Field notes, Tennessee and Kentucky, undated

BC. 60824 Louisville to Nashville Bicycle Check. Newsan Station. (11) 1\frac{1}{2} Foster + Creighton's Switch 2\frac{1}{2} Pegram. Kingston, (10) Aug. Saturday. Newsan. Grarry \frac{1}{2} mile S of R.R. station. 6 ft. Waldron shale, fossils. 16 ft. brown gravelly rock Samples, red courses in white rock. In Sand was found Orthoceras arimulatum Large Orthoceras large 1\frac{1}{2} Waldron shale 66 ft above R.R., RR = lowest exposure The Devonian limestone occurs west of Sam Newsan's house, just above the house of a negro tenant.

10 cm2 This section is as on page 1, but scale = 5 ft to one square = drill hole section. Waldron shale 22'1/2 ft good quarry stone 1 ft soft clayey shale 2's 1 ft limestone 6 1/2 ft soft clayey shaly lime rock, Cherty limestone at least 30 ft of the lower part containing chert especially lower 25 ft. R.R. at Newsom 12 Belfield Robinson's - 10 cm2 A. 22'1/2 ft of good quarry stone at 1/4 mile West of Newsom station on quarry 20 ft of good quarry stone at Newsom station but shale not seen there. 16 ft of good quarry stone at quarry 1/2 mile S of Newsom Station, but the thin layer of quarry rests on a good but probably thin limestone layer, 10 cm2 B. exposure of the soft rock that weathered into clay is found 1/4 mile West of Newsom station, at quarry in S side of railroad, along the track. Between Newsom and Foster and Crescent switch, along road on N. side of Harpeth river, the limestone is 11 feet thick. The lower 2 feet are four pink colored and the next 3 feet are tinged with purple. 12 Sam Walker's house is about 3/4 mile west of Foster and Crescent switch, just W. of the point where the road crosses the RR just before reaching his house. A road comes down hill, and then along the N. bank of the Harpeth river up stream, where this road turns south ward, 5 ft of Devonian limestone are with 4 inches of quarrel stone or top at one point (black shale base) occurs way on opposite side. At Belfield Robinson's cherty layers begin 5 feet below clayey rock.

(13) 1/2 miles W of Pegram, just east of bridge. 8-12 ft Devonian 7 3/4 ft clay shale 15 1/2 ft to quite clayey rock A Devonian contario Orbis, flat valve, flat along middle and interior. Muscular scar occupies about 1/2 of the valve. A Devonian fenestrella form similar to one of those found at Newson. The upper 6 inches of the Devonian contains little black nodules like a some of those found in Devonian of Kentucky + Indiana. The upper 1 foot of Devonian emerges into the basal sandy rock of the black shale, but it contains the Devonian Orbis, similar to that found in the limestone films. Newson Sam Walkup (R&B) Pegram Ashland Baker's 32 ft 23 ft 8-12 ? 12 8- 22 1/2 18 ft + 15 1/2+ 8 1/2+ 7 1/2 ft 30- 22 1/2 ft 35 ft ++ trace 17 1/2 X 8 ft. 8 9/66 4ft. 24 1/2 27 1/2+ 1/2 33 1/4 10 ft 14 ft 14 1/4 23-27 12 1/2 ft 7 Pegram + Corniferous Bledsoe + Linnville Newson + Waldron White's Bend O Laurel South Tunnel+ Asgrod Baker's + Clint on Lefleur Creek + Illinois L.S.

Whites 9 Onarriss along Ashland City pike. Waldron, trichin aloia reticulata. Atrypa reticulata Eucalyptocrinus crassus annott Orthus elegautula. Rhynchonella acirrus Favosites globular, small. Spirifer smaller, very few jets catius Oterinea hira Septaera rhombroidalis, Strophomena patula, this is the flat form at Nevs pm & Waldron. Rhynchonella'd looking form with often nearly globular form. Not rare at Nevson. Rhynchonella Stricklandi have from Eucalyptocrinus ornato form, Spirifer, about 7 tiny plications m. each side of strina, radiating strae. A Myriactus pygidium Calymene Magnimens Sideralia coarse massive chunks, Callipera elegautula The one flat petophemosp'd abull w th distinct striae, Herring without radiating striae Orthus biloba. Dalmanites verrucosus pygidium. Reizix. orax, long thick Orthoceras annycho Meristina Manka. 9 Cant Black Shale 3½ ft. Waldron 2½ ft to 8 ft+ S aurel 22½ ft of top portion is quarried. Some reddish hands it as at Newson. Clinton along Ashland City pike Favosite favozus, Halcyte catenulatus Catharpelyllum calgula, Orthus biforata Orthus feakellites. Silaenus obuli'gnus, Slectambonites elegantula Strophomena flat & 1. patent-- Waldron. Flat 5 Angled Eucalyptocrinus. Dinnacnella folealis? Spirifer Miagonensis olyzimus Branding Philodistys Pluridistye - Whit pet dia m t da --

8 [9cut] at quarry nearest road. Waverly John Swell -12 miles Nash. Black Shale {1 foot, hannah sandy slate with a few muscles of animal color = 2 inches. 4 ft 3 in. {3 feet black shale. {3 inches, hrm sandstone, Waldrn 2 1/2 ft to 8 feet. The lower two feet of shale contain plenty of thin lime stone layers, and this is by far the most fossiliferous part. [arrow] Sannuel 22 1/2 ft of top section is quarried, [9cut] At quarry NE of East, several hundred feet from road. Waverly rests directly on Waldrn, about 8 feet thick. It & frm this and East quarry that the fossils were obtained. At a few places several slabs of Swartzville rock show up above the Waldrn bed, and beneath the Waverly bed. [9cut] Waverly rests directly on Sannel top west of John Swell 600 yds. at old quarries. Here the thin ner fossils were found. Views 1-5 just West of John Scott. Clint m + credited from Sherman. [9cut] along road just west of highest point just west of John Scott. 1/4 mile. Black shale on trace of Waldrum Waldrum complete in chos = 2 inches? very little exposed. Sannel, top well exposed. Practically in contact with the black shale. Thickness 24 1/2 feet. But am difficult to clieting marks from Osgrd. Osgrd not well exposed here, about 10 feet are accredited to it here, this being the unknown section. Clint m? The dirty beds from top of exposed cherty beds to bottom. The bottom will marked. There may be beds higher than the one here found but this is not very likely. Thick- ess at least 27 1/2 feet. [9cut] At another point I secured a measure- ment of the Chirty Clint m with a cloth or line. Thickness of Clint m was 23 feet exactly. The Osgrd above was calculated at 12 feet, and 11 feet of the very irregular Madison was seen below. The section thence was 12 ft. of Osgrd Take upper figure 23 ft. of Clint m. Take upper figure 11 ft of Madison + + base not seen. Fossils found at top of Madison.

10 Baker's Station, SE of station. 8 at northwest end of quarry Black shale 8 ft. Waldron shale, narrowing to only a few feet going eastward, 27½ ft. Laurel limestone. Pycnodontos communis 3-4 feet above base. The lower 2 feet form a transition to the rock below. 7½ feet of Osgood rock, a clayey Waldron like shale near summit near part of quarry. The upper half becomes a crinoidal lime. at one at the northeast end of the quarry. This suggests that the Osgood is likely to be not dis- tinguishable from the Laurel in 2 mile sections. 6½ ft of lower Osgood are exposed just above the Clinton str., north of the negro cabin at SE end of quarry. Rest of the section below at same locality, 12½ feet cherty Clinton cement near foot trps and bottom well shown. All of the fossils found below are here. Raf.4 ft. Leiper's Creek fonder. Belongs to over the massive rock at top of Cambrian Lancaster and Sanditon series. Then above spring just E of negro cabin at SE end of quarry, View 6 or 7. Clinton: Raffineagmina What species? 6 Bledsoe Station. 11 Smirville horizon seems to near lower dorm in the Corniforms. Small Spirifer communis, Olmu 1 mile N of Bledsoe, Jtjf and mutilated Smirville. 82½ Pentam. linata Sam Fleming 78½ Baker black shale at C.F. Hodges. 77 Pentam. linata, common, S FL. 68½ Pentam. linata, common, S FL. 65 Spirifer small C F. Hodges 61 Pentam. oblong. C F Hodges 54 82½ Spirifer Mag, seems only, C.F.Hodges 18 Smirville. Pentam. oblong. Atypical Nth erl anus.. Bledsoe Station. at Sam Fleming's darky, 1 mile NE of Waldron 9½ ft., shale, no fossils. Laurel, Osgood + Clinton, on south side of trench above Frank Carls' home 4 mile N off Bledsoe station. Laurel 39½ ft. exposed. Osgood 20½ft. Frank Carls, lower 5½ ft not common. Clinton. 5½ ft. white, cherty. Favorite farmers. Lower Silurian. View 8+9. Coring. along RR above Sam Fleming's home. The Pent. Linata occurred about 2-3 ft above RR.

12) 7 Smith Tunnel station. 3375 ft to S end of 2nd Tunnel 3300 = 5/8 mile. 150 ft south of S. Tunnel is top of Black Shale. 39 660 ft (810 ft) north end of Black shale in deep cut, 390 ft (1200 ft) south end of this cut. The middle layer at the top of the black shale is well shown in these cuts. (4 mi) (660 ft (1860 ft) north end of deep cut in black shale. 420 ft (2285 ft) south end of cut. Shows practically full thickness of black shale with overlying Waverly, Waldron, and Laurel. 540 ft (2820 ft). Half a mile = 2640 ft) north end of cut. Black shale, Waldron, and Laurel. 300 ft (3120 ft) south end of cut. 150 ft (3270 ft) semaphore electric sign. 630 ft (3900 ft) (3/4 mile = 3960 ft) north end of cut with Laurel + Ozgood. 300 ft (4260 ft) south end of cut. 60 ft (4260 ft) road crossing. View 10+11. Ozgood below, Laurel above. 120 ft (4390 ft) clinton top, 5/8 mi E of rail- road fence. 210 ft (4600 ft) (4520 = 7/8 mile) fence, (1080 ft (5680 ft) (5280 = 1 mile) north end of cut. Clinton + Laurel S quarter. 240 ft S end of cut. Filing regarded as structure of L. S. controlled. (5920 ft) (5940 = 5/8 miles.) 300 ft (6200 ft) N end of cut, Clinton, L.S. quarried an E 2 mi. 7 cent 170 ft (7190 ft) (7260 = 1 3/8 mi) south end of cut, (Total 2 mile S of S.T. station) 1080 ft entrance to long quarry switch, (8270 ft) 8260 ft = 5 3/8 miles. View 12: View of Black Shale with Waverly at top, as sort of darky and carrel, not much stuff at bottom at top of try. (2280 ft) View 1+2. Laurel, with Waldron, at least 5 feet, at top, at top of try. View 3. Ozgood, from lower level of railroad to massive layer above (at least) Plus may be 3 feet in another igneous rock. View 4+5 Clinton basal chert layer at kno's prnt. Controlled L.S. Selrin. Waverly Limest me layer middle (myc 1 ft) Shale black 16 ft) 25 ft Black shale ealthy 8 ft. Waldron at least 5 ft. Laurel 28 ft down 3 1/2 ft transition Ozgood 14 to transition. Clinton 7 or least, Top of Clinton 55-0

14) On road Tank to Linton. Inside northeast of major log hut, north of road, [illegible] mi. west if major church, 2 m, west of Tanks. Clinton with Stricklandina, Halcyte, Ottos flakellite, Favorite favusot Miaferensis in chert fragments @32d + Laurel 38 feet 60 top, of Limestone are exposures, 43 ft from road level to top of Clinton. Chert. Piercerimas in the limestone, W. M. Forehand, at foot of hill, [illegible] mile west of Tank. [illegible] 4 ft above black shale, 4th from Wonder. Seen in clear not distinguishable at me at both end. Trip not 6 1/2 ft Black Shale, No sand - 3 ft. with cherry layers. Clinton 10 ft. not exposed. 9 ft. crystal archs, LS, a little like Sapas level layer in open range. 5 and 4 below the layers with plenty of trachis. Favus below. Tank is 3 miles from Bellevue. It is about S.W. about halfway to Linton and Linton is further up than any map. 15) About 2 miles due west of Franklin is high ridge. On east side is black shale apparently overlying Anna Silic [illegible] on directly, No fragment of Up- pier Silurian seen and sections not on any feet apart. 21 About 4 mi. 20th on the Franklin- Columbia road is a store, 3/4 mile west of the store is a large butt, at top if this butt is black shale apparently resting on Anna Silurian. Same as last. 22 Four miles south of store mentioned in last shotc is Hillsboro, also called Lei- pers Fork. These names do not apply to separate localities as indicated on any map, Leipers Fork is the correct name. P. S. 23 About 3/4 miles west of Hillsboro in road to Fernvale is the home of Mr William Penitt, On south side of road at opening near foot of cliff is Black Shale rest- ing directly m. Anna Silurian. For section see former visit. Dottins Barrel, 2ft layers with nodules chiefly at top + bottom. 5 ft Black shale, 4 in., Chylermate layer, 1ft. dark brown sandy stuff, age not known. 30ft. clayey Anna Silurian limestone. 24 About 6 miles from Hillsboro and 1 mile from Fernvale, just before reaching home of Mrs. Annieorman Black shale resting m. Anna Silurian limestone with fossils. Black shale [illegible] ft. nodules at top, Leipers Fork bed 5 ft. & thus only quadrate and the characterisic Stepflinense. The last is annaday limestone, froaliferous.

16. The large Gethio lymns is found just beneath. The Seijers' Fink bed is crinoidal, crasse, reddish rocks, etc. This bed was found yesterday at W.M. Foreland's place. 20 At the Spring S south of Fernvale The Black Shale is 7½ feet thick. The Spring comes out at base of Black Shale. A short distance southward the Sauran Silurian (Seijers' creek I think), slumps up below the Black Shale. Effervesces of black shale die appear 2m S think going up stream, southward. Plenty of rock between Fernvale * Springs & Spring in m road to Tank. Best take this road from Bellevue. 23 At south end of Hillsford, up the hill west of school house at Spring Black Shale m lower Silurian same section as at spring of Mr. William Perrett marked to Fernvale Springs. 1 mile section also about 2 miles south, up stream 1 mile, sorry not from school house but a broken down bridge. 17 27 Along the Franklin Carter's Creek just 7½ miles out. Then west up the B rd an road 2½ miles. (2½ miles also from B rd m) Barle Potts lives here on S end of Craig Bensley. A short dist once west of lemma a fine spring is found 1m north side of the road. Near top of hill above the spring Black Shale goes up in the large Silu- m! (in Seijers' Fink bed??) Fossils found up to top. There are Lypt nodules. The entire thickness of black shale is certain less than 10 feet. Want at m. At the Sulphur Spring. 1 mile W, 1 B rd m, the Black Shale goes directly on Sauran Silurian line at me, with fossils. This is not the Seijers' Creek bed. Up stream from Tom Fox, Seijers' Creek. Clint m is dirty up to very top. Near top is the Halcyites horizon. Halcytes very abundant after several specimens of the peculiar cup shaped fossil which I once considered a crinoid base, and which I found both at South Funnel and at White's Bend near Oakland City in the Clint m. over.

astylpenya? nearly 3 in. broad with radiate cannel on upper side. 18) Styligenya, half as wide as the large form at Dayton. Ollanus like large form in Coyrod in Indiana - Ollanus ambiguus. Parosites far from large, a form apparently Rhinogenya frandsa. Helicites, and striatulates Orthis flebellites, Orthis elegantula, small. Orthis bifurata, small. Clint in 38 feet thick. Over it is some Silurian thin shale with Arthos spinata about distance above Carol Sutton house, 1/2 mile above Tom. Fox also tranching byrggyaous + Stephenea like form above Olanus Sts ? Rafinesquina? About 1/4 mile N of Fly's store, 200 stops north of W. F. Booker's turnse on left side by road. Above Silu- nian shale, about 4 ft. thk, 1 foot limestone and 1 foot shale with fossils. R.C. Olanus store is 3 miles N of Fly's and Booker is short distance north. Water Valley is 5 miles S of Fly's. At Olanus store above W.F. Book- er's house were found: Arthos flebellite form, Arthos subgradata { in clay above Arthos acutilingta, } Seifer's Creek Arthos acidentula } limestone, Stephenea, several species, Rafinesquina? Notes from former trip, Columbia, Bethell Hotel 1000 Williamsport bridge, 912 Seifer's creek, 1st crossing 900 N E of J.M. Gardners house, about 2 miles S of Fly's store + 2 miles N of Water Valley 970-988 Seifer's creek 1st at gardners, 1070. Section N of J. M. Gardners house. D Top nodules layer, 4 1/2 ft above B, Nodules large, phosphatic. C Shales light blue above, dark below, earthly, not jet black + fossils, 4 1/2 ft. B Top claymudite layer, 2 ft above A A Clayey beds underlying Seifer's Creek mm solid limestone, contains bed 3 inches ?? O 9 ft. crinoidal L.S. limestone, Very richly fossiliferous. Section N of Booker's N of Olanus etc. 3 ft. white crinoid limestone. Clinton. Atropka undistriata. 4 1/2 ft. clayey, soft weathered at L.S. 6 in. lopo limest, fully of fossils 6 in. limest, fully fossils seen at Gardners. 1 ft. blue shale, L.S. fossils, loose, 6 ft. 2 alumin brown Seifer's Creek bed over,

201 Notes from former trips. Tom Fox, 7 ft 4 Upper Silurian section. Worthy Mudule layer, 1 ft above, Black shale, 3½ ft exposed {9½ ft} First Black Shale: 5 ft above Niagara. Above old Ave Spring, Weyer Silurian seems thicker than at last exposure going up the creek, Why former readings were, 3 ft black shale, 44 ft. exposed, 14 ft not exposed, Leigh's creek bed This must be looked up again, J. V. Sinton, Davidson Cr Black shale at 1175 Shivery at Hillston, 1107. 58 32 25 Sinton V. Sinton J. V. Sinton about ½ mile above Ellis Store or Sinton P.O. d) And about ⅔ mile N. of Columbia quadrange, 3 in limestone 21 ft Langel, Pizocinno 6 in, soft mible claygy limstone 3 ft 0 {harder limstone} 1 ft 3 in } 1 ft 7 in, limestone weathering face, {4 ft 10 in. claygy limestone, like Ogrod limestone in southern part of Baker station quarry. Ogrod section upstream, rocks dip south, 15 ft of Climus exposed downstream shirty. 1 mile to J.G. Sinton, where road crosses on the white valley westward about 4 miles to Sinton, about 2 miles to school. c) About ½ mile beyond J.A. Sinton, Jr. where road crosses the stream, going southward, is Black shale resting on Climus, shirty. Black shale 16¼ ft cherty Clinus Halyzites 4 ft not exposed. Creek Helicidite with lagenolite as at Tom Fox Cyclomematilix good. Favrite farman

22 a) Black shale at School house. 5 ft shaly clay, such as is found above Sand Shurian and below Chint in N. of Telarric store on Lefler's Creek. N. of Tom Fox, age of this shale unknown: Sand Shurian? In Sand Shurian limestone are immediately beneath me: Orthus platellites form?! Arthur sub quadrata! Arthur like insculpta'? Strophomena large, deep mm. cular impression. Next after the real large one in size. This form seen at Dayton, Crustella are just it smella to. b) Just N of little branch, South 1/4 mile of Jim Clinton Sr.'s House, 2 ft Cherty Flint on or 2 1/2 ft of the soft shale mentioned in last locality. Sand Shurian limestone, Black Shale on Clinton. 23 Centerville. On road W. down to R R. station. Waverly 4 in. Module layer. 4 1/2 ft. Black shale: then decayed 8 in. Sandstone layer, phosphatic bed 2 1/2 ft. Waldrun shale. Top eroded pretty. 15 3/4 ft Laurel. Piercerinus gemmiformis! Some part not exposed here. R R. section S of barn Centerville Reddish bands in the upper part? Laurel bed, Iron Stained, more cruminal than any place so far seen? 4 in. Module layer, 4 1/2 ft Black shale. 5 in Phosphatic sandstone? 4 in - Waldrun shale, as an accumulation. 25 ft Laurel rock. Piercerinus & Arthur- nis body, transition to Laurel. 4 ft. more solid calcareous rock weather layer calcareous rock. 6 1/2 ft often shaly, sometimes rather firm 12 1/4 ft Clinton. Both on. not seen. 20 ft not exposed. Coarse crinoidal layers, Slipper Creek possibly, not verified best. L.S. Clinton is therefore not thicker than 31 - 83 feet,

(24) Clinton fossils at Centre ville Farms farm's. Halynite Calymulatus Stictoceras branchyng Lyellia central bilateralis Corthis, flabellites, Trifidica Ctenum, complete very good about 9 1/2 feet thin top of Clinton Clinton at Bridge NE of town is 20 ft thick. Bottom not seen. Centre ville Montgomery's mill. Orelinmary section. Waverly, 1 ft trainy, carb. shale. 4 in. varicolour layer. 6ft 3 in. Black shale. 6 to 8 in. Sandy. 28 ft limestone to base of black shale. Colvert in road 57 ft to black shale base, back. 15 ft. Clayey limestone, soft weathering. 72 ft. Total solid limestone rest way up. 25 6 in. Shaly limestone. 9 in. Limestone 4 in. Shaly limestone. 1 ft 3 in limestone 3 ft limestone, 4 ft. uniform clay, fossils. Nothing but rock from creek up to this level. 43 feet above creek. 29 feet below Black shale. Montgomery's Mill. Hickman Cr. Completed section. Waverly, 1 ft. trainy in carbonaceous shale. 4 in. varicolour layer. 6 ft. 3 in. Black shale. 6-8 in. Sandy layer, shaly layers 4-6 in. thick occur limestone, except at very rare when 25 ft to base of Black shale, also solid Spinifer Andorea. Phylinchymella Tennesseeus? Platyctoma Virginicae. Encalyptocorinus coelatus! Encalyptocorinus fortius crassus 4 ft clayey fossils. Here Daffna records above mouth of tunnel at mill ville where he arrived. Total 43 feet looks like the Laurel rock at Centre 28 ft. more solid limestone. Wyekee fault not clearly distinct from rock above. 15 ft. Clayey limestone weathering back, 10 ft. From Duck river to base of section at Montgomery's mill = rise of river.

26) At spring is mile S of Swan Bluff. Black slate. 56 feet of crossbedded lower Silurian and limestone, then, weathering firm, fine-grained, friable fin. chiefly within hips at lynx form and byzaram, at base; at Swan bluff are plants of helicifolds. At Tennessee Mines, between Black shale rests on Lower Silurian crossbedded. Two miles N of Lewis county line, on west side of Swan creek, on little stream bed at fort Hill. Two houses on top of hill going northward. Dan Dun can see black slate, Several chert layers, the intermediate 2 1/2 ft rock all rotted away. Chintun? Layer Silurian crossbedded. 2 2 feet of chert layers with plenty of chinton Lellum, Helicites and tubulatus. Farmite farms. The Helicites rather abundant in one layer. Part of section on next page. Black shale preserving, although distinct in the same chert from vert unit. And Illaero day mines pay good 2 1/2 ft. chert in beds. Farmite farms. 6 ft & inc chert nodules in layers. Helicites common 5 ft up to layer mentioned above. 12 ft below this. All of this whitish limestone. About 1 mile north of Lewis County line, on east side of Swan creek, Anderson Morris lives along road directly north of the locality about 200 yds. W. D. Aydlott's property, bluff 11 feet tough, head and neck of Illaero- gino Day mines in top of masses; looking whitish limestone here. Some part is white and very dense. Mr. chert. In this respect it resembles clearly the lyxite part of last sec- Lime. 1/4 mile south of where we turned to go to the Tennessee Mine farm, can see as layer of black slate directly above the Illaero. 3 1/2 ft & over Silurian up to their level in Wide creek, where I turn off to Dan Dun mine. On creek where road turns N to Tennessee Mine. Phenefield at Mine 7th foot above creek Rock also strongly east. Some layer.

28) Up hollow, at Sam Turner's lease a short distance N of Mrs. Isabella Miss[is]sner 1 mile N of Dean's Switch. Black slate, 6 in. Sandy beds lacey Black slate, 8 ft Clinton nodules iron layers. Lower Silurian deposit Sandy blue with large cutters lignite, + Stephania alternata, Black slate 5 3/4 ft above RR level, Mississippi Meridian Switch. A-A J. L. Dean quarry, 1/2 mile E my hollow above lease, 1/4 mile N. J Deans Switch, 8 in. Middle Layer 2 ft Black slate, not fissile; 2 1/2 ft. Phosphato Sandy layers. Lower Silurian. All along this hollow the Lower Silurian is cross-bedded and is mined for brick phosphate Monday DSL Tuesday B-SL Montgomery M. Wednesday B-SL Swan Creek Thursday BDSL Deans, rain. Friday B-S L Totty's Bend Saturday B 29 Just beneath Waverly bluff, About 225 feet N of Spring mouth of Mrs. Rebecca C. German's house with a spring where Centreville road enters Warren Creek opposite Blue Buck creek on north, On W side y road. Black slate. 9 1/2 ft. Clinton nodules joint with clay nodules, white. Cross-bedded Lower Silurian shunt with shist, alternate a Blue Buck A short distance at the junction of Ugly Creek, a short distance up stream above Sam Wherry's lease on Ugly Brook creek, about 2 miles from Swan Creek, Black shale on Lower Silurian with cutters lignit te, A. occidentalis, + 3 alternated. Up branch above school house, Sec 16 entering W side of Blue Buck, above school house. Black slate, 5 ft unknown. Lower Silurian.

31, at mouth of Tom Bark Hollow Clinton Farnites farrons very common. Fammites viagannus. Halcytes common, at least 13 feet of Clinton. Bone not seen, also trip not seen but apparently no sand here; Black slate. 2 ft white limestone. 10 ft very light exposed. Green? 15 ft solid limestone, white, Lady Clinton Base of Clinton not seen at spring up Tom Bark Hollow. At spring up Terrel's Hollow. Terrel is correct: Halcytes, Farnmites farrons + viasarumis About half way to his spring in black slate? Black slate, 18 ft Clinton. Second limestone At Fagg, 1/2 mile SW. of Totty's Bend PO. 1/2 mile W. of river. 6 1/2 ft Black Slate! 1/2 ft sandstone Farnites farrons 5 ft Clinton diest and white, Dayton &c hard; Lower limestone. Arthur minnat a large blue round; at Godrich, at spring down stream. 31 Clinton at least 16 ft thick. Plenty of chert, especially at trip. So this Clinton or 2 new Carboniferous limestones. No fossils were seen and the rock was not cracked open. It looked very much like Clinton, but the level is 550 and at 569 at least from the limestone in Mountain limestone of Stafford. Bardensburg Palestine.

(32) road J.M. Gardner Water Valley should be longer? elann's line? Fly? stone? oil spring KENTUCKY (33) 14 E. J. Illgate E of Middlebam. Samuel limestone. 4 ft clay & rock 5 ½ ft Ozgrod limestone. 22 ft Claygy Osgrod accretos. 1 ft red, siliceous clinton. 2 ft gas exposed layer. 13 On road to Beckham St. leading N from 4 ¼ ft. Chint & red oil coals [illegible] addithm pike. 2 ft. int exposed. Silifly soft L.S. beds. 4 ft. Gas. bed Muschzenna. Aubny dioradic medium beds, most decayed. 21 Where road branches E. of road to Tucker St. stone red oil coals only 3 ft exposed. 4 ft Clay + Claygy rock. 4 ¼ ft stone...Osgrod reddish siliceous. Claygy Osgrod, full thickness not seen. 22 Magnificent able clinton reddish crinoidal. Cellus platebates. Stiplemura in the elevated bed otherwise no valve flat - Halytites cat crinalis Septalae acervica, Some of the rocks tryed like Madison clinton. Favorite favrons. Rhingorsq Total thickness 12-15 inches. Gas exposed layer with superdister large form, just beneath. On west side of new road from Middle town to Tucker Station, a clint area, Some N of entrance to old Blankens- baker farm. More clinton S along road.

(34) (23) clinton 12 in., baslt, led., 12 in. (24) at broad angle N of Newkirk's. clint. m. 12 in., L.S.; gaster, led. beds (25) H. Dacker house. duplicates of section 1. A clint distance below prs. clint. m. clayey, not measured, 5 ft. clint. m., { Ozford, ?, 22 ft. clay 22 ft. } 12 in. clint. m. limest. m., 12 in. Gasterosperm layers, (26) Cedar Spring Church, on road from jeffersontown to Seatonville. Large bluff. ? limest. m. 2 1/2 ft. white clay, 4 1/2 ft. Ozford limest., red, silic. 17 ft. Ozford clay, purplish blue. 3 ft. basal Ozford. 1 3/8 transhum. red, siliceous. (Clinton) 1 1/2 ft. Clinton (18 in.) varying from red to salmon color. All ovinicidal; Halysites. Favrites favros Pachydictya lirad from with nodules. Orthos hypsita. 3 in. B. blue clay L.S. 34 ft.{ 24 ft. under Madison { 10 ft. after Madison. 5 in. limest. m. th. fossils; claygy, lias limest. 4 ft. Clay rich. Nutter silt. 14 ft. Richly fossiliferous clays merging into fossiliferous limestone below. (27) at Shunk begins my Cedar Springs Church section same as (26). (28) First Errad S., of Fairmont P.O. 18-24 in. of Clinton varying from reddish - to salmon from Fall, same section exposed as at Cedar Spring Church, including Madison & basal Laurel. (29) Harp Spring. B. an act am road N of Elm do. P.O. Clinton with Pleistom fossils 20 sec. Rhynchofra parvora typical Ostrus cles curata, simple nerea flat, but raised at break. Orthos flabellos Fava the farmns. ? Laurel, basal part, 2 7/8 ft. Clay. 5 1/2 ft. Ozford limest. 21 ft. Ozford clay, & numerous nodal layers at top. 8 in. basal Ozford, our chart, red silic. hum. 2 1/2 ft. Clinton, salmon brown, coarse grained + rough irregular bedded. No shrt. - Fine Madison section. No gasterosperm led. at top. No Clint & Madison. - The upper 4 inches of Clinton has white chalky m. in it. This may be the chalky layers Smith wrote.

(30) along W side pike 1/2 mile south of the gate No Mrs Mary & Clarke Clinton sharply defined from Madis- iam. Grani + irregular bedded, sal- mmon brown; 21 inches. Above this are 3-4 inches of reddish silicene rock, Out foot of basal Osgood are not clay. The basal Osgood clays are purplish, all exposed as at Agy Spring including basal sand. This is about mile N. of Mount Washington on Bardstown Pike (31) S.W side of Mt Washington, along Bardstown pike 1 mile S of Mrs Clarke. Osgood formation, 20ft Osgood clay, purple silice, indurated layers 44 in basal Osgood. 24 in transition arch. Farmites farinos red silicene loamery. 22-40 in Clinton salmon brown typical in grain + color to Alzites. No chert in this or the 2 upper layers. 3 miles to Southville. 44 inches of very typical salmon brown chert in are well exposed along the pike several hundred feet southward. The Madison is also well seen at 6-8 foot bands as at Madisiam (31 Chrt) 44 in, Clinton, salmon brown. 31 ft. typical Madison. 2 ft. Lagry larch with very few fossils 5 ft clay with few fossils, 4 in limestone layer fully fossils, 1.8 clay fully fossils. In Clinton Simpsonian flat valve with narrow hinge. Crithis flattables, Rough bedded, irregular sandy patches, Rhinop. or frondosa. This section closely resembles Cedar Spring Church section. Large Cyathiphyllum as at Day tan

{ "text": "(38)\n44 just left reaching school and\nchurch at 14 mile from Bards-\ntown, Crinmumaria is seen\nin the road side. Farther down\nthe hill is a white Niagara looking\nrock with Crotius record but also\nand Orthus Di'mata. Some Silurian\n45 On a right of a mile S with of this\njust before reaching house I\nSteve Loyd's home Crinmumaria\nis very common in the road, This\nis the highest point since passing\nSalt River. From this point\nthe jike goes down hill as far\nas High Grove, along\n46 At Sam Wells' home, at road\nangle, the Crinmumaria layer is\nseen again. After this for a consider-\nable distance the road keeps\nat about the same elevation.\nSam Wills = 11 1/2 mi. from Bards-tom,\n47 Mrs. Geo. Abell's home, 8 1/2 miles\nfrom Bards-town. Here there is\nthin bedded lower Silurian\nwith Orestus Di'mata & Orthus Di'ma-\nta, L. S. form. Later discovered\nthat this was very far in just with\nconnection with problem of area\nat 8 and point at a considerably\nhigher level, there is good lower\nSilurian limestone with fossils.\nThen road goes down to COX Creek,\nand up Cox Creek store 6 mi. from Bards-tom\n39\nIf any Clinton occurs south\nof Mt Washington it is believed\nthat it does not occur until\nwe reach 3 miles N of Bards-\ntown\nNo exposures occur N of Bards-\ntown along the jike.\nGeo\nDepot.\nCross Roads\nBarton's\ncedar\nHuber\nCox Springs\nConcordville\nSmithville,\nJefferson Co.\nBallot.\nMt Washington\nSmithville\nHigh Grove\nCox creek 86,\nBards-town\nHunter\nDocksville\nSamuels\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSamuels\nHunters\nCox Creek\nFairmount\nCedar\nBrook\nCox Brook\nSammels\nHunters\nConcordville\nDocksville\nSam [TRANSCRIPTION_TRUNCATED_DUE_TO_LOOP]

(40) (43) Clermont, & of station Theodore Habrich. Diggin Hill; Bullitt Co., Chapeezee Station. 45 Total Laminar at 33 in Perit. Oblongus, Waldron shale, Atrypa reticularis 8½ ft, Laurel limestone 20 ft quarried, upper 6 in dus politics /Total thickness of/ (42) Laurel is 35 feet measured at Holts station. At Holts station face of Waldron 5 ft above R.R., at Clermont station face Waldron is 12 ft above R.R. Geologic layer at both Clermont & Holts stations. Blue clay layer 18 in, Beyond limestone, 2 ft exposed. (41) At bridge 4, E of Holts the middling Wal- dron is at track level. (40) At bridge 5, S of Holts the top of Waldron is 4 feet below R.R., 16 feet of Lamin- sville stone, forms determinative at me, an exposed just before reaching the bridge. East of bridge 5 the tip of Laurel is oolitic, Strophomena with distant jefications & flat madre. Spirifera with deep jefica. Trims, Whitfield's retida. Top of Waldron about on R.R. level at face E of bridge Black shale on Corniferous (2 ft Conf. see) on Laminville (1½ feet!) (39 cut.) Black shale as far as Cave Spring. Station, at Station Corniferous is 5 ft below R.R. level; (39) Nolen line creek James Honeydew. 23½ ft Osgood clay, purple color, in a little quarry, down creek from home, enters my creek from S.E. Chert m. Orthis flabellata common, 6 ft 8 in below Osgood Clay is silicious, blue rock. Orthis flabellata common 7 ft 2 in below. Beyond clay is crinoidal the rock, 2½ feet below Osgood Clay is very chert. with Favosites favonsa & Orthis flabell. To Stroph. with raised leaf flat. When the road leaves the creek & turns west to Cave Spring at the crinoidal Chert in is 8-9 m. thick. Below is Waldron. Banded fossils.

38 Cane Springs Stn, 1/2 full miles to Shepherdsville. SE of stn, 1/2 mile clay layers. 5 1/2 Good limestone. 5 indurated clay calcareous beyond. 17 ft good lay. imm above, the middle purple film 17 ft. 2 ft basal good lime; 5 1/4 chintz with chalk layers. 6 in, granodolomite. Sheds. 39 E of Cane Spring station The Coniferous rests or contd into mine than 5 ft of Shinnerville. 40 cont at bridge 5, about 1 mi N of Cane Springs, the Cony rests in 11 1/2 feet of Shinnerville as already noted. 37 One and a half miles from Shepherdsville mile or so to Cedar Grove Church the Black shale rests in Crenidal Coniferous. Within directly or not I am sure since the Cretaceous contact was not seen. Below is thick exposed at Innisville. Pentamerus fossils have been seen in some loose blocks beside the road. 36 About 3 miles from Shepherdsville, along the creek below Lick Shelllet, the top of the same, with 3 inches of volcanic rock (very good) at top has been in creek bed. Waldron shale rises above creek level going down creek but not slowly that half a mile below the point where road turns off towards right (E) to go along the ridge (good ridge until the base of sand is not yet seen. Wollers Run old road to Bulls Run Over Washington Road. 35 At Ed Wollers home, about 1 mile from Lick Shelllet, the Coniferous is a very white rock with no fossils (about 3 or 4 feet thick) 20 feet above the Waldron. My finds seen in Coniferous to identify the arch. 34 At Cedar Creek 1/2 miles beyond Ed Wollers home, is base of Good clay, beautiful laminated with red pebble and greenish brown about 18 1/2 ft thick not counting under layers at least.

(44) (34cm) Clinton, 6 feet thick, probably not the Total section. Clint 2 ft from top. Clay indicated at rest thickness underneath. Jared for 1/3 mile in creek bed along road, (33) Oct W. R. Greenwell's linnse, about 1/4 miles from Greenwells Ford orthic clay at top of sand 2 1/3 mi. thick, The beyond limestone not well ex- presd. 34 ft to top 1 sand, 6 ft in midle rock, 6 1/2 put indicated clay rock, after beyond clay. {13-15 ft not expred} 2 ft with limestone with traces of clint at from first Clinton southward. 4 ft granular grained Clinton, chiefly blue, but a portion 6 in from top is salmon tinged in places, Oithus biprost + cutthus platelites at all levels. 4 feet Halysites. End of section at Jess Rulys linnse. (32) Section to mi. beyond W. R. Greenwell's linne, where road goes down into deep valley + then up again. About 200 feet 1/4 mi. are Bates' linne. Lutes. Sand, 2 ft. clays 3 1/2 ft. beyond limest. 22ft beyond clay, purplish gray, 2 1/2 ft. beyond beyond brown clays rock, 10 m. sandstone. Which where not wetland traces of clint at top 15 mi. then redded whited rock, with 20 inela. granular Clinton blue. Madison 19 ft. Madison, 5 ft rather soft clayeyrock. Thin fossiliferous layer in the clayeyrock. About 1 mile from Greenwells fork a few hundred feet by road Bates' divorce Clinton's salmon colored, Clint m. salmon colored, 20 mi. Orthiflatelites. Madison. Columnaria layers is 55 feet below Clinton

46) 20) corniforms many small corals, Niagara. 26 ft. limestone with plenty of chert, and men call it a good rock, into clay in some places? many have to quarry men. This may turn R4 3/3 ft. if a rock of lutes often called prop R4 1/2 ft. Slapstone. Blue ledge hard Dog 22 ft good quarry limestone, there is also chert in there lower layers but somewhat less abundant, Orbingle quarry, N side of Bean glass creek E of Lonerville, 20) Urban Single & son. just above R is what is called the 7 ft. ledge. It contains Pentana likita allied species came as Rleazor. No orthic layer beneath the Blue ledge R. 19) at Mike Syrs dairy, West y dairy is a little quarry. Rock with the Stromboidal agones as at Charleston. Shining that it is Lonerville bed, 18) 3 ft. Devonian. Species+C. Dier! 47) Cyathiphyllum crurmani 5ft, limestone corals, ) Crasse thin-walled 1 1/2 ft, corals in limestone to illustrate chert. 4ft, Niagara. Halcyites, R4 1/2 ft. Slapstone. Blue ledge hard Dog out weather to soft clay here. 13ft good limestone no orthic layer at top; 18) at quarry behind the Lusty farm, Devonian rests on lower shale here than at Single quarry. Appears mostly only in true weathered. 17) At Crossing a private road over Bearpaw creek, at corner tory on Bulls St Estate, ) Black shale or Cornif, in creek bed. 16) Black shale on corniforms a short distance NW of on road to Sydnor Station. 15) On road Middleton to Anchorage In quarry west of road but ambers oblongus a good layer near top of quarry,

(48) 7) Jefferson town on Taylorsonville Pike West, to Tairrorn then SE to grass. at crossing of creek. 36 feet y[ard] Niagara exposed. Blue ledge layer not seen. No exposures of value from 7 to Lanierville along south ern branch f Bearcrafs creek [275] (49) at Mrs. Amos James, 1 mile N of Wicken, on Whica fork. The Niaga directly below the crossing contains Halysites. Pentamer. 2 species. Stramboides? Stellate flat coal. Corniferous. {8 ft soft claygy rock 9 ft solid white l. fossils of soft 5-2 indurated ledges 5 ft white limed, = 7ft ledge f Sonisville =sprained limed out, " {2 ft blue ledge 29 17ft good white limest. used for lime At bittan is [diamond] Shimbros? good space 10ce claygy limest. Not quarried for lime. 11 1ft indurated clay. {10 ft Walden clay 45 {32 ft chert moderate [earthly looking] {13 ft chert very abundant limestone 1 ft top f bgood limest. at Charleston Landing. 1000-990

50) The Louiville limestone. Hamilton Pal. N.Y. Upper Helderberg. Volv. Pl. II, f. 139. Niagara, Catenifera beds: 1879. Hal Siver Helderberg, See Schimpe tenuistriatus Yincardia Phyridmella orientabilis Merieta princeps j.A. Price, 24th Ref. Ind., 1900. 82) It is quite probable that over a large part of the territory lying east and northeast of Greensburg, included in the shale area, the shale, if ever deposited, has been removed. 84) Louiville bed here called the Harts- vilile bed. "realizing the fact, however, that this formation is not very prominent in the immediate vicinity of Hartonville 89) Dev. rest in Samuel S of Greensburg. 99) Small unc onformity 1/2 mile NE of Milford, along Clifty creek, described and figured as being in Daniel creek; should be be- tween Dev. + Louiville think, look up. 101) 3 fut of Hartville bed at Milford. 121) Small unc onformity NW Lamb's Clifty creek. 1 mile NE of Newbern. described as between Dev. + Sam Probably should be between Dev. and Louiville; 128) Sketch of un conformity on Avery quarry, between Dev. + Snyder, 6 ft. Hartonville bed. 133) West bank Flat Rock Creek. 1/2 mile above Senc va. Unconformity. Dev. Louiville. 6 ft.

E Walnut St. cante Dr Alex W Nettelroth Dr Alex Netleroth A C Benedict 2025 Highland Place My Indianapolis car, 2 blk f m line Dr Knapp coll sold to Prof W M Bord at Borden, 21 and on Mason Crn Coll arranged now by Prof Harry Burles J T Barnes Prin 10th Ward Sch Crescent Hill Louisville Geo R Greene S and of Market Place New Albany Orlando Holts Dept Treasurer to Jan 1 Brackish Would be willing to collect with me Beargrass Prof A C Baldwin Supr schools corals, Mt gm Corner Chestnut & Mechanic Co Jeffersonville Dr Alex W Nettelroth Louisville Baxter Ave + Payne st 2108 Van Buren av Herman H Netleroth Lawyer Young 216-5th Does not know fossils Dr John Octerlony. Ochterlony 1045-4th St, b/w Cafe and St Catherine W G McConatlu Prin Normal School 1454-2nd St Old knows very little: Major W G Davis Sold coll to Harvard, 1542-2nd St. Dr J S Clarke? Amplexio shumardi Hel'drites interactivus Hel'drites sub tubulatus Thecia major Alveolites mi'a jarensis Alveolites undulosus Miller Thecia minor Cystidigillum Mi'ajarenses' Ladipora reticulata. Ladipora viticellata Hel'drites reticulata Hel'drites megaritoma Thecia Favositeo Geo Asherman 44 Arcade Cincinnati with Mr Albers

Large Septuena rhomboidalis Big Creek, Jefferson Co., F. H. Unusually large, Good beds Total width = 6.6 cm. Width of flat part of valve = 5. cm Length of flat part of valve = 3.4 cm. Length of bent part of valve = 2.4 Natural size.

Atrypa reticularis. Usually large. Jefferson Co. J. F. H. Big Creek. Osgood beds. Concentric striae more like Wenonam form = are not very wide. In fact even less numerous than in Wenonam form = 1/6 mm or less. X Calymene masuta. Big Creek etc. J. F. H. * X Cyrtia expansa? D very small specimen. Area curved apparently, Big Creek. Osgood beds. J. F. H. * X Orthoceras. External casts not to be dis- tinguished from A. simulator, but as ex- terior form. Big Creek. Osgood beds Jeff. Co. J. F. H.* Whitfieldella cylindrica-subquadrata. Much more like the subquadrata but with numerous anterior margin, Finest specimens or far seen west of Antichine. Big Creek, Jefferson Co., J. F. H,* Osgood. 28 radiating striae Orthus flabellites Superb specimen. Osgood beds. Big Creek. J. F. H.* Jefferson Co. Olectambonites transversalis. First specimen - Big Creek, Osgood, Jefferson Co. J. F. H.

Spirifer Magareneus, Big Creek. Jefferson Cr., J. F. H., * Osgood beds, 22 ribs distinct from for 26-28 Orthoceras anniceps, Big Creek, Jefferson Co. Osgood beds, J. F. H., * Most of the specimens are distinctly annulated and have low indistinct longitudinal ridges crossing and to the curve of the trans- verse striae. About 13-19 longitudinal low ridges. The transverse strice are a little more distant than in recent Waldron forms. Several of the same type of shells have been found at Wavona in the Waldron shale however, and are Osgood specimens from Big Creek resembles ordinary Waldron types & having only low annulation and close strice. a very variable shell. Spirifer Radiata Big Creek, Jefferson Cr., J. F. H., * Osgood beds, Platystoma Magareneus! One specimen like Fig. 2-4, 5-7. Plate 29 as far as fields in collections are concerned. One has longitudinal strice like Fig. 2-4. Both lean mouth of Platystoma as far as I can judge. Big Creek, Osgood. Jeff. Co. J. F. H., * a little broader & plenter than Waldron forms. Strict practically the same. Ceratopyra imbricata. Big Creek Osgood beds, J. F. H. One specimen with 6 radiating depressed grooves at centre. Receptaculites species uncertain, J. F. H.* Osgood bed. Big Creek. Spirifer radiata occurs also just above Cliff creek at Madison. J.F.H., * Spirifer with radiating strice of Sp. endera and concentric ridges of Sp. Rivzusa, is this the ancestral form of cristina? Big Creek, Jefferson Cr. J. F. H., * Osgood beds,

Illabrum near armatus Big Creek Jeff Co. Desvooded. J.F.H. * See my own specimen Foster + Grighton's Switch Nov 1st one Anwarry & mi. S. Sam Newson's lineer. Desomian R.R. section at station. 2 Sam Walker to map & mi. W. of Newson Anaway's rev. S. of Newson shale N. of Harpelt later, New. + F.Granth 3 Sam Walker Belfield Robinson 1 ½ mi. W. of Pegram 4 Ashland City strike fossils Waldam, 6 Anwarry several hundred ft NE. Clinton fossils 7 John Snell Anaway several hundred ft NE W. of John Snell 8 John Scott. a little farther west 9 Baker's 10 Blidzee Sam Fleming 11 C.F. Hodges Frank Earl S. Tunnel. 13, 12 W. of Tank NW of sugar church 14 W.M. Foreland W. of Tank, Franklin 2 mi. West, 15 Road to Hillsboro. William Penn't Sperry Annie Inman 16 W.M. Foreland.

Fernal Springs Hills thr M. J adrol house 2 miles S wth. 16 Barley Coke 2½ mi E y Brstm 17 Sulfur Spring 1 mi W of " Carol Gittin. Carol Gitten Tnn Fox 18 M. F. Borken, Flys store J. M. Bardner 19 M F Borker Tnn Fox 20 J. V. Sipton at Allistand Jim Sinta jr. (c 21 School home (a Jim Sinta Sr. (b 22 Centerville, Rnd to RR station 23 Section along RR. Clinton NW of Bridge NE of Centerville 24 Plantg undsg's Hill Muntgamory Mill 25 ½ mi SE Swan Bluff Tennessee Mines 26 Tim Duncan Andera Morris 27 M D and Cott Tennessee Mines Sam Turners 1 mi NW of Deans 28 J. D Deans quarry Mrs Rebecca C. Orman 29 Sam Merry Blue Buck & Ugh. Brand's ance stlwt home BlueBkt Tan Bark Hollow - Spring, 30 Terrel Hollnr. - Fogg,

Fig 2 Helicites magadana, conchites 2.4 - 2.9 mm. 3 Helicites interstinctus " smallifom 1.8 - 1.4 1.1 Helicites subtruncatus - Syellia puella. Pegram - Syellia discoida ? Pegram 1.75 2. Syellin Americana Bledsoe Syellia papillata Clinton, Nevam, - Olicia major Pegram - Plicia anion Pegram - Alveolites Sanioritatis. Pegram. - Alveolites betwen Magarensand} Pegram. verticullata - Coenites vorticellata Bledsoe Alex Sam olusky - Cladifera reticulata Bledsoe Ortho, bifora Bledsoe - Cladipena ordinata Pegram. - Cladipena aculeata ? See types, - Cladipena cumpladata} - Anodonta pygmaea? Pegram Calcerla jeflens. Aparulum Pegram. - Cystiphyllum murchisonianum Magarens Pegram - Amphlepus Shumard's Pegram

14.) W. M. Forehands, 1/2 mi. W. of Tanks, Clintm, 10 ft., not exprd. 9 ft., Sinendal, a little like Leips. Plenty fossils belnw. Bradwoford. 24.) William Perritt, 3/4 mi. N. of Hillsette. Black shale; 36 ft. Clayey, Ynr Sil. Limest. wth fossils. 25) Mrs. Annie Duncan. Orthus sulquadrata strophenena, characteristic 5ft Leips. Fale, Sinendal, & blw reddish optra Large Orthus gyrus just belnw. 20.) A ferry S. of Ferovals, Leipers Creek bed, 18) Tann Fix Fossils at Elamsette p. 18. j. M. Gardner, p. 19, Bodkins 6 ft. Leipsen. a Schoolhouse N.W. of Ferovals 5 ft clay fossils;

Kentucky. 1 26 - 34 2 27 - 35 3 28 - 35 4 29 - 35 5 30 - 36 6 31 - 36 37 7 32 - 45 8 33 - 44 9 34 - 43 44 10 35 - 43 11 36 - 43 12 37 - 43 13 - 33 38 - 42 14 - 33 39 - 41 42 15 - 47 40 - 40 42 16 - 47 41 - 40 17 - 47 42 - 40 18 - 47 43 - 40 19 - 46 44 - 38 20 - 46 45 - 38 21 - 33 46 - 38 22 - 33 47 - 38 39 23 - 34 48 24 - 34 49 25 - 34 50 Whites - page 6 ? 6 = 7 9 = 9

1 Paristella favosidea, Hall, Cl.- 2 Pachydrus crassa Hall, Cl. (Stictifera) 3 Ferestella prince = Nvagana Archpt, 4 (Sericocarinatum) F. terunicospth. 5 Ferestella Terrnis Cl, 6 Orthus circulus (Orhijidamella) Cl, 7 Leptæna sericea. Clinton 8 Leptaena (Sturplennas) crugata ? 9 Leptaena. (Stropleodonts)prifuda # St Jen. 10 Hypselinesti & Clinton at Archpnt 11 alba in Nvagana, 12 Strophelodonta puica, Hall, Cl.- St, 13 Spini fe radiatus , Cl. widerange, 14 Gyrea sueta = novdrans Roducta 15 now different from myrria, 16 Atrypa bidens junct. 17 Atrypa neglecta (Plyuch.) state 18 # Atrypa reticularis widerange, 19 Atrypa plicatula ? 20 thermiephurica. St 21 plana concava. St. 22 = What fieldella cylindrica upp. lineal Jen. 23 Wm. intermedia Jen. 24 = Pentaceros elegus, Abundant, 25 x Bncana atignera # Carvorinus ornatus upp. L. Sphf. = Allaeirus vexus Clinton, = Cerorus insignis Clinton = Hamolanustus diffebrus cephalus St? ? St. ? Helichites) Coeritas ? Caliphora florida Trenatperia, Stm & pera. Ferastella elegans 10 24 terunicips orlura, Cranigera vinducta Certus fructostricta Certus fasciata # Strophoparellistrata Spine for bicatatus * Atrypa magna * Atrypa interplicata + Atrypa ovellifera = Platyceras Nvaganae + Ostrveus larmickata in " constrictum concillatum modulation