Field Notebook: Newfoundland 1918a

William Lemire, Shipper and Engineer James O'Rourke, Male and Cork. Bth of Carling, Newfoundland.

20. 4402790 1 2 3 4 5 6 7 8 9 Paid mt July 23 $50. 7248620 1 2 3 4 5 6 7 Paid mt July 23 Aug 29 cashed a check for $1000. $200. {600 400 Charles Shuchert 159 ball st. Yale University New Haven, Conn. U. S. A. June 1918. Book I. 3450 doc. 0113

Carl Owen Dunbar, Age 27 years Born at Hallsville, Cherokee Co. Kansas, Jan 1, 1891. Dana Research Fellow in Biology at Yale University Local Draft Board for Cherokee Co., Kansas. Serial no 766. Order no. 1187 Classification 4A. Wayne Steele Edwards. Age 29 years Born near Talmadge, Dickinson Co., Kansas, Dec 18, 1889 Divinity student, Yale University Local Draft Board for Dickinson Co., Kansas. Serial no 1186. Order no. 1789 Classification 5C. New Haven address 1120 Yale Stati Frank H. Probst, Of Ogima and N. Mex. Opp. N. B. Davis, Kimpton, Ont. After Crime Don

Phil. Schuchert 78 Wells St. Brighton 810 N. Fifth St. Cincinnati, Ohio. Emma Schuchert 1900 Mills Ave Normwood, Ohio. Albert E. Schuchert 3937 Regent Ave Normwood, Ohio. Birchy Core Grooming J.H. McEachern, Collector of Customs Tom Kennedy. My shipper in 1910 William Lynch Mate in 1910 Tom D'land. Cord in 1910. J. F. Thorne of Ogre & Sons, Tourist Hotel Jas Parsons? Petries Hotel at Birchy Core. B.D. Lilly, Curling. In 1910 R.R fare round trip New Haven to North Sydney $38.05 North Sydney to Birchy Core. Round trip $14.50 Mr. Richard M. Field #16 Weston St. Jamaica Plain.

Blancallon, Labradora. Edwin S. Grant, Superintendent of Joff Mrs Fishing House. Doctor Armstrong Drift Breufell. Forteau, Labradora Capt. Sam Muscu. May entertain Mrs Harriet Flynn. Point Armon Light Davis Brothers live near here. Entertaining Mr. Richardson Port au Choix to A.S. Darby (good chat) (oil) Anse au Loup. Mrs Barney, "Old lady Barney" stops. Flower Cove, Newfoundland F.B. Cox wrote me from here in 1910 Mrs Normans trading house. L.H. George & Sons. (oil) Current Island Nat. Taylor Bag St. Barbe Only one house here.

Bell Burns Mrs Thomas House Cow Head John Paire Care Stephen Taylor (oil) Dally's Cove Four miles n. of Green Point. Stayed one night here in 1910 Bonne Bay A. Doucette, Noford. Travels Mrs McDonald Martin Caskin. Mr House Manager of li. garris fn Dominion Iron and Steel Co. J. A. Thompson (Crown expert) Port au Port (Probate). Edwards Salary $50 per mtht Quarries " 100 " " (Up to date paid). Drat Engineer 75 " - Raised to 90, Boat helper 60 " " Raised to 75. Hon J. B. Blanford Minister of Mines St Johns Hon George E. Turner Deputy Min. of Mines "

Credits April 29-1918. Received of J. B. Tyrrell his check for $250.00 August 31 Cook at Curling Newfoundland 100.00 P.P.M. Baran to Boston 5.09 Boston Urban League 32.77 P.P.R.to Stephenville 3.80 Steph to Curling 2.25- 43.91 Actual fare from Curling to Boston $39.55 Meals for 2 days 6.00 Slapen 3.00 52.91

Paid Out May 11 Bank chags on Tyrell's check 3.75 " 13 F.R. Plumb Cr for 8 hammus 9.80 Come to Q.H. June 5 '18 " 16 Ames. &g. Inc. for enlarging four maps of Newfoundland 10.00 June 5 Federal Court for 3 jan. photos 6.10 " 5 Telegram to B.O. Lilly 1.05 " 7 " from Mrs. Lilly 1.00 " 10 Variations of emulsions .53 " 14 Telegram to Tyrell .55 " 17 6 Blankets 42.00 " 17 Rumba coat, pants, and hat 10.35 " 17 Safety pins .57 " 17 Mosquito netting 1.60 " 20 Telegram to State Department .70 " 21 Photofilms and chemicals 10.50 " 22 " for Schoenfeld's camera 9.0 " 22 Fly-dope 3.75 " 27 Exchange on $600 American Exp. Ord. 3.00 " 27 3 fares to Boston '19 15.27 " 27 Transfer of luggage/2 Excan B. 17 3.01 " 27 Transfer of " to North Station 3.00 " 28 Telegram to L.B. Lilly, Curly Camp .45 " 29 5 meats on cars 2.90 130.88 & 4

June 29 Carriage tr Depot and Hotel 175

37 4 03 July 23 Paid J.T. Thorne for supplies for trip I owe him $53.32 Paid Aug. 29 23 Paid B.D. Lilly for oil (6 tanks) @ $18 I owe him $37.52 Paid Aug. 29 23 Paid William Lemire from June 20 to July 20 23 " James O'Rourke 24 5 days board for 3 at Carlin @ 2 Aug. 5 owe Lemire for camp purchases 937 03

Photos

Photos

Photos

"Tyrell wants to know "The age of the rocks which underlie the littoral plain on the west side of the Island. "Which series of rocks contain Petroleum? "Whether those Petroleum bearing rocks are lying in such a position as have such structure as would make it likely that they would hold pools of Petroleum." Look to other minerals. Petreints. Keep him informed.

June 28th, 1918. Friday. C. O. Duntan and H. J. Edwards' f[or]ports arrived this morning. The one for Schuchert came two cre[eks?] earlier. It is a sad commentary on the ef[ficiency] of the State Department that it should take two to three weeks to make out f[or]ports after all the evidence me is asked to hand in to show that me is a citizen on a good journey. Even this afternoon before the Federal Court. Shipped tents and beds (six fa[ck]s?) yesterday afternoon on articles to Boston, where I will re-ceed to Newfoundand. Sent the following night letter to B. O. Lilly Curling, Reef: "Have f[or]ports. Write with two assistants evening July fourth, Polan Port. Have launch, two men, provisions and dishes for three meals, Polan Port on outside. Bringing two tents, three cots and bedding, folding stove. Will see you at Curling in two or three days." C. Schuchert. June 29, 1918 Saturday A dark misty morning. Dr. Meare to Boston at 10.33 A.M. Arrived at 2.24 P.M. Fare $5.09 Mr. Tim in his auto called and took Duntan and J to the depot. The day turned out fine at Boston. After adjusting our baggage checked them off to Port

June 29-30. Boston an Basque and railway ties (# 98-31) are return to North P.R. Station to get Atlantic. From here we walked to Squantum to see the Peruvian tillite. So back to Adams House at 9 p.m. m. Had supper and after a little walk went to bed. June 30-1918 Sunday. A fine day. Visited Bunker Hill, Harvard, Copley Square, Public Library, Salem and Marble Head. Left at 9:30 and got back at 9:30 p.m. Saw mud today. July 1-1918 Monday. Left Boston at 8 a.m. and got to Lancaster one hour late at 8:50 a.m., It was a foggy and rainy day. Baggage inspection no more rigorous than usual. Did not care for our comforts and most of the passengers had more, However the jolting across on Duxton and without one he would have been awfules. Toward my left over across the Canadian border. Got to St. John 1:30 hours later. Got a sleeper here (State Room) to Trenton and got tired at 1:30 a.m. Eastern Time. Sleeper Charges for $4 6.60

July 2 -1918. Tuesday. Canada. Left Truro at 6.30 and left for Sydney at 9.45. Had breakfast at the station and then with Dunbar walked thru Victoria Park to see the Cars and Train. Left Truro at 9.30 A.M. and got to Bath Sydney at 9 P.M. Went aboard the steamer and sailed out on a dark rainy night at 10 P.M. Our day was a very Turmoil one due to crying and noisy Children and singing religion Canadians. July 3 -1918. Wednesday. The steamer arrived at Port au Barques at 6 A.M. in a light rain. Then as usual it was a hustle to get off the boat and our luggage wobbled. All had arrived and we got examined in a hurry, had to deposit $ 10.00 on the First cameras to be returned to us when we leave. Our passport must have risen at St John, but any Customs Officer will look after this, but we must give them some days to get the permission for St. John. Also were examined for vaccination and got through practically without examination. One hour later we are at Little River. From the Car windows it does not look promising for anything startling in the way of geology. Got off at Little River 1 or so south to see the area marked by Harley as Cambro-Lilurian. Nothing was the seen of geological importance for 3 miles south of Little River. Being at the Dumps fork and thence southward

4 July 3-1918. Long Range Mountains seen 2 to 5 miles [to Cape Ray] [Wonderful red color minerals] here old igneous mass is the seen, and into which is faulted at the south the basal series of the brinsons. This mass about 200-300 feet thick lies in a synclinal manner. Below are brinson beds, the pieces large size up to 30 inches long and offset but to almost anything. quickly destroyed and with transported Roundel, off in the material of a cliff adding the old igneous rock [the brinsons are] The deposits later, porous as usual and filled in with grass and microccers the further on brinsons with rich matrix, hidden of the surface, are fine and muddy, and they complement a firm and all a rust firm or maroon color. In these high beds an [with minerals] may sometimes from 3 to 8 inches across. Fault Distance away me- half mile. brinson beds Old igneous Chalk and some argillaceous rocks. layers These brinson beds are near the base of the brinson series. Many [granite] of the sandstone brinsons, are completely decomposed, and so soft that one can stick a finger into the carbonized material. The brinson lies on the old igneous (Laurentian) ma- directly terial. There is here no trace of the Cambro-Ordovician, nor is there any limit lines in the brinson conglomerate, nay- or is the matrix line from any limit line in the area, when in the revealed glacial material. Therefore their probably was here at sometime any Cambro-Ordovician.

South of Little River. July 3-1918 Lata Dunbar walked east of Mac Donnell's brook but saw nothing more than the old igneous material, and the granite. Above the Little Crofting River or Inacilik estuary there is a bounding plain of farm land. Not above 20 to 25 feet above the water level. About 3 miles south two higher elevated mountain terraces come the lawn 90 feet (annexed) and the high at about sea level. They run into each other. From here looking back to the Little and Short Crofting River one sees the same terraces jut out in the Gulf as headlands. The foreland goes back to the Long Range, and then these rise boldly out of the low lands to levels up to about 1700 feet. The fault escarp has a slope pattern 45 degrees. Pride valleys run back into the mountains and in some of them we see glacier cirques. The foreland probably once was as high as the Long Range, but because of the soft nature of the rocks there have been worn down to its present low level. The seaward side of the foreland is here made up of the glacial land crust removed by the sea, and back of it in the north are the Carboniferous rocks and back of these the old igneous material. There in a dark greenish and peccable granite, terribly marked and shot through by veins North of Little River

6 July 3 - 1918 of a red granite in seams from 1/6 in wide to others 4 to 5 for thick. All are crossed faultily by small ones only the thinnest to several feet. The dark grey-green rock is much metamorphosed and in places is serpentinized. The granite sometimes appears to be mainly quartz with but little red felspars. Beside the veins of red granite there are included rounded blocks of the red granite now many feet apart. If this inference is correct the dark green masses are younger than the Grey Range granites, see the small collection of green rocks. In going east a inland of Mac Dugarts from Clentam saw that the metamorphosed green rock gave way to pink and grey granite. We one all struck by the great variety of granites and freens here. Clentams notes say: "The granites include fine grained dark grey ones, light grey medium grained granite, coarse grained porphy with large phenocrysts of white felspar, coarse grained red and pink granites and granite breccia to compare to most of these types. The region must have had a complicated green history." Today I am spending my sixtieth birthday geologizing in Newfoundland.

July 4-1918 Thursday. Little River Directly across the estuary from the Little River railway station or one can be seen a fine glacial cinque. There are two cascades coming down at that time and these unite into a small placin that is quite like tunnelled by a stream. Yesterday we saw two other cignes to the south of here. North Lug Range Fault Scarpe Chinqu Lower plain Lake Level We have a photo of it taken in the morning against the sun. Little River Station Almost stormy, with [illegible] About over all we see that the valley walls rise on far less directly than the Lug Range. The sky-line is flatter and long here in sunlight the Lug Range is much dissected by hanging walls one of which ends in cignues. The western face of the Long Range is continuous and at North Branch we see it for 20 miles to the south and once than 10 miles to the north. It has no spurs extending orsting, but in one fault line scarps. The Windsor series rises up on its side to about 500 to 550 feet above the sea, and here it dips steeply into the mountain. We took the tram south 16 miles to North Branch and in the evening came back to Little River. We are impressed by the straight face of the Long Range Hills. It has no spurs and much of the slopes descended at an angle of 45 to 30 degrees. The upper slope appears to represent the undivided fault line scarps. The walls and cignues cutting through it are all longing walls with their bottoms now estimated to be about 3 or 4 feet or less above the level of the river walls. From the floor of the

8 July 4-1918 Little Rive. Rivis really the dips are at first gentle to about 200 feet and then more steeply to 500 or 600 feet. Above the latter is the fault-line scarp face for about 500 to 600 feet more. Still higher there is a more mature and smoothed (glaciated) topography for from 100 to 300 feet more, and it continues to rise back of this to a preplained surface that maybe at 1600 or more feet. [Diagram] Today we saw but one place that I thought might be a moraine. It was near Overfell. All the other valley sides appear to be made of stream boulders and sand clearing from the Long Range side of but little Windings river probably due to its older nature. Not rounded by water. It is stream material and not ice born debis. Here and there one sees large erratic but those seen are in the depths of the valley and are the erratics of the glacial period. While the other material came out of the hanging walls while those had their local glaciers, and enlarged torrential streams. The hanging walls are the pre-glacial walls aggrandized deposited and sharpened by the retreating moring ice. Their side are straight and no marked spurs extend into them. If the fault-line scarp is jumping into feet there has been since the country was glaciated an elevation of the Long Range of at least 500

July 4-1918 North Branch tr to foot Dunbar was the first to see this topographic development and my part is to fit in the details. He walked about 1/4 mile north of North Branch station to the railway bridge over the Cording River and here on the western bank is an exposure of Windsor shale dipping towards the Long Range moun- tain at about 35 degrees. To the east and west of here are is Car- boniferous and maybe are in Windsor. He then crossed over to the east to the wagon road and then north to the second brook flowing into North Branch. A French- Canadian has land here by the name of Peter Muig. He ascends the brook and in 1/4 mile came up an outcrop of Windsor. I con- tinued a little further, but Dunbar and Edmonds on the advice of Muig continued about 1/4 miles farther. They found Windsor in various outcrops all the way and then the dark grey rocks cut by granite igneous dikes like that seen yesterday. From Dunbars notes I take the following. The first out- crop of the Windsor is a gray-green to red shale dipping 26 S, 250 E. A half mile farther up the brook is another outcrop dipping 420 S, 23 E. About 1/4 mile farther is a gay sandstone dipping 230 S, 20 E. A 1/4 mile farther then is a bluff of fine grained layer folded Windsor sandstone. It is badly broken up and crumpled by Norse faults. Evidently we are

10 July 4-1918 North Branch nearing a fault line." The brook bed continues for a few hundreds of yards and then stands critically. Above this the stream narrows quickly and cascades down over the dark darkness the Cars, having dip structures or denus to near the faulty line and here still partly, from rock. The stream is "marked and ochre" with the clearage parallel to the contact with the grinds and critical. About 50 feet farther up stream it is cut by a fine red granite porphyrite dyke about 3 feet thick which stands critically across the stream. It contains flakes of mica as big as any hand." Have a large piece of it. Far down the stream bed one sees pieces of these dikes. "This parallel dike of the same material occurs a few feet higher. About 50 feet higher up stream is a 3 foot vein of nearly pure white quartz." As float this is also seen more than mile downstream. In this upper region of the brook are boulders "of a heavy rock composed of quartz and a flake mineral." We have a sample of it. They come down from higher up in the brook. The contact of the grinds with the igneous rock comes in on this brook at about 400 feet (around) above the Ordway river, and about 1/2 miles of the brook. The contact is therefore well up in the flanks of the Long Range, rather a surprise to me. All of this shows that there is here Mr Conklin on any Oidician, it is all Clark south of Bay St. George.

July 4-1918 Little River The Brindon seen today has an average dip of 22, a thickness of at least 3,100 feet. The cliff on the fault line must also be some thous- and, I think. On Stanley's map ore is reported on this brook. Ore was seen on it then any float of it in the stream. Stanley also reports marble at the head of the brook and therefore marks it as Cambro-Ordovician. Evidently he mistakes the quartz float for marble, or the dikes of quartz for marble. I had the impression that the Carr lies on the flanks of the Long Range Mts in synclinal form. This is an error for the Carr dips towards the mountains from 22 to 25 degrees and close to the pre-Cambrian stands vertical. The papers say that the Reid Company have found ore in moderate amount on the Smith Branch near where we were today. It has been developed some and a siding put in but at present nothing is being done further. I am afraid it is mere enthusiasm. One man said that a 30 foot bed was found by an English specialist and that a million tons of ore is in sight. Yet more men after it. The labels are an ore statement. July 21 ore with Dr. Hatch of Columbia de Dr. Morris. The person said he saw the 30 July ore. Strange that did! After six P.M. Denton and Edmonds crossed the railway and opposite to collections, through the bushes and up the brook into the glacial coupee. They inten- ded to go the glacial lake and the overglaciers back of it, but twice

12 July 4 - 1918 Stephenville Returns at 10 P.M. still twilight over the creek. Key some nothing of the rocks until about 100 feet above the estuary and then of an altitude of 300 feet saw the same spread dark rocks seen earlier in the day at South Branch. Immediately at Little Rims the red sediments are of brindon age, and it must not directly upon the Lamentra man. July 5 - 1918. Friday A dark cold morning. We are off to Stephenville to train where we go next by steam to Port au Port. Arrived at 6.15 P.M. North of South Branch the Long Range Nuts are much more dissected and are jagged. Here one sees, but indistinctly, the fault line scarp. Probably because they are east of the fault line. Opposite South Branch and to the south one gets the impression [one can see] of the ridge that the Conyville Nuts are a series of ridges in rockshell and with the other of the Long Range. Between the two the river valley is about 3 miles wide. As one goes on towards Goffs Station one sees that the Conyville Cliffs are once if a sort table land and in rounded cliffs forming mile valley. The valley descends slowly for 20 Nuts and rises again to a much lower ridge near the Belly of St. Lawrence Lake. The only has the trend of the Nuts - the tops of the Long Nut are a rolling humplain, Miss Conyville Nuts. Table Nuts miles wide a mile Coral,

July 4. Stephenville to Port au Port Looking across from the station at Stephenville to the Long Range, but one sees that they are here again much dissected as north of South Branch. To the south-east of the village some miles there is again here a steep cresting foreig cliff - a fault-line scarph - just like those seen to the south of South Branch and Little River. This must mean that in places the fault line in to the west of Long Range but at others it does not cut the upland masses but somewhere in the Drifson. This explanation also explains why in many places the old topography of the Long Range comes down lower and meets once again the lower levels of the Drifson series. old topograph Fault Line Scarph (Jack Cushing) At Stephenville we found a little boy 13 years old, with a one seater wagon ready to take us to our Friday drive at Port au Port. We are stopping with the Customs Officer Peter Cushing. At the tip of Indian Head mountain that makes Indian Head on the road to Port au Port is the following experience: The dip of three sandstone beds 205, 70 E. This mountain begins about 2 1/2 miles east of Stephenville crossing and is about 3 miles across as the wagon road goes. Rising upon the mountain a short distance after crossing a small brook

July 5, 1918 Port au Port maybe seen exposures of the dinosite in the north gully of the road. Here one of the dinosite is conglomerate but as to what the bottles are made of ore did not determine. This must be done before we leave this area. In about a 1/4 mile one came upon the first exposure of the dinosite [Specimen 1]. Rising of the road one came upon other exposures (Specimen 2) of the same ore, then to a small firm and easily fracturing mass and down a more crystalline ore (see sample). All this in about 1/2 mile. Then in about 1/4 mile one or are near the center of the mountain where there are great exposures of the dinosite, all placiated and especially on the sides of the vertical cliffs. Farth down the eastern side one also saw placied strias and large The strias of these glacial strias have been seen in the eastern side at 66° W. gorges (see their). Just before one came to contact with an alluvial sandstone there was an opening made for prospecting some days. Here the dinosite is most granular. The note on the fore mining face refers to the exposures here. Rising on over this in considerately the sandstone, say for a half mile, when one comes upon another dinosite more quartzitic and with more feldspar than before (See the Specimen). Going down the hill one again came upon great thick mass of the dinosite that continues to the bottom of the mountain, and here are again saw the contact (around alluvial, creating other, say for hills area) as in the top of the mountain amid the sandstone. As this sandstone is a heavy beds and is wholly unlike

July 5 - 1918 Port au Port The Carb here the question must be asked again, what is the age of the sandstone that the diorite cuts? It maybe even if pre-Cambrian age, or one may have to assume that the Indian Head range was a mountain ridge in the Brindon sea floor hard and resistant to the weathering away. Against it and now it finally was deposited the Brindon series completely burying it. Today it sticks out 2290 feet high and on the Brindon is one of 4000 feet thick, these deposits could easily have covered it. Later on the sea Brindon was worn away leaving the Indian Head range sticking out as we see it. Before more to: If the pebbles in the Brindon are of this diorite one will have proved that the Indian Head range is not an intrusion into the Carb. Its age is then unknown. The next day Edwards returned and gathered some pebbles. There are none of diorite but there are of the quartzites. See the speciman. From this we see that the sandstone are pre Brindon. There is nothing of interest to relate further over until we came to Romarre Brook where the Brindon conglomerate and gypsum cliff is well exposed, most of the brook rises Table Mountain to 870 feet and are of Ordovician age for the grounds according to up to Romarre brook (Stansleys map). and forms The placers strikes first seen rising over Indian Head had a strike of 70° E. On the tip of the mountain and 300 feet above the really on the cliff sides we again saw strike and a polished surface striking 68° E.

16 July 6-1918 Saturday Gracch-Potau Pot.- Gleemartown. Rising in Section. Started in at the eastern end of the Granch. Here are long bedded, dense, dark-colored limestone with an occasional thin one of shaly limestone of a greenish red and rusty color. Fossils are exceedingly rare. Got a Stromatoproid, Ceratopyga, and little balls of Cryptogon. Also saw small disinturds of Endocerids, a small circle cephalopod and small machines like shells. The limestone are often striated and in one of the layers saw introduction of enclominate. Also thin beds I saw evidence of some brooding. In some creeps there lies remnant of Lourville but all low white in color. Ho'd 127.30 E. We see well exposed 25' on the western side of the houses on the Granch. Fossils are formed from two of section at eastern end of Granch. Thin follows a thin foot bed of greenish-lacery li. replete with horn Helicostoma, and rarely a small Maclewa. Also an Orthoceras. Cryptogon are common in small beach. All of the greenish beds have fossils and especially Cryptogon. Two feet of shaly red and rusty limestone. Three feet of greenish ornamental marvy dense li. These greenish beds all lie Four feet of shaly red and rusty li. Thin foot of greenish dark colored, marvy li. Four feet milky white dense li Three weeks of greenish-dark-colored li. Four feet of dense lacery light dark colored li. Two feet of greenish-dark colored li. One to two feet of orange-enclomitic Cryptogon li. Twenty (20) feet of light dark colored (marrying local) li. Five feet of hard greenish-dark colored li. with thin layers common.

47 North side of East Baz up to Lead Core. Three feet of same with Cryptogron. Four feet of dense colored li. with little chalk. From foot of lithr to dense colored li. Four feet of premixt dense dark-colored li. with many Ceratipen. Dip foot of light-dense colored li. Three feet of premixt-dense colored li. Three feet of dense-colored laminated li. My characteristic is thin laminae. One foot of redish laminated li. Eight feet of light premixt greenish li. and Billingsella, Ceratipen torta and gastropods (Affilata, Raphistoma). 11-5 feet to top of this layer fine bitumen of section. The fossils are common but poor and very hard to pick. Lot marked A. The bed is replete with small (½ to 2 inch) Cryptogron. Whiter foot Ceratipen are very common. Five feet of dense chloridic grey footy clay bedded dark colored anthers interred. Hardly beds. No fossils Four foot of premixt-dark colored li. replete with small Cryptogron, and Ceratipen and Billingsella. Lot B. Nearly medium bedded Above continue the greeter li. for about 30 feet to an undulatory plane a fine thin grain of Cryptogron here, The should use this undulatory plane to distinguish Beckmantown from Chaggy. This then gives 154 of exposed Beckmantown. Harley determined 100 feet of B. here. The Cryptogrons become more and more common upward and finally made up about one half of the orestand a premixt-dark colored beds. Large leads are nearly zero, rather small balls up to 2 inches and reddish

18 Chazy July 6 Great. Erased. Undulations at about 12 miles taken up by Chazy li. Below the beds are light colored and mottled red li. Above are the dark heart beds of the Chazy magnesian limestone. At one the undulatory zone we began the Chazy. There is at the base about 2 feet of the mottled red layers li, like that of the Beechman ton. This seems to militate against the value of the undulatory zone as a dividing line but if the sea got this material from the Beechman ton then it should have its character under current. In a few feet we get to see an abundance of reptilian Chazy frosts and as they are very different from those of the Beechman ton, then must be a break in definition between the two. Let's frost A. The Chazy frosts do not come in in abundance until 50 feet above the base. Then they are fairly common in the three dense dark gray heavy bedded li. From Gumban I copied this:- "About 14 miles north of the Grants a fault cuts the Chazy, its plain dipping 26° about S 60° E. Beyond this the Chazy continues but the dip is 140 due North. In this part of the Chazy occur the fossil bryoz., and Stromatocrinus. "The north end of this formation has a double fault and be- tween them is a west-south fault, the strike of the east fault dip- ing due north and of the west frost N. 30° W. Coming to the east side of the formation, going south are start down across through the section. A few yards from the frost is a vertical fault bearing due north and south with slicken-sided and floors showing ver- tical movement. On both sides is still Chazy. To the over

July 6 19 Of this promontory in Lead Ore, at the south east angle of this ore is a vertical fault bearing S. 30° E. which lets down the Brandon against the Chazy. The lower 100 feet of the Brandon exposed is a dark brown dolomite, much crushed and broken and dips steeply to the south. These layers have an abundance of marine fossils. Above are strata of clay sandstone, thin reddish of a light olive color. There is also in some beds a fine crystalline crylomite. Sorry mistake. The dip of these beds are clayey and become almost horizontal. Near the south east corner of this ore which is about 200 yards wide the beds are again sharply bent up on arc, exposing the fossiliferous layers of the Brandon which now against the Chazy. The fault plane dipping 30° due east. To the north the Chazy dips 180 ft. 20 ft. Lead Ore Fault Chazy Brandon Lanil. 2 faults greaves “A lead prospect has been tunneled into the crushed part of the Brandon dolomite near the northeast. Inside now and a general denunciation of pyrite and lead are to be seen.” Now go to page 22.

20 Indian Head July 5 - 1918 From Recent notes relating to Indian Head, I take the following: - At the top of the mountains" just out of the prospecting hole there is a large peridotite dike of red granite with great crystals of red feldspar, and sheets of mica, both brown and white 3 or 4 inches across. On either side of this dike for a distance of say 3 feet the dike for a distance of say 3 feet the dark fine grained rock is altered to a mica-schist and is soft and weathering faster than that adjacent. From the dike onward for about 60' the wall is heavy feldded and hard and then getting away farther from the contact the feldding planes are well developed and the sediment is seen to be a fairly even grained dark grey - reddish sandstone. This continues for a considerable distance say 1/4 mile on one cliffy 20" S. 70" E. back toward the dike, the sandstone meets the dike at about the granite dike but is altered and infiltrated with quartz for several feet from the contact. It was clearly injected by the dike since it is dis-torted contemphorally and the dike is not a throaten of some hundreds of feet of this old grey sandstone is shown and it is fairly uniform color and texture. "This sandstone appears to have nothing to do with the Dinbon beds, the latter being variegated in color, with small red and moist beds of shale. The sandstone here exposed looks very old and may be from Precambrian. "Below the sandstone the dike continues most of the

2/ way down the out side of the spit, but near the base the last explorance appears to be the same time again, much more- mouthland. No dinder is seen here. The cross section is as follows: 'dike seem my the speckman. Old Sandtime Permatite dike str Old Sandtime dinite X X X X X X X bridgem comp ment. W<br><br>3 mile<br><br>E Outline of Port au Port area Strike 1 1+5 Albion Point sandune Lead Core Lead core shun (uns) Red mound. Gravel Port aux Port Village Cemetery Church road At berger Peninsula The gravel spits are thrown up by the storms, and are 100 to 200 feet wide and at least six foot above the sea. Quartars note continue as follows:-

"After suffer I went south across the headland in part of Mr. Carlin's home to the edge of Bay St. George. Here the Beeldmantown is present and in thickness all lower than those seen this morning. This section descends from north- last from the knarls to the headland that occurs about 1/2 mile from mouth of Remains Brook. The lowest layers stick out of the matrix just south of the head land dipping a little early north. The line of strike would carry those strata south of Table Port. These strata from the headland at this point which is about 30 feet above orate level, where they are truncated and smoothly polished by the ice, the glacial grooves being directed north but there are also smaller scratches crossing these nearly at right angles. Going northward toward the knarls we can measure a thickness of 500 feet of Beeldmantown, even or the base is not seen. The dips is uniform, a little east of south. What last seen to the knarls there is an unexpounded sandy head, the interval being more than 200 yards." The next day we estimated that there may be another 1000 feet of Beeldmantown between those of Bay of St. George and those of East Bay Port au Port. Together this would give 1000 x 570 x 240 = 1740' The only fossils seen by Denton in these older Beeldman- town are all Cryptogams, and there is an abundance of doge leaves and crag rocks. As we saw sandstone fine grained like those of Havre Bay or maybe that Upper Cambria is included in the 1740'

July 7 - 1918. Sunday. Patan Port This morning walked 4 miles north to the great quarries of the Dominion Iron and Steel Co. Here they got their flux in the upper part of the Beelman town (faulty but put around), and the basal beds of the Chazy (faulty 30 feet to north edge of quarry face). The Beelman town is here a dirty gellor (weathered) and consists of the crumpled clinozircon beds seen yesterday near the Smocks. The Chazy is a dark grey, and is in leaning beds. The town contacts sharply. Here are again saw the line of separation, and at this level there is (either a sliding fault or) a small zone of Chazy to flux, partly intergrade. In sum, cutting slightly transverse the Beelman town. They quarry mostly a drawing up affected. [illegible] At the front we saw one flux x and two men William Lemire (Engineer) and James O'Rourke (Cork). They look like good fellows, drilling and ate in their line. Their day began on the 20th of June. On our way this morning we saw on the road back of the Lead quarry the Windsor here a decided limestone employment (Andriecia pettole). It is the roof off basal Windsor here on the Chazy. The contact one did not see. At about one mile northward one could look into the second lead quarry another parallel faulted area over the Windsor drilled in. This one is entirely deeper but appear to be them.

24 July 7 - 1918 Port au Port Times older than the other one. On the road side back of this second down faulted area we saw the actual contact of the [illegible]. The dip of the bottom is 60 to 70 N 30 W, and the Windsor dips less than 45 degrees due east. Windsor conglomerate here on the level intention where it lies in a roller and running either way on the road to the higher land. The Windsor [illegible] about 6 feet thick here are the actual overlapping basal sliver green sandstone, decided conglomeratic with the limestone joints and angular out angular and jell sizes up to 4 inches across. Above these conglomeratic sandstone of joints 20 to 30 feet thick we saw a little gray (lead metal) in the Windsor dolomite. In the course of the past Dominion Iron and Steel Co we also saw crushed Windsor dolomite. It lay near the upper fault face, dipping away from it as usual (dry) and all round truncated edges of the crushed. As the Windsor overlaps the lead mantom and Chazy in the lower places it is clear that a thin sheet about 100 feet would dip it in the true cross as we say it today. The faulting is therefore not extensive. In the afternoon we examined the eastern side of East Bay from the first exposure of Beechmont on south of the shores between the two through a high sandstone atop of which is the village of Port au Port, at about one and half miles. Near the base of this I saw somewhat for more below a zone of Cystogroms. The dip here is 160 to 30 Dr (time and t). At 125 feet above the base there is a local drag fold that changes into a fault. In the down thrown beds all are crushed Drag fault [illegible] down throw many beds. See the photo.

July 7 -1918 See the top photo of these Cryptogras. Further development being about 100 feet above the railroad track. The Beedmantown is here replete with Cryptograss. [I]t's at 100 feet above the line are Cretacypen, Tintal and Patropodreyus lommadii. At about one mile from the [illegible], there is another fault. It dips and 120 feet down through the B. is to 30 degrees due east. From here in 115 feet mine of B, with many Cryptograss. Here there is also the undulating originally, line that separate the light colored yellowish Beedmantown from the dark-fay Chazy [I]t's the same lithology as in the great quartz seen this many. There can be no doubt that the Beedmantown is decidedly broken for land interval from the Chazy. Cryptograss goes to within 30 feet of the Chazy Chazy, we saw many and here at 115 feet beneath the [illegible] Tintal Cretacypen (have 2 specimens). It is there upon 30 feet of the Beedmantown that we have now seen three times beneath the undulating line that separates the B from the Chazy. What we saw of the Beedmantown this afternoon has a thickness of about 240 feet. The Chazy lies as on the south side of East Beech upon about 2 to 3 feet of marble and beds. Hamley gives the thickness as 870 feet. The Chazy antiquities along the coast for about one mile. On the lower part of the Chazy we saw another core with the Brandon dolomite let down. The northern faulted wall of the core is outcropping striking S. 20 E. Vertical fault Chazy this fault was Core and area not seen. Here are other small faults in the Chazy but all of nearly similar gear things, as the dip remains uniform. Lumban says the Table Head beds are faulted down. This may account for the small thickness seen here, only 74 feet. The same may be true for the Parsons.

26 July 8-1918. Monday. Party Potan Port. Quinlan and I A dark day but start out warm and young Mr Cushin to go along the north shore of Bay of St. George out of the Islands. Hope to get as far north today as either Campbells Creek or Afrikamos Cove. Will be fine at least two days and it may be a third day is consumed. Later, went as far as Ship Cove and returned to Port-au-Port. From the eastern end of the Islands around the point southward and descending the heights consist of an alternating series of light colored and dark clay about 60m thick a thin and heavy beds. Banding is decided in the light beds. Crystalline are practically absent. No many flume are seen ripple with the crusts from 2 to 4 inches across. Fucoids are common and every now and then there three [illegible] mill large depressed gastropods. our fite 973. H (= 985 yards at 260). The crust is not, but thick. The crust by stepping turned a foot thick and under lin are of the best oreocutina described on July 6. Then the middle of the crust saw me gone of intraformational conglomerate. The general dip is 20° N. 20° W. overland As one proceed to the south before the crust turns over and we the above series dark colored continue into many headed [illegible] the surfaces of which creates fun crystal and bare large depressed gastropods and general occur if This cephalopod zone is about 20 feet thick, and about 200 foot along the same time series. small straight cephalopods. Also near near the base [illegible] and a small Billingsella like form (rare specimen). At the top we come upon pink red fine grained sandstones interbedded amid clay and then headed [illegible], some of the sandstone have angular pieces of intraformational conglomerate. We estimate this sandstone series to be about 100 feet thick (have a sample).

Walter 155 Stafford 923 200 200 1/4 X 8 {100} {80} {200} 385 farenheit = Reckman form - Joffin Clandrian 1/348 385 Tft / 1733 ft. 27 Below the sandstone come [illegible] laminated blue cloud dolomites, that are fine over-excavated (very smooth grains), ruffled, with some of interstratified some crystalline or limestone. One is edgewise englement. No joints of any kind, has except for Going back to the line of separation between the sandstone and the laminated dolomites are on just sum exactly sometimes 3 ft but with the cross from 1 to 2 miles across and filled in down to a depth of 3 to 5 inches. One two feet below occur Cyl/togyra, five feet below in a thinned bed of Cyl/togyra. The laminated beds are interbedded with the same fine grains smaller sandstone as different. Ruffling is constant and there are thick beds of crystalline limestone. Never occur the latter better developed anywhere the reason why one can so little own seeing in that the thin plates 1 limestone are washed away to from the edgewise engl. We estimate this beds to be at least 65 feet thick. We are near the end of an accessible section in Mary of San Core about 2 1/2 to 3 miles for the grains. Going a mile or more to the west we go down again the core has the same tendencies as is on the shale at Felipe's Core, where the dip reverses itself and goes up to the west in the next mile, at least 20 feet more of layer than reddish (weathered) sandstone reflect with shirty smooth surfaces that have furries, ruffled and some-circling. We see here [see me specimen] about four faults one duplicating about 100 feet of strata and another that brings up at least 40 feet older strata when the section again crosses on our way to the west. These are in place

28 July 8-1918 Bethel Park au Par decendant limestone lime mixed with the very fine grained sandstone. It is a very shallow marine deposit, sand flat with no organisms. In one place (the raised up fault) here the beds in my foot are very thin, dolomitic sandstone. This probably changed quite some when being got created. In many places we are interesting conglomerate ones of which are extensive, but not or persistent and in thick beds as in the higher dolomites associated with the fine grained sandstones. We then drove on and examined Campbells Creek Core, Abrahams Core and finally Shipos Core. In all of these places we are in the lower part of the sandstone series, or in the line of strike of the formation and do not get out further southward or as to get into older beds. We accordingly at Ships Core decided to turn back and return to Pat au Par. From Shipos Core we have a good and dry drive northward across the crater to Little Green Garden (8 miles) and on to Cape George the western headland of the Peninsula. As far as one can see there are in the distance no high ledges and the right hand makes down to the water. In Felix's Core we have the clearest evidence of an elevated sea beach at about 40 or 50 feet above the sea. A natural terrace upon the sea front here has its surface covered with rounded pebbles just as on the beach below. We can see this old beach and its islands on the beach on which are the picturesque houses and gardens. Spring on eastward we see farther inland and it must higher.

July 8 - 1918 North of Portan Pate 29 elevations, did sea cliffs form cliffs facing the pounding sea. This cliff and its slope took it a minute ero faster more above the present sea level. In resume one can see that the Redman Tm is not less than 1348 feet thick and that it gradually goes on into the lower sand- stone series with an thickness of 385 feet and the base not seen. All must be regarded as one series. If there is any Cambrian in it we do not have the evidence from the faunal side. In Ships Cove Isaac a diomite gone in the sandstone series that fall @milea in it from one inch to 1/2 inches across. This horizon is just only in the upper part of the lower 200 feet seen in Finleys Cove. As far as we have now seen all of the Ordovician formations from northy Romaine North - Portan Pate to Ships Cove have a faint uniform dip to the south. They seem to rise a little to the north but this may be local for the Ships Cove area or rather due to the fact that this place is more striking than the places to the east and west of it. If Finleys map is correct with the oldest formation about Cape St. these older hills Sengey - maybe due to the same anything at some time of the penin- sula or that the hills actually pitch a little to the north. Evidently the same anything we go about Portan Pate the higher the formations in the galped scale. This of course barring the faults that may duplicate the photos.

July 8-1918 Dentals notes As dental notes are more detailed I only report his notes does. “Beginning at the west end of the frarels and going south- west along the shore of Bay St George successive lower beds of the Bell- manum appear all dipping about 20°N, 20°W. Below the upper 155 feet of B. studied northwest of the frarels on July 6 can here ex- plained 1058 feet of similar strata composed of alternating lighter layers with light banding and hearing darker layers. These beds form a belt 920 fathoms wide stippled across the strike. Here we began to study the sequence going from in the series as we went on toward. The series continues without much change for an additional 201 feet, consisting of dolomite in lighter and darker beds alternating, the lighter more then bedded than the darker. Ripple marks are seen at various levels. Some crinoids present. Cryptoagra are well developed. In some of the layers. Choran & red layers of intraforma- tional conglomerate with fairly rounded pebbles, some of which are snicks lay. Bathstords are oft to occur in the layers with Crypto- gra, but more are seen in the lighter banded dolomite. “ This makes a total of 1413 feet below the Chazy. There are come on 20 feet of hearing bedded and more reddish dolomite with kuriononia cephalopods and many specimens of Rellingsella This is a well rounded faunal zone. Below this the dolomite series continues for about 180 much like those above but with a tendency to joint and reddish color [To Johnchurch away

July 8-1918 Quarters notes none of those pink strata are sandstones. See the two samples. This takes us to the point about one-half way to Iron O' Man Creve. Beyond this point we pass into very fine grained dense reddish sandstone which is about 100 feet thick. Our fossils were seen in it, but there are local pockets of intraformational conglomerates. The dip along here is 20° N., 25° W. "Long below the sandstone the sediments gradually change into more dense and red clay then reddish laminated dolomitic limestone which continues for a thickness of 80 feet. These beds show ripple marks at many levels -- in fact every few feet -- and edge-on intraformational conglomerates are developed to an extreme degree, forming cryptogms very few feet through the entire thickness. Sun-cracking was seen at a few levels only, and in some place gigantic ones, the polygons being 2 to 3 feet across. A section through this layer shows that the cracks are still more deep. They were about one inch wide and are filled with matrix of slightly different texture than that of the polygons. Layers of Cryptogms occur at frequent intervals through the beds. Just 3 feet below the giant sun-cracks is a thick layer of Cryptogma, with circles 2 feet across. "This brings us to Iron O' Man Creve, the same strata forming the point on each side, while the creve turns us back up into the higher sections. From here on to Felixo Creve the creve is cliffed and inaccessible but the slope is

July 8-1918 Quentin mine practically parallel to the strike. Felix ore is about seven acres and is divided into 2 parts by 2 small headlands. There has been considerable disturbance in this core. The eastern part has the structure of a syncline and is formed of the laminated series seen at Drum of Drum Core. In the middle part of the core the lower 40 feet of the laminated series is repeated by a fault running N.70 E. and dipping 70 S. 50 W. showing a distinct drag indicating that the west or hanging wall has gone down. "All the beds in this core show effects of metamorphism in them, the schiel is darker reddish than normal. [To John: whether this change appeared to be due to pressure fracturing my mind, and then the aerial status deposited the iron in the course of the process] "The laminated beds are here cut off by another fault run- ing N.70 E and dipping about 75 S.20 E, with a heavy drag and much fracturing of the footwall showing that the west wall has come up. This brings to view 50 feet of loose shales. These are dark and red and in bands 1/2 inch or so in thickness. The surfaces of these bands have a sort of metallic film and they are nearly covered with fine ridges little markings, mist mud cracks and ripples. "Below these layers and as traveling on to the outer edge of Felix Core is exposed about 120 feet of stiff brown shales con- sisting of reddish sandstone in thin beds alternating with some thinner bedded lagers. These are marked at various levels.

July 8 - 1918, Dunbars notes. by rifle marks and sun cracks, and after 1 ages I return for- material empl. "To sum up Felix Gore sea section as restored, Limestr sandstone laminal beds "Bring on tr Campbells Creek these same strata from the coast. And they continue still further forming the coast through Abrahams Ccre and Ships Core. "The strike of these strata at the latter place would carry them outside of Cape Sarge. Presume the dip again just across Campbells Creek and it is 20 deg N, 30 deg W. In the re- gion of Ships Core there is some undulating of the strata. Where we turned back to Abrahams Core and had supper at Mr. Aud- leys house. Returned to Port au Port after supper getting there at 9.30 P.M." This gives a thickness of 1968 fts of Bed or outcrop

July 9-1918 Potan Pok. Tuesday. Opens the morning writing up our notes. Duntar concluded to look over the section to the east of Potan Pok along the coast of Bay St. Sense explored for a mile and extending for another a mile of Romaine North, When he returned he was all non-plussed because all of the strata seemed to be dif- fersent from anything seen yesterday and therefore older. I then con- cluded not to leave Potan Pok until we had more light on the actual thickness of the Beellmantown. After lunch Duntar and Edwards made a traverse across the supposed lower beds, then across the top land air exposing anywhere about the Potan Pok side #Beellmantown# to the east shore of East Bay often we Sunday we saw about 240 feet of the top of the Beellmantown. This exposed area across the strike of the strata has a distance of a little more than 4300 feet. This therefore a total of about 2409 feet of Beellmantown. In resume it is as follows: Top of Beellmantown seen on Sunday afternoon 240 feet Honey pond area 4300 feet across, dip 20° = 1570 " = 1430 Thickness of cliff 100 " TOTAL 1910 " Duntar feels that this estimate is more reliable than the one of Saturday which gave 1998 feet (see page 2) Even on the face of Beellmantown is well known. The eastern Potan Pok section reveals the older Beellmantown and it may once be that to the western section there should be added another 100 feet or = 2068 feet.

July 9 - 1918. Duntan found a contact between the Forest Bellmantion and the Windsor atwr 1/4 miles east of the Catholic Church on the point ahead of Palau Park, shore of Bay St. George. The Bell- mantian here has a dip of 30° N. 33° W. and against it lies the Windsor green sandy shale dipping 10° S. 68° E. Over the western shore agains[t] the Windsor in deposits the Shales, decidedly conglomeritic and lays any way joins a foot rmeace worn of the Bellmantian embedded in the Windsor. He have two photos of the contact. Also a log range mine east to the Byssum at Romaines (2 miles) and in the far distance Indian Head 10 miles from one mine point. Another mine south east across the Bay St. George to Long Range 30 miles or so. West Sand cornul cliff, about 75. Total depth 1 cliff 100 feet Romaines gypsum 2 miles east If the Windsor dip is emtoward to Romaines Byssum then there were here about 1600 foot of strata beneath the gypsum. Yesterday we saw along the road side going up hill just north of Atkersons Cove some Windsor red conglomerate. Evident the road wall offing edge was a thin layer preserved in the dollars. The Windsor is then for everywhere a wall offing to- custom.

July 9 - 1918. The Gravel spits are the more infill. far old and defend Channel. From the south the wars are straight and have thrown of a big fan and wide spit. The northern me is somewhat lower and narrow. As oira can cut this channel and as or may small faults are present in this area it would seem as if we had here another case for a down-letting fault hood, with the rocks disturbed the sea ways could have cut out the neck, and a special times the ice probably plowed through it scouring it out farther. The present spits are probably of post-glacial origin. In regard to the basal Belemnite town on the other side of Bay St. George sandy Portran Park Dumfries notes as follows:- "The lower 200 feet are reddish, very fine and iron grained sandstone. Above this there is a gradual change into dolomite which in thinner bedded and bandred. On top of the suc-ceeding strata are the regular alternations of lighter and darker layers of dolomite. The thickness around here is 500 feet" St. Georges Peninsula now It is clear that the Windsor overlapped the folded Ordovician and in a basin very much like that of today. We have seen nothing as yet of the Silurian Cambrian here in the south, but we have seen three places at Portran Park where the contact between Belemnite town and Chage is broken up by distinct erosion unconformity. This confirms what the fossils show.

July 10-1918 Pot au Park Wednesday. Expected to get up in a fine sunny morning, but instead it rains lightly. It may clear enough for us to get away. At 10.30 A.M. we go aboard our boat. On the shore the shore is pretty and this part not less than 100 feet where the bottom is blue mud and thickly covered with Amygdaloidites. We are anchored in 15 feet of water and see hundreds of the echini with a few fork spray algy. The bottom for the shore the distance is about 500 feet. Flatheads are common but we do not see them until they slowly move about the bottom on the river far in front of our launch. After two hours of going in the launch we camp at 1 P.M. For a small river. Another place safe for the boat. We are now about 10 miles from where we started to start in. It is misty and raining and nothing can be done today. On each side of the river there is an elevated beach 15 feet high that we tend to the southward for a mile or more. At 3 P.M. in the mist Duncan and I walked along the shore north of Ben-mint's Brook for about 4 miles. Coming the brook from the far one at once came upon a long exposure (1/2 miles) of a dural amygdaloidal basalt showing the prair pillar structure very clear. The contact somewhat up-stream of this basalt (the red area marked t on Sharples maps) is from interrupted with a small exposure of sandy shale. Then the trip continues upstream for about 1/2 miles. Every now and then there are included gives a few feet thick of the sediment and in one place there a gore of about 20 feet across of volcanic breccia, bare a piece of it. Of this breccia one sees many patches all along the exposure. The amygdaloidal structure is wonderfully developed and in places made up one-half of the rock.

July 20-1918 Bennits Brook. To the north of the trap appear odales that as a rule are gneissic, often overthrown main horn and green gneissic odales. Only once did we see Haach odale, interwoven with thin beds (4 to 6 in) of fine grained sandstone. These odales continued for at least 1/2 miles north. Their structure is exceedingly complicated by warping and faulting so that one cannot make out the thickness, even guess at it. However there appears to be an overrolled repetition of the beds. The odales then give way to finer grained arkosic sandstones that become more and more coarse grained toward the north. Finally the pebbles attain the size of peas. The cryllostrates in proportion are increased, and the bedding is irregular almost like that of continental deposits that one appears to be of marine origin. The amount of red feldspar is striking, though far less quantity than the quartz particles. In the various samples. There can be no doubt that the basalts are flows and not dykes erupted quickly. We have however no data as to when these flows took place. Their structure is against the idea that they are intrusives.

July 11-1918. Table Head etc series near Potan Pok. Had a bad night in camp due to the cold of the night, slept little, felt all discouraged. Had breakfast and started south along the east shore of Earl Bay at 8:25 A.M. and got to the graphite locality at 9:50 A.M. As the place has no name I am calling it Table Head ever since the formation is of the rare breccia series. The graphite locality is about 2½ miles north of Potan Pok in a small down faulted area. The Chazy here has a dip of 26°N, 68°W. while the Table Head series has a dip of 26°N, 23°W. The distance across the ore is about 340 ft and at the north the Table Head series in again cut off by a fault. Here a sandstone and the Chazy have a dip of 25°N, 62°W. The Table Head series is here 123 ft thick with both ends cut off by faults. Table Head series in Creek Sea here The biggest let down is on the Chazy side, apparently, but there is nothing to prove it there. The shales seem like jamming up around into more sandy because some sand is very intermixed near the top of the whole series and there is at least me think (2-4 miles) sandstone 50 ft from the visible top here. Out of my locality come for 20 foot above the base of the shale. Nothing in time easy to say if the reason or not. The Creek Head sandstone base is not seen as it was faulted against the Table Head series, striking about 10 feet thick. This a medium grained light petrifield very hidden sandstone. It extends

July 11. Tattle Head Core and north along the shore for only 300 feet. This initially outcrops directly by the Crow Head Craglimestone Then all at once comes in the Crow conglomerate. This fault line is here for immediately back of it are the Tattle head Shales. The angular limestone faults are here enormous and two far from exceed 2 foot in diameter. It is a mass of angular broken of Chazy limestone with occasional small pieces of upper Bedlamton. Rarely one sees at once 4 or 5 feet seems to be seen, nor is there any fault to find together the limestone rather than its own debris. In one place one sees a block of upper conglomerate and lower Bedlamton conglomerate about 20 foot long by 6 foot thick. This a block in the Crow Head conglomerate. One half mile north of Tattle head core appears a mass of dark green sandy shales, as if it were inter bedded with the conglomerate. It looks to be the same shale seen at the northern end of the Tattle head core underlying the Crow head conglomerate. Three foot from pebbles only of it. Blue green About one mile north mud shale is squeezed in between the blocks. This may represent an intruded dyke of open shale, now crushed and re-jointed. Conglomerate and in place, part blocks of the shale are present. Then the conglomerate becomes finer and is mixed with the shale. Finally reaching the shale - conglomerate comes in once again not unlike there at the mouth of the exposure. This is an 1/2 sandstone may be about 10 feet thick. There underlying the Crow Head conglomerate, its own mudstone. About 4 miles north of Port au Port are just a few pebbles in shore lips or 3. See the specimen, label says put no 5 but 3 is correct. The next higher sandstones are common and have field for grains. Our small concretions. About 1 mile north of Port au Port are the nice if folded red and green

July 11. Tall Head Cove and mouth. The reddish chalk and sandstone, there are 3 sections taken for the book. Skin Shelly Crest. On the north side of this cliff is the zone of over three feet thick. Cav Shale argl, further the fossils are water worn, one of the fossils underneath. are fresh chunks. No shreds into the grey chalks. All is here much faded and in places marked. Then follows a course to cylomantic eric zone line have been previously. All stand on end, it's quite with folds are. Here the stone section ends and 5.40 P.M. we go aboard our boat and are taken back to Fox Island River camp. For three hours today all of us conduct collecting forms in the Tallo Shale series. The one surprising find is a large fossil milk Phyllogaster. Otherwise we get the same species collected in 1910, but far less of trilobites. In fact our collection of trilobites is for fine food. Just we could not get none. The forms are all marked ac- cording to zones, three in the chalks with proptilite, and 2 in the lime stone range with Proschikfos. The Cav Shale cylomante site like are the succeeding strata are much crushed and stored over one another. This for this reason that one cannot always determine the structures, and as for the throat arm of the Upper Ordovician zone this is generally out of the question. So back to camp and supper at 7 P.M.

42 July 12-1918, Friday, Long Point. A start at 6.30 and had breakfast at 7 A.M. We leave camp at Fox Island Point, and at 9 are on our way past round nears the motu to Long Point. We get to shore at 10.30 A.M. It stormed with thunder and lightning but with not much wind. We kept dry and without mishap. This morning all is fog and we can see only half one mile ahead. As we pass Fox Island we see through the glasses that the land consists of the coarse tessel flow that we examined on July 10 north of Bennett Bora. When we get to the Long Point shore about one-half miles south of the light house we come over to the other side. Here are exposed flint [clay half in shale] sandy shales interbedded with thin fine grained sandstones (2 to 4 inches) and an limy calcid. in the right occasional thin limestone. In the full mile we can see 70 to 100 feet of these strata, dips 20° N. 54°. These strata are replete with the species of Oolith stellithis (very slender, medium, and large), once or than any Richmond- cian strata shore seen before. From the center of this area to the top fossils come in fairly common. Bivalves are most common hackidords [?] for four [thoroughly matted oys], species, all common especially a semiplicate Plectambritis and Bradystria mites, and a Dalmarella. In one layer just below the bivalve zone occur Illaenus, and on this layer we also saw either Dendrocrinus or a similar armed Elytrocirrus. Towards the bottom a large Rafinesquina is common along with Tarrnits, a sponge. On the east shore of the Peninsula are exposed thin bedded mudstone a thick origin at about 5 miles south by three done estined limestone. We estimate the land to be 600 feet wide . . . of it

July 12. Long Point These strata underlie the green shale material about 300 feet, then may retrogress to some extent in the afternoon worked along the inner side of Long Point in the limestone series. What we have seen may amount to 50 feet thick as the beds strike away on the peninsula. We estimate to have seen at least 125' before the facing against the peninsula, but for this maybe the more correct thickness, just of strata. These limestones often have zones of rocks and other pockets interbedded with the dark colored argillaceous limestone. These beds are also riddled with Butcherfish. Some riffle in several places. Also considerable subangular with fragmental cylindrites gone. This all a very shallow water deposit. The limestones gradually go over into the shale series seen in the morning, have about 20 to 30 species. The last dip measured to the north of the light house was 20° N. 60 W. Took to 2½ miles south of the Long Point light and see again the thin beds here are seen this morning on the western side of the Peninsula. In all of this distance we are not more than 150 feet of Richmondian. Later from the boat it looked as if about the same 150 feet of Richmondian continued all the way into West Bay a nearly 1½ miles from Long Point light. In this distance the shore runs along the strata and the strata are but slightly undulating. As the marine clay or somewhat sticky sort ends, so the dip cliffs them near into the land contour, it appears that going north to the point of Long Point the two sets of strata come and other ending today and it is here at the base of western set that we get the best fossils. Let the top of the limestone clear me for a fine Pleurostites. The two sets of strata form partly into me another. All are very shallow water deposits and the Autogria Richmondian turns out the inner horizon. At 7:30 we got to our second camp site in West Bay about 1½ miles from Long Point. We are among the cypress, and a fine outlook across the inlet to the east. We came supper at 9:15 P.M. We are camped about 14 miles south of [illegible]

44 July 13 - 1918 Long Point. Started out with the launch at 8 A.M. and went north five miles. Then crossed the peninsula here 1500 feet wide and came out at Black Duck Cove just south of Black Duck Point. Here the sea throws out a thin bedded sandy clay material with some thin limestone. There are many bookshells in this place. One judges these beds to once be the Rich sandstone and harder than anything else, one saw yesterday on the eastern side of Long Point. Some of the sandstones are red like the Devon but the fossils are those of the Richmondian. Then Dunton walked north about 1/2 mile to Black Duck Point in Maryland and found it to be a coarse brick red decidedly cross-bedded sandstone devoid of fossils but clearly belonging to the Richmondian. It is not so because of the red color and the coarse nature of this sandstone that it was mistaken for half gray to the point in the bedded red sandstone he got specimens of Styphoroma fluctuosa (see the 2/8/1919). See Dunton's account of how let beyond. He then walked on the one half mile and found the oyster beds there to be like those we are collecting in Black Duck Cove. See his description on the next page. On the eastern shore of the Peninsula other we started in we collected a few things in the thin bedded blackish argillaceous limestone just above the series of limestone seen yesterday beneath the clay series of Long Point, slip 200/8/19. The limestones below are here wonderfully interesting for their cups of Monstrupus. Some of the heads are 3 feet in diameter and 2' high. In many places they pear one upon another; there may be half a stratum to 60 feet thick. Every where are scattered individual heads. We have several pictures of these cups. As a rule the heads

These vertical bypns reel extend at times so far they look verticall. Stand as they grew but in many cases they are slow hollowed up and are tumbled down. Single isolated heads and a few supported heads in small beds are common. They're also associated with the ups. There are many joints in these limestone but are exceedingly hard to give Grinnell's reparts (columns are common). Dunbar found one fine ejected like Hicropites. Dunbars note are as follows:- "Following around Black Duck Bay to Mist Point; the point and beyond consists of about 70 feet of thinned ? Richmondian Sandstone. Its moderately fine grained and very small grain tumbled, dipping about 30°. Long ledges running out into the water as far northeast as I can see good, in at least mile, at that point a little village with shutting off my view." extend 200 yards north & west. Dips 30° about 150 ft. Top of section not seen. stills out parallel with peninsula. Mist Point Dunbar has a much more detailed sketch and more ac- curate to nature. Richmondian Sandstone. Thicknes seems 75 feet but the thickness here may be 200 feet. Later we see that these rocks of Mist Point are the basal Devonian Series. Black Duck Bay Area point from mist. Road 600 yards 1300 feet -> Eastern edge cliffs about 100 feet high

"Following around Black Duck Bay to the north east succeeding limestone are seen just at the crater edge and extending out from the line cutting across the strata at a low angle. Dip about "It is a series of limy shale with orange Bruchophus interbedded with thin beds of limy sandstone. "The sandstone show fine ripple marks at many levels, and the interbedded greenish gray shale calcarenite have some fossils like those in the center of the bay, chiefly small hemispheric byssora atoms with aceros, and Plestambrites. Dip about 30 degrees" End of Clemons notes. As we stepped the peninsula across 600 yards and as the strata extend out in the water into the pints of Black Duck Bay about 1300 fath further this distance and a cliff 1500 gives a thickness of 1426 feet. Add to this 70 feet exposed in the cliffs and 50 feet for the Montygan limestone the total thickness of the seen and proved Richmondian is 1557 feet. The base we will see this afternoon. The limestone of Mill Point add another 100 feet = 1661 feet. The turned not be long many. In the afternoon we examined the crater north of our camp in about two miles. Here we first came upon the green and red shale and gray sandstones and clay marls seen on the east shore of East Bay. Then news a fault came in and to the north is a totally different series of strata, all of which are we succession and has referred to the Richmondian. The section as estimated by Clemons is as follows:

July 13. "Following the line for a distance of about 2 1/2 miles to the north and northeast, one passes through ~ great thicknesses of freemill, red and Haclish shale with thin shreds of sandstone, all steeply dipping edges and cut across by the same. These beds only dip about 60° E. There must be a fault here for the succeeding bed dips N. 5° W., and they form a continuous section of 1357 feet in thickness to the base of the Long Point Series [In the present all of these strata must be added to the Parsons series] "The sequence as measured in detail from the base up is as follows: 200 feet. Dark gray to black sandy shale and thin layers of sandstone, dip near N 60° W, 50° E. 200 feet. Freemill clay, even grained sandstone at base but becoming coarser at 15 feet up and passing into conglomerate with the pebbles mostly the size of peas and consisting of quartz, red feldspar, Haclish chert, dark shale etc. Among these are many scattered pebbles of later age which are angular, many of the latter of local material. They are often 6 with a or acorns. These beds become very massive in the upper half. Many round cannon ball-like concretions from 3 to 8 inches in diameter occur. The upper half of the beds consist of an alternation of bands or lenses of conglomerate and free grained sandstone. The upper beds are much jointed and fractured. Smaller a small headland, Fault 100 feet. Grey fine and even grained Haclish freemill shale, weathering dark red. Dip 45° N, 25° E.

July 13, Port Bay. 75 feet. Greenish gray shale sandstone. dips 53° N, 60° E. 215 feet. Fine finable shale like that above, varying from bluish to green and red and in the upper foot interlaid with thin bands of chert. This looks the equivalent of Stanley's slurs in No 5 seen about 2 miles south of these pits [The place we photographed as the pictures are taken], dips 70° N, 60° E. 2 feet gray sandstone 90 feet. Blackish gray fissile shale. 2 feet gray sandstone. 30 feet. Dark shale, partly improved. 90 feet. Greenish gray, very massive sandstone, standing vertically and due forming a headland, at the top grading into the next zone. 65 feet. Greenish brown shale and then slaty sandstone. 75 feet greenish Haull shale. 10 feet gray sandstone. 15 feet greenish shale. 110 feet. Alternating beds of greenish sandstone 2 to 5 feet thick with equal beds of shale. Many peculiar ripple marks on the under surface [Both?] flow structure recently described by J McClure as due to interference ripples]. 200 feet. Red and greenish shale. 40 feet. Interlaid large sandstone layers and often sandy shale. 30 feet. Greenish clud gray shale. 115 feet. Greenish gray sandstone more massive bed.

July 13. Ben Bay. 49 100 feet Dark greenish gray shale much marked and checked into pencil like pieces. Not well exposed. This = 1679 feet beneath the Richmondian. Shortest measured section of similar strata gives 14250 feet. Fault. I cannot tell from the exposure if this fault is of great significance or not. It may mean only a small dislocation or that the following section is in sequence, or there may be a great dislocation. [Richmondian] "120 feet. Marine light gray calcareous sandstone with limestone conglomerate at the base. Dip 50° N. 50° W. 10 feet. Greenish gray shale. 1 foot. Lags of conglomerate with limestone pebbles, angular, subangular and rounded, mostly small but some are 3 inches across. 300+ feet. Interval not exposed. Partly shale. 75 feet. Greenish shale with thin bands of fine sandstone. Dip 50° N. 50° W. 100 feet. Same dull beds very poorly exposed. 225+ feet. Unexposed interval 30 feet. Greenish gray and fissile shale. Dip 57° due N. 15 feet. Greenish gray shale interbedded with five paired bands of sandstone 2 to 4 inches thick. 10 feet. Dark gray to blackish fissile shale. 200 feet. Greenish gray shale interbedded with bands of fine grained calcareous sandstone. At 75 feet above base are lags eroded with the Stauropterus and Dictyorema. These beds are

10 July 13. Best Bay smaller with undulations in dip and the general dip seems gradually to swing to the west through the 200 foot shale and the succeeding unexposed interval. The average dip across the undulations at the profile line gone is N. about 15° W. 150 ± feet. Unexposed interval. 10 feet. Shale and Ling sandstone. Like those above. 100 feet. Unexposed interval. [The significance of this interval cannot yet determine it may mean they the base of the P. Recum or the M.] [recently by Prof. Swartout] 125 feet. Heavily bedded Chenacens Limestone in the first 50 feet, then becoming thinner bedded and more thinly with zones of freshwater shale and shaly thinly limestone. It strikes from a very steep cliff and directly underlies the Monty type zone. dip 43° N. 30° W. But some undulations was noted for a distance of a couple of miles to the northeast where the strike becomes parallel with the line.

July 14-1918, Sunday, Clam Cove. This Sunday morning and we are taking things easy. Hitting of months yesterday and packing four small boxes of goods. In the afternoon at 10 a.m. one went over from West Bay to climb Coney by the canyon road. The distance is 1/2 miles. We came to the shore practically vertical in a small pool (This turned out to be St. Dunman) is steeply standing high red soft coarse sandstone. At first the white ( = Lympus) These later found to be Indigosian stand with a dip of 620S,40E Farther north the Windsor shales are vertical and at 2 miles north by dip to the eastward. Found no faulting in this direction but later on found such near the brook. The "Windsor" of the south horn of Clam Cove turned out to be Lower Permian. Looking back to Clam Cove made the following sketch: maybe 700' high Do these a fault scarps? Precipitous cliffs in places around hundred feet high. These maybe of the Cow Head conglomerate. Freelands probably 200 foot high. Sea land 3 1/4 miles from mountain. cliff 260 260 Continued sea cliff Further south headland.

July 14. This red series is undoubtedly the "Trinodon". This brick red coarse sandstone to conglomerate interbedded with fine grained of red shaly sand-stone. It is all decidedly very banded and is rarely cut through by thin veins of gypsum. The pebbles in the conglomerate as in the sandstone are full kinds of materials off and hard those very quartz feldspar etc. In size the pebbles arrange from 1/4 to 3/8 inch thick layers occur up to one inch across. It all weather down rapidly and seems as has this material was a marine deposit and it reminds me much of the Triassic at New Haven. In some cases all the pebbles of whelkbone slope and hard horn have a varnish over them due to the samples. About 1/2 miles to south of the Trinodon of Clam Cove maybe seen the prolong faulted contact. These strata have the dip of the hard coconal carbon. The dip and strike is at right angles to the Trinodon There is a small broad flaring in near the northern end of Clam Cove. Here we measured the dips, Latom & Co. a number of high Ordovician fossils. Then I went to the south horn of the creek where pencil shale and red shales are all prominent. In the pen area that give a little lying apart a few fossils indicating different Ordovician. Now a stone from them the "Fiddle" Platyophia tipata, and an Arled 2 inch acorn (the pair in front show to fit). The beds are much more eroded, rifled, and round rolling due to wave motion.

July 14, Clam Cave. About 1/8 of a mile from the shore then strikes out a direct line- that makes a mile white stone dipping steeply into the land. The strike of this ridge is only that of the hill mountain and this limestone is full of joints and as Monocline and other faults. Also there occur at about here an iftle for the immigration. pools red are common it is concluded it like the Chagres bank of j & It is therefore more fruitful for the mining in one of the ridges mountains. In about 1/3 of a mile across the land then are two unrelated series of strata - Devonian, Redmondian and [illegible] and they must be separated by a fault. Evidently Long Point is due to faulting and the swell of St. Lamere is cut down in a series of step faults. Dunbars note regarding the strata seen to the south of Clam Bank Cave, and in the Helderbergian is as follows:- "The southern point of Clam Bank Cave is formed of greenish gray sandy shale showing up fine development of sun cracks. These beds are dipping steeply about S 20° E. In the next half mile there is a shallow cave where the strata strikes out in an angle across the shore or that succeeding down layers come in to the southward. About 200 feet of these red shales and their bedded black sandstone are exposed in this second cave. At the south end of this cave is exposed heavy beddened limestone and much cross-bedded deep red sandstone. In the middle of the cave the dip has gradually decreased to 38° S, 20° E, for the conglomerate. At this point about 50 feet of the cave is exposed. Two classes of pebbles are to be seen in the conglomerate. Both of them are well rounded or subrounded and foliated. Those are all of hard rocks, rein quartz, quartzite, as dark specks are all. Some of these are as large as 4 inches across.

July 14. Clam Bank Cove and Smith's Point. On the other hand there are chucks I didn't take but these are angular. For the next quarter mile the strata is parallel to the coast facing up along these rocks. As that forms a thickness of 200 feet of this conformative sandstone is exposed in the cliff and in ledges just of stone. This is the basal conformations of the Cretician and from here on with the strata cuts across the line or their succeeding dip layers are exposed, repeating the sections just seen and continuing for a total thickness of 1000 feet of brown Cretician stratum extending to the mouth of Trout Brook at Three Road Point, a distance I put at 2 1/2 miles. The Cretician section is as follows, beginning at the base: - 200 feet. Heavy bedded, much cross-bedded sandstone and conglomerate. Dark red. 400 feet. shale and thin Italy sandstone mostly red but over-set with greenish gray bands, grading into the following. Banded with small cracks and ripple marks. 100 feet. Greenish gray sandy shale and Italy sandstone with some interbedded clay bands which are replete with fossils for fun kinds. A Spirifer is most common and a small ostracoid. Other layers have Leperditia and other pelecypods, except the Camarocinines. Bearing very fine of the thin layers of Italy sandstone is ripple marked. Many layers are cemented with flinty material. 300 feet. Variegated beds of sandy shale and thin shaly sands.

"stro alternating red and jum, Riffle marked, he did not have time to hunt well on points but it seemed less frail. ifuns." 3450 Box 7 July 14-Note Book 1918 Page 1 Helderbergian About 1 mile northeast of the mouth of Trout Brook or of Three Rock T, along the shore. About 4 mi S. of Glam Bank Cove - C. O. Dunbar col. [illegible]

July 14. Clam Bank Cte and Smithward. On the other hand there are chunks I read it shale but these are angular. For the next quarter mile the strike is parallel to the craft going up being these beds. Or that forms a thick one of sort but I this conglomeratic sandstone is exposed in the cliff and in ledges just off further deeper continuous strat a distance 200 feet and successively m and rmin Rock Point, raies- d explo- but vary. mmy. Tracked with mud cracks and ripple marks. 100 feet greenish gray sandy shale and shaly sandstone with some interbedded lining bands which are replete with fossils in few kinds. A Spirifer is most common and a small one stelloid. Other layers have Leperiidites and other pelecypods, Brachia Camarceirinus, Acuf every one of the thin layers of shaly sandstone is ripple marked. Many layers are crowned with fluvicidal material. 300 feet. Transjucted beds of sandy shale and thin shaly sands.

stro alternating red and [illegible], Riffle marked, he did not have time to hunt well for fossils but it seemed less fossil. ifuns.

July 15—1918. Sunday. West Bay. After breakfast started south east around West Bay to the head into Piccadilly Bay. Car contains red film and black (fine) like they were from camp, much crushed and marked shales with them sometimes. They are of the oysterfaced series, and are probably ejected if from the profile. This is about 2½ miles south of Cape Horn where we came upon blue to black limestone shale and some concretely peeling limestones. One are for light chlorite clay. These strata are related with a peculiar profittile fauna that contain faunal elements of the Beadmontown and Hornawkill. Small Phyllopodites Tetraraphites, Haldymorphites and many other forms occur here. Also a Longina is common. Otherwise nothing. If this is of the Tate head series it is a different and seeming pelm fauna than this one. At the head that distinguishes West Bay from Piccadilly Bay occurs the Car Head Concretions. The man makes a left and side ridge and the thickness may be 500 feet or so. He could not measure it because no bedding can be seen. The Car Head concretions more shows bedding planes. The fragments are small under 1½ inches thick at times one sees piece up to 4 inches. No large masses occur here. All the fragments are of the Chepy and are angular. In Piccadilly Bay at the end of the Car Head cowl, we again came upon the Hornawkill proft-lite fauna but the fauna is far poor developed. Bring further into Piccadilly Bay, after an unrefined space one comes upon another up series of Car Head concretions. Here the fragments are also small but there are pieces up to 2 feet across. This second group must be faulted in to repeat the same succession as...

July 15: Crest Bay. Further south in Piccadilly Bay I shot out the sea bed to the then Causal run to Middle Peninsula and here for a quarter of mile are exposed brick red shale, and chief layers. They seem Hett overlies part of the variegated series. Today we learned little in relation to the succession. The shots are too much marked to determine their thickness. Out side of the limit of grapto-lites collected the day was considered a blank. There too there are wider areas of low craft with no well exposure. It now seems to me that the sequence in northern Newfoundland is the Beekmantown to Table Head series, a distance followed by the Corn Head conglomerate and the following variegated shale and coarse sandstone series; (3) the thick Richmondian series; a long band inter- vened; (4) the Lower Devonian series; and (5) the long Caribou formation sequence. Dunton describes the Table Head series as follows: "Black shales, and li. Ten feet of black shale with grapto-lites is exposed, and below this 20 to 30 feet of black chert with some inter-bedded black shale, grading towards the top into finely flaked chert and shale. Then followed by a considerable thickness of black carbonaceous shale with thin bands of grayish head carbonaceous li., all much cracked. The thickness is about 200 feet but Prof. Schuchert thinks several hundred feet. Then an unexposed interval of 1/8 mile to the Corn Head coal.

First Bay marshen navigated beds. Normanville Tie. [illegible] Car Frank Cupronate Ridge Fault Leased Normanville Tr. Peadell Bay Northeast [illegible] Middle Peninsula strips of shales, Ironshot mine general than drawn. 191 Re: case in Tynells remarks in this area

July 16 - Tuesday. Middle Point. Rained hard last night and this morning there is a raining fog. By 10 A.M., it has cleared enough to start on our journey. Our boat takes us across to the middle of the western side of Middle Point but we see no rocks. We remain in the boat until within a mile of the northern extremity and then proceed on Middle Point (= Middle Peninsula). On shore, there is a [illegible] crushed series of thinly bedded sandstone separated by thin zones of shale all of which are to be seen. [illegible] of greenish or light blue clay. Towards the joint orthogon of the strata are to be seen on either shore. On the eastern side about 1 mile from the point [illegible] spindles of a lime slate with Richardsonian prints like those found at Clear Banks Cove. Other loose pieces were seen along the shore in the next half mile southward. Kept the first slate formed on hand here. These data are [illegible] by boat [illegible] We then proceed about two miles more south-eastward and south south-half of the long shores. Here we are in the consolidated shale series seen in the north part of mine of the Richardsonian sandstone and conglomerate are present. The upper part of the section resembles that found at East Bay. Here, we continue to within 1/2 mile of the Dominion Dam and [illegible] Shale Coquimbo. Here they are unconformably overlain by the Brinkon series. [illegible] All of these shales are named by Hardy as Brinkon series. The genus has a green one foot thick of bi calycomate and the small perforate shell animal. The Brinkon lies nearly horizontal but is undulatory due to deformation. It begins with a braided bed 6 to 10 feet thick. The borders are subangular and a size up to nearly 2 feet across. They appear to be all of the white and black fine grained sandstone and dolomite of the Bedlamation. Above lie thinly bedded shale, sandstone and shales, some sandstones and four conglomerates. A peculiar feature of the chosen beds are their contorted and even folded nature due to slippage while the ones were still soft. [illegible] above and between the beds are granular stratified. See the photos. On these lower beds I saw a few small [illegible] and a rare

60 July 16. Middle Point to near Dominion Quarry. Specimen of the common tree studied but here only half the size of those in the dolomite, the drinon along the shore shows a thickness of about 60 ft. It is exposed along the coast for one-half mile. Then it is faulted against the Talle Head series that is exposed herein and from a little upon a few hundred feet when the drinon is again present up to the Chazy rocks. The latter then continue to the quarry of the Dominion Iron and Steel Co, 4 miles from Port au Port. Of the Talle Head series there is just exposed here are the thin fossil frutle limestone seen on July 10 and that have a thickness of 25 ft. The immediately found three entire specimen of Ambyzium matton and themong payments. One large one half but once more darked. The entire peninsula sticks above sea level at most 8 feet and in then covered with from 6 to 8 feet of peat. At the bottom of the peat are the roots and stems of a stunted forest overwhelmed by the great flora of little plants, Crethuson and many other arctic plants. One walks on it like on a mattress. No trees are on the peninsula, but in a few places there are some stunted emifs in clusters. Denton was greatly interested in this flora, and it reminded me of Labrador and less so of Greenland. There one more great faults on either end of the tranjugated series as one of the sandstone are present, and at the other end there is no Cnr Head conglomerate and the associated sandstone. It is known interesting to see that it is a tranjugated series that follows beneath the Richmondian.

July 16. Middle Point. Our third camp is beside a small horn about one mile east of the old mining farm and about 50 Quarries. This the first camp yet but we will leave it tomorrow. Where the Chazy comes in it is overlain by the Windor Shale or broken amyloante being present. Therefore the Chazy over-lies all the Ord. formations. The horn bottom in which our camp is pitched also has Windsor in it with sides of Chazy. Evidently the region is much faulted by small shifts. If for one day we have done in the south the relations of the Table Head series to the Chazy, nor to the Cow Head amyloante. All contacts are faulted. As the top of the Chazy is faulted we do not know its entire thickness. Of the Table Head series we do not know its thickness at all.

62 July 17 - 1918. Wednesday. Dominion Q. to Bluff Head. The first day in Newfoundland. Before morning. We walked two hours at the Campyge bed about 1/2 mile southwest of the Dominion Quarries, but about one degree entire trilobite. The boat went to Port au Port from rail and gasoline. We had an early lunch and left our third camp at noon in the soft shore and Bluff Head. As we got toward the east side are here a fine area of the Osts boundary of the land, it is plain that the limestone strikes once and once into the sea by the strike of the strike on the Ont. Then the land as are for meander. This is probably the reason why one does not see the li in Hunter Arm. Further more as we go north we get into grayw dolomite. At 2:30 P.M. are we within 1/2 mile of Bluff Head and so ashore, we begin with some marked beds of red shale and olive green sandstone and are so conglomerate like those noted on July 11. It's the continuation of the section then uncompleted, soon all is interbedded coarse sandstones with finer conglomerates like those below. and arkose conglomerates in one place there is a 10 foot bed of conglomerate the fragments of which are made up of the formation itself, ranging from coarse sandstone and shaly sandstone. The boulders are well rounded and range up in size Another thinning gray ones with a patch of Conglomerate. to 18 rocks across. That is 700 to 800 feet of these sandstone. Then a vertical standing little of red shale and dark blue shale interbedded with the sandstone, Then a valley and a gravel fill, it is about 1/4 mile across this core to other. the arches can again expand, here are small marked red shales with zones of then fiddler sandstones. Then a very much crushed zone of the olive-green sandstone with large masses of limestone. The latter are broken for an extent and maybe of the Pabandonion.

Bluff Head to Cole River At first I think the pencil material is diorite but it soon becomes plain farther around towards the north where there is exposed a red thinnning of the upper clivins from sandstone. Bluff Head sticks boldly through the sandstone. Below is the biellared lava like that seen on July 11 and above it the red amygdaloidal tuff while higher the main mass is of a pencil diorite. We have several pictures to try out this later injections into the diorite. Also have several samples. At the contact we see no very small are oretamphrons. The sandstone is of coarse mud level and shale has become flint-like. The lack of crushed against amorphous is striking. Quinton thinks the pillowed lava is a very recent intrusion, even post-Paleogic. This does not seem to me to be true. As we go along the craft north to Cole River = deepentine river we again seem to be in the varigated shale series for several miles and then for about 1/2 mile come up to the river on south, thin red dull dark shale interbedded with with sometimes a limestone. These from the boat seem to be the upper Richmondian series. If so this will be an interesting occurrence. The next day the trees proved to be li = Table Head series = later As we came along the craft we see that Fox Island is cut off by the sea train plane that stands at about 170 foot above sea level. This same level as elevated thinner over an at several places along the main land. In place it is round another cross bedded sand showing plainly that the sea was once here. Back of the ascending slope there and the low cliff. Another elevating tract is at about 25-foot and is crowned with head material, below this. We camp at Cole River (a door stilling hithers man flee) at 7 P.M.

[After seeing the thin bedded limestone-sandstone-calyomate series of Middle Crome on August 28th I concluded that the correlation made in page 67 is in error. This division of the post Carrigatull series described in pages 189, 189a and 190.]

July 18-1918, Thursday. Coal River At 8 A.M. we start with the Trail smith / Coal R. to see the top of the origination series and then the higher thin folded series. The [illegible] series is at hand 4 miles south of Coal River. Near high crushed red shales on either hand. After about 1/2 mile north there are 2 or 3 grams of heavy loddled blue fine medium grained sandstone and thick beds of dark blue-blue shale with a little of mica. A half mile further north there loddled fine grained purplish-gray sandstone are interlaid with greenish slate flint shales. All are highly involved and more or less marked. Over are given conglomerates but not like the Cow Head Limestone conglomerate from which they can be seen, not even fragments. We regard it all as of the series [illegible] (the great base of Red Rock Crag) We again go north about 1 1/2 miles south of Coal River and from here north is an ascending section. to the river there is a highly involved marked out involved series of thin[thin?] loddled sandstones and dark shale. Our may fragments are interformational conglomerates [illegible] in a direction as thick over 2 feet thick and around others of bottle conglomerate seemingly are deriving from as from the Table Head Series. the same formation? But a ornamentally marked and sheared series, We have four pictures for titles from the area. The series must be faulted at both ends to bring up this form mass into the younger origination region. At the south end of the 1/2 mile of Table Head series just described there on an effusive mass of the fillers have been seen or often here. There is another one just north of the Coal river mouth. Near the northern and we get [illegible], [illegible] and Lignite coal near the southern end and foot of ft. The thickness of the series cannot be even estimated though it is intensely folded in the entire 1/2 mile distance seemingly the thickness cannot be less than 700 feet and may be a great deal thicker. Once there one half of the series is shale, green and dark to brown-black limestones. The other half is made of crasings of red sandstone and densely blue [illegible] that folded in thick[thin?] (blue mud?)

66 Cole River - Bay of Islands. Frocks are exceedingly scarce, the whole is a shallow water deposit outcrop we see no ripples nor sea-creeing. Just north of the river mouth igneous man and chalus of the navigated seem cut again fresh. There at least not 700 yrs then another pillow lava effusive appears, there leaves them intact for % mile with just limestone inclusion. Then all is distinct mod to and including Bear Head, Hawleys only cals or we trip but it is one distinct in serpentine. Just to the north of Bear Head [in Bear Cove] there is an isolated reef sticking out of the sea and another smaller one near the land. The outer one was visited by Denton, he states there is about 100 feet of limestone conglomerate here, the parts of limestone up to 3 foot long are generally flat ones and subangular. It in Hawleys and the Cow Head Conglomerate but one higher in the navigated series. From Bear Head north for 2 to 3 miles the hard land between the distinct areas shows along the coast the navigated seem, there it is less marked and lies fairly evenly bedded dipping to the northeast at about 30 to 35 degrees. We left Coral River at 2.45 P.M. and at 7 P.M. we are opposite Woody Island. We got to [illegible] Curling in Bay of Islands at 8.45 P.M. The distance run today was 35 miles, stopping at Tourist Hotel. In going along through the islands of the bay and Hunter Arm one gets the impression that the exposed rocks are of the navigated series, but in the [illegible] there might be little the Table Head Series or even the upper Richmondian.

July 19. Friday Humber Arm He started at 9 A.M. with James O' Routes launch of the Humber Arm in a dark morning. It soon began to rain and it continued or all day. The hardest raining day of the trip. It is our plain that all of Romley's Cambrian-Ordovician (his green area) is Pottergrie. He went up the Humber river about 3½ miles and went ashore at the "Limestone Quarry" where marble is quarried in the paper mills. This is a white and yellowish marble with blue grays standing nearly vertical. It is once or less cracked and in another place was somewhat schistose. See the samples. One mile down stream we saw a dark micaceous schist with grains of schistose limestone. It is much crinkled and deformed. Another mile down stream in Martle Head and it appears to be the same marble seen farther up stream. This marble is all of 3000 feet thick and may considerably exceed this thickness. The schist is as thick though the marble appears to be thicker. He saw these beds for 3½ miles and as the dip is nearly vertical and as the river cuts practically across the strike it is certain that the thickness in fault of what I saw from the railway window in 1900 as ledged rock is truly such that this is an area of vertical strata of not less than 7 to 8 miles across. As this is nothing Paleogric looking at my these rivers and as they are far more metamorphosed than the deformed Paleogrics it is plain that they cannot be regarded as other than a Pottergrie age. The thickness appears to very great. The contact between the Pottergrie highland and the Paleogric lowland along the river is hurried beneath a thick mantle of present sand and boulders. The latter is the old delta of the Humber when the sea level stood above.

68 July 19. Humbu Arm 70 to 200 feet dipper than are. When we got struck 1 mile from the contact ore are dight inclined somewhat metamafilled blue shales and thin zones of sandstone with decided dips having the strike of the Petergore mountains. Farther westward appear red shales along with green shales and thin zones of sandstone cleary of the varigeted series. As for this reason there seem indicated to place all of these strata in the variegated series. It seems hardly possible that the thick Bear mountain dolomite and sandstones could be under the sand delta, and it is certain that if to it is added the Chazy and Table Head series, there will make room due for them between the Petergore and the Variegated series. On the other hand that is here far more marble than the Ordovician caves for. Furthermore the ochist series is something independent of the Ordovician. July 20-1918 Saturday. Curling. It is still raining hard this morning and did not start until 4 p.m. In the morning called on Mr. J. F. Thorne to see what I found him in the supplies in the boat. The bill is $181.38 of which for food is $129.37. The remainder are camp and boat utensils. He will need about 200 gallons of gasoline @ .05 to .06 per gallon, = $10 to 12.00. The oil are get of Mr. Lilly who is agent for the Standard Oil Co. he had to buy 3 more wooden buggies as we now have only three wooden kayaks to slip in. I also see that the trip will cost not far from $2000. The boat cost $640. Total $2640 to Dr. Tyrell. He has paid for it or the boat belongs to Dr. Tyrell.

July 21-1918, Sunday. Curling A fine cool morning. Could not get breakfast until 9.30. He started work at 10 A.M. In the first cut on the railway west of the station they and third bedded light-grey slate. are seen quartzites standing in edge. The interbedded lime shales along close to Schistosity. The strike of the strata is that of the NE to the ESE, NOE 10 degrees. There strikes NNE at all in harmony with the general trend of the NE of Strathgrym map. JN. The thickness of the completion is about 200 feet. In general the dips is stuff at the north. All through the Hunter Arms I think the strata are of the Mancunian series, thank the alternation of green and red shales is less prominent here than to the south. The series is darker or far as the shales is concerned, and the sandstones lighter. While there is at least one very thick green shale we see now. The red slate quarries are in this green bed side of Hunter Arms. I at Sandmuidge a few hundred yards more are again in an interbedded sandstone-shale series. The dips here is to the west with the strata almost on end. Are they're have here thus folding where the sandstones are relieved with minute low dips in between with the shales. At 1/2 miles west of Curling Station in a cut on the railway the sandstones are nearly horizontal, but by green left green in color. All along here the strata are interbedded sandstone and shales. The shales make a laminar or hard (with slate) and the sandstone with quartzites. Along the railway at the base of RNT. On which our attention is attracted to fallen blocks of limestone and carbonate. Looking to the very tip of the mountain we see a nearly horizontally lying member of the Limestone, appearing to be 50 feet thick. The joints are flattened 1/2 to 1 inch. In other places they are as a rule much smaller, thirds and up to 6 or 8 inches long, all subhorizontal. It reminds limestone of the member seen at Bear Creek seen on July 18 (see page 66). The rest of the cut is made up of thick shales with interbedded earthy lime in beds from 3 to 12 inches thick. This thin bedded lime green may be 30 to 40 feet thick. Going on southward and for another mile we come upon another lime crust, that maybe the one seen before, but it seems to be a very fine crust (on the topography). Maybe the one seen before, but it seems to be a very fine crust. Between the two places there is lime shale, much prettier or hard into completely slate. The (50 miles post 409) (more miles from 408 or four miles of Curling Station)

July 21. Curling. bottles of the li appear to be the Fortem of li beds of the Tottelth The material is calcareous and derived from the Cherty series, series, as it gives us another check on the age of these rocks. The li. Congl. of [illegible] Table Head area Bear Cove also appears to be of the Table Head series. In the afternoon marched six miles along the ocean road out of Curling and Lanmoo Spring Point Light. toward Humbert Arm Light House, then Forestall Out. Inside we saw perfect beds of li. Congl. fallen in the cliff atore. We can judge the main of the top of the Out, take from 40 to 50 feet thick. The bottles are all subrounded, foot pieces from 1/2 to 1 1/2 [illegible] more thick, and in length up to 18 inches. Some are very sand stone but most [illegible] like those of the Table Head series. of the pieces are impure li. There is also a little chert. The pieces are irregular jacked together and then in very little cement between the pieces, apparently the same About one mile further on we again come upon li. Congl. and this an occurrence [illegible] time in place. We can see that there are thin gums of the li. Congl. intercalated into slate, the whole making a thickness of about 90 feet. First teller them is 10 feet of li. Congl. then 3 feet of slate, 6 feet of li. Congl., 50 feet of shale, then several more li. Congl. with inter- calated with shale each from 6" to 12" thick. The dip of the beds is 60° N. 20° E. One-quarter mile more over we see the intercalated slate and then bedded slate than an impure li. Over the morning connection with li. Congl. on the railway, [illegible] Curts Brook Where the road crosses a large rapid stream this one hard blue shale, dipping 46° direct west. the dip seems to be S. 45° W. One-quarter mile north of the stream we are again in li. Congl. There, [illegible] One-quarter mile further with the depth 20 N. 30° W. In the next mile we see much of blue shale with an occasional this band of sandstone in impure li. They are in places much consolidated and the dip is [illegible] I'm almost benighted. Much of the time we are on the strike.

layer of li. coal, about 10 feet thick dipping 40 to N, 10 E. Below are 30 feet of coal beds continuing in bands of li. interbedded with shale in which fossils are contained and thence immediately downward the top the conglomerate rocks Above the lophut member layer is an additional 75-foot conglomerate like those below.

July 22, Monday. Mistle Head, Started with James' launch at 8.30 for Burnt nira and got 9 miles Jim Curley by 10.30. Then walked east one mile to mile post 376. Are dwell about here to the east for some miles in a sandy highly micaceous schist and apparently The cryol mine even longer into north. and apparent overlaid with py and red cry olomates. The thickness must be very great. The granite is mil in eight mn even as folding in the stream. It may be ten miles further along the railway to the granite. Duncan visited the schist in Stady for 3 miles The "Limestone Quarry" begins at about 397 1/2 miles and continues For further descript see page 67. along the humber (along the strike) for about one mile. I learn the strike Duncan estimates the thickness at 1500 feet but it may be twice as thick as only to the crest of the mountain. He measured these magnesian limestone practically stand on end and have a strike 1 They in more than one mile there is schist These schists are not so much metamorphosed further east and are different in character, crit with an estimated thickness 1 mi far from me miles. At the main station on the schist series there is a thin-edged blue chalk limestone that in many ways reminds of Ordovician (Redmanation) in its surface weathering effects. (See the sample). Further down streams this is another thick mass of the same kind of delomite and offrite on another side of the humber the contact between the delomites and schist is once shown on the face of the mountain. From here with me estimated the thickness up to the center of the syncline as about 3700 feet thick. From due north to the nine north all in the same and in the air very normal delomites of the western limb of the syncline. These strata end with their north. edges sharply along the strike and make a precipitous mountain face trending and about 1/2 mile across the strike from the lark granite extreme. At mile post 401 along the railway but far better along the slope may be seen several hundred feet of a pinkish and grey thin and thick bedded delomite in magnesian limestone. The dip of these strata is from first decline's shown along the rim, 58 N. 750 W. The exposed stratigraph for 150 yards = 378 feet of thickness. along the rim the dip is 65 N. 85 W.

July 22 Monday. Marble Head. (8 miles thia) (Cruss myplan pic) [illegible] In these strata we saw one grey of interfoliated conglomerate, and another one(s") of very laminated heddry that reminded much of Cryptogramma formation. Here then are drawn in beds, with the slighty marvy layers. As the dip of these old units is the reverse of those of the first seen, and as they are less crushed and metamorphosed I am convinced that they are of the Reedman turn, and apparently of the basal Beddeman turn. [illegible] The great Post-Ordovician section, The Beddeman turn is somewhat obscured beyond mile post 401, and the ground is covered up to about 75-foot above water level by sand and huddle bits of a former delta of this Hudson when the oceanic level stood more than 100 feet higher than now. It is about ½ mile westward before one sees slaty dark blue shale. [illegible] One then goes past Humbin Mount station to at least mile post and telesec like 403 in the mud metamorphosed slate and but little quartzite telegraph dip is to the south, ranging from S 60 W T N 70 W. gives are to be seen. From about mile post 40½ to Curling (406 miles [illegible]) we see some grey of quartzite and a particular thick grey joint underrun with the red slate quarries. In this grey I very clearly huddled orange dark green and also with red for many white field bands. sometimes I saw much of the quartz conglomerate (about half the way) as seen or covered on July 10 and 11 in the upper part of the marigold series, then The thick red shale grey is divided by green shales and gives 9 the next deep slant and I made a more detailed section these strata: quartzite and they extend for about 1½ miles up to Curling village.

July 22. Marble Head. I am now convinced that we have found the base of the Ordovician at mile post 401. If we could see the actual contact between the Beidmantown, and the Portoroe marbles they would more certainly be an angular unconformity has. In any event Marble Head and all the beds of the Humbler from mile post 401 are of Portogric age. Dunton for a time thought that the Portorgie marbles folded over again (and united with the Beidmantown making the two a continuous series, to me is an impossibility for these reasons. The Portorgic marbles are of two series and the first one is altogether too thick for the Beidmantown. Then there is nothing that I know of in the Ord. To fill up the place of the schist series a mile thick unless we say that the variegated series is the equivalent, or that over the second marble must be the equivalent of the first one and the structure quite different from what it appears. Dunton takes the view that all of the drifts are of Portorgic age, and that the variegated series rests on them. East of the red slate quarries there is a zone of them hidden in, and blue shales with zones of li., enyl. It appears to be the same li., enyl. seen yesterday to the east of Gurling. What the relations are to the red shales was not determined, the next day it was clear that they were headed and is therefore myself born in the north (Hoot and my sketch tunnel of this evening. They are looking up all animals for the Reid Railway Co. They report 13 feet of clean coal in the Ordov again (? South Branch). The total thickness of the bed is nearer 30 feet.

July 23 - 1918. Tuesday. Curling. Raining again today but not so hard as last Friday. Re-examined the western part of Curling to the third quartzite felsur, the red and grey slate quarries. This section is described in more detail by me. See page 81. In the afternoon paid Mr. Thorne for sampling $20, Mr. Lilly $110 for oil, Mrs. Lemming for service $90, and Mr. O'Rourke $75, for service. The strata of Hunter Arm are all, seemingly, of the navigated series and the section rises from east to west. The metamorphism and crushing is most marked in the east and is not decided in the first two 1/2 miles where some of the shale, tate on schist and talcose character (a yellow-white smooth clay). In the afternoon Dunbar made an attempt to get to the mountains to the north of Hunter river and to the north of the abandoned Hunter rally a more antique rally than the present one. Here are exposed unmistakable Upper Beekmantown strata with Ceratites, and below these he saw an abundance of lower spires fossils. For them proves the presence of the Beekmantown. Above the Beck- mantown are thin and much darker irregular a thinly like li. that are cer- tains of the Chazy. What the relations of these beds are to the great marble axis could not, however, be determined. Dunbar is still inclined to think that the marble series is Beekmantown - Upper Cambrian but cannot account for the greater thickness of the marbles than anything we know (2000 feet). Accordingly he would explain the relation of the Beekmantown - Marble series as one due to faulting, and that the marble is Post-cambrian. (In the geology map this page 52-)

July 24th 1918 Wednesday Middle Arm Bay of Hinds Left Curling at 8:30 in a dark stormy morning. It rained hard during the night. At 11:45 we are inside of Middle Arm and in the fishing camp house of James O'Roake on Croft. It is here that he comes to the face to catch kenny until late January. His name is Ben Brads Croft. Before lunch we looked at the rocks but so far have failed to determine the age of the strata. It maybe that we are in the Lower Cambrian. They are dark blue-black shale with thin beds of limy sandstone and partly there may also be many thin beds of laminated sandstones. Crinite spores are present considerably parting limestone there are also occasional thin gyres of intraformational conglomerate and at least one gyre of conglomerate in which the fossils are up to 3 inches thick as the specimens of Lower Cambrian age, but many horizons in the laminated sandstone are many fragments of their shell lingulids. It is this evidence that leads me to believe that there was due a joint thickness of L.C. To the north from camp there are parallel beds and thin conglomerate. We tried by aim at this area in the evening but found no fossil evidence very little. There are many thin gyres of intraformational conglomerates and at least two thin ones, one about 4 feet thick the other 6 foot thick. In those two conglomerates the pebbles are all of thin flat pieces face size up to 12 and from 18 inches across. They are usually of two thirds and both look to me like the strata in which the crinoids creeps. The small pebbles are all well rounded but the large pieces may be quite angular. To me it seemed that the pebbles came out yet hard when they were incorporated in the conglomerate for many are bent to fit into other pieces and one sometimes crooked. The dip of this series is very hard to make from 30 to 45, more usually which I cannot remember. I do not think this formation can be the Tally Head series for we then should have found some of its fossils. Furthermore there are not enough of limestones to agree with the T.H. formation. On the other hand the

July 24. Middle Arm. 77 form of thick lelled liguila in Ordic is a decided character for Cambrian age. If it is not Loro Camh, it may be that it is Upper Cambrian. Certainly it does not agree with any formation seen before. The thickness is considerable and may be several thousands of feet (1020 fathms) In the afternoon out boat troll up to the head of Middle Arm To the northward in Penguin Arm and to the southward in South Arm at Penquin Head + to the high head known as Penguin Head. We went ashore and found it a thengon from me truth. Take the lorn dolomite seen at "Limestone Quarry" in the stream. The thickness appears and True what we had in the streamer, about 1500 This lend seems to be of quiet face, rights raised, To 2000 feet. Then followed the equivalent of the schist series, here far [around the word] less metamorphosed and lying in undulating and locally marked folds. The same is at the pretty Ragland Head. It's an immense magnesian series and shows creathery phenomena like that seen at the outer station along the Drembar River. In the Towards the south-east across the big Ragnachris distance we saw the several or higher and thicker dolomite series all [orth-] dipping Towards the east and striking about N. 30° E. See page 83. There is no doubt that one estimate of the thickness of the Portugese seen in the streamer is correct. Now we see that there is a succession towards the east and that the two marble series are distinct, separated by the middle schist, and followed to the east by another and distinct schists. The two marbles are not duplicates of one another. Accordingly the great Portuguese series is a continuous sequence and the two marbles are of different ages separated by the third schist, here in Middle Arm - a long-shaly series also of great thickness. To the east of the supposed Cambrian series there is another formation before after D. had seen it; I.C. of Ormy Bay leaves certain that the style belong one side of I.C. age. (See page) The Portuguese marbles come in. This he did not discerning. The two have normal dips. A3

July 25-1918 Thursday. Day to Bonne Bay. We leave Middle Arm at 9 A.M. in a fair day. Go near to the south of Eagle Island we see that the sea has cut its top floor about 70 feet above present sea-level. On the top is a thin mantle of gravel. A good deal of the strata of Eagle Island are of a Hood and shale, with plenty sandstone. We are camped at 4:30 P.M. in the middle of East Arm on the Lower Cambrian strata, a short distance southeast of the main town saw mill. This mill is located on Deer Brook. The flies are terrible. On rock. Prediction for rain tomorrow. We walked about a half mile along the shore southeast of the arm and saw the Lower Cambrian. No particular results but two cysts and a wheel of Cleavelandus. July 26-1918 Friday. East Arm of Bonne Bay. This, midges and mosquitoes terrible. It is misting and raining. After a miserable breakfast we along the shore towards the mouth of the arm, and past the main town saw mill. The strata of the Lower Cambrian keep of the south-easterly dip to the saw mill and for a ½ mile further they then reverse their dip and dip southerly. The material are shales, and sandy shales with considerable light pink and marlstone quartzites. Near one Cleavelandus (John Strait). Also considerable siltstones are present. Fossils should be common if there out for this. The dip from the Deer Creek below camp to Robinsons station is in the average 3:15° E. Just past the saw mill they are picked up a number of granite specimens in masses that come down the brook. If they do then the Lower Cambrian beds in these granites. It is very possible that the L.C. does not lie on the granite but has overlain them before erosion of the Palagonite. So was at this work that we began our section of 1910 and continued up the north shore towards the head of the

July 26. East Arm of Bonne Bay. and almost into Brett Bay. arm. My description of it then tallies and what are so now. As one looks at the head land that has the East arm tides in with side of it, has the strata dipping also to the southeast just as I drew it in my note book of 1900. The north shore of East arm is therefore made of [?] Diffen Cambrian and Beedmantown strata. These strata come in again along the north of East Arm near Reedys farm. Dunton and Californias came up Deer Brook and finally up to 1600 but above the sea and saw no other rocks than the L.C. Our granite is visible from at the top of the hill up to 2000 feet and the topography is not one of granite, Dunton says it is all L.C. As the slope of the mountain is about that of the L.C., there may be no great thickness of L.C. to be added to the section. Yet there may be several hundred feet of strata here. Dunton says that only of the strata seen are quartzite with some sandy shales. It seems best that one should say that at least 500 feet L.C. may come in between the seam base and the granite, and it may be that the thickness is even a good deal thicker. In the afternoon launched up East Arm but the tide was at its height and could not get out any where to see the L.C. as the rocks in most places make no tender showing the dips into the water. On the north shore of Brett Bay near the point into this bay there is a thick light colored quartzite that I take to be the base of the Diffen Cambrian = Beedmantown. These rocks strike across the bay into the headland that makes the land between East and Brett Bays. In this peninsula there is away 1900 feet of old miles including the above mentioned quartzite below, are probably Beedmantown. If any in Diffen Cambrian it is got to be proven. Later Dunton will visit the place again when the tide is low to see the contact between the L. Cambria and Beedmantown.

80. Deer Brook Bay is at the eastern end of East Arm. What Shore calls Deer Brook at the western point seems to have no name. Evidently Richardson's section was measured at the eastern end of East Arm and not in the center of the arms extending east. In the late afternoon and evening Duncan went back along the north shore to see for contact between the L.C. and Bear Mountain. On the latter he found a very irregular interval before he came upon the L. Cambrian. They two trails leads. My notes are continued on page 84. Duncan climbed Miller Brook and at 350 feet above the sea or here still in the L.C. quartzites. Here the strata dipped about 20° nearly south. They then climbed up the east to an altitude of 1600 feet and where still in the same quartzites. From here they could plainly see the Cambrian all the way to the tops of the hills.

July 23 Cwlly. Continuation of page 75. Dunbar's notes Dunbar's notes are as follows: "Beginning at the north eastern response along the R.R. beneath the slate quarry. [The section is ascending] 75 feet greenish-black shale 60 feet greenish-black shale like that below interbedded with beds of conglomerate, black lias. Of these the lower bed is about 6 feet thick. There may be other beds just above or not exactly repeated by the faulting and shearing of the shales. The fossils are distinctly flat ones and surrounded in the cliffs. 310 feet shale, mostly greenish and sandy with several feet of redish and slaty at the top. Much weathered. Dip varies from 20 to 30, average 30 degrees. 80 feet grey micaceous and heavy bedded siliceous sandstone (best exposed above the slate quarry where its heels off the cliff as thick as brick cars). It is a coarse grained and argillace with a few grains of quartz and many grains of white feldspar. In places, the grains are as large as small peas. 90 feet greenish grey shales, much weathered. 190 feet red slate (being quarried for roofing slates). 53 feet greenish grey shaly sandstone. 130 feet greenish grey, interbedded sandy shale 240 feet red slate. Dip 35-N. 60-W. 46 feet blackish, sandy shale and sandstone 80 feet red shales. "Furthermore on the exploration is not continuous but the dip continues in the same direction in all of the explorations seen and the material seems to be mostly greenish black shale, much weathered. There is an exposure of these 75 yards west of that above, and again about 700 yards further east where it is more exposed

82 July 23. Aurigny. Dentars notes. in a hole near Parsons Tomist note. Just down the hill 150 yards farther over there is an exposure of 20 feet of purish grey sandstone dipping 20N, 75W. To follow second visit my age 75. Dentars notes as follows:- "At the mouth of Dale Cre, and just not far there is a small exposure of dark flint li., dipping 60N, 80W. In it occur many obscure gastropods of the Cuv spired oraculite type. At one of Leuseurella ocara. To the west there in an uneven bedded interval of 90 yards. The follows a section of the bed formation as follows 95 feet flint marble. 10 feet of white and mottled marble 32 feet of white marble 10 feet blue marble. 2 feet laminated beds like Cryptogron. 3 feet blue marble 2 feet laminated beds, 158 feet of marble and magnesian li. mostly blue but with some white and buff. At the top Cratophra torta comes in and is common. in a layer 1 foot thick. Ranges of a few feet. 210 feet flint and light pinkish marble and magnesia li. Dip, 45N, 80W." Further along down dark li., this looked chagy. This parts are more complete after the faulting here are the changed dips.

July 24. Continuation of page 77. Duntars notes. [illegible] Thicknes of strata not measured, but rough estimates appear to [illegible] equivalent thickness to those seen on the Hunter, see the photos of this again. "Drift the Laurel are situated along the south side of Middle Cove but did not go above farrowing tree. On the Peterburg appear Hardish Shales dipping steeply to the westward for a foot thickmen, finally a thin zone of red shales and further on a heavy bed of buff clined rock which maybe quartzite n'domite. Then the middle of Long Cove the exposures are not so good and we had to stay further up shore because of the shoals, but the dip is seem to be almost vertical. Further north along the west side of this cove and along Corp's Point the strata are dipping to the eastward and belong to the Hard Shale and rounded beds studied this morning. "Afternoon studies in the East Arm of Barne Bay where we saw the Lower Cambrian or once developed it appears very fracture that the beds seen between Penguin Head and Long Cove along the south shore of Goose Arm belong here."

July 27-1918, Saturday. East Arm Bonne Bay. In the afternoon it is fine, warm and clear. A dark slightly raining morning. We leave camp and spend the morning looking at the northeast shore of East Arm. This enters from the river or southern end of Deer Brook Bay into the entrance of East Bay is made up of Lower Cambrian. The higher strata are in Deer Brook Bay and again about 1/2 miles southeast of camp. The aurising of the section takes place about one-half mile to the northeast of the crater from which the there is thickened broad and plunging anticlinal structure here, from the cross of which is locally known as Mill Brook. Near the former strata are at hand, in the main fault is white fine grained quartzite. Other crucial Lower the exposed strata have the lower of the section. Cambrian is for a while in unlitown, but it may be several hundred feet, and it may be considerably more. The top of the L.C. is also unknown, and it of to both ends of the arm. crosses in. The entire mountain side of the northeastern shore is L.C., the from the very top down (transition from 30 to 75 degrees) the shale dipping down the mountain sides into the crater. The dip and strikes of the formation is not uniform, but being local undulations and in places cur The probable cliffs is to the northeast and finally runs in Deer Brook Bay. some faults of no marked trend. We made or serious attempt to collect L.C. fossils. We have gotten too tired to master the difficulties, said it's The western shore of Deer Brook Bay is of trap, and the Reed mountain appears where the bay flows out into the arm. Where the crater is about 3/2 to 1/2 mile wide with the dip of the Lower Cambrian and the Reed mountain fairly The Reed mountain line is slightly from the center, and if in limits to have been it, the area was then 10000 sq. constant. At this point the Reed mountain, or the typical rock, thin and thick bedded dark and light colored dolomite with interlaced material and exposure for jointed same ferromagnesium close together. Confonates. Also white layers, and in one place the white over turn of into fettle, and embedded in an interlace material conglomerate with angular surface the dip is 35 S. 60 W. The distance from to Reed. From C. is about 1/2 miles (Reed) fences. There are at times entire beds 2 or more feet thick of Chert.

July 27. Bonne Bay. In the dimlite introduced in the dimlite. One breath not an irregular cliff due originally to diagenetic change. In one place we saw more than given face of undoubted first hot quartz rock, when a thin strip Before we round the due to go into Reddy str. we saw a Piloceras of wetheri, str. Some members of this below the Canyon where left in 1908 by traphia and Billingsella. For the next horizon of the latter form on them. After lunch are continued around the dead-land that makes into Reddy's Hawks. The Redmontman continued the dead-land and we soon saw that Horn- legs snip is many in that there is no track anywhere how old the craft all the The Redmontman forms the top of about 200-foot slate column area. gray into Reddy's Houten. Finally we came upon the Chazy that has an abundance of form kinds of which most are are Maclurens and Stormtowers. Also saw in abundance. this units doubt and Eniforms the common Lependitias. The strike of the Chazy beds carried across the water to the headland this divides East from for South term struck far to the west of the fold dead land in which the Redmontman is exposed. The bed near Reddy's headtopp pg 85 N.70NW. We then crossed over to the fold head-land facing Reddy's Houten all this apparently are of the fifteen upper chief of the Redmontman. of which is composed of the Rister Bedmont man, many hundreds of feet thick. We came in 1910, test soon found the Ceratocera beds and 50 feet below them occur the Billingsella small Maclurens and the Bathynurus tail. All of the forms are poor (due the few accessories). Above the Ceratocera beds the Bedmontman is continued for 375 feet more, The dipthere is 50 degree due north. further Then following the headland around the Chazy appears with many form and 90 feet above the base occur Lependitias. We estimated the but it may be thinner. Chazy to be about 300 feet thick. Here at 320 feet above the base occur dark earthy concretedly fructing li, they are thought of first over the Table came & above them head sand, but once Chazy but dark colored li. --same with the same form as below. Leonella are common. Also got Trachichelia acuminata (C? amorph) Above the Chazy comes in a dark Hue slate series that becomes

86 July 27. Bonre Bay, Bad's Havern (Bald Cliff, and) with them sandstone gneiss. Thin or schistose as to repeat our forms. Performs itself once in sandy upward. We estimated this whole series to be at least 1500 feet thick and as it comes in above the Cheyaz and beneath the river-green sandstone - conglomerate series, the force of this whole ought to be [illegible] table head and Parson's sandstone. At the head round the dip of these last slates is 45 S. 45 W. The last of the sandy-slate chain adds another has a dip of 45 S. 45 W. and the river green sandstone a dip of 60-70° N. 45 E. . So it therefore seems that the two series are unrelated to one another and have faults. The whole of the Cow River conglomerate series in faulting out here, relation, the high dips of the sandstone changes to Iron and Hatteras but again it rises again in the gravity direction making an anticline here. They are for into the southern half of Smith's Arm and to the south of Bonne Bay reserve red shale. The crop further north then becomes horn and miles out on in the distance other red shale gives it is plain that the magnified series continues above the pure sandstone-conglomerate series. at Hell Core We camped at 6 P.M., about two miles south of the village of Bonree Bay, in Smith's Arm. The first bed of red shale is at our camp and on this, As I sit before the tent and look to the north over arm Smith's Arm and the land that smokes into Reddys Havern. I see in the far-ground the high range of Lawn Cambrick hills. Back of it further to the south rises an ornament to 2160 feet. Porters' shots are possible in this mountain, back of the latter and once to the west rises a peninsular mountain to 2560 feet. The craggy of granite. Still further to the northwest is the Big Ridge pencil apparently of granite and at a level of 2000 feet and more. All of these measurements are according to Admiralty charts. In five mountain scene this one and the others of Bonree Bay. See other pages 183-

87 July 27. Bonne Bay. Bembaus nts. See next page 86, see another map. 58° Lighthouse Lobster Cove Austrian Head Redde Point I could keep a good 1 small rowing long survey Sine Pt. Bonne Bay Mipana Pt. Hole Cove Rede River Kee Cove all from Caribou 58° 40' 2290 Spending Camp. Drimian Cove Companion Pt. 1960 Austalands Red Cove Sandstone Entrance Pt. East Arm Boggy Ore Point Ukudrine Creek Sine Cove all from mountain Borod Bay Ignious Man Eastern Head Brock Bay Village Shell Cove Drainaged delta Redde Cove Entrance Pt. South Arm All Direction Station [illegible] [illegible] Bermontown Appland → ↓ 284 [illegible] in attendance, [illegible], etc. These kids take on the character of the Chags and other an attendance of pastafarians. About popular of those Chaggs kids from the front out to Redde Haven, dep 85° 70' W.

86 July 27. Bonne Bay, [illegible] doc. 113 apparently of granite and at a level of 2000 feet and more. All of these measurements are according to Admiralty Charts. The fire mountain over this one and the others of Bonne Bay. See also pages 183--

goes with page 86. Bonne Bay [illegible] Chubbs Take Shore Middle Haven Red Cliffs East Cove [illegible] Gorge Take the road Bonne Bay Danetown Parcipated trees Red stakes. Mud Flats Heavy bedded denotations of Free Pines Map of Bonne Bay

doc. 113

July 27. Bonne Bay. Dembars mts Dembar's mts are as follows: He cruised along the northeast side of the East Arm into Deer Brook Bay. At about the saw mill on Charles Creek Brook, the strike of the L.C. trends around so that in general the beds dip off to the southwest and finally south, and in Deer Brook Bay a little north of west. As a result we rise in the section going toward Deer Brook. In detail the the dip varies frequently as much as 30 or 40 degrees but in general it is as stated. There seems to be a broad and steeply plunging anticlinal structure at about the saw mill where we find the coarse exposed layers of the L.C. farther over rise through the L.C. in going along shore either way. It can't seem that the opposite shore of the Arm is formed of Bredmant and dolomite, the strike of these beds also tending in general conformity with both of the Cambrian and with the other line. On Deer Brook Arm we begin in the lower part of the Bredmantion. Buff to light gray dolomitic li. like those seen near the "Scarels" at Polson Pits. Here the dip is 35° S. 65° W. The section rises slowly toward Reddys Harbour. The upper Bredmantion becomes darker gray in color and weather rough with irregular stringers of quartz standing up in relief on the surface. [See Q. for the Oil company]. The section continues across the next little curve with patches 200 foot of slate and dol. and the dip gradually steepens up to vertical. We then pass into 30 feet of dark slate colored beds that weather to chifts, and then heavier reddish clay gray moy. li. again with small Brachinites in abundance, Lefendition, etc. These beds take on the character of the Chazy and show an abundance of gastropods. About 100 feet from the Chazy beds form the point next to Reddys Harbour. Dip 85° N. 70° W.

July 28. Bonne Bay Sunday. It rained off and on during the night and this morning there is fog. Mr G.W. Denton and Edwards start off for the day to climb the divide mountain faced from camp. There is still fog at 1 P.M. At 3 P.M. it is clear and they can see a long distance. They returned to camp at 6 P.M. In the afternoon I traveled along the "Government Road" along shore about 2 miles to where I could see the head of Smith farm. Red and green shales (with 5 to 25 feet) with thin gray of coarse sandstone occur in the first mile and than it is sandy shales with thicker gray of sandstone. A little on 2 miles from the head of the farm there is a thick gray clay added coarse sandstone and here it steeply (with about 100 feet) (rises into a cliff with the cliffs for the most part. From this one sees that the Bonne Bay sometime is at the base of the granulated series. The thickness of the series in therefore very great, for about 5000 feet of granulated in turn added to the (footprint) (with about 200 foot thick) (extinct) outcrops to the head of the farm. One mile south of our camp is Hell Cove. There is a large broken escarpment down the mountain side, where the Government Road crosses, the horn may be seen mass of serpentine more or less crushed and brecciated. Of it there two samples. It is this rock that make the rugged and corroded hills between the Polygno and the Table Land to the west. These hills are known as Over Tops. From the Table Land Denton brought several samples of the divinite" and rein material cutting it. These are coming from the top of the Table Land is at an elevation of over 2000 feet (2336 feet according to the Admiralty Chart).

89 July 29-1918. Monday. Bonne Bay to Pauls Inlet. Left Hee Cre camp at 9 A.M. Brought gps at Bonne Bay and then across to new Redelp Haven. The day is fine with no breeze apparent in the bay. Are then went across Bonne Bay from the old gps to Norris Point. The outer southern form made up of the Table Head slate and then to the northeast are cut off by trap. This is the only place around here that we can see green scots [illegible] and they melted into the land and finally come out at Deer Brook Bay. From north shore of Bonne Bay this green scot's walk westward the in sand to the outer side of Heele Cre. Between here and the next cre - Heide Cre the dominant form is composed of much marked and [illegible] line a expansive fault due to the proximity of the trap. The dip is 40 northeast at similar quantity from 2 hours [illegible] sandstone. These sandstones [crossed out] and dark slate [underlined] the time [illegible] far by part of the north side of Eggon Bay - fast Drifmore Point broke Haven to North Point light House line 25 kms are much marked, faulted and generally disturbed. description. The thickness must be considerably greater than 2000 feet. In all this distance we see no red scots. The dips in fairly constant at about 1/3 the i.e. from Heide Cre to [illegible] three Drifmore and Green Point, a distance of many two miles may out are then the cliffs are consider marked or that a calculated time in thrilling cannot be accounts. Two miles / sandstone at 30 = 5700 feet/1 strata (minimum) per 90). as we move from 40 degrees across the strike the thickness is means 4500 feet. [crossed out] the north point of the cre Are went on here again in Leister Cre and from here onwards there seems to be from a transition from the Cns Head Geyl create into the Bonne Bay sandstone. Here are interbedded thin sandstones, green and flood shale, flood chert grows over two feet thick, limestone conglomerates with the pebbles surrounded and the heels from inches to 4 feet thick, and then leaded light blue limestone intruded with clay shale, one of which are more than 1/2 to 2 miles thick. In the flood shale one gets one clear scale of an Articuloiden. Almost from Leister Cre northward to Cns Head the freeland to the west of the Long Range is very low and flat. It does not seem to rise to more than

90 July 29-1918 Bonne Bay to Cow Head. if that much 75 feet All of the Paleogene rocks are cut off at this level by the intruding sea and the intermediate areas filled in most sand brought by the streams from the Bay Bays, it is the same elevated beach that we have seen so often. On page 89 it was stated that the Bonne Bay section in two miles of fairly constant dips gave a thickness of 4500 feet. To this it would seem should be added once faced crossed to Cross Point Light. In addition to the strata from Hell Cove crossed Cross Point, North Arm are three added. This is a distance of 21/2 miles and at 35 degrees around gives an additional 7000 feet. As at Final Point the strata receive this dip this would reduce the distance to about 11/2 miles and a thickness of about 4500 feet. Whichever way one turns this is a thickness of the Bonne Bay series - Paraglated series if at least 9000 feet and then maybe even more than 10,000 feet. It seems none of these statements can be relied upon as they are all based on general Narrations. As we get opposite Bony Head on the Cross Mountain calls me to deal to see and p.119 that Sirs Monroe is made of a stratified sand (Day 82). This is certainly true. The question now arises what is the age of these strata. If they are Parageneic they are faulted off in relation to the granite of the Bay Bays, farther north. The distance from the Cambrian out of East Arm to the northern side of Sirs Monroe (2600 feet high) is 4 miles. At 25 degrees dip this would give a thickness of over 8500 feet of Parageneic. This would account for the upper marbles (3700 feet) and the middle schist (5200 feet). On the other hand Dunton calls my attention to the swinging around of the Cambrian strata of East Arm into Deer Bone Bay. If this turning is continued to take in Sir's Monroe then what we saw in the Cambrian on the upper part of the Mt. Dunton rather think the rocks are of Parageneic age. Or any, you think it - are Parageneic, in any event one have cut off get from the presence a chance of Parageneic in Bonne Bay.

The Long Range mountains here in the north are more dissected, have large rolling country from the interior, and their western front approaches usually gradually to those of the low foreland. One sees one fault scar face as in the south at Little River. The tops of the mountains are also somewhat more irregular than the foreplain is clearly formed. The range is badly faulted but in early time came up 7 to 20 miles. The foreland in turn approaches within them 75 feet = a sea terrace. From Deiters notes: - "The thickness of the Bonne Bay series over the goal from the north edge of Bird Cove to a mile beyond Higgan Point are once carrying the strata at about an angle of 450 and the beds were dipping about 210° to the southeast for the whole distance of nearly 2 miles. This could indicate a thickness of over 4700 feet. The faulted and disturbed strata which continue past Roche Hachin may in fact at least duplicate those mentioned but probably would add some thickness. Around his route in this section no any sandstone or granite as that opposite the village of Bonne Bay, or that the sandstone and red shales of South Arm should apparently be added. Logan estimated this sandstone as 2000 feet and it appears that the red shales above have a thickness of over 1400 feet. If we add to the 2000 feet of granite as exposed between Baddis Haven and Entrance Point 4000 feet of red and grey shales and so, exposed between the latter point and Horal Point and another 4700 feet of shales and shale as, exposed for Bird Cove past Higgan Point the Bonne Bay series (which we have here calling the varigated series) attain a thickness of 19,500 feet. These figures are of estimates from a running foot but in any event the first series of os. and rl. must be 8700 or 10,500 feet thick."

92 July 30-1918 Tuesday, Car Head. a squall arose storm in arising, it clear a fair all day. That may throw away. In the morning studied the conglomerate of the peninsula along the northern shore side on the shores of Car Core (at Car Head Station), going from the sound spit northeast about one mile, or not quite to the outer or western point of the peninsula. in thickness, up to 20 feet long About all of the material here is of the Red man town and the strata are the higher in the circle on the peninsula. We saw one large block about 2 by 3 feet with many Ceratopia otherwise saw no fossils in the Rocks. In the bedded material between conglomerate groups the thin beds are usually of li, thick chalk bands are here and argonaceous li. These beds are usually 1 to 3 wide, thickly separated by black shale or dark shale li. There often Hole! interbedding a thickness of 20 feet. Take three different layers of these thin bedded strata and while all have traces of pteridites these are not common until one comes upon the outer outlying one, and especially in the thicker zone of argonaceous li. Here Pelycosopters and Tetrapopters and other forms are common, scattered some of the better material. There is very little along the shores of Car Core to suggest any other material than that of the Red man town, all magnesian limestone, many of the blocks daring chalk weathering out at the surface. Some of this chalk is certainly of dia genetic origin but most if it is produced by weathering. The strata near the eastern end where are are compact near the sand spit dip S 30 E, take only ones have swung around to S 45 W. In the afternoon we examined the shores of the eastern side of the peninsula where most all of the fishing houses are. Coming over the peninsula in line with Steary Island (the peninsular off a point of about 1900 foot, and as the dip is S 30 E there is about 930 feet of Car Head Conglomerate in here. Farther west on the outer shore of Car Head peninsula the strata swings around once and the dip here outside, into a dip of 30 degrees this should give a thickness of 1200 foot is about 20 degrees due south, all the inner part the peninsular is about a half-mile.

Ms. Cambrian From the threadled limestone underneath this bed of limestone conglomerate we collected a number of small Lingulas and many fragments of trilobites. These preserved ones came from a small hole about 4 feet long by 18 inches thick in the middle of li. cong. All the other specimens came from the thick about my right, thick white shale underneath before. Masses of threadeds underneath the heavy zone of li. cong. that I photographed me as fast blocks of Cambria li. dropped into the Corr Head conglomerate. In the quarter mile of the outer side of the peninsula examined this afternoon there is at the tip a heavy zone of li. cong. from 15 to 20 feet thick and below are the threadeds of Cambria li. anywhere from 10 to 20 feet thick. all of the conglomerate here is made of Upper Cambrian material. See any photo of these places. For many places the Cambrian in small cones is included in a bent and even crumpled condition. This deformation must have taken place before the pieces were included in the conglomerate and after Cam- of these bent strata brian time. The date of deformation was probably post Tattle Head. Even in the Phyllographus beds there are conglomerate zones and while these are of small pebbles (inches across) and not just yet they are li. cong. not un- like those of other parts of the Corr Head conglomerate. They must be of intraformational character. The whole of the strata of the peninsula are distinctly bedded and we can't fail to note the dips. When we comes upon the threadeds zones of either the Phyllographus or Cambrian, the impression left is that they must be regular de- deposited posits between the conglomerate zones. Yet the fossils secured are entirely not of keeping with the design in which they seem for Reedmanutons and Upper cambrian fossils cannot be living in post Tattle Head time. See elsewhere noted. Several times there many large holes of intraformational conglomerate included in the Corr Head conglomerate. These are not of the first little type.

July 31—1919, Wednesday. Cor Head. The wind howled all night but we are secure behind our wind break built of logs. Every now and then it rained. This morning there is no sign that the wind is to let down soon. We reexamined the Corl Core side and the Phyllographer zone. Clent found at least two places here with Reed mountain prints. An orthid, two called cephalopods and a tail of a trilobite. The first thin redded mass, going into contact in a distant core gives an idea of a thick 500 foot log and about 20 foot thick. On closer view one sees that after deposition it has been broken up by faults into three or four and slightly offset independent masses. The curious feature of these once called thin red beds—eye lets lie, separated by dark green shales in that they have lenses of intraformational coal over at for 2 to 50 foot long and for an inch thick to 30 inches thick. Further once the thin redded lies give evidence of churning up in the sea, the intraformational coal ones not made by washing of semi-exposed samples but by storm waves turning up the bottom and redepositing them; on this mass there are also good pieces of black chalk an inch or two thick. Pieces of this chalk are common in the intraformational coal. The fossils are as rule flat and once inches long but there are also angular bits, pieces of it are first seen, that these pieces were still unconsolidated when seen in their first nature, and when bent are often crooked to accommodate the bending. Blocks of these intraformational coals are not rare in the Corl Head coal. The next diphen mass is of a similar character about 20 feet thick and several hundred foot long. This mass is characterized by large 1 mm thin tuts vertical in the lie, with the tuts usually filled with coal minute grains, like

Finally this man is traced westward, all ground up into small blocks some for long and turned about in any direction, and even ground up into particles under an inch across. Farther on to the west comes in the Phylloid grits, shales and then bedded and 2 or 3 foot thick Li. grits from C Head chat. This man is about +600 feet long by 20 feet thick. Other similar masses occur farther over. These are not so regularly placed in regard to the dip as the other more eastern ones. One is impressed with the regularity of the dip usually around 30 degrees. Even the rocks when large and flat are set in the angle conforming with this dip. Or are the great blocks of these bedded li, thick not always with or keep a dip. At the western point Dunstan enters one great mass standing vertical. To have great blocks many put a length and more, hundreds of feet long all laid down in one general direction coming here, it occurred in a sort slide. Therefore the dip land must have been to the east of Carr Head from which the material slid into the sea and there once frozen. The dips are now one can actually be foresetting slopes instead of dipping slopes due to deformation, or maybe from eastwards compound or series Dunstan was agrees that Cnr Head is a conglomerate and that grit blocks at least +600 x 20 feet occur in it. He says the evidence for this is most plain among the Cambrian strata on the outer side of the peninsula. Here the blocks are less large, in dimensions see any note of 1910. In the afternoon we again collected Cambrian fossils. Dunstan got 2 sealy entire trilobites. Otherwise we got less than yesterday. The highest part of Cnr Head (206 feet) is also made up of Li. Congl. Thus for all of the peninsula may be regarded as of Li. Congl.

96 August 1-1918 Thursday. Camp Head. The wind shifted late yesterday afternoon to the northeast and during the night it did blow very hard. This morning the wind is still strong but the sea is still too rough for us to use our boat. It rained lightly during the night. At 8:30 A.M. we concluded to travel to the Hamors of Pauls inlet by way of the Government Road along the telegraph line, The distance to the Chamms along the straight line is not far from 5 1/2 miles. The walking for me- [illegible] the distance in through the pitchy-flank-arthuron swamps and the rest throug the boggy bush. I returned to camp near dead. He began to see the then looked light-blue li, and limy shales separated by their green shale gree along the shores of the ridge that makes the fault of the Hamors about one mile from the Chamms. Here strike dips 35° S.45°E. At the Hamors limestone conglomerate are present in the same area and then liturgy cornel grus each from 2 1/2 to 5 or 6 feet thick. They are made of flat limestone [illegible] pebbles usually fairly well surrounded on the edges and with there are as- sociated Chagga-Beckmontown shales up to 2 feet again. On the other hand me gone about 4 feet thick seemed to be intrusive and because the shale, more all hard and squezed into one another and much resembled the red hereath deposited in an undulatory area. Between the li conglomerate and the thin fridled li there are gones of greenish shales and from them gones of red-shales but also There are also black shales in very thin layers and in a loose piece I was able to take out are somewhat limy. Beyond the Hamors on the north one can clear see in the letters account more red shales and red li. as described by Logan. Across the strike these beds are visible for about 1400 feet and with a dip of 35 degrees then gives a thickness of 750 feet. On the other hand Logan mention the li conglomerate "in a small anticlinal dillroll" which is about one mile from the Chamms.

97 Measuring across the strike from this place to where we saw the last of the Cow Head, the distance in 9/10 of a mile and at only 20 degrees that gives a thick- ness of over 1500 feet for this part of the Cow Head embayment. Richardson gives the total thickness for this formation as 700 feet which is entirely too small. At the Narrows, Richardson got Orthoceras, Lingula, Athleta and Le- kandites in the bi, and pectolite in the shale. We saw two from Lingulas in the lying shale to the west of the Narrows, and at the latter place first measure pieces of each shore with pectolites. I wonder if the other things were rather only of the bi. engl. Certainly they do not recur in the depositional limits. One a half miles from the head of the inner key Logan reports hears Redbeds and brownish bi, standing nearly vertical with a thickness of about 826 feet. These are followed by the Laurentian gneiss, and Logan thinks this re- lations is at faulted area. From this locality to the Cow Head engl, the distance is about 3 miles and what is in their more towns because there are no exposures. For more see pages 103-105. All along the outer shores north of North Point Light (Bonne Bay) or west to Cow Head where we saw Laurentian borders, there are all granite-gneisses, and in this unite the granites of the East Arm of Bonne Bay. In a rough way one may say that the gneisses are the squeezed red granites of the East Arm area.

See with page 97. And pages 103-105. Coral Head Telegraph line Mainly sand and clay. Tidal Island Outer Bay St. Pauls Inlet Broom Point The Dunes Inner Bay Anticlinel killed mud shale. Coral Head series dip 30 S. 45 W. Ledge of li. shal. dip 36 S. 45 E. 200 feet of li. shale, dip 42 S. 40 E. Granite prism 310 foot of greenish black shale with thin bands of li. and chert, Stanniferous. dip 60-75 S. 50 E. 6 feet of coarse li. shale, with flakes of to 5 foot ocean standing outcrops, Barred S. 60 W. Diat-fy li. very much crushed dip. 70 N. 40 E. Map of St Pauls Inlet.

doc.113

July 30. Diemars notes, Lee pays 92-3. "The phenomena seen this morning are the most unusual and trelievable I have ever seen. Just masses of relatively soft, incompetent shely beds hundreds of feet long which are full of prints that should be of the Reelmantown, lying between conglomerates formed of heavy hard Reelmantown limestone and yet these heavy bedded li, are in masses many all under 10 feet acros. What transporting agency could carry off incompetent troubles of sand unhealed of divisions and at the same time always reduce the hard strata to far smaller masses? The situation is more confusing because lenses of li, Congl. are common within the whole mass. "In the afternoon we started around the north side of Cow Head and here we found in the li, cong., past masses of thin bedded dark slate shelly li, that are clean and unmarred off "truckles" which carry Woffa Cambrian trilobites. Many of these troubles are tens of feet long and the largest perhaps 200 feet. The evidence here is problems that one is forced to the conclusion that they are trouble ners, impossible as it seems" July 31. Diemars notes, on the north side of Cow Head "Starting from camp, the beds dip about 30° S. 30E., or the strike comes the shore down low angle and all the beds run out to sea at the east. Below one area of heavy li, cong., having a thickness of about 20 feet. This bed is about 1/3 composed of large troubles of light gray Reelmantown li, carrying from 1 to 4 feet a diameter. In one of these we found Christopher tota and in several others Reelmantown cephalopods. These large troubles are surrounded by an arrangement of smaller pebbles and all of which are made of darker, dark colored

99 thin bedded li., or the boulder are decidedly flattish. The layers of these measure about one acre and less than 2 miles thick. All are practically angular. Of one of the boulders about 5 feet long by 2½ acres composed itself of li., cyl. Beyond this bed of cyl. error, the first large piece of precipitate shale forming about 20 feet thick and extending for a total length of more or less; its east end goes out to sea and the west finally going into the bank above the shore. The mass is composed of bands of dense fine-grained dark gray li. 1 to 2 miles thick and alternating with equal thicknesses of almost fresh blue-green shale. There are frequent interbedded small layers of intermediate li., cyl. 1½ to 3 feet thick and a few feet long but then in one layer here a foot thick and 50 feet long tapering toward each edge. It becomes evident that we are dealing with two independent li. cyl., an older one of Bedl-erontum age recurring interbedded in the Bedl-erontum shales and the white in turn embedded as boulder in the late Ordovician Carthell conglomerate. "Of the upper 8 feet of this shale mass, their clay continues for the full length of 50 feet, being separated by 3 or 4 bands of cyl. in the western half of its length from the same family the shale mass which is so often it forms a bar stretch and is poorly exposed. (and hidden in the section.) "Following this mass of shale is another 20 feet of leary li., cyl. In this bed the boulders average much smaller than in that below but we exceptional one of left gray li. is about 2 diameters. There are 2 large boulders made of li., cyl. like that interbedded in the shales (picture exits). "Following this is another past-banded mass of thin dark li. with shale. One block is about 20 feet thick and 100 feet long to where it goes.

July 31. Dechants arts. into the sea, and almost continues on its course and in another arm of this hended sandy li, which swings around once into the land dipping S. 45- W. This bed is characterized by worm holes, which are vertical and always cut out in pairs 1/2 to 3/4 inch apart. These holes range from 1/8 to 3/8 inch in diameter and often have a filling of tiny limestone grains. Proceeding onward one can diagonally over a thickness of li. clay and then strike another long bed a "piddle" of purrish-Haell shale and sandy li, with layers of Haec chalk. The li. banks are more or less irregular, ranging from 1 to 6 inches thick and are thinny. In this shale bed are 3 banks of intrastratified clay, one above another, ranging from 8 to 20 inches thick and separated by from 4 to 20 inches of the hended shale and li. In this infraclay there are some piddles of Haec chalk and others up to 8 inches across are made up of Dechmontown li. Many of the piddles show crushing to fit the other after deposition. Beyond this gone comes very heavy li. clay, with many bands of li. 6 feet across (and one 12 feet across was seen), between which are many masses of this heddled shaly material all marked and smaled of many the bears boulders. This interjops along shore for a distance of about 100 yards and then comes the great "Phyllagrophytus piddle" which is about 450 feet long by 20 feet thick, and clips at S. 30 E., its east end lost in the sea and its west end striking into the land. It is composed of interbedded layers of black chalk, dark gray li. and shale. Phyllagrophytus are very abundant. After crossing another arm of li. clay, one comes to another great mass of beds about like the Phyllagrophytus bed but this mass is about 100 feet

thick and dips 20 S. 50 W. From here on there is an alternation of heavy coyl. and large masses of shale beds, more or less bent and crumbled up until we reach the lighthouse factory in the dark fog cave on the south side of the head. Here we find a man of shale 100 feet long by 20 feet thick dipping 75 S. 40 E. Each of the three frigus at the end of the head are formed of heavy coyl concretos. Between the first two is the largest single "bottle" of Hale seen. It stands on edge dipping 70 S. 35 E. and is clearly exposed for 500 feet. On the west end of the head above the last frigus the Cow Head series becomes sandy and then banded but below these layers are others of heavy coyl. forming the reef along the head below the lighthouse. The dip here is 40 S. 40 E. "To sum up: 1. Along the south side of the head there are several great masses of thin-bedded shale strata yielding large Beidmantum fossils, embedded in a very coarse li. coyl., derived from higher layers of the Beidmantum. 2. These hale masses are of relatively soft and incompetent strata, are weathered into caves or low strips between layers of li. coyl., whereas the li. layers of the Redmantrum are heavy and resistant so that we have usually seen them forming hills or cliffs. 3 The great masses of geoplolithium shale are from 100 to 500 long and from 20 to 100 feet thick whereas the largest piece of the associated li. seen was about 12 feet in largest diameter [I saw one there 20 foot long], and nearly all are less than half as much.

"4. These large flatish masses of paptolitic forms shale are in a general way oriented so their bedding corresponds with that of the Cuyll Series; all dip to the northeast, mostly at angles between 30 and 35 degrees, but not all agree in the latter respect, some being nearly flat, while others dip 70 degrees; some strike 30 N. by East and others as much as 400 south of east. "5. For the east half of the head no small masses of the chalcedony were seen associated with the large ores but for a distance north of the Chylographte mass (which is known in the series) smaller masses of zinc sizes were mixed up in the Cuyll ore. "6. On the south side of the head nothing but Reedman's turn could be seen while on the northwest side there were many masses of thin handed Upper Cambrian li, forming "bottles" in the Cuyll and ranging in size up to 200 feet long, and on this side no Reedman's turn shale could be seen. "7. No traces of either Chazy or Tarkio Head formations were found in the Cuyll Series."

August 2, 1908 Friday. Our Head - St Pauls Inlet. A fine sunny day but I am too tired and rheumatic to make use of it. Stay in camp and write notes. Duncan took the boat and at 8:30 started again for St Pauls Inlet. He returned at 2:30 P.M. with good results. In the afternoon he visited Stearny Island one mile northwest of Our Head and then the reefs to the northeast of Our Head known as White Rock Islets. His notes are as follows: "With the boat returned to St Pauls Inlet. At a point on the south side about 1/2 miles from the head of the bay, where a horn descends from a cirque in the North shore and forms a catarfact near where the Laurentian red-granite-gneiss is exposed. The plane of schistosity seem to dip steeply almost due south. Pro- ceding northeast along the south shore we find no exposure for a distance of about 200 yards. Then a small exposure of dark-gray li, weathering buff colored which is extremely crushed and is interbedded with some muddy layers which have been altered to schist. There is then another short unexposed interval when the li. is exposed again and continues to the prominent point where it forms a high naked bluff. The eastern part of the li, weathering buff colored on the surface but in dark-gray or fracture, fine grained and dense. The western part of the section weather darker dark-gray. The whole thickness of the li. has been so thoroughly crushed that it appears all loose and shows no bedding planes except near the eastern margin. Here they appear to dip 70° N. 46° E. The strike makes an angle of about 35° with the shore where the beds are exposed, for a distance of about 1/3 mile. This would indicate a thickness of 730 feet of the li. This abnormal dip to the northeast another local feature.

"104 August 2-1918. Dentais notes. St Pauls Inlet" connected with the extensive faulting along the contact with the gneiss. "Proceeding northward the shore is low and entered with floccial and lead tondus for a distance of 2 miles to a prominent point about 1 mile east of the southwest corner of the inner bay. At this point the Carr Head li ceyl. is well exposed for a distance of 100 yards along the strike. About 6o feet of li. ceyl. beds are here exposed standing vertically on edge and striking S. 60 W. The conglomerate is coarse, with many tondus of light gray li., from 2 to 5 feet across. "The next exposure is a small island a little over a mile northwest of the last point and about 1/4 mile from the west shore of the bay. Here exposed shale strata consisting of greenish-black shales and clays, interbedded with thin bands of compact dark-gray li. and tondus of that. These beds are somewhat crinkled, the dip varying from 60 to 75 deg S. 50 E. They have a thickness of 310 feet, occupying a width of 120 yards. "About 1/4 mile northwest of this island is another rocky point in the shore composed of about 200 feet of li. ceyl. beds, dipping 42 deg S. 40 deg E. Further north the shore is low till near the Darrars. A low rocky ledge about 1/2 mile off the end of the inner of the long peninsulas from the north shore is made up of heavy layers of li. ceyl. dipping about 35 deg S. 45 deg E. "Outside the darrars the shores are very low with no other de- promances except a low hill near the north shore of the middle of the inner bay. Because of the very shallow water I did not get to this level bed with the planes, should plainly see the strata of ceyl.

{ "text": "Aug 2-1918, Alenais note, St. Pauls Inlet.\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n [TRANSCRIPTION_TRUNCATED_DUE_TO_LOOP]

106 August 2-1918. Dentars notes. Stearing Island. "In the afternoon with the launch went across from Cow Head to Stearing Island. The dip here is the same as that at Cow Head, about 20 S.30 E. There is positive or anticlinal structure here. At the southwest end of the island we came upon a "bottle" of shaly strata 50 foot thick and 500 foot long to where it goes into the water. It consists mostly of black carbonaceous and limy shales with greenish interstraded thin layers of dense dark-gray li. The dip of the bedding in this mass of shaly material is 20 S.30 E. "Other large masses of black shale occur on this end of the island but none were seen on the northeast end though this is directly in the strike of the shale masses. The whole island is composed of the heaviest sort of conglomerate. Bottles of li. 8 to 15 foot across are very abundant and from these they range up to 135 x 50 feet. Many are from 20 to 30 feet across. These layer bottles are of light gray color and fine gained texture and are much degraded by by fire jointing. "These large blocks appear to be of Chazy li. The fundamental block is 4 x 6 foot which is crowded with coiled cephalopods of C. characten, and with them are associated a remarkable layer tilitite. On other blocks of 18 feet across we saw Chazy forams, trilobites, brachiopods and part. Identified M. acuminata and Rafin. aurora. "The extreme coarseness of the limestone conglomerate seems to indicate that we are near the base of the Cow Head conglo. Once one finds the li. also in such large "bottles" it does not seem quite so unreason- able to find large masses of shale.

Aug. 2 - 1918. Luntai's notes, Stearing Island. "The width of the island across the strike is 100 yards which at a dip of 20 degrees gives 100 feet of beds clearly exposed. In addition there is a lower rock reef formed by coral. 200 yards further north-west, parallel to the island, it can be seen to dip in the same direction, and this would indicate an additional 200 feet of strata. The width of the straight between Stearing Island and Cow Head measured across the strike is 1600 feet which at 20° dip would include 1600 ft of strata. The greater width across the head at right angles to the strike is 3000 feet and here the dip is about 30° making the thickness around 1500 feet. This makes a total thickness of 3300 feet of heavy coral limestone between the outer reef of Stearing Island and the inner side of Cow Head." [This is by no means all of the Cow Head conglomerate for all of the strata seen at the Harrows on August 1 - page 97 and at least 1500 feet thick are to be added. Further off the inner bay there is once Cow Head formation found at distance or that even more is like added. As the core now stands we see that the Cow Head formation has a maximum thickness of at least 5000 feet and in probably some places. When the basal angle, which are all present the Cow Head once if course be further thick and may not exceed 2000 feet.] "At 6 P.M. we rounded the corner and went to the White Rock Isles for a little while. The reef is formed in narrow stringy islands running north-westward from Cow Head to the point north of Hallow Bay (Cow Horn). The reef has a length of one mile. This comprised

108 Boxes of material Box 1 Packed at Cashion House Potomac Park, has all the material collected south of here, and the Reedmontown other Park au Park and to the north. Boxes 2-5. Material from Talle Head Cove and Sky Point south to Herr Bay. Box 6. Ammonites from Fort Bay, Collected July 15-1918. " 7 Helix bygian. Material collected July 14, 1918 " 8 Material J July 15-18-1918. Also later material " 9 Cow Head. Phyllograpus, part of Cow Head conglomerate July 30-31 " 10 Cow Head Cambrian below. Hartnurse Bonne Bay. The few forms from Cow Head- Pauls inlet. Also other odds and ends. J li. cays in which the fossils are small, averaging not more 2 inches, caves with scattered ones of a foot or two across. It is distributed in grey massive layers 6 to 18 feet across with once overlaid bedding plains between. While most of the shells are angular some tend to be rounded. The cliffs here on the first layer island is 355.308. and these layers have reproduced are about 100 feet thick. They appear to strike into the core where the fishing houses of Cow Head peninsula are located.

[illegible]

"K&T" 8680 Cost of Trip Price if seemd land launch ---------------- $ 640.00 Paid in dry These bills were paid by Doctr Tynell. -------------------------- Paid J.T. Thorre for camp sufflics -- $ 303.39 July 23 Paid on the first $ 200. Rest Aug. 29 Paid B.D. Lillie for 6 barrels of oil ----------------------- 147.59 July 23 Paid on the last $ 110. Rest Aug. 29 July 23 Paid William Lemire for months salary -------------- 90.00 " " 23 " James O' Rourke " " " --------------------- 70.00 Aug. 31 " " " " " for 42 days @ $ ----------------- 126.00 " " 31 " William Lemire for 42 " @ $25 ------------------ 105.00