Field notes, Tennessee, 1901

Kennedy 1901

"1426 K&T" If found, send by mail to A. Foerste Grand Ave. Dayton, Ohio.

L. V. Sevier. Nashville Tenn. State Ag. Dept. Tennessee Indian, Hardin, and Horse Creeks and would like to [illegible] Col. [illegible], at present Giles John Crosman, 9 miles from Savannah. Tennessee - 1901. Savannah - Horse Creek sections. 1. Watson's Mill. about 3/4 mi. from Savannah, about 6 mi. above mouth of Horse Creek. = Paulk's Mill On Savannah & Clifton road. [white rock] 6 ft + clay layers with 2 nice limestone above in the clay. Covered by soil + top of this clayey section not seen. 5 1/2 ft gray bluish quarry stone, like Laurel of Indiana in appearance. Contains: Dalmunites verrucosus, pygidia canum, headless canum, Illacurus ixonus collected. 3 ft. clay blue above, red below with Retzia, Rhynchonelladul-dicensis. collected. 15 in. red limestone, weathering readily. 6 ft. red clayey rock weathering to a clay. 6 ft. section ends at stream level. [red rock section] A quarter of a mile down the creek, at a cave the following notes are seen: 3 1/2 ft. rock, pure white, like quarried stone at Paulk's Mill. 1 ft. shaly stuff. 34 ft. red clayey, and hard limer stone alternating.

2. Turkey creek empties into Horse creek 3/4 mi. above Watson's mill and shows upper part of section very feebly near mouth. 3. Iron bridge across Horse creek, 4 mi. above Watson's Mill. About 25 ft. of rock, white, some of it quarried, belongs to bottom of Silurian section Below the red rock series. Coffee sand rests directly on top. 4. Lick Ford, at mouth of Willoughby creek, 1 mi. above Iron Bridge across Horse creek. Ordinary Willoughby cement rock at Ford. 5. Eastward, up Willoughby's creek, as far as road passes school house, its ordinary Ordovician cement rock lines the creek. In places it is 15 feet thick. Capped by Coffee sand. 6. Welch's Mill = Maddox mill = Old Graham Mill. About 2 mi. alove Willoughby creek. 5 mi. SE of Sa- Coffee sand with silicified tree trunks at base; on 23 ft. white limestone above. Also belo- 2-7 ft. of a rock which may be Clinton. It is hard and flinty. 15 ft. Ordovician cement rock like the cement rock at Willoughby and Clinton. The white rock first mentioned is cracked at different levels. It seems to belong below the red cloey rocks of other sections ac- cording to this section. I visited this section with T. B. Kerr of Sa- varnah. 7. Dodd's Mill, about 1/4 mi. above Welch's Mill. Mr. Ordovician seen. Coffee sand on 38 ft. of white limestone like that at base of Silurian at Welch's Mill. Idee Ross, 8. Sulphur Spring, on Ross & Araldi's place, about a mile above Dodd's Mill, a little N. of the Florence road. Coffee sand above. A = 4 in limestone 3 ft. white clay with fossils in thin limestone slivers. 35 ft. red rock clayey, 5 ft. white rock like rock at Dodd's Mill. This completes section to creek level. alove A, up branch at spring, is some white rock, at least 12 feet. There is any upper of a lower white section with red between.

9. Calybeats Spring, 1/2 mi. above Sulphur Spring, on East side of Horse creek. A short dist. once down the river from the spring are 15 ft. of white limestone = top of Silu- rion. This is overlaid by at least 60 ft. of Lower Helderberg, con- taining large round crinoid- al bodies through their whole extent apparently. Small fossils (Lower Helderberg?) occur just above the Silurian limo- stone. 10. S.E. of Mr. Cal. Blomtis Home, 2 miles above Calybeate spring, along Horse creek. The top of the Lower Helderberg contains the large round Crinoidal bodies. There is a trace of Black shale, nor well exposed, and the Marne gy is abundantly exposed. Cerro Gordo - Saltillo. 11. Cave Spring, on road from Sa- vanna to Cerro Gordo, 1/4 mi. E. of Cerro Gordo. A little whitish clay, resting on 35 ft. red rock, clayey at least. 28 ft. white limestone below. 12. Cerro Gordo. Brown sand and gravel (chiefly the latter) = Coffee sand? 8 1/2 ft. very fossiliferous clay with limestone shivers. 5 1/2 ft. freeb. limed, very fossilif. 3 ft 9 in. Clayey limest. " " 2 ft 4 in. mud clay 4 in. limestone {Merriz cas- 3 1/3 ft. white clay to origin. fossilifera} 2 ft. massive indurated clay bed as at Rize Mill 26 ft. red rock, becoming more clay at top, but turning to red and fairly solid near whitish limestone below. 32 1/2 feet white rock 10 feet not exposed on account of high water. 13. Saltillo 1 mile S. of town, on Miles creek, at site of old mill, 1/4 mi. West of river is abundant Ordovician ce-

ment rock like that at Clifton, It slopes strongly eastward, and at the river there occurs plenty of white limestone with a little red intercalated at base, which is probably partly Roemer's bed. At the Landing a well 50 feet deep struck plenty of Black slate, and apparently lime rotten phosphate rock; depths unknown. [illegible] mile site, only whitish limestone like that along the river above the mouth of Wiles creek, is seen. R. S. Dany, Saltillo, has his all about Sherman ville blades. J. S. Holland went along with dany on Saltillo visit. Clifton and Glenville. 14- Back of At and below Landing. Cliftin. 2 Roemer's 2 wh clay soft red clay or shale 16 1/2 ft. red shaly sluff with some hard clay or 4 layers and 15 1/2 ft. soft red shaly rock, estimated at 12 1/2 clays 18 ft. white cracked limestone, estimated 12 1/2 solid L. 3 1/2 measured 3 15 B 2 1/2 C G D 15- Glenville. Roemer's 2 wh. clay, red clayey concret & ligne-stone 22 1/2 limestone rubble and solid 21 1/2 lowest red 2 layer clay 1 1/2 lime- stone 3 1/2 hard lay 1/2 soft red clay 1/2 hard L. 1/2 soft faintly solid faint limestone. 21 1/2 more solid shelving soft red L. Bayard 12 3 3/4 limestone 3 3/4

At Clifton Landing, the Clifton is underlaid by 16 1/2 ft. 16 1/2 ft. of Ciu. Brmp and (illegible) 22 ft. of cement rock (illegible) A Roemer's bed at Clifton, Astylospangia praemorsa. stellatum-sulcata incisv-lobata imbricatv-articulata Palaeocrinus crater Astracospangia anomicros Famites farma as figured by R. Famites Gothlandicus. Fig II. '' discoidea. '' fibrosa Heliolites interincta. Thecategites hemisphericus Cyathosphyllum Steenwardsi. Finestella anticostata, Laryocrinus ornatus Platycrinus Tennesseeensis Saccocrinus speciosus Cystocrinus Tennesseeensis Artius elegantula fossiflica triloba Leptaea nleambvidalis Spinifer oligoptycha. Atrypa reticularis marginalis A Clift, Wilzonia Wilsoni. Pentamerus galeatus spiny Calceda Tennesseeensis Platynoma Magarensis Calymene Magarensis Sphaerexellum mirino Maerus barrieris Aler Spinifer fagoji, Pegram tyho Spinifer simplex, very small as at Bledae. Spinifer becoming simple towards margin, Strphamera long hinge line, small form, ruleaa mm. Artus, new species of Hall from Tennessee, Encrinoorus Alvedites large openings, Heliolites subtrubelatus Padcydictya same as at Pegram. Petraia Waygenussis. Petraia Farreinganae. Cyrtia arecta, not arched V Spirorbis Callipera elegantula.

A. at Glenkirke, (not found) (at Clifton) Daburgua caudata, Atleyiis tenuida Lampterocrinus Tennessee; Callyporq elegantula Theria Swinderana Rhynchonella Tennessee; Cladipora flexilis Plasmospa, B. Base of Laurel, Top of Ozgord at Clifton, Stephano crinns Ozgordma; Pizorizinus genusiformis. Super-top of Stephulo-crinus. C. Crinoidal bed in Ozgord, Clifton Lituites. Very com mon. Ithydithes Dlaerius commune Cyclacrena '' Artlercas very . Platyceras. Pizocrinus + Stephano crinns are found within 2 ft. of Clon- tin in the Ozgord. Atrypa reticularis in Ozgord. Caryocrinus found within 2 ft. of top of Ozgord. D. Clinton at Clifton, Platy striphria lafonata?male Arttuis elegantula Atrypa re-marginulis Atrypa clinton corrugate fem. Plectam limites sericea Tripleria Arturi Cyclonema lilix Ilaerimus Daytanensis, Favrites favosa Halysites cataractatus Included from Cardo- vician at base = Rhynchonella capax Artleis sub-quadrata; D. Clinton at Glenkirke. Tinged with Ilaerius Daytocrassus salubrynn glabello, or more light trim and whitish. Cardavician just bel ou Clinton at Glenkirke: Rhynchonella capax.

Bronsport Furnace, 16. S. Y Bronsport Furnace, Artlerceras amygens occurs in red series, 15 feet below base of Roerner's bed, at 2nd glade. Hill S. Y Furnace, Top free of 84' Colorado, angle of dip 60° 17. On road from Vices store to Furnace, its large round Favourites new species, grows 33 feet above the variegated red bed. 18. at Mamor Slade along road from Vices to Perry- ville, it is 50 ½ feet from top of the red rock to the top of the very criminal layer with Centromatites Reinwardtii 19. at Mamond Slade off the road, it is 63 feet from bottom of creek to very fro- miferous bed, and 93 ½ feet to top of hill. The Furnace at the Landing was erected in 1839-40. The Furnace at Bronsport Furnace was put up in 1849. therefore after Roerner's visit. Mrs. Hettie Fisher Decaturville Mrs. Ellen Allen Decatur ville, Mrs. Anna K Mc Millen Between Decaturville & Buckners Mill, at Ellic Fisher & Mrs. S. Y Sulphur Sp. From all about Roerner's view to.

Perryville. Photo, Mrs. Mary Young. Perryville, Tenn. Judge Head of Chicago. Head of Double Sisters Island to Shannsville or Bobs, west side of river. 20. Perry, NW corner of town, 8 and stake at fence level. 1½ ft Thin limestone full of brzyans and other Lime Welderburg fossils. 14¾ ft. Weathered to richly fossiliferous clay, 16 ft. {2 ft. fine grained blue limest. 3½ ft. At top is Encalyptoviri- nus but flatter, also flat Strophurella corrugata, rest of section not recorded. 7 ft 3 in. Crinoidal zone. 6 in. Cascinium Layer 2 ft 10 in. Top of layer full of Orthin obllata? Encalyptovirinus crassus at top. 4½ ft. Rover's bed. Coarsely Crinoidal fn, 1 ft. at top. Perryville + Linden. 21. Perryville, Amarry, N Eastum. 8 ft layers partly exposed, 11½ ft. 2 after than rock below full of fossils. 10½ ft. solid crinoidal lmk Astracopangia americanus. 22. Linden, 1 mmi. N, est Mr. William H. Patton, 6½ ft. Black Shale 1 ft. Sandstone. 19½ {6½ ft. not exposed {7¾ ft. more shaly beds very friable {5½ ft. solid limest. massive. Rover's bed. 17½ ft. Spring at house. Near lower end of stream the top of Rover's bed is 52 ft above the stream bed and contains Astracopangia americanus at top, Collected. Also Stellation- sulcata. Chas. Diggin, Culp, Tenn. wants Photo of derrick.

23. East of William Birdwin's house on hill side. Opposite road leading from Short creek into Corn creek road, Black Shale. 18 in. Sandstone 88 ft. Rovenor's bed. Conchidium anypino? within 10 feet of base of section. 24. Up Corn Creek, 1 mi. above mouth of creek. Above John M. Birdwin's house. At spring on S. side of creek at foot of bluff. Black shale 3 ft. Dark blue carb. sandstone, 1 ft. Black shale, 1 3/4 ft. Sandstone, 72 ft. Rovernor's bed, 25. 26) 1 mi. E. of Linden. Up Short creek. N. m. road side. 4 mi. Mr. J. J. S. Journey's home, Black Shale 2 ft Sandstone 11 ft. Lower Helderberg. Rovenor's bed. 27) 1/4 mi. E. of Linden. Up Short Creek. At forksof where Jack's Branch comes in from SE and up that branch. Near E. Duncan's house. (tenant) 3 in. Blue Sandy Rock, 2 ft. Black Shale 2 ft. Sandstone 18 ft. Rovernor's bed. 18 1/2 ft. Abundant coals. Bottom of section at spring in Short creek. 28) Webb's Mill. 1 1/2 mi. S. of Lin- den. Rise Mill. Nodular layer, 4 1/2 ft. Black shale, 2 ft Sandstone. 65 1/4 ft Rovenor's bed. 11 ft. Reddish Rock - Variegated bed

28 Cut, Astraeaspis ensicauda is found 16 ft. at the top of red rock, above a 5 ft. in- durated clay layer. Massive looking but spalling off ir- regularly. Cumberland City, 29 - Along RR West of John Bradus house 3 mi. S. of Farm. Just N. of crossing of main county road th Erin. In ascending order, going S. towards the crossing. In a cut is a thick section of the Clinton rocks of Chipton= Ordovician: badly decayed and recently reduced to drab stuff here but better preserved at one point along the RR almost 2 mi. from farm. 22 ft. White limestone, Clin- ton, like Dighton limestone, upper 12 ft with chert layers, Lower 10 ft massive. For- writes favours in an erratic part. 14 ft. Soft red clayey rock = As good, More whitish at base. Thickness may be 19 feet but there is probably a cause faulting here. 7 ft. Red limestone, with Stephano- nus Cypri-densis + Pizo-crinus gemini formis becoming less red + clayey above!

2 ft. limestone, slightly crinoidal 3 ft. reddish clay. May be thicker, if not faulted. White + much cracked rock like some of the Roemer lime, stones and some J Laurel also. The grade seems along road at John Bradus in an E to N direction. Fortier S. is Niagara (Lans- ville?) overlaid by Lower Hel- derberg (fossils) and still far- ter S. is Silicenus Group. Black shale not exposed here. 30) East of angle of Public road to Erin, E of John Bradus' homse. Black Shale is seen up a quaggy in the N side of the little stream flowing westward and passing just S of John Bradus's house. Under Welderby fossils, thin section, as at RR cut, 169 ft. limestone, Astraeopagia meniscus near base. Very flat Favorite favros about 3/5 way up. Faulting may have increased the section here. 20 ft not exposed. 32 ft. Layered red rock, pretty well exposed. Massive-- ? Massive red limestone, dense and red, like some below the red layers at Chipton, but red instead of light red. B one not exposed here. 31. Christopher Schmidt: At old Furnace on SW edge of basin. Black shale. Also limestone exposures. The latter contain peculiar fossils. Faulting in here. 32. Dr. W. B. Scott. On western edge of basin, at about the middle of its length. Here the various sponges were found in the regular Roemer beds. There overly soft red layered rocks and hard massive limestone, correlating the John Bradus section. Below the red mass- ive rock, south of the house, is the Osgood with the Ove- crinus + Stephanocrinus,

32 cont. Rushing's Creek. & mi. S. from Big Sandy Station. On Brick horse farm. Bluff nearest me, 15 ft. with plenty of fossils (Lower Held. ?) 250 yds. E of horse m creek, Road runs by a stable to the bluff. Reported as above by a farmer. Not seen by me. 33. West of town, along the river, Black shale is exposed. The Lower Helderberg shows ammonites and fossils. The massive red rock be- low the red clay section is faulted up against the Lower Helderberg here.

Stop - * Lobelville. N. Berry Cr. 4-5 stores. Look up A.W. Dodson for board. * Beardstown, 7 mi. S. 3 stores, B'll Edwards. * Farmers Valley, & Cold Bluff, John Wiley * Flat Woods, Dr. John Haggard. * Forty eight. Tennessee River. Waterloo- Hotel 1/2 mi. from river, Riverton Hotel 1/2 mi. from river. Eastport Mr. Walker. 1 mi. off p.r. line. Bookeer Woods on West side. The Red Sulphur Springs Hotel is 3 mi. off. Pickwick. The White Sulphur Springs Hotel is 1 mi. from landing. Steam lines Sept. 15. Hamburg. Finest place in the world. Bed bug hotel. Pittsburg Landing. Store. Boarding house. Mrs. Cleambers, Crumps. Right up on the hill from landing is dwelling house Mr. Luder. Savannahs Hotel - Coffee Landing. Good place. Big store. Digges on West side. Can stay. Cerrv Birds. Two stores, Mr. Weller is best. Mr. Martin. 1/2 mi. beyond Batt Springs. Near the 5 mi. post turn to the left. Hinden 1/2 dollar ferry, if rig is used. Telephone to Hinden for rig and state if you leave trunk. Berryville & rd hotel. Wells store. Can stay. 0 B's transport. No st Sleeping place. + New Era Store + 3 dwelling houses. Lego. Dr. Strickland. Peters. Store. Sick. Duke N. Blackwell, Bobs. W side. Store. Can stay. Bluffs for 2 mi down river. Swallow Bluff. Store. Can stay one night. Altiller. Mrs. Clark #2.00 Clifton. Squire Haggard. Visited by Head and Harris. Johnsonville to Birdzing Creek. Mouth of Big Sandy. Good. Mr. Buckingharn.

Mrs. Milligan, great collector of Ten- nesse Waspura fossils lives at Jacks ville, Illinois, about 20 mi. west of Springfield. Ordovician exposures occur on Horse, Indian, Hardin + Beechcreeks xxx On upper part of Beech creek, not more than 4 mi. from Waynes- boro is a path fit and thus one met with in the same stream as going towards its mouth. Cliff m 15 ft.. calcareous shale, 23 ft. fine limestone, Rhyrch. capax dentata Colom. stellata 70 ft. Orthus bed, smooth slays and clay, Variegated bed. occurs on Big Sandy, at local done. S within Henry Cr Birding week Benton Cr From Helderberg, White Sulphur Spgs. S. Hardin Cr. Commencing at a mi. of Big Sandy upstream for 5 or 6 mi. in Henry Cr. S. Benton + in Decatur. 30 ft. at Beardstown, or rather 3 mi. below it. better. Black Shale & Merius can beds seen. 2 mi. al me mi. north of St affals.

839 Williams Mill, 5 mi. above mouth of Big Sandy. Henry C. 50 feet. Cherty beds with fossils: Oniskany? 840 Tributary of Birdsming, S Benton Cr. like last. ~ Oniskany? also? 841 White Sulphur Spgs. Establishment or upper Weld. Chert with fossils. About 1 mi. from Spgs. on upper site side is bluff 2 mi. long, with Lmr. Weld. at base. Cherty beds = Oniskany? 842. Buffalo River, Perry C. 843. Nix 844 A B G ant. Indian Creek, 14 mi. from Waynesboro, 22 ft. Savannah. Silicified fossils, 10 ft. Holo. 845. Craven Mills a short distance below Gants & W. Helder. 35. Meriscos, two forms: ledge at Craven's Mills. 65 ft. of limestone with Meriscos. 20 ft Variegated, also well seen at Craven's. 846 2½ mi. W. of Gants; bed, 25 ft. filled with corals, 847. Hardin C. Col. Smith. 9 mi. from Savannah, on Waynesboro road. 20 ft bed. tec in any, 848 Bath Spgs. S Decatur, 20 ft bed fossils. Meriscos film. 29 N of RR bridge N of Riverside Tenn. at base of Laurel = 1½ mi. Ngabens Creek. Holozygites, 4 in. long. species unknown Diacrinites gemmiformis, common, Oithroceras large forma. 29a Variey with cherty layers. 11 ft + 8" sandstone, firm, range of fish remains throughout. The replicatio in ripples along the base, a one of thin 4 in. lms. 8" siliceous cherty stone, occupying position of black shale eastward, a new idea for me. 8" Nix. L. badly weathered, crumbled to a clayey limestone mass. 5° W massive limestone, traces of reeds; 10 10" lay. 6" white limestone, 2 ft. crumbling, with Oithia filosa. 10 2" covered. Probably clay. 36° 3" limestone. Strongly reddish in some of the layers. Among others at the very top. The upper leaf more massive. The lower leaf after + weathering back. 4° Gorgon? Bedded in rather thin courses, with a few thicker course, at the base. At the top is 2½ ft clay with in conformity between this a bed above = Laurel.

5°9" Crossbedded chinkm, at present very f[illegible] in places. 5°9" greenish Ordovician clay ac. finally exposed. clim up with favarites favorn? flat with corallides 3 mm. across, Habyrite catenulatus dicranus ambiguus type, (Legrand?) 3D. Ordovician W.M Harward's on road to Trace creek, N of Buffalo river. 14½" Clay 8° weathered clay limestone - Mr pressic at least some 6 mm. 11° Fossiliferous weathered clay rock. Fossils chiefly in upper half. 32 Mt. Ed. Walker - on Tucker Branch road. 50¾" Sandstone, greenish = Warally 8" to much finegrained rock full of discophute nodules up to 7" thick, 1° Black shale 4" Sandstone. 1° 8" Dark shaly fine grained ark with Lingula subsquata. Takes the place of the phleplate rock at base of section at Pegrambridge. Further down the road at a spring & farther Sandstone = Warally + phleophate nodules. Black Shale 1° 8" Shaly rock. 7° Fine grained sandy rock. This can hardly be Silurian. It does not show evidences of layering. 3° 8" clay. 10° 8" clay rock spalling. B 5° 9" Calcareous clay Fossils. 5° 6" limestone, upper part is a shaly lime stone. 3° covered 3° limestone. B = Favarites Forbesi, Dicranus Clifton pentagonus type. The Roemer bygogram, lim spider's disc abraded.

33) Waverly No.2 and strata. 1° Black sandy massive, =Black shale beds, 2° 6" dark rock, sandy } =rock films 1° mica shale 3° dark rock, sandy) Bladestalk level. No phosphatic nodules or genuine black shale seen. 34) At Old Mill, Mill Creek. 6" Sandstone like blmn, phosphatic ind.=2in. 5° 2" Sandstone =delaying b.lmn (Black Sh.) at top of Niagara: The conegites hemisphericus, Byf. & R. Roemer? 44° 4" Limestone, which if it soft, I could not with certainty identify, by any of it as variegated, Or white and not studded in my, at top. Just below mouth of Mill Creek is cliff 75 feet high, Tor steep to climb except at aids. Not visited. The brim sandstone layer belong- ing below the Black Shale is exposed from 1 mi above the mouth of Owl Creek along the valley of OB by Coppermine Creek as far as other OB by- Buffalo River. Up Owl creek it is fol- lowed ½ mi, to a small water fall. Silurian section does not exceed 20 feet along those valleys, Only Roemer had seen. 35) On road N of Buffalo between Big Depression & Hype Creeks. Sandy rock delaying blmn Black Sh. 25° Silurian section with Astraea sp., mja, meriacus The conegites, hemisphericus Arthur, with varying ventral lobe elegatula species, var. of this. Conophyme elegans? Streptelasma large borealis, Pterocrinus genini /primi?/ large Amplexus shumardi small. 36) W. of Dr. Carvens, ½ mi. Waverly 1 foot greenish ss with plants of phosphatic nodules, about 7 feet of SS delaying blmn the Black shale. Silurian, Roemer's beds.

37) at mouth of Little afensom, NW of Flat Woods. Wavely. Nodules, pleophatic in Sandstone. 90'6" Sandy rock takes place of Black Shale. Silurian with Oliva maj'n at top. 12° below Astraea mya menicns 90' belw top - Coral with flat rach Total Sil. on section exposed is 48° above Buffalo River. Wavely 2 ft 2 in chiefly shaly, phosphated, in upper 4". 7ft solid massive SS, Silurian No Lower Helderberg, W. F. Pate, Versailles, stayed wth J. C. Whittaker, lives NW of Flat Woods on road to Buffalo. Palaeonema ratera found by Mr. Whittaker in Tate Hollow, 50 yds from place where road forks going NE. Still's out from Buffalo River. 31 = 8) Special Cothran. E of limestone bluff, Wavely, 2 mi SW of Trace Creek. 90 Sandstone. Nodule layer at top. 4° Laysrock spalling. See section 32. 60½° Limestone rock down to where the line is covered by waters of the Buffalo River. 36° above the Buffalo river there is a bed that weathers away back. It is a soft limestone. The variegated bed delays below this level I think. Petrified Tree. Pine logg Hill - Grave gard. Between Rutherford and Horse Creek. This place is called Lutts Post Office. Tree is found in road beyond the post office going towards Waterlrr. Petrified Tree. 7 mis. N of Cypress Spr, on head waters of Weather- ford Fork of Indian Creek. On one of the forks. On Jack Mar- tin's farm. In hollow below his colm in his field. NE of Whittony Stand? S. of Victory Spr.

2\frac{1}{2}^\circ Banditank, phosph nodules in yelb b. 2\frac{1}{4}^\circ White limestone, NW of 5\frac{1}{2}^\circ Covered but at top with white crystalline layer 22\frac{1}{2}^\circ limed m., most p. a clayey massi 77. 16\frac{1}{2}^\circ limestone, white, well bedded. 54. 10^\circ Covered perfectly white & soft. 38. 12^\circ 6" limestone, white, well bedded, but distinctly bedded. 8^\circ 5" did limestone. Rather massi 16. -6^\circ 6" Massive, 2d limed m. 7. 1^\circ Iron stuff, du Clift section at the Clinton level. 25^\circ -20^\circ unknown. End or clay? Doulful thic 48. 7^\circ Leiper Creek bed, = Richmond, Cement Rock, artins emacerata 41) W.D. Helton. About 3\frac{1}{2} mi. NW of Waynesboro on Beech Creek. The Cement Rock comes off and on as far as when Big and Little Beech creeks come together. 42.) Six miles W. of Waynesboro. About 1 mi. W. Main Hardin Creek, up Brewer Branch where road to Martin's Mill crosses the land & goes up hill. Wastly, 5\frac{1}{2}^\circ Dark blued shale. 5\frac{1}{2}^\circ Covered. Iron part limed stuff. 11^\circ SS. replacing Black Shale. ? 20^\circ Clay+ limestone with Thecystegites Hem limestone in creek bottom. 6 mi. from Martins Mill. 45. Dr. G.R. Yeiser E of house at road cross. About 200 yds N of Indian Creek. 80^\circ 6" SS. replacing Black Shale limestone, full of small hyozoans, W. of house. with Lingula subspatulata. 5\frac{1}{2}^\circ Shaly stuff dark limnish blud. 9^\circ SS replacing Black Shale clay + crumbling thin limestone with Disthaeospongia primissima, Macrodus Stricklandi.

Free D Atylopyra praemosa, stellatum etc. Munita tumida way up. Munita Saffordi C Thin carboniferous limestone. Rhynch. Saffordi. Meristella, clay ate Rhyn. chamelloid prima et Waldenii. Liptrochia. M. militaris Rhynch. A little like Pennsylvanian. sensi. Eypidula Roemeri Rhyn. aspleni Nuculapina B Fine grained limestone. Strephomena pulchana. Uncomalno Strictlandi. Rhynch. suspecta Nuculapina, Eypidula A Coarse grained limestone. Rhynchomella Saffordi. Calyptrea. Stroph. jeaterata Rhyn. Strictlandi common. Specificer Saffordi? Callspora elegantula Dalman to apparently with only an angle at top of tail projecting, Stricta sulplarma Walderndii Stroph. elegyferia with very strong terid. Strictaform Sulby? Dalmanites long spine slightly frontal projecting 46) NE end of Martins Mill, in Tenn. SS replacing Black shale: 14" limed nu. Saffordi mtilida tumida D 28' 9" Bluish shaly, tutiloite, tumida to BCB 50 Coarse SS, A 57" Grad to coarse conglomerate. Roemer Base not seen here. 45') Admissa from Cravens Mill. 5'10'' SS, replacing Black Shale. todo 32 22" encrusted, Inner part bluish c. thinn 9'10" Massive Coarse SS, 55" Roemer bed. 44" Variegated bed. Larger with lines of one, Not the reddish massive limestone.

47 1 mi. down from Martins Mills. 60 SS replacing Black Shale, at least 6. 40 60 2i Crase SS. Romaine Just below the SS replacing Black shale was found Asterophyngia incisa lobata. 48) At school house E of Grant plan but further joint mapped, the Pseudo Limestone, crasse limestone + overlying orthocoral limestone form a massive wall. The rouble (sic) limestone are being more massive than. Beneath the pseudo L.H. the rouble recedes. The top of the Romaine bed is also crasse ground and in places makes a vertical cliff with the underlying Pseudo LH etc. Views recorded 1.2.3, Abt. J.T. Herwin Abraham Lincoln. Silliey's Mill on Horse Creek Hardin Co. Head of people at two (sic) hand Romaine Height of Jewels height = access between Romaine & pseudo L.H. Massive = Pseudo L.H.

14) Clifton Landing, 6° clay shale to top of Clinton. 9½° Shaly beds, clay, 5 feet & in., harder. mine bed not very hard. capax, Steph. like Philtexta and com + coarse like that follows with Rhynch. 6° mine clay lined in. Some fairly hard 3' 6" to top of coarsest limestone. 9° 6" to lowest Simpsoniana filtexta? 5½ 3' 4" Warren bed, chn. Plate 12, George Pitts, Clifton Tenn. Colored. at the Cement Works Rhynchonella capax was found at very base of Richmond crance limestone, above about 4-6 inches of Warren bed. This led thing out northwest = W. There is no conformity between Warren bed + Trenton. The Warren rests on rock 2 feet lower in the scale at E end of landing than at W. end, 122 mi Johnsonville 10.49 Olmos. mi Newsom 12.49 2.04 Johnsonville 2.53 Union City 4.48 Union City 7.52 5.21 Cair 1.13 Tamms 3.00 Tamms 3.42½ Thebes Frid.

Clifton sh. 15½ ft cl. 19 ft 3½ ft ? Trace Gule sh. 33½ ft + Wagnerdies sh. 26-25 ft ? Drk. c.l. 7 ft ? Bazadets Clifton Lick pond, M loughly Creek 15 ft + L Maddry well L. Saltville Glenbeader Chamberland City Centerville Leipers Creek White Oak 841. White Sulphur Springs Establishment on Held. Masses of chert with fossils abundant in surface. Section opposite Springs = Hill above bluff. 4) capped by sand + gravel - ferrug. conglomerate. 3) Siliceous Gr. 75 ft. 2) Black Sh. represented by SS, with slaty seams 3 ft. 1) Bluish l. abounding in chert nodules and layers. All fossiliferous, with thick bedded layers at top and base. 63 ft. About a mile from the Springs on the opposite side of the river is a bluff, 2 or more miles in length, at the base of which the Helderberg rocks are exposed. It may be that the section above described is on this bluff, opposite the Springs. 844. C) Near A.B. Grant, Sixty fossils. 845. Section A.B. Grant to Graven's Mills. Grant bed described as Helderberg Limestone. * 846. 2½ mi. W. of Grant, 10 feet blue-black shale is bed 25 ft thick well filled with Niagara corals. 847.S) Col Smith, 9 miles from Savannah on Wagner's road. Fossils from bed about 20 feet thick (at & county!) 848 D) Bath Springs, Fossilized zoft = Held.? Ledge of hard l. 3 ft. thick. Slaty limestone 18 ft. Merriam's, variegated l. at bottom of bluff. { White Sulphur S'gs Hotel 1 mi. fr. Landing at Pickett. Wm. Martin, 2 mi. beyond Bath Spgs. go 5 mi. past turn to left.

C. S. Smith. 847 Amizophyllum Agassiz. Nucleospina concentrica Rhyndaspis frumna Bath Spgs. 848 Amizph. Agassiz; Aeicystites Anna. Spirifus Suffredi. Nuclosp. concentrica Rhyndaspis globosa Rhyndospinafrumma. 817. Nearly 4 miles from river at Clifton caps ridge overlooking Eagle creek. Silicious grp. partly concealed, 53 ft. Black Shale (Waverly here) 50 ft. (34 ft thick shale, 8 ft finegrained SS in it, Gingula sulspatulata, 8 ft massive SS) Lower Helderberg 25 ft. gray crinoidal, fossils scarce at this point. Merrizous l. Spruge bearing bed 90 ft highly fossiliferous (Where measured. Was this measured on Eagle creek? Variegated bed (includes Os good + Clinton) 96 feet. Merrizous spruge bed first all measured 4 mi. E of Clifton, and Varieg. at Clifton. 835. Lower Held. in valleys of Dunstan and Hardins creeks is generally wanting, locally in thin beds. Low. Held. absent in upper part of valley of Buffalo but on map begins at Flat Woods and goes down to Linden. Bell no drill at Linden. Black Shale Linden. Lower Helderberg. Loaded with fossils. 842 On Buffalo River in Perry county, F. Frazz. 835 3 miles below Bearstone on Buffalo R., Black Shale. Bill Edwards. Lower Helderbg. 30 ft. loaded with fossils, Merrizous bed. Four miles above mouth of Buffalo, by a local swell, it is exposed in a Bluff. Lower Held. 50 ft. Nearest place is Bakerville. Nearest land- ing is Cuba. Good Stopping place. 2½ miles, not far from Dudley's Ferry. Dr. Whitfield. Mapped from edge of Hickman to Mentgnercy well on Duck river, but not in Humphreys on Duck river. However it states in text; — Lower Held. along valley of Duck river scarcey reaches Hickman Co. Decatur Co. 831 In the southern part of Barton, well developed at a number of points. L.H. 840. Tributary of Birdcagle in southern part of Barton Co. 836. Low. Held. Commencing at mouth of Big Sandy and extending up valley 5 or 6 mi; 839. Williams Mill, about 5 mi. above mouth. Orange sand + gravel. Lower argillaceous masses, fossils, several layers of gray limestone. Black shaly limestone, 50 feet.

Quarry, Taylor's Quarry, About 1½ mile east of Iron City, on the north side of the Railroad to Columbia. 3 inches broad Heavin well bedded Wavy with layered lean, 5½ ft thin. Ledged wavyly, shaly, arched at Phosphatic nodules 10 inches greenish shale like Wavy face at Mt Pleasant. 6 in. genuine fossil Chattanooga black shale. 15 in. layer of greenish fine grained rock = equivalent of Hardin sandstone, 6 in. shaly rock, weathered to deep brown, also belonging to Hardin sandstone. Unconformity distinctly seen at quarry, on Silurian. Rock" massive layers, 13-18 inches thick. About 10 feet exposed here. Rock contained 6-7 specimens of Pizocirrus genus formis and Large Orthocerat. At first crossing of road over Railroad, about ½ mile E East of Iron City, the total thickness of the Silurian is 5.5 feet. at least is 1 foot of coarser conglomerate. 1-3 inches. Rests upon a bluish fine grained limestone in thin shaly beds. Quarry, 1 mi., N of Iron City, on west side of RR to Columbia. A 15 inch layer of greenish fine grained rock B 6 inch. brown, shaly rock, weathering back. Unconformity line distinctly seen at quar- ry, black slate Trip. of Silurian. C Rock massive with Pizocirrus genus pluriceras (1) many of them; Orthocerat but not any found. Rock in beds 13-18 in this thick. At south end of quarry large is seen in Chattanooga black slate - 6 inches. Wavy like rock. 16 in. brown ledge = Hardin? or Wavy? 9 in. brown shaly, shaly rock like above. 19 ft. This is the quarry stone of last week, 1½ft. Clay shale 5 inches limestone 1 ft clay Walden? 23 ft. in world limestone layers white except within 3 feet of base when it is often red. 3 ft 3"/2" inches shaly rock. 2 ft 8 inches crossed bed ferruginous slate. Orthocerat and Marries.

Cedar and Clarks ants. 3 in. to 12 in. Clinton chert (Favorite farm 2 ft 6 in. ferruginous limestone. 6 in.} hard lined beds with bed joints. 7 in.} Ooliticambrites? Softer shelled clay rock, nearly clay, corresponding to clay arch at Mannie's 15\frac{1}{2}ft down to creek level will resemble inch Clinton Favorite farmoz globular mass 3 inches in diameter. Pentamerella. as at Riverside. Triflesia artica" as at Clifton, Large attuid shell as at Clifton? Dlaenus Daylanceus's, Zygdenticus calyculus. Bellerophon species, top of lower bank septaria, sleuthridalis, bryozoan. Horizom inarticulans, at base of cliff north of Cedar Pt along the railroad. Spiriifer large, Devonian, authority in sectum to correspond. Did it come by train from some source of limestone for our furnaces? Waldron Hyolithes like Newson, Rhyndocheria and two species not yet identified including crithoids. Top of Ordovician, well tested limestone. Dinottina sub-quadrata. Rhynchostoma mannii Strigilamera planumalma Stiphromera plaurdmeta Mannie clay, Rhynchostoma mannii. Califera Brasferia quadrian gulos, ? Waldron bed ? Orthoceras annycus small, Atryka reticulans Crones. Olecton. brutes small as at Newson? Stphaurisimus gemuniformis? Atryka dispearlik nut ans. Spindja endra (Rhyndocheria) swax Lorkup Ddlerandula elegantula, Septamentum indicali large Secanocrinus Above Waldron bed a road to Taylors gary? Steflo crinious P. zerrimus gemuniformis. Pizorimus pentagonal form?

Friday PM 10 Train at Dayton. Saturday M 11 Iron City, to Taylors Amarry, Sunday 12 Iron City to Cedar Point. Monday 13 Iron City. Out depot exp. to Waterloo. Tuesday 14 Waterloo, Brush & Bluff Cr. to Riverton. Wednesday 15 Riverton to Pickwick, E bluff. Thursday 16 Pickwick, E+W. bluff. Friday 17 Pylburn Top LH, Calybeate Spgs. Saturday 18, Savannah, Col. Smith. Sunday 19 Savannah Monday 20. Savannah, Bath Spgs, Swalim Bluff. Tuesday 21, Small nr Bluff. Wednesday 22. Small nr Bluff Slifton, Legr. Thursday 23 Legr, New Era Friday 24. New Era, Kelley, Bakerville, Saturday 25 Bakerville, Sunday 26 Bakerville, Cuba, Steamer Monday 27, Darrville to Cumberland City 5/2 Tuesday 28 In bed. Cumberland City, BD84. Wednesday 29 Sat around hotels Cumberland City. Thursday 30 Collected Cumberland City, Annie Friday 31 Cincinnati. Pylburn bluff opposite Pickwick; x, Bluff creek. 1. Most southern bluff,<Shot Hollow a. Anderson branch b. Johnson branch. 2. Middle bluff c Boyer branch. 3. Pylburn bluff proper, Harris, Leeth, Pickwick (dam). Eastern 1. At west southern end of bluff, next to Bluff creek, at base of section = A-11 ft. ssive to top of first set of sand rock. Very fine ground limest one with much dust. One good connecting Carrarovi- nings at top. Caraverversions at all levels. Collected. B,- 13 feet Carrarovers very good at top. C - 16 1/2 ft. Fin would see next row 30C + 19 ft to bony fossil limestone clay, led 1ft thick. My C+ 50 1/2 feet to black shale loam 3 in. 20 in / 2 sandy ohg shale = 4 in at bottom hard. (4 in soft. 12 in 2 andy ohg erik). large Dalremusite py gidium mined from lo, thin through out this section, 17 1/2 ft below top is lighter sandy loam with plenty of

C. along upper part = Meristella? meris. Strophoranita Beckeri. The large crinoid found by lady at lowest. Another very profiferous closely bed 6 inches thick is found at top of C. Camarosi- nus, spred, Olenardi, Sympentle- matium, Orthotetes nodonthanus. Leptaea rhodolpidali - cral with flat base like Carrostes Forbesi, Favosite with convex base, Atrypa reticularis. Spiniferina cycloptera crane zigzag species, with large cardinal areas. Spinfu with about 3 or 4 lateral publications and radiale striae, distinct. Spinfura. probably cycloptena. Black shale 9 in. Camarostoc clint & spinifer collected rock = 5-6 ft thick, with fossils. w. 72½ ft. Top of Massanuda. Massive clasts above. Dives. Stroph. muller fernith lifeless crinoid. V 57½ ft top 16 in new, possibly large U 57 ft. base of very fossiliferous layer. T 50½ ft soft dark cinced 33 ft). 19¾ ft little S 42 ft large Camarotocelina exposed. R 33 ft solid, cement me. Camarostinus at top River. Section at east end of bluff. Black shale lwrzn. Possibly above? 50½ ft. C - 16½ ft. B - 23 ft. A - 11 ft. 101 ft. Top of R = Camarostinus. Str - lecheri. Spinifer cycloptena. Large crinoid hole at lowest. Stroph. punctulafera? Olenodictyum. Camarostinus 42 feet below massive bedded 51½ feet below Black Shale lwrzn. 72½ 6.1½ 21 feet 23 feet above top of lower bluff section. Carnary crinoid 42 feet above bedded with favosite fauna. Crinoids at largest at base 50 ft to top of massive bed. There is a crinoidal layer at top with spinifer cycloptena. Spinophyta in black shale

John Henry Johnson, 7 miles east of Savannah, Biscaypint bed faintly exposed with Microceramus Plutagnus form, etc. Col. Jim Smith. 9 mi. E of Savan-nah. Strike in front of house between house & road & along road: Brown limestone, across Boone Creek S. of road, 1/8 mi., limestone clear- more solid limestone above the clay, fossils forms beds. Above is sand & gravel. No Black shale or Waverly kept along road so far east due to Cutacens & Tertiary erosion, Belongs to John Boddin now - Col Smith's place. Hagler Mill is in Buffalo river, Bluff on east side, about 75 ft high, cross river at the mill = ford. About one mile and a half below Baker ville, about 5 miles from Bacherville to mouth of Buffalo. Ledbetter Landing, 8 miles from Holladay. Mr. Rize at Ledbetter has a store. I've wagon running in all the time here from Holladay. Can stay an night with Mr. Rize. Can stay with W. F. Harrison at Holladay, good place. W. F. Kuehn. 11/29 - 5th St N. goes in our department. Met his brother Gustav Kuehn. Olive Hill, at Frank Robertson vi 4 mi.; Meet y Olive Hill, near Pine Grave Church, down hill E in a branch. Grave yard Hollow, 1/2 mi. E of Pine grove. M.D. E. C. Morris. Savannah. Fossils Base of Camarocian section at Calyciate Spring. Dalmarella subcarinata Rhipidomella 2 or 3 species Lystalna rhomboidali Stylenella punctulifera Spirtia v. Deltys. Bilobites Famites

Fossils Col Jim Smith, 1 mi E of Savannah. Diaphorostoma nigeranese, Dictyomella Meristina mariae roemeri Merista tennesseensis, common Trematospira Homoeospira schucherti, Homoeospira Nucleospira concentrica Spinifer erispus? Astrypha reticularis newnhamensis Micrulum stricklandi, smaller than typical. Micrulum tennesseensis, Milenia zaffridi Camarostachia like neglecta Camarostachia acinus? Sygidula roemeri Orthothetes subplana Dalmavella elegantula small Rhipidomella Callipera elegantula. E of Jim Smith 8 mi E of Savannah, Cyathphyllum radiale Complexus shumardii Favrite Plazmipora follos Thecia, Astylamanum versicorum. & of George Wilem, 7½ mi E of Savannah. 38 Homoeospira? Amphitheca? Nucleospira concentrica Nucleospira piriformis? Merista tennesseensis Astrypha reticularis newnhamensis Milenia zaffridi Sygidula roemeri Stylomenella psilongata? Stylomenella laxiflaticus Leptasteria pleurotoidalis Dalmavella elegantula, typical 1/2in. Rhipidomella Rhipidomella zaffridi Lecanospinus piriformis Astylamanum versicorum In front of John Henry Johnson, 7 mi E of Savannah. 38 Trematospira? very small Spinifer zaffridi? Camarostachia like neglecta Rhipidomella Perminnus milligani.

"Steamboat" Photo 2: Coffee and, just below Coffee Landing. Term, Bedding will shown at Bluff, Bluff about 1/2 mi. mg. Rock bluff begins at Cravers and extends down the river. 10-15 feet of Barnesport bed in 15-20 feet of Dixon bed. Dip up the river. At Carr Buds Belm Landing, 20 ft? Heavy cracked limestone below, Above this is Dixon bed - more clayey streaked north red, 12-15 ft ? Above is Barnesport bed, massive bed for 5 ft. Slim bedded + white layers above, 20 ft. Dip fairly A short distance down the river the dip is up the river. Apparently cracked limestone. Further downstream the Dixon bed equivalent is nearly level the dips slowly down river. Dolosted bed white + red alternating. 10-20 ft ? Overlaid by 30-40 ft of Barnesport bed. Dip continues down stream. Overlaid by cliff forming stuff. Look up to see if Anna Helderby. May be this thmple not her bring whether this limestone is clifty and thick. Next I can design rock appears small Steamboat Bluff begins about 1/2 mi. above Saltillo, Hard layers 8 ft. per 5 ft more clayey with a little red, over 15 feet swiftly hard. All = Glenbork bed. 1/2 mi. below Saltillo. Glenbork bed, at first level then dipping down stream overlaid by Dixon bed dipping strongly down stream. This Dixon bed finds thin bedded. A consider- le joint consists of an inferior whit ish limestone interbedded with some clayey reddish streaked above Pleasant Belm or Pleasant 1/2 mi., rock dip up stream 20 ft. Glenbork, overlaid by base of Dixon bed. Then dips down Black Ark - is this a dyke at Govern- ment loght; just above Kelley Land- ing. At Kelley Landing + below a great thickness of Glenbork with dipping up stream. Resting on Saltillo limestone - east northern exposure. 10-15 feet of Saltil- lo limestone exposed. Just above Swallow Bluff the rock dips down stream, the Glenbork resting on the Saltillo limestone from all -> The thin bedded Glenbork 3.0 ft. is overlaid by heavy bedded 15 ft.

steamcat Below Grand Vizor, E side river. Rocks dip upstream Glensirk bed massive above, now thinbedded below. Levely lndroican partly exposed, about 10-15 feet at highest point of arch. The nature of the lndroican not to be determined at distance downstream. Presently 3ft clay, in 15 foot thin redded limestone. Not case since the thin bedded limestone may be beyond. However Gordon- my level certain at middle of arch although several exposed. Further down stream is illam bedded stuff still down stream, D ix m ?? Then a strong dip upstream, Glensirk bed. Massive beds over thin bedded section. About 1 mile into into Cliffrivered. Take left hand up a little piece, down a little piece, about 200 yds on the level to a big gate on left down 150 yds trip plain road to spring. House in far side of gate on left side of road. Gate keep fence on left all way to Martins store 1/4 mi, to Martins store about 1/2 mi to gate. W.N.Davis house S & Co S Exp N, From Bath Spring up to gate at beginning of lane at grad: 37 ft. 19 feet largely reddish clay stuff (= total of 56 ft) several whitish limestone layers above level of shed- 18 1/2 feet no experience along road. (= total of 74 1/2 ft - up to certain Bermudant bed.) 14 feet up to a hard layer in soft whitish clay ends at 88 1/2 ft, C 22 feet of Bermudant soft white clayey stuff (= total of 110 1/2 ft.) B Hard Limestone 5 1/2 ft thick. (total of 116 ft) A 19 feet to top of white limestone exposed (= total of 135 ft) 21 ft to top of drill = 157° Collected with D.C. Horton, E. 19 foot at top. Stillation calcating. the Cluecortopite, the small Blefield wells as Carna at Col-Smith, the Maynurse with raised ridge on outside of road. D 7 1/2 ft Hard Limestone. C 22 foot Lime rocks I wrote collected = Henderley & S afford B 4 ft hard limestone = 3 feet large of S affrid A 17 ft. Merizine warhouse Compression +3 area trip. collected Vincented bed.

Swallow Bluff. N. end of fold. Boyred measure. C 6" Chert y Clinton 318" limestone of Clinton, a Saltillo limestone = Near middle of arch = 31 feet thick, Dense hard limestone one beds 2-4 inches more shale than limestone. [illegible] F5 4 ft 9½ ft -Thin bedded limestone. D8½ Beyond here hard massive ledge. vertical. G. 6ft whitish cracked limestone and a rather thin beds, H. 11 ft limiest with reddish crinoidal spicules rather then bedded. I. 11 ft: A considerable joint near more massive bedded. (Total 53¼ ft.) J Waldron bed. 3½ mi fossiliferous [illegible] 22" that hard limestone led with shale or wanted to be not readily recognizable, 20 inches, reddish clayey stuff. weathering beds. K 21 ft S.L.D limestone, cracked (Total 76¾ feet) L Slabs froze, which raise the bed to 79ft at first. Fossils. Lower C. Bath. Spgs. Meristea tennesseensis commun. Atropus reticulatus novozanensis Wilimia zaffardi. Spiridula remesii. Micrinulus tennesseensis Camarostrecha like aspect a but larger. Homospira schucherti, Dalmanella elegantula Nucleospira concentrica Leptaena neombridiola. Calymene Mayarensis Pentremites, more where closer than typical Favrites forbesi, Withathea myelasma, Callipora elegantula Cheunzagites, one. Diaphanostrea Mayarensis Phijidomella zaffardi. Amphistruca. Rhipidomella. Spirifera zaffardi of Safford look up, Camarostrecha acuminus Spirige look up, Amisophyllum Agassizi. Look up. Chert in Swallow Bluff Ollaerens more like Madinmenes thinn Calymene vogdesi, Leptaena Neombridiola Dalmanella elegantula Atropa marginata

Fossils. Buth Springs Layer A Caryerinus aratus Cup shaped sponge craters verrucosum stellatum-sulcatum Gutbergsponge maricens Chonetes commun ellaenus glabella Pentamerites typical Atypa amplicolus Waldron Led. Montgomery's Mill Centreville. Near Fly Jrm City. Clinton cherty. Beside near gne X wp 29° Riverside, Clinton embedded Crg. nearly gne X wp 46° Swallow Bluff. Chint in cherty Massiv Crg.? X wp 53° Clifton. Glenbirke

Steambat. Below landing at Martinez, Saltillo lime stone. No division directly above. Below government light is Saltillo limestone. The rock directly overlying may be Richmond limestone here. Plenty of red clay with farther up. Both [illegible] on anticlimes here. There is no questioning the absence of Wasmumic clay at least. Apparently 8 feet of Richmond and limestone, first in apparently massive and 4 ft thick. A 2 mile exposure = 2 miles? \frac{1}{2} mi [illegible] along canyon very thickly, [illegible] layers stuff over Saltillo limestone, should be visited. Legr SE 450 yds. NW 400 yds, E 3/4 mile, Shift m. {50 feet [illegible] and soft weathering clays linement me with cherty nodules + sponges. 75\degree {75 feet. About 25 feet at base are harder 1/2\degree white clay base of B2 zone, 1 foot 42\frac{1}{2}\degree slope. 42\frac{1}{2} ft. = 88\frac{1}{2} ft above Waldron. From here m red at least equals white 14\frac{1}{2}\degree {14\frac{1}{2}\degree, \Delta total = 14\frac{1}{2} ft. {{other red clay band at 3\degree, 7\degree, 10\frac{1}{2}\degree, 12\frac{1}{2}\degree, First red clay band. 31\frac{1}{2} feet of crucheled limestone. Waldron bed. Martinez at top of 75 foot section mentioned above. Above is 22 feet hard limestone on the lwr, soft clay slope above. The top must larger and named Canyonm, squatus. Total Baramount ex- posed = 98\frac{1}{2} ft. = 100 ft in round numbers. = About 4 mi. up river above cement mill. Dip 7/7 in 100 steps 16 ft solid red rock beneath Waldron. No exposures for several hundred yards down stream.

Legs, Short Creek W.E Ashley P.Dennan? Above? 300 yd. 3 ft 4 in. of black shaly stuff and hard rock alterna- ting, full of Sturgeta, 5 in shaly 6 in argil 4 in shale 6 in argil 19 in shaly 19 6 ft Hardin SS. at top Macindaw Shale? and byfucate? 8 yd shale Pennantville 43 feet below Hardin SS Solid Limestone for 59 feet below Hardin SS. SE of Kelley's Landing, on west side of creek My Bee Creek. 12 days good, thick as at Clinton m. white coarse 17 1/2 ft. Richmudgy 50 ft + shale (?) New Era above 10 feet at top concretion everywhere except 41ft B transport bed exposed, Stalactite inclinations? 2 ft. White clay above Perm.-font 39 ft Dixie bed. Total 69 ft above Waldm. {spotty exposed, 10 ft. { Whitish + reddish limestone, 22 ft. whitish limestone, Waldm bed. 31 ft reddish limestone rather thin, 5 ft whitish limestone then Waldm bed 3 1/2 ft. 9 in. limet at top. 27 ft rather hard reddish limestone. 3 ft reddish + white limestone? to measure? 6 1/2 ft rather soft + reddish, like Regrod ? 20 ft {hard white limestone.-56 1/2 ft below Waldm. orinidal for lime 12 feet at least, mm dense + whitish in & ft above. 12 ft {Lown Sil = Ordov. limet. coarse Bachman fragmental at top made up of ? Entirely to today concentrated. Calc. scatters - large scale byssum flabellus weathering to benn planifolia 2 ft coarse limestone crm-mented shells believed to be also Richmund? Saltville Limestone? No cash recognizable as limetm.

Fine exposure below Walnut ckl, Great vertical cliffs Brownport. Parker's Landing, Below Linding & redial limestone, Take left hand at blacksmith shop, gr 2 miles to spring on R Hand Side, near a school house among trees, cross creek, gr along a lane, fence m right, intersects main road and 200 yds up in school house. Turn to right, go on half a mile road forks, turn left here. About 3 miles to Bakersville. Big Sandy. On east side of Tennessee opposite mouth of Big Sandy is Standing Rock ckl. At forks of creek 5 mi, from Tennessee river is exposure. Fring there on both sides of both creeks are fossils. Black slate, 2ft black shale? 5 ft reddish gulfshat slates purlate 5ft black slate. 5ft coarse sandy. 3ft Conifers? ? 10 ft ? 43 ft top of cherty limestone to base of 2am at river edge. Camden chert! Clinton Burcham, about 4 mi NW of Baker ville, in road to Warady, cross gate and turn east along edge of hill to Henry McClure's house. Exposure of Conifers is at begin- ning of bluff beyond the house, on W face of bluff at end of bluff. The Camden chert along river face of bluff. The Conifers seems to occur only at western end= beginning of bluff, above Buffalo river level to 50 ft above at highest elevation. The Bluff is at the Wheel on the Buffalo river.

Sam Dixm, [illegible] C Photo Robert Steele [illegible] [illegible] 40 310 [illegible] N70E 125- track 310 169 N45E [illegible] M 176 field road GC N35 W 60 ft. old road John Bunn da. straight north Salt Cl S 30 W 50 claym 32 S 30 W 600 20 920 50 520 70 [illegible] 180 oldmints Mow-15 2nd cult [illegible] N 4 E S 30 W [illegible] 100 Warila [illegible] 90 East 70 Saturday 200 140 600 N15W [illegible] [illegible] 310W 584 310W field road house 360 N15W 250 212 S 37 W culvert 40 150 [illegible] Mow-16 N35 E 200 N14E [illegible] [illegible] 84 L 169 [illegible] 275 S 40 W 167 61 culvert

Bledsoe Rogers Centerville, Montgomery Fly. Riverside Bakersville. Morr & Co Slegm Clifton Glenbreds Shadley Bluff Baxk 5th 8. Pyramid Bluff Adam Bluff 2am C&O. Pix 37 4/2z 14 1/2 Ly, 32 3 1/2 Vel. 1 - 1 - 1 68 - 192 - 2 - 1 1 - 4 - 1 448-682-877

S 12 W 55 S 15 W 215 Write N 40 W to trade house. S 15 W 160 Beginning of Penn's tract. S 15 W. 72 (M 537 L 200 BG &c) S 15-W 40 End of tract the land house is N 40 W.

(4) N60E 80 N40E 50 N20W 466 G not home or left. N 170 Lane turns off here Lane: N60E 50 N20E 120 N60E 160 N60E 200 N100 80 Horn to N W 50 (Lane continues West to hill 300, hill front gives N&S forming valley. Field Lane, S20E 70 Stable R S 80 and of stables, E 250 coming exp. hill (N75E) 150 N60E 80 N40E 95 N80E 65 S70E 56 E 100 Obtuse 11. Breeders'WH S85E 160 Neglected endy Grant place, N80E 66 river. River runs N40E 220 path on left again, hut or left N80E 100 river bluff 12 N50E 140 end of river bluff. (Regular road crosses river to NW N40E 40 to regular road Regular road N46E 75 School on left. 3) S45W 55 N60E 150 S85E 180 Church N < B hardly 2½ mi. S75E 120 212 Road goes up stream (N45E to bluff where road turns off (N45E 55 = to river.) S40E 244 to river, N80E 100 to T Gate & W Gate N30W 80 N30E 216 N40E 140 N65E 196 S80E 125 N55E 15 river, N55E 25 cross river. N55E 20 N60E 76 N70E 330 N25E 140 N80E 40 Gate left on church left river on right N60E 175 " N80E 500 to along wire woods. 80 to corner of fence From U bluff to Grant, N20W 58 N10E 55

*N 50 W N 55 W N 5 E N 35 W *S 70 W W S 40 W N 10 W 4 mi. R. Return, S 10 E S 15 E S 60 E S 60 E S 50 E S 80 E S 20 E S 10 E S 15 E S 75 E S 75 E S 5 W 3 mi. S S 50 E S 80 E S 46 E Gate E 450 Along River, Left road. 1180 Cross River to W. 180 to bluff, No path on each side. 235 (Place) Phillippo, across m at 190) 3 mi. to Olive Hill; Lemm river across fields 770 path wagon's 200 420 to Main road R 225 Phillippo km S N 18 W. N N 10 W N x N 18 E S 40 W S 25 W W S 75 W x N 85 W N 75 W N 40 W N 85 W N 45 W N 70 W S 65 W S 70 W S 65 W N 65 W N 60 W N 50 W N 45 W N 45 W 1). N 18 W. N N 10 W N x N 18 E S 40 W S 25 W W S 75 W x N 85 W N 75 W N 40 W N 85 W N 45 W N 70 W S 65 W S 70 W S 65 W N 65 W N 60 W N 50 W N 45 W N 45 W 565 60 520 80 115 (40-80 River) 220 312 44 300 Bluff with uncertainty = S 800 (75 to my bluff.) 450 60 Road off to right E 100 150 140 Hill on right E 180 SS replacing Black Slide with fish slate 4 in lmy. Not well preserved but stratum clean. (49) = 14 old No. 260 Bluff on right Course SE. Varies Rock bed begins 265 Road turns off N 55 E of bluff, 100 Major land on right 160 Road turns to left across will T 80 500 School on Cyprian draws m, with Church B 175 Road off S 80 E to the house. Brand, Mill Market 13.40 2,680 450 2,330 Gate Grants field. River due left. Bluff due left of river Road off to right E Hill on right E SS replacing Black Slide with fish slate 4 in lmy. Not well preserved but stratum clean. (49) = 14 old No. Bluff on right Course SE. Varies Rock bed begins Road turns off N 55 E of bluff, Major land on right Road turns to left across will T School on Cyprian draws m, with Church B Road off S 80 E to the house. A

Trace Creek 3/4 mi. Riverside S 70 E 85+65= 15.0 37 S 81 E 170 4 S 45 E 38 N 70 E 279+59= 332 80 E 115 +99 = 242 20 N 60 E 67 16 N 45 E 100 25 N 80 E 22 1/2 240 14 (220 Creek N 20 E) S 20 E 11 436 109 RR S 40 E 40 S 60 E 100 trace turn S 150 middle of N 20 E 3+5 1/2 section 2 mi. W. of Trace Cr. 25 60 1/2 248 36 5 27 = 13 10 27 = 2.6 ft. 6 94 15.6 4 ft 2 78 39 - 13 264 132 - 11 2 3 [illegible] 11 1788 44 15-60

6°+1°+6°+13½°. 3½ ft mr Hyman L for Wilson by way. L. Jim Drvin L Albert Finton, School house. L Old Smith. Fordon place, cross budge wooden bridge. 2nd bridge this side is a gate.

Trace Cuts