Field notes, undated (2)

Half way between Difficult creek and 620 Orthothynchula veynara. 11 ft arg. rock. Sorne orthothy.. chula, 3½ ft Harder the edge north, Orthoptychula & other crumm 2¼ laid blue l, frosty crystals var & dingharry: 5½ ft Inteval / with hard bluel at top. River level; The Orthothyph chula rock appears to 20 coming down or dipping down the stream, The rocks above the Ortho... chula linings are arg. rock and frosty forms, if it get less frosty forms further up as in case of Diff. Cleyer. The fact was not former. One top of the experiences is too steep here. Black slate between Wolf creek and Hilly creek at water level, At foot of shore below Hilly creek is Black Slate on south hand dipping slowly down the area.

600. Rock rises nearly my breast breast above. 28 ft thin bedded rock, arg, not seen. 4 ft 6 in massive spalling arg. rock, 1 ft. Blue limestone. 1 ft. Arg. rock, rather blue. Fossils few, Down stream after an unknown interval, prolificous arg. rock once in ! With difficulty the thin bedded rock appears to be from Riverclunch, but I don't seem, The top of prolificous part should be Anderton but fossils few, 629. Rocks nearly horizontal, fate try to get at rocks as that beneath. Obs. 25 ft apparently of same kind. 5 1/2 ft arg. rock. shrine Riverclunch 22 ft arg. rock, moderate fossils, 3 ft arg. rock, poorly Faver sandst, blue in part All of these rocks should be congreville.

"Bellw 629, just above Belk's Island, in SW shore Orthorynchula and Cyprinee vallan dinghami occur 11yt above river. But over here is a dense thac line gone although are in layers. It is this dense sheet below the great thickness of arg. and of the Corryville which suggest the Orthorynchula bearing little stry; eely, This would place about 11 feet of Fair mount below about 53 feet of Ingrille as far as present arts will indicate. Opposite the middle of Belk Island the arch rises. It has been rising since upper part of island. This tings up the arch belm this Orthorynchula bearing with zonal Strips, which may well lower, we get some vallan- dinghami; Crustellaria, Plat. ponderosa c. Pt erina almis 2a medium size. Stephenuana at top of sectin equals fella removed a good There is about point of 15 foot section here in flat way trangular vertical valves as, with typical many s'illness; The upper Fairmount consists of three rather thin bedded limestone fully fossils,

"My characters: Latchia occur opposite the middle of Belle Island and her "helm-tipper" described on preceding page. Tetradium is rare, one collected, From the middle Belle Is- land there is a slight dip from stream which fails to bring the Upper Formation down to river level, opposite the lower end of Belle Island and there is an equal slight rise in the Upper Form. in front. The rocks are essen- tially horizontal here. 631. Just below Belle Island, Latchia and Tetradium are common, with ophic chaula veins in same layers as to the latter indicating a vertical range of at least 25 feet of ophic chaula. The rock sizes gradu- ally down stream and sinks again slopely as far as that from it the river. But is essen- tially horizontal. The ridge fossils forms just must be about 20 feet thick. The concrete forms the vertical ridge part of the cliff.

631 some of same kind of as. No. Chaly. Plt. Pseudana stromm upka and wth Plat. pseudanadae, Apt. rick, lower half scaling 12 ft vertical with Plat. jermcnesa 14ft thick bedded, 5ft fissile fen, more argillaceom with phymacula lufcent. 3 3 ft sinteral, wppr farrunnt 4 1/2 Detraction & Lutechia 7 ft interval River level From the stony lens in the river below 631 the rock appear to rise slightly down stream but ve is practically horizontal. At the head in the river a mile and a half above Beano Creek a sort of sandy rock some 2 less cross bedded, rises slowly down stream. It resembles the rock underlying the top of the Author's included beds at 631. But there are practically no fossils here. A party of this so-called sandstone looks quite massive. Further down stream the sand rock dips down stream and a prodigious ark comes in above. The profile essentially linsignial, further.

"Geologically the upper rock resembles the Falnamut. A short distance farther down stream the top of the layer with Labeclia crassata & Tetradium rull, comes in 8 ft above the top of the so called sandstone horizon. Here with Rhynchula & F.ana associated with Oysterea rull andingle came just above the sandstone str by that the with Rhynchula layer rests in this so called sandstone horizon. Down stream the nodular lower Orthorhyaculea beds containing Labeclia &m time to be exposed. The lowest rock seen as far is the 2 and 1/4th, about 15 feet thick, belov the Orthorhynchula rock. Farther down stream the Labeclia and Tetradium come in about 6 ft above top of cross bedded Sandy layers. Ortho rhynchula cross a short distance below the Sandy rocks.

"just below Pleasant creek, On right bank of river going down stream there is a little Creek coming in, through a valley of some size but the creek is not named; Here Labechka comes in with Orthorygnula bed about 10 feet above river. Also for others as here collected, the Crayville shows up well on the face of the cliff, with that part of the orth. slugs which have overlying the Labechka well displayed. The rocks here are practically horizontal; the locality is about 1/3 mile above Beacon creek, Down as far as Beacon creek the rocks are practically horizontal with the Orthoryg. chula beds forming the base of the section.

Rheena. Refinesquina, Pl. pindara, Helotella of zinnata type but not coarse clefted or meshy. Cyst scaras roll and dingy sand, 0 J. y exp rone. 8 1/2 ft Refinesquina, 5 1/2 ft C rare byrgano, Sinup's illomen d'are, 4 1/2 ft Strephodula plana concava c. 5 ft, Orthorhynchula Lindellaria 7ft {Lactria c. Tetradium rare. Githo. Rhynchula 1ft, Tetradium common break, 4 ft normal, merging into into arg. rick, normala, a short dist and up river from 8; the cross bedded only coarsely granular lower and creelled (and layers) come to fu about 5 feet above river level. This ink belongs below the Ortho- rhynchula design if correctly interpreted, it has the cross bedded appearance. The rock dips down the arm and further down the river the Lactria in the lower part of the with rhynchula layers is common.

681, Cythereas vallandingham: Stephenson plant canyoxa. Hadrilla sea sinuata. Rafinesquina, with rhyncholite in Orthoclyna chula layers which here are well stratu- fied blue limestones. Covered by at least 25 ft of lime- stone, with abundant fossils among which plat. ponderosa is very common. This rock is quite similar to the underlying ortho but proba- dy in the lower part of what I have been calling the Cygnillite. It is more argil- lacous than the Orthorhy- chula rock, the hygrophy- are much less and plat. Ponderosa + Hadrillia make up most of the fossils. It ranges upward into more typical Cygnillite rock. At top the typical Rhyncholite layer Richardson comes in, with heavier layers seen the same. Also some clean ver layers near the top; in heavier layers near the top one finds fine blue, fine grained limestone. No fossils probably just below the Calmerock's limestone.

681. [illegible] 60 ft Congniile, 8 ft Near the Blue Mota with Bryozoa and Agamentas with few animal with high clods. 6½ ft similar rock but with con- siderable Argonite interbedded. 23 ft out crowd. Both strata a Type of ordinal rock with Lobechia + Petradium 21 ft Similar rock to above = blue rock, of which upper 7 ft: Lobechia rock. Cross bedded granular are called sandy rock not measured, The rocks h are seen rising as far as 681. The rock C an- times to rise down the river, but before reaching the point where the river turns north, the rock becomes practically horizontal. Bthm. Half a mile above Long Island the rock suddenly rises still more with Raphine grusae abundant bryozoa + with Argonite, bnt no Lobechia seen then very smooth with long Bottom island i reached.

at head of Long Bottom Delight Stream, Stromeremmeras will magnetism villeniers is abundant for the first time. Because it is associa ated with Orthorhombicula, this horizon is assumed to be above the thin orellied sandstone layers, on the other side there has a vertical distribution of at least 6 ft and is very abundant. The rock dips slowly down stream the length of the island. On Stromeremmeras show up at edge of river, On dip down stream entrance and then the rock rises again slowly but is practically hori- zontal. Just before reaching the dirty side of the river 1 out ward stromeremera magnetism was found near sides cape, but in Labrador was seen. At stormy head of river above 56 Tetradium, Strom. eragon ill. is abundant. Several para leaches p2 na willi, artho- rhynchula are Labeled. No regnum Lledria Layer, One Bacharjena willi 41/2 in depth and 9/16 is mud at mud point.

656. The arch is fairly born and ed up to this point. One Sabetha but no Sabetha layer, one Stone, mayor Allen's, several Cathryllychnula. just below Little Indian Reeks: one Tetradium large and fine at river's edge. The 2nd rips down sheer and higher layers come in full of byr zoms, with Cathryllychnula, The arch is practically horizon tal below this point. Where the rim bends north, the arch rises gradually from sheer, and then becomes just a little horizontal. No arches exposed at river's edge from town in river to head of Blackfish Bar. Below Blackfish Bar, where the river turns west, the arch rises toward the turning point slightly, But Whynchula, Refining seeing Tetradium single at top of Strophepneuma lyrigin. The later is chiefly the triangular a reasate Mayon'dleness. The Strophepneuma layer is about 6 ft thick separately, One Sabetha, One great Sabetha but belong to bar. Five Cathryllychnula.

The grey granular cross-bedded arched sandy rock appears to come in after the base of the section at the head of the river. below Black fish. I am not of this is the case, no fossils langer was detected. D own stream, the rock dips slightly downward but is practically horizontal. Above Blanken ships Island, at end of cliff exposures, Tetracinn vicus with Ortho. rhyn clada in upper part of Orthorhyn cleda section. Along the 68 Mile breakway rock is exposed on S bank, Orth rhyn cleda lies nearly horizontal, Then the rock dips rather strongly toward Campbell Island and then by down. The tip of the Orth rhyn- cleda lies near river level. Just above Campbells Island the rock rises again slightly, but as a whole the rock is horizontal with the Orthrhyn cleda beds at water level. Other rhyn cleda, St repsemeena encags vellenes, Crestellaria, Rhapidosgonia On N bank below Campbell In- land, the rock rises a little agreemently Orthrhyncleda rock,

At the sandy the river NW, half a mile westy creelboro bar, Refines guma common. Orthrhyne chula? Numinous byzgrams. The rock is nearly horizont al. To me, well hidden himselfe. Form part not anglic lace not regular and the lower part of the orthrhynchula section probably was not exposed. Not well identified horizon, Above Sherr Island Refines guma common. Fully byzgrams. But however one resembling Orth rhyn chula beds but no characteris- tic fossils found. It might be lower Camville although this is supposed to be rather different by its byzgrams and tr. cnt now chiefly Pl. fenderm. and Helentella. Rock prac- tically horizont al. This near in the top transitional Ortho- rhynchula rock.

670. From the turn of the river east of the Rock House the ark rises miraculously down stream. Since Stephenson near plane convexa also mays- villeners, between 10 and 12 feet above river. Orthoryn- clema stones. || Then the ark dips gently toward the Rock House or that the Step-plemene led comes down to water level at the Rock House. Refines grain is cream 7 feet above the steppe venea hinge at Rock House, 21 feet from River at Rock Hne. to top of orthorynchala beca? fine in which hyrps are me abundants above this level there are arg. beds inter bedded in what might be called the transversal mac beds. West from the Rock House as far as The bend in the river the rocks are essenti- ally derigenous, here the river turns south. A rather thin fed bed here fine limestone on sides down the creek form a clear coal creek.

At Clear-crat Creek a Cyrtoceras roll and one beam and a single Orthorynchula suggest the presence of the Orthorynchula beds but the strike dips rapidly down stream from here and from the lower Congerville is at river's edge. The next exposures come beyond Craw Creek. The Ridley Ortho- ryhynchula brown is not ex- prired here at all. About a third of a mile west of Craw Creek several, the Congerville bed appears to be at water's edge. No abundant Bryozans lensy Ples., found except Albertella. From here the rock is essentially horizontal, as far as 70 miles locality. Here the rock rises strongly down stream! The lower rock at river edge is Congerville. At 70 the rock has risen enough to expose the Ortho- ryhynchula beds with Raf- es gregina in upper layers, then below with Orthoryn- chula, Comatellaria's STE- frii forms, rugos williams, and such othera as this; above 70, on W side of river, the rock dips down slowly.

at Dave creek, or Millast, Refining mine c. Nemans synonym is natural line l, Strathelena may villeusi; is chunn & ft above rim level, at mouth of Dave a Middle creek. The hyzom riderizes at least 20ft above this. This creek is at sharp turn of river NW, above Miller's Creek, The rock is practically horizontal tal here. The rock is practically horizont at as far as the shelf strata and then rises slightly down stream, but is practically hori- zontal in about half a mile below the Shelf strata. After this there are no exposures along the water's edge, at about 73 1/2 miles, Refining Quinn occurs but no con- ductive Orthophychnula bed fossils were found. Then the rock appears to dip down stream slightly, but sufficiently to cause the Curyville to set down to waters edge a great distance. There is exposures for long distance in west side of river.

Cap. Orchard & Brommell landing at g[a]r[da]y's route. The Grignille is driven at water edge w/ large Plas, then dense, and Wistella drift at any rock, this rock is nearly horizontal. At the port of Willis creek shoral The same Grignille rock is exposed, dipping slightly down stream. = nearly horizontal. 660 At Yiche Creek the T roller landing stone used to be but it is now down now. Black Whale 5 1/2 ft peculiar to rounded rock, age unknown. {9 ft indurated arg. massive rock, speckling, breaking up into thin saw layers at several horizons, but chiefly massive. 9 ft of arg. rock, identical with the gravel w/ its weeping rock but weathering to very thin bedded, clayy material. } {9 in. f[ra]g[me]nts from island E. 2 in. clay. 9 in argill. dome edged limeta. about conformable. 11 in clay shale, w/ hygro-mous care. 13 in. D[ye] coloured b. in several layers, very hard but the affected in their laminae which are well acted on or so to make much the thin lags.

666 contd. 76 in, weathering thin and soft. 11 in, ? arch similar to preceding but in three layers. 10.5 ft. Argill., silt, upon part very thin bedded and gelatinous, lower part more medium bedded. 5 ft. Arg. limestone, medium bedded, weathering readily into thin laminae at various elevations, 22 in. L. drecrbed, with short modules or lenses, the top surface of this rock is fretted with water borings. 8.5 ft. Similar rock as above, smaller modules This rock looks as though made up of very thin layers held together as so to make up an immense number of layers. 28 ft partly exposed but covered with debris as though there might have been thin bedded argillaceous layers here, but these were not seen. 1.5 ft. thin laminated L. forming an aggregate layer base of Richmond? 21 ft Congerville underls bdy is Andersonian. Refines & grinning Cherry run, mine with Masuta argillaceae in niterhus. 18 ft ? nterial. Refining graving C 6 ft Outcrop, Congerville. River level.

The rock dips slowly down stream To Albany Landing. South of Whetstone creek the rock is practically horizontal, as far down as Spearman Island, From Spearman Island there are no exposures as far as 80 mile locality, a quantity of a mile above 80 mile locality the rock is per- fectedly horizontal, From so mile locality the rock runs gradually toward Argos creek. Rafinesquina, Plat, junderson, Websterella, Bry- gyramna occur in transition beds at top of earth structure below horizon but I may be mistaken about this feature as characteristic of the upper Formation and absence the lower Cragville. Rafines- quana occurs in the Bygyran horizon. An excellent stuf occurs an argillaceous member 11 ft above Dora bed in large lime slab, associated with Constellaria. The bygyran member has largest thickness for 6 ft above,

"[illegible]" 3ft limestone mine. 2ft limestone fully chert nodules. 11ft thin bedded layers. In several layers. 14ft Mine like limestone long but fine layers. With tendency to split up in 2ft fine argill. Massive rock chert nodules in upper 1 hi. 2/3 Mine massive arg. Rock with with traces of fossils nodules in upper y inches. 2ft Massive arg. Rock with chert Nodules 6in Two layers similar to one with chert mixed in as to be massive. 14th thin more stratified rock. Argill arg. limestone one. The upper part of the Grinnell and mines few fossils, flat sandstone beds down.

At the turn of the river below Bakers mill bar, the rock dips strongly down the run, and then rises slowly. Next the rocks became nearly horizontal, then up slightly downward, and rise again with not changing the elevation of the face of the Richmond over the river road since the land west of Cross Creek. Next the rocks rise slightly, then dips slightly. The rest remaining horizon- tally horizontally. The section described a former trip from spring from Remix creek, just above the mouth,

Mary Rennie creek. In upper garden, rift my lower 3/4, Hinda 40 ft like landed Nicotin 1st clays. 6 in arg. rock. This tadded. 12 ft clays. 27 ft Plain bedded Richmond, Lumelli br much landym. {1ft. frosty fumes arg. I, {2 1/2 ft Mtn picked c} These two above probably are top sections at Albany Landings. 8 ft thin bedded Richmoud. 1 1/4 ft arg. I. with chert 3 ft thin tadded. 5 ft arg. I. with chert & sandles in upper 15 inches and in lower 15 inches 14 ft thin tadded. The route winds as far as the land in the hollow and then rises slightly, it crosses me to rise southward, I could drive down here for B miles wide in a biggy since I am a biggy guy, and a good road goes to Crowns creek.

"The rock continues to rise 1 toward the 85 mile stretch, the lower lying rocks appearing then headed. When seen from the boat, a good section could be worked out here, since the upper Craigville will dip west farther down than can and the dip is very even. Other inverections should be carefully measured. At Alexander B on the rock rises rapidly, it becomes horizontal at the bend of the river after which suddenly, the rock then dips down again. There is a north tract at Barkerville. According to my correct usable total dips here, these sections should be worked out.

6 miles from Burnsville on road to Albany in all Fork Hill, South side of Fork, beyond Beck creek, Black Shale. 1 ft chert nodules on mass 1 ft ms. massive and jointly breathing thin bedded. 1 ft sile with chert nodules + layers with Pterchi dyptera entomo-dna and Platy-Horizelura, Chert with vertical worm trings. 2ft Massive ms. d. No Upper Silurian here. Probably about the same as Albany Ginding section.

"Russia Calf 2074 " P11, 3rd Cts. F12 Gouache F13 Enam F14 Utruled