician. This is the first exposure of Carbon crew along the RR going W from Vincenlng. Sat. night. Enyingville. Sunday m. Salt lick. Monday. Flemingsburg. Tuesday. Manchester Wednesday. Mayenville. Thursday. Flemingsburg Friday. Concord. Saturday. Mayenville Sunday. Mayville Monday.

34 Almy RR 12mi, N of Hillesden, 3 ft. Belfast bed. 5 ft 6 in. s/h massive chert with 10 mi. clay soft. 6 in. limestone 3 ft. partly exposed, partly chiefly the clay with a little limestone. 2 ft 2 in. chiefly light brown or thin limestone, fine grained, 4 in. the clay soft 6 in. s/h limestone. 4 ft 2 in. almost entirely clay, with limestone at 1 1/2 & 3 ft levels thin. 6 in. Wave marked layer 1 ft. the clay 4 in. Wave marked layer, the lime st are few some is through to the ridges remaining as lenses flat on bottom, 1 ft 7 in. three clay, 6 in. limestone we not fern ginn 1) 2 merch it wave marked in places, at least crossed did. 15 in. strongly fern ginnous dark. 2 in. lighter red purple limestone 2 in. brown tinged with red, this and the last layer homogen to light brown limestone ones clay 4 in clay 4 in light brown limestone thin, 9 in clay 2 mi limestone light brown 8 in clay 2 in. thin to layers 3 ft clay 1 in limestone, lenses. 10 in clay thin. 6 in. several limestone layers. 1 1/2 ft clay. 4 in. limestone 4 in. clay 1 ft. 7 mi.) limestone, a part is slightly fern ginnous 4 in clay 8 in limestone R Leptaea sh mutridalis Dorabella elegansula Prasjena Crambites small brygones fair. Certus s natro plicatius m fold The strongly wave marked layers cont and the large intertidal beds.

35) Road to Farmville. Both clay + sandy clay shales. White clay at least 11 feet. Belfast bed nearly 5 feet. Clintan massive 5 ft 8 in. clints. 36) Along creek west of Farmville. clint or face to. 37) S. of Cranes Creek on road to Plummers Mill, 80 ft of white Osgood clay above creek level. No limestone at base; thought to be Osgood much thicker. 35 ft steeper slope not exposed, Black Shale, large exposure. 38) Above road corner (Smith) 1 miles part of Plummers Landing on Stoketon Creek Road. Called the Big Sandy Ford. Black Slate, No evidence of limestone beneath. 39) SE end of Munse's Hill SE of school. Osgood thin clay. 3 ft crinoid massive limestone, 5th Dev, or Silurian. 5 1/2 ft hard exposed green clay at least at top. Clints in Black Shale. 40) A short distance (1/4 mi) S of Ramseys Chapel. Osgood thin clay. Silurian or Dev rock crin, 6 ft 6 in. Greenish shale 5 1/2 ft. Black shale large section. 41) West of W. A. Lewman's house or spring. 1 1/4 mi S of Fox Sp. Osgood clay shale. 1 ft 10 in solid limestone. 4 ft 3 in rotten cavernous lime at me. 42. 3/4 mi. S of Fox Spring, 9 ft of Silurian Dev limestone. At F Lewman Wallingford he took me over bridge.

Fossils in Middle Richmond, Concord, Physicthrema capax. Nebrtella insculpta. Plectanmites sericea. Strophomena plumulata. Dinutilus antiquedact. Palasphyllus divaricans. Leptaena st. m. ridalis. Portora retusa, Columnaria dimunifera Stephelasma orminclum Hebetella sinuata Strophomena annulata Platystia falc. antilibrata typus Will E. H. Curran, 28 3 in 16 ft. Dalmarella ingra 2-1/2 ft. Stephelasma muticum 5 ft. 1 ft. Stroph. nutans? 5-1/2 ft. Stroph. austriann 58 ft. 15 3 11- 16-9 Lower exp. at RR bridge E of Concord. 11-1/2 ft. klmw O Dmr. Caseyi + Stroph. muticum. 6 ft. klmw Ost., mutans zone: 1-1/2 ft. (33) 5 ft. klmw O Sh. mutans small, No Dalm. Scolumnaria in lower strata. 0 Creek Stephelasma mut cum of or um. Caseyi. 2-1/2 ft. lowest Dalmarella alt ingra a, Dalm. 3 ft 10 in., Dalmaralla ut ingra almea 13 ft 5 in. base of limestone larger with lowest Physicthrema capax, Strophomena plumulata, Dalmarella ut ingra recurv at various levels up to this point. above 18 ft. 7 in. Stropheplumulata + Dalmarella ut ingra cumina up to this level, at this level the limestones are separated by some clay become recent clay; themselves to a certain extent fossils, 20) 21 ft 3 in Clay limestone with abundant Stephomena retusa. 27 ft 7 in. Chiffy clay, few fossils. 28 ft heavy klmw with Leptaena sternoidalis but this is from down down. 20ft 33 ft 6 in Stroph. plumulata in thin clay. 39 ft Hebetella insculpta loose. 47 ft Nebrtella insculpta, lowest exp. mine at my RR corner, just above Portora retusa + Cystoceras. Columnaria.

49 ft 2 in. highest I debertella inculta. 60 ft. Fossils m sec and page preceding found in 11 feet below this level. 153 ft to base of massive cherty clinton. (2 3/4 massive) 46 ft from J clinton to [illegible] clay layer above clinton & below lower limestone. 190 ft. top of ridge with jolenty of massive brown rock boulders, with white clay slint distance beneath. 53 feet at top of ledmician op- pacment & along with out C'lum. It me to any extent & with- out easily found fossils. The extreme form of limestone facing but seems to indi- cate the above, Petraldium 8 in high loose joint above lowest limest me about 5 1/2 ft above I debertella inculta zone. Columnarform 5 1/2 in. across 5 ft above I debertella inculta zone + great ledm said limestone as described above. 35 Mayenville. About 2 1/2 miles S of town along C+O R.R. Stepharena plana - cross-a- section = 104 ft. above level of R R track where first seen, 1 mile from town, at track level 2 1/2 miles from town. 7 in limestone coarsely fossiliferous lemn-bryozoms, - thin band above. 3 ft 8 in. cluffy shaly clay with 1 or 2 of one inch lenticled clay arch at top. 10 in. limestone hard crupfered chiefly of Dalmanella multisecta. Waved on top. red Dalmanella 10 in shaly clay. 6 in hard limestone fossiliferous 5 ft 3 in shaly clay. 5 in. Two thin bands of [illegible] limestone. 2ft. Shaly clay 6 in. fresh limestone Cephalas & few Dalan. multisecta on top. This pool occurs at intermediate levels. 5 ft 10 in. chiefly shaly clay. 8 in solid fers. cl. 5 in shaly clay. 6 in arid fossil cl. Dalmanmultisecta

8 in. shaly clay. 2 in. limestone. 2 ft 10 in. clay shale 4 in. fossil limest 4 in. clay shale 2 in. fossil limestone 8 in. clay shale 4 in. thinly bedded limestone, clay 3 in. clay shale, 5 ft. l. full of shells, plane-convex. 8 in. chiefly clay shale with 1 in. banding l. with strips plane- convexa in middle. 4 in. limestone with plane- convex. 5 in. clay shale, 2 in. limestone. 3 in. clay shale, 1 in. limestone no 7 in. clay shale 4 in. l. fossil ferns, 6 in. clay shale 4 in. l. 3 in. shaly clay 5 in. fossil l. 5 in. clay 3 in. fossil l. 6 in. clay, 1 in. clayey limestone no 37. 1 ft 9 in. chiefly clay 8 in. fossil l. 4 in. clay 4 in. thinly bedded l. 3 in. fossil l. 2 in. clay 1 ft 7 in. limestone, with strips plane- convexa. (total) 15 ft 8 in. 1 ft this clay 1 ft 4 in. fossil l.

Students Collection, Concord, Ry. Dimorthus subquadrata. 10 feet above Hebertella inesculpta zone and in lime material brought down from above. along RR. C. Phlyochotrema capax. Begins where Dalmanella becomes common along Sycamore creek, R, be- comes common in Dimorthus subquadrata zone C Hebertella inesculpta rather C in several layers in a (horizon) zone 1 foot thick at level of RR track C, Protarea vetusta. Several well pre- served specimens in Dimorthus subquadrata zone. Plectambrites cericea. Very abundant in Dimorthus subqua: drata zone. Stephanona serrata. Common at a measured level above Dal- manella zone, Sparingly in Dimorthus subquadrata zone. 39 Waynesville Limer half. Concord. Ry, Prasopora unipitalis. Ceramypnella granulosa Bythospa arcki Nildanmella tenua Patrima varians Callpora submodra Mistrorpella quadrata Amplexana spatalva Perlipera decipiens

Arthur M. Miller. July 29, 1901. Estill Springs, Splendid exposures of whole series from Clinton to Black shale in immediate vicinity of Spring, and extending up Station Camp Creek to south of Kentucky River. Hand level section on road leading up White Oak Creek from the forks of the road at the branch. (See Beattyville Topographic Sheet, U.S.G.S.) 655 feet above tide to 780 feet. a little farther down stream a few layers containing Cycloneria bilix(?) are considered Upper Cincinnati. =1 mile North of Irvine & then up creek. Black shale 18 ft. Massive cherty Cornij. lined 58 ft Whitish shale with celeste crystals, Osgrod. With this limestone plates at 32, 25 and 22 feet above base, ac- cording to drawing. Exact elevation must not be taken too exactly from this since it was on a scale of 1 space for 5 feet. Bryozoa layers occur & to 10 feet above base, 3 feet layer with prominent radiate structures - crinofort like, 1 foot thick, above 2 ft layer, persistent, & reddish limestone. 24 feet of whitish shale, Osgrod, with thin reddish limestone containing ? algaeite + Ferro- sites, 22 feet above base. Red- ddish limestone interbedded with whitish shale occurs in lower 8 feet. 22 ft. Covered, {?} Reddish magnesian lime- stone with chert & button = Clinton.

North Pine on Queen Crescent in Whitley Cr. Black shale, approx. 100° White Niagara shale, 30° Clinton in same dir., 100° shales. Clinton, light Blue limestones. Red Clinton in same in SW 7 Cumberland Cr near Maurice Cr. line 47 18½ =166 ft almost strph. planicurvata comm. road crossing 20ft rather sandy rather sandy lyxus very common. rather clayey, layers beds. modesta also - lyrx beds. modesta common. layer Parcellus modeta 103½ lyrph beds. wartzone undatme few fossils carvated cmt ated undat me fossils few strph. planicurvata common. 21 strph. planicurvata rather rare

North Pine on Queen Crescent in Whitley Cr. Black Shale, approx. 108° White Niagara shale at 30 clinton limestone. 108° Shales. Clinton. Blue Limestone. Red Clinton iron ore in SW of Cumberland Cr near Main Cr. line. 47 =166ft almost straph. planic. convexa comm. road crossing rather sandy 196 2 andy 35 ft {20ft rather sandy 15 rather sandy common. 166½ rather clayey 19½ {19½ rather clayey. lower beds. 150 modesta 42½ 14 modesta rare. lyrx bds. 132 especially 12½ modosta common, ear middle 2ft clay Parcellus modesta 103½ 13½ lyrx bds. modestus 3½ 3⅓ undist zone 90 51ft 17½ undist few fossils 86 few 8½ calcated fossils 21 calcated 18½ undist few fossils few 18½ straph. planic convexa common 21 straph. planic convexa rather rare

Salt Lick, Vanceburg. 3 Blankenship str. 7 Valley, PO, 3 zone. foll. 4 creeks. SE lnk. above valley, +3 Hacksmith, str. +3½ Hazeltin PO. +5 Glemment fols, lnk th (+5¼ Glen Sprng) m stn (+6¼ Escalapria Springe) Kinnery, str 1 49 B water ville gm's canal. Nashville 12 min path. 3½ lnk. no. 10 am Re at mile - 4 am. Blgd Slate Honey Sprngs Glemment 1½ Hazelt in Hacksmith ½ 3 Breedkin sprg. Glenn spgr. 5 off. Ritzlann Poplar Farm. 4 Valley 3 Blankenship Vanceburg

Left S 14 W, 65 S 24 W 35 S 24 W 60 Rad. turns of L. S 70 W 76 bridge N 72 W 75 N 35 W 40 N 47 W 34 Black Slate m. W 25 creek m. R. N 8 W 50 simply corners a R Bl. dle m L, N 19 W 2.0 N 78 W 31 S 60 W 30 21 S 48 W 100 S 28 W 15 S 2 W 30 S 45 W 10 bridge stream -> m stream L, S 45 W 55 stream bed S 52 W 70 S 78 W 50 Burnt culvert Church S 85 W 32 S 85 W 50 Clarkesburg N 86 W 6 cross roads) School L, N 86 W 84 Church & Christian A N 96 W 46 Mollie Calvat RB Store L, N 86 W 33 30 oak hem lock N 86 W 15 County Rd m R, N 86 W 31 Greenfield, m R N 86 W 11 N 32 W 27 Warply? C N 60 W 30 S 80 W 50 Warply b S 80 W 50 Warply! D S 85 W, 27 Jess Hamlin, 51 S 85 W 175 rad & corner R S 85 W 35 Warply, N 85 W 60 Rad to Green River R N 85 W 15 Creek m L W 25 Fine Valley a R S 78 W, 23 Wood culvert. S 78 W 85 S 88 W 35 Wine S 38 W 3 wood culvert Fork bridge S 38 W 30 Road R School sw Fine Valley, S 38 W 50 S 45 W 190 Church R Road L. S 54 W 60 to Forks of Fine Valley. S 54 W 20 S 70 W Valley, S 10 E 32 Bridge S 10 E 24 Church Rond L. S 10 E 20 Small bridge, Warply a R to Gladin gait, Left end, from last. S 54 E 60 S 70 E 29 S 30 E 47 S 40 E 39 Lapla Vermilion S 48 E 45 S 52 E 20 White clay Bot. district S 8 E 15 Richard D Beach JI, S 20 E 24 Curtis Carrington S 15 W 13 Bl, St in bed John S 10 W 37 Bl st, nobody m

S SSW 13 S 15W 40 S 22W 50 light the sides S 65W 40 S 35W 36 S 40W 28 S 10W 26 free tae, S 5W 18 freest an S 10 E 33 S 15 top of ridge. S 12 lane on R S 32 E 10. Boone Harris's {5 mi to Kinney Pike {2 mi to Valley. 27/2 A. Christian church W of Charles, brgs Holyrite genuine, smell in fine weddle. 13 ft of Lower Helderby expndd on H.T. Goose Jr. farm, 4 ft partly expnd below that 20th. B. Millie Calvert, 11 ft of Lura Held, expndd North of house at spring - And still further north is Black Slate above level of Lower Helderby. C. W of Black Slaternity, The massive Low Helderby is underlain by a yellowish clay clay pretty stratified forming a sort of clay sink. D. E of Jess A Gumbsins. Coarse limestone 29 ft ex- pndd, firm, hinged with red. Long stretch above with broken rock but no Black Slate. This is far above level of B. Can this be above Black Slate? Further study, climbing up hill N proves this is heavily

cfy. Laph Vermillion 50 ft nor tx exposures. 50ft slate, blackish in places purplish. 71ft clay + thin layers of slate, 16 ft rock, well stratified above. orin'd at but sandy looking + nr's & once. Will stratify at all levels + a sandy looking gray whine. 88 ft Clay, white + purplish deferate w d McCaldining at Valley, jmet to le Bgsrd directly below rock again. left to the lmost layer in Laph Vermillion section. Othel unknown. It seems to that this section is injured and tht ther is a fault line. The black slate section is altogether too small and I can not get a clear section line. The liknest we seen at Clin 'tim Church's altars& ment. Valley S 54 W 20 McCaldining S 70 W 6 21tc S 70 W 34 farml/grand S 85- w 50 Bgsrd clay bigection N 78 W 93 fine lgs. cl. sectin N 70 W 62 Alfred Hoffman, N 80 W 92 Fine lgs cl, sectin N 70 W 90 lgs. cl. N58 W 59 Bgsrd. N170 W 39 Bgsrd. N45 W 40 Stream road m R N65 W 98 Bgsrd m R, N46 W 10 old slate N 46 W 34 school Liberty co N 46 W 17 Church Grove IV 46 W 70 fine bag + lower held more than 100 ft bgz. N46W 30 N50 W 71 wood central, Cgg N 65 W 35 main valley. 2½ mth to creek's Run 7 mither to Elvis N 68 W 76 road m right, N 80 W 10 S 60 W 18 NED Dzuglume S 50 W 34 section Dzuglume S 80 W 23 Ironfeld Black) S 56 W 17 Y.M. Dzugm L S 58 W 10 Road to Indian Flats S 58 W 6 Sam. Aids S 45W/18 Csg. Op. s 5 W 2.0 s 10 E 13 s 30W/13 55

Alfred Huffman. We will lack of limerize, Black slate said to be faulted. [illegible] will. 18 ft sandy rock well stratified. 1ft very crinoidal and fossils. 110 ft Bedford clay bottom of valley, This would be a good place to get fossils from Lime Heldenberg, I must see. The Ostracods seen at McCle- downey occur here also. They occur in this shale (limestone?) lie boreled now to occur in Bedford clay or maybe sand, at least within 30 ft of top. The crinoidal limestones fowards by cut mine Limerica? B after single fault. tone erthed. section NE of Duncan house 11ft similar to below. 16'2 brown sandy, flat, rock massive 160 feet Bedford clay, bare not seen 57 lesg. S 5E 20' S 18 W 65' beyond, same ostracods S 5W 70 les. S 50 W 50 les, S 75 W 120. Gz. Bartley Harrison, Rad. S 75 W 7 At creek one 27 m of l. in thin beds dipping E. Is this 2ft bed massive? How the beds are thin. W 44 les. N 8E W 46 S 5E W 24 bridge. model, beyond S 58 W 15. W.H. Lawrence store, 2'2 mi to Odellton. Rilelt S 55 W 7 Cross Roads same girdage lesg. mule S 55 W 165 les. Micahund S 75 W 40 Parnis crop V 8E W 45 N 8E W 17 Chisty Cl. S 55 W 24 Hebertella S 55 W 29 bridge, creek occurrences 70 W 48 lesg. Chisty Cl. S 18 W 35 cabin S 38 W (5 simpson at S 26 W 25 springdale S 66 W 38 family farm yard S 66 W 50 S 88 W 136 N 8E W 35 S 8E W 120 S 8E W 45 church Bogdham N 75 W 66

WS Lawrence et al. Coming to chip 150 ft & perhaps 160 ft beyond clay. Which thin in m shall be studied at various levels, 3ft brownish limed me. 3ft white clay, 1/2 ft limestone. 8 inches clay C 6 inches l, stringy, wave marked, 4ft clay with a little thin lime stone 1 inch thick, several layers. Beysserans in them thin beds as well as in C. 8 inches, limestone. Don Road NE, about 50 feet m of stree. Rock dips SE following meas- urements for thickness at top. C 6ft 9 in to top of fairly solid layer 4ft clay. C 6 in wavy layers. 5ft chiefly clay, 17ft clay with thin beds one 1/2 foot about 4in white. 4in unknown very cherty limestone. [illegible] 59 C Phylloporeina expansa Ostracodplua Daylucensis. Spirulina shumwaldiis. Rhinospora frandrea, Cysth. felyllium, calceola, Platyspithus with 2 + with many plications m/fold. calyomenia inapalense Deltanella elephantula A fair collection of infragans could be made here. 100 yds West of M & Church 100 yds east of Sam Cooper limestone. 34 ft to top of some fragment 7 1/2 ft cherty Chert in. Kni 5 1/2 foot first cherty. [illegible] 2an W bridge agt

road west N 60 W 12 Perkins me NW 60 W 18 Folsboro, Between Calvin Creek and this place the road appears to turn about on the level with the top heavy lime stone of the bedrock e. series just below the road Orchard shale paper N58W46RroadR, Church NW N72W40 N82W30 Old bridge S 86 W 50 Road 1. S 86 W 37 S 72 W 65 meq paper N 75 W 29 Road R N 75 W 60 N 65 W 148 school h N 82 W 86 N. 82 W 60 S 88 W 22 Road crossing S 88 W 17 S 75 W 36 N 66 W 20 mail carrier Jno Kirkland N 66 W 100 line N 85 W 49 Mason county N 85 W 4 Road R Lewis Co. 1/2 mi. E of Mason Co. along road. corner of Chet Clinton, widm Ruth Cole, 17ft clay, some of it purple. 4 1/2 ft thin sandy loam much meq sandy clay, byzraus abou dant. 17 1/2 ft clay few fossils. Upper half y section whitish with thin clay clay rock. 9 1/2 ft sandy clay byrzoans about dant 48 1/2 47 ft limestone layers common, will Rhynechtrema capax at top Strigotelaema nectricum at top Helvertella insculpta at top. 95ft Below Oscar Worrick At old school house Brown Run School 190ft from Clinton down to layers with Leptaena crenul ridalis, comm. Rhynechtrema dentatum This means 95 feet below Helvertella insculpta layer, and 40 feet below Strigla. C mecodcuss zone and 35 ft below lowest Stratelaema at Cornrd. Suppose I turn this section should occur at about this zone. NW William King's house.

The contuted beds of the arnnd at one series above the sliph. I can't cover zone alon of well at the creeks. I mi' and 1½ miles west of the Lem's Cr line in the Cabin creek brad. The first creek leads up to Rockerville. The second creek is followed by the Mays ville forks. The contuted layer shows up well also on east side of RR bridge east of Springsdale a considerable distance above the railroad. Put's mouth, Pluto 6,7,8. Maraly clay for paning bricks. Peables Cr. 3 mi. E of Putem mt center. Visited Adams fire brick Cr Peables paning brick 3 mi E of Putem mths. 432½ 20 ft the fly SS. weathering friable, 412¼ 22 ft pretty exposed, 390¾ 7½ ft middle of 16 inch coal pool. 383 5 ft No 2 clay softer than No 1 white clay. 78-378 Base of No 2 clay. This is soft **374 ft pretty exposed since 330 330 Rather 2½'d freestone for 5 ft. [slant rather] hard 308 Mine freestone sets in. Below not 275 Top continues first one layer 160 Base of freestone layers 50 top of paning brick clay 0 core of paning brick clay Peables source of clay,

Copied 1916 From RR bridge By Springfield 550 W to top of hill on south side of strike. 33 1/2 297 1/2 33 108 1/2 path at edge of woods up to Wehritella mine, next layer, are perforated with Leptaene mineral nodules, that am limits layer runs above, in abun- dance. 118 ft from surface path at edge of woods to road at base of word. O. total from Wehritella mine cleft a down 226 1/2 ft. 25 ft from road down to walnut tree at which wide fence angles. Total = 25 1/2 ft down. 48 1/2 ft down to top of RR bridge. Total = 300 ft 17 1/2 ft down to house O. Hole = 317 1/2 ft down. (Roof of house = 297 1/2 ft down, house at cliff end) Copied 1906. 65 13 ft down to top of red roof of station building: total of 330 1/2 ft. At RR bridge Strph. plani- curvesa with characteristic gyrogam forma extend, up to top of bridge, This is 15 ft below top of terrace at cliff. 57 ft above top of building at bridge is base of Gyrox beds, 38 1/2 ft above top of building at bridge is top of surface cont red layer. 66 ft above top of building at bridge is side Gyrox beds, with undulate line max 13 feet higher up. 55 ft top of cleft to present good lineaments, Top cont. ordered bed = 36 1/2 ft above top of building. Between 52 and 61 1/2 ft above building there is much massive limestone but few fossils. Between

Copied 1916 6 ½ and 6 5/8 ft above building lynx become common but lynx not very common above 66 ½ ft above building lynx is common at 80 ft above building orchestra is com. mm. Height of building is 15 ft. Top of R.R. bridge is 5 ½ ft above top of building 16 ½ ft from top of station to top of bridge, 24 ft from top of bridge to tree on bridge, 24 73 ½ ftm top of station to wal- ut at angle of wire fence, Iraine = 277 ½ 69 ½ 208 48. at least 256 to base of str. pl. common 138 ft from base of lynx to Rhys, dentatum bed, Copied 1916 Iberisella incultata at 332 ½ ft above tree R.R. bridge E d spiral date 17. (Stemmonia encadenizzone) -- 277 ½ (Colitis nea Nymphaidalis & Rh. dentatum) -- (237 ½) can path at top of woods 33 2/5 99 ½ 233 19 220 1.3 99 ½ 112 ½ 30V 332 277 55 277 ½ -24 253 ½ road at foot of woods -- 106 lynx common on -- 5 -- 99 ½ -- 94 ½ - 98 ½ from common lower good linelet, -- 88 -- (30) (21) nutnant angle wire fence -- 81 (85 - 94 ½ massive lime- tree common to 1 upper cuticle -- (69 ½ dead.) -- 45 ½ (29 ½) Top of house -- 33 at bridge. Top of bridge -- 24' above top of simple place with many bush of ferns? -- 18 ½ at bridge. top of station -- 7 ½ bridge top of house to top of station = 25 ½ ft

Coyled 1914 22 ft lime consolidated layer Down to ware nummulite Limestone. 4 ft pure nummulitic without Stiph. planicavexa Face of Maysville Junction connecting with Junction to S Springfield 11ft SW of Summit Coyled 1966/9 Hebertella insculpta where road turns from N 65 E to S slightly down hill at oak tree, with Lepidocena rhomboidalis to top of H. insculpta, Rhycthelasma capax Stiph. planimulbra + elongata, 12 1/2 ft, then C & clay, many fossils. 10 1/2 ft rubble lime, fragile rather crummy, Dalmanella jugosa 4 ft rubble. 1 ft limestone with Dalj. jugosa, + Stiph. planimulbra. 4 ft Down to Dalman. jugosa, C & clay. 3 ft Limestone + clay. Staphs may be emendements? 2 ft Gypsum Strigotelasoma custum. 8 1/2 ft chiefly limestone and clay. Hebertella sinuata is common. Lepidospira troch- d spira + involuta, 45 ydams. 5 1/2 ft chiefly clay rubble limestone, fully Hebertella sinuata and Parapersona lespitalis, resembles top of Warren bed in Ohio + Indiana but much more fossiliferous. Hebertella is quite overestimated Lepidospira trochena, 11 ft Chiefly rubble clay + few Hebertella + Parapersona. very little in upper half, Neorhizopogonla from Coney 62.

Copied 1916 2 ft down to top of old large tree stump at angle yard, 5 1/2 chiefly clay rock & some l. with few Rebutella ornata? Syndiospira Hardenti = mullly clay rock. 69'3down 17 6 ft. chiefly very limy but no weather ering shell. 11 9 ft joint exposed, several good limy layers. 84 1/2 2 2 ft down to top of dense blue caly limestone with large specimens lynx, 11 ft dense clay limestone, blue, dark. Gryphacera com- mom in some of the lime layers. Here are the 97 dense blue limestones above the lynx beds at Cottage Comm. section, above recently Red River in the Riel locality. Top of characteristic lynx clay limestone full of lynx 14 ft lynx beds, - ruggy limestone deposited {Rynchelmenon dendatum Lowe, 11 1/2 ft limestone, chiefly dense- quite unexpressive layers. I have not seen. Copied 1916 71 This must be the shaly mfs reptiform beds of the Harrows mill section, {Rebutella incalypta appears again East of at and timed line is still east of R.G. Har- mers {Rebutella miccalyptha occurs also first east y blue clay strad from Smart to Days mill jinnoits pike. East of Henry Eden, & of Days top of lynx beds, 82 1/2 ft mullly stone with lynx when could not examine it 15 ft pure shelly limestone, dense blue quite unexpressiforms 45 ft rubble stone with large trees preservet better than at any in more typical lynx beds 18 ft comparatively unexpressive Top layers with Straphismona planicurvata. 40'9-760

East of Wyoming. Residual chalk in chalk, 10ft whitch clay, 11ft brownish sandy clay, from sandy clay to, 16½ ft sand clay with much sandy clay - Middle Bid. 33ft s and clay limestone + [illegible] but the top might be included in cremum at top. This is sandy. Hebertella maculifera rather 97) 7 2 ft sandy clay limestones with 15 ft bp of ashin J & beds 2 ½ft (6 in L + Steph. jelgannum at top). 2 another thank you man C, head wear 5 ½ beginning of good exposures 18 ½ thank you man in road. 20 large oak or left, Hebertella leds, 17 ft chilly dense three clay limestone with few fossil lynx at base common. linestones with byrux abroad out Middle Riden and 73 Forbes four m. upon grant of Middle Ridimnd. Between 10-13 ft above fore Plectant nites is cmmum, after Byth. Jean gracilis at least very small di'ometa. Steph. vitrata very rare. About 3 ft above bare Steph. vitrata. Phlydrotrema capax hardly preserved. Base of Middle Ridenmd and Tje of Lower Ridenmnd [illegible] Resimaequina Stephanomum planum lona Calycoccia? Phlydrothrema capax stipitolaena, Part area vitrata, Hebertella maculifera. Plect. stipitola. The preceding forms are fairly common from bed down to the more calcareous limestone as 8 ft down. There was no Dinotites nitigradata found in the Middle Ridenmd, searched carefully. 18ft below top of Hebertella maculifera a single Dae manella jussana was found, Steph. veslata large at 26½ ft below top of Hebertella

insculpta layer, must have come from about the horizon excellent interior of ventral valve. Steph. ma planumtina also occurs here From 23 ft blm. the insculpta larger than Rhynchella similata is its chief fossil borer. 3y greater heads: excellent. 35 feet blm top of W. insculpta Stephennema delarumtina rare but loose, as far down as top of dense lime such 81 ft blm in top of H. insculpta bed. While this suggests Rich- mound age, the great thickness of the Lynn Rch mound in that case is against it. Collected Sargra 0-5 ft above this level = 81-76 ft blm W. insculpta 5 of Rhynch. dentatum from just above dense lime lay limestone. Also Septum ridiculus. This is probably identical with the Rhe. dentatum layer at the Browns Pond section in same part of Redcliffe about 2 mi, 1 mi E of Lynn co. line. The dense blue limestone con- tains very few fossils. The first specimens large enough to be and called lynx occur 14 1/2 ft blm top of massive blue dense limestone. 1 Rhynchostea dentatum appeared to occur (lose) near this point this part of section (14 ft down.) The top of lynx lowest ones are 14 ft below dense. These lynx bed layers appear to be very much decreasing down for 15 ft when exposure ends.

Secn 25 S of Owingsville, 2 ft B above layers? Chinta alms 24½ ft greenish white clay, 15 ft pinky limed mes occasional clay. 27½ ft sandy liminalo comm in sandy Ptychotema capax, Strepelasma Din. antiquata not rare. middle 3½ ft sandy rock and clay Din. antiquata low 1½ ft sandy limestone {Pleodanmites {Lapraena 13 ft chiefly clay {Chondrida, {Ambonychia minor, Syndesmia nodar, Stroph. Danumtma c num in a short distance above and below this. 11½ parts chiefly Nebristella 5 inches bed, 8 ft rubble clay rock, Nebristella at base. 2½ ft Hebertella rubble, ½ ft Nebristella line l. wth Pr. hospitalis, 11 ft Hebrstella + Pr. bontotula clay nubble. 10 ft rubble abundant clay nubble, but fossils rare. ½ ft heavy dense blue l. 5 ft Lomely clay. 10 ft not opened. Limestone fully the same high grace as the layers just above the clay rocks forming the first lynx beds, in Wyoming 25 sec 13 W. cherty clint m base 80 ft below top of. 77 On a former trip, Geptaea plum briddis appears to have been collected in the lowest limestone of this section. The line of this section does not appear to agree well with the lower line section east of Wyoming but the upper and Middle Richmond + upper part of the Inner Richmond are all right.

79 Loc. 24. clinton, clay strph. sulcata clay streph. planumlna clay & limestone, striphelasma calix with morspora clay layers l. Heraspiora, byss. Rhy. dentatum morspora staly. Rhy. calyx. Dim. only rudata strephs. 60 ft. to top of dirty Devonian. 3 ft thinner l. with some clay. 6 1/2 ft thin l interlceded wth clay. 5 1/2 ft clay 4 in very limestone. 4 in clay. - 1 ft cement, strong ferruginous, 2 1/2 ft clay, lime, 9 in very many limestone. large crinoid. 2 1/2 in clay. 1ft 2 in. irregular limestone. 10 in massive. 6 in clay 10 ft massive clinton old record 24 Loc. 60" white clay 3" Thim l. = trubble 6 1/2" Thin lrmml l. 5 1/2" White Clay 1 1/2" { Strong f. phus in mo, zoned red purple, Wing. One Whitfieldella. 2" limestone large crinoid teeth 1 1/2" clay 6"-15" strong name marked layers 3" chalky clay 90 3" limestone.

1/8- 3/4 mi E J [illegible] Mill clint clinton. 15 in. Belfast bed. 24 ft greenish clay, 27-2 1/2 sandy clay c, in 2andy clay. 5 1/2 ft massive candy limestone, sirex alazma strophomena which? strophmere plammutosa Heterella sirmata. 12 3/4 ft not exposed well, probably 2 andy clay, 17 ft blue clay rock craching irregularly, well expred, 5 1/2 ft 2 andy clay wih [illegible] praepera more very common, Praespera biofostably abundant in 6 1/2 feet 2 andy clay. [illegible] alazma. [illegible] abundance of Heterella residentialis here and in 2 layers slum 3 ft have the layrode, [illegible], lameilbandus Praespera. 4 1/2 ft bluish clay rock much liska up. Praespera canner, 8 in. blue limestone. 12 ft 9 in. rubble limestone compred largely of byzizan remains same as last [illegible] Heterella, Plarystrophca, 8/1 In the lower part lynx is found, 18 ft. date blue clay rock nearly impressed lifeless. 30 ft typical lynx beds, 24 ft down to creek. At [illegible] We'll the lower 12 ft of this part are seen to be nearal wih out fossils (Heterella sirmata) and the remaninde contains lynx, Paris N of town River Level Plectamtruite sericea [illegible] horntage Dalmavella Trenton} zygospina From River almost up to RR Other borealis. [illegible] [illegible] At R R + above.

Manosilla Limestone creek, Middle Ntca. C F Olethreutes ? Whidella? with lynx. Near middle. Large Olot. & two lynx. Whidella there, not thru the basin lynx 9 1/2 ft clay + some good C. whidellii? 50-7 4ft- 5 in c. Dalmarella common 9 1/4 ft clay very muddy 6 in partially loose & 2 1/2 feet S 1 1st hole to, this first creek with two. B F [3 1/2 ft clay from to collected 31-2 2 ft chiefly massive l. worn mudlet 27-8 4 in c. bit Olot. if not a 1" wide. 3 1/2 ft clay, 2ft chiefly massive l. 3 ft clay, Strickella near base mill. 4 in lined me south, very moderate Strickum ballii + Cyclonema (16) A F [4 1/2 foot? middle Ntca. [12 ft from] I met bed full of straph, Chalcis, worn my ankle deep, To left of large clams, Turn at current. Results ? The sheet once about 200 yards. B are of section. AF = 0--12 ft CF = 41-1 to 50-7 EF = 70-4 to 73-6 GF = 116 to 134-6 IF = 201- 213 1/2 BF = 27-8 to 31-2 DF = 50-7 to 56-1 Balumfel. = 96 to 116 FF HF = 185 1/2 to 199. (83) minum plan. zule. Whinago lake Tut. I reditch, R R section Used, for thin see the 16 1/2 ft with Sump. plastic aneva Inward but not ajzened!! At above of thin 30 ft = sandy loose plastic aneva Cyprina, 37 ft to face of ledge with straph. off Turnado S.W bridge along east leading? 5 1/2 ft to top wavy layers middle EF 3ft 26b chiefly l. ? 20-4 10 1/4 in t of heavyz & ft thuds. under regular bridge 9 3/2 ft 3 1/2 ft thin lined if dug least used up. 56-1 D F [5 2 ft clay 2 lin red me wave 50-7 middle Ntca.

Fire exposures at first sta. in east of Winton, Utah? Mt Washington end of Flynn, Christm. creek section. 40 ft Madison beds. 43) 3 ft bry. Plant silt with Sta. vetusta. 54) 11 ft clayey silt w/ gray thinl. fragment w/ h. primata. Rhy. capax. An. retusa, Bertarea, Stroph. 60) 6 ft middle Redmond silt. Strophelasma small Madison specy. Stoph, vetusta, Bertarea. Rhy. capax, strophelasma nutten. Dimitius subzugaclata 6' 1/3 yrs thinest w/st clay, Brehma. Strophclasma and stroph selecta, St. planumbina, like me at Concord, P 5-3 silt + Clay Columbaria Columbaria, few Columbaria 4 ft end of clay limestone w/ th 61-2 1/2 ft Tetradonum (at top). 61-9 3 1/2 ft. Columbarium small. + 75-3 Tetradonum in silt to silt 10th at top. 75-5 1/2 ft silt & clay, at top is Columbaria's small + Beatrix Beatricensis middle 74-3 2 ft silt & clay, at top is Columbarium, apparently alveolata, some smallite, free and large in size, calcareous. Hays Spring 2' 1/2 ft clay. 6 ft Inner Laurel rock. 23 1/2 ft from top of Santa y or at least of the solid basal Wagona to top of a clay bed over which the upper part is clay silt. This is the original clay, thick non? Christman l. 40 ft beneath Clinton + 3 in thick. w/ Stroph, vetusta. 8 ft white s., silt w/ th Strophelasma, Bertarea, Stb. vetusta Bh.capax Strophplanumbina S of Flyng's Crete, K {mt Washington, M come shale type in N W V and Beatrix Indication of I 5 ft middle l. with Calpocaris -- Sencor is upper layer. emmm, zygnata, leucitey transposition? (under the silt). 45-1 blue & quest, upper bed w/ th Bone of the large crayfish, with 13 ft) Tetradium, + to Plod. laterita (see Birds and Crustacean, bone

5\1 MA Washington larger 3ft T.B., J. lativentricida, fossils collected. 11ft Barton drnm. is Lepidae- nea shumbridalia. fos- sils collected at Lefpae- nie lmnign, = 40 ft Madison 21 ft Middle Rich. 22 ft dwn to lowest Streptelasma. 4 mi E y Bardstown in '87 Fredericktown further N.y. creek. 6ft 8in. massive Bardstown rock. @ 2ft white clayish. Flor Tetradium 19 7ft Tetradium abundant white clay rock. 21 6ft banded Madison rock. 27 6ft clay, sandy, limestone band near middle? Stafieldrema rusticum. 25\2ft very fossiliferous clay, sandy. Dimorphus sulguadrula, Streptel. aeum rusticum, Physilestroma cajox. Stapf retusta. 4 ft clay rock. weathering to clay: Stapfi retusta at base. 42\4ft Alcyonaria - alveolata (stellata) Calcifescia Leda. Massive ends at top and also near base. A several lints, largest alveola to 2\2ft across, evidently single. 42\1ft Blue Limestone. Streptelasma retusta). 3 in. Charonaria shells. 49\28 + white rubble. 47\2-2\2ft Tetradium large in upper part of white rubble.

20 in, then blue l, with Columbaria halli 55 inches below top small 1 ft white clayey stuff with Electrica Plated - undulation but lace, believed to be in situ, 1ft clay rubble with fossils. 10 ft not exposed, unfractured from bed in ceiling; Frederick's inn level. (4) 1st solid blue clay pitch and clay shale hard 4 ft limed with Hygra Helvitica and Platystrigilia at 27 All the rest (shady?) sandy 66ft beach, bellow Coral bed 6 ft sandy clay shale with lugs 30mos + Helvitica + Platystigma 3 1/4 9 in hard and massive, L. 4 1/2 ft blue l + clay pitch hard with fossils ? ?qually blue measurement from core grade last year, late vista bp? 90ft down to face of section with Platystrigilia + Refin ers a nina, lynx at 27 ups 35 ft down to lynx 'Garage' in bed of sinder, No attempt to locate highest lynx. Chemistry of Pottering Linn J Shaw? Scott, Greenwood & Co. 19 Endgate Hill, E.C. London, 1904, 17 sh. 6 d. Viscount. glaze - vitrifiable enamel and transparent for painted translucent for enamel Gold Chm Delft ware, 17th Cent fruit - citrage 7-5- sand 2-5- grind fine & dry, powdered with silver nitrate heat in crucible greens fire. grind with beer- apply to well heated ware. in muffle cause glaze to flow and let cold avoid vapor of burning vegetables. 89

Pottery Hand book of Practical Pottery for Art Teachers & Students. Chasement Hall, London. 1903. 2 vol. = 5 sh. each. Gum arabic, light pencil, India ink, Decoration. Underglaze colors. Camels hair brush Fat oil of temperature etc. Hardening in, Red heat to burn off the oil. Glazing, dip or spray on. dry glaze in wooden tub, pour in warm water, mix two jars through 200 mesh. From off and water, keep in tub lined. Glaze thickness of milk. Stir thin while dipping. Dry. Remove glaze from places where subjects are to be placed = saddles. Steam escapes, cure kiln 2 hrs = hard kiln pencil art etc 1 hr = porcelain enamel colors Cool in 1 hour. Glaze. flint 100 ground frit 26.5 Frits china clay 45 flint 20 Paris white 55 bone white 17 corax 78 st me 80 zinc 30 white lead 70 Run glaze. White lead 160 Cray 32 st me 50 flint 52 10. Z30 8.2 & a Barber 709. T 828, Driggs, Harfen. 1881 May. Miss McGaughlin. Riverton. 1880 foot kiln. Underglaze color set as new with specification as possible with- out complete red clay Bmore Viera, ? yellow Ramping Birch ? cream & white Chattanooga T NEW only underglaze need. Painting, printing oil on linen tissue paper, orphy rubbed with soft flannel, & after fingers, plucked off. underglaze paint washed off. Majolica = color mixed with the glaze.

Orthuni retroza at Arnheim m franco f Straight creek, along straight creek in front of Miss Kate Berry, yns. Ds. to Bridge Leptaeina shunt widals in creek bed. Ojiforist Find Burr Leptaeina almenridals, jmet Holnor; Other menjoury'sen. Opposite Allan Barr Leptaeina shuntnidals of my Steffcheimgua crandam sis to 30 ft above level of creek, at Black franco Columbian clay a large limestone oval bed by fallen stratified beds. O of Leptaeina - almd 5 ft above creek, lateral betwena cm cn densin bug f Leptaeine this = 25 ft alnd. 6 ft up to the & mc endensis, 12 ft to f fine clay, dnn to stony wayy banded sand 7½ ft of f Leptaeina shunt ridals D. Suprae 95- to largest 2p inch wide, with flat flnx femg thin limer & mud clay. 7 ft abht - estimated formerly 6 ft dded in quarry today. many layers ni above face, crns 5½ft coarse sandy (limer and) cl 7½ fment & fly inter bedded, 4½ft Red resquine less thmderous 1½ fts met me. bent moraine, less cream a color 3 ft 9 in clay f. Lymx abundant at top - have removed 2 layer Ohio River and Columbus R.R. PM PM AM AM PM PM 5.30 12.55 6.50 Rydes 8.45 4.05 8.30 6.15 1.40 7.35 Geet. 9.00 3.20 8.45 6.50 2.15 8.10 Sardin'. 8.20 2.25 7.10 --- -25½ -10 ft. -26

N.J. Blanchet 3/4 mi. N. of Blanchet, Platystophia 15/43 small, Dol. multiseeta croweana. 1 1/4 mi. N. of Blanchet 30-28/42-42 Two mi. N of Blanchet. 0/42 Three mi. N. J. Blanchet, 2/41 Anisomera pallid? D. multiseeta. 1 mi. N. J Wazen. Ky, Rulwell ln, 35 ft belw Rd Track, at Williamsoun, 97 AF = Leptalnia rhuan bridalis zone. 11 ft below the 3 ft bed forming trip of laticosta zone at S. J Mt. Washington. Warm BF = 3/4= top of Platy. laticosta bed at S. J Mt Washington. Ky. Base of Lower Richmond. AO = 0-5 ft below Orthorhynculus La beds, 1 mi. N. of Paint Lick. Hy. Middle Fairmount BO = Orthorhynchulus bed, 1 mi. N. of Paint Lick, Hy Middle Fairmount CO = Cliff Strph. mayserillensis horizon 1 mi. N of Paint Lick, Ky Base of Fairmount AQC Crittenden Sherman Dry Ridge. Ky. Bellevue. Bellevue. Multeseta beds. Upper part of Fairmount. Multiseta is virg abundent in upper part of Fairmount in Fairmount section 1 Cm + is less Common in Middle F.

AW. = Rhynchotrema dentatum zone. E of Wyoming, Ky. Warren BW. = Leptaea nevadensis zone. E of Rectortville. Lewis Cr. Ky. Warren AR = 0-14 ft below Stuepstaema SW of Sunset Ky. = SW of Hellerby. Ky. Warrented? Praesfena layer, [illegible] BR = Praesfena lespitalis zone at It war dis Hill. 4 Loc. -- 1/2 mi. S of Rocky bar, in 1st my of stream 65 ft below top J Arthus I localis & Rhynchon- trema. 170 ft below layer with clay nodules in erinoidal limest me. 3a Loc. East of Rocky bar along road up will along my lane rocks along road side, probably join uppen 25 ft of the Trenton, Associated with strph. like plan convesa, Platystrophis and all, Arthus's localis. 3 Loc. -- Rocky Bar, Ky. 20 ft below top of Trenton. Up gully east of stone. 17009 inches = Based Utica east of Hatt m = 57 of [illegible], 3/4 Lexingtn, W. J B enz m. 3/4 mi. E of Hatt m. 20 ft above base of Utica E by Hatt m. Stroph. hallie zone. W of Hatt m. = 90-100 ft above base of Utica, not corrected, Middle Utica Tip of Middle Utica. E by J.F. Lea. W of Hatt m. 137 ft above base of Utica, not corrected, Base of Belt Type. W of Hattnmly, just above lower Stroph. mayevillensis - 1 mi. E of Conserlatum Ky. - Base of Farm out W of Anttu, above 2 ft clay bed, above strph. [illegible]. 97

Falmouth Base of Utica, 115 ft above bridge M J turn. 10 ft below base of Utica = a short distance below Tip of Trent in limestone row, 105 ft above bridge, at sharp turn of road. 45-55 ft below the Utica. Falmouth Rg, =60 to 70 ft above bridge, just below heavy timber trees. 38-45 ft above River - above railroad North of bridge, Falmouth. Ridgeland Tunacillas x Maysville x Vevay x caden Saluda (Madison) White water Liberty Wagner ville x Ann being Warren Mt Auburn Cornville Billarne { Fairmount Mt Hope, Meyer Meadle Lover.

Rne Rm. 8 ft soft clay, 4 in. limestone 4-6 in. blue hydrated ore 3 ft. red v.d. Plana?pta expansa Callopna magnifera Lita Clemella divicens? Lepidina plinulidalis Cylmena Dayi varae Salen quella elegantula Artotites Doyla from Fairfies 45 44 Black shale. Dev. 8" light brown claysck, shaly, 4" more solid, worm markings, 10 3" light brown argil pebbly exposed, 10 light brown rock, cherty, '10 same, cherty, few fossils, 20 5" Same, casts of crails, chert little, 2" chert, Crails plenty, 10 1" light brown limsted clay?, coal, 1" chert, Crails, 10/10" light brown l. cherty, crals, 10 8" light brown l., fossils few, 2" Dark blue sandy fish layer, (110 8" = Devonian l. section.) (10" = Maximum thickness fish layers) 23° clay dense?, part L (35° clay Mt measured E J William Johnson, E of L 44. 5 ft limsted clay, 7-2 ft blue clay, Plum creek, 4 in. light brown limestone, 8 in clay 1 ft ferruginous limestone large crinoid heads in lower part. 5 in limsted, large swm's beads at good whit? Fildella 7 in clay 4 in limsted int. 7 in clay 1 ft ferruginous limsted ms.

at William Johnson L 44 By mey Clint m, Ray Clert, Hatch registration NE of 27 above about 3/4 gins Plc [illegible] references, [illegible] Dla Partes 4 new by Porth bynd 3 5 with 1 Red hence. yinced in with Zalechia modulata, Strept. canadensis; Columnaire alveolus, Beatrix (55 ft shaly Rivierinoi.) 5 ft clay under [illegible] fen, 14t limestone mit Zalechia [illegible], a few Zalechia higher up in merging 5 ft bed already noticed. (5 ft limestone ripple ol g) presb rattle common. Rhy. dentatum met Anderson at by less than Lepet alb & abulim ovals of every all levels; Olat, lyrus few, large. [illegible] 2ft clay rock, massive, few fen. 2 ft very fine graded the lime stone dense, in sand layers, [illegible] fronts 6 ft shaly clay rock [illegible] fronts 3 size of section not seen one. (At least 15 ft total of this shaly rock farther [illegible] with Anderson & [illegible], Edmonds Lynx) C 113 = 1/2 mi N of experience At huge swath of Red Amuse Ovithyga cluda is abundant throughout 10 ft section without & above-mentioned 1ft thick? shaly section by no 5 ft higher up; about 1/2 mi N of Redhome stroph mayorillensis & abundant, Tom Anderson, 2 mi N of Redhome, [illegible] by bridge. Not after with 2-3 in limestone & abundant stro mayorillensis

"M. hedge & ms of Clarke Garrard's lady deceased Late Ed. Muller, 1877 cypha - crassa Actinostoma - fissicosta. mechilaria ? test dinama, murmonas? Syn. fu bertae ella (?) 2nd ed., p. 296. "Ostrea circinnatiora," n. sp. Wm. R. Sn, Cincinnati, Ohio, Preferred instead of ostrea costata Hall 1845 Am. Jour. Sci. and Arts; This is a very small species found associated with other minute fossils in Vine Street hill. " F.) 2. Tangential section, similarly enlarged. In this specimen the circulation of the vessels have been filled with gelatinous greens mud, and the skeleton has been subsequently dissolved. mitson and clem. bide Stromatoporidea. Actinostromidae, Actigenista ma Clathrodichya Stylo dichym Lade chrydis. Inche chia radiale pillars variable Plate 21 Rae anelle radiate pillars Beatrixee tabulate central comb minute radiate viewed plate. D ostromma Stromatoporidea Stromatopora Stromato porella Parallelism Syringostroma Idiostromidae Idinostoma Annatostrina Anaphlypora Sta chrydis 2. che rassa, n.sp., p. 82, for the Circinnatae simp of elm. Fig 1 (plate II) 2 bed's living sp.; vertical section enlarged 12 times. Elm with simple Wyege with elm's calcit

Bectrea modulna, Fig 1, Con G. Marthm G. = modulata! 2 (not modulna) 3 modulna Under Park Gr, Wst end left homs Anticasts: cast by Richardson. Fig 4 5 cast by Webster 6 7 8 Popular Mechanics, 15.3 1/2 13.6 17 1/2,00. 4 9 2 8 4 13 1/4 1/2 39 1/2 39 6 13 6 26. Bergunto Run of Dodd, Fate 2 1/2 mi West, Charles ville Dolmanella exceeding common Fate: but not seen except top Animalrodment. 5 1/4 ft 20 1/4 ft 8men in limestone + gellen with Dolmanella jupana (corium) a clay section + Byssomyx a+ (animal rodent) 16 1/4 at a mudbedded with much clay) guess much later. Both limestone ells in with Dolomanella limestone in that the Dolbany not a great quantity of clay, at distant level, associated.) 3 1/4-- Dolmanella in thin limestone Dolmanella jupana a clay, small quantity some crusts. 50 Clay + clay limestone & novel Cyclna. Westrypa in sandstone? terbedded. A clm encountered. 50 C" Clay with much less clay rocks 60 6" Nodular clay rock Rafinesquina Animal, dont a giganta striph. cm on dinner.

R From top in 1in limestone. 2ft 6in siliceous bed, with Leptana 4th. 5 ft 6in clay with little thin limestone. Delstila msspta lower bed with ware marked limestone at top and several limestone layers below, Waremarked layer at top, sulcata str. mutans, mutanox concens, neglecta neglecta quadrata neglectax vetusta vetusta - Charles nilemi. vetusta Lydæna rhomboidali, Phynchthæum cepheo dentatum. Streptelasma Lelechinie Ostracium, R. clay with few lamellibranchs limestone with Pleuroon Byrrhomychia + M. dravidicus. Disparthus mutigdict. 2ft 4in stiff clay + clays L. 8" Leptæana sedica, strept layers of L. 10" stiff clay 8" Stroph. plasmantum - ant.- venti comman. in zones layers of L, pl 603" l + clay, interbedded, plane Bma. 4" Distot. incrustata in 2"L at 4" L. Nth. str. neglecta with large pebbles from chell Lays (se next page) 4" l. with str. neglecta B 104" clay 10" round L. with neglecta musanta 3" to top 1 limestone with str. neglecta+ 4" to top 1 layer fully plasmantum. 207" to top 1 layer forming falls. 3 toes layers 9in Raphaeognine disturbed {9in clay chief 5in siliceous limetum, tiny 2 in Byrrhomylicus.

Velgsta Repenta in some layer above Distended layer several feet. lagoon layer, b/ J Robert inscripta disturial 12 ft. layer flat Distadium Limered. 2wi. Het. in 2 calypso. 9' overall 2ft 3in Disturbed Layer large land overall 3ft - to typical col. total - 1ft. clay with 2in lath, shell, shingle B. above there is sulcata clam in some places within 3 ft of poster bed, above the bed, and becomes rather common w/ 3 ft below bottom or inscripta,

Stephans crinns deformis, Rowley, near Big Creek P.O., Big Creek. Gujrno. Steph. gninqnepartitus, Rowley, near, Big Creek P.O., G. R. Greene 127 W. Market St.

F. K Dark grey lowest Thelco Alexo Del. Balanites Danae M+W Compare with Tennessee live specimen at Glenkirk H, [illegible]? Tall spine. Plerinea Thelocensis Mc JW, Meristella ? Centromella Billingsiana Street olygnatis sulphureus. Largest Centromella Billingsiana: length .63 breadth .50 convexity .34 Cest. [illegible] slight meristal sinns Like Cosoro Mouthfield -ella. Swington 87 L. Stephens 41 L. Port au 46 L. Olympia 49 Salt tick, 54 C H Graves Olympia 12y, [illegible] St George Hotel Winchester, 12y,

Prof. Porter, Kentucky