Eastport quadrangle notebook # 5, 1908

Breger, Carpel Leventhal

Unknown

Smithsonian Institution Archives

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Geological Survey (U.S.) Paleontology Geology

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Field Notes 1st original notes taken in field, numbered as No.5. Taken originally on loose sheets. I have arranged them in order of map blocks & sec Also dehydrants also abstracts of field notes and lists of species arranged by order of map blocks. +SN Culled or aided farmers of Saratoga area CSB Note Book 5. 1908 pasted on placed other maps over Moore's Movable Markers (Patented 1903) John C. Moore Corporation, Rochester, N.Y. Barger, original field notes des taken in field No.5 806 1908

RARY OF WILLIAMS.

11.8 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 In the railroad cuts in the S.W. corner of Pennamquan Lake occurs a series of very dark blue-black massive shales resembling in texture & color the Quoddy plate series. No fossils were observed evidencing very obscure traces. May have been mineralized graphites. Strike N 8° E dip 24° E About 400 yards west of the railroad station at Apple Junction occurs a cut exposing some gray & dark blue evenly laminated shales. No fossils. These shales are better exposed in the little creek just north of the railroad where they are seen to Strike N. 11-15° E, dip East 19-20° Some more of the shales appear in another RR cut a couple of hundred yards S.W. of the creek. The shale here contain very rare what app pears to be C graphite, and is readily expressive Nephrites-like Antlers as which places these shales in the Quoddy series. Fossils = strom. edge of 11.8 2 Quoddy plate series 1/1/8 31 Breger. 1/1/8 A

[illegible] 32.

1.3.9 Peruamaquon Lake, S, About 300 yards N.W. of the Bridge there occur in the hill side S. of the road some purple shales & brown phylitic mudst. striking N 60° W. dipping 30° N. E.: they contain an abun- dance of casts of Leperditia, or rather what appears to be Leperditia but these seen on all surfaces do not show any organic nature & are more totally small mud balls = 1.3.9 A

Plain Quadrille Ruling Patented 1906, John C. Moore Corporation, Rochester, N. Y. Aug. 27 '08. In the railroad cut at the S.W. corner of the bench in 120.8 occurs a crossing of "galbre" and white rhyolite "micro granito" dike. 120.8 The nearby country rock appears to be flow breccia of basic andesite highly injected with the white rhyolite. The rhyolite is a white to pinkish white glass, but near the boundary with the galbre dike it becomes darker in color. The rhyolite is highly mineralized with pale colored gyrite. Specimen rhyolite 120.8 (D) The "galbre" (= coarse diabase) dikes trend S.W. x N.E. and there are suggestions of finer grained texture near contact. The galbre appears to cut across and in- terrupt the rhyolite. About 300 yards to the south there occurs along the railroad (east side) an ex- 1.30 posure of basic andesitic flow breccia. Recently weathered surface is green; older weathered surface resembles "galbre" surface; fresh cuts are gray tinged with green & frequently tinged with purplish-black Specimen 130.2 (D) Over 100 feet of this are exposed. Next to the south, there occurs at the north end of the deep railroad cut some 5-10 feet of dark blue-black tuffaceous shale. 52.30 These bedded shaly tufts or tuffaceous shales overly a series of frag- mental massive tufta outcropping in the 130.2 (D) cut and to the south over a width of a couple of hundred yards. over

are very light ga are very light gray in color, but on freshly weathered surfaces are exceedingly dark, almost black. Specimen is numbered 1:30:2: A slight fault plane with accompany(2) ing fault brecciation is visible in the west side of the RR.cut, trending N.25 degrees east. Southwest of the RR.cut occurs a series of exposures over 100 feet broad of gray and green-gray bedded, typical, basic tuffs, striking N.60 degrees west, dip, 29 degrees N.E. At the southwest side of Wilson' Stream at the RR.bridge occur some 4 or 5 feet of gray shale, striking N.55 de grees west,dip 32 degrees N.E., and which are flanked on the southwest by a gabbro mass of which latter a width of 50 feet is exposed. The next exposure to the south is in central 1:30:4, at the RR.curve where occur some fragmental tuffs of the same type as 4:1:4:(1);i.e.- color on fresh weathered surfaces bottle green with conspicuous pink fragments. The most abun- dant fragments however are light and dark g gray in a matrix of green.

SL 123.6 A In the roadway about 25 yards north of the FR. crossing occur some gray splintery shales, strike N.47W. dip 27 N.E., splintering N.58 E. Fossils (not collected) Stenoscisma sp.......occasional ?Chonetes sp.......rare Tentaculites .........rare Crinoid stems..........occasional These represent the Kelly Point gray shales of the Denbo series. 1.23.6 (A)

Wilson Stream Inlet In the core in S.E. 1,52,6, on the west side of Wilson Stream appear some fragiliferous gray- white rhyolites somewhat mac- erated. These are overlain by a purplish to purple red porphyry which is usually hard & glassy, frequently softer & occasionally contains scattered fragments then resembling a tuff. A gray rhyo- lite porphyrite seems to intrude this, but possibly is brought up by faulting. The massive purple rhyo- lites are overlain by bedded purplish tuffs. These latter, about 20 feet thick are exposed at the outlet of Meadow Brook and underly the fossiliferous sed- iments which crop out farther up Wilson Stream.

Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 East part of square 100 ft broadly sloped road. Light colored (lavender to gray) gray palyolite underlying (to west of) purple tuffs, palyolite flow lines N.64°W to N.75°W. dipping +45° N.E. The tuffs and corn posed of small purple fragments the size of a pea or smaller & with occasional small gray basic-looking fragments. The purplish massive palyolite forms the entire 100 ft broad on the S. side of the road where it continues in a ridge S.E. to just abt S. of the middle of the 1.22.2/5 line. On the east side of the road for the N.E. corner of 1.22.5 occurs a mass of green-gray amygdaloidal tuff, which reappears a couple of hundred yards S.E. in the road in N.W. and continues S.E. as far as At the junction of 1.22.6- 1.23.4 the tuff has a width of nearly 7 25 ft N.E. x S.W. The trap is composed of amygdal- noidal, west & coarse N.N.W. 1.22.6 amygdaloids in bands striking N.144° W. dip + 30° N.E. Amy Specimen Amy amygdaloidal specimen 1.22.1. 1.22.2/5 1.22.6 1.226 A

"near east edge" of 1.22.6, N.E. of road as. In place the trap becomes darker "of a slightly purplish" huge."Such a specimen is 1.23.4 (.) (massive, fine grained) 1.23.4 from east central 1.23.4 100 yards. N.E. of the house of Mr.--a prospect hole was dug in the trap which is here much fractured & ferriferous: To the S.E. the trap becomes very much broader, or 350 ft. road & extends 5E beyond the T corners Reddish brown truffs seen on the 1.23. E line & on the little hill at E central 1.23.8. At latter locality show unevenly strata truffs near west end of level stake N.10 deg E dip 30 deg N.E., slanting nearly same direction N.25 deg dip S.E.

Railroad bridge over Wilson Stream, - 1:50:4 (A) In the southwest corner where the rr. bridge crosses Wilson Stream, occurs in outcrop of some five feet of fine-grained, light-grey, dense sediment striking N.50 degrees west, dip- ing 72 degrees N.E. The rock resembles the Wilson Stream fossiliferous beds of "Hardscrabble", Dennysville. It is high- ly sheared. The shearing trends N.42 degrees east. A search for fossils revealed only an obscure impression of what may have been an Orthids (Delamerella), very doubtfully organic. The specia imen is 1:50:4 (A)

An exposure occurs in the road 1.30 S.E. of the R.R. at 135 A.T. on 1, 20, 7. The rock is of light color & fragmental, all, hard & either a tuff or flow breccia. Too obscure to determine which. A similar exposure occurs western the road in front of Mr. Robinson's ~ 1.40.3 But both the S.W. & South of Mr. Robinson for a couple of hundred yards occur good ex- posures of flow breccia similar to 1, 30, 2. (l) Fragmental beds occurs in the hill in 1.41.1. The flow Breccia Type of matrix occurs only sparsely, (ni:e - matrix forming a net work about large fragments which are usually one 2 miles x flow lined & this network stands out more high above the fragments, the latter being depressed).

9 Quadrille Ruled Form. John C Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 In northern 1.35.2 there begins back of the house a gray glyphy tuff (rhyolite) which bends E. Eastward across the trail & after crossing the railroad tracks bends abruptly to the east for a hundred yards and reappears forming the little 80 ft. knoll S.W. of the RR. Station this Rhyolite tuff glyphy in depths, 50 ft. broad on outcrop, and where it bends to the east -- underlaid by some nor 15- ft. of gray shale striking N. 8 8 W. & dipping north at an angle of 150. sl 1352 A These gray shales (silty) contain an occasional Grammopora lamelli Branch. There as near the Garnet Point (not shale species N. 77 Lbsc. collected these gray shales are correlated within as gray band in the Pembroke gmple or else as the top of the Garnet Point member. 1.35.2 A In the upper 80' where RR crosses Wilson Stream occurs a white firm ft of fine grained light gray dense sediment striking N. 50 W dipping 70 N.E. The rock resembles the Wilson Stream formation led of Schuyerville, but largely over 1.30.4 A

obared. The clean up came N. Y. 50 E A search of fossils revealed only an obscure impression & which may have been an Orthio (Dolanin ella), very doubtfully organic. Eguals 1.30.4 A

10 1.43.4 A SL 1.43.4 A On the road near the east edge of 1.43.4 crops out a highly Amygdaloidal trap. This does not again show to the north, but the ridge under which it is presumed to be may be followed for 100 ft + N 15° W up to the bend of the brook where at one point amygd- aloidal trap boulders are exceed- ingly abundant. Between this ridge and the brook, about 100 yds. North of the house of Mr. [illegible] there occurs about 70 yds. East of the trap (?) ridge an exposure of gray shales one seam of which contains Platyschisma common murchisona sp. acavi. ostreocods of Dilobella " Gastrop zone 1.43.4 A

1. Quadrille Ruled Form. Patented 1906. John C. Moore Corporation, Rochester, N.Y. Oak Hill is composed of a thick mass of basic tuffs which occasionally contain fossils here & there. The rock v mode forms once if the fossils is similar to 1.55.1 A. These tuffs appear massive but occasional ledges on the west end show strike N.10°E & N. 15°W; dip 40° E. This strike is so as variance with the strikes above & below as well as with the general trend as to suggest cross bedding in a delta or sandy local deposit. The basic tuffs of Oak Hill do not again crop out either to the N.W. nor to the S.E., and that they are not faulted away is proven by the absence of any extensive faulting in the vicinity. Fossils were observed in particular in the N.E. face of the mountain some 60 ft below the top = {Platy schisma common Murchisonia occasional 1.55.1 A then argon shale)} not collected 1.43.6 Oak Hill. 1.43.6 A 1.43.6 A Not seen

12 1.43.8. the amygdaloidal trap occurring in the road near east edge of 1.43.2 may be followed S. E. and at a distance of 150 ft. S.20 deg. from the road, begins an escarp- ment of this trap which extends to the house of Mr. Tom Smith a mile or so S.E. Opposite the beginning of this escarpment also about 100 yards to the west there is a light purplish, argillaceous [illegible] mud resembling clay- slate at first sight, and under- lain by similar colored and green gray loose tufts interbedded. strike 56.18 deg. in course of 100 yds. 46.18 deg. The green gray tufts frequently show copper glauze lining the cavities from which the fragments of the tuft have been dissolved away. Mineralized specimens = 1.43.8 (1) The overlying light purplish = 1.43.8 (2) tufts around Fossils in the green tufts are rare and. A Selzodus like Lamelibranch was found: 1.43.8(A) 56.18 deg. 1.43.8 A Referee 30 28 26 24 22 20 18 16 14 12 10 8 6 4 2

Punshin Oak Hill 13 Quadrille Ruled Form. Patented 1906. John C. Moore Corporation, Rochester, N. Y. SL 143.9 A 1.43.9 A Gray splinter shales crop out along the roadway to Mr. Tom Smith's on the S.W. side of Oak Hill. V 50.20 . The fossils were collected north of the road at extreme N. edge of square Chonetes nova scoticus Dalmanella Stenoscisma pulchra Retzia barrandei Spirifer crispus = Bonerina Cleidophorus ovatus C. " sp. B. Cypricardinia platyphyllus Actinopterella spp. indet. Pteronitella retroflexa Calymene Dalmanites Beyr. kloedeni (U) Sulciceras Ceratiocaris Crinoid stems 1.44.2 A Gray splinter shales in road in front of Mr. Fred Syragus's Chonetes bastini Stenoscisma pulchra Tentaculites Crinoid stems not collected [illegible] 28 30 26 24 22 20 18 16 14 12 10 8 6 4 2

14 Exposure are very numerous to the west of the house 2 south of "Wooden Creek in northwest 1.51, 5. The rock is here a tuff, the fragments very frequently standing out in relief above the matrix. These larger fragments as also the largest X are a light gray colored glass possibly laze. The fragments are light gray v dark gray usually not over an inch. In one or two hands however occur large fragments on a foot thick of banded andesite W chalc ("base tuff"). 2 specimens are This latter is a hard light colored tuff of fine grain v small fragments matrix whitish, fragments small (less than 1/2 inch) gray. The rock is bedded, strike N 37 W dip 30 NE 151, 5. (1) (2)

Page Hill The west shore of Wilson Stream opposite the cor along 153.7-8, performed of a flow shalyite which gives in its upper portion and a duller red colour. The strike is N. 75° W dip 38° NE, the shalyite becomes an agglomerate - 153.8 [illegible] below the lower 50 feet and at the base as exposed a few feet for make dull red muds. These seem as the point in 153.8 and are splintered N 40° E in which direction (approximately) indicate a fault plane since the red muds plant against an acid porphyry tuff which forms the joint. This porphyry tuff is also greatly sheared [N 38° E] for over 50 feet S.E. of the contact. The porphyry with contours & the top of Knibley's Point and is of a prevailing light color. Red more than dark red not occur at all. No usual colors are various shades of a light gray with blue fragment occasionally pink. Strike N 12°-15° W dip 32° E. for near 100 yds S.E. of fault, and strike N. 32° W dip 28° NE. Between here the Point

Quadrille Ruled Form. Patented 1906. John C. Moore Corporation, Rochester, N. Y. A ridge of shales composed of bedded lentic fuse tuffs forms the crest of the hill and overlies a massive basit cliff which forms a contin- uous escarpment as far S.E. as the Ox Cove Road beyond. The strike is N. 55° E., dip 30° N.E. The fauna of shales at crest of ridge is large Cyrtodonta occasional Spiroorbis common Platyschisma occasional Pentagonal Crinoid stems " One seam contains in abundance Stenosisma pulchra Exclusively. The rock recalls 4.5.2 A. This fauna overlies 1.54.6 A. 1.54.2 A 1.54.2 A

(7 Quadrille Ruled Form. Patented 1906. John C. Moore Corporation, Rochester, N. Y. The ridge of basic tuffs in- 1.57.6 A cluding 1.57.2 A can be followed southeasterly for 5000 ft. or more to beyond the house of Mr. — in S.W. 1.55.4 The rock forms a conspicuous escarpment through this length. In the fields in west central 1.57.6 about 125 yards north of the house of Mr. H. W. Carter & there occur underneath the tuffs an exposure of some 10 ft. of gray splintery shales N°6— The rock is fossiliferous containing seams of Murchisonia (cf. Young's Cove) with Chonetes bastini C " nova-scotica Cypricardinia platyphyllus Paracyclas Tentaculites Crinoid stems Pholidops

Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 Ox Corn 154.9 A west shore of head of Ox Cove. (see plano Valle Street) 15 feet of shales of gray color. Strike N. 10°E (dip 22° E.) to N. 25°W (dip 8° N. E.) weely - rue green x purple aingydel white puple red nunds. ordinal shales fauna Lingula striata rare Orbiculidea (Large) rare Chonetes bastini abundant Dalmanella (schroerer are)

The same band of shale as 1.54.9 A reappear in the little indentation on the east side of the head of Ox Cove underlying the gray bands; fine triffs overlying the purple red member. The fauna is the same, only a few specimens chiefly rhodis were collected 1.54.9 showing Dilobella sp abundant Chonetes costinii dalmarella stenosieva Lingula strata cantabuli etc.

The long ridge trending N.W. from 1.55/1 into 1.4/5 is composed in part of a thick mass of highly amygdaloidal trap with the augddules commonly concentrated into bunches. Southeast of the road the trap exhibit well marked flow breccia structure. Over this trap (to the N.E.) and separated from it by a valley like depression 75- 100 yards wide is a gray playdate porphyry tuff which may be followed from the Pembroke-Dempsville road S.E. to the Penamaguen river near Small's Island. The interval between the porphyry tuff & the amygdal- oridal trap shows exposures only in 1.55/1 A where S.E. of the road the rock is a very massive basic tuff with residual pumice fragments while N.W. of the road the basic materials show sluire bedding into gray shales. These gray shaly-basic tufts contain fossils = Platyschisma common PMurchisonia (Forrotoma) comm. Bellerophon 3-lobatus occasional " "var. acutus rare Stenoscisma sp. occasional (w/o with gastri). Paracyclas, Vanuxemia(?), small Cleidophora lamellibr. occasional

Quadrille Ruled Form. Patented 1906. John C. Moore Corporation, Rochester, N. Y. The south end of the 80 foot knoll in N.W. corner of 1.55/1 - S.W. 1.45/7 is composed of an 8 foot ledge of gray shale striking N. 33° W., dip 10° N.E., splintering N. 52° E. The line of strike abuts against the intrusive massive trap which forms the hill. The south edge of this trap runs S. 70° E into the amygdaloidal flow forming the high ridge. The fossils in the shale = 1.55/1. B. Orbiculoidea small rare sp. large occasional Chonetes bastini occasional Stenoscisma pulchra common Retzia barranderi occasional Cleidophorus ovatus rare C " sp. " Actinopterella 2 or 3 spp. occasional Pteronitella sp. " {Dawsonoceras sp. rare Encrusting (Bryozoan) " Cornulites serpularis " Crinoid stems abundant Ostracods " {Dilobella most abundant Beyrichia sp.

2 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 2.25.8A. Perry (Upper Dam Shales). B.L.Breger, Collector July 28, 1907. Notebook 2, page 54. Note 1. Lingula cornea(?) Sow. Rare Note 2. L. " minima Sow. Common = Sympygella shaleri sp. nov. Anodontopsis angustifrons McCoy Rare. Cypicardella (fig³) same as 6.5.8A² Very Common "Lophospira" (Streptotrochus) incisum Lindate Common at a seam. Note 3. Drepanella? (Tetradella) sp (fig¹) Common Note 4 Entomis(?) sp (? Gastropod fragment). Rare Leperditia hisingeri (fig 5) Occasional note 5 L. " sp -- (fig 4) Note 1. A recurvite form 6 mm long and 3.5 mm wide comparable with this species. Note 2 Small shells 7mm long and 3.4 mm wide having the elongate outline of this species. Note 3 Same as 6.5.8A² etc; Note 4 Probably a gastropod fragment. Note 5 A tall species having the eye tubercle low down far below the lirige.

x10 1 x10 2 3 1/2 x 1/2 4 5

Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 2.32.9 A. Sipp Bay [Pembroke purple shale] C.L. Briggs Collector Aug. 13, 1907 Notebook 2, Page 98. Lingula minima Sow. occasional Grammysia cingulata Hi. & var. " Anodontopsis angustifrons (?) rare Cypricardella (?) sp. (same? as 6.5.8.) rare Platyschisma helicites Sow. Common Drepanella [?] (same as 2.52.3 A) Rare Beyrichia salteriana Jones & var. Common E.K.(Oesel) " tuberculata (Bo Kloeent?) var. Occasional Aparchites (?) Rar. Lepeditria (very tall, figs. 1,2,3.) Occasional L " (very low, elongate pgs.4.) " Onchus sp. Rare. Note 1. Flatter in front of the post umbonal ridges than in the gibbous typical forms.

71.67 45 25 x 6.7 3.5 x 6.7 x 5 1 2 6.6 x 6.1 x 5 Left and right valves form a came infura slower net apart and apparently representing came indivi dual. 3 66 x 4.1 x 5 4 x 5 4.75 x 2-1 cf. 538.C4 x 5 B.d. noetingi (arisaig). x 5 salteneus B. knedoni vats. x 10 B. postulosa Hall var. noettingi (arisaig) postulosa x 10 B. striatexpiralis x 10 Aparchitces

23 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 2.32.9 B. Sipp's Bay (Pembroke purple shale) B.L Breger, collector: August 14, 1907. Notebook 2, page 86, 93. Grammysia cingulata rare " " var. triangulata Salter Oceans Anodontopsis near angustifrons Meby " Platyschisma helicites Sow. " Leperditia (2329A, very tall form, but smaller) " salteriana Touley Beyrichra Woodoni var's. Common " tuberculata var's & hoettingi Redd. Common - Arisaig Bythocypris(?) sp. Rare.

x10 B. gustulora Hall. x10 B. 2 1/6 x 1 7/32 cf. Beyriela gemiflata Weller. x10

24 Quadrille Ruled Form. John C Moore Corporation, Rochester, N.Y. Binder and holes in leaves, each Patented 1906 2.42.8.A Hersey Cove (Purple Shale) C.L.Breger Collector Aug.31st, 1907. Notebook 3, page 9. Lingula minima Sow. Occasional Grammysia cingulata Haugner " Platyschisma helictes Sow. Abundant. Drepanella sp.B (same as 2.52:3 A) Beyrichia tuberculata (typica) H.H. Occas. Note1. B" " var. aequilatera Hall Common B" Kloeden var.(f.gibba Salter) Rare. (Bythocypris (?) sp. " (Stage K Orsel) Beyrichia salteriana Jones ... Leperditia sp.# (very tall same as) Common 2.32.9A figs 1,2,3 L" sp (very low, elongate,

25 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 2.52.3:A Hersey Cove. Purple Shale. B. L. Brager collector Aug. 31, 1907. Notebook 3, page 9. Sow (fragments). Lingula minima Occas. Grammysa triangulata Sater Occas. Platyschisma helicites Sow. Abundant Beyrichia tuberculata [typica] Drepanella sp. B. (see over) Common. Occasional Leporditia 2 spp. same as 2.52.8A Common. {2.32.9A Onchus sp. Rare.

Drepanella sp B Similar at first sight to the Drepanella (Tetradella) sp. of the Broad Cove, Moose Island, and Perry slate beds; but in this present form the central tubercle is farther back; the anterior lobe entirely lacking, and the posterior lobe fainter, narrower, and decidedly less developed.

26 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. V. Binder and holes in leaves, each Patented 1906 3.43.6A. Southwest shore Carlow Rd. C.L Breger, Collector June 13, 1907 Notebook 1, page 48 Lingula cornea Sow. common Anodontopsis angustifrons Mclay M1268? Surquyple shaleri sp. nov. b.w.r very abundant Diaphorostoma glaucinoides Sow. common Tetradella clarkei sp undist (cf 3.444 A) occasional Cytherellina f siliqua(?). rare.

3/6 x 1 sometimes with longer spire as in fig. 3 fig. 2 x 3 fig. 3 "fish scale" [Instaby Lirgula cornua]

27 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 3.43.6 B. Carlow Isld (RR cut) L.D. Breger, Collector. Notebook 1, page 45. June 15, 1907. Lingula cornea Sow. Common Anodontopsis angustifrons McCay Very Abundant. note 1. Tetradella (fig over) occasional Manlius Cytherellina(?) sp. Bythocypris sp. " note 2. Leperditia (figs over.) Abundant. L. hisingeri Selms., var. " L. " of angustifera Whitf. Occas. L. of hudsonica Hall. " note 1. The anterior & posterior lobes are isolated; they do not meet below, the 2 middle lobes are equal and their lower ends curve and meet below forming a horseshoe the base of which appears to be swollen into a tubercle. The loose slice is quite distinct from the anterior & posterior lobes. Also same form also occurs at 3.44.4 A. note 2. The commonest species (see figs 1,4) a low form like L. alta with fuller front than L. hisingeri. It is not so tall as L. alta. It is probably L. hisingeri Selms., var. A second form represented by figures 5&6 is a very tall species nearest to L. hudsonica Hall also not quite identical also similar to L. cæca Jones, but not so flat in front. fig 3 represents the L. angustifera Whitfield type, which is swollen ventro-posteriorly. This is probably merely the mature female.

3/4 mm x 2.0 x 5 fig 1 tetradella clarkei fig. 2 3.6 x 0.5 2+8 x 5 3.4 x 1.85 2+85 fig 3 swollen x 10 5 x 3.75 fig. 5 x 5 4.7 x 3. x 5 x 25 fig 4A anterior change of m.

28 Quadrille Ruled Form. Patented 1906. John C. Moore Corporation, Rochester, N. Y. June 13, 1907. Shales may be observed along the south west shore of the island striking N.55 east and dipping 23 degrees N.W. Just north of a little trap dike which cuts the gray shales and occasional quartz- itic bands that make up the sediments of the island occur some seams of Mod- iolonsoid lamellibranchs and Lingula cornea. These fossils are 3/43.6:A. The shaly beds of the southwestern part of Carlow Island are abundantly wave- and ripple-marked, and rain prints are very common. A diabase porphyry dike cuts across the sediments and shows good contact variations. 1033 is the normal por- phyry four feet from the contact. 1074 is the contact phase, a foot from the contact. Just above this diabase porphyry dike occur shales containing both sun- shrinkage cracks and rain prints on the same surface. Some shales occur in a little railroad cut near the south end of the island, and contain the same lamell- branchs (not collected) as 3.43.6:A. (This cut should not be confused with the fossiliferous rr.cut near the cen- tre of the island, containing 3.43.6.B copied from Note Book 1, p. 43.

Plain Quadrille Ruling Patented 1906. John C. Moore Corporation, Rochester, N. Y. Saturday, June 15, 1907. 29 After finding that the Leperditia beds included all the Silurians exposed Carlow on Pleasant Point, search was made to Island find out to what extent if any, these rr. beds continued southward on Carlow Isl- cut and. The lamellibranch beds 3.43.6:A Notebook 1, page 43) were followed along the shore; then ensued the wave-marked, rain-printed and mud-cracked gray shales calcareous nodular layers, and quartzitic ic seams with only an occasional lamelli- branch, until reaching up to the rail- road cut(the northerly rr/cut containing shales; this cut includes the letter "l" in "Carlow" as on the chart, and is just north of the road running N.75 E to the house) where some coarse shales are cut by a rhyolite(?) dike which crops out in the west side of the rr.cut. On the east east side of the cut the shales continue uninterruptedly or nearly so, and con- tain Leperditia in thin calcareous seams A Leperditia occurs scattered rarely thruout the shales, but there are also several seams of lamellibranchs, with some Lingula cornea. Some Trimitoids also also occur as well as Tetradella. The fossils from this cut are 3.43.6:B 3.43.6 (B) (copied from notebook 1, page 45.

30 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 2 4 6 8 10 12 14 16 18 20 22 24 26 28 30

31 Quadrille Ruled Form. John C Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 3444A. Moose Island, north end C L Breger, Collector Notebook 1, page June 1907 Lingula cornea Sow. occasional, Temeside Anodontopsis angustifrons Mc Coy very Abund. "Lidlow" Diaphorostoma glacinoides Sow occasional Temeside Aparchites (fig 15) rare Primitia mundula (fig 7) rare P" sp B (fig 10) rare P" ( ) sp. alpha (fig 6) common P" ( " ) sp B (fig 7 slender). Ultrichia? (Bollia ?) sp (page 12-14) occasional Kloedenia sp B (fig 1) Tetradella sp. clarkes james very abund. Manlius {2,3} T. " " var's. Drepanella (Tetradella ?) sp (fig 4,5) abundant ? Leperditia near hisingerti lehmi (fig 16). rare. Cytherellina near siliqua abundant " or Bythocypris sp. " " Cyprosina (?) sp. (fig 8) rare Onchus sp. rare.

Kloedenia fig. 1 High outline, first furrow median, vert. cal half height, constricted in middle. middle lobe decidedly larger than poster. or lobe. 2 Tetradella (2) clarkei var. Tetradella 3 4 5 Drepanella 15 Aparechites (x 10) 6 Primitia ( 7 var. 8 Paint concavity Pontocypris mara maru Golen macrocypris Vignei cf Cyprosisma juve, 1881 9 Primitia mundula type 10 x 10 Primitia Cytellina bythocyprea. 11 12 13 14 Uricetia 16 Liquorita Eutanyeri

(Hinchley Point) Quadrille Ruled Form. (see also CB note 43/27) John C Moore Corporation, Rochester, N. V. Binder and holes in leaves, each Patented 1906 4.3.2 (A) Playlute gorpity turf forming the north prow of Hinchley Pt. The field upon plantypluts are very large & alms - at the mass is a grayish color. (B) Covered 58 feet broad. At the top in one joint there crop out 3 feet of embedded gray shale containing sparsely Stenocistma of pulchra & ?Actinopterella sp. (C) Over a width of 22 feet above crop out some shales which are similar to ?4.3.2.A² near the top but be - come gray-green, and gray reddish mottled lower down and discolored in the upper part small pea-sized rounded pellets of quartz. These shales are like 4.3.2.A¹ of 1907 and strike N.61°W. dip 32°N.E. (B) Covered for a width of 52 ft (C) Over a width of 115 ft above crop out 55 feet of blue calcarous - shaly massive dark bedded shale. The rock is of a dark blue color, very dense & hard fine grained and contains an abundance of fossils in various stages. The fossils

Halysites sp - occasional Favosites of hemisphere? common Chonetes nova-scoticus [corne]tus Leptostrophia common Stenosclisma pulchra abundant Wilsonia wilsoni abundant Spirifer Erispus [simplex?] small common Whitfieldella(?) or Hyatella sp {common in one seam} Orthoceras sp rare Trochoceras rare Horistoma sp occasional a few of the above were collected 4.3.2 B = 4.3.2 B . Strike N. 54-61° W. average strike N. 57° W. dip 30° N.E., (F) Covered 73 feet broad (G) Measures very black - bedded, dense colored shaly beds of dark blue color - 4.3.2 G similar to 4.3.2 B but with more common & with Halysites pre- dominating rather than Favosites These beds strike N. 54-57° W. and dip 32° N.E., and are 32 feet thick (modal of outcrop 60 ft.) (H) Very dark red shuff, at first sight loose, but showing occas- ionally a quartz phenocryt, and amber silicite fragments. The Top strikes N. 56° W. and dips 32° N.E. . These form the main thug may to 100 ft or more thick

33 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 Defle, Derryville. 4 24' W. S.W. side river bank 5.20' W. of barn, very dark black and porphyry with enalaged fragments (pink & gray) green rock - 275 feet gray fragmentary and porphyry, proof @ 60 A.T.

Quadrille Ruled Form. John C Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 34 Aug. 24, 1908. 1. Gray fragments rhyolite tuff with pink fragments flanked on the east by dark bluish-red rhyo- lite. 2. At S.W. end of section 2 occurs a ledge trending N.W. of same tuff as at locality 1, flanked on east by same dark flow. This flow occupies a width of 120 feet normal to strike (illegible) and is followed by gray quartziferous tuffs with some pink fragments, which extend to within 20 feet of Little Creek. Here a gray flow similar to the base of the gray rhyolite of Hollowell Island occurs. A specimen from rock bed = 4.2.7(1) Quartz phenocrysts less very common. To feet to N.E. the flows a lighter gray & quartz glass common. Specimen (P.S... 4.2.7) is a watertight gray tuff not a glass, which is sparsely fragmental fragments whitish clay). These tuffs continue nearly to the Garden store and then are followed by (3) Exposure of gray and gray-thin dimite glassy rhyolite flow oc- curring in the river & roadway from N. of Garden store to 50 feet N. of large church. over Road Wash/10 4.2.7. 4.2.7(1) 4.2.7(2)

At the clunch, the phylacton the roadway is a dense black in color & is seen to grade upward into a blue-black, blue-gray gray & whitish gray in a space of 25 feet and is followed by whitish gray tufts which crop out 50 ft. N. of the clunch. These tufts contain an occasional pink or red feldspar fragment

35 Quadrille Ruled Form. Patented 1906. John C. Moore Corporation, Rochester, N.Y. Duck Harbor Shale In the little cove on the south side of Duck Harbor, n.w. of the salt marsh occurs a thick series of tuffaceous agglomerates, yellowish gray slag to v gray trap mostly rounded, occasionally some quick fragments. In these agglomerates there occurs a particular pocket of blue-gray slates turned on edge striking N.12°E, 4 feet thick, 10 feet broad. Fossils: Crinoids. Coral (Rugose, simple) Lingula 2 spp Eichwaldia (Chonetes cornutus (small nucicurate)). Orthis davidsoni Dalmanella spp. Leptostrophia expatetta Bilobites biloba Spirifer elevatus Strophonella euglypha 5" radiatus #2 Spirifer simplex Hyolithes Bellerophon # Kronoceras angulatum Murchisonia ? Stenosicisma (small Conchidium) Orthoceras Synphoria Eurychilina # A large globular species with hexagonal reticulate sculpture somewhat like but a little larger than the eye of Dalmanites. #2. Very smooth no pliations; striae crossed by fine funnel.

Reperted C & B Nov 4, 1908 36 Dec ch's oct '12 '08 Quadrille Ruled Form. Patented 1906. John C. Moore Corporation, Rochester, N. Y. 4.24.8 Duck Harbor (4 feet olive shales. 4.24.8 A Crinoids occasional Rugose Coral (simple) " Lingula 2 spp. rare #1 Lophostrophia f. perplana very rare Strophomenella f. Euglypha " #2 ?Chonetes cornutus" rare Orthus f. davidsoni occasional Dalmanella sp Bilobites triloba sternum (im) common swell (on are) ?Eichwaldia reticulata rare spirifer elevatus occasional 5 " craspa var. simplex " #3 5" radiatus " Hyotheca rare Bellerophon " Muricisona " #4 Turbois gastropod #5 Eumorphalus sp Orthoceras sp. Kronoceras angulatum "valent." #6 Siphona sp. occasional Eurycalina sp. 0 #’ A species with coarse flexuous striae of the perplana type. #2 Very small & coarse ribbed (?Orthis davidsoni) #3 Small, no plications, folds sinus & entire surface covered with radiating striae which are crossed under a hand lens by extremely fine concentric striae. #4. f Platyschisma but very nearly flat #5 Whorls contiguous rounded plane coiled #6 With genal & dorsal spine no ? glabellar spine, glabella pustulose. 30 28 26 24 22 20 18 16 14 12 10 8 6 4 2

37 Section from 190 Piece in Y16 & Uniform Section team N.S. Pinnacle Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 30 28 26 24 22 20 18 16 14 12 10 8 6 4 2

38 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 83 2 4 6 8 10 12 14 16 18 20 22 24 26 28 30

Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 39 N° of Summer's Secreter in document from Loos 30 28 26 24 22 20 18 16 14 12 10 8 6 4 2

1. Gray porphyry tuff w/ 1cm fragment of bright pink & weathered palygote. 205 feet broad. 2. Gritty. Rather fine grained trap from amygdaloidal. Width 350 feet 3. Covered (Scarlet valley) 50 feet broad 4A Creamy dark red and tuff. Fragments rather small, pink & reddish black. Strike N 37° W. dip 35° N. E. width 120 feet. At the base are 4 feet of tuffs of dark gray-red tinges w/ in weathering white & minute frag- ments (reddish black) showing on black surfaces or weathered surfaces. 4B Covered. 40 feet in an excavated valley. 4C Dark red porphyry tuff. Strike N. 37° W. dip 35° N. E. Similar to No 4A, charged with large quartz crys & palygorn phenocrysts. Matrix dark red. Rubble dark red. width weather dark color & minute dark bright red. Rubbles very small & much spumous Rock easily mistaken for soft flow. Close jointing N 64° E 4D Also tuff, similar to 4 but the matrix is a general gray in streak of dark red & rock weathers light color typically white. Specimen fine tuff is associated with darker phases turning toward reddish gray 100ft broad. 5. Covered 570 feet half of which is in a depressed sag. 6F Fragmented and tuff w/ fragments.

40 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 large, commonly an inch or over. Fragments more conspicuous than glauconyate fragment mostly dull purple andesite-schistose Cut by 25 foot gables dike trending N. 32° E. Surface color normal, light width 170 feet 4 & Acid Buffs of a dull red-purple forming resisting edges of dark classic looking surface. Fragments smaller dark red purple matrix a duller red purple frequently the stuff no mottled greenish dull red purple commonly there are no feldspar phenocrysts at all width 620 5' Gray basic looking buffs with occasional light pink look and fragment. Matrix mauve gray fragments commonly divided between close of sample color or darker gray. Pink fragments rare. Width 330 feet exposed trending 4° E - nearly to river.

2 4 6 8 10 12 14 16 18 20 22 24 26 28 [illegible] John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 Quadrule Ruled Form.

42 Plain Quadrille Ruling Patented 1966. John C. Moore Corporation, Rochester, N. Y. Shales occurring in the road (see Bastin map) with seams full of Murchisonia. This is below Murchisona zone of Young's Cove. In the south west in 5/1/13 occur some gray shales ( see Bastin map) with Steroscirra v-[illegible] Regiselia = 5/1/1 A not coll 5/1/1 B not coll

Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 5.2.9 A. - Long Cove, Pembrokeshire Neck. G. L. Breger. Coll. August 1907. Notebook 2, p. 86. Pholidops implicata Sow. occasional. Leptostrophia sp. α (near ornatella Salter) rare. U. Ludlow Chonetes nova-scoticus bastini abund. Stenosciuma sp. α (= pulchra Sow. + lacunosa non-Dalman). V. Ludlow Dalmanella sp. α occasional "Retzia (near) salteri Davidson common Wenlock Ptychospira (?) (f. Anabara parata Clarke) occasional Brazil. Delthyris near rugacosta Hall rare Arisaig fig. 3. Grammysia triangular Salter (2043 var's) rare Telestowe Cleidorhorus sp. nov. α " Arisaig (fig.1.) Cypricardella [near laevis Sow] occar. Telestowe. Anodontopsis near angustifrons McCoy " Pterinea (Follmannella) danbyi McCoy rare U.Ludlow. Actinopterella 4 or 5 spp. abundant Pteronitella retroflexa Walcunt. occasional Silur. fig.2. Schizodus sp. rare Goniophora transiens Bill " Arisaig fig.6: Modiomorphα (near complanata Sow.) " U.Ludlow Cyclonema rare Horostoma f. discors Sow. rare Murchisonia (f. articulata Sow.) occasional Murchisonia " Acisina " Holopea rare Orthoceras ibex (Sow. emend Salter) rare. Orthoceras ludense Sow. rare. Calymene f.tuberculata x blumenbachii but smooth common Dalmanites Phacops sp. rare Cornulites serpularis Schloth. (2043 var's) common Conchicolites sp. tenius Sow. very common L. Ludlow. Tentaculites " Spirorbis sp. (free, thick, smooth) rare 30 28 26 24 22 20 18 16 14 12 10 8 6 4 2

(1) Cypricardella: mediocris very depressed. Glossites no medial suture. (2) Grammysara triangularis Sulter var. fig (3) fig. 5. deepressed convex but not so flat as fig 1 (x2) fig. 5 Achisona sp. 4 Murchisonia Beyrichia sp. occasional Crinoids, 3 or 4 genera Monetypa (small, branching) common ?Striatopora sp. rare. Tricoids (narrow, branching; "Butthotrophis") rare.

44 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 5.2.9.B. - Long Cove, Pembrokeshire C.L. Breger Coll., Aug. 1907. Notebook 2, page 67 Orbiculoidea sp. α (small wood, well jointed) R manlins Chonetes novascoticus bastini C Dalmanella sp. α (near orbicularis edgelliana) A " sp. β (ribs finer, more numerous) C Camarotoechia vacuosa Sow. (non-Dalman) C U.Ludlow Grammysia cingulata Hisinger. R Ugotland (Cyrtodonta (1)) sp. videt. R Modiomorpha sp. α (cf. M. complanata Sow. O M. conophora curvata Clarke " " sp. β (cf. Grammysioidea semisulcata Mich.) R Pteronitella retroflexa Wahlberg O Ugotland. Actinopterella sp. O Orthoceras sp. (smooth). R " (Dawsonoceras) sp. (annulated) R Crinoid joints O

45 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 5.2.9.C. Long Cove Pembrokeshire. C.L. Breger, Coll. Aug. 1907 Notebook 2, p. 67. Crinoid joints (small) common Cornulites arcuatus Cours. occassional Conchicolites sp. rare Chonetes nova-scotius bastini common Dalmanella sp. α (near orbicularis-edgelliana) abundant Stenoscisma { lacunosa Sow. nov-Dalen: common { + pulchra Sow. Grammysia academica Bill. rare Arisaig fig. 1st Isooulia sp. (large, depressed crowes)# " Dallhouse's Macroclus(?) baileyi Clarke, var. nov. rare Chapman Pteronitella venusta Bill. " Arisaig Actinopterella (rays very fine, numerous. # of some species from Bolensvian Etage & under "Isoarca" Barrande.

depressa corvul

Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 46 5.2.9. D - Long Cove, Pembrooke Neck. C.L. Breger, Coll August 1907 Notebook 2 page 67 no. 1146. Chonetes nova-scotius bastini common Dalmanella sp a rare Stenoscisma pulchra Sow. "

47 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 5.2.9 E Long Cove, Pembroke Neck. C. L. Preger Coll. August 1907. notebook 2, page 67 Actinopterella sp. rare. very large, slightly oblique, gently convex. sag & wing devoid of ribs; ribs few & faint fused to posterior part of body.

48 Quadrille Ruled Form. John C Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 53.8A. Schooner Coor, Paulroke Rock. B.L Breger, Collector. Notebook 2, pages 48. July 25, 1907. NO BRACHIOPODS. Bellerophon (Tropidodiscus) carinatus Sow. Occas. Bell. "(Plectonotus) trilobatus Sow. Common Platyschisma heliotes Sow. Common Holopea (small, high spired, very Rare very deep sutures). Cyrtodonta sp. Grammysia cingulata common Rare Dilobella (Bollia) sp # Common Bythocypris sp. Occas Pontocypris(?) sp. R Primitiopsis (Sstr. Jours 1887-8). R (smooth, of Aparachites but not anterior vertical partition). # This species is very variable. One variety has two dorsal tubercles with a pit between of the genus Ulrichia. In other forms these two tubercles may curve below into a simple horseshoe (= common type), or may be prolonged dorsally in erect spines like Aechmina. The horseshoe type also develops in old forms a faint vertical lobe fore and aft making a 4-lobed animal of Bollia or Tetradella.

49 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 5.38B Schooner Cove, Pembroke Neck C.L. Breger, Collector July 25, 1967 NO BRACHIOPODS Gastropod gen. nov. (see 5.38 C³) Abundant. Platyschisma helcites Sow Rare Cyrtodonta spindet. (Grammysia cingulata recorded in the field) Rare 30 28 26 24 22 20 18 16 14 12 10 8 6 4 2

Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 5.3.8: G'. Schooner Cove Paulrobs Neck. B L Bregger, Collector. July 27, 1907 Notebook 3, page 52. NO BRACHIOPODS Cyrtdonta sp. α Occas. C " sp Y (high rhombic) Occas. Bellerophon (Tropidodiscus) carinatus Abund. Bell" (Plectonotus) 3-lobatus Abund. Murchisonia (Hormotoma?) sp. Common M " (Coelocaulus?) sp " M " (? Ganiostropha) sp Occas. Platyschisma helicites Sw. Abundant Gastropod gen. nov. (see C³) Rare. Spirobis sp. α Common Dilobella sp. β (only the central Common Bythocypris (?) sp. Rare. Beyrichia sp indet (sp. B). Rare.

57 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 5.3.8. C². Schooner Cove, Penobscot Neck. C.L Breger Collector. July 27, 1907. Notebook 2, page 52. NO BRACHIOPODS. 1. Megambonia? (with wing, devoid of radl. gams as in C³) Rare 2. Grammysta cingulata Shaver Common 3. Cyrtodonta sp α (see C⁴) Occas. 4. C. " sp. B (see C⁴) Occas. 5. Bellerophon (Tropidodiscus) carinatus Occas. 6. Bell" (Plectonotus) trilobatus Common 7. Murchisona (?) Coelocaulis sp. Rare 8. Platyschisma helicites Sow. Common 9. Gastropod gen. nov. (see C³) Occas. 10. Spirorbis sp. α Occas. Vol 2. Gram-triquetra + archer

52 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 5.3.8 C³ Schisoner Cove Pembroke Neck C.L. Breger Collector July 27, 1907. Notebook 2, page [illegible] 52. 1 Bellerophon (Tropidodiscus) carinatus Sow. Abund. 2 Bell" (Pleptonotus) trilobatus Sow. Occas. 3 Bell." (Patellostium) expansus Sow. Rare. 4 Bell." globatus (?) Sow. Rare 5 Platyschisma helictes Sow. Very Common 6 Murchisonia (?) (whorl round devoid of all ornamentation). Occas. Rare 7 Gastropod. gen. nov. # ([illegible]). 8 Grammysis triangulata Sow. Occas. 9 Megambonia (?) (f. erect inflated) radii). Rare 10 Cyrtodonta sp. B. (see 5.3.8 C4) Rare. 11 Spiorbis sp. A Abundant. # A remote high spiraled shell having blade like rim or flange at the sutures. See figure over. It may prove to be only the external mold of the umbilicus of Bellerophon trilobatus.

53 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 5.3.8.C" Schooner Cove, Pembroke Neck C.L. Breger Collector. July 27, 1907. Notebook 2, page 51 NO BRACHIOPODS Grammysia cingulata Hainger Occas. G" triangulata & vars. Comm. Grammysioidea sp. indet. Occas. f3.1 Cytodonta sp. α (elongate, ridged) Com. f3.2 C " " sp. B (shorter, globular) Com. Pteronitella (?) obliqua, gibbous } "megambonia" lamellosa shell, Lower Held. Platyschisma helicites Sow! Comm. Bellerophon trilobatus Sow. Occas. Murchisonia (Hormotoma?) sp. Rare. Gastropod gen. nov. (see 5.3.8C²) " Spirorbis sp. α Abundant. 5." sp. B (lugey, annulate, resembling Rare. achignud joint in external weld) f3 Leperditia sp.{ high; no eye spot on cast Rare muscular pit central Dilobella ? (Bollia) sp. Rare. #Holopella sp. #Bellerophon carinatus Sow #. Recorded in the field notes

gibbosus agtodonte Oleaster 2 3 globular x 2 5.75 mm F. 2.32.9A the outline is that of Primula (Uparchites) muricata Eichw. see Jones 1890. cf. also Leperditia parallela Schmidt

54 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 5.3.8. D Schooner Cove, Pembroke Neck. C. L. Breger, collector, July 27, 1907. Notebook 2. p. 52-53. Orbiculoidea sp. B Common Lingula sp. (large) Rare Chonetes nova-scoticus bastini Occas. Modiolopsis sp. a rare Clidophorus ovatus Sow. Common Cypricardella sp. B (see 5.3.8 F.) Rare Isoculia (cf. 5.29 C.) Rare. Actinopterella sp. Rare. Hyolithes sp. Occasional Cyclonema sp. (same as E) " Orthoceras ludense Sow. " Beyrichia kloedeni pennsylvanica & Occas. B." tuberculata f. æquilatera A " Bythocypris sp. rare

Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 5.3.8 E. Solisone Cove, Pembroke Neck. C. L Breger, Collector. July 30, 1907. Notebook 2, page 55. Orbiculoidea sp. B. Chonetes nova-scoticus bastini Dalmanella sp. a occasional " abundant. Nuculites (Clidophorus) ovata Sow. rare Ctenodonta sp (same outline as preceding, but without septum ) " Modiolopsis sp. A Actinopterella spp midst common. Hyolithes sp Murchisonia (?Goniostropha) sp " rare " occas. M " (Harmotoma) Cyclonema (high spiraled ? mid tent, swell for riblets to alternate ) Common Orthoceras punctostriatum Hall. occasional, arisay. Tentaculites tenuis Sow. rare. Beyrichia kloeberi var pennsylvanica J Cow B" tuberculata var of aequilatera H. occas B" " var of above, but tuberculat. Rare Bythocypris sp. occas.

Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 56 5.3.8.F Schooner Cove Pembroke neck. B. L Breger, Coll. July 31, 1907. Notebook 2, page 55, 56. Lingula (subgenus nov.) sp.nov. near striata Sow. R. U.Ludlow Orbiculoidea sp.B Conc Chonetes nova-scotica bastini R. Dalmarella sp. a Very Abund. Stenosisma Stenoscisma? + pulchra Sow Occas. U.Ludlow Nuculites (Clidophorus) f ovatus, Sow. non(?) Hall. Conc. Arisaig Tilestones. f.s.(Cypricardella sp.B R. mor "Modiolopsis" a (= platyphyllus Salter, varum) A. U.Ludlow " a var alpha (= m exilis Bill.) C Arisaig Actinopterella 2 or 3 spp C. (Cyclonema (coarsely striati; high) Murichisonia (Hormotoma) sp. pateilostrium) Bellerophon (Pinnulites) expansus Sow. # R Delicate? Holopella sp. indet. RO Hyolithes sp. O Orthoceras punctostriatum Hall R Arisaig O. (Dawsonoceras). elegantulum Hall (perelegans Salter) O Arisaig. O f. myrice Bill. R Monticulopora #2 sp. a (large, arborescent) Avistlam. " sp. B (like a but encrusting) RO Monotrypa sp. (small). O. Crinoid joints & columns Serpulata sp. R. Beyrichia sp. B tuberculata var equilatera H.) K. #2 over * Note very fine wrinkled markings under lens of, Phragmostoma natator.

moderately covered strongly marked #2. Monticulospora - Large, arborescent, 1 cm or more thick. Clusters of cells a little larger are scattered among the normal size but not elevated.

57 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 538. G. - Schooner Cove Pembroke Neck. C.L. Broger Collector July 31 1907 Notebook 2, page 56. Orbiculoidea sp. B Chonetes nova-scotica Hall Dalmanella sp. α (very variable) Stenoscisma(?) sp γ (24-26 highly elevated ribs no fold-sinus; ribs not sulcate. Spirorbis (?) sp. β (spire elevated, distal, whorls angulated. Resembles recent). R Valvatea. Crinoid joints (small) C Catenipora sp. ? indet. K

58 Quadrille Ruled Form. John C Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 5.38. H Schooner Cove Pembroke Neck. C L Breger, Collector July 21, 1907. Notebook 2, page 56-57. Monticulipora sp. a (see 5.38 F). A Hindia fibrosa Sow. C Chonetes nova scoticus Hall R. Dalmanella sp. a occa. Stenoscisma pulchra Sow. C Actinopterella (cf. 5.2.9. E) . R Cornulites serpularius Schloth R 30 28 26 24 22 20 18 16 14 12 10 8 6 4 2

59 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 5.3.8. K Schooner Cove Pembrokesh. B.T. Breger Collector Aug 1 1907 Notebook 2 page 57 58 Orbiculoida sp. B occasional Chonetes nova-scotius Hall rare Dalmanella sp. α abundant Stenoscisma { lacunosa Sow now-Dalman common + pulchra Sow. Grammysza cingulata Heilinger rare M. 1311 "Modiolopsis" sp. α (platyphyllus Salter, var.) rare Actinopterella sp. occa. Cyclonema sp. indet. rare Orthoceras ludense Sow. common. O. (Dawsonoceras) f. { dimidiatum Sow # rare L. Ludlow f. americanum Foord Gurfele Cornulites serpularius Schlth. rare Crinoids see figures over. occasional # possibly a gigantic Cornulites over 3 meters long. 30 28 26 24 22 20 18 16 14 12 10 8 6 4 2

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60 Quadrille Ruled Form. John C Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 5.3.8. L. Schooner Cove, Pembroke Neck. C.L Breger, Collector, Notebook 3, page 59 August 1, 1907 Crinoid joints (small) common Orbiculoidea sp. B. rare Chonetes nova-scotica bastini " Dalmanella sp. a abundant Stenoscisma sp. Y (see 5.3.8. G.) occurs. " {lacunosa Sow. non-Dalman common, piperidulus {+ pulchra Sow Nuculites (Clidophorus) fovata Sow. nov? Hall R. "Modiolopsis" sp. a (platyphyllus Salter var.) C. " " sp. a var. alpha (= exilis Bill.) O Actinopterella 3 or 4 spp. O (Cyclonema sp. a (same as 5.3.8 F')) O Murchisonia (Hormotoma) sp(" ) O Orthoceras ludense Sow. O D."(Dawsonoceras) sp.indet.(?annulatum) R Cornulites sp. (large of bellulus). O C " serpularius Sow. O Dalmanites sp. a R Calymene sp. B(pygidium very finely tub- O erculate or punctate, not smooth; of C. Blumenbachi) 30 28 26 24 22 20 18 16 14 12 10 8 6 4 2

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Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 5.3.8. L² Schooner Cove, Pembroke Neck. L.D. Breger, Collector August 1, 1907. Notebook 2, page 59 Dalmanella sp. α Abund. Stenoscisma lacunosa Sow. von Deluv. Abund. + pulchra Sow. Modiomorpha sp. undet. Rare Orthoceras ludense Rare Dalmanites sp. Rare Vioa .sp. (ou Orthoceras). R Crinoid joints (minute) Common.

Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 5.3.8. m! Schooner Gorse Pembroke Rock C.L. Brerger, Collector, Notebook 2, page 61. August 12, 1907 Orbiculoidea sp. B. Rare. Lingula (subgen nov.) sp. nov. occasional Chonetes nova-scoticus Hall Abund " bastini Wauss Br. A" Dalmarella sp. α A" Stenoscisma flacunosa Sow. non-Dalman very Common. + pulchra Sow. "Macrodus" cf. baileyi Clarke. R. Dallmais Modiolopsis sp. α A " var. alpha R. Modiomorpha sp. indet. R. b.g. Cytherodon Billings. R. Arusaig Actinopterella 3 or 4 spp. A Pteronitella retroflexa Walcott. R Murchisonia (Hormotoma) sp. Oc. Cyclonema sp. indet. R. Orthoceras punctostriatum Hall R. Arusaig Dalmanites sp. (finely tuberculate R Calymene sp. (finely tuberculate) R. Beyrichia [strobopolbina] cf. freuteri Kr. Occas. Arusaig Beyrichia kloedeni var. academica Jouse " Dallhoser. " " 3 or 4 var's (mostly pennsylvanic) Abund. Bythocypris sp. indet. Very Common. Cypridina sp. indet. Rare. Cornulites serpularius Schloth. Oc. Tentaculites tenuis Sow. very common Trachyderma (str.), sp nov near coriaceum Phillips R. Planolites sp. R. Crinoid joints (small) A. Fish scales (marked with close set wrinkles of Lingula, subgen. nov. R

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63 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 5.3.8 M² Schooner Cove, Pembroke Neck. C.L.Bresger, Collector. August 12, '07. Notebook 2, p. 61 Orbiculoidea sp (large). Oc. Lingula (subgen. nov.) sp nov Oc. Chonetes nova-scoticus Ab. " " bastini Ab. Dalmanella sp α Ab. D. " sp. β (striae much more numerous) R D. " sp (very near orbicularis Sow) R Stenoseisma lacunosa Sow non Dalm. very Com. S" pulchra Sow Oc. " sp γ Nuculites (Clidophorus) sp flovata Sow. R "Isoarca" (Barraude) sp undet. R Actinopterella spp. Com. Phacops(?) (?Dalmanites) round pygidium R Calymene sp (very finely tuberculate) Oc. Beyrichia kloedeni var acadica Com. " Bollha 3 or 4 vari Ab. Dilobella (?) sp nov ftriscatus Com. Beyrichia maecoyiana Hall Oc. B. (kloedenia) granulat Hall. Oc. Coymans Bythocypris sp. Ab. Pontocypris sp. Oc. Cornulites serpularius Schloth Ot. Tentaculites tenuis Sow. Com. Crinoid joints (small) Com. Fish scales (cf. 5.3.8 M²) R.

6p Quadrille Ruled Form. John C. Moore Corporation, Rochester, N.Y. Binder and holes in leaves, each Patented 1906 5.38 m³ Schooner Cove, Pembroke Neck S.L. Berger, Collector Aug. 1,2, 1907. Notebook 2, page 60 Chonetes novascoticus Hall Abund. Arisaig " " var. bastini " Dalmanella sp. α " " sp. β (ornamentation finer) coin. " " sp. γ (cf. sp. β & very near orbicularis Sow. Coin) Stenoscisma { lacunosa Sow. nov Dalman Abund. U.Ludlow S. " + S. pulchra Sow occas. sp. γ. Grammysia cingulata Heinsius R "Leptodus" pembrokensis Billings Oc. Nuculites (Clidophorus) f. ovata Sow. Oc. " (C) sp. β (more elongate & strie stronger) R " (?) sp. (gen indet. straight hinge of Arca) R Actinopterella 2 or 3 spp. very Common Pteronitella retroflexa, Wahlenburg R Cyrtodonta (depressed convex sp.) R Cypricardella f. laevis Sow. R. Modiomorpha 2 spp. Occas. Modiolopsis sp. α Abundant Paracyclas f. quadrata Salter Occas. U.Ludlow Goniophora transiens Bill. Arisaig. Ctenodonta sp. (see fig. over) R Hyolithes sp. Oc. Murchisonia (Hormotoma) sp. Oc. Cyclonema R. Bawsonoceras f. elegantulum Hall Arising. Arseaig. Orthoceras punctostriatum Hall R Bellerophon expansus Sow. (brown slit band & sinus wth R spiral striae) Dalmanites (finely tuberculate). Occas. Primitia mundula Jones R Kloedenia f. granulata Hall. "R Beyrichia penns: kloedeni var. mccoyiana J. De Abund. B" " kloedeni var. pennsylvanica R. B" " var. acadica Jones 30 28 26 24 22 20 18 16 14 12 10 8 6 4 2 OVER

Comm. Beyrichia tuberculata var (aequilatera) Hall. Com. B. " maccoyana var Jones. Com. Bolha f. trisulcata Hall. Com. Cytherellina siliqua Jones & var's Very Common Bythocypris Occas. Pontocypris Common Tentaculites tenuis Sow. occas. Cornulites serpularius Selloth. Common Crinoid joints

65 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 5.3.8 N (1136.) Schooner Cove, Pembroke Neck C.L. Breger Collector Aug 2, 1907 Notebook 2, page 61. Chonetes nova-scoticus occasional Stenoscisma pulchra Sow. common ?? Dalmanella sp. α Rare Actinopterella sp. occasional Tentaculites tenuis Sow. rare Cytherellina silva Jones occasional Bythocypris sp. o "

(Quadrille Ruled Form. John C Moore Corporation, Rochester, N. V. Binder and holes in leaves, each Patented 1906) 538. O. Schooner Cove, Pawtucket Neck. B.L. Breger, Collector, August 1907. notebook 2, page 62. Sternoscisma lacunosa Sow. (rev. Dall). C. U. Lubbock, (moderately convex, but not globular; 5 ribs or folds, 4 on sinus, 5 or 9 on each side; ribs imbricate; fold x sinus moderately well pronounced). (cf. F. mainensis Billings, pauciplicate forms, but Billings species has the ribs flatter & lacks the imbrication).

67 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 5. 3. 8. P<sup>1137</sup> Schooner Bow, Pembroke Neck C. L. Berger, Collector August 1907 Notebook 2, page 63. Stenoscisma sp. y. Occasional.

6327B - The hundred and fifty feet or so of dark blue thin shales of 6421 m, A, and 6327A are overlain by 50 to 100 ft. of very light gray shales in which scattered fossils may be observed but which surely no means common. Different species turn up at the time and it is possible that a very large fauna could be collected. In an hour and a half or thereabouts two were observed: Camarotoechia common Lingula (2 spp.) R. Orbiculoidea O Whitfieldella R. Meristella bella K. Nucula? (cf. Anodontopsis bullata, Gy) occas. Cypricardinia of platyphyllus X ocas. Goniophora (small R Pterinea danbyi' (small) R. Dalman(?) sp. R Edmondia (flattish ?) R Orthonota (short, high) occasional Hypothes sp. common ? Chetetes p (? Dalmanella) occasional Murchisonia (round whorled) R. I think this may be above Schroner even more been before June 10/11

69 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 5.22.9.A Falls Point (west side) C.L Breger Collector August 21 '07 Notebook 3, page 16. over note 1 Orbiculoidea sp. Rare " 2 Leptostrophia Common " 3 Strophonella " " 4 Chonetes Rare " 5? Dalmanella sp. X Common D " sp. W. " Wilsonia wilsoni (very large) Very abundant Aymestry " 6 Stenoscisma Common " 7 ?Atrypa reticularis (?Dalmanella) Occas. Aymestry, Lower Cyrtinopsis crispus Sheinger Rare Mytilarca (?Plethomytilus) sp. Occas. Pteronitella retroflexa Walil (small) Rare Pterinea (Tollmannella) danbyi McCoy. Occas. Actinopterella hians McCoy " Aymestry Actinopterella "reticulata" Sow." nov. Rhe. " Aymestry Act. " 1 or 2 additional spp. R. Notes: A "(?) (_____) sp. R. Crannysioidea(?) sp. R. Polytropis near carinatus Sow. R Aymestry Pleuromaria (?) f. Polytropis rugosus Sow. R. Lower Ludlow. " 9 Orthoceras (Kionoceras) near virgatum Sow. Oc. " " " 10 Trochoceras (Sphyradoceras) " trochoides Barr. Oc. Aymestry. Calymene sp. (sparsely tuberculate). OC. ??? Dalmanites (recorded in field notes, not observed, probably a Calymene pygidium.

Note 1. A small species with distant sharply elevated lamellae. Note 2. Leptostrophia near Ornataella but the ornamentation is finer & more fasciculate. Note 3. A gently convex species, with orna- mentation varyingly fasciculate. Note 4. A wide species smaller than C. nova-scotica, and more closely striate than the young of C. nova-scotica. Note 5. Two or three species of Dalman- ella are here included, all of them distinct from the Silsomes Cove form: One species shows a strong rumenlature in pedicle valve resembling Schizophoria. Note 6. Near S pulchra Sow. but with stronger dental lamellae. Placations 18-18 angular on interior subrounded exteriorly. Fold seems merely not developed. Rarely 3 median ribs elevated into fold. Note 7. A very finely plicate almost striate form, if this species: Possibly a coarse Dalmanella. Note 8. Without radial ornamentation but having a very strong concentrically ripose ornamentation. Note 9. A species having the principal ornamentation vertical flutings about 1 mm apart in normal adults and at over 25 on surface no finer inter- fluting. In the young stages cancellations are present of which there are no indication in the adult. Note 10. A Prochoeras with slightly elevated spire ornamentation as in Barrande's species but the longitudinal flutings are slightly less pronounced in our shell.

70 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 5.33.1:G. Falls Point. Pembroke Neck. C.L. Berger, Collector August 10, 1907 Notebook 2, pp. 73, 74. Crinoid stem Rare Chonetes nova scoticus (?) (rather coarse) " 30 28 26 24 22 20 18 16 14 12 10 8 6 4 2

71 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 5.33.1: K. Falls Point, Pembroke Neck. G.L. Brager, Collector August 10, 1907. Notebook 2, page 73-- Orbiculoidea (a finely beIIastriate form). Common Lingula (subgenu) of tæniola H.B.C. Rare Chonetes (smallish & very coarse). Occasion Dalmanella of a " Stenoscisma sp indet. Actinopterella sp. indet. Rare Dalmanites sp. (listed in field). Rare ?Tentaculites sp. (? crinoid stem) Rare Crinoid joints Common

72 Race Pt July 6. In the core west of Race Point gabbro outcrops continuous along the southeast and east shores and in the hillback on the land. The northeast point of the Core is com- posed (porphyritic gneiss) abyolite trapp only rarely contain- s a few fragments. These form the North Shore of Race Point excepting the east corner where gabbro again comes to the shore. There is also a dike of gabbro near the East corner, the dike trending N. 20° E. The east shore of the Point is composed of the same massive porphyritic and trapp as on the west shore. A thick mass of gabbro interrupts this series. North of this gabbro area which is in S. W. 5° 34.4' to the stubby dip shore in some of the porphyritic trapp, the strike varies from N. 13° W. to N. 20° W., dip 33° - 36° E. respect- sively. Of the two little points on the south side of Race Point, the east one is composed of gabbro with a shooting of porphyritic the east shore and a bit of addituff at the S.W. corner (Sdb) Diabase) 9 to 20ft

73 5. 33. 8 Scales appear a little over 100 yds. w. f. south of the house of Mr. ____ and galbro formerly the hill to the north. The gables comes down to the shore and forms the west prong of the little point in s. e. corner of 5. 33. 8, and the galbro is continued into a long ledge reef along or on the C & G S. chart. The little corals between the two prongs shows no outcrop, except on the east side where 10 [illegible] ft. of sediment dep under silt ho N. 30° W. and dip 30° under a mass of very coarse galbro. The residuel breccy and distinctly coaly fine grained. The limestone scales are scattered in many seams of fossil. This zone appears to be the same as that occurring at the head of Douglity Cove in 5. 54. 6. the fauna include Lepetena rhomboidalis abundant Leptostrophia common Chonetes cornuta common Dalmanella 2 spp. common Stromatisma cf pulchra uncommon Wilsonia wiltoni occasional Spirifer crispus common S" ", elevata Atrypa reticularis occasional Actinoptarella hiants trans common A" reticularis. occasional Tollmannella danby rare

Dawsonoceras (?) sp. Kionoceras sp rare rare Dalmanites sp occasional Calymene sp ''

74 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 July 6, 1908 Forming the west shore of the Cove to East of the Cliffs 5.33.8 B. of Mr. ---- are a series of Exposures of this gray shale only slightly splintered and containing an abundance of fossils. The shale strikes N. 12° W° and dip 33° E. About 60 ft. are exposed The fossils occur in seams and (?) of "Chonetes V Planus" cervia (?) stenocerna (3) Paracycles. Paracyclus is common throughout the fauna included: Lingula 2 spp rare Orbiculoida 2 spp rare Leptostrophia 2-3 spp rare Leptena rhomboidalis common Chonetes novascoticus rarer Ch "cornuta" abundant Dalmanella sp. occasional Steposcerma (?) plechra abundant Wilsonia wilsoni occasional Retzia barranderi rare Spirifer crispus occasional A Cleidopora ovatus Sui Crinim

Pteronitella retroflexa rare Belerophon (P.) expansus Sowerby Euomphalus (low spired) rare Hypolithes rare The shells are cut by a fine grained gallery or coarse trap like trending N.40°W.

75 533.9 Race Point of the tip points forming the south part of Race Point, the western out shows outcrops of gray & grayish-blue shale on the southwest & south sides, sup- ported by a couple of miles of and plunging N40°E., which form the extreme S.E. tip of the point. Work of clay by the shales strike N. 28° W. and dry 33° E. N.E. They contain Dalmarella Stenoscisma Wilsonia rare occasional "" One very fossiliferous seam contains: Dalmarella (remnants) Spirifer crispa (Euell) abundant Atrypa retic. podder coarse & Almondont large/ Crinoid joints (large) common On the south side of the point, the shales strike N 55° W. for a short space.

76 5/43.2 280 long point extending S.E. in 5/43.2 is composed of a back bone of galatro projecting out at the end of the point where it is flanked on the west by some fragmental acc. truffs. Overlying the galbro are some very hard, coarse grained or sandy chells only rarely showing bedding. The strike varies from N 15W to N 32 W and dip 20 N.E. the average strike parallel to the shore. These whole, contain what appear to be fossil canalis but no fossils yet recognized they underly some light gray or pinkish fine siltstone which which appear below lalf tide level. In the galbro appears in a dice offset from the main mass at the upper 6th. and as the upper quarlier appears a thin 3 foot dike of trap which shows clawerene columnar structure. The thin trap dike trends N x S. There are no outcrops in the long core extending to west 5/43.2 nor in the core in N.E. 5/43.2.

Coffin Neck. 77 Quadrille Ruled Form. Patented 1906. John C. Moore Corporation, Rochester, N. Y. Coffin Neck (1) The east shore of Coffin Neck beginning near N boundary of S 44-3 is formed of a gray & gray white rhyolite tuff usually dis- tinctly fragmental frequently appear- ing glassy. There is flanked on the east by a coarse diabase dike which occurs inside the high land line & comes to the shore at the little point north of the brook in S.W. 34-9. Tray To the north of this bed mass there follow a series of sed- iments about 100 ft. thick forming the second or middle point just west of the letter N in "Nutter Cove" of these sediments the lower 50 feet are gray dust-glasses alternating with blue gray fine crystalline tuffs & some little splintery blue shale. These are followed by 12 feet of ridged basic tuffs of sandy texture. These lower 62 feet contain: Stenosirema (not lacunosa) stump Dalmanella (coarse) common Spirifer crispus rare Actinoptrella " Orthoceras " In the twelve feet of coarse tuffaceous shales occur along with the Stenosirema a few specimens of Wilsonia wherin.

Overlying the sandy-textured beds with Wilsonia, Stenoceras, cutintrap some 35 feet of blue- grey shales containing 5.34.9 C Chonetes nova-scoticus occae. Leptæna rhomboidalis rare (Leptæna) Dalmanella (large) . occae Stenoscisma (large). common Spirifer crispus occasional Paracyclas sp rare, Beyrichia kloeden, common " æquilatera occasional Kloedenia Cytherellina siliqua " The strike of these sediments is N. 50° W. dip 32° N.E. The shales of 5.34.9 C are overlain by a trap intrusion which forms the hill N.E. corner of Coffin Point, [illegible].

78 Coffin neck (2) In the west of the trap mero there occur on the north side of Coffin neck some gray grit tuff (macara?) overlying distinctly loose bedded tuff. These slates 40-40 and recur on the second point on the east side of the core in 5.34.8. the west side of this next point is composed of acid tuff and the west side of the core is composed of reddish acid tuff & bluff tuffs. At one locality on the west shore of the core the tuff tuffs are rather argillaceous & exhibit mud balls - 5.34.8 (1) west The acid tuffs continue all along the north shore of Coffin neck. On the east shore of the west point little coral is in 5.34.7 very are about 10 ft & fossils - are numerous & containing an abund- ance of fossils, chiefly wilsonia wilsoni abund Stenoscisma? samoas " = 5.34.7 Dalmanella 5.34.9 B.C. " A Chonetes cornutus " occasional LEPTOSTROPHIA ORNATELLA SPIRIFER CRISPUS RETZIA BARBANDEI

"The rhyolite tuffs continue all along the west shore of Coffin Week, interrupted in a dozen or more places by coarse diabase dikes. East of Gooseberry Island, a couple of hundred yards north of a little diabase island there occurs on the west side of Coffin Week an exposure of some 30 feet of blue gray splinty shales ? 32.30 underlying gray white clay tuff and shutting off to the north against a diabase sill which forms the west flanks of the 80 ft. hill in 5.44.3. Possibly collected here on the occasion of Prof. Williams visit = chiefly Dalmanella Sterrocrina, Chonetes nova- cornutus or cornutus Parrylos & small lamellibranchi. A couple of seams in the shale exposed mostly below high tide contain an abundance of ? Atrypa reticularis moderately coarse ? Lopstena rhomboidalis Leptostrophia Chonetes cornutus Wilsonia etc etc 5.44.3 A (new) 5.44.3 A2

79 5.44.9 A. Coffin The south shore of [illegible] Cove neck is formed by a series of acid tuffs striking N. 140° W. at the west end and N. 22° W. near the east end. These are frequently bedded and on the east shore of a shallow cove (near east edge T 5.44.9) occurs some 20 feet of tuffaceous fragmentiferous shale, with some tuff bands containing fossils. The fauna includes: Chonetes cornutus common Leptostrophia ornatella rare Dalmanella ? spp abundant Stenoscisma ? spp "" Wilsonia wilsoni common 5.44.9 Sphyradoceras rare Cornulites occasional Calymene "" Monotrypa abundant Monticlipora common Retzia barrandei common

50 Superficial Crossed striae Coffin M. On the south side of Coffin Neck just north of the South line of T. 45, Y there occur some of crossing glacial striae. The striae occur on a coarse diabase dike which has been Roche- mountained into a low near flat ridge. The common-est striae are trend N. 42° W. These are crossed by a series of less frequent striae which Trend N. 55° W. while both are crossed by a rare series of striae trending N. 35½° W.

81 Lyons Neck (1) 5.45.1 Out the east side of Lyons Neck A m N. 5. 45.1 about 40 yards worth of the brook outcrops 3 feet of gray rhyolite tuff overlain in area 40 ft. broad at the base of which are exposed 6 or > feet of blue shale. V 10.35. Total shale probably 21/2 ft. thick. Fossils in seams in the shale include Dalmanella abund Stenoscisma pichra comm. Orbiculoidea occasional monotrypa "/" 5.45.1 a The shales are overlain to the north by an exposure of some 17 ft. of rhyolite tuffs (massive) and Ellen outcrops a ledge of 6 ft. of blue shale forming the shore line A 3.35 This shale contains the same ware Dalmanella abund Stenoscisma occ. Orbiculoidea "/" monotrypa "/" Actinopterella rare 5.45.1 B. The northerly strike brings (A) to the shore again and just north of the S. boundary of 5. 35. 7 the strike N20 V 20.350 brings both A B and the tuffs into outcrop once more. In 5.35.7 the south of the joint is a strip about 100 yards wide in which of which outcrop some 35 or 40 ft. of shales of 5.45.1. B. Out the point there out- crops a trap intrusion bounded 5.35.7

on the east by some 50 feet of bedded basaltic tuffs v35.37 v24.40 overlain opposite the island by clear shale interbedded with tuff seams 6 or 7 feet of these shales outcrop v40.37 = 5.35.7 containing A Balvanella abundant Choustra bastini common Steroschema " pulchra + lacunosa " Nunclersonia Similar shales with the same fauna 5.35.7.A outcrop in the west side of the islands off the shore The main mass of these islands is composed of a very coarse reddish argillite tuff massive. Both tuffs & shales are cut in the east & west by trap 5.35.7A2 (not coll.)

82 Lyons Neck (2) The shore to the west of the island is formed by some basic tuffs while the East shore of the point ni 5.35.4 is composed of trap the main mass of the point's west side is composed of ceded and x semi-acid tuffs which also form the tiny island ni s.e. 5.34.6. The point to the s. of this island is composed of massive trap which extends with the 80 ft. hill at the N. end of the neck. The south side of the point shores (near west end) a couple of feet of contorted shale strike nearly east-west dip north. I In the little cove common to northern 5.34.9 - 5.44.7. occurs a series of exposures of acid tuffs & shales. The little point on the line shores on the east face 25 feet of massive acid tuffs overlying and grading down into 10 feet of blue shale. The upper part of the shale contains fragments & grades into the tuffs & this part contains few Dalmanella's & Sterosserina = (not coll). The shales proper form the tip of the little point sand are very highly fossiliferous containing 5.34.9 A' not coll. Dalmanella abundant Chronetes costini occasional Sterosserina spulchra lacunosa very common monotrypelle " " Murchisonia common 5.34.9 A Asriostoma rare actinopertella 28 26 24 22 20 18 16 14 12 10 8 6 4 2

"There ten feet of shales are underlain by a 7 foot mass of acid tuff and next to this west is a mass of shale 33 feet thick occurring in the tiny little cove in 5.34.9. These shales contain the the same fauna as 5.34.9 A Dalmavella abund Stenoseriura very common pullevia lacunosa The sharp point in N.E. 5.34.9 is a mass of trap. To the west of this point occurs a series of alternating shales x thin tuff x tuffaceous shale bands. Some of the tuff bands are several feet thick; usually gray acid. These alternating tufts x shales, cut by intrusive masses continue as far as the cove in S.W. 5.35.7 where a uniform mass of a couple of hundred feet of shales occurs. The fossils in the shales, 5.35.7 B. of these series are mostly Dalmavella & Stenoseriura same as N. E. 8 sides. 5.45.7 B not coll.

83 Lyons Week (3) the core running into S.W. 544.7 is flanked on the S.W. by nearly 100 feet of acid & similar tuffs with little shale & trffaceous shale. These tuffs overly a galbo intrusion which forms the hill. Another thick rhyolite tuff near gray-white, massive, ocure on the west flank of this trap was forming a strap about 250 ft. broad along the west side of Lyons Week

5.35. 5 A. Orbiculoidea sp. rare Lingula (complanata type) " Chonetes denysi Camarotoechia sp. " Cypricardinia "platyphyllus" occasional Actinopterella sp. " Dawsonoceras sp. Rare Orthoceras (of O. myrice type) " Coleolus (? Onchus spine) Phthonia sp. rare

85 Plain Quadrille Ruling. Patented 1906. John C. Moore Corporation, Rochester, N.Y. 5.35.5 B. Orbiculoidea occasional Lingula rare Camarotoechia " ? Dalmanella " Murchisonia (round-whorled, rare but common in a seam a foot below the turffe. m" sp. B. (angular whorled rare ? Holopella (? imperfect Murchisonia?) rare

Plain Quadrille Ruling. Patented 1906. John C. Moore Corporation, Rochester, N. Y. 5.45.3 A¹ Dalmanella 5.45. 3 A² ?Hindia fibrosa (?Chonetes) abund. Dalmanella rare Camarotoechia rare ? Spirifer ? vanuxemi occas 5.45.3 A³ Camarotoechia abundant Chonetes denysi "." Dalmanella "." Actinopterella occasional Cypricardinia "platyphyllus" rare Cyrtodonta (large) common-abund. in seams Cornulites Occasional etc., etc.

Quadrille Ruled Form. Patented 1906. John C. Moore Corporation, Rochester, N. Y. 87 5.45.6 The 120 foot [illegible] in 5.45.6 is composed of a mass of coarse diabase in which is caught up a narrow strip of bedded rhyolite glass tuffs or "petro-silex" which is fossiliferous. The sediment me about 25 feet thick, outcrop just north of the road on the S.W. side of the hill & strike N-60° W. dip 35° N.E. The fauna includes an occasional Actinopterella occasional Stenoscisma " Murchisonia " Crinoid stems Fossils scarce Along the north shore of Loring Cove there crops out in S.W. 5.45.6 a thickness of 25 feet of slanting gray shale >25-30 underlying ~ 1/5 foot <X35-30 light colored gray white and buff which in turn underlies the intrusive trap. Fossils very abundant in the shales including Chonetes bastini abundant 5.45.6 Dalmanella " B. Stenoscisma common Actinopterella occasional Crinoid stems common

58 5.55.3. In northern 5.55.3 just northwest of the curve of the inlet a thick (25 ft.) trap dike comes down to the shore. There is followed to the east by about 10 feet of rhyolitic tuffs and about 40 ft. farther east in a conspicuous ledge [illegible] tuffs (massive). In the interval between the and x lassic tuffs crops out some couple of feet of gray shale holding Dalmanella (Schroederi Conc) Abund. Chonetes bastini occasional Stenoscisma sp. " Orbiculoida sp. " Crinoid stems " The strike is N. 10° W. dip 40° E. These splintery gray shales reappear at the south at the angle of the inlet forming a tiny waterfall and at this point the trap dike appears to the east of the shales. 5.55.3 A

89 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 Hallowell Island Surface Geol Rock Rock extremely fine sand

90 Near the boundary of 5:51, 4 the shale is formed for about 10 yds. along the line of strike of some sediments. These strike N. 22° W., dp. 28°-30°. The rock is a couple of feet of banded shale weathering in banded agglomerate fashion and underly a couple of feet of monotonous shale. The top of the first contains at one place a cluster of Conchidium knighti, while a couple fads of the same occur on the same surface & a few inches higher the same form as 5:51, 5a. The fossils observed here are: Plectambonites occasional Leptena rhomboidalis common Chonetes cornutus Dalmanella (conn.) occasional Stenoscisma cf. acinus common Wilsonia wilsoni occasional Meristella (new large) " Atrypa rugostriata-marginata " Spirifer crispus small " Kionoceras myrice rare Favosites ?pyramidalis " These shales appear to overtly a base flow which occurs along the left side less than fifty feet back from the shore. If this be so, the shale probably fill the gap between the two brooks. See section 5:51, A 5:51/4 Sediments of Edmunds formation. Conchidium knighti 5:51,1 A not collected

Quadrille Ruled Form. John C Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 Aug 5, 1908 5 250 brook 400 brook 5.51.5 Eld. 51.5 13' <- 200 yds. horizontal: 1" = 20 ft vertical 1" = 10 ft The point in S.W. 5.51.5 is composed of a thick galbee mass trending N 55°E and mills on the opposite point N.E. of the latter Run Burnet Creeks West of this is a series of sediments which may be traced for a distance of 305 ft. normal to the strike, until near the brook occur some light gray amygdoloidal diabases; the adyaz dip. 62° (35°-40°) 37° giving a thickness of over 160 ft for the shales exposed. These are massive bedded, striking N. 52° 10° W. dip East. 190 feet east of the top of the trap flow occur some 6 feet of highly fossiliferous sediments which are exposed at K below high Lodi Foreels very abundant? includs Plectambonites (Caye) common Leptrena rhomboidalis " Strophomena sp. occasional Strophellla g profunda " Leptostrphia sp rare Chonetes cornutus occasional Dalmanella (varae) common 5.51.5 A 28 26 24 22 20 18 16 14 12 10 8 6 4 2

Stenoscisma sp frequent occasional Wilsonia wilsoni " Conchidium knighti rare Gypidula galeata common Meristella sp common Atrypa reticularis occasional frugiculus marginata " Spirifer crispus (small) " Ctenodonta sp rare Cyrtodonta sp " Actinoptereilla sp occasional Kionoceras myrice rare Trochoceras " Calymene sp rare Dalmanites sp " Rugose coral rare Cornu? ?h common Spirorbis sp rare Halysites sp rare

Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 Aug. 8, 1905 On the east side of Burnt Base 5-57-5 just south of Birmingham Nat. there occurs a cliff of rocks striking N. 22° W. dip 32° N.E. which may be the equivalent of the Wilson Stream zone at Drungville &. The rock is well bedded thick banded very fine grained, dense light siliceo-calcareous kind of a light gray & gray blue color showing in places a little undulated gray shale. Fossil are abundant in several seams one of the seams about 2 foot from the top of the fossil lime bed is an intermittent 0-3 well coral reef of Polyartes as at Drungville. The entire forms of these beds (which are 200 yards east of A) include 5-57-5- Chonetes cornutus (small) Leptostrophia ornatella (small in situ), Strophomena Dalmanella g edseliana D. (of Rhipidomella) sp. Stenoscisma of acrus Rhynchonella stricklandi Wilsonia wilsoni (common band) fura Spirifer elevatus Hyatella or Whitfieldella sp Cammysia cingulata (large) Pteronidella retroflexa Modiolopsis sp murelisoma ? Spirra ductata Natalis, Leuthim & corla. B 13 R. f. Com " " Rare Common Occasional

Horistoma sp Tentaculites sp rare rare The f[illegible]ferous rocks underly light-gray fine grained tuffs which compose the lower buff of Birmingham Mt. on the west side: at about 150 A.T. these rocks are over laid by acid looking fragmental tuffs (specimen 5-51.5 [3]) while the top on the west side is composed of loose tuff. Along the east of the mountain there is an exposed step 170 ft broad trending with the strike N 35° W. (dp 30° N.E.) and apparently indicating shale. The rocks on the east side of the mountain are loose tuffs. Specimen from the hill top = 5-51.5 [1]

93 Quadrille Ruled Form. John C Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 The fossiliferous sediment of 551-5 B - as exposed more fully near the 551.5-8 line where over 50 feet of them may be observed striking W 54°, and dipping 37° E. They underlie a modern gray fragmental and tuff over 50 feet thick. A couple parallel faults re-expose these shale down to the joint in N.W 551.9 551 F 84 phygy phygy fragmental 32-37° F F 551-9 550 19,37 22,52

Aug. 7, 1908 On the west shore of Burns core there occurs on the S. side of the point in central 5. 51. 8. a finely amygdaloidal rock of finely flexured or fault fractured. Further south nearly 100 yds. on the south side of the corelet the fault brecciated zone continues, while with the development of a caliche zone, nearly a foot thick trending N. 70° W. This amygdaloidal rock continues along the shore and is occasionally covered with coarse sandy fluvial- course sediment often con- taining black fragments. The amygdaloid is frequently banded. The amygdals are in linchets not in bands. The sediments over the amygdaloid contain fossils chiefly Stenoscisma also 5. 51. 8. Dalmarella occasional mytharca occasional A. calyptone occasional Halyzites (flora) common the fossils may be collected West & southwest of the little island

95. South Point, Carrys' Place Core Quadrille Ruled Form. John C. Moore Corporation, Rochester, N.Y. Binder and holes in leaves, each Patented 1906 On the west slope of the point extending (confined) of Military Bay) now from 8.2.3 into 5.52.9 there occurs a thick mass of the groundmass stuff which are blue changed field of dark silexite plate fragments. The fragments are half an inch to 2 inches in thickness and usually of a very dark purplish color. The porphyritic stuff extend about three fifths the distance N.W. from the head of the little core to to in 8.2.3 to the joint in 5.52.9 where and in their under partly by a series of laked smalls or Cornstove flags which display good bedding for a thickness of 40 feet and are underlainly assumed an equal thickness of unbedded silted shales. The shales are of a gray to a light blue color band in the lower part of the stratified portion contain an abundance of fossils in several strata. The fauna includes Crinoid joints Occas. Striatopora Rare Orbiculoidea sp. Rare Leptostrophia ornatella Occas. Chonetes cornuta Abundant Dalmanella sp. Common Wilsonia wilsoni Abundant 5.52.9 5.52.9 A

Spirifer crispus occasional Pteronitella retroflexa Common Follmannella darbyi (unothyr) occas Actinoptere lle sp. occasional "Nuculites Rare Modiomorpha (myfuebelle strate ) Rare Murichisona (Hormotoma) sp R. Dawsonoceras perelegantula Rare Dalmanites sp ocas. These abales are underlain by "granitoid" tuffs, and both are cut by a coarse basic dike which forms the point in S. W. 57-52-9. The fossiliferous shells strike N. 60°W. and dip East 35°45°.

96 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N.Y. Binder and holes in leaves, each Patented 1906 Carrying Place Cove On the Southeast side of Carrying Place Cove passing into Wintertown there occurs west of the point in western 5-53-7 and passing recently into 5-52-9, a fine series of exposures of shales. The upper few feet are thin, fine-grained, indurated beds similar to 5-52-9 A and contain a similar fauna, Unknown etc. This fauna not collected, except a single specimen of Bellithophora (globular form), Strike N. 40° W., dip. 35° N. E. These tough indurated shales overlie a series of more profile shale in which slaty cleavage was dominant over the bedding. Strike of cleavage N. 40° E., dip. 60° S. E. These shales are cut by a basal dike extending N. 30° E. The entire shale series may be 250 feet thick and just east of the point overlies a series of dark indurated slick-bedded shaly limestone containing grains of feldspar, glimmer-cysts, etc., and several seams full of fossils occur here. And thick bedded sediment etc. and include a very varied 5-52-9 C fauna. Wilsonia Leptostrophia spp. Chonetes cornuta C" bastini? occasional but abundant in a seam, lower down [illegible] ?Strophonella Dalmanella Rhudland Very Common Common Rare Rare

Stenocystma sp. (Ludwiga) common 5" very large (gamoplicate) occasional Spirifer crispus Day small " " elevatus " Helmquayella dautyi rare Otivintelle retroflera rare Actinoptrella rare Paracyclas occasional Oriostoma junatua occasional Henrotumaria rare Euvampolins (smooth, low-spine) rare Orthoceras long. rare Dansonverrea dividiatum occan Trochocerus rare Forsetia occasional Helophyllium common Neonistrops occasional Encrinatus Puyozae Rare Delimausti occasional Placops rare Colymen rare The cryptate porphyres underlying this foralifer or sediment show flow structure in places

Quadrille Ruled Form. John C Moore Corporation, Rochester, N. Y., Binder and holes in leaves, each Patented 1906 Straight Bay July 1 '08 The east shore of Straight Bay from the core ordering 5.53.6 - 5.57.4' to the west 4th of the square is com- posed of ledges of gabbro alternating with shale, the gabbro predominating. The shale is irregularly folded and appears to have the structure of massive wedges within the gabbro. In eastern 5.53.6 the strike is N. 35° W., dip 35° N.E. In middle 5.53.6 the strike is N. 18° W. dip 37° E. From the west quarter of 5.53.6 southeasterly to the south quarter of 5.53.5 5.53.5 the east shore of the beds of Straight Bay is composed of gabbro.

"Carrying Place Cove Quadrille Ruled Form. John C. Moore Corporation, Rochester, N.Y., Binder and holes in leaves, each Patented 1906 5-53-7 A on the south edge of 5-53-7 there crop out some tough indurated dark blue shale striking along the shore line N x 5° W and dipping 26° to the East. These shales for about 15 feet thickness overly 8-3-1 A and contain a fauna of chiefly Spirifer crepus (small) & Dalmanella. The fauna 5-53-7 A include: Brinoid Joaote Occasional Dalmanelle Common Cleiostra cornuta occasional Pholidops simplicata (?) " Latta Stereocisma of Acina Rure Spirifer crepus (small). Common Dalmanites occas. Orthoceras lindera (?) " Stria topora R. Grammysioolest. R. # The strike swings around from N 5° W on the south to N 2° E on the north. Following the strike of 5-53-7 northward we find that the shales remain rather below are softer plated. These softer slaty shales form the first point in zonalism 5-53-7 and strike N 5° W and dip N 85° E, 28°. The slaty cleavage strikes N 32° E and dips southeast about 45°. Fossils indistinct same as 5-53-7 A till Atropa reticularis added. Continuing northward the shales still appear slaty with strike N 5° W. Dip 28° E. Slaty cleavage chiefly N 35° E, dy 50° SE. These shales contain fossils at a locality about 1½ to ¼ mile up.

99 5.53.78 the second joint fossils: the fauna the being the same as 5.53.7A except that the Dalmanella & Spirella are rarer & Atrypa abundant Pholidops implicata R Chonetes cornuta R R common Dalmanella (?) Atrypa reticularis R. Loxonema (?) Orthoceras

100 5. 53. 7 C June 30, 1908. On the east shore of Barry's Hole Cove Southwest of the Grove Neck School occurs a long exposure of thick series of friable shales with occasionally a black indurated layers. The shales are dark blue in color strike N. 23-36° W. and dip 23°-42° (average about 30°) N.E. These shales, excepting the more indurat- ed layers are severely slated or splintering 'the platy planes extending N. 45° E and dipping 60° S.E., Fossils are discernible in the shale even where thinly slated and include Orbiculoides sp. Rare Chonetes cornuta Common Steroscisma f. pulchra Occasional Spirifer crispus (small) Common Kronoceras sp. = Rare Small rapidly tapering, nine flutings: Horizontal strata: The fauna revere Chonetes, Spirifer x Steroscisanae scattered throughout the shales. The fauna collected is mostly from the little cove in N.E. 5. 53. 7

101 5.54.2/3 Dougherty Point The tip of Dougherty Point is a massive very coarse grained gabbro the east margin of which trend N. 50° W. It is flanked on the east by shales which extend to the tiny Coveley opposite the letter "D". The strike of these shalies sweeps around from N. 15° E. thru N. 5° E. to N. 30° W. at the southern end. The dip is 37° N.E. These shales underly a series of massive labeled blue shales sloping inderectly extending as far down the east side of Dougherty Point as the letter long west of the letter "O" in Cove. The strike is N. 30° W. in the upper portion becoming N. 42° W. over the major part. Westward down Dougherty Point the west side as far as the E. spurs of 5.54.2 a massive gabbro underlay which there drop out at three points some 30 feet of gray fossiliferous shales striking N. 50° 10° or 15° E. respect from N. 55° and dipping East at an angle of 37°. Fossils are most abundant in the central area about 125 yds. south of the Ledge reefs and show a fauna of 5.54.2: A H.E.R. 30 28 26 24 22 20 18 16 14 12 10 8 6 4 2

Chonetes nova scotica another with Stenosisma of borealis, and a third with Stenoscima & Wilsonia. The entire fauna includes 5. 54, 2A Chonetes nova-scoticus. Abundant. Dalmanella f. edgelliana common. Stenoscisma of borealis very common. s. "" of pulchra (larger) common. Wilsonia wilsoni common. Spirifer crispa large rare. Follmannella danbyi common. Actinoptarella sp. rare.

102 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 5.54. 3 Doughty Cave. The west side of Doughty Cave is made up of massive indurated olive shale which rarely show folding. The two ridges are roche-moutoneed but in the hillside about the old Doughty homestead the splintering of the shale is well shown trending N. 50° E. The strike varies from N. 30° W. in the north getting to N. 42° W. in the middle & back to N. 30° W. at the head of Doughty Cove. At the head of the Cave just west of the little brook a few forams was collected: Chonetes novascotiensis occ. Dalmabella less common Stenoscisma of borealis " " The same species as are common in the 5.54.2 shales. These indurated shales are overlain by still more indurated shales exceedingly hard and very fossiliferous, but unfortunately the rocks too much baked by an overlying gabbro sill and roche- moutoneed to warrant collecting. A few fragments were chipped off. 5.54. 3 B Butterfaune include so far as observed in the field: Leptæna rhomboida 1/3 abundant Stenoscisma of psilra common Atrypa reticularis less common 2 4 6 8 10 12 14 16 18 20 22 24 26 28 30

Wilsonia wilsoni occasional Trochoceras sp (large) rare Kionoceras rare The strike is N 28° W. Dip 33° NE

Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 103 57-54-2 The point at the junction of 57.54.2-5-7-2 is composed of compact exposed slabs of massive ledges of phyllite porphyry-truff showing in place, stratification, striking N.30°W. This is overlain on the east side of the little point by thin egg-blue phyllitic flags, and the rounded point joining the junction of 57-54-2-5 occurs some caked slate-blue shales near the southeast corner of 57-54-3 occur some more caked blue shale seen striking N.35°W.

104 Quadrille Ruled Form. John C Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 July 1, 05 In the little cove to northwest of the house we saw black some blue slated shales appear east of the little stream. The strike is here N. 10° W., dip 35° N.E. The shale are of a dark blue color with a few gray bands and are black bedded & splintered. An Outglenas was observed. At the brook in the southwest corner of the cove a very coarse diorite intrusion is found. Northerward shales form the west shore of the cove. 100 yards north of the Brook the strike is N. 5° E., dip 34°, E. This strike is continued northerward to the n.w. corner of the cove, just back of the west shore there runs a gabbro- diorite intrusion in places moderately coarse grained, elsewhere more course and coming to the shore in places. It is not more than 25 feet thick. On the shore in N.W. 5.54.4 appear some very dark black bedded shales occasionally with dark fragments & at first sight resembling basic tuff. These are interstratified with gray phyllite lined shales & with ordinary blue splintery shales, a black (SPh) layer of tuff with rounded thin shale fragments as far as I can also appears. In the gage in the little cove bordering 5.54.4 - SPh occur outcrops of gabbro trending N.35° W on the east contact = The point extending from 176?

5.54.7 up until 5.54.1 is composed of fine grained non amygdaloidal trap overlying very dark blue exceedingly baked shale. The latter strikes N.20° W. and dips N.E. about 30°. In the south-west corner of the core in N.E. 5.54.7 this underlying shale strikes N.25°W.

Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 105 July 1, 1908. 5.54.6 Near the southwestern corner of the Cove west of Dougherty Point occurs a bottle patch of gray & grayish blue shale striking N. 36 E. and dipping at a slight angle about 24° to the East. Slight splintering is well developed, thc cleavage being N.50°E. Fossils were here, they are distorted & difficult of extraction but the fauna 5.54.6A show. 5.54.6A Lingula sp occasional Valmanella " Steroscisma pulchra common Pellmannella danbyi rare (or a large actinopora) Crinoid joints occasional Following up down Straight Bay along the west shore of Dougherty Point we find dark greenish shale, baked. The strike indistinct but apparently N. 40°W. These shale are too much sweared to contain determinable fossils, but a crinoid joint was recog- nized. As the little brook occurs, a thin gabbro sill trending N.55°W and north of the brook occurs a thick series of massive shales containing large feldspar phenocrysts and some fossils which show ( 5. 54.6 B) Chonetes cornuta common Delmanella sp occasional Spirifer crispus (minute) rare Normotoma sp occasional over

Another collection about 30 yds. North above a similar form with the addition of (? ) Wilsonia wilsoni & Bellerephon trilobatus 5.54.6;C.

106 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 6. 5. 568 A² Broad Cove, Eastport. C. L. Breger, Collector. August 26, 1907. Notebook 3, page 2. Buthotrephis sp. Common. Lingula cornea? Sow. Rare. = Symmysella cheloni? ? or ?? Anodontopsis angustifrons Mc Coy. Abundant. (Cypri cardella) sp. (fig over). Occasional "Lophospira" (Streptotrochus?) incisu Lindstrom Common Highest (tall variety of Lindstroemi sp. Silurian of Gotland) Tetradella sp. (see 3.44.4A). occasional Drepanella? (Tetradella ?) same as very abundant. figs. 45; 3.44.4A

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see maps, both sides of pasted page 17, book 2 see notes, Notebook 2, p.28, 34 109Y 1093 1092 6.24.7.B 6.24.7.A 107 In the little cove in the middle of 6:24:7 occurs a mix- ture of acid and basic intrusives in shales and limestones. The so-called acid is specimen 1092, diabase dike is 1093, mutual relations not ascertainable. On the west side occurs a "Granite sill" arkose band of quartz and pink feldspars) in the limestones. The arkose is cut by a thick diabase dike of the same lithic type as 1097. A fault probably runs diagonally across the dike, as shales are brought up on its southwest side, striking N.35 degrees E., dip ZERO-1 degree E., and these flat shales but against limestones striking N.35 degrees East16 and pitching to the west at an angle of 70 degrees. The diabase dike forms the west shore of the little cove a18 far as the point of the main shore. On this point and to the west occurs a little cliff or shale striking N.5-10 degrees East, and dipping only 6-11 degrees to the west. The shales up under a coarse diabase dike. The sediments here include, at the base, 12-15 feet of very friable gray shales with ex- tremely sheftered slaty cleavage, and without gelseous mat- ter. These are followed by 20 feet of massive, thickbedded shales directly under the gabro dike. In the thin, shattered lower shales, there were found a single Ceratocystis (Large Beyrichia?), and a single Lemnibranch (oblique Pteronit- ela, or Teleotertia. These two specimens are 6:24:7.(A). The OVER OVER 30 28 26 24 22 20 18 16 14 12 10 8 6 4 2 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 3/12/80

These shales may be more fossiliferous, but are too much shattered to show any other spec- imens. The more massive upper shales are quite fossiliferous, and contain several Beyrichia species and a low-spired Naticoid gastropod. These fossils are 6:24:7:(B), and the entire fauna includes (coll.1908) Beyrichia tuberculata.............common Beyrichia salteriana .............common Platyschisma helicites ............common Lingula minima...................common Grammysia sp.......................occasional Pteronitella sp....................rare Leiopteria sp......................occasional cf. Pterotheca sp..................rare (?)Leperditia sp..................rare

108 1107 1108 1109 6:24:7: C The point forming the southeast shore of the little gove in central 6:24:7 is composed of a series of better limestones of which there are exposed about 60 feet. These limestones show a strike swinging around from N. 25 degrees west to N. 65 degrees west in traveling northwestwardly, and continuing a few yards to the west we find some gray shales striking East-west and dipping North. The shales dip under the limestones, in case as seems probable, there is no fault disturbing the relations. The precise contact between shales and limestones does not show, the interval being covered, ex- certing for the outcrop of an intrusive diabase sill (1193) West of the little shale outcrop mentioned we find an abrupt change in the strike which indicates a fault trending N. 20 degrees west. The shales were nearly flat, striking N. 20 degrees west and showing an anticline with dips of 10 degrees to both east and west. This anticline is local and- arently confined to the vicinity of the fault plane as the shales in the southeast corner of the gove strike N. 35 degrees east and dip east 15 degrees, and on the west side of the gove the shales again dip N. 35 degrees East and are flat. The gove appears to be a triangular wedge of shale cut off on both east and west by a fault plane. The specimen 1092

Along the east portion of this wedge and instead of being an acid in trusive is a light colored glassy arkosic mud, massive, unbedded, and apparently about 20 feet thick. It contains in the lower quarter a seam one to five inches thick in which Bastin discovered Platyschisma helicites in abundance and large size, - over an inch thick. The seam also contains some large lamellibranchs with Cyrtodonta-like dent- ition and resembling Megalonus in outline altho the precise outline is only very obscurely preserved. These fossils are C:24:7(C). This band of rock is tuffaceous, - inclosing small angular fragments of pink rhyolite, and rounded pebbles of half an inch thickness (1/4 to 1 1/4 inches) of gray rock, cf. limestone (?). Below this, the rock resembles the fine grained freestone bands of Birch Point in lithol- ogy. A specimen is 1107. Above it the rock is mottled and includes bits of pink rhyolite, equals 1108. Specimen 1109 is the diabase dike on the northwest side of the cove.

109 Federal Harbor 6.41.7 6.41.7 A - A quarter of a mile west of the south tip of Federal Harbor and west of the road, on the line between 6.41 & 6.51. Stratigraphically about 600 ft. or more below 6.41.8 F. Camarotoecia abundant Chonetes denysi abundant Dalmanella common Grammysia cingulata var. occasional Actinopterella 2 or 3 spp. common Pteronitella retroflexa occasional Goniophora (2 spp.) ", Cypricardinia "platyphyllus" ", Ctenodonta (2 spp.) ", various Camellibranchia common Myrchisonia 2 or 3 spp. ", Corbulites rare Trilobites (Dalmanites or Calymene) rare.

110 Federal Hth 6418A Plain Quadrille Ruling. Patented 1906. John C. Moore Corporation, Rochester, N. Y. 6.41.8A... rhyolite fume tuffs... [illegible] abundant foot 150 feet Camarotoechia abundant Chonetes denysi common Dalmanella (Schoner) (ntype) rare (common in one or 2 seams) Cyrtodonta abundant Actinopterella rare murchisonia rare Platyschisma occasional Tentaculites " Crinoid joints common. This is a Schooner Cove shale fauna commingled with the Platyschisma x Cyrtodonta fauna of the Schooner Cove gastropod-Carnellibranch beds. 6.41.8A underlies 6.41.5a by about 60 feet stratigraphically

Plain Quadrille Ruling. Patented 1906. John C. Moore Corporation, Rochester, N. Y. Federal Harbor 6.41.8 B Cypriocardinia "platyphyllus" common 6.41.8 C.- Actinopterezza rare. 6.41.8 D.- Dalmanella common Camarotoechia R Orbiculoidea R Actinopterezza O Orthoceras fluidense R 6.41.8 E.- Dalmanella common Camarotoechia sp R. Cypriocardinia "platyphyllus" occasional Orthoceras f. fluidense rare 6.41.8 F.- Dalmanella occasional. Various faunas at the west end of Federal Harbor in descending order stratigraphically. all except B are below Ar. III 6,41,8 B-7

(12 Federal Harbors 641.5 Plain Quadrille Ruling. Patented 1906. John C. Moore Corporation, Rochester, N. Y. 641.5 A. 35 feet of shales stratigraphically about 60 ft. above 641.8A, and beneath the rhyolite flow Dalmanella (Schoneer Cregeensis) abundant Camarotoechia common Orbiculidea occasional Actinopterezza common Cypricardinia (?) "platyphillus" occasional Murchisonia rare Cyclonema rare a typical Schooner Cove shale fauna. This immediately underlies the rhyolite lava flow, of Federal Harbor region stratigraphically; a gabbro sill intervenes geograph- ically. aug 27 07 now 641.5 diff that both sides abt falling in center

Horan Head Plain Quadrille Ruling, Patented 1906, John C. Moore Corporation, Rochester, N. Y. Horan No. 6.42.4 A-D 6.42.4 A. - Murchisonia sp. rare 6.42.4 B. - Leperditia abundant about 25 ft. below 6.42.4 A. 6.42.4 C. - Cyrtodonta sp. rare of Schooner Cove Gastropod- cancellibranch beds species immediately overlying A 6.42.4 D separated from C (overlying) C) by 200 ft. and r. basic tuffs Camarotoechia 2 spp. abundant Spirifer vanuxemi common Chonetes denysi rare Dalmanella rare Orbiculoidea rare Choetetes (cf. Monotrypa furcata) abundant Favosites rare Calymene common Dalmanites occasional Actinopterella occasional These underly a couple of feet of phylolite tuffs and then after gabbro intrusion there appear some purple basic volcanics between 2 pumaceous traps. The rocks overlying these basics are 6.42.1 M, 6.42.1A, 6.32.7 A, 6.32.7 B.

Horan Deal, Plain Quadrille Ruling. Patented 1906. John C. Moore Corporation, Rochester, N. Y. 114 Horan 18/1 M.+A 6.42. / M. Immediately overlying the purple lassic & jurasic are 150 feet of dark blue thin shales a couple of feet immediately over the jurassic contain a few rugose corals and Favorites together with 6.42./M the latter occurring through the basal 20 ft. of shales and including Dalmarella common Whitfieldella very common Camarotoechia occasional Lingula rare Orbiculoidea rare Actinopterella occasional. --------------------------------- 6.42./A. In the hundred & thirty or more feet of thin dark blue shales above M, fossils are very rare. 6.42./A in the lower part of the shales was found a round whorled Murchisonia & an Orthoceras 6. 73.7 A. In the upper part occurs a few Nucula (Ctenodonta) around & a Hypotheca rare. -------------------------------- 6.42,1 Zuff mill. ? Baltaerts 148w 6.42,1

115 Quadrille Ruled Form. Patented 1906. John C. Moore Corporation, Rochester, N. Y. 6.44 2/5 At the head of the core running north thru 6.44.5 into 6.44.2 occurs a series of exposures of fossiliferous shales overlying intruded rhyolite & underlying intrusive trap. The rhyolite is exposed on the west side of the core & is of a greenish & bright salmon pink color & exhibits beautiful flow line structures - Specimen 6.44.2 (1). The flow lines are very variable in strike & dip from point to point. The shales are exposed to best advantage at the head of the core on the east side. Strike N. 7° W, dip 48° A E. About 33 ft. are exposed here but the total thickness of shales to the trap intrusion on the east is probably over 200 ft. The shales are gray in color & are characterized by a vast abundance of Lamellibranchs. These occur in such profusion as to literally compose the bulk of the rock for thicknesses of as much as 2 feet. The lamellibranchs are of only 2 variable forms "(1) Grammysia, (2) a concentrically stratified (non-ribbed) Actinoptrella", or oblique, eared Pteronitella. The sediments are flanked on the east by the trap which forms a lovely escarpment in the east side of the core. Over

The lamellibranch beds of 6.44.2 A are quite evidently the same as those occurring on Serui Island & the southwest. The fossils of 6.44.2 A occur in their normal position, i.e. convex side of the shells up, showing that these strata are not overturned.

116 Quadrille Ruled Form. Patented 1906. John C. Moore Corporation, Rochester, N. Y. 6.45. 7/7 Second Week South of the Canal on the east shore there occur flanking the trap mass which forms the hill, a series of limestones & overlying shale. The limestones are exposed for a thickness of about 100 ft along the shore & in the hillside below the house of Mr. Van Morton (For strike & dip see map). In this thickness the limestones predominate over the thin black shale partings. The limestone is of a lead gray color, rather con- cretionary or rather centumlar in aspect some of the bands clining in & plunging out. The fossils in these limestones include some Peyrichias & a peculiar furcoid. 6.45. 7 A. Over the limestones to the north occurs a series of exposures of shales of a dark bluish color & characterized by the oc- currence of thin limestone bands (thick or less) frequently at every foot or less. About 290 feet of these shales are exposed here gute evidently belonging with the series of similar shales exposed S. of the North Arctic Ferry wharf. 6.45. 7 The fossils in the shale & thin bands are and include Tetradella clarkoi sp B Leperditia sp.

Plain Quadrille Ruling. Patented 1906. John C. Moore Corporation, Rochester, N. Y. 6.526 A Spirifer vanuxemi common 6.526 B. Spirifer vanuxemi common " f. cyclopterus abundant " "elevatus" occasional Chonetes f. cornuta " Dalmanella rare Orbiculoidea occasional ?Sphyradoceras (?Dawsonoceras) rare Calymene occas.

(18) Plain Quadrille Ruling. Patented 1906. John C. Moore Corporation, Rochester, N. Y. 6.52.8A, Spirifer crispus vanxemi f " but larger Dalmanella (in clusters) Camarotoechia Chonetes cornuta occas. Wilsonia saffordi occas. Pholidops sp common Crania rare Calymene rare Dalmanites " ? Pterinea danbyi " Sphyradoceras sp occasional

119 Plain Quadrille Ruling. Patented 1906. John C. Moore Corporation, Rochester, N. Y. 6, 53, 2 A. (C.L.B. 347) very Cyrtodonta(large) abundant

7238A 120 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N.Y. Binder and holes in leaves, each Patented 1906 July 29, 1908. [illegible] [illegible] Columnar fossils of Peg Lake District. B. =7.23.8 A [illegible] large morista f.5.51-5ta [illegible] [illegible] [illegible] [illegible] [illegible] [illegible] [illegible] [illegible] [illegible] [illegible] [illegible]

Halls mill 121 John C. Moore Corporation, Rochester, N. Y. Quadrille Ruled Form. Binder and holes in leaves, each Patented 1906 7.41+ ? 9.9.1908 G F Gravel Halls mill Bregan's notes on fossils from Halls Mill, along the stream be- tween Rocky & Orange lakes. Later col- lections by E.S.Baith are from approx. the same beds. E.S.B. 12/21/10, a. 12 inches dark gray sandstone b. 6 inches whitish gray mud full fresh foldpar c. 7 ½ inches dark gray shale (the A) but less sandy and in the upper half as a 1½ inch layer of dark purplish thin shale with fossils. Fossils - Stenoscisma stenocima with rbs 18-20, round no fold nor seams, no lamellae. of moderately large size. d. 3 inches brownalgrnk fdeparthere - crust agglmerats e. 7 inches light general gray indurated muds f. 4-7 feet of dark gray buff mud dock blue chalk fragments. g. measure along the flow between the lower foot or so smothering into horizontal lands about an inch thick. 6 feet express.

7418 122 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 trap founds 5 = five feet Pholidops implicata (camellose) rare Orbiculoidea Leptostrophia Stenoscisma sp pulchra common sten. multiplicata rare Wilsonia wilsoni rare Spirifer cyclopterus tutwil occasional to stults Atrypa retic of aspera common Grammysia cingulata rare Mytilarca sp rare Actinopterella sp rare ? Pleidophorus ovatus rare Gastropods & Enonysphaloid rare Bellotopion sparcia " Corrugates arpelarene Cornoid joints common Peyscilia occasional the atrypa punice found at the northeast corner of Orange Lake E of south of Picketwood Mountain she rock is a dense fine grained silicene, silystate mud of gray color overlying the trap intrusion which forms the Mountain. See trap is intended between the forsnifurn beds & the silystone flinty tuffs found at the various of the lake to the west [over] 74184 Orange Lake D: ilorus isolitym N. E. Lake Orange Lakko. Classified by Breger as Edmunds. E.S.B.

On the eastern island in T.41.7 occurs rhyolite flow trending N.5°W, and the same flow occurs on the point on the south side of the Lake here trending N.5°E. This flow dips under porphyritic gray rhyolite tuff which occurs on the west side of the point in central T.41.7. Next east follow the trap intrusion forming Richardson Mountain, and then comes the fossiliferous sediment. About 10 feet of these are exposed striking N.55°E. and dipping 30°, S.E. Then after covered interval about 75 feet broad crop out three feet more of fossiliferous sediments and these dip under a mass of fragmental tuffs.

7426 123 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 July 2 1908 A few rods east of the dam at the head of Roaring Lake, there occurs on the south side of the highway an exposure of thin gray shaly shale flanked on the east by a distance above the shale and underneath a rhyolite flow and inset a massive volcanic converting of more shale, rhyolite flow & tuff, then flows over a thick base lava, with a length of underlying tuff across the visible underlayment and tuff, rhyolite & acid flow. Ingers for details see section: see 8-5 13 notes on 7426, 7423, 7431, 2, 4, July with, 1908. The entire series strikes N. 20° E. and dips East about 40°. The fossiliferous gray shales in this highway contain: Lingula "striata" type Rare Orbiculoidea sp. " Chonetes cornutus Common Leptostropha ornata Common Prophonall (?) sp. Rather Rare Leptana rhomboidae " Stenoscisma cf. acinus Common vilsonia wilsoni Occasional Spirifer crispus (var.) " Atrypa reticularis Rare Meristella(?) sp. " Teronitella retroflexa " Eumphales (?) sp.) Occasional monotypella sp. Trails of Edmunds formation at Roaring Lake. 7426:4

Simple rugose coral Dalmantites sp. Crinoid joints Tentaculites sp. Hyolithes sp. Race ty Very common rare rare The Wilsonia is confined to a seam. The Leptostrophina are abundant in one seam. The fauna is very similar to S 21.1 A on the Wisting River and also to the strata west of Race Point.

124 Aug. 3, 1908 At the head of the inlet near the mill occurs a large mass of gabbro over 100 yds. broad exposed at and near the end of the mill on both side of the pond and on the west side of the inlet S of the mill. This is flanked on the west by a couple of feet of tough blue shales striking N. 38° W. & underlain by basal looking tuffs visible on the north side of the mill pond in the woods. The tuffs here strike N. 25° W. Y dip 28° N.E. The shale reappear under the gabbro on the west side of the inlet striking N. 25° W. & dipping 26° N.E. The tuffs beneath appear on the point S. N.W. S. 1. 5. Drop & gabbro form the shore down to the road except for some dark looking rhyolite tuffs caught up in the bed near S.W. edge of S. 1. 5'. A thick strike trends across the road N. 70° W. dip along the shore, N. 70° W. brought down of the new bridge appear some and tuffs striking N. 12° W. & dipping E. 25° Bell's Mills 8. I. 4. 5

125 6/13 B2 + c Aug 7, 1908 The acid tuffs overlying S 1.6 A continue in a thick unbedded mass along the east side as far as the tiny core no. of the middle of S 1.3 where a series of banded stuccaceous sediments occur striking N 25 to 40° W and dipping NE 30°. On the west side of the corelet are observed a few bands with only Wilsonia - while both sides of the corelet are formed by about 75 feet of slightly sandy gray shales in which contain on the west side some Wilsonia? [complicate large] collectibles S 1.3 A unbedded S 1.3 B On the east side of the core beneath a mass of galber which form the point at no. S 1.3, the shales contain no Wilsonia's but instead common Leptostrophia elongata, wavelitus, "Chonetes cornuta common Spirifer var [x]crispus small), var simplex occasional Hypolithes sp Dalmanites of downinga rare Calymene sp # A couple of seams in the shale on the west side above the Wilsonia's con- tom Chonetes cornutus occasional S 1.3, B2 Dalmarella sp common Stereocisma common Wilsonia wilsoni (common) Spirifer crispus (small) , occasional Actinoptrella sp. rare (not seen) Hem

126 8/1.6 Aug. 7, 1908 On the east side of Gravel Point occur some very dark red & some gray fragmental tuffs which contain dark fragments of a dark gray & black color. These tuffs appear to be basic & specimens are S. I. 6 (1) & (2). At the same time the tuffs contain a large amount of pink rhyolite fragments, many of which exhibit flow lines: A specimen approaching more nearly an and tuff is S. I. 6 (3). After an unexposed interval of 150 yards, there occurs at the N.E. corner of the cove some 8 or 10 feet of gray shale with an abundance of fossils, chiefly shells of Chonastes cornutus & nova-scoticus, with steposcisma & some coarse Dalmanella; these resemble the Schreiner Cove series but a closer search revealed the presence of Wilsonia in a couple of bands, & also Spines of cyclopterus (5 mbr. on the side), a very large Tullmannella danby (concentrically striate), & Aviculopecten S. I. 6 sp. These Chonester zone shells are 50-54.2 on the west side of Gravelity Point. A couple of faults of 50 to 100 feet displace the succession somewhat but above the shale are 5 feet of rather laked or rhyolitic sediment and then comes a thick massive cliff of acid porphyritic fragmental tuff.

This now appears to be recorded in sandstone shales, but on Burnet Creek on the S.1.2-3 line the red tuffs reappear & again on at S.E.5°51'.8 the south side of the little cove at which latter locality the red tuffs are overlain by some beds of bedded and stuff. striking N.20°W. dip 30°NE. These red tuffs are 50 feet thick and intervene between the lower tuffs & shales. purple

8/18 Aug 4, 1908 In the extreme N.W. corner of the core near 7 well point can exposed cone 6 or 7 feet of tough blue shales which along with the other beds exposed in the core strike N 10-12° W and Dip 26° E. A thin gallo sill veins beneath the shale, and next below over a series of exposures of about 25 feet of very dark rhyolitic trapps. The shale at the head of the core contain fossils which consist almost exclusively of small new coarse bryozoa. 8/18 A Hill Gr 127 8/18

Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 Aug 5, 1908 1. Thin bedded argile shale, dark blue in color. Strike N 60° W. Dip 26° E. Three feet are exposed in the slungy just below high water mark & it is possible that the core west of the Field Point is eaten out of similar shales as the just outcrop to the west are also in this shale, 175 yds distant (s. l. s. A Aug 4, 1908). The shales on the west side of Field Point show fossils tho these are rather efficient of extraction. The fauna includes Lingula sp rare Orbiculoidea sp rare Chonetes cornuta occasional Leptostrophia sp " Sfenoscisma sp common Palmanella sp rare ? Wilsonia spilsoni rare Paracyclas sp Common Actinopterella sp occasional Norm Orthoceras rare Orthoceras " Hoplithes 2. Overlying s.l.s.B are 15 inches of dense fine grained light gray lunds in a single massive bed. 3. Then overlying are 14 inches of friable dark blue shale similar to s.l.s.B. and holding the same fauna. (Not collected) s.l.s.B³ 4. Thin follows a thick series of massive fine grained light gray lunds which are occasionally ale

"[illegible]" Landed a few pieces of fragmental tuffs, strike N 6° W & dip 26° E. These form the bulk of the cliff on the west side of the Point. Fossils are found in several bands 8/1/86 W. [illegible] Stenoscisma g pulchra Common Wilsonia p. [illegible] less common Dalmarella rare Herostoma occasional rare Cornulites (large) In one place where for a distance of some ten feet the rocks of B show thick bedded cleavage planes striking N 52° E & dipping 35-5° E. These might easily be mistaken for the dip bedding planes. 8/1/86 is 48 feet thick and is overlain by a 40 foot series of fragmental tuffs which show bedding only in the upper portion; these tuffs form the point and the upper surface strikes N 8° W & dips 27° East. A two foot band of hard indurated shale occurs 5 feet below the top. The upper five feet are massive

Aug. 5. Above the coarsely fragmental massive buff till probably 8 1/8 fragments follow to the east some 8 feet of banded or laminated gray x bluish black sandy shale with a couple of 3 inch bands of small gray fragments. Three form the south end and 1 the large group of Field PT. and strike N. 11° W. dip 27° East Above these are exposed at 8 below high tide on the east side of well perfect grave of field PT some 6 thick bedded, rough indurated blue, calcareous shale, bed striking N. 12° W. and dipping 28° East. About 20 feet of these beds are exposed at the external (75 yd wide) to the west shore of the east group may become separated in turn can softer shales. Fragmental buff are the next rocks to the east. Fossils are abundant in several seams near the base x lower five feet and include a very rich varied fauna. Lingula lewisi Orbiculoidea MONOMORELLA Leptostrophia Strophomena (? Strophonella) Chonetes cornutus Dalmanella cf. edgelliana D" (?) Rhipidomella) sp. Stenoscisma over

Wilsonia wilsoni Spirifer elevatus Atrypa reticularis (coarse) Mytilarca sp. Pteronitella naviforme Coura& Actinopterella reticulata Sow. Follmanella danbyi McCoy Grammysia cingulata Kringer Cyrtodonta sp. Horio stoma Loxonema(?) murchisonia (Hormotoma) Bellerophon expansus (?) Orthoceras (Kionoceras) "myrice" O" bellatum (?) or ludense Trochoceras sp. Calymene Dalmanites Cornulites

Quadrille Ruled Form. John C Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 130 At the north edge of 8:3:1 oc- curs in the shingle above latitude an exposure of Lavenderish- mudstone argillaceous rhyolite- which side of which a band specimen is 8.3.1: 1. The strike 8.3.1:1. is a little east of N. and dip N. 8 Fossile very scarce = include trails joints or Rhynebonelle? from R ? Lingula or Leperdita Worm (see 5.59.7 A)

Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 131 8.21.1 F N 65° W. F. N. 6° W. (strike) 6.32 ft. A 35, 30 A 30 30 H 20.28 H 20 0.48 E [illegible] N 55° E (str.) N 30° N 60° E (str.) N 20° N 70° E (str.) strike strike N 20° W dip 26° E strike N 30° E dip 28° E furny or choidal end dip N 70° E dry mud shells with calcareous bands fossils above 8.21.1 A N calcareous bands = 8.21.1 M. fossil below calc. band = 8.21.1 N (over) 30 26 24 22 20 18 16 14 12 10 8 6 4 2

8.21.1. N. 1 Chonetes cornuta occasion 2 Leptostrophia (3) 3 Strophonella (?) 4 Leptena rhomboidalis very common 5 Dalmanella common 6 Stenoscisma & putchra common 7 Wilsonia occasional 8 Cypidula (with 5 or 6 central common laurel, side smooth) 9 Atrypa reticularis rare 10 modiolopsoid - rare " Trochoceras " " Caymerne occasion 13 Dalmanites 8.21.1. M includes Nos. 1,2,4,5,6,7,9 12 & 13 of the above together with a moderate amount. areas of corala (trigone? ? Darwites), also /horostoma sp. Rare

Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 South of the point in the extreme south edge of 8:21:4 the porphyry tuffs are cut by a coarse trap or fine gabbro dike trending N. 75 degrees west. North of the point a similar trap dike trends N. 15 degrees west. North of the point, in the midst of the porphyrytuffs ap- ppears some 10 feet of dark red shales or rather muds, strike N.15 degrees east, dip 37 degrees east. These may be the same band as the red mud with pebbles in 8:21:7.

133 8:21:1:(A) Along the south part of 8:21:1, the porphyritic tuffs strike N.8. along a distance of 100 yards, altho small modifi- cations of a rod or so may produce localized modifications of strike. The dip is 28 degrees east. On the south side of the southern point in 8:21:1 occur some fossiliferous shales intercalated in the tuffs. The diagrammatic section above, normal to the strike, shows the tuffs followed by a covered area 66 feet broad, th n crop out for a width of 12 feet some layers of fossiliferous blue shales and thicker-bedded, calcaro- shaly or indurated layers. These are followed by a nearly cropped slice, 20 feet broad (for a couple of feet in this space crop out some very soft, thin, blue-grey shales which cleave vertically. They are full of poorly preserved fossils,-not collected- of the same fauna as 8:21:1.A. After this covered space follows a width of 22 feet containing light marine grey hard, non-fossiliferous shales. These underly more porphyritic Tufts 19pts. tuffs. These beds strike N.20-22 degrees E., and dip 27-28 degrees east. This gives a total of some sixty feet of shales between the tuffs. The fossils occur in several seams. 6 = 6 feet Hor.v vert.

One seam has an abundance of Chonetes nova- scoticus; another of large Stenoscisma; another of Le tostrophia; another of Orthids and Chonetes cornutus. The total fauna includ es Orbiculoides........... occasional Lingula lewisi ...........rare Leptostrophia, 3 or 4 spp.....common Chonetes nova-scoticus......abund.in 1 sear c " " cornutus..........occasional Dalmanella sp.............common Rhypidomella cf.hybridus.... common Stenoscisma cf.acinus....... occasional S. " cf.pulchra ....... common S. " cf.lacunosaSow... occasional Wilsonia (pauciplicate)...... common Cyrtinopsis crispus(small)... common Pteronitella naviforme(radiae) rare Euomphalus (low spire)...... rare Dawsonoceras sp........... rare Calymene (very large)....... occasional Dalmanites ............... occasional Favosites ................ occasional Monotrypoid ............. occasional Crinoid joints ........... common

134 Northeast of the Bricklayer (which on extreme west edge of 8.21.7) occur several meters of sediment consisting of dark blue muds, tuffaceous shales and matrixstone agglomerate trace fossils are very abundant especially in several seams, the poorly preserved. The bed is highly inclined, strike N. 7° W., dip 63° East. The fauna includes Strophomena common Chonetes cornuta very " Palmanella " " Rhypidomella (?) f. hybrida " " Stenosisma " " Wilsonia (ganniplicate) common Spirifer crispa occasional Cypricardina common Crinoids " Favosites occasional. The shales are overlain by massive way thick bedded over tuffs with some strike & dip, and which form the point at the east end of the Narrows. The north side of this point is composed of massive hard galbros. A patch of lavenderish gray mottled massive mud occurs in the point of the cave exit off by 8.21.7 A

"more galbros and [illegible] in the point in N.W. 8.21.7" (a problem) by a cent. I found 50 feet (exposed) of black bedded porphyry tuff, successively lower & normally with angular lapillae. A specimen without the lapillae is [no 5]. These tuffs are of a very dark matrix with dark fragments, quite different from the typical and tuffs. They appear to be basic. They are underlain by a washed agglomerate in a mound of dark red color. The strike runs around from N 60 just above the middle of 8.21.7 to N.30 E. at the lower edge. Dip 27-530 E.

135 Quadrille Ruled Form. Patented 1906. John C. Moore Corporation, Rochester, N. Y. Back of the house of Mr.Saunders, the hill in northern 8:31:3/6 is com- pos ed of the greenish shales,or tuffaceous shales, highly slated.There is a little blue glassy rhyolite. The south shore of East Stream in 8;31;3 is composed of highly slated shales, supported on th east by a hillock of rhyolite. The slaty cleavage trends N.57 degrees east, and is nearly vertic- al. The bedding is very indistinct. It appears to strike N.5 degrees east and dip west at a very low angle, but this appearance may possibly be due to jointing. The slates are cut at the "Narrows" in the western part of 8:31:3 by a 20-foot gabbro dike. The slates reappear beginning in 8:31:2 eastern quarter, where the cleavage trends N.60 degrees east and is nearly vertical (dips 85 degrees south-east). Here again there are many planes developed striking N.8 degrees east and dipping west at an angle of 33 degrees. These appear to represent strike and dip. The slates continue as far as Moon Brook, and are cut by two gabbro sills, the eastern one extending N.E., and the western one, a dike, trending N.50 degrees west. The little bay about Moon Brook 8:31:1 is gabbro excepting the northwest corner where a strip of slate appears. To the west, the gabbro again appears on the rounded little point in eastern 8:31:1. The gabbro contains here long black lathes nearly a centimetre in length(hornblende?) and on the east margin has lavenderish- 30 28 26 24 22 OVE R 18 16 14 12 10 8 6 4 2

purple spots and also green epidote spots.

136 Plain Quadrille Ruling. Patented 1906. John C. Moore Corporation, Rochester, N.Y. 9.2.3.B Lingula sp. occasional Modiolopsis sp. rare.

137 9,2:3 6 On the east shore of Smith Bay opposite Davis Point occur some gray & black shales alutting over coarse intrusive diabase. The shales strike N42°E are turned up on edge and are perpendicularly slickensided. No fossils occur. The diabase shows no distortion nor other evidence of undue disturbance.

138 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 Stratification is shown in the sands and gravels along the top of the little cliffs for several hundred feet along the shore line The little bay in the S.E. section of-- 9.51.3 runs in a [illegible] coarse gray sand T. good quality. It reaches some clay & till and higher up in the hill is more till. [till] [sand] [clay]

PERRY..... WEST-TUBCO 139 Along the highway and to the southwest in 9:1:1, 9:1:4, and 8:5:5 are frequent exposures of the Perry shales and conglomerates. The conglomerate occurs in only one outcrop (outcrop 1) along the road forming the 40-foot knoll in n. 9:1:4. To the west and southwest, the elongate 60-foot knoll in w. central 9:1:4 and the little knoll near the margin are both composed of red shales rising abruptly out of a flat of Pleistocene clay. The red shales eg. in outcrop (outcrop 4) on both sides of the road at the 40-ft. contour on the east edge of 8:5:5, and reappear (outcrop 5) forming the 40-ft. knoll in s.w. 8:5:5. RELATIONS - south of outcrop 1, there occurs a thick diabase dike trending N 65-70 degrees east, and which may be traced westerly for a mile or more into the diabase mass forming the 100-ft. hill in 8:5:8, and also occurring easterly on the road in n.-central 9:1:5. This diabase mass is not immediately associated with the jerry but intrudes some black shales which outcrop between it and the jerry in the barnyard west of the house of Tr.----- in s.e. 9:1:4. These shales probably occupy the depression which may be followed to the east, lying between the trap on the south and the jerry on the north, south of it trap mass occurs some rhoyolite. This is gray in color where it outcrops in the road south of the creek on the east edge of 9:1:28 4.; and it is better exposed in the hillside 150 yards, more or less, southwest of the house. In northeastern 8:5:8, the rhy- 30 26 24 22 20 18 16 14 12 10 8 6 4 2

olite to the south of the trap is a bright pink. Near outcrop 4, the Perry is again associated with dark gray shales, a great thickness of which (over 200 feet) outcrop 100-200 yards S.60degrees west from the house of Mr.X--(house in S.W.9:1:1) These shales are cut by a thick mass of trap, the ledge trending N.50 degrees west which probably represents the direction of the dike altho S.80 degrees west, some 450 feet, is another good trap outcrop. The shales strike N.50 degrees E.( N.40-57 E) and dip at a high angle ,- about 60 degrees- to the northwest. The shales appear to the west of the trap and again to the north, outcropping within 115 yards S.60 degrees W. from the house. The knoll in s.w. 8:5:3,-Outcrop 5- is composed of red shale. An outcrop on the southwest side of the hill over 200 yards from the road (about 70 ft.above tide on S.W. edge of 8.5.3. shows both red Perry shale and gray Silurian shale abutting against each other in a vertical (?) fault which trends N.15 degrees E. and which appears to mark the west limit of the Perry.

Quadrille Ruled Form. John C Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 140 FLOW brownish gray to red phylolite weathering pink Idea porphyritic dark lead gray to green-gray & blue-gray basalt tuff, weathering dark dark red tuffa, matrix a feldspar porphyry with or less reddish fragments varying shades of dark red. Feldspar crystals usually abundant. Flows of

B37 Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 On the north side of West Quoddy Head extending from west of the pond in the S.E. corner of B.2.8. to eastern B.3:7, there occurs a series of exposures of a blue- black clay slate abutting against coarse diabase( "gabbro") on both east and west. Near the east contact the strike is N.35 E., dip 50 S.E.; along the middle of the series the strike is N.55-60 E. (nearer the former), dip S.E., 38-50 aver- age 42 degrees. The total thickness here exposed is exposed is a little over 500 feet. Slaty cleavage same as strike, dips 50-60 degrees S.E. Fossils are common in one seam at the base of an 8-inch calcareous band:- Crinoid stems....................abund. Leptseena rhomboidalis.........occasional Flectamtonites transversalis...rare Strophonella or Le tostrophia..rare (nearly flat; striae fasciculate) Chonetes cornutus.............rare Dalmanclla , 2 spp............occas. Stenosscisma..................occas. Atrypa reticularis............occas. Spirifer radiatus.............rare Cyrtinopsis crispus var......occas. Tentaculites sp...............rare Acidaspis.....................rare Synphoria.....................rare A couple of inches above the base of this calcareous seam in a shale parting there occurs abundantly Monograptus In the shales immediately beneath the calcareous band occur ( O V E R )

16 Crinoid stems....................abund. Chonetes cornutus .............rare Stenoscisma sp..................rare Dalmanella sp...................rare There were also found in loose pieces of the slate a specimen of Electambonites and another of an umbilicate Naticoid together with crinoid stems.

Fannas & Eastport Quad These lists are primarily the list of collections made at each locality and reported as preliminary faunal lists by Capt. Berger, & by others reported to H.S.W., by letters; other taken out of original field note books by W.S.W. - with other lists supplied by H.S.W. from his field notes - Intended to include every fauna form discovered during one survey of the quad. To Which are added the list by formations, prefaced by Berger before H.S.W. took charge of the work in Nov. Dec. 7 (90.

John C. Moore Corporation, Rochester, N.Y. Binder and holes in leaves, each Patented 1906. January or Cobbscork quadrangle (Eastfort, Maine) [illegible]

John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906. Notes on Formations by C.B.

Temside shales - Lingula cornea Sow; (no other brachiopods) Small Mollusopsids-(no Nuculoids, no Perinoids, etc. Ludlowist.) Bopyrostroma glaucomides Sow &k (no other gastropods) No cephalopods Ceritoceras, etc.; Beyrichia Noodenia, etc. (Tetrabrachia) fish scales. Passage beds 14000 - 22000 (100-120) wae. Downton Sandstone - 3500 + (30-50) wae. No corals, corallines, nor crinoids Lingula minima Sow; (no other brachiopods) Small Mollusopsids (no Nuculoids, no Perinoids etc.) Platyrhizoma hebetes Sow. (no other gastropods) No cephalopods Ceritoceras ext.; Beyrichia, Noodenia, etc. fishes Upper Ludlow Whiteliffie shales 6000 (250-280) Lingula remains & occa.sioria; corallines Lingula striata, orbiculidea; Pholad's. No strophomenoids (Leptenia, Strophonella, Leptostrophe ex. Chonetes striatella, Dalmanella, orbicularis), Stenosismia No Wilsonia, Gebyria? Dalmanella, orbicularis; Stenosmia Spirifer, etyavus (NO ATRYPAE); Dayla novaculaet. (wae.) Nuthrichonia, Nuculoids; modiolopsids; Grammysia etc. Orthoceras, Hyolithes, Ballemnophs; Tentaculites (Cornulites) ca.ymerie, Dalmanites, ostracods; Middle Ludlow Aynestry Instrn 10000 (15-400) wae. 1400 ft. Strata invariab. Forresty & Bered Schist 2625 ft. Searier.

Lower Ludlow 4700 ft. N. Wales. 12000 ft. English Lake Distr. Wenlock 2500 ft. Deutet's Cve, Iceland 20-4th. Llanymon 2000 ft. Central Wales Jun 9th. Llandoveryan 2000 ft. Llandreyn & Hay Hill S. Wales. Aymestrian { geved Ramassa Klinta Närrstorp Bjersjölagårds } Total 790 metres : 2625 feet. Deronnon 3470 ft.

Schooner Cove 5 Kelly Pt. gray shales (normal fauna, Dalmanella scarebr) 4 Leighton Point basic vacids tuffs with little shale (normal) fauua with favmuies of Platyschisma) 3 Schooner Cove gastropod-lamelli- branuch zone (see over) 2 Schooner Cove shales or Federal Harbor normal fauna 1 Long Cove Coarse acid tuffs includ- ing Long Cove fossiliferous shales. normal fauna + "Retzia's"

rhyolite. Perry dam red shales. Fauna same as Shackford + Leperditia. pleasant point gray & red shales; Anodontopsis, Lingula; ostracods; Leperditia. Moose Island gray shales; green/red argillites, rhyo- lite flow & tufts, trap flow. Anodontopsis; Lingula; ostra- cods; Diaphorostoma (no Streptotrochus; no Leperditia) Shackford dark shales. Anodent- opsis etc; Streptotrochus; Ostracods; Lingula; (no Leperditia) Birch Point shales, basic tufts & limestones. Leperditia & Ostracods. (Lingula, lamellibranchs & gastro- poda unknown or rare) Moose Island {No Corals" corallines, no crinoids Lingula; 2 or 3 spp. chiefly L. cornea Sow. (Temaside) No Orbiculoidea, Pholidops etc. nor articulate Brach. Anodontopsis bulla McCay (Uludlow-Passage, Westmoreland) Small Modioloisoids {No Nuculoid's" Pterinords, no Grammysis etc. Streptotrochus incisum Lindstr. (Highest Gotland) Diaphorostoma glaucinoides Sow. (Passage beds). No other gastropods; no Cephalopods; no "pteropods" Aparchites sp. Primitia cf. mundula type P."[E]" cf. remulina type Teloedenia sp. Ulrichia sp. # Tetradella clarkii Jones var's. (Manlius) Cytherellina Leperditia NO TRILOBITES

Pembroke purple shale { 2. Thick series of rhyolite tuffs & flows with a little red shale 1. Purple-red, splintery shales with occasional bands of gray shale, the latter 10 to 50 ft. thick & only occasional in conspicuous as compared with the red shale. } {No corals, corallines, no crinoids. Lingula minima Sow. (Downton) {No other Brachiopods Grammysia cingulata His (Highest England) " " var. triangulata Salter. (V. Ludlow) Small modiolopsoids No Nuculoids, no Pterinoids Platyschisma helictes Sow. (Downton) {no other Gastropods, no Cephalopods, no stero-pods. #| Drepanella sp. B Beyrichia tuberculata var's.} Etage K (Oesel) #B " salteriana v var's. B " kloedeni var. gibba Salter. (V. Ludlow) Leperclitia NO TRILOBITES

Garnet Point gray shales. Splintery gray shales, with a porphyry-tuff at top, and one or two similar bands near the base. Hauna saws as overlying Peurbroke purple shale.

Whitcliffe Long Cone & Bohemian Cn. Dinter, Leighty + Kelly ft. Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 Pholidops implicata Sw Orbiculoidea sp B. Lingula (mulgemor.) g. L. striata Chonetes novascotiens Dalmanella sp a, B Stenoscisma (pulella Sow) lacunosa Sow. non Salin) NO STROPHU MENOIDS, ATRYPA WILSON TA Clidophorus ovatus Modiolopsis sp. α (platyphyllus Satter, var.) Actinopterella 4 or 5 spp. Cyclonema murchisonia (?) (Hormotoma) Bellerophon (Patellost) expansus Sow. Hyolithes Tentaculites tenuis-ornata Mc Coy (but not var.) Orthoceras punctostriatum Hall & NO Dawsonoceras elegantulum (perchym) TROCHUCERAS monotrypa Crinoids Beyrichia kloedeni var. Kloedenia pennsylvanica Dalmanites calymene 30 28 26 24 22 20 18 16 14 12 10. 8 6 4 2

New below in Lakehead mini locating the 6526's frame with Yinfan between Megan & Robert,

Schooner Cove Gastropod Zone. intercalatus in Whitcliffe No Brachiopods Platyschisma helcites Murchisonia Bellerophon trilobatus " carinatus " expansus " globatus new gastropod Spirorbis large Grammlyciids ? Byrtodontas. Dilobella (Bolliia) (in trilobites)

Downton (Lingula minima) Lingula minima grammysia ? Platyselmene no brachiop. for Angles. or large lamell. no other Gastropros. Beyr. tuberculata (cypria ) (!) Beyr " var. pustulosa !! Beyr " setlingi " salteriana Leperditia Anchura 1200-2200 Purple shell Pembroke Dyk Loc Pembroke to head of Saffs Bay 600 Garrett point, gray, & twelve cast of Razor Island. * Leach 27.

Broad Cove fauna Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 x Lingula Swinina x ? (+ cornea (?) x Amodontopore x x Cypricardella x x Streptotrochus micianus Lindb. x Prepanella ? sp. nov. (80) Tetracella clarkes x recurring in Perry red shale along with Leperditia

Falls Point Falls Point & Benj[illegible] Chonetes (small, coarse) Leptostrophia Strophonella Leptaea rhomboidalis Dalinanella Sterosciena Wilonia - Spirifer crispus - vanuxeni Atrypa reticularis Polytropis (gastropod) Trochoceras Sphyrodceras cephalopod. Mytilarca [illegible] ? Aymelt?)

Ree also Mormon Co 5.35.5A. Dark blue thaly. Above the Obenbier zone of dark Naly, comes in before Strehopfuhl & Whitchelly