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Campbell Co. 0590 Soil}\ Benjamin Beall's land. 591 " 592 Sub} Alexandria. 1856. 1315. Marly Shale. \frac{1}{4} mi. from Newport, on Alexandria pike. Between Newport & Belleme, 01316. Marl from Siliceous Undetm. 10 ft. from surface. Gallows Gap. 1875 O1320. Sandy Ferruginous clay. 1875 3ft from surface. Int Vernon road, \frac{1}{2} mi. from Alexandria pike. Reddish trans. glacial ? 1321. Ferruginous clay. Glacial ? Side of road, 1 mi. N of G.R. out; Creek. North lead waters of Philip's creeks. A branch 1875. follows the road north, 1322. Waulding sand. Glacial or Fairmont? 1875 \frac{1}{2} mi. NE of Newport Reservoir. See map 1324) Soil, Glu. G.B. Hodge farm 1875 ) Flat Woods. Waters of Philip's creek. 1\frac{1}{2} mi SE of Grants Lick. a few pebbles of milky quartz. 1325. Same locality as 1324. after April. 1875. About 1 mi nearly S 1326. Same 1327. of Grants Lick P.O. 1327. is said to have siliceous underneath. Three feet 1324-1327 may be Fairmont soil. 1328. Spur of hill 60 feet above soils 1324-1327. 1875 Same locality as last 1329) Soil. Sartrey's land. 1875 \frac{1}{8} mi. from Newport. Alexandria pike. 1330) Subsoil. 1334.) Limestone, full of fossils. 1mi S of Cold Spring P.O. 1331. Soil. with chert. Over undetm Waters of Pond creek, near Pond creek P.O. on new pike. 4 mi SW of Alexan dria. Claryville P.O.? 1875 1335) Marly Shale. 2 mi S of Newport. Licking 3 mi. creek, 50 ft above high water marks. 1875 1336} Same locality. Marly shale, Beds are 30 ft thick. There came 60 ft above high water.
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3 mi. NW of Court house at Hamilton, NW branch of Two mile creek, along by road from 704 N to 869. Hole Olympus stone moderately slimy does not occur between 727 and 730, the remainder out well exposed. Dinethis ritoma, single good specimen at 760. This is lower than supposed, but the place may have displaced a slight distance. Numerous shallow exposures along the roadside this level. 3 mi. W of North of Hamilton, 1/2 mi West of 860 in section 15, the same faded cement out at the base of the Waynesville bed, as along Salmon Run is found. A good Oreuthis ritoma in a lime but mineralized fossil the interior occurred 20 ft lower. According to this the Dineths ritoma range should be placed here at about 780 ft. Acidaspis onealli. Thrax with 10 segments, The pleurae with two spines, Posterior spine of posterior segment = 4 mm. Anterior spine of first in segment = scarcely one mm. Posterior spine of 5th segment = 3 mm. middle lobe of thora near anterior end = 4 mm. lateral lobe 4 mm. mean middle length of body, not counting the spirals. Oxydium with 2 spines 6 mm long, 4 intermediate spines 1/3 mm long, and at least 3 lateral spines of which the inner two are about 1/3 mm long. Head and spines of oxydium rather distinctly scarred. A second oxydium has the interne- dicti spines scarcely 1/2 in long. Slight difference. Thigh bank of Four mile Tallawudy creek. 2-2 mi. N of Oxford, west end part of section 11, found by Dr. Stephen R Williams, in lava part of Waynesville bed,
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NE of Riley Dinuthis retorsa 22 ft above creek, in SE corner 16, Septaeon obam Xor'dalis is fairly common or just below Dalmanella injura same distance below. That also near bryx. 3 mi NW 7 Mile Po. Herbilla insulpa 50 ft below eros strata where sections 16, 17, 20, 21 meet. One will meet the creek must be partly at time of Waynesville. Henry Krumler farm below iron bridge in Dry Fork, Herbilla - and culpta. 10 ft down - Septaeon obam brydalis common, occur in intervening sections also. 14 ft total. Refinguerina distubbed layer. 16 ft 7ft total Stroph. neglecta, 17 ft total. Stroph. malting typical 18 ft total Stroph. antaus + Septaeon obam brydalis, 7 Stroph. planumulus. 20 ft total Stroph. neglecta. 20 ft - 22 ft Stroph. neglecta - Stroph. miles very common, 23. D. minima retorsa Stroph. planum- luna, Crania laevis injura, 26 Septaeon cerca + Dalmanella injura both rare. 36'q Dan's inculpta dan'tu retorta - lineulla and? x Herbert illa 2 culpta 8-71 ft above sea level. W Gary mill, 3/4 mi. W of Millville, 2 mi NW along N/S road, NE q crossroad 1 mi West of Millville. 771 ft above sea level - top nodular layer of Ambeum. The wedging limestones and clays well be jossed - 4ft w/ plenty JD almanac at top, thick heavy bedded coarse limestone layer 8 in thick near base J Waynesville. 1757 ft = Din retorsa accoding to calculations. Dinuthis retorsa 2 mi E of school house No 6 in section 27, 3 1/2 mi W of Millville. at about 755 8 q school S in section 20, 2 1/2 mi NW of Seven Mile Po = Dinuthis retorsa.
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7. 3/4 mi S J Daytonville. Stream NW G. Teutanks. Upper Nebulosa neglecta 15 ft interval 20 ft interval Strongeneu neglecta 5 ft interval. 2ft Lynx Hebetella in angula 7 ft at river level. 1485 Upper incalyptra 22 1463 Small incalyptra 520 1413 Base magnoskill. 28 1390 river level. 8. Chreat name strong West dip. Dunetius antognachata Pistolantrites atirica abundant Hebetella shanlicka Strong new marks & a few Ammonite fossils of several kinds, most with in the y Magnosville & Iron y Shell. 9. Half mile west of Charleston, imme- diately S of bridge, Rivers 5 ft above East Fork. Cincendensis very common in clinks containing numerous shelly muss good for k baling. 10 Lynx + Leptolina just my knife. Eddies Run 1 mi E & County line, mile from Decatur to West Munier in Adamas Cri Cincendensis commun. Strong feet. 181/2 ft interval. '3 ft leptona rare. 5 ft interval. 1ft Leptaina Nesumtridali abundant 10 ft interval. 1ft Lynx Dalmanella associated, part in separate layers. R = 3 1/4 mi NW y Bent mill on dirt road, across Eagle Creek. My watch. 1630 Mjeka incalyptra Larger 161/2 ft interval Strong new neglecta & retorta, 3ft interval, neglecta retorta. Strong ammonites. 1600 bed y edge creek. S, 3 miles NW y Bent millle Smith & North y Gordon Run, up stream south of Eagle Creek, 1805 Clinton about 5 ft above base, 1690 Calazyga threads over lower mezzosa, 1689-1680 fusida + planumfma very common. 1670 Cincendensis. Strong clay beds. 1645 Eagle creek 1830 top of hill 1820 Bale y Clinton
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Vanceburg, Shale Points R 3½ ft fine wave marks 56½ in. 3 ft interval, with freestone layers at top, top of section. 8 ft interval, chiefly shale, but several 3 ft freestone larger. I have not seen. 5 ft 5 in. Interval. Shaly = rubble shales. 1¼ ft 1 in freestone layer. good. 1½ ft interval. 2 ft 7 in heavy freestone layers. 10 ft chiefly shaly, with some freestone. 11¾ ft freestone lingers. 10 ft chiefly shale. quarried 4¾ ft 3 layers of freestone, could be A at mine. 8½ ft shale with several layers of free 21½ ft chiefly covered. Bannock apple lace and shales. 62 ft 29½ ft Mine from top carmacaceous shale Mine Carmacaceous shale 19 ft to face of clay stratum 13½ ft to thick end of bog, Mine carmace leathery, lace macs shale. Argillaceous and shale - Top of Olive shale 40 ft Lower part soft but carmacaceous nearby. 103½ ft interval. Light colored, soft clay shale Chagrin Formation. 60½ ft From part of olive shale down to bottom of out at bridge on pipe. Impala Williams limestone and large limonite about 10 ft below top of white division of black slate, 95 ft Ferruginous shale rubble 42¾ ft Ferruginous clay shale rubble 59½ with little freestone. 13 ft freestone & shaly 18½ ft freestone & shale < fresh collected. 11 ft 3 in freestone ledge. various levels. 37 ft interval, freestone blocks at 16 ft freestone abundant, family cherry on it good Tarramus midway 2½ ft. stone. Nodular stratum of impure lime abundant. Tarramus rather rare. 23½ ft interval with heavy freestone layers intervals up to top. galls & heavy layers at various 44 ft freestone with Tarramus & anda 2 ft 1 in freestone layer, solid. 5½ ft interval shale. *4ft {3¾ ft} freestone ledges, canada galli {2in 1½ ft} chummm. 8ft 6 in interval, purple ferruginous shale 1 ft freestone with canada galli abundant ferruginous. 46½ ft shaly interval. I remember mine 5½ ft freestone 31½ ft little freestone, ferruginous near top R. (clay) & sandy shale rubble into
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Vanceburg, Alum Rock X 38\frac{1}{2} ft (internal top - freestone full of Barnums inner 11 in weathered to white clay, my rubbings, no chance. 15\frac{1}{2} ft S unbury Black shale certain, 2ft 6 in freestone layer top = ripple marked 3 ft 6 in freestone layer top = ripple marked 4 in freestone. 2 ft 10 in several freestone layers, top layer ripple marked. 14 ft 5 in freestone layer, top = ripple marked shaly at base. 1 ft 1 in freestone, ripple marked at top, 4 ft freestone, several layers, 1 ft 8 in freestone, top = ripple marked, base = shaly. 1 ft freestone, shaly at base. 1 ft 5 in freestone layer. 11 in freestone in rather thin layers. 7 in freestone str 2 layers, top of top layer with ripple marks. except near top and base 36 ft 9 in internal, chiefly shale rubble, but covers 4 in freestone 5 ft 6 in arg. shale rubble. 1 ft freestone layer. 6 ft chiefly shale rubble, covered, 1 ft 6 in freestone layer, shaly at base. 2 ft 2 in freestone layer, internal at base B 1 ft 7 in shaly. 7 in freestone. 2 ft shaly, 10 in freestone. 1 ft 1 in shaly, 1 ft 6 in freestone layers - top wave-A marked. 38\frac{1}{2} ft 14\frac{3}{4} ft 3 ft 2/1 42\frac{3}{4} ft 50\frac{1}{2} ft 1 ft shaly. 2 ft 3 freestone layers. 7 ft 6 in {jumbled chalk formed top = 2\frac{1}{2} 1 ft 8 in freestone. 21\frac{1}{2} ft chiefly shaly, inner part more argillaceous and weathering, in lower 5 ft to whitish clay, No phlychastic nodules. Top of Alum shale certain, 24\frac{1}{2} ft 3 in drawn to ROR large, Lynne Williams and chert 15 ft del no top
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Vanceburg. Shale Point B₂ R- 1ft. Benavista Gts ledge. 3) 21 ft {Including white clay section above (Sunning + Sunning shale film, 4) 16'3" Bera SS, 3 ft layer, w/ parting near middle, 9 in layer, 6 in thin shale free-st me, 1ft 3in layer, ripple marks 1 in layer fine ripple marks 5 in layer fine ripple marks 5 in layer fine ripple marks 9 in layer 10 in several layers w/ ripple marks layer. 1ft 11ft 4in layer w/ ripple marks 7 in thin shale layers w/ ripple m 10 in layer, splt thing in two. 8 in layer. 9 in weathering apt and shaly, 1ft 6 in layer. S now y free cding - 14ft 8 in, D to rep away due to washing wt y clay along edges and desity of y free-st me layers. 340's ft chiefly shaly free-st me rubble. Bednd. shale mgh {37'2"ft chiefly shaly free-st me rubble surface 4in free-st me 1ft 3 in shaly 4 in free-st me 5 ft chiefly shaly free-st me rubble. A₂ Vanceburg Shale Point 2) Bednd SS 3ft 2 in free-st me layer, largest seen. 1ft 3 in shale 4 in free-st me. 3ft 11 in shaly. 1ft 2 in free-st me 1 ft shale 2ft 7in free-st me, irregular bar 2 in free-st me irregular bar, 1ft 5 in shaly 9 in free-st me. 5ft 6 in chiefly shaly covered in part 9 in free-st me. 6 in shale 1ft 9 in free-st me 1ft 2in free-st me 8'4" 4 in chiefly shaly 7 in free-st me. 1 ft free-st me. 1ft covered 9 in free-st me. 8ft 6in {2ft 3in shale 3 in free-st me 9 in shale 2 in free-st me 1ft 4 in shale 3 in free-st me 3 in shale 4 in free-st me 3 in shale, 4 in free-st me difference due to crumpling 21ft 6in. chiefly covered, Bednd. =Sunn Bednd. shale at base.
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Linmoreville. Rollway section, 1/4 mi up the bottom from the station, and up the second hollow on the west side for 1/4 mi, then up the railway northward. at forty section below B1000 there are 38 ft additional of freestone, and shale freestone making a total of 274 1/2 ft. Below the Maxville limestone without exposing the argillaceous shale quarried by the Peebles Co at the base of their grassies. 5 1/2 ft {Middle part brecciated, {Maxville limestone, arenaceous look, {18 ft Covered {22 ft Thin shaly freestone rubble. {13 ft. Into shaly rubble, rather coarse pieces, {Nine massive freestone, weatherly, {25 ft Shaly freestone, {2 ft Massive angular layers of freestone, {10 ft thin freestone shale rubble, covered section, {21 ft Rather massive freestones, {(21 ft shaly freestone, {(17 1/2 ft shaly freestone a little Base of rollway exposure. thick, 92 ft interval, B 1000 - Freestone layers 1ft thick weathering like large modular slabs. Linmoreville, a quarter of a mile westward along the top of the elm's river cliffs, a layer of fine clay overlies more firmly the top of the Maxville limestone, zigging down into it about 5 ft. Maxville section at that locality, 6 ft fire clay, green flint clay. {2 ft very brecciated, disintegrated irregular surfaces, {2 ft Massive brecciated in part, {integrates easily, {1ft 6 in soft rather coarse breccia diz- {1ft 8 in massive coarse grey l. {at base coarse, 1ft 7 in massive stratum grey lime brecc. 2 inches irregular shaly n breccia parting, 1 ft coarse act grey limestone, lower surface uneven. 1ft + a - stratum of soft coarse breccia. 10 ft massive compact limestone with some calcite brecciated pieces, 21 ft Massive grey coarse limestone brecciated in part. 5 ft very sandy light grey limestone, Some particles rounded + worn
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Oliver shale exposed at Harrison chapel, near J B Harrisons store, 6 miles above mouth of Laurel, at mouth of Grassy Fork. Smoking shale exposed south of Harrison chapel 2 mile, in road to mouth of Laurel. 4 mile farther on the same road, the Smoking shale is underlaid by characteristic Berea sandstone with ripple marks, along the Oliver river. The Smoking shale underlaid by the typical Berea sandstone, and overlaid by 3 feet Bernal at a city ledge and a considerable section of pinkish clay as at Bernal Vista, is exposed at the Pine Hill School about 2 miles from the mouth of the Laurel, coming from Harrison Chapel way. Beyond Copers store at Gran Lodge the Bedford SS is exposed. at Mrs. W H Blakeney's place store, about 4 mile east of the bridge the Smoking is exposed. About 200 yds up Laurel from work crushing near mouth of Laurel Sm. oily shale The City ledge with the underlying Smoking shale is exposed half way between Ringlese and the Tannery, or 2 miles below Ringless on Trace fork of Kinnickinic creeks. Along RR SE of Ringless the City always shales are well exposed, at near Big Cut the Black Hand SS ? comes in. On county line at Big Cut. Top of exposure. 16 ft 6 in thin bedded to sandy white see cutpage SS, rapid dips a cross bedded, pink, only the latter. 5 ft 6 in Massive coarse grained SS with irregular lamist nodules of iron. From me at top of Maxwellville line. 42 ft. Massive light gray limestone, pk. exposed along road extending my at eight angles to cut. Collected forints at top direction after 10 feet. Top of cut. 28 ft. Massive c rase lime, ap- parently with mud and sand slightly fossil, forms with Semolina ant gradations + turgidica. On 5 miles (arrow) 8 ft. Red arg, shale. Bridge 38 ft above track. 29 ft 6 in thin bed, fine silt mine
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A third of a mile North of Petersville, a road turns off Westward up a small creek, and 300 yds Westward forks, one branch going up a steep hill, Northward; A bird half way up the hill, the Sunbury shale is 15 feet thick, and is underlaid shaly sand at me, and about 5 feet below the Sunbury, a 2 inch striation is distinctly visible marked, probably indicating the equivalent of the Berea sand at me. 1/2 mile West of Noah, road turns off towards left, and goes down steep hill. Here Massive sand at me is exposed at top of hill = 85 ft. An interval of 45 ft between between this de and top of Sunbury Sunbury = 14 ft 6 in. Black shale. Barnwell shaly sand at me, with a few ripple marks, at least 8 ft. Interval unknown. Ohio black shale not well exposed. Top of Black shale about 110 feet above spike junction level accords my to estimate only, At Glenn Springs the Silurian lime stone has a sort of light smoky brown color and is, 13 ft 6 in. thick, with black chalky above and beyond clay shale below. A mile + one half from Glenn Spring and 2/3 mile South of Beulah's Spring from base of Ohio shale to base of of Sunbury shale, = about 156 1/2 ft, 13 ft 8 in Silur limestone, Sunbury, in Berea equivalent, a 3 in. layer of sand- at me is beautifully ripple marked. Below this is 10 ft of thin shaly sand at me and the same material occurs above the ripple marked layer. The Berea has lost its characteristic appearance except for the one ripple marked 20. layer. Base 5 ft Sunbury shale exposed, 5 ft covered. 16 ft white clay purple at top, 1 ft layer of freest lime. 10 ft chiefly crowned clay shale and several free lime layers 44 ft practically continuous very soft dreamy freest lime layers. 22 1/2 ft chiefly crowned. chiefly clay shale + thin pure lime. 1 ft strong pure lime 20 ft covered. No evidence of heavy pure lime layers 1ft 3 in. heavy free lime layer of white
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My gully snaps, calls my road comes at Valley then up hill along g. 15 ft S Imburg shale fragments covered. 15 ft covered. 3 ft freestone massive. 7 in freestone, 3 in freestone, nipple marked. 9 in hard lime. 9 in weathering to chalybeate freestone 1ft 2in freestone? 81ft covered, partly fairly accurately: 22.3 Ohir shale certain, 22-1/2 ft covered, probably Chir o shale zone generic covered with shale fragments. 48 1/2 ft most minor and fairly error working side. See below! Trace 1 measured section, 11 1/2 ft rotten massive layers 6" up thin limestone, layers covered 22 ft chalybeate limestone at base, rest 8" ft massive limestone layers. Most minor cliffs will expand 4 miles west of [illegible] Valley, at Harlan Hill. Flats collects section of most minor measure, in former trips, W.C. More found calgonumana and juncea and Whiteidella siltica. Found also Leptodora in minor beds. NE g stn at [illegible] 4in limestone 6" clay 9 in limestone 3 in clay 8 in limestone, in several layers, 4ft clay cleft on top. Immediately S of bridge across Indian Run hand of Colby, 1/2 mile SW of Poplar Flats, moved to history. Plants. 1ft 3in Clinton base, white 1ft 3in Belfast, clay with a few thin layers. 6ft additional Saluda clay, partly purple. cured. The limestone layers in the Belfast bed are whitish as the Doytlin limestone, and these limestone layers contain [illegible] simulate from incidentals - finity and an depression new lake. Directly NW of Poplar Flats 7 limestone 1ft limestone 1/2 limestone 4in clay 3 limestone 6 in limestone 2ft 3in clay 1in limestone 6 in limestone, 1in clay 1ft clay in 12 layers, layers 2 in limestone, 3 in clay 1 in limestone. 2 in clay 4 in limestone. 6 in several + clay layers. 1ft 3in chalybeate clay, then limestone about 3 in limestone top.
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Sectionally quartzite in northern edge of West Union, on Ogleby Fork road. Projection 19 5/8 2ft and Massive ferrimisch gravel. 2 ft. " which l., splitting into 2 layers; 1 ft 4in. massive black l. duller marl, 6 in thick l., breaking up into 2 marly layers, 11 ft 9 in. an massive cemented, central part chinnical) and above this a thin nodular layer, 4 ft 6 in. massive third gravel with surface as are- terial, upper surface was marked. 2 ft 10 in., ferrimisch ferrimisch crass l. 3 ft Same as above, but with cherty noduled layers, 1 ft 8 in. massive ferrimisch coarsely worn marled at top. Base of spath. odent quartzite. Black argillaceous Osgood shales almost directly be- neth; At Benterville, the Clinton forms the summit of the ridge. About half way between Benta- vil and West Union there is a small knoll which jurn- both carries the system shall part of the West Union cliff. Loc. 1. Five miles east of Flemingsburg, Staff Wallingford road. Black shale hill on property of Charles Blanchet. 1 ft Black slate, partly Sinking, 2.5 ft shaly sandstone, partly Berea and Bedford. 113 ft Ohio shale. 46 ft red clay, apparently in upper part of Oxford. At least two limited sue fragments visible in the clay, and hence not supposed to be West Union, 27 ft red clay with ferriminnous frag- mets of limestone common, 18 ft red clay with thin limestone fragments such as are common in upper part of Crab Orchard. 36 ft clay shale undated older of Crab Orchard age. Level 1, strike in front of home of John Parker. I think the density of Crab Orchard could be determined along future since Clinton's exposed eastward.
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21/\nR on road from Wallingford to Fox Spring,\n13 ft argillaceous shale Conshohocken?\n32 ft 6 in Dray Branch. First ones thick,\n9 in clay shales, making of almost\nenire section.\n11 in fresh one.\nShale, thin, whitish.\n23 ft, 9 in Covered, chiefly argillaceous. Taunton\n17 ft Sunbury shale,\n18 1/2 ft. Bedford Berea - shaly sandstone.\n14 ft Covered, Bristol's chiefly Bedford.\n172 ft Blue shale exposed.\n16 1/2 ft of dark brown shale with about 20\nlayers of greenish clay = Conshohocken?\ncircular clay shales.\n11 ft argillaceous shale.\nR. Ferry's massive mudular clay\nlayers,\n14+44\n3) 1/2 mi. N.W. R & Y McKee, the West\nUnion, richly fossiliferous and\neasy to collect, is 9 1/2 ft thick.\n\nsolden Seal a Yellow Root and\nGinzing, at home of RY\nMcKee's house, near N.W. Union\nMills,\n4) At George Hamm's house, 1/2 mi\nS.W. R & Y McKee, the West Union,\nphotographed, is\n\nat George Hamm's\nBlack Shale shaly? Conshohocken?\ndirect one, massive.\n4 ft carbonaceous, richly fossiliferous.\n1 ft 9 in Sandy fine grained limestone.\n2 ft 6 in before third clay shale...\nto bottom, charming,\nmoderate uncertainty.\n5) One and one half miles N.W. Union\nmills, the West Union is 9 1/2 ft thick\nand consists of lower massive\nlayers and upper shaly ones, fossil\nappearing rather scarce.\nJust North of home of Frank Marshall.\n\nat short distance south of house, the\nWest Union, all massive limestone,\nrather richly fossiliferous, is 8 ft thick.\n\nat mouth of Anderson's Branch,\nWest Union is enormous.\n6) John Branner 1 mi N.W. Union Mills.\nChert shale.\n2 ft Shale and a little greenish clay,\nshale layers\nfor the purpleish, very black\n5 1/2 ft shaly light greenish clay, with 3 or\n7 1/2 ft West Union L. Have just exposed.\nMr. Fieldella in West Union.
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Some difficulty as fact, Breeze Sandstone = Glassland, 20ft Builder limestone above the builder limestone of the Lantern Sand and Supply limestone quarry, 46ft Limestone exposed in quarry. Top of Yzgan. 84ft Yzgan. 16ft Black Sand, exposed. Limelight Point Cut: on Minchhead and North Fork RR. 6 miles by Paragon Sham Sandstone. 5½ ft cored, {37ft 6 in White limestone, Fossiliferous} {7 ft White} {2 ft brownish clayey material} {3 ft 6 in greenish fine clay bands purple marl beds} {13 ft 6 in Massive whitish L.} - - - 1 ft thin Limestone + clay layers interbedded. 7 ft 3 in Yellowish very fine grained limestone. Porphyroids at base. C 4ft 3 in slate cored clay fine clay, with siliceous and small nodules the size of wheat grains. A purplish colored band just above the middle, 14 ft Massive stratum of light slate now cored, some what crystalline L. with a few fossils. 9 in = finished clay interbedded with limestone like that above. 6ft 3in Massive stratum of light grey fine grained L. or lithographic stone, weather- to yellow, in some places chrysolocane. 1 ft 6 in Massive somewhat crys- talline L. R See 2nd page following. Same section as above. 153 ft Sharon conglomerate. Massive quartzite 20+ cuple with white grants, pebbles irregularly arranged, forming cliff along structure. 5½ ft cored 2.1 ft most exposed, recessive to medium bedded dark grey course grained & crystalline L. freshly prisms. Very fossil iferous 4-5 ft below top. 18ft Cored, except for loose blocks of limestone. 4 ft 6 in coarse grained to crys- talline dark grey limestone. Topy cut. T {3 ft 6 in Massive grey L. {4 ft Massive stratum of slightly grey somewhat crystalline limestone. 2ft yellowish clay with white fragments probably due to decomposition.}
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Limestone Quarry 3 mi. West of Olive Hill. R > 4 ft shallow parting irregular. 1 ft 3 in shales thin vargely finely tree creted, fossils rare. H 5 ft Thin to medium bedded compact Marlshy sl. G 7ft 8 in Very massive and white crystalline. F 4 ft 6 in. Hematite and rone over bedded, very f.g and gray blue color mathat yellow D, 8 ft 3 in Three to four inch limestone, meaty owing nodules, especially in lower part with clay partings thicker in lower nodular to one. Clay-No 2 fire clay. Brecia in the clay looks irregularly This focal brecciated part. This Breccia extends up to 5 in above C 3 ft 5 in Clay, dark green below, purplish above, with Breccia minimal in lower 2 in. 3 in Brecciated top of same charac ter as underlying limestone, E 6 ft 3 in Very dense grayish brown limestone, mythin fayar pressure brecciated, fraved layers across the quarry, This limestone runs as a heavily 2 ft 6 in. Very white + dense l, like Daytona l. 1-2 in clay parting. B 6 ft 2 in White, or gray, small grained l. Basics claysly, irregular contact 5 like that at base of Linckerlin Park. A 8 ft Brech mass, very friage grined l. Base of quarry but not of lime and Analyzes by Mortimer Works, 1 measuring ledger, only. ledgers 1 + 2 H = No 1. Silica needed for clay G = No 2 .60 with no contain. D+F=No3. 11.75 for small Si? E=No4 4.70 B No 5 3.90 A=No 6 8.15 Top expression 4 ft 6 in Medium to massive bedded, R compact, short modules. Below A there is at least 5 ft of limestone, Mine probably the amount should be 9 ft instead of 5 ft. Bedrock from Lcaen's Products Nitrous' D cut away. Semimula subquadrata
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Section of Highland Stone Crs quartz, 1 mile E of Colvin Hill. Top of exposure. 5 ft 2 in. 5 ft chert argillaceous. 1 ft dark blue compact clay, fossiliferous at top. 1ft 6in. greenish argillaceous with two thin argillizations. Lowest layer (?) fossiliferous at base. 2 ft 2 in. Massive hard compact dark clear fossiliferous clay, weathered face very from exposure? 10 in. dark blue compact clay. 3 ft 2 in. dark chalky grey compact clay, 2 ft dark compact clay. 5 ft 6 in. (covered) Probably Carboniferous Probably this part is a clay layer. The top surface of next lower layer contains spirifera mudley quartz sandstones, Again quartz sands, clear large sections corroded. 4ft 6in. Three strata of black crystalline clay with shale partings, the upper one containing a moderate chalky layer. 3 ft 3 in. thick indurated shaly grey 1 ft mud, with shale partings, straggling sandstone, with thin shells. 6ft 10in. Massive fissure filled grey clay with chert near top Crust of iron ore on surface. 5 ft massive light grey crystalline clay stylolites plane. 3 ft 6 in. Massive light grey crystalline clay, stylolite plane. 11 ft. Massive to medium bedded dark coloured fissure compact clay, which weathers into strata not breaking up into massive slate by flattening. 1ft 5in. Dark coloured compact fissure clay 1 in shale parting. 1 ft 11 in. Compact fissure dark coloured clay 1 in shale parting. 3 ft Thin bedded dark coloured marl, layers of cement with a trace of green shale parting, Probably the upper part of the Bristol or strata in the other quarries. 5 ft for main part of quarry exposure prior to this inquiry. 3 in. yellow fine clay decorated with thin jet pieces. 14 ft Massive crystalline Ochreous This partly badly shot up by quarrying Finest place is quartz. 27 ft covered. 2 ft 2 in. Massive light grey compact clay, creek level.
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Directly east of Wignewing: Sparcest moss. 19ft (Salvina soft greenish very fine) min. 15 ft small turf brown mixed with little 2nd 12ft clay and clay with fossils? <1½ft Pleuroamblyta ovata (7½ft) [illegible] 1½ft Helotrella his cresta linigra; (Simple plannul mar. 1½ ft in turf with Rh. caprea Streptelaone) 3 in. limestone layer. 1½ft, intercal. (Styph. neglecta ralo, The plannulata very abundant. 2½ft Styph. neglecta Styph. planum lons. [illegible] to paul common 4½ ft. St in tufren Rh caprea, Styph. planum lons. common. 2½ ft. Styphana blend and plannulata. < S thy place. (Left camara on the side) porta. 2½ft Styph. plannul mar. < Rhynia peramellera Staph. elongata, 2 ft wit Styph. planum [illegible] nathal < Styph. planum lons. common and plann in a thick limestone layer. 10 ft interval with plannullia lons from Staphygnula neglecta. 17ft intervals with Helotrella ovata h. ryege & ft from four point of [illegible] down hill {tuned whl may have changed} 5ft Plannulla + plannul mar lons ( compact argil layer) 10 ft Tetradium rhizang ovatum? 4½ ft argill. limestone? Ostracod fossils + [illegible] 5 ft chiefly green capillary soil mixed clay. 15 ft 3in & 6 in well bedded limestone interbedded with clay shale. Left hand Rh. divaricata in rock nearly, 14ft 9in Zama and nath for an argillaceous rock? limestone - Zama [illegible] 10 ft 3 in interval U Cyphus crassum? Wt Aubina Calcalia distincta? N. Allen Crennum. 19 Salvina 15 White water 31 L. Letch
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Loc 12. 100 yds SW of Blackwater Station, in Wayne County) Covered - Partally the fine clay of Paragon. 13 ft of same massive limestone at the top this limestone cherty, partially chatty brecciated and Paragon. 3 ft 6 in. Thinner bedded light grey L with thin jaspified chert inclusions. 3 ft Modular-cherty limestone, with Litho- statue part forming 'Fryingpan' zone saw. 2 ft Fine-grained compact light grey limestone with Spinelite rc. - Ammodate's are uninformable centar, 2 ft 5 in. of fine-grained siliceous limestone, equivalent to the bathographic or yellow limestone of the Paragon section. Only from here especially within this Color or lithoclinder a few, full section not exposed here. 1 ft 7 in Covered. At Tresala 119, a short distance NW Y Station, 1/4 N of Blackwater Station (covered.) 5 ft Firmest and Urkes, medium (at "Firmest one" quarry, equivalent to thin bedded lags, finnish yellow. Presently. 2 ft 4 in Very basal, light grey, weathering 2 ft 7 in greenish+ greenish fine clay. 11 ft. Massive L with black brecciated L at top. - 12 ft further north. 4 ft 7 in Thinner bedded light grey L with fossils. 2 ft 6 in Modular Lithic parts into an layers, (=3 ft thick further north) 1 ft 9 in Thin bedded light grey compact fine-grained fossiliferous. 4 ft Massive bedded bluish grey fossiliferous limestone with no yellow. 9 ft 6 in Covered, Dorothy mine. Cut off the black brecciated layer above the fine clay at Paragon. At Paragon below, just above the fine clay.
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A) 1 mi NE of Olympia Springs, west of bury across Mud Rock branch. Cornfield: 10 inches in the drier, Cold soil. Barred valley, Cot Orchard clay shales On land of Jim Robinson A little feet Ciger. 5 1/4 rad B) Gunrad from Olympia Spring to Spring Springs, about half mile east of Olympia Springs road, Top of hill flat. 7 ft greenish argy clay shale, - ferruginous vesicle layer. 11 ft greenish argy. clay. 13ft 2 in freestone + Tamarunas in intervals 19 ft (considered here as a t series) greenish day, slatemic ferruginus. 4 ft 9 in argy. clay shale. cycithic series foots. 6 in freestone with Tamarunas weath. bar=45 ft 3 ft 6 in greenish clay 12ft 4in Sunbury black fissile shale, 12 ft 6 in [Argillic] argy. clay shales 1/2 Bedford + Beren Olive Shale. C) 1/2 mi W of Olympia Springs 5 1/4 ft greenish argy, arenaceous clay shales works. 2 ft weath cracks to lgy vesicular striae. 7 freest arg. + Tamarunas s modules. 28 ft (a middle clay in the ferruginous, 12 ft 9 in Sunbury shale. 5 ft 7 in Berea Bedford greenish argy, arenaceous sh with a little black shale about 6 in above tone. Olive Shale. m road to Point Le. a distance? D) 1/2 mi West of Olympia Springs, greenish clay shale. 2 ft 3 in SS. weathering into large circles 10 ft 6 in Sinuitte shales. 12 ft Sunbury shale. 2 in at base of Berea Bedford. 48 ft actually exposed Olive Shale down to face of Cicer's 3/14 quilt next ward. Total actual thickness not known, at Blue Bark Creek. ( 8 in this field a brownish limestone ) 1 ft thin lignitic an layers, 2ft freestone with clay at top and Cinlococia undulate in slate columns in the middle and fine joints, Cot Orchard clay shales.
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Directly S of Natural Bridge Station on road up to the Bridge. Type of exposure. 38½ ft Limestone, St. Benet's? 17½ ft 6 in Limestone. On top & cap. [illegible] 2½ ft with interstratified layers. 25 ft Limestone, yellowish firm grained over the base but not bottom cyclical. Type mainly argillaceous St. Benet's clay rich, Matthews & Wilkins quarry, 14 ft 9 in Rockcastle 29½ ft St. Benet's 1 ft 8 in fine clay. 5 {25 ft 3 in St. John's exposed. Litlustration layer not seen. 10} [25 ft] St. John's at Nat Bridge) Matthews and Wilkins quarry Lexington Eastern RR, partly of Natural Bridge Station 2 miles. R> 18½ ft massive white chalk. 1 ft 8 in fine clay speckled and pebbly. 12 ft 6 in fine grained whitish grey. [illegible] layer 1¼ 6 in from top. 2 ft 2 in darker blue. Precipitated layer. 4½ ft 3 in St. Julian's rock to work on layer but not so dark and demonstration better. But finding a large mass are led. 4½ ft 4 in massive white chalk beddings. 2½ ft exposed at edge of quarry. 2½ ft Limestone layer with chert. regarded as Lithostratigraphic Layer 1½ ft Limestone. Formerly mine was opened. 6 ft medium bedded compact act grey. 8½ ft 9 in green argill, shales. The upper 3½ ft 3 in is light grey clay & present fine line zone of non-conformity with this limestone over 2½ ft thin bedded grey & [illegible] 1½ ft 4 in Massive stratum July 1. 1 m. St. John's pathing. 2½ ft 10 in Massive l.g. L. at about 1 mile H½ ft 9 in Thin bedded greenish grey in St. John's quarry
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Immediately S of tractenville, 300 yds south of Hanging Park, is Strophomena megastellensis common only about 20-30 feet above creek level. About 2 miles south of tractenville, in Liberty and St. Stephen's Bay Stromella is common near tractville; About 1 mile before reaching Ridds tall, a short distance beyond Joe Snort's store, Petrrophylla and Lyrce occur on the lower hillsides but Stromennae megastellensis is found at creek level. Along Frye's creek, 100 yds N of Ridds tale, the Devonian rests upon the edges of Ordovician strata, no layer in which it rests out comes Brachyphora dorsi-folli rather common but my other forms have been seen. Along its immediate east of Ridd's table a splint of Lyrce was found a very short distance beneath the Devonian. The first layer at the face of the Devonian is 8 inches thick. East of Humphrey Bross farm mills, 6 m NE of Liberty, the other shale rests on a great thickness of limestone clayrock mills. In a steep gully N of tract West Glen of John Binnis, 3 mi NE of Liberty Middle base Cuyahoga 38 ft. Olor shale. (S something?) Jackole 65 ft horsetoe unpossibleness Ordovician alms as at least unality. At the base of the Olor shale there is, in descending order: 5 m avg. shale, greenish. 6 m silty sandy grit. This leaves for the Olor shale section to thickness of 37 ft 6 m. The middle-gray part is phosphatic; especially the clay part; and was frequently restricted along the Creek fork and River. 100 ft NE road up second gully, E of home of Jack Napier, 13 mi NE Liberty TJ. J. zebrin, 1 ft Olor shale. 6 m greenish unossy layers; phosphatic 27-32 ft Ordovician clay rock cracking to middle not possible forms conformity layer in association Cuyahoga dinosaur 1 1/2 in. Petradaium nummo abundant della Minerva 10 in. Lyrce with Platystegria x Hebat. Glammarita calli, Beatrix or -ondata, middle Richum and base about 30 ft unpossibleness from Liberty directly west of home of George Combs on Liberty Huntmill Lake Burse (something)
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300 yds North of Durham's store at Messinac, on Whippsworth Branch Robinson creek, a short distance south I found James Samp. Chapman cove, facing Mary 47ft - chlor shale. 11 in french argill. base of chlor j shale (white to bluish very hard l.) 1ft 7in (thickening to 1ft 9in) of massive layer of Devonian limestone. various kinds of fossils. 1ft 6in finnish very ferruginous sandy shale. 7ft 6in thin bedded arg. Ordovician limest one (14ft > in thickness for this drain section, by rule) per- fectly corresponding to the layers beneath the Cephaena sand above the gray horizon The Devonian limestone extends up the branch some 500-700yds at the farm of Mike Wintersley. Fossils for which I named him, this locality were collected. Devonian argillaceous shaly and clay. ? 2 fossils? 100 yds NW of Peck, in road to Messinac, directly west of leasey Mrs Martha A Tucker. T.M. & Ppmrs. 3ft 3in chlor shale. 5 to 6 inches finnish ferruginous sandy stuff belonging to base of chlor shale. 14 ft Ordovician thin bedded argill, limest one as at Messinac. A quarter of a mile north of Peck directly opposite the house of Willt Overstreet, in bed of McClune branch of Robinson creek. chlor shale with 5 sandy limest lenses & fulls long and 2 inches thick at thickest point 4 in less silvery face of chlor shale, and a 3 inch layer of similar sandy limest one at the base, belonging to the chlor shale section. 6 in Devon limestone strong thin medium grained 9in Dev. L. strong blue, Retzius limbriata.
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A mile and three quarters from Pink Branch P.O, about a mile south of Smith Fork & Rolling River, at its fork Celi's shale not crd where creek crosses the road Celi's fissile shale. remains from forms & beds: 6 in thick black arg. calcareous calca. 2 ft. Black fissile coal, shale. 3 1/2 ft. Coal cinders. 2 1/2 D. downward, with large crinoid stems. &s. divided by thin internal 1ft 7 in. D. to l. white, fine grained limestone. 8 ft. Limestone angrite. 1ft 9 in. Wormy limestone, Columbian's call'd, large specimens: 6 in. Fissile, arg., & thin Merriille & Platypus beds. 19ft 9 in. thinner laddered arg., as a. clevermact & Poek sections. Tetradian crinoid, occass lives 13 ft below the D. to l. 2+ belings at about the same limestone as the Columbian's, see Camp with collections To see. About 30s feet south of house of Mrs Mary Morgannah, and a little further S by the Running Mtn. Dism. Lyzr occurs in the creek along the road side, about 60 to ft further south. Brazzpora linepithus & fissured. The preceding sections 6 ft & of limestone. abundant fossils just below the Brazzpora lonsym. 200 yds S with 1 turn of Clay Evans, on same road, bluff on east side 1 road, 400yds S of Rolling Fork at Pleasant Valley church. 2 ft internal from forms. Platystegum lyx lonsym. 3ft internal, from forms. Plat lyrx. Rhy. dentatus Teficanna stems & delto lonsym. 3 1/2 ft 10 in fissilifacs internal. 4ft arg., hard layers 4-8 inches thick, with black clay partings, 4 in angles with Brazzpora linepithus; Brazz. cheek.