Field notes, Kentucky (?), circa 1901-1902

K1375 [illegible]

29 29) North of Floyd's Fork. Hays Spring. 2 2/3 ft Clay. Upper Ozgood. 5 1/2 ft Ozgood limestone. 21 ft. Thick Ozgood clay. Some indurated layers at top 1 1/2 ft Transition rock See page 8. 15 in. Salmon brown Clinton. {Fairly hard just below Clinton, 25 ft {Madison -- weathered to thin bedded stuff. (No gasteropod bed at top) 3 ft More like banded Madison. 8 ft. Clay rock spalling in all directions. 2 1/2 ft Soft clay. {2-3 in. Limestone with Strophomena plamumbma Streptelasma rusticum Rhynchothema capax The rocks next mentioned consists chiefly of small limestone rubble. Very little limestone in hard layers. 5 1/2 ft 5 1/2 ft Strophomena plamumbma at base 5 1/2 ft Protasoa retusta common Streplasma planumblma common 11 ft Protasea retusta at top 0 -- Streptelasma rusticum = 6.6 ft below Clinton. 1 ft. Soft dark blue clay. 0 ft Columnaria balli? with conallite separate at top as as to leave separate epithica. 9 ft. Soft clay limestone. Soft clay. Fossils. 31 ft. Fairly solid limestone. With very few fossils 3 in. Coarse coal. pebbles = 3 in. That part of the section below the double line was recorded at locality = 30

2) 29a) South of Floyd's Fork. Immediately S of the Bridge, On Streptelasma rustic road to Mt Washington. Abundant Richmnd fossils in soft rubble clay begin 15 ft higher th an next layer 0 Streptelasma rusticum. 1ft Soft dark blue clay. Columnaria with enalls to separate at top in place and having separate epitheca. 9ft. Soft clayey limestone and soft clay. 31 ft Fairly solid limestone. Practically with out fossils or with very few. 3 in. Crasse cong. pebbles - 3 in. n dim. 12 ft. Solid l. with very few fossils. 12 ft. Softer clay. Clayey than limestone, full of byzograms & Othris Laticesta, var. The large part of the Floyd's Fork section, as far up as the Streptelas. ma rusticum layer, contains a considerable amount of fairly solid limestone. The streple ma planulumma comes in with the soft clay full of rubble limestone, in the Richmond gr.ups, above. 30) 30) 1 3/4 mi. from Floyd's bridge North of Mrs. Mary & Clarke. Upper Ozgood clay 5 ft Ozgood limest. = Lower Laval? 17 ft Lower Ozgood clay 2 ft Bazal Niagara 2 1/2ft Salmon brun Clinton. { 3ft. weathering thin bedded. Massive smith. 20 ft 6 ft. banded Madizian. 11 ft. weathering thin bedded. 3 1/2 ft banded Madizian. 8 ft. Members to thin bedded Madizian. ? 2 ft Harder bed, clayey, spally. thin. 13 1/2 ft. Clayey. Fossils get scarce towards thp 3 1/2 ft Portarea, Streptelasma, Rhynchotrema limest. Capax, Str. planum plumina, small. rubble. Abundant Linn Richmnd fauna. At base Str. planulumina begins to be common. 5 ft. Limest. Rubble. with fossils. Str. planum boma is found 2 ft above base. 2 in. limest. Streptelasma. 3 ft. clay and clayey limest. At base is limest. with Streptelasma Columnaria 22 ft. rubble limest. Fossils common but no Richmnd and fossils are recog- nized. 3 ft clayey. 5 ft 6 in. (Why = 10 ft ?) with Tetradium. 15 ft 9 in. Massive l. with globose Chatelets as at Hurrard's mill. 14 ft. Massive l. interbedded with soft clay. 12 ft soft clay. 2 ft. Clayey limest. full of fossils, byzogo ans, & Othris Laticesta.

31 4) South of Mt Washington, along Whitaker's creek, along Bardest and pike. Salmom brook Clinton. 3 1/2 ft. Hard bedded Madison. 8 ft. { Poor massive Madison above. Sandy clay below owing to weathering 1 1/2 ft full of fossils. 3 in. limestone. 23 1/2 ft Concretinany rubble limestone full of fossils. Calcite! at top = Steph. sulcata + Orthus occidentalis, with scarcely distinct dorsal zinnos. 4 1/2 ft Concretinany rubble limestone, at base with Beatricia undulata + Neterispon- gia at top is Steptolaema rusticum. 12 ft covered, Probably like rock beneath. 41 ft. Massive Madison Limer. Quite massive until near base when it became argillaceous rock. 5 ft. Soft clay rock. 2 ft 8 in. Clayey limestone with Costel- laria perminero? One large Orthus lynx with sub-quadrate form. = The bed at base of Flyods Fork section. 2 ft 6 in. Hard limestone with fossils. 19 1/2 ft. Clay rock limestone full of fossils. One strong Orthus lynx = sub-quadrate form. Hard limestone. Top 4 in. = flat. Below = crossbedded. Beautifully exposed by weathering. Cross bedding due to wave action, forming crescentic sweeps. Waves from the West. Almost 20 ft clay. Shale runs N 40 W. (5) Sweep of Waves from S.W. Photo 5. Clinton. Photo 6,7. Waves 20 ft Waves. a very dark blue sandy layer of lime- stone contains Orthus lynx more ab- brudantly {1/2 ft. More, crossbedded sandy limestone Coarse dark blue limestone with Orthus lynx abundant down to level of creek at Jasper's store, a short distance N. of where the road towards Grinnell's Ford turns off westward. Base of Orthus lynx bed not seen here. 2 ft total Grinnel's Ford to Jasper's store = 4 mi. Saville " " " " = 3/4 " Gar rock " " " " = 2 " Grinnell's Ford to Lick Skillet = S 4 mi. Shepherdsville " " " " = W 3 mi.

6. 200 ft. south of Asa Yates, 1/8 mi. S. of Greenwell's Ford. 4 ft 2 in. Clinton. salmon brown + siliceous, siliceous red on top. 26 ft. banded Madison. 20 ft The upper part grades into the Madison. Only the lower 9 feet fossiliforms, only Lower Richmond fossils seen. 11 ft. At top Stephomena planumbra in clay- ma. Clayey. Steptolaema occurs 2 feet above Coral bed and also in thin blue limestone 2 in. above coral bed. 1 ft. Columnaria halli red. Corals abundant. Tetradrinus varius just beneath. 9 ft covered. Probably soft clay rock. 6 ft. Limestone layers with fossils in clayish between Road turns off W up Yates Hill. 35 ft. Lona Madison, solid, green claygy rock. 1ft 8in. Columnaria halli rather common. 12 ft. Various clayey rocks. 6 ft. Fossiliferous claygy limestone, weathering to clay with Orthus laticosta var. 5 in. Solid blue limeast. with fossils. 9 ft. Fossils above, less common below. 2 ft. Level sandy rock with rough top, varying crossbedded layer, one second level rock on second crossbedded layer with coarse Orthus bynx silicified, Wine Sandy rock with Orthus bynx film. Section ends within 50 feet of Mr. Mont Roby's house. 32 Cont. from page 9. 32 A X=From Greenwell's Ford E 1/2 mi. then up steep hill Cedar glades due to abundant Ozgood clay Ozgood clay purple near base 3 ft 10 in. basal Niagara, in solid 8in. layers. 2 ft. Clinton. Kirby Jones Section = 32 A From X Road Turn S 46 W for 3/4 mi. then S 70 E on gravel road for 1/2 mi. and then down hill along fine section. = good steep section. 5 1/2 ft. solid limestone - Lower Gannel? 2 ft claygy limestone upper Ozgood clay? 18 ft Ozgood clay 5 1/2 ft basal Niagara = thick layers. 1 ft. grey Clinton. With fossils. 25 ft banded Madison. 11 ft brown sandy clay. 2 1/2 ft clay with Steph. planumbra. 3 ft limestone rubble with Steph. sulcata, Rhynch. casea, Portancia retusta, Steph. planumbra, Near top are thin lime- stone layers with Steph. planumbra. 6 ft Steph. planumbra begins at top of rubble limestone 1 in. Thin limestone with Column. alvedata. 2 ft 2 in. rubble stone. 8 in. Steptelaema 6 in. above coral in limestone 1 ft. Coral bed. 15 ft soft 2 ft solid. 11 ft. Part weathered to porous rubble. 38 1/2 ft = Lona Madison, solid rock. 0 ft Rock with Orthus laticosta var. Greenwell's Ford 7 32 32A Section 1/2 mile altitude

8 Clinton with Plectambonites sericea. Plinospira frondosa typical. Orthis (Palmarucella) elegantula. (Strophe). Orthothetes sufflame. - flat but raised at beak. Orthis flabellites Farmites favosus. 21 ft. Ozford clay 8 in. basal ozford, or chert, reddish in mm. siliceous. 2 1/2 ft. Clinton. salmon brown. coarse grained and rough irregular bedded. No chert. Upper 4 inches with whitish stretches. This may be the clerty part southwards. [= N. of Flagde Fork. 29 Cont. from page 1. 30 Cont. from page 3. The basal ozford clay is purplish. All exposed as at Hago Spring. 2 ft. basal Niagara. 3-4 in. of reddish siliceous rock. 21 in. salmon brown, coarse + irregularly bedded. [= 1 mi. N. of Mount Washington) 31 Cont. from page 4. oxford limestone. 20 ft ozford clay. Purple below, indicated above. 44 in. basal ozford Niagara No chert 24 in. Transition red silt with Farmites favosus. 22-48 in. salmon brown typ. Clinton. Halysites Orthothetes with flat valve and raised beak. Orthis flabellites. Plinospira frondosa typ. Doljellum Daytonense, large specimens. Very R rough bedded clinton with sandy patches. 9 32 Cont. from page 6 Lannel S of Asa Lutes brine. 2 ft. clayey 3 1/2 ft. ozford limestone 22 ft ozford clay purple at base. 2 1/2 ft. basal Niagara. light grey clayey rock. 10 in. hard stone. Whitish where not weathered. Traces of chert at top. 15 in. Thin bedded whitish rock. 20 in. granular blue clinton. A few hundred feet N of Asa Lutes brine the Clinton is salmon colored, 20 inches thick, and contains Orthis flabellites.

33 at W.R. Greenwell's house, about 1/4 miles from Greenwells Ford. Ordovician layer 2-3 inches thick. Laurel. 34 Besgod limestone not well exposed feet to top of laurel from next 6 ft harden rock 6 1/2 feet indurated clay rock. 13-15 ft of softer Besgod clay. lower part not well exposed. Whole = Besgod clay section. 2 ft rotten limestone with traces of chert in lower part = called Clinton southward. 4 ft. Granular grained Clinton, chiefly blue, but a portion 6 in. from the top is salmon tinged in places. Contains Halysites, Orthus l'frnata and Orthus flabellites, at all levels in case of last two species. End of section at Jess Ruby's house. 34 Cedar creek 1/2 mi. beyond Ted Weller. Besgod clay. lower part = 18 1/2 ft. beautifully banded with red purple and greenish brown. Brasal Niagara not measured. 6 ft. Clinton, probably not the total section. Chert 2 ft from top. Indurated clay above the Clinton. thickness unknown. Exposed for 1/3 mi. in creek, along the road 35 Weller's house. About 1 mi. N of skillet. Coniferous. very white. No fossils. about 20 ft. above the (Louisville?) Waldron shale. 36 About 3 mi. from Shepherdsville, along the creek below Lick Skillet. Weller's Run? Bulls Run at Mt. Washington Road. Waldron shale 3 in. Ordovician rock. Laurel. base not seen but thick section exposed along creek. 37 One and a half mile from Shepherdsville on road to Cedar Grove Church. Black shale Crinoidal Coniferous. Thick exp. of Louisville Pentacrinus elongus in loose blocks beside the road.

38 Cane Springs store, 10 full miles to Shepherdsville, SE of store. 1/2 mile Clay layer 5 1/2 ft. Ozgood limestone. 5 ft. indurated clay, calcareous. 17 ft Ozgood clay, brown above, blue middle, purple below. 2 ft. basal Ozgood. pnn. 5 3/4 ft. Clinton with cherty layers. 6 in. & gradual bluish Clinton. Photos 6 (200ft) 7-150, 8-40 ft, 9-10 feet off from Ozgood clay exposure. 39 Along boundary creek, E of Cane Spg. Stat. 3/4 mile east of station. Black shale, Corniferous, coarsely crinoidal. Thickness unknown. 3-5 ft Louisville varies from 3 - 5 feet in thickness at different points. 9 ft. Waldron shale 1 ft. Oolitic. Laurel not measured. Ozgood clay not measured Ozgood limestone " " 23 1/2 Ozgood clay sample below, exposed in a little gully on E side of creek N of horse with distillery &. 4 ft Basal Ozgood limestone decaying crumbling stuff 12 13 Clinton. top of clert is 1 foot belaw top of Clinton. In lime layer 7 feet belaw top of Clinton ocur: nom forams on top of l. layer. Clathropsa frondosa. Phacops na multi fida with less numerous branches. Orcithis flabellites Dalyuanella elegantula. Plectommites transversalis Strephomella patentia with outer margin not turned up. About 7-9 feet belaw top of Clinton & for 2 feet above fossil layer the rock contains Calcite masses. The cherty layers begin higher up. On a former visit the following Clinton notes were secured: Orcithis flabellites is common 6 ft 8 in. below Ozgood clay base, in siliceous bluish rock. Orcithis flabellites common also 7 ft 2 in. below Ozgood clay in crinoidal blue rock. What clert is 2 feet below Ozgood clay base and it contains Foraminiferous, Orthis flabellites, Orthothetes flat with raised beak. Where road leaves creek and turns W. to Cane Spring store, the crinoid Clinton is 8-9 in. thick. 13-17 Madison section. Only lower 4-5 ft are Calp bounded. The very fossiliferous Richwood begins 12 ft down.

14. 39 A. E of William McBurdor's house, at End of glen or valley, entering boun- dary creek. 2\/2 mi. from Carson Springs Sta. Clinton. ->9 ft below Clinton is highest Spange. 18ft sandy decayed Madison. Mst Spanges are found now at the top of the fossiliferous expo- sure. If the base of the banded Madison is 15 feet below the Clinton, thetopofthebandedMadisionis probably still beneath the spange layer. The thickness of the richly fossilif- ous Richmond section was not measured. It equals about 5 feet as near as I can remember. One stray Columnaria was found, pre- sumably C. abecata but no record was made. Further along the track Columnaria halli occurs 17 feet below top of richly fossil. Richmond section. 9feetCornith on theC.halli layer where C. halli occurs in association with Tetradinium minimus, Platano 23 B Samuels. 9ft{1/2clayinsoil. 71/2 ft. massive with Calcites of Clinton. 5ft weathering to clay. 1/2 ft. thin limestone. 4 ft Madison like rock. 40 At bridge 5, E. of Hobbs. 1mi. N. of Carson Spgs. E.ofbridge. Black Shale coarsely crinoid Corniferous. 2 feet seen. 11/2 ft. Louisville 18 feet = 2nd measuremen {TopofWaldronaboutinRRlevel. about 7 feet of Waldron shale. oolitic top of Laurel with orthoethes subplanus Spirifer endora Multifieldella nitida. W.ofbridge.16ftLouisville.forsmdol.l. TopofWaldronis4feetbelowRR level. In Waldron = Rhyn. concata. spiriferendona.sp.radiata.Orthophyllum. 41 At bridge 4, east of Hobbs, the middle of Waldron is at track level. 42 Small Pentana. olivigerous in Louisville, 5 ft above railroad Hobbs station. BaseofWaldronis5ftaboveRR. oolitic layer{Topaboutmidwayatupretail 35ft Laurel down to shale in Laurel. See Burdston section. The exposed out 18mi. Blue clay shale 3 fossils in white lay Limestone = Lower Laurel? 2ft seen. Therore Halich. Dizza of well. Chapelze Station. Bullitt Cr. Chapelze In Waldron shale - Rhynch. concata, Spirif. endora, Spirifer radiola, Orthophyllum.

Clermont. Photo 1 Walsdr. 2 Walsdr + Lane. 3 Walsdr. 45 ft Lorriville 33 ft above base occur Pectum oblongus. A species of Holoptychites with club like form and grooved top was col- lected at each end of quarries, one mi. E of station. 9 ft Walsdr shale, with Atrypa retic- ularis. 1 face = 12 ft above RR track. 6 in. oolitic. In places 12 in. thick. Laurel limestone. Upon 20 ft quarried. Quarries extend about 1 mi. from Clermont E to Hoffs station. 18 ft below top occur Calymene Waigeneri, crenm., and Orthoceras angens but larger, No longitudinal striations as in O. annulatum. Laurel rock used for 1. 14th St bridge. Louisville except 2 pieces Indiana side which came from Utica 2. Crescent Hill Reservoir. 3. Most equal walls at Louisville. Locks made from Bedford rock. 4. Near all L + N bridge work in Ky. 5. Curling in Louisville. Good deal. 6. Baptist church. Bardstown. Quarried April in 1862. Belong to L + N. R.R. 43 44 Just south of school & church at 14 mile post from Bardstown on Mt Washington road. Columnaria halli on road side. Farther down hill side on WJ road is whitish limestone with Gyra Silurica Orthus occi- dentalis + Orthus lafnata 45 An eighth of a mi. S of 44, just S of Steve Loyds house. Columnaria halli abundant on road side = highest point between Salt River & High Grave. 46 Road angle at Same Wells house = 11 1/2 mi. N of Bardstown. Columnaria halli: Road remains at about same level for long dis- tance S. 47 Mrs. Ber. Abell, 8 1/2 mi. N of Bards town. Thin bedded Lime Silurian a considerable distance below the Clinton. In fact very far below. If any Clinton occurs N of Bards town it is believed to occur not further North than 3 miles of town No exposures of Clinton occur any where near the pike.

18 48 E side of Bardstown. ? 47ft 8 ft. isolated patches of limestone at E edge of town 25 ft. continuous exposure Upper Laurel 1 ft blue clay 11 feet limestone Lower Laurel. 2 ft weathering to soft blue clay. 1 ft 8 in. limestone, very good. 41ft 36 ft clay shale, purple below. 2-3 ft light brown, arenaceous lime- stone breaking up into pieces 4-6 in. square. Of the basal Niagara forming the rock last mentioned, the upper foot con-sists of fairly good limestone while the lower foot weathers soft Clinton See also page 21. S. of bridge. 1 ft l. not cherty. Highest cherty layer with Orth. Steter subplanus 13 ft Lower cherty layer with fossils on next page = A 7ft 5 in. l. arenaceous, with calcito in lower third. Ordovician See page 20. Further S. 800 ft. 1 ft not cherty, Highest cherty bed - 8ft 9 in. Current cherty bed 12 ft brown-ish arenaceous rock with calcite throughout entire thickness 19 Clinton Fossils A. Clinton just S of bridge. 13 feet below top in cherty layer. Calymene Togderi large head + large pygidium. Gonoceras very small, pygidium as large or smaller than in G. Therseri but = punctatus partly. Illaeus Dauglensis pygidium. Cyclonia Clinton var. with raised revolving striae very distinct but not so strong as in C. variocana. ? Spirifer like Niagaraensis, small. Artus flabellites, Dalmanella elegantula Platystrophia 2 plications in sinus. Both small + large form. Streplecama Hanoverensis also interior of ventral valve. Is this Sto. patenta? Plectambites elegantula small. Plectambites transversalis. large. Rynchomella scobina. Hemitrypa Ulrichi Palaeodictya bifurcata. Rhindsorka fundosa. Photo 4. White streak at base = Lower cherty layer, to top of highest cherty Clinton. Photo 5. Near view of cherty Clinton.

Ordovician. 29 ft. 1 ft thin bedded Tetradium. 7 ft clayey limestone. 10 ft soft clay. No fossils. " limestone full of fossils. Top 4' fossiferous section = 11 feet above coral bed. Coral bed. Columnaria alvedata Calpescia criciformis. Ordovician fossils. - Pleurostoma capax rare. - Platystrophia acutiliata. - Diexetis subquadrata - Streph rugosa = vetusta? - Rafinesquina alternata large. Alev form very flat = fracta. - Platystrophia bifurcata - Streptelasma recticium. - Perarea vetusta. - Hygropiza urdista - Strephomena ancata, small form. Fine interwin as at Dayton. - Byssorhchia radiata. Siphonspira, small acute Siphonspia turpicus plena. - Hebutella occidentalis. Clint m. S. of bridge. 13 feet from top of cherty layer to lowest cherty layer. 2 ft 8 in. {13 in total me of quarried clints} bbed 12 in. layer of l. limestone 7 in. layer of l. limestone {4 3/4 ft massive rock with calcite 5ft6in trumps, especially in lower half. 9 in. with numerous worm borings at top. Thin banded. Clayey rock, soft, Tetradium.

22 49 See page 25 At Withrow's Run, 1 mi. W. of Bardstown. East side of Creek. 2/3 ft. basal Niagara 1/2 ft. weathering clay. 12 3/4 ft. Thin bedded Clinton. 11 ft. Thick bedded massive arenaceous with calcite. 2/3 ft. Thin bedded layer 5 ft. Weathering soft. 5 1/2 ft. Banded Madison, greenish + red from. 8 ft 9 in. Clay rock hard above soft below. 1 inch. Thin bedded l. with Stephomeria plenty. 5 ft. blue clay rock + limest. with fossils 1 ft. coral bed. Columnaria abbrevata 20 ft. down to creek level. About 5 feet below top coral bed is Palaeophyllum divaricatus + Portarea retusa = About on level with lower coral bed? Photo 10. 3 years more broken by sheets. 50 [illegible] See page 26 West side of Withrow's Creek, W. of Bardstown. Photo 11. Bottom projecting layer is thin bedded layer at top of Ordovician. The top distinct layer is base of well bedded Clinton. Photo 2,3,4. of second set. Junction of arenaceous Clinton in base and soft top of Lower Silurian. The thin bedded layer is between. 51 23 Buffalo creek 3 mi. W. of Bardstown. {2 ft. weathering soft, especially Coralrag 8 ft 4 in. Thin bedded Clinton. 10 ft. Massive Clinton. 5 in. Thin bedded. -1 1/2 ft. clay rock spalling. weathering soft. 6 ft. Banded Madison. 6 1/2 ft. looks like Greenish Madison. Not banded. Weathering soft. 52 East side of creek. West of Cedar Creek, 5 mi. W. of Bardstown. ? {8 in. oolitic layer 10 feet poor exposure. 34 1/2 feet continuous Laurel exposure 2 ft. clay layer in the Laurel 9 1/2 ft. limestone rotten below. 25 ft. Ozark clay. 6 ft Basal Ozark + top of Clinton. 5 ft. thin bedded Clinton intact chest. 6 ft massive with calcite. 2 ft softer rock. Is this Ordovician? It weather more readily than underlying part but breaks up brownish like rock above. I am not certain whether the Laurel exceeds 35 feet in that part of the section overlying the Laurel clay. The section appears thick but this may be due to a considerable westward dip of the rock.

24 61 Near mouth of Cedar Creek W. of Bardstown. Black Slate 8 ft. Coniferous Upper Laurel, not measured Clay not exposed. 5 1/2 ft of limestone as at this Cedar creek exposure. 25 ft Oz good clay on S side of creek [30 ft Oz good clay m N side of creek] = 27 1/2 ft on average 1 1/2 ft. limestone, solid here, lime half weathers elsewhere. 2 ft with chert. 5 1/2 ft thin bedded 14 ft with calcite Ordland. 5 ft indurated clay above, Ordovician. 2ft 6in. Madison rock, 10 1/2 ft. Clayey 1/2 ft. One Cd. alveolata. 5 ft. Fossils in clay rock. 1ft. Coral bed. Tetradium. Cd. halli. 7 1/2 ft down to creek. 49 Cont. from p. 22) 25 (Observed Later than map 22) Written via Rm. W. of Bardstown. 1 1/2 mi. 36 ft. Oz good clay. 13ft 8in. Regular bedded Clint not fossil Mg. 11ft 8in. Massive Ordland rock. {1 ft thin bedded top of Madison. 5 ft 2 in. Softer Madison 6 ft hard Madison 2ft 6in. Rock like above but softer. 3 1/2 ft. Clayey rock weathered to soft stuff 4 in. Fossils in clay rock. 1 in Thin limestone full of good Streph. plummuloma (= vetusta) 3ft 9 in. Clayey rock with fossils 1ft 5 in. Clay rock with fossils. At top is lowest thin fossiliferous hard thin limestone. 3ft. soft clay rock. At very top are almost Protocera and Str. plummuloma 3 ft Great Coral bed, chiefly in middle 2 feet. Calporecia cribiformis rather common at one point. Largest cribiformis = 8 in. Columnaria alveolata. Streptelasma rusticum. (2ft. A strong Columnaria alveolata at top of clay rock. 7 in. Hard blue limestone. Horizon marker. 11 in. Clay rock. 9 in. Clay rock. Streptelasma. 4in. Clay rock. One Cd. alveolata. 3 ft 2 in. Clay rock. One Streptelasma 8 1/2 ft. Covered, probably soft clay shard 3 ft. Clay rock. Some Madison land top. 0 Creek bed. Lower Madison.

26 at 30 Times Distillery, at RR crossing. Waldron, only 4 ft exposed. 8 in. Top of Laurel limestone oolitic R Corniferous chert with small Ambrevelia abundant. 7 1/2 ft. Louisville. 9 1/2 ft. Waldron 8 in. Oolitic Laurel. S Oolitic top of Laurel. 71 Cut E of Goshurg or 1 foot limest, lower half weathering soft. 10 ft. more white & bedded well. 8 ft. Massive Botland, with calcite. 10 in thin bedded layer. 4 ft clay, soft at top and bottom. 8 ft. Madison bed. 18 ft soft greenish clays rock. 1 ft. Coral bed, Columnaria alvedata Electr. 12. Cut. Well bedded Clinton begins above the middle. 73 1/4 mi. NW of Botland. Lower Laurel (bular clay) at top of hill. 72 West of Needmore, in Cane Run, NW of Botland. Above bridge down to below bridge. 45 feet Ozgood clay, S of bridge. Thick section probably due to cliff of rock towards north here. 1 ft limestone weathering below. 16 1/2 ft. whiter & better bedded. 6 ft. Massive, Lower 6 in. thin bedded but not distinct from the rest. 1 ft. clay rock. 1 ft. soft clay. 5 ft. Greenwich clay rock with Tetradi- nus at all levels. Madison bed. 72B Stewart creek E of Bardstown. Fine exposure of Laurel clay Lower Laurel Ozgood clay Clinton well bedded and Botland bed 72A Cove creek entering Mill creek in B. pike. Botland bed. 1 ft Thin bedded top of Madison. 7 ft. White clay rock full of Tetradius. Heavy Massive Madison. 22 ft Hard blue clay at top of coralliferous Rich- mond, contains distinct trigas. Rubble limestone and clay. Great coral bed.

28 97 A N.W. of Fredericksburg, from Chester Cecili house, at bend of road, to trip of drill at farthest end of ascent by Bardstown pike. Ostracoderm bed with abundant Star- murt spenid grnthos. Massive. 24 ft covered 2 ft Massive coral bed. 20 ft {white rubble limestone. unknown. 17 ft Madison soft clayey 4 ft. Massive Madison 14 1/2 ft covered 15 ft. Thin bedded clayey limeate above Irregularly bedded clay rock belw. 9 ft. Thin bedded clayey limestone Beatrice 2 ft 4 in. Massive limestone. 8 ft 2 in. Limestone & Clay with some fossils. 0 Orthis lynx typical, abundant. 21 ft. Orthis lynx and Ambl. Casei in blue l. rubble. Lynx bed appar- ently not thicker than 30 ft. Expe- cure two interruptions below for study. 86 ft Not well exposed along pike, but the lower 30 ft. fossils for us on hill side on W. side of pike. Strphomena plana convexa. at base of section. 29 1/4 mi. N. of Balltown. Corniferous. Lawell. Considerable thickness. 74 1/2 mi. S.W. of Balltown. Tip of Lannel not seen. 22 ft {Lanrel { Good limestone. 27 1/2 ft. Ozgood clay, Dip 5 in crease. 23 ft measured vertically! Lama 6 1/2 feet = massive. 2 mi. Trace of thin bedded layers. 5 1/2 feet partly bed below, weathering soft. 6 feet rather massive. Madison? 13 feet weathering soft with Orthis and fossils near the middle. 1 foot. Coral bed. Colummaria alveo- lata. 2 mi. N. of Abbey La Trappe m Balltown road. 21 in. Coarsely crinoidal Corniferous. Lannel not oolitic at top. Photo 5. 1mi. N. of Abbey of La Trappe.

30 V Meet of La Trappe. Black shale. 11-16 ft. limestone felar. More thin and claye also. Upper Lannel. 7\frac{1}{2} ft. Limestone. Lower Lannel. { 2 ft soft clay. upper Osgood clay. 1\frac{1}{2} ft. fern clay limost. in attaining to rubble. } 31 ft. soft clay. Osgood. Clinton - trip. 88. Half a mile (= \frac{5}{4} mi ?) N of New Hope. Black shale. 8 in. thin crinoid. Coniferous. 5 ft. Lannel l. (= Osgood limestone ?) 35 ft Osgood clay 11\frac{1}{2} ft. cherty Clinton. 2 in. chert bed. distinct. 4 ft. massive, with calcite. 4 in. soft clay. with lone Tetradium. 2 feet forming whitish limestone where Tetradium is common 3 feet 8 in. blue clay rock. 89 Tilford Station. Distillery N of New Hope. 4 ft. Coniferous. Crinoidal, cherty. Plenty of chert. 1\frac{1}{2} ft. brown sandy {conglomeratic above with rock very small pebbles, Fish teeth and other fish remains in lower 1 foot. 5\frac{1}{2} ft. clay limestone. No chert. Osgood? 19\frac{1}{2} ft Cherty cherty at middle + trip Massive at base, with calcite { Soft blue clay } 23 ft. {Madison like rock not well expressed. Great Coral bed. Columnaria alver-lata. 90 Willow Spring Distillery. Between Cone Holler & Tilford Station. For upper 5\frac{1}{2} feet see section above. 12 feet to top of very cherty layer. 2 in. good chert bed. 7 ft 4 in. Massive Clinton with calcite. 6 in. Largely. 2 ft 3 in. Tetradium abound ant but not as common as at New Hope. 5 ft. Harder Madison bed. Softer Madison bed.

32. 109 E. of D cut. 5 ft 3 in. Corniferous. 1mra 2½ feet very crinoidal. 5 ft soft Ozgood clay, Clintm massive looking, with calcite in upper 2 feet. Top chert layer is found 2 feet below top of Clintm. The massive appearance probably due to absence of weathering since the exposure in the cut is quite fresh. A E West of Chicago. Impossible to determine just how much Clinton was preserved. The following observations are the result of careful measurements. Black Shale 1 foot brown rock Corniferous 6 in. crinoidal rock 15 feet Clintm. Lower 5 feet = massive 8 in. thin bedded. 2 ft with Tetradinn. 4 ft. Madison bed but here it is weathered so as to be very soft. 6 ft. weathering softer than bed above. 8 ft. hard at top, softer below. 2 ft. Coral bed. Columnaria halli; B F 33. Chicago. West of distillery in N.W. part of Turn. Black shale. 2½ft Corniferous 6 in. brown rock {2 ft. crinoidal 15 ft Clintm Thin bedded 110 West of Loretto. Black slate. cornif 6 in. brown rock with cross larrons. orus 3 in. not exposed. 17½ ft Clintm. Soft clayey rock. 105. North of Loretto. Black slate. Corniferous. {2ft 3 in. of brown rock ? with volute burrows at top 9 in. white the crinoidal b. weathered away in places. 3 ft 3 in. regular bedded, contain ing calcite + 2 rare chert. 7 feet. Massive Clintm. with calcite, 6 feet 9 in. soft clayey at top Madism bed, top.

34. 113 A Lang Smith, 1/2 mi. SE of Chicago, in St. Margt road. 5 ft. Clinton. Massive basal part + calcite 1 ft thin bedded layer, 5 ft. clayey rock, like Mad. below, but softer. 5 1/2 ft. Madison, slightly harder than above. 12 ft. After Rock. 1 ft. Great Coal bed, in places forming a hard b. bed. Columaria halli. Streptelasma rusticum + other Richmond fossils. 16 1/2 ft) Below coal bed just described are various thin blue limestone beds with Labeckia diversis + Calospe cia cribriformis. One thier with Leperditia calcigena. The levels at which these beds occur have not been recorded 1 1/2 ft. Dense blue l. with Leperditia caecigena, small garterpods and Labeckia diversis. 40 feet of Lower Madison. Base not seen here. The Orthus lynx bed should occur about 27 feet lower down. 114 35 W. D. Miles. Black slate. 5 ft. Clinton. E of house is Clinton, chert on the road side. The 5 feet of Clinton are found 400 ft S of his house, in S. side of creek crossing. 4 feet of clay rock, spalling, On the lower part occurs Tetradium Where Tetradium is common the rock becomes hard as at New Hope. 2 ft. poorly exposed. 1 ft hard rock. 4 ft poorly exposed. 4 ft hard clay rock.

36 124 NE corner of Raywile, where road to Chicago turns down hill and crosses the creek. 1901. Black Shale. 5 ft criminal Devonian? 8 ft Clinton. Lowest layer with calcite, but no chert. Contains Neliites, Dactylocietya, calycula. 7 ft soft clayey Northward, but an indurated clay rock Southwards. 3 ft 4 in. hard clay rock with calcite chert 8 ft 9 in. clay rock. spalling. 2 ft harder clay rock. 6 1/2 ft. soft clayey with thin limestone beds in lower half, containing Richmond fossils. 1 ft. Coral bed. Cor. alve data. halli. Calopocia, Tetradinum. There are fossils for 7 feet below this Coral bed. Here there is a 3 inch limestone layer with fossils = collected. 37 Later observation 1902. 7 ft. Bedded cherty Clinton. 7 ft massive crystals of calcite. Botland. 10 1/2 ft. Clay rock. spalling. No fossils. 3 ft. massive clay. 4 ft 9 in. chiefly clayey with thin limestone containing Richmond fossils 1 ft above bed 4 in close bedded blue l. with Richmond fossils. 2 ft 6 in. some fossiliferous clay rock. 0 Coral bed. Columnarijena halli, Calopocia cribiformis. Streptelasma. 4 ft. fossilifero clay, blue. ver Richmond fossils.

38 E of Raywick. 126 Black shale 5½ ft. Dervian k. crinoidal, 3½ ft Ozgard clay. 6 ft 8 in. cherty, well bedded Clintm. 10 ½ ft. More massive. Botland. 9½ ft. Clay rock. Spalling much. No fossils, 3 ft. More massive clay rock. 5½ ft. Soft the clay rock. Perforated Col. halli. 1½ ft. Coral bed. Tetradimm. Col. halli. Calycrécia criniformis, Labechea smooth, 11 ft. the clay rock. Same corals. 2 ft. Great coral bed, Cyl. halli. Cal. criniformis = common. Smooth Beatriæa, as NWY Frederictown Tetradimm. 3½ ft. Blue clays limestone rubble. 2 ft. Massive blue lead limestone. 125 A. E end of Raywick & of spike. 5 ft Coniferous. 8 ft crown 7½ ft Clinton (cherty ?) 125 About 500 feet east of last, at turn of road. Ozgard clay. 6 ft Clinton, w/ th. chert near base, over clay rock with calcite - Botland? will a 4 inch layer of clay separating the Clinton and Botland. 127 39 W. of W.M. Van Cleves store. 1 mi. E of Raywick Coniferous. 6 ft not expnd. clayey. 6 ft. 9 in. Clintm, cherty. 3 ft. hard brine rock with calcite. 5 ft clay rock, chiefly soft. 2 ft hard clay rock with calcite. 10 ft clay rock, no fossils 0 Corbinaria oblongata, Poor bed. Coral difficult to recognize. 7½ ft. Green soft clay rock. 1½ ft. Great coral bed. Col. halli. 11½ ft. (Upper half full of Richen and fossils at NE corner of Raywick ?) clays 1½ ft. Coral bed, thick in corals. Col. halli. 2 ft soft. 2 ft Very hard the limestone with int fossils, seen at Chicago. Belmo is bedded clayey limestone rock = Inner Madison. Photo b. School house 3 mi. E of Ray- wick.

124 Raynick. Richmond fossils. Nebertella sinnata - cmm Strophomena sulcata 3 specimens Rhynchotrema capax 1 Stipetasma rectum 1 Beatrice undulatum 2 Platystrophia top form C Protrea vetusta 1 Byssmychia radiata 4 Heterospongia subarosa 2 39 A Cane Springs. Richmond fossils. Strophomena retusta? ccc Rafinesquina like pacta 1 Lophospira Trapidaphra ccc Lophaspira perangularata, Var. cc Stipetasma rectum 3 Rhynchotrema capax 3 zygospira modesta 3 Nebertella sinnata C Protrea vetusta 1 Platystrophia top form C Tridinum fibratum 1 Platystrophia acutilicata 1 " half way to " several. nt Washngtn Ky. Beatrice undulata. Madison Ind. Heterospongia aspera. Large faverdu- lar. Corroreville, Ind. Beatrice undulata. Bellerophon gibbatum Richmond Ind. Beatrice undulata. 48 Bardstown. Rafinesquina alternata pacta 8 Strophomena retusta - c Rhynchotrema capax - C Strophomena sulcata - 3 Dimuthus subquadrate 1 Platystrophia acutilicata 1 " half way to " " " C zygospira modesta c Stipetasma rectum 5 Protrea vetusta 1 Byssmychia radiata 1 Lophospira trispiphora C Lophaspira perangularata acuminata) C but not so acute SE of Lebanon. Wudd, beyond Sulphur Spg. Beatrice undulisa 1 Beatrice undulata 1 Platystrophia laticata? c Nebertella sinnata 1 Heterospongia Kurtti 3+1. Lophaspira aurpla C Lophaspia Bardeni c Near town. Lebanon. Orthis lynx c Platystrophia laticata c Nebertella sinnata Lophaspia burdeni Heterospongia Kurtti - 4

{ "text": "Stramatopora subcylindrica.\n\nVol. 7, p. 20.\n\nThe form of this species is an oval-cylindrical tube, somewhat compressed, filled centrally with the core, with clay. Prominent conical elevations vary in height from 1-10th to 1-20th of an inch in size, distributed irregularly over the surface. Radiating lines, more or less conspicuous, crossing the apices and slopes of the prominences, giving some of them a stellate appearance. On the general surface are shown distinct circular or elongate spirilla, about 1/20 of an inch apart and less numerous. The oscula in any face parts of any kind observed.\n\nA microscopic section shows an irregular porous structure of the interior of the body.\n\nThe specimen used for the description is 2½ in the long, slightly arched in one side and nearly straight in the opposite side; 3/4ths of an inch widest in diameter at one end; 1-10th of an inch in thickness over 1 inch in the middle, and 1/8 an inch at the other end; 1/2th 1 an inch in this channel from the inner surface to the bulb-like foot. How much larger the specimen may have been is not known, as both ends have a fractured appearance.\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n [TRANSCRIPTION_TRUNCATED_DUE_TO_LOOP]

Ottawa Naturalist. I, Mr. Drummer Labiidae Hurricane Billings. Labeo via. Stamp on hurricane types in Mus. of Geol Surv. of Canada. From Cape Smythe, Lake Umm. Collected by Dr. R Bell in 1859 (Not by Fund) Pl. VII p 1/2 Fords paper - Labeo via or Tetra albin phalatus - in custody Fig 1a & Fords paper = small part of large number Labeo via. 5 1/2 in. arms, - In arms. Either are thus: J Billings, Dr McAdam states that Cape Smythe material is better preserved than that of any other lake.

[illegible] Mr Cake Grinabdean Linote Glytstocino frinkito, Shunna [illegible], p. 110?, 154, 194, 219. QuX 73, p. 263 Itcorrcinno feckruno Skinnera [illegible] p. 110?; 154, 219 QuX 73, p. 263 Cunndo, central undetermined genus + specios. Glytstrinum. 2 undescribd species QuX 73, p. 263. Ocalocater? [illegible] Galacator? QuX II, p. 110, 219 Dantaster ? [illegible], p. 154 QuX 73, p. 263.

Capo & inaudax limes\n10. Tentaculites incarnino, Shumard\nRept I+II. p. 110, 154, 195, 218, Rept '73. p. 263.\nTentaculites major. Nho. name, partly\nfor the next species. (Rept'73. p. 263.\n*Tentaculites tenuistriatus M + W:\nVd III. p. 341. Cites from Cincinnati\nGrimp Alex. Cr. 900.\nAnricula, n. sp. Rept I+II. p\n*Pterinea rhodezensis, M + W:\nVd. III. p. 354. Cites from Troy N.P.\nS'humard, Alex. Cr. 902.\nOsterus. 2 or 3 sp.\nRept II. p. 154\nCathysa\n*Septacrina suezacosta,' Shumard\nRepto I+II. p 110 ?, 154 ?, 205, 219.\nRept '73. p. 264\n*Tentacrinus n. sp.\nRept II. p. 219\nGuthria 21/22 centenario, Shumard,\nRepto I+II. p. 110 ?, 154 ?, 205, 219.\nRept '73. p. 264.\n*stroptolychnium subplenum,\nVd II. Cites from Cincinnati et\nTentacrina. Cr. 902. p. 349.\n*Carcinella O.'kingiana, M + W:\nVd III. p. 352. Thin. large bed y\nquy L'incotium, Alex. Cr. 902.\n*Maisnella\nVd. III. p. 354. Figured in plate C.\nNot received.\nDunacrinus, 2 or 3 sp.\nRept II. p. 219.\n*Cyrtolito incrucato. M + W:\nVd III. Cites from Cincinnati &o. Alex.\nC O. p. 27. 340. Tentacrinus 2 or 3 sp.\nVd II. p. 219\nOleucocrinaria\nVd I + II. p. 154, 219.\nOleucocrinaria\n*Cyrtosmena\nVd III. plate. Figured for not described.

Mr. Lake & Iiandeau limestone. Cypbaekio Girardeaensis, Steward. Rept I+II. p.110, 154, 197, Rept'73 p.263 Vet. III. Selinao Alex.en. p.27. Guecinunuo delfordeno, Steward. Rept II. p.154, 198, 219, Rept'73 p.263 Acidaleio Haeii, Steward. Rept I+II. p.110, 154, 200, 219, Rept'73p263 acidical, Proetno deprecato, Steward, Nt de- Rept's I+II. p.110, 154, 219, Rept'73 p.263 Cheiurus Rept II. p.154, 219, Oaophus Rept's I+II. p.110. Can this have been the importanca of true Triite. I found ur Oaaphus and it seems out of place in our Upper Silurian fauna. Seel. he associated in same bed in St. Cyphacteo, Acidaleio & Proetno canad. one, Alex p., 219, x Oaophus canadica, Canada Vot. III. Selinao. Alexander C.p. 27. This species was described by Canada from the Chagy & New York. x Admanites (neke + Wetlka) D. dancse. Vet. III. p. 2 ani, above Daleo. in Stuart part of Weyer's Siluria.

O'neill delevano, Shimnand, 1855=71 Wno. manue. Cited from Cole. G'aradewm b'isud', Cylindri? S'irac'deum'sh'man'x. Cista frim W'p'lar S'id, = Costa G'ar., decor'da'ta'wstif'. 2 un', alba Costa S. 'var'dewm. G'bypr'stinne f'in'liato. N'z dete'rminab'le. 1855. According to W. + Sp. Cist. frim Costa G'aradewm b. frutx- dy 2 un': alba Cista G'zar'wckwm. C'lw'nar'a'ma in a'p'g'dio. H'pale: '52 frum ca'c'rim in mo'st no Cista di Sh'mmard '57 tr 9' frum N'x- gao y Cista S'in'do can Cr. 1 un' at ao & h'p b'u'ds f'on ary. Te'ta'sad'to in 'sw'mno. Sh'mmard: '57 2 un': alba Cista G'zar'dewm. Te'ta'sad'to in'aq'. S'h'mmard= Wno. ma'rie- in a'sue b'stadt. hton-ni'nico flo'rwmo. Sh'mmaw '57 in 2 cwo 'lrcdty, Wno. Gut liu 'W'ta'm'wntae'. S'h'mma'd, '55. Cist frum 2 un'. alba Cista G'r.ar'dewm. S'p'alatae n'a'vicita & knu'ead: '57 = O'lfinor'yinua aec to Sh'mckl, Cisted from Costa G'zar'dewm L. W'ur'd'ciaria 'wra'jia, H'ale', Cited frum caleno 'li'n'est su in W'sc'cri'a. Rep: IV Re'ept'me'to Queni'. Halle, Cited as charac- teristic y du G'aldem L. Mac'linrea ma'gna', do Sareen, is a Char' specim frim N'w. Yrk. 'm'v'i'tia'da di- C'or'ib'd M'. cano'da + a'nif'r'undata from the G'aldea y W'scen'ria. Tr'a'd'ci'mea 'n'ch'b'ic'c'inum. Halle is given a name frim the clergy to the Indian w Rivers Br'axpin N.y. Sud'w'to d'l angusto in cited frum Ar Que' to & A'y. St'a'di'sticia 'l'en'tic'ulae is cited frum the Duarte to the Hudson River Ga. 'Mand'e'aria g'racili. Halle is given at Inaust y la Hueren R'ioin Ga. 'Mand'earia con'v'in'sera, Sh'mmard, Cisted frum the Duarte at Glenc', S+ Years Cr. W'y.

i Callistemo Ranifel. Renna, 1860 Niagara Wright & Decatur Co., Tills in Main, Wno. B Nelsan: Bancalupt. Neri / R Ruma. 8acc comme Tomascenero. Place = 1875 S. spezzino Ornea, Niagara Decatur & Camp Co, + 9old in Sp. Oler. Manchipiturnio Tomascenero. Brean 1866. N'as Doc + Wmpceca. Tyllo in Main, Wno. Bvolcar & smg Ucsurp'corino zidatio w + sp u. Sp. Niagara Gr. Decatur in The w + Sp. Ccl. Lacc'ch'urno Laccia. Renna, N'as Gen Co. Tarn. Wno: Bruno: Ruccia, 1852 Sinotopora florvora (Hall) Noted by Shuman at 1 mi., above Sheffield's Landing. Lake Niagara, 10 miles from Niagara. Shutepora Mississinewic) Neck + Matha b'irardom Cr. 1868. Noted from Greenfield, near Barkley's Landing. Oddy Co. Chisino Wual coniferio. Cited from the Niagara L. 1 mi. above Shefields Landing, h Shumard. Wno. Noms. 55-71. Coda Girardean Cr. Bucchinano fructatio, Medlening '21, Cited h Shumard from Niagara at 1 mi. above Shefields Land. Coda Bucchinano de'cir'deaa. Shumard, 1855. Cited from Coda Girardean L'inostem, about 2 mi. above Coda Girardean. Cobuscera nigra, Shumard, 1855. Cita gregaroid fruct. flor. Nela. at 1 mi. below Stremingham, but in '55-71 other from Niagara 1 mi. above Sht- nich Landings. Coda Girardean Cr. {Calyptrae allied to C. recorta), 9 ur dalacerpo (2 species) Niagara L. {Calymperes (2 species) /m. other ssp. 55 Noted from near Niagara, 2 mi. above Floto. Shumard, 1855. Cit O'v'scarpio Hott. Shumard, 1855. Cit in Coda Girardean L'inostem. in cota Girardean Cr. Tm.-2. No.

i 2 distretto Tennessee' Northen 1890. Cefzon. Waugue Co. Tenn. A-n- gorag'n. Tyle in 90 State Cir. Springfield. Sampferdettino Terremporesse's, Dec- aer. 1860. Decaton + Waguo Co. Miller. Mnn. D'nean. Molochinno n'foll'i'mo. H all. Caffamouth aldo in N'nega - an g wosteln Tenn. W+Sp Molochinno ch'cignro. W + Sp. 21.Sp. N'a'gana Gn. N'boar st un'enne'sb + St. Cane Jnd. Tyleo in Cell. q Rugalded by Deuce in 'Ilerria with his Ca'terino Molochinno Decezon. W + Sp. 21.Sp. Laoro, S Ic. D'cano Tenn. 1860. p. 48. Allegianno Typhno. W+Sp. N'a'gan. Gn. in W+ Sp. Cir'd. Waugue + Decaton Co. Tyleo in Wrathon Cir'd. Springfield. + in Molochinno Decezon's. W + Sp. 21.Sp. = Legocchino Lacoro y Recove. Typho N'ag an Gn. Western: W+Sp. Bucachet v chiamo 'dina aldi. W + Sp. ag Minn. J Cimp. 2 d. T n. 6 Sp. 1892. = Ga. Western: W+Sp. N'ag an Gn. Waguo Co Tenn. Typho in 90 State Cir'd. Bucachet v chiamo 'dina aldi. 1875. N'a-6an- M'n'bo Locd near Nashville. Deca- S.S. C only Cir'd. Tun + Waguo Co Tenn. Tyleo in Tom.

Ogygocerinum apudescens. S.A. Miller. 1883 Ductus grapt., Cista Grenadiana in S.A. Mullen Cell. Glyptocerinum Tommolelli. Murchon. 1874. Munson + Wrennesia, upper part ? Hudson River Gr. Sykesen Cat. of Wh. D. S. Gonzoletti. Citta d'Albano di Roma. Studien über die Tausendfüssler von Dr. F. Müller. Diversorium &c. sculphuratum, Abdi. Gen. Hidd. Albomum NB + (Farr Cr.) Wh. New York VI III 20 Oct., VII III Ogygocerinum Halli. Sgron. Niagara Grapt. (?) Stenariella. Ky. Type lost. Out specimen in Orden Coll. at New D residence. J nd. See W + Sp. Wasteglycerinum MacKe. Syon. 1861. Niagara Gr. offiers on Cr. Ky. Type in Murch. Coll. in Ordn Museum Ky.

Shumard collection at Washington Univ at St Louis, In charge of Dr Hamulach. In Wathens private collection in at the State University of Illinois Sp. or Champlain. Sec "I" in charge of C. W. Dodge In apper collection, with types by dr J Shumard, one Chalybeite in Whig county, Madison Co., Ind. New Greenfield and 2 miles North of New Harmony, Ind. on day of Mr Vida Morgan, better known as "Fort Garden" In + Fort Garden, Mr Vida Morgan, better known as "Fort Garden". and, Dr Morgan's garden, in charge of Prof J Gorden, Charles J Gorden, and Dr J. V. Smith, Jr., in charge of garden. Dr A C Vandeleur, in charge of gardens, D.C. Vandeleur, Mr. Mr A & Vandeleur, in charge of gardens.

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