Field notes, Kentucky, undated, 2 volumes

Foerste, Aug. F (Aug. Frederic), 1862-1936
Unknown
Smithsonian Institution Archives
Original Source
Source Material:
Image from the Biodiversity Heritage Library. Contributed by Smithsonian Institution Archives. | www.biodiversitylibrary.org
Geology

Document Pages

145 Pages
Page 1
No text detected
Read Page
Page 2
No text detected
Read Page
Page 3
No text detected
Read Page
Page 4
No text detected
Read Page
Page 5
Indian Fields. Oil Spring, SE of hotel, at the Oil spring. Also location of Soda spring. Level of the Soda Spring. 14" Fissile Black shale. 3" Nine solid layers, earthy, bluish gray, weathering irregularly shale. 12" More slaly, part of it (near top) very fissile and black. 10" Solid, light brown, like breccia- ted layer, but not brecciated. 12" Strongly brecciated and weathered or as to bring out this brecciated idea splendidly !!! Wish I could get a photographer Celestite, Crispall stones, Cyathophyllina and Favosites Corals. 2", Black shale 14" Solid, light brown limestone. Contains black nodules near base, up to 5/8 in. in length. Oil spring issues at this level or just below: In order Top of hill with nodules possibly 35-40 ft Black shale. 15 ft Clay layers in Black slate especial- ly lower part. 75 ft Black Slate Soda Springs.
Read Page
Page 6
North east of hotel 100 yds, in a little run west of the creek, Oil Springs Hotel. Black shale 13m solid limestone. 10 in brecciated layer 14 in solid limestone. 18in limestone without caronims 18 in freely exposed, solid in part 4 in Not exposed, soft 15 in. Solid limestone hard, siliceous 1 m. Rotten stone, 5m 3 in. broken shale with nodules. 4 in rotten stone 4 in Jannbim limestone with Black nodules. A 46in crinoidal siltstone 1ft of base, with corals (Hindea also?) Chert in middle + upper part. 18 in Argyllacens rock, Yarrest Der, with proboseth, tuber- ulated plates black nodules 8R. Plum creek locality. Photo 1. Plum creek clay. Plate A. Plum creek clay. On west side of Plum Creek east of the road. Photo shows top of Plum creek clay. The base is slight ly below creek level here. Thickness of Plum creek clay exposed here is 5ft 3 in. Elkton limestone rather heavy here. Direct east of George Mc Intosh home. Elkins limestone. Cystophyllinae & alveolus are rare. (Leptaena subtruncialis) Delorania elegantula Plate, striatopora longimensis 3 placent. 5 specimen layers about 6ft below the top. nearby [Strophomella] like patina but apparently with multangular net wire. Stricklandiina near top? 13ft Estill clay. 14 in. = 2ft layer limestone. 17ft Vrae limestone & Lagdome 18in Argyllacens light brown limestone 1ft crinoidal l. with cnids. A 6 in. soft argyllacens rock, see preceding page.
Read Page
Page 7
Along trip of road; working what is left of Black shale, between Plum creek & Tipton Ferry, = sand and gravel, shelles 3\" in my mi brome cores. Strine for- mation. N side of Tipton ferry. 16\" ft 2\" ft Layer to face of Devonian, Collected macro fossils Plotter 2 Devonian limestone State B along RR West of Day City. Opp, Green McDowells Lane. 1 mi West of Day City East of loc. 2; 1 mi. SE of Indian Fields, along the road running north, in the north side of Suble- gend creek, Devonian 20 ft clay with macro fossils beneath =8\"3\" 9 m. l. = 2 ft layer. 13\" ft Estill clay. 6 \"4\" fells lime stme. max exposed. 5\"\"2 ft not exposed. Sublegend creek Brown or Brunner, 4 mi SE of Indian Fields. Devonian 20 ft. Clay, macro fossils. 9 m. limestone me - 2 ft layer. 9 inches at not measured here (Top of Elkings limestone just strikelandrinia in bottom of creek. 13 ft estill clay Top of elkings limestone with strikelandrinia, me agreed with John Griff.
Read Page
Page 8
Al near North Fork of Sulphur creek, 1 mi. E of North of Riddville. 36 ft about estimated 50 ft about estimated interval. 29 ft Pseudr Madison measured 21 1/4 estimated, 136 ft Richmond, Measurement mid of center. 8period Plate 3 Contract of Irvine Plate C Kintzary clay perpendicular + Rids rising above the 2 mile. Taken from point slightly east of most northern pointy Riddville line geology North Fork of Riddville, Direction of river, towards S E from here. Photo 4 Ridden out below Plate D Clinton, at Hornback corner of L+E RR = 1 1/2 mi. Wg India Fields. 70 ft to mile grade Photo 5 2nd cut west of Plate E Hornback curve. Lower part of Richmond, Photo 6. I invest Riddmond, just E of my face Stationery- point along RR, east of three: above same in other notebook. Collected 9 most Richmon and line for analysis, 20 ft of this section. 5 immediately above is clay sort of Middle beds of Richmond. Immediately film is thick that section at face of Ridmon, not exposed, possibly 20 ft thick, but impossible to tell. Lynx beds here. The home in middle of road at eastern Lynx exposure is that of Thur Wild Abbott, 2nd cut E of Abbot's Lynx ex- posure, I invest part of Middle Richmon and north of gabling clay exposure. Collected 3 for analysis, 30 ft up to magrinite clay at west end of cut. 8 sample near base,
Read Page
Page 9
Photo 5. Plate E preceding here. Massive layer in preceding site is 18m thick = massive bed at Spencer, E of ridge with "slate" on it. This cut adjoins the East on the east; I 17ft up to layer with Strophomena jellensis. Granular crumms. Fossiliferous layers will expose at extreme east of this cut: Strophomena planumformis, Galeatella occidentalis, Strophalasma striata cum, Orbally Phynchitesima capax. Photo 5 Plate E massive bed at base at far end of view. Fossiliferous layer at top of second block about halfway up the exposure. 17ft of thin bedded rock above the free lopherma layer first mentioned, at least just off path leading down to gran iturbide. Collected clay here. Clint on base 22ft clayey, top 16ft cliff slatey, slate as before. 17ft at least of thin bedded free lophera SPR, collected; see by me. 18ft? exposed great W path, along evel of RR, trades. 12ft vitrinite. 1 1/2ft ferr pruss, (the 18m, massive bed wit 53ft vitrinite. Top of layers fed at creek at june Hornbacks. Photo 1. B. [illegible], Plume Creek & Plate E. top of Clinton slate 7ft talcum limited ores 5ft Plume Creek clay 2nd cut & of Hornbacks ores, The next cut east cut gives fossiliferous layers within 2 feet of top of talcious lime stones. Stickleandimia is found here. Tertiary clay is above. These places great west of the great fall. At yeast pit = black shale 18m Devonian bed; decayer 7ft clay, over water limestone.
Read Page
Page 10
Mine clay at great clay part 3/4 miles west of Indian Fields varies from 2 to 5 ft in thickness. Contains fossils, is very sandy. Photo 2 OB View across A Mine plain to Rocks beyond from cly part 3/4 mi west of Mine southeast a west ward. Photo 3 OB View across the Indian coal fields. From 5 mi W of Indian Fields RR Station. Photo 4 B view of 9 mi = 2 feet ledge at locality east of Broadway Bruner. A1. 1 mi NE of Kiddville, along road following North Fork of Gulbegeffd, in out grou ery Cr. Lower Richmond Middle Part, Aug. F. Foerste, Aug. 1905. B.1. 2 mi W of Indian Fields, at first cut east of Tom Will abbott. Clark Cr. Lowest part of Lower Richmond, Aug. 1905. B2. 2 mi W of Indian Fields, at 2nd cut east of Tom Will abbott Middle part of Lower Richmond; B3. Cut just west of paths leading down to Jim Hornback, 17½ - 25 ft above heavy ledge at base of Middle Richmond. B.4 22-35 ft bel or level of Clinton, Base of Upper Richmond. Hornback Curve, 3 mi. W of Indian Fields. B5. Hornback curve. Middle part of Upper Richmond. 10-22½. Bel or base of Clint B6. Hornback Curve. Top Richmond. 0-10 ft
Read Page
Page 11
B7. Cut east of Homback curve, 1 1/4 mi. WY Indian Fields, Clark Co. Massive base f clint in a Brazo field bed. B8. 2nd cut E of Homback, uper well bedded part of clint, In Brazo field bed, 1 1/4 mi. WY Indian Fields. B9. Plumm creek clay, 2nd cut E of Homback curve, 1 1/8 mi. WY Indian Field, This is last in photo ex- posure. B10. 3rd cut E of Homback Curve. telkins line- ates, B11. Ferruginous layer near top of telkins limestone, = 0-2 ft below top, just WY great full Jami W. of Indian Fields. B12. Estill clay, 1st cut next great fill. WY Indian Fields, 1 1/2 mi. B13. Macr limestone, 1 1/2 mi. SE of Indian Fields 1 7/8 mi. E of Brandon Branch, WY Lillys and up N road. B14. Big clay pit 1 1/2 mi. West of Indian Fields, Crab erland clay proper.
Read Page
Page 12
II No 1269. page 16. Limits to Drum ore-bank one and a half miles from Old Slate Furnace; Bath Cr. Bed is -12 ft thick, (incl?) the Clinton Grp.; Collected by Philip N. Moore. II No 1652. p. 18. Limits from Slate Furnace Ore-banks, Harvard Hill. Upper Silu-rian formation. P.N.Moore, No 1653. p. 19. When part of bed 4 preceding. No. 1654. Limits to me at Chalybeate springs, Pilot Mtn. P N Moore. No 1655. Limits paid to be 20 ft thick, from near Springville in road to Slate creek. P.N.Moore, Madison Cr. 2168. p.51. Sept.4. Clay; Milton Barlow, from near Bylletown, Bed 4 feet thick, in Black Shale. John R Proctor. Clay of a light, irregular grey color. Irregularly and imperfectly laminated. Quite plastic. Burns to a delicate light red flesh- or cream color, creamy white. 2169. Clay of remarkable thin cleanness; on the road leading from Macr to Beldham, about a mile and a half from Waco. Probably below the Coniferous limestone me. John R Proctor. a compact clay, generally of a light olive-grey color, but crined irregularly with ochreous & ferruginous bits plastic. Calcines quite hard, of a hand-some light brick color. 2170. Indurated clay from C.L. Searcy, near Bellist Cr. Be- neath the Coniferous limestone Bed 18 ft thick or so. JRP. a light olive grey laminated Clay; mottled with ochreous & orange-colored
Read Page
Page 13
foreign infiltrations. The minerals are cutated. It is quite plastic. Burns to a handsome flesh color. Dried at 212° F. Silica 62.56 64.566 62.58 Alumina 24.78 20.16 22.94 Iron peroxide 1.80 4.20 3.76 Lime Trace .213 .56 Magnesia .317 .641 .425 Potash 3.276 5.054 5.28 Lime .294 None .308 Combined H2O+ 6.973 5.166 4.147 No. No. No. 2168 2169 2170 Madison continued Marly shales of Madison Co. 2186, page 52, 4th Rept. Marly shale, in the road near A. Lakes place. Drum- mig creek. Niagara group. Our dive peg is brownish grey, somewhat firm shale, mottled in parts. Quite plastic with water when powdered. Calcines to a light brick color. 2187. Marly shale or indurated marly clay, on the hill 200 ft. due south of Dr. Free- man's house. Probably the same bed as No. 2170, be- neath the Canifer and lowest one. The bed is 6 ft. thick in some parts. And contains gypsum. In R. Miller Generally in thin soft; irregular laminated, of a light olive-grey color, irregularly varied with brownish yellow and a ochreous. Contains gypsum in irregular crystals. Is quite plastic in the water. Burns quite hard, of a handsome light brick color.
Read Page
Page 14
Madison A. Limestone. Silica Alumina & Impure oxide Iron sulphato gypsum Silex Magnesia Potash Ioda Combined H2O, CO2 and base No 42.30 20.84 4.12 19.285 13.32 .461 2.387 .357 16.221 2184 48.78 17.32 3.24 .496 4.768 .24 5.871 2187 Just below Dowina. 2189. Shelly limestone near bottom of Muddy creek, 2 miles N.E. Cumptown. "Limestone and shales" Probably Clinton. John R. Procter. Of a dark mottled grey color, generally quite friable; some portions are compact. 2190. Impure limestone, top of Cumberland and shale, Upper 12 inches. From below the mill -- a dam on Muddy creek. E. Elliott in a pretty firm, fine-grained, or compact rock, of a handsome light olive grey color. 2191. Impure limestone, top of Cumberland and shale from 18 to 30 feet below the massive imp limestone of the Silurian or Muddy creek. Rather darker than the next one -- color on chips is not so that.
Read Page
Page 15
2192. Impure limestone, resting on top of Cumberland shales, Bottom stratum. From below the mill dam on Muddy creek. A granular limest- one, somewhat cellu- lar, cut showing some petroleum which gives it a brownish color. It weathers ochrous. 2193. Impure limestone, Nia- gara, Top stratum, 8 in. thick. From below the mill dam on Muddy creek. Elliston. An impure granular limestone; somewhat cellular, dark brownish- grey, somewhat mottled, contains petroleum the infiltration of which gave the dark color to the rock. Weathers fer- ruginous. 2194. Impure limestone. Second from top. From just below mill dam on Muddy creek. Elliston. Resembles preceding. But is darker colored. Contains petroleum & some iron pyrites. 2195. Impure limestone, Niagara, Third stratum from top. From below mill dam on Muddy creek. Elliston. Resembles preceding. Rather finer grained and harder, contains petroleum. Exterior surface weathers ferru- ginous. 2196. Impure limestone, Clinton group? From the quarry north of Rogersville, a compact a fine granular rock, semi- fossiliferous, of an olive grey color, in some parts brownish. Con- tains some iron pyrites. 2197. Limestone from below the Canda-gallo grit at the gap of the Canferus limestone. a fine granular, brow- nish grey rock, gives the odor of petroleum when heated, and probably con- tains this mineral.
Read Page
Page 16
2198. Bituminous limestone from above the Corniferous limestone, 3-10 ft thick, from near Elliston. Generally of a dull, brunswick black, or grey black color. Some pieces with bands of a lighter grey tint. It is a fine globular rock. 2199. Impure limestone. Top of the Corniferous lime- stone. Total thickness 15 feet, with intercalated beds of pure limestone 6 in each twelve. A simple fine granular a compact rock. Samples from different levels are varied. Some are brunswick-black, someumber-colored, and some intermediate in tint. 2000 Limestone, on the road one mile south of Mrs S. J. Embry. intercalates with the so-called Black Band and bituminous limestone A dull buff grey fine globular rock with some slight infiltration of lime decated cross oxide. June 5 noon Embry, Sept 3, 48.53 11.29 10.33 17.656 3.70 1.696 3.47 6.1567 24.74 27.173 5.614 lime carbonate " magnesia " alumina silica Boric acid iron peroxid potada soda Bituminous shale water & loss Siliceous shale My lime " " " calcia 58.86 20.10 2.996 3.90 - .576 1.276 .054 1.396 10.87 9.980 25.592 18.794 4.785 20.98 50.96 27.972 .5.96 3.554 .276 .087 6.493 4.12 28.538 13.319 2192 2193 2194 N.V. N.V. Not act. Not act. N.V. N.V. 2189 2190 2191 silica, ferrum oxide
Read Page
Page 17
2195 No Si lica Si O s S i c acid Lithium Hydroxide Arida Potash Ox Sulphurid Ox Peroxid Phosphoric acid Alumina Magn. Carb. Lime carb. 47.58 36.58 41.15 43.06 35.16 51.20 17.133 16.541 13.908 9.994 4.446 10.98 4.61 9.04 7.942 7.754 1.89 2.640 2.060 1.540 13.022 11.287 7.339 1174x. 6.117 18.19 31.99 20.99 2.09485 23.044 24.113 19.689 28.672 26.615 8.158 8.781 6.384 4.756 2.212 11.829 2.099 2.099 No. 2199 2198 2197 D v. 2198 M r. 2198 2197 M r. 2196 2195 2200 Dint with Black chicle 2198 Eating Black chicle. 2199 D v. 2197 D v. 2193 Ellins?l? 2194 talkings? a Clinto? 2195 Elkins?, a Clint 2192 Bray Clinton 2190 Richmond 2191 Richmond 2189 Richmond
Read Page
Page 18
Madison Cr. 2209. page 62. 4th Rep't. Sulphur water from a spring on the farm of C.L. Searcy, Elliston, in the Niagara Group. Composition of saline contents of this water, in 1000 parts, Lime carb. .2040 Held in Magnesia carb. .0322 solution Iron carb + phosphat .0172 & carbinic Silica .0045 acid. Lime sulphate .4301 left dis- Calcium chloride .0124 solved Magnesium chlorid .0920 in H2O Potassium chlorid. .0380 after eva- Sodium chlorid. .3221 poring. Soda carbinat. .0837 Silica .0018 Lithium strontium + sodium sulphide traces. Organic matter & loss .3294 Total solid matter in 1000 parts = 1.5774. Free CO2 & H2S not deter- ermined. Bryle Cr. 2281. Plumbatic modules (copperites) at base of Marble, Bryle Cr. Butterious matter, Ferrus carbinat., 2910 Wt of P2O5
Read Page
Page 19
Nelem Cr. 2393. Sandstone. Phosphatic. From the black Devonian slate in the B set or dist- rict, locally 10 in. thick, Contains fish & other organic remains. Blue sandstone partly made up of large grains of quartz, some- what rounded, mixed with dark colored gran- cules and broken organic remains. 67.04 silica. {alumina iron ox'd time magnesia} 11.162 P2O5 .019 Potash Nelem Cr. 2394. Limestone - ferruginous, From near top of upper Brid- gon River beds Cumberland Sandstone & shales, Near farm of S.P. Stiles, 4 mi. Mr Bardston. a fine granular rock of dull grey color, turning yellow in a wetland pen- ting. 2395. Limestone ferruginous, From near S.P. Stiles farm. Cumberland sand- stone & shales, a fine granular rock of brownish yellow or color color. lime calc. 81.58 61.24 magn. calc 1.501 8.915- al. & iron oxid 2.978 4.317 P2O5 phosphoric acid 1.202 .563 Potash .423 .443 soda .248 .254 siliceous residu 11.120 22.52 Moisture & loss .948 1.748 Nr Nr 2394 2395
Read Page
Page 20
Clarke Cr. 2469. Plensphatic limestone Stewarts Mill, Lubbegus creek. Clarke Cr. Oriskany formation. A dark brown, cum- glomerate rock, contain- ing many dark colored fragments of fossil animal remains. 2470. Plensphatic limestone From near Harward's creek Clarke Cr. Oriskany formation ? An im- pure form of fine lime- stone rock, gray brown with ochreous material in spots, contains fossil impressions. Lime carb. 21.38 33.98 Magn. Carb. 3.055 11.185 Alx & iron oxid n e n e P2O5 9.71 1.842 Pet ash .83 n e Soda .228 n e Silice insoluble 27.58 31.72 Nv Nv 2469 2470 Lewis Cr. 2484. Limestone, hydraulic, sent to Mr. Pardee by Mr. W. J. Richards of Vanclebur, Lewis Cr. a dull gray fine granular rock, with faint lines of stratification. Lime carb. 48.79 = 27.322 lime Magn. carb. 37.482 = 17.834 magnesia Iron ox & al 2.49 P2O5 .143 Pet ash .49 Soda .058 Silica soluble 1.150 Insoluble silica + silicates 8.850 moisture + loss .547
Read Page
Page 21
Madison Co. 2496. Shaley Clay. From land of FW Lewis, 2 miles S of Buttern, about 100 yds to the left of Big Hill turn pike almost pp. The blache on'th sdrj y FW Lewis. Bed 4-5 ft thck. On Niagara slab, I dem'y mfer 10 in. lclaminated clays soft shale y n light Mr Fidler, grey colr in the ex- terin, darler gould + brownish yell awith grey in the interior. 2497. Shaley clay, same as last. From 10-20 in. below surface. M. Fidler. Silica Al. = 20.68 or perx .396. Lime Magnesia Potash Soda H+O, CO₂ etc 59.000 24.64 1.456 1.096 5.500 .217 8.091 M. 2496 42.56 20.98 8.68 7.247 4.819 .166 15.548 IV 2497 NE y Berea Madison Co 2499. Marl shale orj thin pigg's land, 4 miles north (= NE?) of Berea near the road from Berea to its Big Hill Turnpike, by way of Buttern. The locality is called Blue Fork, Wavy formation resting on Black shale. Wm Fidler. Silica Al + fer perx Or O5 lime carb. Magn. carb. Potash Soda Combined H2O etc 69.152 20.39 trace .145 2.289 3.754 .747 2.920,
Read Page
Page 22
Lincoln G. 1873. Clay from head waters of Carlen river, on land of Mr. Thos W. Varma, Bed 2-4 ft from the surface, said to be 42-45 feet thick, resting on black shale which is 50 ft thick. Clay imperfectly laminated of a dark olive-green color, passing to a gray buff color. Silica. 61.58 Alum 23.946 Iron peroxide 5.814 Lime .201 Magnesia .850 Pot ash 1.542 Soda .362 H2O + loss 5.705 P2 O5 Not better 1874. Crab Orchard Springs, Salts, put up by Crab- Orchard salts co. J B Wilder & Co. Louisville. 1875 Crab Orchard Salt. Arthur Peters Co. Louisville. Mag. Sulphate 54.842 60.627 Soda " 13.566 8.26 Pot ash " 2.707 2.814 Lime " 2,149 1,795 Litlula " .038 .028 Sodium chloride 2,954 1,874. Lime carb. .032 .018 Magn " .089 .036 Iron peroxid .078 .028 Silica .124 .118 Total of crystall- 23,421 24.402 Zation + loss 1874 1875-
Read Page
Page 23
Madison Cr. 1876. Potter's clay. Quality 1. Upper Silurian. Black, gruni E of Richm nd. A light soft grey clay with some ochreous stains + infiltration. 1876. Potter's clay. Quality 2. Same locality, of a bluish greyish, Silica 59.976 56.96 Al. Iron & mag. Oxid 27.640 28.74 Lime carb, .280 .20 Magnesia .606 .752 Pot ash 3.931 2.502 Soda .547 .315 Combined H2O loss 7.020 10.531 Nr Nr 1876a 1876b B atty Co. For Olympian & Spring see 1p. 17, (363 cut. 200's) 1989. Ferruginous Magnesia limestone. lime diath under Black Dermia shale, Lime carb, 54.06 Mag. Carb, 34.027 Iron carb, 11.532 or Os .006 Pot ash .143 Soda .040 Silica .280
Read Page
Page 24
Bath Cr. 2575. Inn Ore. from Carmel Rice, property of Captai M G Allen. Clint- Ore of yellowish brown color of usual struc- ture & clints ferric, 2576. Inn Ore from Burns' Lands, Clinton, Reddish. 2577. Inn Ore. Mrs Warren near head of Buck Run Bath Cr, Clinton. Ore of structure & clints clean, reddish brown clin, Inn Perox, 47.63 51.43 58.576 Al, 5.468 5.132 3.72 Lime carb, 14.560 13.08 15.16 Mag ’’ 9.974 9.444 4.528 P2O5 1.202 1.138 1.01 Silica 7.16 7.800 6.96 H2O expelled at 212 1.143 .693 1.607 CO2 H2O etc, 10.863 11.283 8.445 Cr of inn ---- | 36.001 40.999. NV NV 100 2575 2576 2577 Fleming Cr, Wells, see p 39, Part 3 A. Warren Cr, Wells ​see p. 129, Part 3 A.
Read Page
Page 25
Index, Black slate limestones Bullitt Co. Vol 2, OS, p. 141,-490 Madison G. Vol 4. OS, p 119.-888 Madison G. 4 OS, 212-1123 Nelson Co. 3. OS, 343-711 What are Black slate limestones? Coniferous limestones. Madison Co., Vol V., NS, p. 451, No. 2199. Madison Co. Vol V., NS, p. 451. No. 2200 Jefferson Co. Vol 4 OS. p. 195- Upper Sil? No. 1077. Jefferson Co. Vol 4, p. 195, Upper Sil.? 1078. Upper Silurian Niagan Bullitt Co., Vol 4. OS, p. 165. No. 856, 857 Estill Co. Vol 4 OS, p. 146-937. Garland Co. Vol 4. OS. p. 156,-985- Madison G. Vol 5. NS, p. 449 No. 2193-2194 2195 Nelson Co., Vol. 4, OS, p. 231. No. 1166 a, 1167. Jefferson Co. Vol 4, OS, p. 195- 1077-1081. Clinta. Batt. Co., Vol. 4, OS, p. 68.-796 797 Fleming Co. Vol 4, OS, p. 161.-973, Crab Orchard clay Madison Co., Vol V., NS, p. 445, No. 2169, 2170. p. 446, No 2186-2187, Upper Silurian marl clay. Jefferson Co., Vol 4, OS, p. 192. No. 1069, marly shale.
Read Page
Page 26
Br yle Cr. No. 2270. Chalybeate Mineral Water. From a well 8 ft deep, at the Camp Ground near Danville junction. E D Fr. 2271. Old Chalybeate Spring Water, on Knoxville branch of L & N R R, + half a mile from Danville junction, at Alum Springs. Joseph Maxwell 2272. Chalybeate Water. From the so-called Plump Gun Spring. Alum Springs. CO2 not est. Held in { Fe CO3 solution } Mg CO3 by CO2 { Ca CO3 Mg CO3 see next page. Fe SO4 Sulphate of Potash .1977 '' Lime .0235 '' Soda .2917 '' Ammonia .1521 Magnesium Chloride. .2250 Sodium '' Free H2SO4 Silica Undetermined + cmo No. 2270 Photo 5 B, RR cut at Brassfield. The Devonian forms 3 massive layers, and the cutting black shale forms the top layer, about as thick as the middle layer of Devonian limestone. Photo 6 B. Photo front side of 2 views, broken from road 4 mi W of Brassfield across RR & old drum valley to brine fence palmetto & forests toymud. Photo 1 C. Photo West side of preceding. Brassfield locality Devonian L. 15 ft clay - Gabil. celcine limestone, at west of first straight stretch after 1st bend SE? Brassfield orchard and inclined white layers also = tops m' clint distance E? fence within platters to distant 30-32 ft interval from m. f. skims l. to top of very massive Brassfield limestone.
Read Page
Page 27
No 2 C, Elkino limestone in BR cut, 2nd cut east after 1st turn SE of Brass field; 7 ft elkino L exposed with weathered clay on top. No 3 C, Elkino limestone, 11ft overhanging ledge. 3'0"4" elkino limestone? mud clay, Clay section Plum Creek. No 4 C. Photo. Elkino limestone 11 ft. Top thin marshell in 2 feet. 3'0"4" Elkino limestone thin overhanging ledge clay, Plum creek, No 5 C. Photo. Elkino lime- stone, all the more massive part is 9 feet wide; it will be exposed. Clay at time covered by rubble drift. No 6 C. Photo. Plum creek clay, 4 ft 3 in thick. Level line at base of clay. Projec- ting limestone at top. Corrected section from Brass- field to Pandola. Dermian: 15 ft testill clay 11 ft elkino t, after 2ft very thin. 3'0"4" elkino l. mine clay, 3 ft 3 in clay, Plum creek. 1'ft 10 in. Thin clay L, & clay. 2'6" Massive L. with 6-9 in volute repeat at top. Large crinoid heads here. Pholpiddella in large part 1 yard more large just above. 12'3" from top of crinoid head limestone to top of the very massive clay. 6" at least of very massive l. Difference in testill clay near Brassfield, and in clay over macro limestone near Pandola. 18 9.55 23.57 46. 71.5
Read Page
Page 28
Darne, Ky. up to Dormion, clay with out arg.shale 7½ ft abundant thin arg shale in clay, 10 ft water limnet me. 2 ft limnet me ---- 14½ ft est'll clay telern limestone w/lt. strckl and n'a near ly. A3 Plate One first layer + over- D7 Photo lying W. wrth great a trace of vertigin Cret ac ch and clay beneath the sand? Hugh Riddell about Met with not down to roofing. 4½ 162 10 LOC 65 & act of College Hill. Per. Almost me. 14 ft Wacry w/ vertigin clay, 8 in = 2 ft larger. 14 ft est'll clay, 11 ft {telern limestone estimated thm limnet me inter bedded at ba 4 ft 3 in. { Omm creek clay with 10 in mineral leads I met them {What fieldella bigger, m/lt large { larger is more marked, see belw chink me. The top of next layer. 5½ ft limnet me & clay inter bedded, 7½ ft well bedded Chinkery gr'ey clay, 16 in. massive base of Chinkary 33 ft. whistly, oyster, cement claygy. sedim lagated. 1½ ft heavy lamella calc aren cut entirely {sgr & well bedded. 84 ft Is large heavy layers, all sandey, 67 ft telern al. up to expense. { 3 in. limnet me, small ext rooted Hyphlophy. 9 in clay rock. 1½ ft massive limnet me. 18½ ft shaly rock, thickeded. No lynx. - 6½ ft lynx not rare 15 ft lynx very few? 10 ft lynx real common but not ohy common as in Mt Om- brain elsewhere.
Read Page
Page 29
Photo'd taken from road south of where road to Miami City turns off, N of College Hill looking east across Pineyplains towards Bay City. 67 A North of College Hill N of where road clearly turns off to Jackson Ferry, 17½ ft Devonian upper part on, 5" clay 6½ft thin li with wacr from 2' 5½" clay, no fossils noticed, 6 in limest = 2" ft Layer now with strong faunericidal markings, 8½" clay, intercal. 7½"ellowish cl. with Shucklamden at top, estimated thick- ess {2 ft 6" Plumm creek clay 3" limestone 6" clay 6" clay + limestone} 66 B. No side of valley N of College Hill 1ft like blue oolitic rock, 9 in black shale 3ft limrock with canada gallcom m's 4ft chert abundant, corals 2½ ft white crin. limestone with 10 ft light from massive Devonian fossils few, Dr Spring has within 2 ft of face. 60 S A wacr, south of street, 50p hills, 11"ft base of Devonian 7½ ft Wacr limest oner 18 in. 2" ft layer. 13 ft Estell clay, 5½" thin bedded shelly cl & cl, 3ft 6in rather heavy telloviscl, 6ft intervaal shelly Plumm creek c 2½ ft White pudding lage. 1ft large crinoid headon f reeke.
Read Page
Page 30
"1/2 mil West of Tunnel N.Y William, Garrard } 75 1/2 ft Middlet } Switzerland ) 12 1/2 ft. } 197 ft. What type? such like the Garrard = apparently int. elevated wth. Strethmann, Grayson Illinois. 5 1/2 ft limit line layou wth 10ft lateral contact me? 60 ft to Marvin Trenby limso. 5 1/2 ft to next fence. wille section, and Garret Gate as in map. fence east of Stephs. 8 1/2 ft to base of Garrard SS. This [illegible] Recessual builder at top wth 113 feet from Catherys top to forest fence. I did not plot on how to have to check up Sublities. Strephs seems there a just Up 4 dreamy L, with clay pellets + behind to Le top of Catherys = 10 ft above RR at first cut N.Y bridge 54. and this is same level as E end y bridge 54. No plot and notes below but an plenty above. William, Ky. Middlet Lura when red in measured along RR with err correction in dlp., = 93 1/2 Correct thickness = 12.1 1/2 Dip = 2.8 ft. Photo 3D = Base of Garrard, 7ft up to 2nd RR crossing E y G Millin. = locality 87. = Base of Garrard. 12ft up to RR cross E y G William. 3 ft up to RR crossing George Williams, 17ft up to bridge 12 ft up, to bridge G 1. 10 1/2 ft up to bridge 60. 3 1/2 ft up to tressle 59. same elevation at William Station as at W end of my note next below in other notes. 2 1/2 ft up to W end y switch. Bridges 56 & 57 at about same level as east end y Tunnel, East end y Tunnel = about 25 1/2 ft. above base of N.Yca. Base y Tunnel: about 18 ft above base of N.Yca. West end y Tunnel Bridge 55 = about 11ft above base of N.Yca,
Read Page
Page 31
Richmond & West 16½ ft, same kind of rock as below up to RR depot at Richmond 22 ft reddish clay rock Lynx fairly common at base. Up to bridge across R.R. 1 mile by Richmond 33 feet very rough arg. Irish Lynx not specially common. From here rather few smart joints at T 13 ft. Very single stone Lynx fairly common, rough like Lynx red. 22 ft clay rock, mostly few and W occasional Lynx, slightly like Lynx beds. x 16½ ft thin shale, clay, or possibly clay up in Argosville section. 5½ ft with rhyncholeavy abundant, 5½ ft beds with With Rhynchochela & Lynx. like Lynx beds, Resembles Lynx beds. 5½ ft Lynx, similar to type. (rock with few sharp mayonilline) or that the great bed is 2 of this many. U 3 miles west of Richmond to next locality W.Bridy 68 22 to 27 ft up 6 Bridge, With in Strp. shale beds near mayochut 18 and 1½ of Will Park S½ RR cut, 28 ft & around base at 2nd R.R crossing east of G. Williams to V 34 Wilks Point, many beds with Strpsh. Mayonilline m. Totals 95 ft Cathups tip. 12½ Witten tip Sec 87 9¾ Ganau tip Sec 86 28 Strife tip Sec U
Read Page
Page 32
Black sulphur water. Iron cont + H2S in contact with air decompose + produce the black sulphide of iron; should be used only fresh at spring. Sulphur water. Mineralable = with minimum sulphide. Chalybeate waters Bicarbonate of iron, sulphat waters. Fresh at Spring, Chalybeate Sulphate of iron. Saline waters Sodium chloride. Saline water Sulphates chiefly. Bryle Co. No 2270 Chalybeate Mineral Water, Well & 1/2 deep at Camp G and near Danville Junction, 2271. Old Chalybeate Spring Water. Alma Springs, 1/2 mile from junction on T.F.R. 2272. Chopfower Spring at Alma Springs. 2273. Small basin about 50 yds from 2270 2274. Bred well 40 ft deep, about 150 yds from 2270. 2275 Black Sulphur Water! Alma Springs, 1/2 mile from Danville Junction, 2276. Black Sulphur Water, Linney's well = Spring, at Linnietta Springs, formerly called Central Ry. Camp & Grounds. 2277. Peterslem Spring, well 8 ft deep, at Alma Springs; 2278. Oppea Mineral Water, Salus Spring at Linnietta Springs.
Read Page
Page 33
Bygle Co 2279, Rattles Spring, at Finnietta Springs, 2280, Peters' Spring, Finnietta Springs, 2280 A. dart well, 40ft deep. 300-400 yds from junction City depot, D. Finnelle, and about 41 yds from 2279 2280 B. Partus Well, 10ft deep, well at Finnietta Springs, Clark Co 2471, Magnesium Mineral Water, at Ridgville, J.E. Graves, 2472, Oil Spring, near Gulf- grove, A.M. Easton. One acre ground Corner of Blackledge 2473 Chalybeate Spring, Stratts Mill, near Gull Grove, near Austin City, 2474, Bride Spring, at Stratt's Mill, Multiple acid. 2474 (bis) Pure Sulphur water. C.C. & Easton, near Gulf Grove, Black dale, W.M. Kinney.
Read Page
Page 34
Nr 856, Lime stone on H C Pim- dell farm, Bullitt Cr. Ken n at Gap of the Rurks, Wjpeu Silurian Fossils. Nr 857 Myfan Sulphian. NR 856 NR 857 CaCr3 50.98 52.88 My Cr3 37.74 37.57) Al + oxides of Fe + Mn 2.70 1.640 P2O5 Trace Trace H2SO4 Wast, .067 Potash .463 .270 Soda .226 .198 Silica + mal. silicate 6.380 5.98 Water + loss 1.504 1.388 888 Limestone Trace of Black slate, Clarke Cr. Ky., The dense calcareous portion of the gray black slate, found also in Madison Bath Pwell, Estill, tc. CaCO3 40.280 MgCO3 15.903 Al. oxides of Fe and Mn + phosphates 9.460 H2SO4 1.025- Potash .436 Soda .164 Silica + med. Silicates 23.180 Bituminous matter 9.552. Water + loss
Read Page
Page 35
889. Sandst memith v:l, J may Marcellus shale, Oil Springs, Clarke Gr, 12 dark grey L. with ots Sil- calcareous spar, fine grani- tite impregnated with fluid bitumen. Weathered sur- faces of a dull buff col. CaCO3 56.76 Mg CO3 21.302 Al Oxiding Fe+ Mn 11.260 P2O5 .438 H2SO4 .372 O Ash .193 Soda .103 Silica (hard, old) 2.480 Bituminous matter Tot & Loss 7.092 946. Clay, Pitters clay? 4 mile NW of Irvine in the Pittsmd township, Centre. Light buff clay with streaks of red earth. Appears to be principally fine quartz-sand with a few minute specks of decaying mica. Silica 71.75 Al. 17.58 Oxyd Fe 2.420 Lime, none Magnesia .547 H2SO4 .112 O Ash 2.271 Soda .322. H2 expelled at red heat 4.400 Total .568 23.57 ft to 10 miles, 324 steps. 32.4 2.35 1.620 972 648 5280) 6.142 (1.44 miles 5250 23340 21120 22.200
Read Page
Page 36
947. Building stone. 5 miles from Driese, on th Richmond turnpike, Estill c. Dark gray, fine grained, many small scales of mica, Ca CO3 41.380 Mg Cr3 3.019 Comb'd Fe 4.321 Oxided Fe 2.365 Al .806 Brown Oxide of Mn .480 B2 O3 .374 H2 SO4 1.471 Clark .482 Soda .019 Silica + Insol'd Mat. 18.680 973 Magnesium limestone on Clinton, Hillsborough. Dull, dirty - buff, impure, with round beads, much scale of mica, & brownish streaks of oxide of iron. 973 Ca CO3 = 42.680 71.700 Mg CO3 = 25.358 9.931 Fe CO3 5.115-5 Mn Cr3 .421 Oxided Fe = 11.073 Al. 1.060 B2 O3- .848 .630 H2 SO4 .324 .337 S Ark. .290 .371 Soda .033 .139 Silicate Insol'd 10.580 2.88 H2 O & Loss 1.858 1.872 Brown Oxide of Mn al. 12.24 al. Nr674. Yellow Red Brown earth, on ensergetal C. 1/2 m. E of Mt Carmel, Fleming c.
Read Page
Page 37
1068 Banded Building Stone 75 ft above Dean Marsh Near the Court house at Granville Ry. = Madison Red. CaC13 45,880 My CrO 22,911 Al. Oxid Fe + Mn.. 5,760 P2O5 .220 H2SO4 .269 R2CO3 .347 SrO ..372 Silica reduced trilby reductg Cont. of Srde 3,00 Inert silica 18,520 H2O + loss 2,721 1068 1069, 26,88 1,687 7,260 .694 .406 .965 .012 silica) 59,90 2,196 1069 Marl Iron, Chewnick creek Jefferson Crk. Greensh grey, clay like substance, 1083, Saline efflorescence on cypruses from Devonian Black slate, near David town End., 5 mi from Clarks- mj. Ferris Cr. Ry. yellowish white. Sulphate of Al, 25,585 of Fe 15,653 " " of My 1,000 " " of alkaline Subst. 8,000 Slate (Impurities) + Invertible parts 1,000 H2O + loss 48,762
Read Page
Page 38
1085 Yellow Magnesian limestone, under Silicia, Salt lick Creek, 4 miles above Clark's dam, Lewis Cr. R2, Brownish buff Ferruginous l. Full of small cysts & ex- terior surface or scales to be scratched off a nail. 1086. Sandstone of handsome dark-buff cyl. at fork of Salt Lick Creek, Adam Bantam farm, Lewis Cr. 1085 1086 CaO of Ca. 55.240 trace " Mg. 27.820 .732 Al. oxid Fe & Mn 12.280 51.800 Pr ox .207 .118 H2O by .152 .200 Potash .163 trace Srde .124 trace Sulph. third calc. 2.500 96.920 H2O loss 1.428 2.230 1122. Peters clay marl, W. 1123. Magnesian limestone, good building at me, from Wm. Corrigins farm, at Kellity's Madison Co. 1124 Black shale, plates of black marl Co. 1122 1123 1124. silica 62.58 silica= . al. 21.98 al.oxid Fe 63.120 oxi. of Fe 4.78 +Mn. 29.60 ) 8.560 Glauber trace CaCO3-30.729 CaO+Ca 11.180 Magnesia 11.76 2.0034 oxides of alumina Pr Ox matt. .271 .143 H2SO4 .234 .509 16.53 Peroxide 2.607 .374 1.343 Srde .500 .058 Bitumatter Hydroxides at red heat 6.140 14.180 +H2O= 1.599 12.00
Read Page
Page 39
Lime beds near edge of Main & Fleming Crs. 1181, 1132, 1133, 1131 1132 1133 CaCO3 75.44 87.98 77.34 Mg CO3 4.283 1.721 2.309 Al Ox FeOx 3.751 2.200 3.910 PbS .409 .348 .310 H2SO4 .474 .373 2.423(Fe) Pyrite .540 .289 .424 SiO2 .292 .047 .068 Siliceous material 14.44 6.38 13.98 Yrns .663 .666 Melon Cr Magnesian Limestone, 1165 B & detention green way. 1166 Rolling Fork, Upper Hill 1167 Mr Tinkmans building 2d Ave, Melon Cr,
Read Page
Page 40
Melena Co. [illegible] one from the Turnpike Head of [illegible] Creek. CaCO3 93.98 Mg CO3 2.797 Al, Ox of Fd Min .264 BrO5 .054 H2SO4 .338 Potash .189 Soda trace Silicated oil, 3.040 Scotts Hill, in Trimmble Co. Stems: Madison beds + [illegible] copax, Streph. [illegible], [illegible] metacony, D., orthos nitgua. Acet n. + [illegible]mnia metile acide. & mends Hill Kentucky river. Carroll Co. New toll gate near New Gilbert is [illegible] emacerata + Streph., W.agrillanodes. 720 340 235 235 ----- ----- 3850 1700 2310 1020 1540 680 5280) 18.0940' (342) 15840 .15/5280) 799.00(.157 22450 5250 21120 27160 14300 26406 7000
Read Page
Page 41
Round to Raywick, Col. J.B. Wather, 1¾ mi. west of centre of Lelamr, 's new' Weery when road turns off north. N20°W from house to gully or quilled mtn, near lower part of which, 62 feet below the level of the house is found top of 1 Platy strata a lynx range. About 5½ ft. below this we can Rhynechthema dentatum, and 2 feet lower is found Left hand shelvedridals. The creek mount is surely 10 feet lower, but this was not measured. Rhynchotoma dentatum was found also in RR cut on N side of the rail road NW of this locality, M.F. Pale, 340 steps to forks of road 77) 340 (4.4x11= 308 4.4 2½) 4.84 dip of 48 ft 11'0" total dip = 58ft 16½ ft from fence up to large hyrgrain Hingle C Bs own, 2¼ miles due from C not three mi. Lelamr, dire by opposite to the principal Devonian mentioned below. Principal light grey Devonian l. (37ft Psndro-Madiarn, clay shale, bedded, 4½t with fully fossils including Paraferra-Pichum, ½t clay shale. Paraferra 3½ft clay shale top range of Pl. lynx, 41 ft thicknessy Black Shale wry high Bannn at my track. at Factory road. a dip of 11 ft in 77 steps, N 77) 770 steps (10x11= 110ft dip.) Up a gully S.E. of Bar Darty E of highest part of hill S of Church, 25ft to top of hill. Devonian chert linn and down to next part - rudules. 143 ft up to Platy sta felicia highest ridge 5½t whitish l. Rafinesquinia. 5½t blue l. 5½t blue l. with strph + Pl. lynx, 5 ½ t up to S strph ways in blue limestone 5½ ft creek up to Straphimena rugosa linn in blue limestone one.
Read Page
Page 42
Rhynchothrema deptatum, about 1 mile south of Vincelo, on east side of Carey creek, and is side of branch trip- ting into Carey Creek, on top of a hill, and probably is 2 mile from south of a branch, a cabin is situated op- pposite the locality at the N side of the branch, and a house is nearer head in the branch, I easily found on top of a ridge that extends between this branch and a branch which is larger and further south. The locality is south of the local by when Dr. J. M. Crum just attended but few Depriciana are found with these. associated with Rh. deptatum = split ended form of Pl. lynx, Alex Pl. Acadillei aty, W F Pate. Lynsey, a Velem near Bloom- field, W F Pate saw some specimens near Bloomfield. P Leptaena Menintri depts, about 1 1/2 and SE of Camillass Grahamen, which is about 4 miles from DeLavan on the D canal side jades, Town along a country road SE, and 1 1/2 mile down that road turns sharply to left crosses a branch 3/4 mi in this branch above the road crossing. Formed on S side of a little branch emptying into big branch just E. Strophomena sulcata, at distillery in Bristol Bards Town Road about 12 mi W of Bardstown. At foot of Long Hill 4 mi E of Bardstown on Springfield pike, At top of long hill on RR west of Beech Fork, from Springfield to Bardstown.
Read Page
Page 43
"O" [illegible] "linnneyi" 2 1/2 mi (?) in jakes short distance from the RR from Springfield toward Boardman, The stream to the W of RR. The jake is near the RR just past E of 2 and RR. The RR int can be seen directly from the jake, and a large tree stand in the west of the jake. There is a water gate nearby [illegible]. Beatrissa ( "californio"?) in quarry as you go down the hill to bridge over Rolling Fork, on the route to Brad- furtenville, 6 miles from Delawon, on N side of road before reaching Rolling Fork 1 mile from ) Deep Creek, Beatrissa may in the head waters of Abbe Stokes Not on creek but on one of its branches. I think proper matter. Pematophila quaduplicata ad W.F. Pate thinks thus: I said to have been a from from near Paris, Pematophila graminifera Pate thinks he has a specimen. Githis elytra 18-24 feet above the Birdseye, Millville in Woodford county! The jet Pike leaves the Old Cross jake in the bottom of a branch 200 yds from intersection with Old Cross jake. Hundreds of fine spec are found in very thick elevages. at old reservoir just bgn the park and E of Peak, Mill jake, near Frank- fork. And almost everywhere at this limiton.
Read Page
Page 44
R D Murrell on Caney Creek road, From here .144 miles North to main exposure of which is believed to be lowest exposure along creek. Clayg rock with interbedded limestone not aiming strath magnillensis, R D Murrell = .367 miles from forks of Caney creek North of line. From Forks of road: .151 miles to line of chalky gully where I made my section, 18th July. From Forks of road: .493 miles to next forks of road northward, 10ft rise road. From R D Murrell to forks of road where B myt and road & Bethelca road meet = .860 miles. 12 ft from lowest exposure at Forks of Caney North of R D Murrell to top of strongly conglomerated layers, 16ft further up to base of gully, section = 28 yd from lowest point where outcrops exposed at fork of road N of R D Murrell to base of gully section. 22 ft divide road gully section to next fork northward, Dip and cal culated at 110ft. Total = 132 ft, from gully to forks of road. 26 ft measured with out regard to dip from forks of road to top of clayg with 10ft. Lynx formation To nodules at top of lower Infer- ior face of Bichmond = 8 ft. mile, total = 34 ft, Dip and calculated at 13 ft. Gr and total = 47 ft = Forks to nodules. 182 ft from gully to forks 179 ft from gully to nodules calculated. 170 ft measured vertically The top of the Warren, in about 20ft, is either soft clay rock. The next lower part is the hard, dense blue clay limestone containing sharp conchoderma, with cerat, etc, which form the fossil silicified, which occur on the little summits at Murrells to, just beneath the Devonian Nodules. 41 ft Underlies of Black Shale
Read Page
Page 45
826 Paris 794 Millers Bay 842 Cross leaded Henry L in Cather 810 Cross leaded l in the gathropies. 826 Carlsade 845 Cl'tam limits 860 Tunnel 810 Base of Massive Middle Eden 765 Try of Cathay, 660 Myers Parkers Hill 612 Bridge over Yicking. 631 Try of Catherp 615 Pleasant Valley 706 Tunnel 725 Tunnel 885 Carran 645 Spring 35 Nestim 52 Johnson 55 Helena 520 Mill Creek 578 Marshall 735 Bridge 802 Summit Spleen Outlet or in of direct valve. (Dalmamella giposa, ?) specimen 11 ft clay + limestone. No lypx. 8 1/2 ft limestone with lypx, on then the Mt Anbrun S. 22 ft only exposed, partially c & cl, limestone Lypx beds always blue above the cave level and are over at bottom. This appears to be 24 ft of direct, white grained lypx only 25 1/2 fine lypx foot opening to summit. 8 1/2 ft typical lypx comes up to this level above the river.
Read Page
Page 46
First cut W of Pendleton Station Banded Madonna. First cut E of Pendleton Station Well bedded clay rock with inclined strata, Cut runs N to S. Three for film horizontally, at lower endy cut there is well bedded sand, clay rock with fossils very few and poor W-sign 2nd cut E of Pendleton Thin clay layers with badly weathered thin limestone with Streptelas ma. Fossils very poor. At E end of cut = massive 2 foot layer of blue limestone with Streptelasma, planuloma, 3rd exposure E side of RR contains Tetradiella, striiformis Spe. large Spirina & Discala just below thin 2 foot limestone. About 5-6 ft. below the left Edge of limestone about 18 specimen of zygospira kentuckiensis were found, 4th cut shows Pendleton shales Labeclia 5th cut shows Tetradiella & Glimma- nia near top W-end. The Climacaria has the septae carving clear to the centre and therefore may be alveolata, but the cells are large and it may be a new species. Resembles C macrod specimen. Climax maria crurum. See section 5 south of Salt River for this limestone. The Prasinella is very large, some specimens 3 in in diameter. Top of Ukraine - cut E 4 times as left of road. Leptaea nodulosa 7 ft. of top of next cut. Discotroza farthedown. Leptaea common at next little cut in limestone at top of cut, In next cut very, much more above, Discotroza returns again just above this limestone. The Leptaea abandoned in their preceding cut occurred at least 6 ft higher up.
Read Page
Page 47
Pendleton, Going East. 8 ft Bone of Mason's Madison (spalling clay) 3 1/2 ft {Well bedded, rather thin bedded 2 ft Intermediate layers (sands from Neb and Iowa fault) {Contains Strepelasma in middle part} but good decayed. {After my, especially in Lynn} {Thin bedded limestones from.} 11ft = 17 ft by actual measurement now. Semmn., also Strph. plummulum 1 1/2 ft Ill assorted, with Strepelasma {Nerada Tetradium = Bill Buckwheat} 5 ft {Clay with Liripia, with trifolium, <-by gypsum neutralization horizon {in a clay mudhole} 13 ft {Tetradium in clayrock nothing 4ft Clay rock, from half up alling. I Brazzera and Debitella gigantea 4 1/2 Dark clay in clay rock, Yabchua, Large 7 ft., clay rich, 3 1/2 ft Darker clay interbedded with clayrock 5 ft Light greenish grey clay. 1 1/2 ft {Chlamydo-chiffis in lower part {Thickening of Chlamydo and Liripia, {Smith Yabchua, Large Brazzera 2 1/2 ft {Up to Chlamydania Layer, associated {Layer but is not regular. 5 1/2 ft {Very clayey, corresponds to cordular {type} {blue limestone of typical Weston 2 2. ft (up to top of fresh forms clayey) 6 ft up to me strag Leptaena in clay shale, 2 ft up to Debitella retusa, excellent ope. Leptaena communis limestone. Pendleton - page No. dim not measur adian. James Richmond, needs correcting. De Morthis, No Lyx.
Read Page
Page 48
No text detected
Read Page
Page 49
Pendleton. Going east. Bore of Masson's Madison. {spelling clay} 8 ft Well bedded, rather than bedded 3 ft Intermediate layers. T fossils ferns, N and dark joints Continous Striped clays in middle part, but quite decayed, 12 ft {fossils, especially in lower thin bedded limestone front. 17ft = 17 ft by actual measurement. Sewer man, also Strath. blamundon. 1 1/2 ft [Masson's] with Streltelaena { Norella? } Etradian = Bull beck ridin' 5 ft {clay with Lepraria, with trirams, < Zygasparus breunichis and horiz { in a clay marble} 13ft {Tracium in decayed weather. 4ft Clay rock, from half of alling. 1 Brazzera and Nebatell's grimate 4ft Dark clay in clay rock, Yalechra, large 7 ft, Clay rock, 3 1/2 ft Darker clay in bedded with clay rock 5 ft Light greenish grey clay 1 1/2 ft {Aluminum shiffs in lower part { Thickerings of Columnaria design, { Smith Yaledora, Large Bracifera 2 1/2 ft [nj] to Columnaria's layer, are also { layers but is not irregular. 5 1/2 ft (very clayey, corresponds to circular style {blue limestones of typical Writon 22 ft {up to top of fossil forms. Clayey} 6 ft up to me strong Leptasma in clay shale, 2 ft up to Dinotus retusa, excellent spe. Leptasma communis limestone Pendleton - page M Masson's Madison not measured {mine clayey Madison, 2 3 ft, corrected, 18 1/2 ft corrected for dip Jasiliams Richmond, 51 ft not corrected 28 ft, generally needs correcting. Dinorthus. No lyx.
Read Page
Page 50
H.C. Black, Bedford, Ky. On S side of Corn Creek, about 4 miles from Bedford, fine exposure from top of Madison ward by spiritual Silurian down to Trenton, thin limestone in clay with Pla. caprea, Steph. acmaea, Dimenz. quadrata, Black, service forms. Steph. velata, 6 1/2 ft from creek to base of Clinton, 74 1/2 ft to top of basal Osmond, 16 ft to top of ridge, recovered in N side, Laurel limestone well ex- pored farther north and far upward which is a little over 5 miles farther north, Half a mile farther north, on the S side of the south fork of Corn Creek, the Madison rock is well exposed on the east side of the road, exposure about N & S. 5 1/2 miles to Bedford, 27 1/2 ft from rock with Steph. velata to base of Magnesian Madison, 32 feet more to top of an arcuate Silurian exposed. Top of basal Os- mond is at least 6 feet up. Clinton plainly exposed. 27 1/2 ft to first layer of Limestone, the face of the Limestone occurs below this, 70 ft to top of ridge, but no exposure. 5 ft. Clinton like rock, 1 foot addi- tional rock at base resembling the same. Beneath this is indicated Madison, Magn. Formable contact between line of Clinton + top of Madis-on or that within 15 ft the thickness of the Clinton is about 3 1/2 feet, the lower part being gone where there was an elevation in the Madison. Dimenz. reticulata: 24 ft below rock layer containing Steph. probably Concentricus; looks very much like good vertical view of this species, also several small Dalmanella fissosa, like from former considered typical. 11 feet above this to the Lymnea etc. lected. The rock here is,
Read Page
Page 51
irregular and resclnful that I have this time called Wasen Mr Dalmanella seen / 5½ ft up to layer looks like Wassen with Kucina, last words, to, 7ft further up in Dalmarella abroad and in rather thin line of me shivers, formerly called Layer of Richmond,) Septaena Shimbriddis was found 2 ft lower in layer with plenty of Refines quinnagot on edge, By this I mean lower than Dinmitis returning. Retina layers in a same level, a bridge. Mr ends noticed at back of madism at within 4 Cobs rich crossings while the grad was good, it even in the incline down to Milton. Opposite W. this Barilli's home is a gully and at head of this gully, about two thirds is the Dinmitis returne locality! Dinmitis retoma lignum is 2 ft. 9 in. thick. Kendal's branch. Milliners, Aug 30th W. V. p. 378: Believe Black shale sediment was derived from Cincinnati platian along the black shale at top at Savage Corners and melted Coniferous forests while at the same period far Appalachian side of Cumberland channel there was sediments of a differ- it character. George H. Girty ! 1898. Carl Springs, in Guilbfort Creek 2 mi SE of Indian Fields, Clark Co. Ky, Lingula (Lingula)fordii William. circa, n. sp. Leiohyulus gradicatala Vancsen Pleurodus armatus, Blade Sprangites Harmensis, Dawson? 7 Dalmanella alba data. Strigph., Nucula quadridens Gyn Lingula 11ft mediae. Retoma — 2½ ft Septaena Shimbriddis Ref. n. edy. plus
Read Page
Page 52
2 m. - 5 my Jeffersonville, Montgomery Co. Simulifera Williamsoni, Orticylidae sp. Quina guadalupatensis, ? Monstula, f. Bashfordi, Hall m? Plett. afra cralis, nsp. Spargis (Turnerus) Davan? Ligua williamsonia, Berea Ky., Van Vechten, = Lingula spatulata, p. a.s. N. Munximus Palmer's Fish & Game, Vol. XVII. January, Annals of the New York Academy of Science. I suspect they represent a ? gigantic Placoderm as yet undescribed 1889, Trans. N.Y. Acad. Science Vol. XVI. p 282-304 Bashford Dean.
Read Page
Page 53
Bored Well, Jefferson ton East, M. & E. Kline's Place. Silicic Acid 8.381 Calcium Sulphate 26.042 Magnesium Sulphate 61.700 Calcium Bicarbonate 89.635 Sodium Chloride 559.852 Magnesium Bicarbonate 17.956 Sodium Sulphate 1.194 Potassium Sulphate .324 Calcium Nitrate .255 Manganese Bicarbonate Trace Sodium Borate Trace Sulphuretted Hydrogen Gas 1.566 Iron Bicarbonate 1.003 Alumina 2.053 Sodium Phosphate Trace Bromide and Iodides Trace Free Carbonic Acid Gas 6.960 Lithia None Organic Matter None Total Solids 756,420
Read Page
Page 54
Benesereth Creek SE of Jefferson Town. 605 ft Strph retusa; Strpjt, very robust, Psilomea commun. 601-4t. Bridge Benesereth, 593+ t. Creek bed with Stroph. rare. Neobella + Platyst. common. On pipe to Fisherville, 675 Tpt of Strph retusa zone, 645 Tpt of Columnaria halli, in assoc 15 in- dies thick, mid-exp. forid. Main Neobelleta horizn. 625½ Massive clay rock-top, with Prasodpora hospitalis. 586 Columnaria alverlata. Tetradium in clayrock contains very many Prasopora hospitalis 85-77 576 Dist of Neobelleta & Platystrophia, 570 Sharply highest Platystrophia's lynx seen. What is in Warren cld? 540 Floyd's creek bed. Half mile west of Fisherville, along RR, at west end of switch. Platystrophia lynx. Abundant. Leptaena shumtridalis Abundant. Rhynchotroma dentatum 15 spcc. Alvania scalibra large. No Plectamblyites seen Some of the Pl. lyinx specimens are also- tightly above the level at which Leptaena shumtridalis is most abundant, Tyclimena = large Amberin type, Calymmenae callicephalo, rather small; Calymmena callicephalo full size. Dalmanella like gwynne vanyalbe. Szelio's sp'gan, dorsal spine P'yramid. D. northis retroorda, 3 good spec. central intima, 2 ventral extera at water end of series of cutaways railroad level = ½ sec west of Fisherville, Large Columnaria alverlata - large cells not large crsalla, new form of pseudo Madram, just east of Floyd fork trestle. Met Floyd's bridge. At West end I first cut a zigzagger Kentuckianum, at top of heavy ledge. navigated by claggy limestone rubble fully formed on which secure Strophelasma, small. Neobelleta Platystrophia Mlving good branching tryx'para Strud. planumal mcd alifala
Read Page
Page 55
About 13 feet up is Columnaria's shell, forming bed. Measure- ment not very exact an account of dip. Section part 24 West of part 24 = white clayey framilifer, one section with, = section = 13 ft. unexcd. x Pictarea retusta cumanum. x Strigph. planctona, crunmm. x Plea mullata species. x Nebulella recerdentula median depths 2 in bypus middle shell and extending ring shells to front, Strigelaesma - ommel. x Strigela mesura retusta typical. Planchostoma copax, not sillovs Dimnthus ontgundrata. x Strigla. sulcata. Planchostoma copax, gutturo form, x Shepeldaema large, straight, 4 in. White nodular small calcareous nodule 5 1/2 ft. at top of Middle Richumna section. West of RR crossing signal board is more white clay rock with Strigelaesma retusa, Strigelaesma large. 25 ft. Thimbledee Madium, seal thickness not known an accunt of dip for which I tried to make ad plane, 12 1/2 ft Mason Madium, unexcd., 3 1/2 ft framilifer and thiz erad bed, thimbledee. 3 1/2 ft Top of Madium section. Masonic. 1 1/4 Clinton Nalginites ostelculatus, small tubes, Helisites ant tubulation, Overlead bridge on road to Pott's farm hinneedad. Miss Liddy Morry, home atop. clinton at RR = 715 ft judging from level on bridge, = 700 east of Liddy Morry 40 mile. Within part of massive madium seen 1 mi. east of Tucker's, Gosford clay in front cut west, Clinton top in bottom of gulley on right. 19 3/4 ft from Gosford Clay 5 1/2 ft Gosford limestone and Forest Land. 3 1/2 ft Upper Gosford Clay, 14 ft. I Land were simply denude bed with red oolite crytallized set into numerous large alline rounded masses, rock ballast by 17 in. 7 in. 15 in. 3 in. 11 in. 5 in. 2 2 in. = {10 over 12} x acting double ledge overlying layers weathered yellowish. rich. Photo 1: E.F. Tucker at N side of RR,
Read Page
Page 56
Contact between Ozford & Clinton just east of Kent 21. - 662 ft. Bred exposure of almost full beyond section beneath overhead bridge less than half a mile east of the Om entering Chanc- ell from ME, 1 mi. West of Tinter Next cut west, west of long fill, when RR curves northward there is massive banded Madison. But lizard clay is exposed N of RR, above RR track level = 1 mi East of Jefferson. Tucker J.M. Desire report, location of prominent buildings. 695 Jefferson 7 AM. 555 Fisherville 655 Charles 742 Switch east of Veedale 734 Veedale 715 Jones 722 RR crossing 715 Eleventh St. 700 Shelbyville. 8 AM, 702. Shelbyville, Strips. mayonillensis, comm m. Dalmanella emacrata comm m. at bridge and across Clear Creek. 790 Road corner 1 mi E of Shelbyville 805 J.A. Matthew's mail box - bu'ghest. front road. Strips. mayonillensis, comm m, Dalmanella emacrata comm m. Calligera nodosa. 2 1/2 mi, East of Shelbyville. Constellaria comm m. 760 Heavy limestone layers, down to 760 with Stl. mayonillensis Intertwined with sands, looking G and layers down to 745 at least; also Constit Lana, 735 In front of E. Pinkster, same fossils as above, in plenty of coarse grained limestone. Strips. phragm Williams, Constellaria etc. 730. Just east of E Pinkster no firmest are not plenty Dalmacilla emacrata & after Strips where mayonillensis. Below this level Dalmanella emacrata, very abundant in coarse limestone, but also in the sand G and thin beds. Strips. are layers illensis few but present. Platyz strips phragm Williams Johnson small. Observation comm m small.
Read Page
Page 57
702 Bridge level across Gunst creek, 9th G. M. Section at Gunst creek, 6 ft up to lowest Stagh. mayrillensis 13 ft up to bridge level, face of Nott's prs. 9½ft to top of heavy l, with D. emacrata. Gunst creek level abundant. .690 Base of not l type at Gunst bridge. 722 Bridge over Gunst creek at 10,15 770 S V S head. First house Ey bridges 740 At bridge over branch of Gunst creek, 4 mi E of Shelbyville. 726 To top of heavy rock, 2ft thick, like that considered at base of not l type section at Bridge over Gunst creek, but good strag. mayrillensis occurs beneath, with high occurence. 850 Plat. lyng abundant up to this level. 860 Camparatively impsiliforms sec- tion since last record, a and, appearing, up to R. A jamison, about 1 mi. West of Clay village, west of deep valley of branch of Tick creek, 43½mi East of Shelbyville. 847, Just before Machinery southend of sharp turn in road, 3¼mi Ws of Clay village. 805 Bridge east fork up bend. 815 ft Plat. lyng, very few, but large 17½ft up to bridge, ½ mi W of Clayville, creek level at bridge, with Strag. mayrillensis 5 ft above creek, in lumps full of hygrymae and few Strags. mayrillensis. Mr. Dolanmella noticed but my short stretch made here. This cannot be near upper part of Farm but where Plat. lyng and Strag. mayrillensis come close together. 875 road corner in Clayville at 12,15 888. Platysta? sp. plat. lyng layers, Planchartrema dentatum, What lens- you is this. Followed by layer of nodular saddle. 945. Apparently the same flat lyng layers as at 888. There appears to be a north and dip equal to that of the road between here and bottoming hill, Then there is rocks crossing the road with strike N 25 E, And dip 20 east. This strike cutting Stiglephmena mayrillensis. 985. Strag. splacated thick layer of limestone full of Dolanmella emacrata resembles the heavy bed here recorded above and at first considered as face of not l type bed. 1015. Sandy Garrend looking rock with limestone layers with Del. emacrata = ½th of first size
Read Page
Page 58
A slight dip in road of 15 ft feet on both side which is Hellatilla with Streptelasma ginning as it = apparently Streptelasma divar- cana. Also small Steps. Canaden. sis = Richmond, Thinfne fault here. Smith & Here cheat rubble ejectares, Possibly Richmond stuff hauled here? Do not know. 1040 ft Same 2andy & arrand stuff as up to last locality but the thin limestone layers have shor- Streph. magnivillerosi as well as Dalmacinnella emacerata, -Not Hype, 1085 Up to begin Georg Butler's farm in east side of road. Exposes chiefly a clayer stuff like we've seen. 11/12 At top of first ridge here road drops again. The cheat line appears to have dropped less and still to be embedded in residual clay. 1085 Dip to this level. No intercp. 1130 To top of next ridge. No outcrop. Have cheat at mid point in last half mile along road. Madden/prim 1055 To this point the road continues as a wage road, at its near west part there is an exposure of rock striking about N 70 E and dipping 80 N. Is this road rock. Following side road eastward, The exposures show up as calcuted like Duffin Layer. No bedding can be made out here. Rock of the same general nature shows up along the main ridge road going southward, chiefly central and chiefly. It is difficult to tell what is dip and what is all due to throwing. 1070 When road turned down, = plenty of the Madisen like rock, along the road goin' down. Here a byroad turns off up, little turned the west. This Madison like rock probably is the G arrand sandet me, To She no up to 1108. But at this level there is limestone in 2 andy thin slate. The limestone Can't show Seftelasma about out and Dalmacella emacerata few. Forther down too well the limestone contains smilings of animate ori- arrid beads. 950. Road Turns off NW to farme. To this point the rock strikes 3 with road and at my the road from first offpoint where the side road turns west up hill, at 1070. "939 Rock restricted appearing here. Dalmacella emacerata. Pleaundomts arrived. 920 J. B. Wellman, Along this road, between Wellman's home and his farm is Platystepha lygus, large in the road way. Robust kind once further in the Madison like rock inside and above
Read Page
Page 59
870, a short distance south of farm (Middlemans) along the road is thick lime limestone with Streptelasma; Richmond Strephoma planulata etc. mn. 890 a quarter of a mile S of Wildman's Plat. Lynx is abundant, Further south we collected rock again with Streptelasma and then, further south, rock striking about E+ W + dipping fully 40 degrees North. Slighly rotated. Particles retain a 840 here I turn off from creek road turned West. 752 Hemp Ridge) 700 Shellyville Barometer ap- pearantly changed but slightly Today, White Pike Fich crosses mud road from Sucker to Middleton, Clinton's at 655 about 5 ft Upper Cogord limestone. 3 1/2 ft Wyan Cogord Clay, Bed of main Laurel bed, at Mrs. Wilton's house corner 662 at Walter J wanis Road corner, 758 Inner Laurel, Upper Cogord clay 5 ft Upper Cogord L. 19 ft Lower Cogord clay 18th Clinton, Calam in Brown, High Led. Shady Grove. East end of Middle- time pike, west of last holloway 3 ft Wyan Cogord Clay 6 ft Upper Cogord limestone Inner Cogord clay. 1 1/2 yards clay. Edgar Coy quarry, 1 1/3 miles East of Abdenage on C+O RR, Inverville have only Gyp-o-chrome. 12 ft Walden clay, measured. 22 1/2 ft Laurel rock exposed above water, 10 1/2 ft shows up east of the quarry + its clay rocks exposed. We rock for building & crushed stone, $15,000 per year business.
Read Page
Page 60
Near 4 miles NE of LaGrange on L&NR S and inclining angle. Rest of Laurel sect with deled dol 20'" fine rock as at base of quarry E Anchor, Well bedded, 3-4 inch course approximately. 30' - brown clay upper. Photo 4,5,6. 70'" Oolitic limestone. Photos 2 & 3. Dip + measurements 1st. 23'06" from the top clay, estimated fin 106' Clinton. 10 Trachytic Madison. About 2 mi NE of LaGrange on L&N Railroad to 1 mile NE of La- Grange, From LaGrange Clinton is seen at Steam level at side of RR, = 1 mile NE of LaGrange. Further NE is seen Oolitic Clay Oolitic limestone and red upper Oolitic clay. The top of Lower group 60' about the elevation when walking "clay should come in judging from experience further NE. Hence there must be a fault near summit line with a throwing about 45 feet. The fine spring on N side of RR is ones from beneath bogged home-stone. LaGrange 8 mi to Westport, jukes. Brandtine by Mr. Hitt. East of LaGrange, on S mill, and at RR bed, at gun arrives. By rail not 4 turns. 12 in Clinton. Road ballast. 18 in ? 18 in ? Trachytic. Building Rock. 18 in? Saluda bed is quarried also at this point. Massive Saluda is seen used also by son North of La Grange, east of jukes, Charlie Runley's quarry at Sweezy Jeffersonville makes lower Laurel. j. w. Black quarry, 2 mi SW of Jeffersonville. Makes upper part of Laurel rock, especially three layers. 8 inches 11 inches 10 inches 8 inches 16 inches 5 in 5 in 5 in Level of Clinton directly south of Jeffersonville = 639 ft.
Read Page
Page 61
Concord Ky. Clinton base. 48 ft Upper Richmond, Lower front fossiliferae, How much of this is Sabuda? 57 ft Middle Richmond. 57 ft. Nebulella incompeta. 47 ft. Lower Richmond. 152 ft = Total Richmond. 5 ft down to Stephencradenei; 6½ ft down to Streptochasmae in Kearns beds. 36¼ ft down to Ochyrothromus dentatum & Design. 412. Gatchell & Sons, 1 square west of traction Station Saluda Lago, Sabuda iferous Bird de Bid. lluminogen mmi. Large Livipiza. fina Fentuckiana? pura St. Jude Bird. ria. ur one f Warrenia tho retro a Lugo.
Read Page
Page 62
Cacia,
Read Page
Page 63
Concord Ky. clinton face. 48 ft Upper Richmond, Lower part fossiliferous. How much of this is Salida? 57 ft Middle Richmond. 57 ft. Nebatella incompleta. 47 ft. Lower Richmond, 152 ft = Total Richmond. 5 ft above to Streptelasma. 6½ ft down to Streptelasma in Marble bed. 36½ ft down to Othyschotoma dentatum & Prism. 4/12. Gatchell & Sons, 1 square west of fraction station Candlet on P. 53° Massive Salida 23° Mucilag. Salida 18½° Fossiliferous Whit de Rock. mud. 1° 6″ Streptelasma layer 5° Giripformis, Large Lirapisa. Zygarkia Pentu Seleni. 36° 6″ Cluepora St. Louis Pika. murid. 1° 6″ Colemania. 8½ Nordulan dome f Warren rid at level. 28° Diasthis retrusa layer.
Read Page
Page 64
Harrod's creek, From traction bridge 200 ofts north to first wild smell south of road bridge, Traction bridge. 20 ft Nt exposed well. Limestone, Sand base. Only exposures (near top) Mefra Osford clay with Limestone interlidded California elegans Orthis flabellites 3" 6" { Zaphrentis Diplorastrina, Orting other species. Mefra brown clay wth Dictyonella, Encalyph. wcrinum, Septaene, Otopya reticulare, 6 ft Osford limestone. Lower foot is more clay limestone. Contained Halcyzites at lower third division 9 ft clay clay rock, Madison like) of gallery. 3ft chiefly pinkish clay 8ft 6in. Clay rock. Chintin with Orthis flabellites Rhizospina vennera. Florida Heights, 60ft from base of quarry to first not crop of Devonian limestone, but trip 50 ft of this section is not exposed. 55 ft up = Churchillian many jeli cate mss, abundant, Halcyzites Catculatus. Rocks more massive than in case of Sandel. White clay at top is residua al clay due to decay of limestone. 16ft from base of Quarry to R R level; where 8 ft fills belongs to Louisville form RR level = 439 8 ft = Walden according to frowan. Photo. 5, 517 Same quarry. 515 Devonian crists, 8½ Not well expred 15 ft wjfer quarry rock, better bedded + makes better build- ing rock. 36½ ft barn n main quarry, used for crushed rocks for road material 8ft too soft for road ma- terial. Blue 22project me a clay and = Walden.
Read Page
Page 65
1 2) 3) 4) 5) Anchorage July 9, '06. D 19 ft belm Freys Hill creyer is Derrinia Silurian contact. Plenty of corals within 5 feet above, = 672 ft above sea, P. Von Allman, East side of White creek, near Headwaters, shale strata leading east from Freys Hill. Louisville limestone with Pentam erous Margos + large Halcytes, = maxes? up to level of bridge = 720 at least. Derrinia not seen at all. Dr Herbert Cornell, quarry, 3 mile East of County line and 1 mi west of Pierre Valley, 1/2 mile N'W'th of R.R. Lower Louisville l. Waldron clay. Upper Laurel l. is quarried here. Well bedded layers, Failure east. Base of Waldron clay = 740 ft. Chrtm at 670 on Brunsboro ridge, east of Pierre Valley, Forky Hardred creek, 6) West of Pierre valley, branch of Hards Creek. Top of upper Oxford clay = 674. This indicates Chrtm at 644 about. 7) Quarry from W'thington N to Black Barde Base of Chrtm = 562. This is 130 ft film corner 691 in County line, and thin Silurian section = 60 yards. 85 562 647 30 145 ft about. silurian top should be not over 697 or 700 but as another foot Derrinia was found at Freys Hill, I really Louisville is not 60 ft thick here. water level of creek at bridge is about 470 Bridge level is 485. 15 ft from water level to Colunnaria Pennsylv. fms. found near base of Brideland. In this case looked like calcarea. Septarian found but 10 ft belm, this level or 5 ft down creek. Plenty of middle Silurian nubble on this clay bank. Good sea in a bit not standard. Colunnaria at 485 Base Chrtm at 562 475 Col. 77 ft & travel. 97
Read Page
Page 66
(NE) east of Black Bridge, [illegible] [illegible] transition edge of Silurian = 565 ft) 9. NE of Forks of Road from Black Bridge to Poplar Grove School house. 208 85 623 Doverian shingle, at 788 Louisville Limestone = 30 ft ? Top of Waldron at 678 Does the Louisville limestone thin out eastward? 10. Silurian up to 690 certain, No evidence of Doverian up to 712. 11. Doverian shelled 761 about a mile and a half east of Poplar Grove School house. 761 125 625 Bennetsville July (12) Doverian chert at 762 at 34 mi. NW 1/4 town in Poplar Grove on structure jute. Base of Waldron is at about 712. Hence thickness of Doveri vile here is about 38 ft. It again suggests thinning to the Bennettsville Limestone far to the East ? (13) On south sided valley, Waldron clay = 13 ft, well exposed. Doverian chert is found out 17 ft farther. Therefore Doverian away from bank than 30 ft above Waldron clay or at 12 as far as exposures are now shown. (14) Chert was exposed at 6 26, 2ft9in, upper brown clay, 16 1/2 ft lime & sand clay, 5 1/2 ft bry. limestone, 4 ft large Micropora. 12 in Silurian Doverian chert. 14 mi. transition. 28 ft medium marlstone 20 ft thin shelled Mediam, fossilifer, widely Hibbertella & syngrana, but also Silexellomera, Strept. retusa, Drepanorhina separa very large & get fossils 8 ft above bank w/ other clams at same level but not abundant about 2 ft.
Read Page
Page 67
12 ft Streph retusa & Dianthus anuligratus, not well exposed. Dr to determine limits but approximately correct. 8½ ft Tmmdo base, large Streptelasma sallum common & my left arm. 9 ft at face. Ostarea retusata Strepfld. asma 8 ft more clayey & front serves. 17 ft sandoidal clay arch, partly by the Psendr Madison. The face of this arch is at crossing of creek = 102½ ft below limit on face. Left alms V. mutridalis comes above by 1 this Psendr Madison. The large Liripis a begins 5 ft above face, Tmmdo nears at face. 8¾ft 10in Found 2 specimens of Calapedia in lower part of lowest fossilifer section, about 16 to 19 ft from creek, above the Leptaena chon- lirigals zone. Believed to be in silt. (5) Going up hill again. Deroni an clert is found at 701½ ft. Lairsville lined as = 17½ ft + about. And Walden clay is immediately beneath. 70½₀ -630. (6) 2 miles S E of Stay Light. 740 Dermon clert rubble within 5 ft q 719¾ = face of Walden. mb of Walden. 43 ft = Daniel - exact measurement 3ft = Upper Beyrd clay 70 5ft 4in = lower blmd me 16½ in = Lower Beyrd clay 719 12m = Basel Wagon 72 < 22m = Clint my, Salmon 64½ (18in = In mortum) 647 8 72 7.91 7.80 6.21 (7) Head of Morris Creek. Base of Walden = 719, 72 (5 up) Walden thence = 732 out Silenian cert arm up to 740. Mr Dermon clert seen, 64½ Base of Silenian = About 646 about. Among her is upper part of Daniel, Well bedded, plenty of chalk. Chalk is whitish. (8) New and I map, 767 Nadyphyllum 7 specimens: Dm, disintegrated. Hemolides finetua calyx 1 inch. Stimbrdes calyx 4/8 to ½ inch. shme of small masses common. Best anderna up to 765 at least 13 13 71 977
Read Page
Page 68
19) One and one half mile from Skylight to Hallos Landing. 654 Face of Waldron, According to this the face of St. Louis Mine should be at 580 and Deronian should be at "about 680" 20) 685 Top of Waldron. Base of Waldron is = 672 ft about, 14 ft Grinnville exposed, Base of Deronian about 700 21) 3/4 mile west of Skylight. Deronian Chert Abundant, 22) One mile NW of Shiloh Church 729 681 668 597 Deronian chert at 694, Grinnville estimated at 13 ft, 597 23) 1 1/2 miles SW of Antioch Church. On July. 715 Deronian chert w/it flaky byglum 24) 1 1/2 miles NW of great sink springs and in Smith side of Taylors creek, 675 = Deronian chert. Clearly corals, one Hydran hygclimus. 25) Smith & Taylors creek, Almy road, 6560 Deronian chert. Underlying Grinnville limestone at least 16" and probably 20 ft thick. Grinnville sh't also Pentamerus Hougas and Stromatides, 1 inch Corals, finely striated. This species appears common in lower 15 ft of Grinnville limestone. 73 101 17 26) Smith side of Sinking Fork, Almy road, 665 15"t Deronian limestone, Crabs, 5 1/2 Holgites in Grinnville limestone, 10 ft Massive Grinnville w/it Pentamerus. 22"t Ordinarly Grinnville limestone 27) Road Galena to Wolford Landing, 666 Der chert 12 ft further up, 63 ft Grinnville limest mke exposed 607 Top of Waldron. Glacial boulders quite numerous. 28) On Wolford road. 654 Deronian chert. 29) Near with end of Wolford road 566 13 553 11 49.2 566 Top of Waldron clay. 599 1/2 High led Grinnville exposure 630 = About where Der, should come in.
Read Page
Page 69
30) Humming landing road, Mary Goshen. Glacial pebbles & shale, granite gneiss, 31) Immediately above - Den cheat w/gniss. 645½ Devonian limestone w/ft crabs, 642 highest Limestone exposed with Stromatodes 1hr of Oalyces. 608 Limestone layers very persistent. The Waldron was not [illegible] typified line, but may be 25 ft. [illegible] down if the Louisville limestone in this neighborhood is 63ft thick. 32) SWest of Goshen 1½ mile, 678 Devonian limestone with spirogi & Encrinalites, w/ritm. The crab layer may be beneath. 33) 1½ miles SW of Goshen. 643 Devonian cheat, crabs, abundant. 34) Going up hill south of Pond creek, 642 Devonian crabs cheat. 622 Louisville w/ stromatodes. After Devonian is about 642 and plenty of Devonian cheat down to 630f. Not any hard beds, 35) Just before reaching road corner 647 2½ miles & northwest of Goshen. 635 Plenty of limestone w/ft Derv. crabs. 641 limestone w/ft Derv. hard joints. >>>>> Perfect <<<< 36) 1¼ miles NE of Prospect 598 Devonian limestone with plenty of Devonian crabs. 37) 1½ miles NE of Prospect. 628 Dev limestone & Corals. 38) ⅓ mile SW of Road crossing 647 614 Silurian limestone w/ft. Stromatodes. 39) 637 Dev cheat w/ft crabs. 578 44 ft Louisville, 71 15ft Waldron = 598 at base. / 508 40) 620 Dev limestone with plenty of crabs resting on Louisville limestone. 578 Top of Waldron. Thickness of Louisville: 42 ft 563 = 71 = 492
Read Page
Page 70
41 One mile SE of Harmony ending, DevL, Stiplemurid shells abundant. 16 ft Limestone, DevL with gssis. 5ft material {Dev limestone crabs abundant, 5 1/2 intervals [Devl crabs abundant - brnty. fossils seen here, Top of Louisville at abt 620 Louisville at least 57 ft thick, 42) Sml easty corner 647. Devonian with crabs large. 593 Top of Louisville, 43.) NW of bridge 494 in River Road near Hamrbly. Top of Waldron at 555 44) Near road corner just west of Harrods Cr. River Rd. 483 Base of Clinton, calcumhrous 3ft thick. just filled road corner. 45) East of bridge Harrods Cr. River Road 586 Base of Waldron clay. 46) 1/2 mi NW of Harrods Creek River Road, 552 Top of Waldron clay, 549 = about base of Waldron. 47) Half a mile West of Harrods Cr. River pike. 590 Base of Devl limestone in plenty of layer clays. about 43 ft - Louisville, 48) Waldron 14 ft thick 518 Base of Waldron. 532 = Top of Waldron. 5/8 71 447 620 57 5613 15 548 71 477
Read Page
Page 71
Jefferson ave. 49) 2 miles SE of Jefferson ave, 686 Clinton level, very carboniferal. 50) 683 Clinton base? lower exposed clay, good clints. 51) Between Ragn & Shrink's Branch, 689 Clinton base? 618 Crummania alveolata ? abundant. 612 Calapezia 611 Crummania calycina. 52) Mass of ht clay but not of the Clinton. No Clinton seen for last mile. 53) 664 Only main coal bed, alveolate? 44 ft lower is Calapezia & Crumman. 1/2 ft lower is streptelasma medulla. Calycina layer is lower still. 54) 595 Phyllotheca dentatum, Septena alpin-tricheti, Platystyle lynx. COH 5/15/61 55) 527 Septema alpin-tricheti Platystyla lynx Dimorphum retusa excellent. Dec. 56) 588 > immense masses of Calycina. some 2 ft wide and 1/30" thick. 596-2 Upon Crummania alveolata? layers, cores large 1 ft and abundant 598-2 Retred low layers abundant, Streptomen retusa & strephela mina. 619 Freely abundant up to Vau level. Farther up they are more scattered. 57) 2 ft 4 in salsum from clints. 3 ft lared triasema. From exposed clay 2ft grayblue w. 18 1/2" 18m, my sample 25 ft. 15th day, 5 1/2 exposed liment as 2 ft 9 in. Upon exposed clay. 677 T of Mjpy exposed clay. The bricks have been shipped down all along the road. While mud has been mined at dead level, good place for low exposed clay, Cedar fades above Jennisse from hill from Oxford.
Read Page
Page 72
58) About 2\/2 miles S of Jefferson Twp West of Cherritt Creek. Oxford limestone Lower Oxford clay, 2 ft basal Niagara. 648 -> Clint on. Regular type, 1/2 tracted ferric, 59) about 2 ft 6 in basal Niagara, 6 in Clint on Jefferson's lignite flora, 10-7 led, 17\/2 ft lower Oxford, 5 ft Oxford limestone, 2 ft 9 in Upper Oxford clay, 680 3 \/2 ft interval, = 648 ft for Clint on base. 60) Short house. 1\/2 miles West of Seaterville. 651 = base of Oxford limestone 17 1/2 ft = hidden out of Oxford clay lower. 633\/2 = top of basal Niagara, Oxford limestone was quarried here. 630 = base of Clint on. 61) Upper Oxford clay, Oxford limestone, Lower Oxford clay 3 ft Basal Niagara 2 ft Salmon brook Clinton -- about 612 62) 632 = top of Oxford limestone 604\/2 = Clint on base therefore 63) 2 ft up to Clint on base. 23 ft up = sandy stuff decayed up to 642 39 ft up = solid black lime -- up to 619? 23 ft up = up to 580? 5 ft up small Columnaria balls, Large calcina. 2 ft across. 3 \/2 ft up to top of basal Niagara, 19 ft interval up to gate = 660 correct as far as fence record goes, 660 = gate 641 = top of Oxford limestone. 3 \/2 ft Oxford L; base at 6-37\/2 18 ft Oxford clay lower. 5 ft (5 ft Clint on basal Niagara, not exposed) 62 ft interval. Columnaria layers, balls 5 ft interval large calcina. 2 ft across,
Read Page
Page 73
Jeffersonium 64) 599 Clinton base, 66 ft up to base of Clinton. 7½ ft up to Schrodium layer; Columnaria calcina, 65) 633 Up 1 bezrd limestone. 5 ft bezrd limestone. Bezrd clay brown, Clinton, all red shinn, AA) medium Weldian road. Clinton base 21 in. Turgation rock. 50 ft to base of frame thin rocks. 110 ft to tip of great coral reef, 9 in. heavy limestone lower gypsa. 13½ ft up to base of heavy c. Sunnams hike deposits 7½ ft up to layer with Spirulalayer? 26½ to top of clay rocks top of Weldian Dimulus reticulata layers sand, 66) 618 Clinton base East along RR is Rafinesquina alternata. film medium gray, Calciumare Billimund form, medium size and Heterella crassa straita in 17½ feet. Photo, 1. Quarry east of Tucker, Lower Laurel, about the lowest however. See former notes. Photos, 2,3. Osgrid formation at overhead bridge about 1¼ miles east of Jefferson inn, Photo, 4. Same as last but closer in side of open clay toward the west with very oblique almost horizontal fault plane, Photo 5. Florida Heights Inn's- nile limestone, 4 PM, Photo 6. Weldian Clay at quarry east of an damage.
Read Page
Page 74
Madison cl. mau 000 Dol. -Lio sp. -x x nrd. -Din. Dalm. gast, nrd, CMned Din Cfb, mediana vetus man Pendleton knd cribri zygoph. Salina colum nrd. Din Photo 1.2. Laurel limestone in grassy 1/2 east of Anding. In this quarry the top 17 ft. = building rock, other comes angler and good chiefly for cemented rock = about 13 ft. At base is little bedded shale = good building rock.
Read Page
Page 75
129 50 541 12 43 5 20 2 3 80 Bulletin 64 ce. Orth. Helix, Cole warrm Diml Calycina bed, 63) 57) 56) 57) ce. Tetrad. calye. half, calye. Din, 9 in 50) ce. 14) mean skin 7) E dult half calye. striptelas, strips C re ab almus Calyc, cal. edge, + half Rt berr + alum. helx helm.
Read Page
Page 76
Records 67) 2ft Coral Wagona. 20 in Clinton calamine linn, 673 - Face of Clinton, About 15 ft above level of main work is huge Colum- naria layer, with a sandy clay full of fossils beneath; these fossils middle Stcep- telmeria medium con- mom and me Portasia, Large Petrodom occurs alwy above the columnaria layer. 68) S E of Ostronoter, 3/4 mile, 686 Base of calamine from Chlton. 69) Silurian to very topy build but a few silicified Devonian fossils which must have dropped a considerable distance, otherwise this would have been much Dev. Shut here while it is the Siluria which in Chmra, up to the top, 750 Base of Waldson Top of hill 78 70 NE & Browns Inn. 5 1/2 ft. Igneville short above this level. 13ft Annsville with Port annus) (which could just have dropped) 16 1/2 ft to base of exposure of Johnsville 9 1/2 ft from road to face of Waldon. 71) 646 Base of Chinton 20 SWy Ostronomer, Monday week, 635 Base of Chinton Clinton - 2 ft 4 in Base Wagona - 3ft 1. 73 654 Top of basal limestone 74) 720 Devonian chert, enals + gregaria.
Read Page
Page 77
Shipped from July 19, 1906, Shepherdsville, Ky. 1) Waldron clay, Cox Quarry. 1½ mi East of Anchorage 2) Upper Laurel 0-17 ft bdm Waldron Cox Quarry 1½ miles Easty Anchorage 3) Clinton #67 locality, ½ miles NW by Beards 4) Louisville limestone, Building Ledges. 8-23ft bdm Dermin. Florida Heights quarry, 5) Louisville limestone, Road Ballast, 23-60 ft bdm Dermin., Florida Heights, Different mtn. July 21, 6) Cezord, upper 13ft, 1½ mile E of Jefferson mtn., at overhead Bridge 7) Cezord lower 5½ft. Northy Seaterville. 8) Cezord, upper 13 ft. Northy Seatmtnly 9) Lower Laurel quarry ¼ mi, East of Junction 10) Upper Cezord clay, above Cezord limestone. 11) Cezord limestone La Grange Shepherdsville lls. 75) Westy Flygods fork. 473 ft top of limestone exposures. Italy sites; Murfiddlella very small Centaurus Mr Strimbrodes. 6x prime extends from to 444' 29 ft. 76) Easty Flygods Fork, as far as line of G. De Hough. Same rock, 77) At crest crossed by grad, nodular stuff collected. Plinthatic? 78) Backy linnse in mm. R.F.B. Louisville l. with Enclichione numerous plications, manner from at 500 ft level; Mr Dern was seen, 79) West of G.W. Peacock, Louisville limestone with Enclichio manner and numerous plications collected. 80) "Bomeheirt's" home. S.liverian up to this level. Shelves strongly west. 81) 82) Pleasant Grove school house. limestone assumed to be Silurian 3 end mark = 577 ft but Silurian runs above this, 83) Silurian up to 600 ft level. 84
Read Page
Page 78
8 Pleasant Grove Church, Silurian at 530 Lyellia, Smith y Pleasant Grove Church, Waldron 19½ ft. Top of Waldron = 532 ft. Glenville = 48 ft. at least according my to this, 86) Ridgeway Ford (Chutes Ford) 16½ ft Waldron clay, 47½ ft Lancel limestone 21 in clay shale, Upper Oxford clay 7½ ft limestone getting clay. + toward base, exposed limestone, 87) Silurian limestone. J. A. Rigg. road corner. 88) Stamfordes farm, well preserved. Lyellia in short lime. 89 Silurian up to 640 at least. 90 William Cellies, Silurian. 91) From 617 to 631 = 14 ft clayey possibly Waldron but too faint exposed for certainty. 92) Good exposure of Waldron line from 614 up, 93) 631 - [face of] Waldron] Cedar cr 94) Oscar Cowers 640 = face of Waldron] 95) 648, face of Waldron, 96) 662 face of Waldron. 97) 26 in. Upper Oxford clay, 619 = top of Oxford limestone, 6 ft Oxford limestone. about 20 ft from Oxford clay well exposed, 98) Upper Oxford clay, well exposed. Oxford limestone, + top = 640 Lower Oxford clay 99) Fine exposure 532 617 64 42 46 8 570 18 430 402 562 35.4 22 36 450 538 430 522
Read Page
Page 79
Wt Washington 100) 670 base of Cayford limestone, 101) 707 = top of cayford limestone 102) 719 = tip of cayford limestone 103) On first 1 leaves. The Cayford limestone and liver Cayford clay are well exposed, 11 ft intercal level - top of section, 702 691 = top of Cayford limestone. 104. Cayford limestone, solid 1 ft. Cayford limestone weather. Laby 1ft. Cayford limestone 4ft massive, Cayford clay layer - 2.2 ft. Cedar glade 662 = Clinton trip, 3 ft facal Mazana 3 ft Clinton a clino form. 105) 684 Clinton tip, column brown, 106) 690 = top of calmer layer Clinton 107 Base of fossiliferous section. Heterophragm. 615 = top of pseudo-Madisonny - 2.7 ft 5.88 = lower endr Madisonny Modular Lagruttle - 2.2 ft with layers like Grand Madian rather sparse by scattered in it. Large limestone 2.2 ft. clay slubly 3 ft. 561 top of fossiliferous section, 3 intercalal of 3 ft. = Baryl Richmandy Nickle Large Platy. Lynx. Large quadrati form, absolutely fossiliferous - 2 ft also Riddman base of Nickle. Strange uns bedded limestone 2ft 6in. Shared extent of this limestone, con- tains large Olatz, lynx 3 ft very irregularly willy limestone, from top few except on surface if any layer near the tip, = fossil blotchy in form and section. Riddly fossiliferous, 7 ft. Leptaena trip of lineyze at which Leptaenas crinium, Olatzera plus very much elongated along longline as in my acutelineata for until I can not distinguish it. 14 ft interval poorly exposed, just a thly all my fossiliferous strata limestone stuff. field of loft as main judging from section east of Pipe handle Floyd and West y Fisherville along RR. Are the Rhy. ductatum worn in upper part of this section?
Read Page
Page 80
107) Continued, 543 D in other retusa lenticula, near clitella with leptacma obliqua ridgel Leptacma occurs me ft below at least. Line Columnaria fortilis delay between middle & Ann Rill ends. 108) 720 = top of Aggrad limestone, 109) top of lagrod limestone = 729 110) 705 = top red Aggrad limestone. But preceding records seem not reliable the should lead to top of largest layers of Lame nel since these limest layers occur in other periods above the Aggrad clay, and normally are 2 to 4 feet thick. Aggrad limestone 5½ ft. Gmu brown clay 25¼ ft. Basal Micajack 2ft Salina Clinton 3ft Cedar glades unit of here along Aggrad clay. Here. In the part of lower Aggrad clay is reddish purple in bands. 111) 38 in = Clinton, Cedar glades 20 ft. 112) No clear confined line but deep red day probably caused by disintegration of the rock. 113) 642 Columnaria halli 114) Only luster at highest point show presence of Madison, ~ 706. = 20m top -j massive Madison. 115 Madison massive, Middle part at 649½ to 7 upper Columnaria halli layers. Stone layer occurs about 5 ft below down- also Col. beds. No other data seen here. Top of lower Madison at 649. 116) Red bed = near base of psender- Madison with characteristic Columnaria alberta. 117) Large flat layers and ammonites lypograms- good collecting ground but no Leptacma. Partly lower Rill. sand and coarse bed at Ann Rill creek.
Read Page
Page 81
(118) 612 = top of Maender Madison, 628½ = top of (upper?) Glumersberg hard layers, gray massin clays. Believed to be upper layers. (119) Weker part of Massner Madison. (120) columnar overlaid with lower Peender Madison, 14 ft internal, Fossils, hystrans etc, 6½ internal mirrors. 653- top yellow bedded layers. fossils & clay, 643½ crossbedded layers, clay. strongly crossbedded layers in creek bottom. Main cleft at 632½ as three photographed at Mount Washington. Large flit crypt clumps 2 ft down. 8ft internal. Rough limestone but not this trict of arms included (121) North y Floyd Ford 628 = top y Lower Bigyard clay (122) Willing Mt Washington, 617 = lower Clinton Mt Washington (123) tree. 609 Salmon River Clinton 2½ ft.) (124) 634½ Salmon River Clinton base (125) 655½ Salmon River Clinton base (126) NW y Oils, 670 = top of big yard limestone, about 640 = Clinton base. (127) Just east y house 640=Clinton base (128) William Eldridge 5½ Caperalizard. 2ft 9in Wyper clay, clay, 5½ 19½ft lower Bigyard clay, 30ft 2ft 4ft basal Mississara. 30ft &m Salmon Clinton. Clinton face = 628,5
Read Page
Page 82
129) SW corny bt Washington 639 base of Clinton base of Niagara = 2 ft. Clinton - 3 ft. 130) Mt Auburn. Pl. Lynx ferrum. 131). Upper onto very strongly cross layered full y large Pl. Lync ferrum- diathely tilting 132) at mouth of stream, Top of cross cross layered layers, 133) 485 - Rhynchotrema dentatum bone but apparently not far from place. 639/522 2111.3 5-58 5-22 540 617/522 9.5x 3/4 521/5 135) 3ft Upper Cayuga clay 629 = top of upper Cayuga clay, 134) Cayuga limestone. Lower Cayuga clay = 21 in. ft, 603 base Niagara 3 ft Dirt m - 3 ft. base of Clinton ~ 597 ft. 137) Top of Waldron clay 138) Top of Waldron clay, = 643 139) 627 = top of Waldron clay, 140) upper Cayuga clay 2ft 9 in. base of upper Cayuga clay = 4 ft above cedar creek, 141) 583 = base of Waldron clay, 142) Niagara cluit, yellow 5th emboldas 143) base of Clinton - 522 fts 22 ft lower Cayuga clay 608 marks 4-2ft base Niagara 28 ft. 3ft transition. 16 ft Laurel horse 3ft6 inClinton. 3ft 4in upper Cayuga clay 24 ft Madison. 5 1/4 in lower limestone
Read Page
Page 83
144 Silurian chert with Stromatodes, 145) 30½ ft Yamel, apparently located at by, 146) 39½ ft Linnville - 544 10½ ft Linnville - 545 16½ ft Waldron clay - 479½ 24 ft Yamel. Chimborazo calculated at 394 ft., 147) Silurian chert with Stromatodes at 569, 148) 4 mi WJ Thixton, 682 = base of Waldron. 121) Hemp Springs, upper Ozford clay 3 ft. Ozford limestone 6½ ft. 149) at bridge, NY Bementon on bank Base of Pickettania 475 Miles. 150) Barny Waldron at mt 668 151) Cedar Creek, just above creek occurs the Waldron clay apparently. Only exposed, 152) Round corner, Silurian chert with Lyellia Stromatodes. 153) Church 685 = Chert with Stromatodes Lyellia. Calculate the distance of Linnville between here and 151. 154) 190. Between here and 687 and 670 the land is flat like meridional land east of Shepherdsville. 155) 675 = Medullary deformed residual ma- terial like that found from decay of Permian material but in Permian clay. 156) 666 = Linnville with Halysites. Not good evidence of any big fault line. Permian residual material. 157) (51) top of Linnville exposure cherty limestone
Read Page
Page 84
158) 615 Stram bode clust fragments Solid turned one immediately below 159) 632 = top of Silurian clust with Stram brds, and estd old dark Der vian residual nodular stuff immediately above 160) Silurian clust up to 640, 161) Decayed material which may have been dermian at about 640, 162) Flat plain's like country from line eastward + south east, 163) Up to 660 Stram brds with Siluria clust; 164) Nodular delmi like that called possibly of Dervonian origin, 165) Rock is led of Fern creek. S.f. Midden lay is here, it must be immediately down since quarry exists at bridge level. 166) Lyellia in crete in zita, 167) 2 mile S of Noroling, Silurian up to 500, Cincridium and Halgerite, Lyellia, 168) Silurian 169) Silurian at about 540 170) Silurian at 545 Stram brds, 171) Rather large quarry. Louenville District. 172) Silurian limestone up to 540 173) Rather large quarry, 550 174) Lyellia at 530 175) Lyellia at 550, 176) Silurian
Read Page
Page 85
177) Silurian up to 495 and Lydian ville clay in creek bottom. Colour late thickiness here. 178) Lydianville down to creek bottom, 133) N.W. Madway Irons 5½ ft sandy free-lime and clay-milk, large bryoz. 1½ ft from top. Lefelasma at base. Oratophis cyphomamma. 14 ft firm above down to level with Rhyn-cholina dentatum in silt. This is at entrance of Wajm wood cutt off shed into the creek, for crossing to west side. 10 ft drive to lift a strongly cracked bedded layers, with Lefelasma down as far as explorer got - almost to base. 179) Retrosa distinct above the Rhyn-cholina dentatum horizon here. 180) 100yds N of Mr Christ Richardson Lefelasma + retrosa occur about 5 ft massive coarse limestone. Rhynch. dentatum & Charnia bella - coarse layer, not seen alone to with Lefelasma. What have placed 182) First lime begun and come by. 665 = top of coarse Columnaria halls layer, very large a 22 thin the layer below in the pseudo-Madison. (600 = above base of pseudo-Madison.) 181) Top of massive Columnaria halls = 665 ft. Stargt Lefelasma & Silophic retrusa occur above, imme-diately, 183) 568 = top of massive limestone with Lefelasma alive, at point west of 607 ft level on jibber. 135) retrusa is found just below coarse 5 ft layer. large, whether in silt or not if not known but should not be impossible. It is found just beneath coarse layer with Rhynch. dentatum & 5 ft down drive. Retrosa thin for apparently 6th about below coarse 5½ limestone layer. 184) 588 = top of massive Columnaria 652 = Christen. interval = 64 ft. 185) 2ft Upper Lizard clay 7ft Oxford limestone
Read Page
Page 86
(186) N of Grinnell Ford 2 ft calumet Clinton, 14 ft next green, Madison - 609 19½ massive Madison cap to base of massive Madison. 25½ Strath v. which immediately above, Sthomina halli. 17ft more fossil forms in top of massive crals, 16ft tender madison + circular clay rock, 33½ tender Madison, heavy it w, ledge at tip, cap forms at face, 8ft wrinkled clay shale almost non-fossil. 11ft, less fossil forms above Plat lying above + thin fossils, below 3½ ft massive crass limestone, 476 = base of coarse limestone. caged badly to a clay rock battle 60 ft coarse limestone lower part dun 52 ft brown boggy clay, 111ft lower boggy clay with few fossils 1½ ft local Niagara 2 ft transition, 187 8½ ft up to top of local Niagara, .544 = Clinton in 2 ft upper boggy clay. 5 ft coarse limestone are boggy clay lower
Read Page
Page 87
Jeffersitown 188) Silurian, quarry off the road. 189) Dermian at 620 Louisville. 190) Silurian in situ up to 560 191) shelly crinoidal whitish limestone, crinoids common, Upper Devonian. black shale remnant very rare, at 540. 192) Black slate exposed by telephone fault hole. 193) Black shale - crinoidal limestone contact at 528; Dermian limestone is ferruginous at very top? 194) whitish limestone believed to be Dermian; 195) no exposure here 196) nor black slate struck in well, only a creek said to be a blue creek, and therefore limestone touched?. 197) Louisville up to 557. Quarry on Finley branch, 198) Contact of Coral Dermian with Louisville is well exposed at 511 199) No exposure since 198; 200) nor exposure but limestone is struck at dawn. This must be Dermian since black slate veins simile down stream. 201) up to 510 Silurian in yard sized gravel, no Dermian exposed. 202) Silurian exposure near creek level 204) nor exposure 205) Dermian crabs + gregaria at 470 in clay and solid limestone.
Read Page
Page 88
206. Southern Brick and Tile Co, & 1st clay pit, Residual Permian clay containing chert clumps wit Marmatia entabulata. Cr millin brick; 3 in. to 12 inch tile, 618 Park Ave., Louisville, Ky. 207) Silurian with Halgerta lyellia, Strombodes up to 480 at least. 208) Drilled me up to 522. No good evi- dence of any of my being Permian but doubt I know. Or one it seemed Silurian. Farmers say no black slate struck in wells, only limestone looked above 540, 209) Lyellia up to 520. 210) Conchidium beds with radiating gelication. Limestone from com- mence up to 509 & just south of S. Red Heart Cement No limestone on top of ridges in wells. 211) In this neighborhood our slate is struck in wells on ridges, 212) Barretton road & W J B neckel, Top of Silurian with Halgertonia to 485 overlaid by Permian crabs and gregaria. 213 Black slate or residual limestone at 618, west of James house, near home on Smith, 214) 665 = oolitic top of gannel with 11ft of Waldron above, rest of Waldron not present owing to weathering. 215) oolitic top of gannel at 649: strong southward dip, 216) Lyellia up to 700, 217) Quarry in Louisville L. 218) Strombodes Cheeca Stratum, or 'im at about 710.
Read Page
Page 89
219) Only Silurian material seen up to 720. 220) Silurian up to 700 221) Silurian with Halysites to 688 at least Deriv. siltie wit sphcerodonta w/it wide apart shies. 222) Clut at 682 emaculated Deruvian but evidence is not clear, may have dropped; 223) Silurian up to 680 at least. Coralogy slut can not be identified with confidence, 224) Silurian up to 645. Stream enters. carehere. 225) Silurian to 650. Crulogy, slut can not be dentified; 226) Silurian limestone up to 620, Fine Sprng. Lyella. 227) Deruvian slat with cnals, 228) streambeds in Louisville, Deruvian contact w/cnals immediatel above. Crinoidal limeste far- thir up. No Black Slate seen, bwn in Louisville ty., out about 575 that measured. Middleturn 229) Silurian up to 710 at least; no evi- dence of Deruvian between this and Widdletan. 230) Nothing but Silurian seen up to 665 at least, probably up to 680 at leas 231) No evidence of anything except Siluria cast there as far as 229. Silurian at least up to 690. 232) Only Silurian seen here. No Deruvian or far since Widdletan. 233) No evidence of Deruvian from this point NE.
Read Page
Page 90
234) Devonian crnl led in creek bottom at 580. 235) Cavernidal top of Devmian lower at me 236) First black shale eff came at 565 Rest m Carniforme - Devonian l; 237) Black shale brought up by telephone poker 238) Chert, age unknown, up to 575 Silurian Devonian (crnl) contig at 567, 239) 594 = Silurian chert up to this level also in the next corner, a few large Devonian crnl also in the mixture partially dropped. 240) Chert age uncertain, up to 615 at least; 241) Chert probably Silurian up to 652; may be Devonian above but dont know. 242) Chert at top at road corner first, 16y Silurian. Madison, Ind, 99 Rest not exposed. 28 ft Diff rock of Daniel. 57 in thin folded sand; 3ft 1in. Upper Cagford clay Obitus 3+4. 4ft 4 in, Ozford limestone. 13 ft Lower Capord, Chertm 5 +6, 21 inches to arenite m, 21 miles Clinton. 53 ft Madison down to top y Coal bed Chief. 16 ft fossils present but relatively few; 25 ½ ft down to Hebertella maculata, rare. 35 ½ ft below Heb. maculata to Byg beds;
Read Page
Page 91
(243) One mile east of Wrothington, Shrubdes, Pentamerus at Brad Cmrs, at least as high as 720 (244) 686 - Spirifer gregaria in clusts also Crals. (245) 679 = Spirifer gregaria clust, (246) 638 - Silurian with Pentamerus & Crnal bed of Deronian, + gregaria further up (247) 642 = Silurian-Deronian Ctn- tact firstally. Deronian clust with Crals abundant. Silurian wth Pentamerus (248) Silurians up to 610 at least as far as ) (an quote not from cut in lines above. Base of Waldron at about 565. judging from cut in levels (249) 541 = Face of Waldron. (250) Deronian end bed in pit w/t 598 Silurian top = 5 ft Crnal well exposed, (251) Deronian Crals abundant at 598 at town yard, (252) 590 Silurian - Der. cral contact well exposed; (253) 590 Deronian Crnal Clust abundant. (254) a very large Crnal 6 inches in diameter at the Volcano order, at 585, remainder of Deronian Crnal bed which is at 583 also, 533 = top of Waldron clay = 50 ft fn Smirnille led for very accurate. 520 70 450 (255) 544 = Deronian Crals in situ app- parently, what does this mean? (256) 573½ - Deronian Crnal bed in contact with Silurian. 15 ft of Deronian exposed here. Collected from upper part of exposure = thick cement bed I think, (257) Orthoqeras annulatum, large Crnal in Lancel arch near middle
Read Page
Page 92
258) 555 Silurian, [illegible], front, selected, 259) 592. Silurian with Strombode, Devonian chest stone. Fossils. 256, Stephendorita concava J S perplana J S spirifer fornacula Atropa reticularis. Allypus [illegible] J S Chonetes yandellanus Santamarella anata? Munidella barizoni J Paryclaeus linata s Olenstrmaric submarginata J S
Read Page
Page 93
Shepherdsville. 37) dd 1 ½ miles from Shepherdsville on road to Cedar Grove Church. Black Shale in critical Conifer- ous 2 miles with Post among Myriads 36) dd 3 miles from Shepherdsville, along Oak Elm Lick Skillet. Bull's Run = Miller's Run, with Wash- ington gravel. Walden clay Gravel to top of gravel -- 3 in. 35) dd Old Mellers' fence, 1 mi from Lick Skillet, Coniferous - very white - 4 ft perpendicular 2 inches = 20 ft. Do this correct? Walden clay. 34) dd Cedar Creek, ½ mile beyond Red Miller = base of Cypress clay, beautifully laid with red pebble - 18
Read Page
Page 94
Shepherdsville. 38) st 1 1/2 miles from Shepherdville in road to Cedar Grove Church Black Shale on criminal Creek mud Limestone with Peat amongst it 36) dd 3 miles from Shepherdville, along Cedar Lick Skullct, Bells Run = Miller's Run, with lignite clay. Malden clay carboniferous coal to top of Sandal 3 in. 35) dd Ed. Weller's farm, 1 mi. fr Cedar Skullct; Limestone - very white - 4 ft. n 2 intercal. 20 ft., others are Malden clay. 34) st Cedar Creek, 3 miles beyond Miller = Lower of Caywood clay; clean limestone with red flake, >18 in. of Lower Caywood clay; clay is 6 ft. w/ cloudy local partly clay? W of Fisherville section, 1. Saluda bed. 2. Whitewater division of Richland mud, above Columnarite bed; 3 mi. West of Pope Lick creek, 3c Upper part of Breeds-Madison section of Magnesian bed; 1 1/4 mi. West of Fisherville, 5 miles west of Pope Lick creek.
Read Page
Page 95
950 Shep, Lordsville. -S- 60 turns S 17 E - 170 Read R to Yelann Jct, ---E 210 Small stream. At Stream is Den Limestone Top contact with Black Slate, Den limestone 6 & ft exposed Crassly divided, especially upper 3 ft. - cement rock enclosed not exposed, ---E -- 50 turns, N80E -- 265 turn N30E --- 45 - creek, Buffalo Run, Wagana Limestone. Of 4 exposures at 465 Alweta. ---E 94 turns N30 E 125 Wagana limestone N30 E 129 at Henry C Hamilton 508 almesra & Den Crags crassly divided limestone: upper part of Den, l. N30E = 152 turns, Blacksl like to low, N80 E = 105 turns to contact. 512 ft above sea level, cut not crasse subdivided by Den. l. and D black slate. Time gained lined me presently by - probably Wagana, seems 5 & ft lower down. ---E 6 turns N75 E -- 64 turns N50 E --- 180 turn to E Magruder stree in left. Wagana l. at 565 & Magruder store, N50 E - 46 turns --E- -- 38 turns N65E -- 50 turns, turn left to Victory ridge road. S.10 E - 15 turns Lick skillet store. S35E 15turns Cedar Gr over road turn, off line = 14 to Cedar Grave church. Road then turns off to right by creek! x S75 E - 105 N85 E -- 65 N50 E - 110 N --- -- 37 N75E - 170 turns Barry Waldin at 525 almezza. --E John Ostone # -E 40 turns creek small crags ---E 18 S70 E 85 road on left 340 E Waldin clay 12 ft thick 101 steps to level of road N65 E - 246 to Cedar Grove church or right. Road straight ahead goes to Southside. About 8 miles from Shepherdsville, S20E -- 100 steps x S --- 130 turns S 5DE - 78 turns S20 E -- 140 turns S 80 E - 146 turns!
Read Page
Page 96
S 85 E - 160 turns Amanda Bonman --E -- 83 S 85 E -- 88 [illegible] Waldron line at 670 above sea, S 70 E 97 S 85 E -- 86 N 80 E -- 50 to Waldron line at 700 ft above Sea level, N 80 E - 85 N 35 E - 110. Devil cruminal not extend but along road side as road ballast. Black slate hill begins here. N 75 E 55 turns, S 80 E 76 turns, -- E 30 to road lining left -Bristleton, road. About 2 1/2 miles to Kirby Jones place, S 30 E - 63 S -- 60 S 15 E - 137 - at 675 Devil line, cruminal with black slate above. Devil - 4 1/2 ft thick. All cruminal, S 20 W - 23 stream Devil well exposed. Ferruginous at top: -jumps to farm. S -- 25 S 35 W - 40 S 10 W - 48 S 10 W - 58 S 5 W - 70 to top of Mayana exposure at 735 above sea, Devil not exposed here. May be present. King's L - 8 ft rests on Waldron clay. S 5 W - 20 S 45 E - 20 S 70 E - 45 S 35 E - 44 Waldron line at 720 S = S 40 E - 48 Road turned left -unkroad, gives to S latitude S 40 road about 1 mi E of Kirby Jones, line to creek meet of Latitude, 5 mi to S Latitude. S 40 E - 5 S 10 E - 106 to [illegible] Springs Str S 10 E - 60 S 40 E 31 [illegible] S 40 E - 32 = top of the line [illegible] long day through exposed electrified line front, S 20 E) - 100 creek bottom. S 60 W - 84 S 80 W - 23 R S 35 W road to Deatville, W - 145 turns, 720 above sea, top of Mayana exposure. May not be top of entire Mayana. but seems that way --W -- 160 S 40 W - 105 N 80 W 160 S 55 W - 40 turn Cane Springs Station, R S 35 W. - 111 S 10 W - 236 to creek on county line, Christon line = 670 Waldron well exposed near top of hill returning westward,
Read Page
Page 97
S. N5 E - 45 N15W - 55 N25W - 70 N60W - 15 N5W - 90 N35E - 24 N15W - 30 N - 55 N15W - 50 N5W - 75 N15W - 52 N65W - 160 N15E - 25 N75E - 28 N15W - 90 N55W - 20 N45W - 90 Opposite Fancy Dave Graves Store, 2 mi. E of Cedar creek church, 1/4 mi from Kirby Jones. N30E - 90 N5E - 20 N10E - 10 tree of Clinto, 690 N10E - 14 Creek branch y Saluda 20 ft massive Saluda N25E - 50 road at left S85E - 70 top of [illegible] above clay above left bog l, N30W - 35 N30E - 216 N10E - 20 Walden Laze 760ft N10E - 115 fence l. N40E - 60 tree of Clinto stream flows across road northward so that Cedar creek lying at left side of road. N10E - 20 road from left, N10E - 42 N45E - 30 N30E - 65 road off left N80E - 166 N50E - 55 S75E - 50 Kirby Jones, Valley turns east in split. wide road from here White creek east of Fancy runs into Cedar creek about 1/2 north and then Cedar creek runs south and turn s all above about a mile farther on, about 6 or 7 miles below Greenville Jct. - about 3 mi or 2 mi below Ridgeway Jct.
Read Page
Page 98
N65W, -- 300 N65W 122 Streef O & Crenshaw x N65W -- 28 x N55W -- 75 x N65W -- 30 x N60W -- 45 Road on left, x N-55W. 36 x N70W -- 60 x N55W -- 100 x N45W ---- 50 x N-70W 65 Road my R Y S80W -- 20 Meek x S60W 46 x . . W. 30 Cedar Grove Church, 300 Slate Hill. 301 Black slate at 527 up this far at least, 302 at 480. may be black slate here but if so, it is so badly weathered that the black color shows only in a few thin layers, Rest is light colored. 303 at 490 Light colored soil may mean Wavaly. 304 Good Black slate exposure at 480, 305 at 495 Black slate tip with phosphatic nodules 10 inches long at maximum. 38-1/2 ft light Hardlay Sinietta. Sinietta Clay believed to extend at least 27-1/2 ft farther up = total of at least 65 ft. 306. Black slate tip. 307 Plenty of black slate this far west. 308 exposures seen between 307 and 308, at 308 at a level of 466 and for some distance below -- 460 at least, Wavaly clay showing. Whether slumped down a gulf I do not know. 309 Sawmill at 500. 308 Black slate tip at 464 judging by phosphatic nodules at lake of Sinietta clay exposure. 310 Sinietta clay in stream bottom.
Read Page
Page 99
311 White salt wells need to be, 420 Limestone clay, fine exposures in low distances in every direction from here. No Black slate, 312 Fine Limestone clay exposures up to 57 at least. Nimbu ranging here. 313 At 457 There is Black shale top with phosphatic nodules well exposed. 314 No exposures since 313 and 315 but here at 314 a Waraby clay rock with ferruginous nodules in place and much sandstone rock tumbled around here to creek beds, above 539 level = about 545, 315 Here the grey bed contains clay shaly rock with iron nodules. 316 Waraby clay shaly rock with iron nodules, fine exposures on North side of river. 317 Same Waraby clay shaly rock (2yds) with iron nodules. Iron nodules very abundant 150 ft further m. 318 Same rock as at 317. 319 Limestone at about 820 Borders. 320 At 552 is top of Black slate with phosphatic nodules. 321 Nothing but limestone clay since 320, 322 White clayey stuff, almost like Limestone clay but with ferruginous nodules. Looks like Limestone clay at least 323 Black slate top not clearly exposed 324 Silurian limestone, top about 1 ft above RR grade. 325 The same limestone with Stern matfordids may be followed up to here. No evidence of Den limestone. 326 Limestone exposures abundant. 327 Black slate the rim only by very shallow roadside ditch. 328 Black slate down to creek level, Shepherdsville. 329 Niagara limestone up to 482. Black slate at 493. Intermediate part not exposed. 330 Cincinnati Den, limestone, 1 ft ex- persed. Thickness unknown = Craggy Cincinnati, at 493 Niagara top = 1 ft lower down. 331 Niagara limestone up to 490, 332 Niagara limestone all way to next 333 Niagara limestone, at 498. 334 Niagara limestone, at 480 335 Niagara limestone 336 Niagara limestone up to 493. Broad form of Halysites. Massive star matrix and coral. 337 Denmanl. at opening of house Alameda Park Plastering down, spirifer diversica-tus! in limestone closely resembling Niagara limestone. Total thick- ess unknown, excellent contact with Black slate
Read Page
Page 100
Bridles 8 At Brad Criner: 573 Zinetta See but not the base; 19/2 Up: ferruginous nodules large, abundant. 24 1/2 ft. from base; ferruginous nodules large, abundant, 33 1/2 ft. up, from base since 24 1/2 ft. ferr. cinnops nodules occur at vari ous intervals, large & abundant. 4 1/2 ft. per face. Ferruginous nodules not large, 53 clay. Since 30 the Zinetta clay gradually has become harder and more chalky but it still weather whitish + soft clay, at 53 is plenty of ferruginous nodular material. Up to 637 ferruginous nodules are seen in the clay shale. This clay are just as abundant as lower planes. Clay does just exactly the same and soft but tends to lie more broken up so that flakes fragments weathering dark blade gives a light brown. At 643 is the first layer of rock like fine freest one, 4 in thick, with ferruginous nod ules absent clay quite below, a change from stuff weather- cloy to that weathering more only takes place near 624 In reality it very gradual. From 643 to 660 occasionally freestone layers, 2 to 3 in thick and occasional ferruginous nodules occur. Up to 681 since 660 flares rock, with occasional ferr nodules but no clay; free at at least some well exposed. At 725 thin & ferruginous nodules but these have been crushed scarcely since 637 and more so since 615, except at occasional intervals. Up to 745 there is clayey shale with very little ferruginous in it. Collected clay between 695 and Up to 798 the order is flitch clay, ark, with ferruginous nodules rare. Fossils nearly but very few up to 817 came as last - rock. Collected from 745 to 817: Up to 836 from 817 A cramer part of the shale is indurated as to flake like a bastard freestone, but it is very coarse of all badly, weathering into to a new kind of rock as between 745 and 817. Between 817 and 860 the shale as a massive hard and flinty rocks and weathers to my rock.
Read Page
Page 101
AT 863 the rocks slightly cherty and at 871 it becomes more distinctly cherty, Up to 889 from 871 there are indist. fragments in crease, but almost all of the rock consists of rocks like upper travely clay rocks kindly cracked up into small fragments or layer mass, where as underneath, Collected from 830 to 860. Going northward along ridge road from 986, the formation cherty rises to 876. From 820 further S., [illegible], I found one at 874, at 869 some- what cherty limestone. Beneath this is upper Wawky shaly clay rock. Beneath this is the more solid freest and like rocks as in road East of D. roads, from 850 down to 800 and down to 780, much less solid so that it weather shaly when dry exposed but appears much more solid when freshly exposed. Beneath this level the shaly clay Wawky rock appears practically with no ferruginous modules [illegible] From edge to 540 892 and northward still lower but exposures are too poor for measurement. 450 - No evidence of anything so low as Ginietta clay as creek bed at 473, = 1/2 mi. S by South Park Sta. From End Ridge along the road following east side gravel road, for 1/2 mile only gulfish from Wawky above the Ginietta clay is shewn. Rest of this stretch as far as 451 there apparently is Ginietta clay but exposures are poor. 452 - One + a half miles north west of Barkers Shaly Wawky just above Ginietta clay, a top of Ginietta clay. Ferruginous Modules can be in British clay; Henry R Sanders knows where Specimens on Butts or Wawdy were formerly found, about 10 miles east of Warren by mi No 520 on west side of branch.
Read Page
Page 102
453 ME17 Brooke's black slate & chert beneath. 454. Miagani, with Nalginites & chert above, chert with Igellia, presence or absence of Dornin not determined, at 500, 455 Black slate in field at road side, at 524, 456 Black slate a coarse grained. Dorlimpet are with Silicite with Nalginites, 3 ft below contact of Dor. wll Black slate. Therefore Dorlimpet are can not be thicker than 3ft but may be thinner. Oppy Dor. limpet as at 493, 457 Silurian limestone but under exposed here, or is not known whether Dor. Limestone is present or absent here since Black slate is not seen. due 11,15 to Divine. 1,08 going west 5,45 " 2 + 3,50 OM, W. Incketers Jos De Jarnatt Sarah De Jar nette 35 - 35 1/2 miles E y Versailles - about 30 ft thin bedded chaly rock with upper 5 ft in the layers 3-4 mil thick. not 1/2 mile &.7, just next of lyme stone is it found clearly rather, its character burning? at just 36 miles east y Versailles and for short distance next anthorony melullus abundant above the Staph. and agyrillensis limnea. The by j The limnea is medium sized. Planoceraspa The Pecharyera humilis occurs a short distance below to a Staph. planagipervx and quite further below Littl magnuchela abundent.
Read Page
Page 103
Fred Brawn. Brooklyn NY, Allen. Fordyce Knob. 1/4 mi S of Borden, 5 ft mill. 20 ft Chert, red ark, with spinfur 2 spec 47 ft shaley. 1 ft SS solid. 1 ft SS solid. 10 ft shaley 8 ft SS intermediate, not er massive 22 ft SS. Massive. SS massive, with Derbya large + fairly abundant in one thr layers. 35 ft Massive SS with large Derbya at various intervals. 24 ft weathering shaley, probably like underlying bed origin ally 16 ft indurated argillaceous arkite weathering shaley. 18 ft indurated clay creek with spiffur and abundant Derbya, Forks of mad. West Y. Borden, N of RR, Arch end 2kft? 31 ft massive SS 132+ RR crossing up to mass reflectin Interval is shaly stuff. Dr. Stalkers farms McKinley Rdst. 1/4 mi SW of Borden, Top of hill. Chert, red ark. It an rds bury. Contact uncertain. 33 ft + shaley. 6 in SS solid. 11 ft shaley. 10 ft massive SS, with Derbya at intervals. Derbya common layer in me layers. 30 ft large Derbya common at various intervals. 35 ft Derbya common at various, intervals. Indurated argillaceous freestone, weathering shaley at various levels. 20 ft Derbya rather rare. 24 ft interval. Indurated argillaceous 12 ft intercald shale 70 ft softer argillaceous material. 22 ft down to crossing of road over creek. 5 ft interval. Hard rock layer in creek. The stuff in this bank looks like the stuff underlying the typical Derbya clay, which forms the upper part of the New Providence formation.
Read Page
Page 104
William M. Stone. Carrwood. Limestone fossils S of farm and also 50 yds bury East Crookton on the road leading to Cani wood = Bazzards Rock. 1 3/4 mi E of Binder, along side of AR Behind denard. 400yds SW of Chester 3 1/2 in wide originally 4 in wide? 15 in deep. - 14 feet free lime on clay & silt, 1 ft limestone due 14 ft clay shale, Fenestellids. 1 ft 3 in L. with Fenestellids.. .. 14 ft shale. Top + in working clay shale at time 5 1/2. Limestone. Fenestellidae Comm. mat 11 ft argillaceous rock, weathering shaley, 40 ft very cherty in places. Some 60 ft wt h argillaceous shaley coarse. Upper part massive. Cherty near top. Fenestella comm 5 1/2 ft argillaceous rock with L. at tops. 6 ft massive limestone. 6 ft more shaley & argillaceous ma in conformity to a fault // along the jake. Also on the fresh vertical surfaces large cherty stems. These do not this types of some laggars are fully the local warlords here. Up a fully 23 1/2 ft limestone closely similar to 2 ft limestone full of flinty cherty masses. 13 ft fine argillaceous with weathering shaley. The deposition has taken place here. --- tail low forming a strongly incormform sand what cross-bedded. abundance of rounded leads. White b. opts. fossils very scarce. Not even can grained, crinoid, white cherty in Harwood's 29 ft Harwoodshgsl. coarse E. Fairview W apparently are unconformable contact draging to the same series. 7 ft more shaley than underlying rock, but h- 14 ft massive 2 sandy rock rather argillaceous, with few crinoid stems & a few fossil shells. 66 ft argillaceous indicated flinty like weathering shaley.
Read Page
Page 105
5\frac{1}{2}ft + appill shale. 231\frac{1}{2}ft up from Olicr shale 3ft SS, 127 ft. 101\frac{1}{2}ft up I - 4"pf. Rhup. annella arani C anomm. 8\frac{1}{2}ft crnnidos c up to this level. 89ft up 2 to 3\frac{1}{2}"& H --- lamizon, freely G another imm nodule layer. 3\frac{1}{2} ft. Basil's scorei imm nodules 5ft app to another inm nodule lay, Basil's score. 77" First heavy inm nodular layers = F 10\frac{1}{2}ft up. Forest fern. E 1ft up = 1in l. = 66\frac{1}{2}ft up. 5ft up = two in ch l. D Another lim set me layer - 60\frac{1}{2}ft up, 11 ft. internal. C \frac{1}{2}ft crnnidal limnest me layer. B-44ft up = two inch crnnidal liment to 6in. 5ft up interval. 23\frac{1}{2}ft black slate to face side expore. B Chief Rhup. anani lamizon. B-C Rlh. annm in this interal but not very common. D chief --- lamizone. 55 228\frac{1}{2} J 101\frac{1}{2} I 97\frac{1}{2} H 89 G 85\frac{1}{2} F 77 E 66\frac{1}{2} C 49\frac{1}{2} C B 44 D C: B 44 23\frac{1}{2} 127 101 228
Read Page
Page 106
No text detected
Read Page
Page 107
No text detected
Read Page
Page 108
F. P. Hoover, Blomfield, Ky., 107 590 483 Lanuel n 13 60
Read Page
Page 109
Sawder, Harvey, I take road to Preachersville at first lane on this side of bridge turn left, about 300 gas from pike to house, north side of lane. Widow Jones lives there now. "1 1/2 mi. from G. Orch. My mill inroad Dix river, 30 yards from river. Start John, with clay road, will road turn off at school drone in 1 part of town, cross the Dix river, at Hunter's End, about 4 mile beyond the End, in Fall Lick road. Foley, Andrew, From centre of town go east and then NE past the center 200 to 300 yards. "1 mi from centre of orch to Fall Lick road, "Spearm well, the one you can drive up to before you reach the bridge. My section "1 mi from G. Orch on Lancaster pike" Field Well at Crab Orchard Springs NW of Hotel 100 yds "in lot of property of Crab Orchard Spri's" Grove Well right across from the office of Crab Orchard Springs "in the yard of its property of Crab Orchard Spri. Mrs Caldwell. Sulphur water at Browns Spring, well known on Lancaster pike. Take next turn off toward E along lane, after passing the school house. Salt Sulphur Water. Adams, A. Crab Orchard Springs. Brown Spring, 1/2 mi. from Crab Orchard, on Lancaster Turn pike. Hurand Sulphur Well 1 1/2 mi. from Crab Orchard on the New Vinegar road. Bryants Spring near G. Orch. in the valley. From Par- sons Springs W to Star Sulphur water. Must see a mine run near.
Read Page
Page 110
How to determine Sp gr of limestone other tests. How to make use of bogrod clay for drainage. How to recognize presence of bogrod clay. Core drills rather than churned drills for testing. Incorrect test at Tuckers reported 70 ft limestone, springs, important layers of clay, pits in clay residual for watering animals. struffy but which strata prove large areas of wedging rock, both wire there cores have been free fracturing instead of plication, strata may not have been as much subdivided than as m. an. Delman alla emaculata forve plicatio in glensidry. Gathering Cedar or gladesy logs, purple colr not found in Walden therefore a distrugizing feature of the bogrod. Southern grazing lopyx and maymillerus farms. D. J rocks useful in connectin with placing of wells and cesspools.
Read Page
Page 111
July 2 Monday S L 2 jefferson ave, 3 Tuesday B D S L 6 4 Wednesday B L 8 5 Thursday B S L 11 6 Friday B 12 20 Sunday Mt Washington S L 19 Thursday Dinner at Ting B S L 20 Friday Dinner at Louisville B S L 21 Saturday, Rig Watford grad ½ B D S L 22 Sunday Rig East J Cedar G, ¼ B D S L 23 Monday Rig West J Cedar G, ¼ B D S L 24 Tuesday, Bardstown pike B D S L 25 Wednesday W J McCullicks Run B D 26 = whole week board 2½ cargo rig, Louisville & Atlantic, Nicholas P a P a Miller 7.18 11.47 2.27 655 Richmond 754 11.38 1.40 P 6.14 Pondla 6.30 12.05 1.35 7.35-600 Swope 7.02 12.37 12.53 7.01 a 7.30 11.05 12.25 6.35 P a
Read Page
Page 112
1) Epsom well J. E. Grave, walled well at first, drilled in kettle. Afterwards day to 10 feet hole in diam & opened at, ?8. 2) G L Butler owner (Gins Mill) East of pipe, between road to left W & road to right E in Riddville. Dug well walled up. Some feind water here, but no salts made. 1) J. E. Grave. Own making salts about 20 yrs ago. Made salts for a short while. Only well at Kidd- vile or vicinity where salts were made. 3) J. Harvey Boone, about 1 mi. SW of Gunsbridge nothing known about a well. He lived in the branch entering it from creek from the west. 4) Soda Springs is 75 yards west of the Ovel Spring, on property of William Hule, walled. like to have chemical analysis, = SW of Hotel 5) L D Stone, From Right angle go west 1/2 mi, to forks road He met Sterling & Merritt, then S on Merritt road, to first land next. Home lives just South of this land. Chiltin PO discontinued last year Pigg's Stand (Store) Louisville Oil & Gas Syndi- cate, W. W. Watts, Pres. Louisville Ky. B. B. Wind, Winchester, 1480 ft. Oil Spring. E D Veach Lexington. A S Well Kidd, E. O Transylvania Co. Lexington George Mc Intosh The 7ft clay layer in Clum Creek Shaber, Nearly open to bicycle sta
Read Page
Page 113
Cincinnati to Winchester Th. 2.80 Winchester, b. h. Th. Fr. 1.00 Winchester to Indian F Fr. .40 Oil Spring dinner Fr. .50 Indian Fields to Clay City Fr. .25 Clay City, Suf. L. & O: Fr. Sa 1.00 Rig one day Sa 3.00 Indian Fields d to d Sa Su 2.00 Indian Fields to Lexington [crossed out] 1.00 8.95 Lexington, hotel, one day Su M 3.00 Lexingtn to Richmond M 1.00 B ms M .25 Hotel Glynburn M Tu 1.00 Richmond to Pandora Tu .40 Dinner Tu .25 Pandora to Darine Tu .35 Darine to Richmond Tu .70 Hotel Glynburn Tu W 1.50 B ms W .25 Richmond to Walby & return W .35 Rig & dinner W 1.50 Hotel Glynbum W Th 1.50 Richmond to William Th .20 21.20 Dinner, G'or William Th .25 Hotel Glynburn Th F 1.50 Hack F .15 Richmond to Stamford F 1.04 Hack F .15 Rig's F 1.50 Hotel St Croix, St and FS 1.07 Stamford to Lexington by S 1.45 $28.24 Sunday at Lebanon Falls lodge there 1 Fri 1 Sat Sunday [illegible] 272 steps 152 93 1-9 12 4 4 6 11 9 h. 3y-y 28
Read Page
Page 114
"Intro." Lizietta clay NEY Berea, Lizietta Duffin layer Duffin cut Limestone Duffin cut Phosphatic. Great Clay Irvine, Paula Crab claw Waco lime Estill clay Irvine Elkins lime Plum creek Paula Brassfield Ridgeland Derniandl. Louisville upper, Louisville lime Walden clay Laurel volcanic Laurel. Osgood Clay, Bardston. a. Clinton well fedded Bardston. Botland Bardston. Madison Bardston. Plender Madison NW Washington 2.125; 3.5 " x" 54 Lizietta Duffin Limestone Phosphatic. Great Clay Waco. Estill. Elkins. Plum creek Brassfield Paula. Louisville upper Louisville lime Walden Clamint Laurel. Clermont, Osgood. Coon Sp., Tully Depost. Clinton Gasburg Bardston. Bardston. Botland Gasburg Bardston. Barley Willis. Old Analyses in Shalers former reports etc. + Analyses of wells Bygle Cr. Clarke Cr. p. 119. p.p. 173 ff. p. 279.
Read Page
Page 115
Look up wells of Garrard co in old Survey reports. Indian Fields. Where did J. Harry Boone live? in sec[?] of Red River twice 10mi. mit. Where sections 2186, 2187, analyzed? Peters. Clays of Madison Co. Indian Fields. Black sulphur well, L.D. Stone in road from Hiddsville to nr north of Red River. Where was the Soda spring near Lulbsand creek? Marlingst in Co. Where was Walter's Lick? Made salt here. Lebanon. Where were the Plantation Licks, 2 mi. NW of Raymond. 565 Clay Licks 1 mi S of Raymond 576 Able Spring 4 mi S of Leba- ni. 579 13 568 Between Boston and Bardstown. Thickness of Louisville bed at Boston, 59 3/4 mi. E of Bntm. 58 2 mi. E y " 54. Devonian? Devonian at 54 + 56. Thickness of Portland at 56. Between Bntm + Ballardown, 67 = 2'1/4mi. E y Bntm, Walden. 61 = Half way = Laurel. 74 = Laurel at Balltown. Lower Laurel clay + limestone, Cane Springs section. Gasking section. Ozgrod base. Huntownville. Is Columbia's above data found here? Oral Orchard, locating following springs: Grove Brave Field Itound Glebon Foly Sander Bryant Choley Field Valley sulphur Root-sulphur Stone-sulphur Well.
Read Page
Page 116
Wanted. Correct location of Wood lawn or Woodland and of Need more with reference to Gasburg. Dudderan's mill in Dix river, reached from Richm and junc- tion (- Roeland) On spring this Columbiana is crossed. marked on map. J.T. Lyon, about a mile from Halls gap station. Rock quarried here, could be dressed with an axe. East of Halls Gap station 1 mi. on Ottenheim pike in S E direction Maywood = Hall's G adjts. James' Mill in Dix river. a road to Preacher ville Spring well at Mr. J.E.Groves Kiddrille, In what bed was this well opened? Olympian Springs, Coniferous? about 1/2 mi. n.w of main springs at Old Chalybeate Spring, At Minden. G.D. Cooke Prop. Hotel. Use water. Prof. Harper's clemson College South Carolina. Tobacco.
Read Page
Page 117
[illegible] 1 [illegible]
Read Page
Page 118
No text detected
Read Page
Page 119
No text detected
Read Page
Page 120
No text detected
Read Page
Page 121
D W Dennis Richmond Rly Fossils 1877. 163 Vine Street 463 Noah Rads
Read Page
Page 122
No text detected
Read Page
Page 123
Wilderness Quarry E end of Abandoned RR Trimble quarry. Beech quarry, 5 ft (5/14) 24 2 ft. porro massive l, 9 ft medium porous massive l, 5ft 6 in, very porous massive l, bituminous! 7ft 6 in, Massive l, fern remains cc at base. Q 2/4 3 in, shale. 3 1/2 ft. Massive l, + stromat records + large Halycites nymus, 3 ft Limestone + shaly interlaided 10 ft Massive layers Cyathophyllum, Lissaria, Trinoidal fragments, Favrites, Acarina, 21 2 ft Massive l, weathering very soft, Trinoidal, favrities present at mouth of quarry, Favrites collected. 2ft 9 in Massive very porous bedded layers or rather irregularly bedded. R 6ft 6 in well bedded + laminated; cherry. fossils few. Probably clayey limestone, at any rate quarry stop at this level.
Read Page
Page 124
corporation quarry Frank sink quarry S.J Marshall jk see. cavernous within 1 ft of lane Same large cavonies, with caverns exposed at RR quay. 8 ft. Cavernous l. weathering to rather thin bedded rubbles platy ma. Q 3 ft Shaly, + many small strephelid zones flat on one side 2 ft 6 in Linnest me Halynites megnolage ce at top, 3 in Shaly, chief coral horizon 14 4 ft 3 in Massive zone cavernous 5 ft 6 in. Massive. Much less cavernous. 1 ft 3 in Massive layer.
Read Page
Page 125
No text detected
Read Page
Page 126
Q Quarry S of Walnut Street on Waldey Clinton. This quarry is about 330 W of Brink quarry. all in situ in upper part of quarry Eve implications like me collected Stromat forrid with radiate lining Streptid asme, short but broadly flattened Small globule small celled Farnvites . But may large Farnvites Cronical globule small celled Pointed flat. lashed Streptid asme Polygites vex no large Conevites round stems out, 14"ft expred, limnut are, below the 3ft clay Layer of the Brink quarry 31 ft natural, covered, going N60 W to another quarry take of linnos S of Walnut street . (4ft bti. la'must me weathering shaly but not cherty(R) 6 in. qeyl. somewhat crinoidal. 2ft 6 in. formed me weathering shaly S 6 in hard, gzy, ripple marked. crests N5W 3 ft apart 3 1/2 in. high. 4 in. hard, gzy. R (Cherty shaly layers like those at RR quarry are) represented along farm lane SW of quarry by flat chert fragments in soil 4 5- 28- 17 in 3 1/ 13 18
Read Page
Page 127
along farm lane sWj Linn zearry S of Walnut, 58. s> 10 ft interval. T Whitfieldella calimost me. Expired also west ward along a same farm lane but up the western hill side 25 ft interval see next page for shorter right measure ment, U Whitfieldella cylindrica, [illegible] [illegible], [illegible] along pen canal direction like
Read Page
Page 128
1st [illegible] S of Walnut street. Culley east of small stream early crinoidal limestone, slid. 11 ft interval. T crinoidal l. + Whitfieldella cc. Aptyxa reticularis. Schmattella. 20ft 17 ft interval dark clay rock weathering soft. 1½ ft interval. 1½ ft firmish rock, of minestly crinoidal in place. U 1 ft. crinoidal l. full of Whitfieldella, some Aptyxa reticularis. 1½ ft interval, shaly limestone 2 ft massive limestone, firm. Whitfieldella cc locally near middle of this layer. 8ft 2 ft. Weathering badly = firmish limestone. 1¼ firmish l., fairly solid. ½ ft shaly l. + soft shaly stuff. 1 ft firmish l.
Read Page
Page 129
NE of B[illegible] 2ft creamy crinoidal l, interbedded with thin clay 14ft north inter bedded greywacked shaly limestone. 4.5ft moderately crinoidal l, massive 5.5ft creamy crinoidal l, massive sponges 3 pumice 14ft massive l, somewhat crinoidal, massive 48 13ft interval, measured E through the hill, 61 ft (T) Whitfieldella rock like me if the layers at the localities S of Walnut Street in small gulley N of Spring St farm house on E side of this hill. Whitfieldella crop at about same time on West side of hill by quarry — 21 11.5 ft of sandy l, exposures, best exposed in lower 3 ft of section. — 9.5 U | 1/2ft very typical Whitfieldella layer here. — 9 9ft limestone l. massive. [illegible] Crat Orchard clay shale, 57
Read Page
Page 130
"Hillston Condensed section 30? Hillston 20. 157 1/2 P { 11 ft Black bituminous shaly l. + Pentamerus - 146 1/2 61 26 ft Covered, 24 ft exposed at RR quarry = Pentamerus beds, -96 1/2 Q-3 ft shale with flat backed Streptelasma -98 1/2 { 3 1/2 ft Massive l. + Wabynites maximus 3 ft limestone + shale interbedded 10 ft, Mississippian l., chalc. 2 ft Large Fossils Collected, R 2 3/4 ft Massive l. Very irregularly bedded 72 1/2 6 1/2 ft Well bedded + laminated cherty shaly l. Tremella -66 5 ft Covered - S 1/2 Walnut St. -61 13 ft Coarse Crinoidal in part - covered by Walnut St.-48 7 1/2 ft additional at Bishu dam) Massive l, S- 1/2 ft Partly crinoidal l. Ripple marking { exposed also 10 ft interval. S 1/2 Walnut* at Bishu dam T - 1/2 ft Whitfieldella, iogen daga, 20 ft chiefly its matrix ark. 48 U- 1/2 ft Whitfieldella cc. 6 9 ft brownish l. massive O 62 ft Crab Orchard Clay 3 1/2 ft O agyrin 5 ft foraminifera cherts with lower 1/2 strongly crinkled 5 ft strata have marked layers.
Read Page
Page 131
(9- 4145 36) 28,0(8 2184 NEV Birmingham
Read Page
Page 132
New Bishops dam Of grey gritty New Bishop dam, 55 ft interval, all massive rock. 9 ft gneiss, with lower ft pretty cleated, 5 1/2 ft dolerite cut through, 66 ft continuous cut indurated clay} 3 1/2 ft Daytim limestone 4 ft strongly ferruginous chintz, very irregularly bedded, lens-shaped masses in. 1 ft strongly mottled ferruginous chintz. Ripple marks N 80 or S 2 - 2 1/2 ft deep 2 1/2 in alveolar type, cross folded toward south: 6 village N
Read Page
Page 133
Valley Hill. Hills Mr 20. Core. 11ft black bituminous shale & stuff with Pentamerus ce. in plenty greenstone, 61 24ft interval Road runs of [illegible] Pike toward south 26 ft. interval, Base of Pentamerus zone Flat s tepid azma layer,
Read Page
Page 134
"Hillshrew College & Ambrose hills. There is no certainty where the basal beds of the Pentameros beds in the following section come in. Hence the coarse crinoidal limit we may come in in the lower part of the Pentameros section. Apparently, however, the crinoidal beds have a strong local westward dip here, Westward 25 mi., along the Danville pike there is a quarry S of the road with sheifeldasma with flat back wings partly thrust local rock. The overlying rocks should be the basal part of this zone lithologically but contains no Pentameros, if mi W, but N of Danville pike, is quarry with Pentamerus ce at top but not in underlying section. About 10 ft lower is blue cement me top with flat backed sheifeldasma. At quarry mentioned S of Danville pike the blue lo is underlaid by shaly clay beds as at RR quarry, but blue L here is the upper, On Danville pike. SW of Hillsboro. Pentameros! But not known. 15 ft - interval. 13 ft coarse crinoidal NW of College building N Cincinnati pike crinoidal L may correspond to lower part of Pentameros L section,
Read Page
Page 135
XIV Wammy, Ral. Lin Garp. Pt I, O'Kant, Springs Osgy Pt O'Kont beds, Pt II O4, 3+4, Crebstron - Anctoth. Sut cent + Cant, Cyl. dipida. mm't & mm, spicula. Qm't + ly, shcra. XV, 'mr's 't'p'ri crvngsta. Willd + O4 2, On coll, 1/2th anthora, Ogla in O'llo cell, Non top 7 lobb Gm., other procta. Qal, O4, III, Stmmatops. O4 3+4, Oal, Pt IV, Crude + 'm'fect O4 2+3 Drethmatic of Cassimone, O4 2+3 Drethmatic of Cassimone, XVI O4 H, P'al. Cas On Pt's m'trally. Qal, Cus On, Pt's m'trally Pt 3, On 'f'rovo Willd + Qal, O'Kant, Crvngsta. XVII
Read Page
Page 136
XIV under my bed, in group. Pt I, plants, springer casey pt Bloomfield, Pt II, Palisings, Pt 3+y, crickets - anoth-er- Sutent & Cant. Caledonide, mint & tan, shrubs, Dirt + Ivy XV mrs' trip to cleveland, william & aunt, 2nd anthro. agile in other city, new hp 1 with gown, other friends, Pt I, Pt II, IV, crickets + minted XVI Orthotriches Cusciniaceae, '20 'sandy', ap. a., Pt 2+3 Pt 4. Rd. bus on Rt, mountain road + mnt of farm land, Pt 3, & friends, XVII, Pt I, mnt of farm land XVIII Pt 2+y, O'Neil, pt 21,'50, p.a., & pt 42,
Read Page
Page 137
XIV Inamung Ool. Gin Camp. Pt I, Plant Spring Aggy Pt Pleasant bed, Pt II, Palenathy, Cricketon - Anoth Lk. Pt 3+y, Sut end+ Cnf. Cal depida. munt+ Oran! Owl + 1by shcrr, XV, Pt 2, Pt I, munt+ Crngsta. Wulst + Rgty in Qctte celli, Nw bp 1 lubb Cswm, Atten frondy. Ool, Pt II, Strmnation. Pt 3+y, Ool, Pt IV, Cndt + Mnrch? XVI Pt 2+3 Onthustic of Gssimono, Pt H, Ool. Gin San, Rvi munt+ Oal, Pt V, munt+ Qctte frondy. Pt 3, Oat frangl, Wulst Qctta XVII, Ool, Pt VI muntation
Read Page
Page 138
XIV Pt I, Olant, Springs Casey pt Olant bed Pt I Pt II, Parknthy, Crchtrcn - Anct h Lo. Sut cnt + Cant, Col depda. mltnt + mtl shuc, Olnt + 12y XV, pt 2, On cbl, n lth cntlhp, Oglr w Fstn Ccl, Rwr hp 7 bbb Cmm, oltr Fmnts, Rel, pt, III, Stmtnplps. pt 3+4, Ol, pt IV, Crd + Wlcr XVI pt 2+3 Ontlctrct of Ascsmine, '20 Pt 4, Rel. Cln On Pt, mtnclpm XVII, pt 4, mlnt + Col Fmd pt 3, Otl Fmblttds Fdd XVIII, Rel pt VI, mntrslpnn
Read Page
Page 139
XIV Pt I, Olati, Springs Oat Pt Pleasant beds, Pt II Pt I, Olati - Sanitarium. Pt II, Palerithy, Pt III, Palm Beaches - Sanitarium. Sut cact + Cact, Col. depuda, [illegible] Pt 2, Pt 1, Olati beds, Olati in Oatati City, New hp 1 bedd Cown, Other Springs, Pt IV, St. Ivesation. Rt, Pt III, Sanitation. P+3+4, R+IV, Cact + Muth. Oat 2+3 Pt V, Olati - Sanitarium. Pt VI, Olati, Springs, Pt VII, in Pt, Olati beds, Pt VIII, Cact + Cact. [illegible] [illegible]
Read Page
Page 140
XIV Pt I, Plants Springe Aspy pt Bleamant beds, Pt II Pt II, Paleothings, Cricketwin - Smorth F. Sut cent t Cant. cold dipuda. mint & min spuce, Gnut & hy spuce, XV, Mcaltripon crungeto, wild+ Gota Pt 2, ou cal, v th catches, Pt 3, mcal trip l tubs from, other plants. Pt III, Stenotripum. Pt IV, Oal, Pt II, Crude + Miftrix Oat 3+y, XVI Orthocentricl Descentium, Oat 2+3 Pt 4, Pal. ou on, Pt V, muttcaly. Oat 4, XVII, on munt & from, Pt 3, but frowe, will do, Pt IV, on cal, munt & from. XVIII BCD AE go soft all thum munt calthay [illegible] [illegible] [illegible]
Read Page
Page 141
XIV Pt I, Olant, Springs Pt I, Olant, Red, Lin Grp. Agry &t Slonant beds O2 I O4, 3+4, Pt II, Palathy, Cricktown - Smptth F. Sue cont & Caf, coll dipslo. inclt Oren, Oar + 15y spccs. XV, mct cypri crvsta, Wlkt & O2 2, Pt 2, Ogru in Gslk Cks, Nm hp l thd Cmms, other forms, Oel, Ot, III, St innatips. XVI Orthoceras of Asgctwns, .20, cmrs, apcs, O4 2+3 Pt 4, Red, Cu Sn, RY mctslm. XVII, Oth inclt &t Fmlle Fld Pt 3, Gt Dsgrd, Wlkt Fld XVIII, Pt IV, SHAX O4 1+2 [illegible] [illegible]
Read Page
Page 142
XIV Pt I, Olant, Springe Pt II, Pt Oleanat htdo Pt II Pt II, Palenthly, Cricketin. - Anctth. Sut cntt Cnt, Gll. tprda. Inkt &rtn! stucco. Owrt & 1y'stlcvo. XV, mrd r'pion cr'ngsta. Wldu+ Pt 2, su cnt, 'ltm cnttda, &rg in Oclt cldi, Nrm tp 7 tddo Cnm, &ttv fprnt, Ool, Pt III, Strmntym. Pt 3+4, Oal, Pt IV, Cntd & mthft XVI Duthtic of Usgs'rs, Pt 2+3 Pt H, Col. Gm Sn P'tr muntcltm XVII, Qtn inult & Clttrndk: Pt 3, Gut frnvo Wldo tdo XVIII Palpr VI mntrntym Pt 142, Pal. pt Swhyn tn Pt 2+4, Gt 2+4, Pal. pt Sthgtn tn Pal. mrtgm &d nrd. P. 189. Pt VIII,
Read Page
Page 143
Drewthorp, New England F. 3, B. Good - Green Lake, N.Y. Grindme = Wren Street, N.Y. Indian River Dam Farm of George, Putnam Co. Balko II., & Fig. 19. Garden and Farm. See my notebook on the opposite page. 1916 N. F. O'Kelly with 905 U.S. 27½ Branfield. S. S. N. Z. L.L.8. U.S. S 1 or 2 weeks Branfield at least 5th mile in week and at first mile in field. 513½ E. and blank above in Branfield, 902 ft U.S.G.S.
Read Page
Page 144
No text detected
Read Page
Page 145
OXFORD NOTE BOOK No. 364.
Read Page