Field Notebook: Bermuda, New Brunswick, Quebec, Vermont 1929

Schuchert, Charles; Cooper, G. Arthur

1929

Yale Peabody Museum of Natural History

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Source Material:
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paleontology stratigraphy fossils

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320 Pages

doc. 0139 If found by anyone please return to Professor Charles Schuchert Yale University New Haven Conn. A.S.Q. 1929. 7080 = Gaspe 7712 = Bermuda

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July and August 1924 7080 July 23 - 2 trees by freight from Jacquet River, N.B. " - 1 small tree prepaid to Reedemann 16 - 3 trees by freight from Dalhousie, N.B. Aug. 3 - 1 tree by freight from Pats Daniel, Quebec. 12 - 2 trees " " Perce', Quebec, Shipped by Ernest Biard. 17 - Four trees from Grand Mere.

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begin [7712] New Haven - New York, Jan 2 - 1929. Last night I finished felling my two tags, and this morning I am off to the Museum at the usual time. Had the usual breakfast at the Graduate Club with Dr. Loney, and he told me more of the con- dition of the one of the new edition of the Pearson text. book. One chapter by Balemans (On Deposits) and the one by Duncan are not yet in his hands, but all were due in a few days. Loney hopes to complete it soon and deliver to Wiley's not later than the fifteenth of this month. At the office I read over once my paper "Chamber- lains Philosophy on Correlation", and now Men Le Vene is sending me final copy, it will go to Professor Bastin in a few days. Also my Vice Presidential Address in one form or another to Science, and the other copy to Dr. Joe of Amer. to Secretary Bush, Duncan took my baggage to the railway. Then to bank for traveling money and to adjust my account. Took a lemon Duncan, and at 2.48 P.M. he took me to the railway and I am off for New York City. Put up as usual at the Murray Hill Hotel, where I have been staying for about 35 years.

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New York City Jan 3-1929, Thursday. A bright cold morning. After reading a little in the morning "The World" I went off in a cab to pier 42. Got to the pier at 9:45 A.M., and soon was aboard the large and to me palatial steamer Aaron. I had purchased berth 98, but on arriving found berths as- signed to a room with but one berth - 275. On the steamer and the Royal Mail is doing me honors, and Evidently became I am a Professor of Chief Mr. Dreezy of Bordtarn made them. The steam ship Aaron is registered at 17,000 Tons and swarms with dogs all in blue and once flecked shirts. All appear to be English, at least one with whom talk. Just as I expected English service is more delicate than abroad American shipping. At 10:45 a hand-bell is well shaken and soon "all that are aboard" have gone ashore and promptly at eleven we move out into the North River in Hudson. An hour later I sit in the main cabin, and it's has quiet air. The bustle of New York and its own daydreams autos are gone and so far I am on the quiet waters of the Atlantic, my third time. First with Gray to Greenland (1897), to Germany in 1903, and now to Bermuda. The several other times in those waters do not count.

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"The Steamer [illegible] does not appear to be fully loaded, but I cannot judge better than from her in for my first meal. At dinner the steamer gives each guest a little memento - rules and regulation - and in it is a list of passengers. It has 58 First class and 16 in- termediate. I am at the second table headed by one of the officers. The Captain sits at table 1 and he enter- tains some ladies. At dinner some ladies and a few men are in evening dress. This afternoon I saw several whales at sporting. There were at least four, and they appear to go in pairs. So far the sea is remarkably smooth. There are white caps, but the waves are hardly more than six feet deep. The pitching is very slight and rolling there is none, backed to Promenade Deck about a half dozen times, and need exaggerating the rest of the day. As usual at sea I am getting the headache pro- phetic of sea-sickness. So far it is not alarming.

Aboard Avon, Friday Jan 4 -1929 The sea was smooth last night and got all day. I have come down with a headache. Tried several times to remain in deck, but finally gave it up and lay down in the cabin. Missed luncheon. Retired at 8.30. The sea is a little more oravy but upon the whole rather smooth. Had a light dinner, Aboard Avon, Saturday Jan.5 -1929. Stayed abed until eight in the morning, when Mr Nailor the steward said the Bermudas were in sight. So I dressed in a hurry, had a light breakfast and then remained in deck... We came upon the islands of the north- near St. Davids lighthouse, from St. Georges East side, and here a corallato pilot came out in a very dry and manner that proved by four other men to take us in to Hamilton, up the side he climbed and then into the pilot house. We then steamed south past a military station along the northwest side of the islands and finally to the entrance to Hamilton. About 20 the southwestern Ireland Island is a rather large naval station. We had to wait to let a steamer out - the Park Victoria - and then we steamed in the- - Cofflers Island and Spanish Point - two or three more islands with the range of clear so that one could have time alone between... The wind is fine to south- east and blew the ship away from shore. Lines were dressed ashore and finally we came warped against the "coral stone"

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May. It was 11.45 o'clock when we were alone and in a few minutes we were through the Custom House. Autos are not allowed here, but Tour and occasional road trucks do come. Carriages galore and all are operated by clever gentlemen. Bicycles are common and some ladies go to market on them. In a few minutes more I am aboard a very high three-wheeled string omnibus — the Langton Hotel Bus — and so we go to the mall and up upon one of the higher hills in Hamilton. There's a splendid garden all about with lots of flowers and creepers and cedar trees. Had lunch and then was shown a room in the cottage which I concluded to take for a spell to see if I liked it. It is to cost $42 per meal for the first month and $50 for a week for the remainder of my stay. Later finding no conveniences here I told the manager that I would change to a room 18 in the hotel proper in the morning. For 1½ hours strolled about Hamilton to see the stores. Go any large ones, and hardly any are attractive. So far in the way of local souvenirs saw nothing of artistic value. The stars are neither English or American and since the majority of decorations are imitations (maybe some are Spanish mixtures) and of the less good kind here is little local talent, and what outside talent there is appears to be I am indifferent kind.

Prof. Charles Schuchert, Emeri- tus, of the Invertebrate Paleonto- logy Department of Yale Univer- sity, New Haven, Conn., arrived in the colony via the R.M.S. "Avon" last Saturday for the winter sea- son and is registered at the Hotel Langton. The professor has been commissioned by the authorities to write another volume to his al- ready fairly large Collection. * * * These are P. hermundensis crassimatus. The Physa = Luccinea hantoniensis

7712 Hamilton, Bermuda, Jan. 6-1929, Sunday As one room in the cottage was cold, smelly and cheerless I had a poor night. This morning it is cloudy and windy from the southwest, and warmer outside than in the cottage. After breakfast moved into the Hotel Seymour and took room 18 on the second floor looking south- east. Have concluded to adapt myself to the Layton since the first class hotels all charge from $8 to $20 per day. And besides one must have to keep dressed all the time. In the afternoon walked along with Alice about 1 1/2 miles towards the Flatts and Fraseati's Hotel. Thursday Jan 10-1929 After breakfast intended to walk to town but in Cedar Ave saw a cliff with some red clay and so began to look for snails. Found some Poecilognites, this red clay lies in a hollow and on the in thickness up to about 12 inches. The shells are common but most appear good or dry young. From 2 to 6 feet Beneath the red clay in soft unconsolidated hilly fossil shell-sand formed layer, better and some com- mon snail shells. Here also small Physa's and occur

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Several species of small marine bivalve shells, Evi- dently the wind blew these marine shells along with the shell sand, and he nails all together in the ore bed, Made a small collection and later on clean-ed them. Saturday Jan 12- 1929 A warm sunny morning, so concluded to walk to the Flatts Vill age (near five miles east) and have lunch at Frascatti. This place is where O'Neill stopped and collected. Therefore thought I would get a lot of sea life to see, and I did but most of it is in the Aquarium built in 1936. Here one sees a splendid collection of tropical fishes, nearly all three shaw have fight arms, On many of the tanks are anemones, the common one an ivory white with long and thick tentacles attracts to one first. (He said to be the largest in Bermuda.) The tentacles are slowly waving but not more than one inch, and often a whole bunch will move together slowly in one direction as the he other. The impulse of change is rather rapid, but the motion is very slow. They show about 40-5 kinds of anemones. The fishes were trunk to the tentacles. The Haell echinus pink very long and slender spine is also known, One was crawling and it spread its tentacles both easily more than 3/8 of an inch. The little ones near the bottom are most active and are evi-dently

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sensory; the long tube-feet getting in hold and letting go or could be placed seen. This echinus crawled over the rocks fairly from miles in a half hour. Along shore I saw hundreds of these and a short spined echinus. The long spined me how the curious habit of having five to six stomachs one after shells both open the aperture. Can this be a protective device? Along the shore I also saw several very large and fat and black starfishes. They find the echini in the whiteish shell sand are emporious objects. The aquarium also had two species of very ornate and highly colored [illegible], but one crab. The Lobsters are always slowly crawling about in a very leisurely way, and with their long tentacles constantly feeling about and the same with their long legs. They stand up as if on stilts. Another tank had almost half a dozen octopus. One was fastened to the glass front, holding on with but few suckers, fairly from them that glue are folded. When they crawl are facts do it. Their arms are extremely flexible and the tips usually tightly curled but in three turns. Their eyes are on- stantly looking and changing about. Evidently they can- not get along. Curious of the aquarium starfishes. The others laid in the tanks, because they are beautiful and

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moraine. Entrance fee 150 cents and quite a number come in each day often driving from Hamilton to Ot, begin elsewhere. Everywhere the shore-line is rocky and one sees [illegible] no peaches at all. Sometimes at the head you find erve them a sheer sand flat. Have been usually much steep and unlit and in the sand one could make quite a collection of tiny shells both gastropods and tivalves. On the hells between tides are one around to Derpula, Patellas and at low tide Chamas and this species of corals are emmm. The star coral, Didem- [illegible] from is yellow and a Mura is a green-white. They show no life activities. Tuesday, Jan 15 - 1929 In the afternoon took the ferry over to Inverurie Hotel and then walked over to Riddells Bay and the Surf Club. At the head of this little bay saw the first of the Man prove true that yes are one the warmest part of the world. The bay is replete with urns-like algae and on it live millions of a little hip opened and ornate gastropods. There saw so many shells together before.

"Wednesday Jan. 16, 1929. Again by ferry to Innisfree Hotel. Called east and then south to get to the South Shore, but missed the short roads and so had a long tramp. Intended to come out to the South Shore Hotel but instead ar- rived one mile over. Along the South Shore road from Bearwell came upon a broad cutting that was rich in Puccinia ignita. About a half mile farther was where the road is nearest the sea, formed over the fields when the dunes at high cliffs, probably 75 feet above sea level. Here was a grove about one foot thick the snails are wonderfully common and as they creation out free one can get to P. termulensis in fine speci- mens by the hundreds. Also got four or five other snails. Our share all that I can use. In the road side cutting came a poor large gastropod, to me commonly used by the digenease hermit crab, and which one of them had dropped off the hill side when I found it. Today saw no associated marine shells flown into the dunes as I did some days ago. The card reef here are out a few hundred feet and to the Atlantic Ocean. Inside the reef saw several fine sculpins atolls as figured by Perill,

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Saturday Feb 2-1929 Left the Langton Hotel and took up quarters at Hamilton Hotel, room 440 at seven dollars a day - this rate is inf or low when taken by the month. March 4-1929 Mrs Pirson and Mrs Mc Longlin called in evening. They are stopping at the Imperial Towers more on to the Inverurie. March 5-1929. Had Mrs Pirson and her sister to lunch. March 10-1929 Had dinner with Mrs Pirson at the Inver- urie. March 13-1929 Professor Tayler called on me in the evening. To- morrow he is to take me to St. Beafes and in the way to explain the various soils in the Paget formation. He now has 1 or two of the Dalsingham

and 4 in the Poyet. Thursday March 14-1929. Sagles had a one horse phaeton of the Prion Hotel and at 9 A.M. we are off for Poynthers Quay opposite the Harrington House. Here the snails helomi are exceedingly common in jiries and solution holes in the Walsingham. Where the large shells are present one sees only variations of the species and very many other forms. In one other solution hole down a joint occur tens of thousands of these snails but all are small, and the brief is quite showing that the age of the formations are different. Of the big specimens give no good ones, but if the other smaller ones for many. Then spent 15 minutes in Leamington Cave, marked frits local pencil-like stalactite, they are full lengths up to 12 feet long and none hardly thicker than 3/8 inch and apparently hollow. The cave is not very croft, at least one need not run around. In two places the cave goes to sea level, and in both stalactites are in the water showing the sea level to have been lower than it is now. We had lunch at the St. Sergos Hotel, and after the meal we looked at three different snails. At Shore Hills Hotel we examined a large

Otherwise the Robinsonham is a deere district like the Pajek, but as a rule i more indicated that in places one sees the soft sandy holes. Pagntes quarry is own by te government for road metal material.

quarry in the Bralsingham forlary 70 feet above sea. It is clear dunned, and on this town a oiled and one sol- utum hole goes down about 12 feet. On this red oil saw my shells. The Brolsingham here has casts of large shells and the older gives the appearance of being marine limestone instead of dune deposit. Have two reel samples. Then to Strkes Point, where the Bralsingham has into a thin red oiled, then about 8 feet like the Devon- shire formation as a rule 1 to 2 feet thick but in place full roll on down to 6 feet. Over the Devonshire line another oil and in place the two oils come to - gather. Lost our sample here. Left hotel to the hotel at 9 P.M. Friday, March 15-1929. Took the Bus to Brondland Cave and then walked 3/4 mile to Papertus Quarry seen yesterday. Saw many more shells out of the young joint, and finally got about one dozen from specimens of the my large Melonios. This quarry is full of small caves, but most of them have no onais, but much stalactite and stalagmites. All of the other caves (3) are in this same area and all are in the Bralsingham.

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Saturday, March 16-1929 Spent the morning with Prof. Dayles in seeing the oaks to the south of Hotel Inverurie to the south shae. My first locality he had seen further east and here we can see superposed two soils. In one place they come to within five feet of one another and then separate ate wide. The old typography was similar to the present though less high. Oagles says the older dunes are furthest inland, and the youngest ones near the shores. Therefore my large lot of shells should be of some sort or very young. The oldest soil seen today is at the Inverurie terrace a few feet above low tide. It is less than one foot thick and in thought to lie on the Dalsingham that now shows but little above tide. All in all Dayles appears to have four soils in the Paget and one at the top of the Dalsingham, in the afternoon brought gifts things and then called up to said on the train in the morning. Paid up my hotel bills and have about $20 left to take me to Char Haran. Had dinner at the Princess Hotel with the Dayles' and their daughter and son.

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Sunday March 17 - 1929 It is raining and Howing some as I got aboard the steamer Avon this morning. Again they gave me a room all to myself mr 110 on te B deck. It is an outside room. I have now been in Bermuda ten weeks and have seen considerable of the island. All in all it is a very enjoyable winter place, but a rather expen- sive one. Poef Dales came to see me off. Later in the day the sun is out, and the ship is not laboring much. All in all the day passes and my headache is light. Monday, March 18 - 1929 During the night the wind began to blow harder for the north-west and kicked up considerable of a sea. All day the ship pitched a good deal and every few minutes the propellers are out of the water and then shake the room from stern to stem. Did not risk getting up larger than to go to the toilet room, but the steward Mr Harton kept me all I could eat. But oh how tired some of the sea and the uncertainty of life.

Tuesday, March 19, 1929 Late yesterday the wind let down and for the ship eased up, and this morning is going easily. Bed-ridden with head-ache and back-ache I got up and put on deck before breakfast. It felt good again to be around and walking. Had a light lunch and slept up and about. Because if the head winds are not expected at their full force 3 to 4 P.M. Distance between ports 696 miles, and if one got in at 4 P.M., it must have taken 54 hours for the 700 miles = about 13 miles per hour. Saying the vessel did it in 48 hours = 14 1/2 " " " Steamer Aron can take 412 passengers, besides of 290 first class and some intermediate. We got to the pilot boat nearly 3 hours before landing. Stopped for Medical Examination at 4:45 and at 5 P.M. the Customs Officers came aboard. Got to the dock at 5:45 and for trump baggage examination at 6:00. Arrived at Murray Chief Hotel a little after 7 P.M. Had the first real satisfying meal in many days. Then bought tickets to New Haven and had my bag checked by the hotel porter and returned at 9:30.

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end [7712] Wednesday March 20 1929. Had a good work in all the comfort of the Murray Hill Hotel, and a fine breakfast at 6.30. Read the New York World and at 10 A.M. came off to New Haven. And so my Bermuda trip has come to a successful close.

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7080 7080 Trip with [illegible] Arthur Cooper to New Brunswick and the Gaspe' country July 10-1929 to Dept.

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New Haven, Conn., July 10 1929 About 7.45 A.M. Am Carlson was before my home with his Lizzy and in a bright warm day we are off for the Saratoga county. We mistred through Williamstown, Danville, Putnam, Delton, to Broceton Man where we had lunch. At 12.45 we are off again through Clinton, Lawrence, Lawrence, Starahill, Cerresting to Ports- onmouth where we registered at the Reddingham Hotel at 5.15 P.M. Here we will stay for the night. Joras at this good hotel came gears up and liked it very much, quiet and reserved. Came 201 miles Lincoln, Maine, July 11-1929 Left Portsmouth at 8 A.M. for Portland, and then through Lewiston and Augusta where we had lunch. Then onto Waterville where we examined for a half hour the Lillarian Silly State, and for three pieces with Meritshirts. Then through Chewport to Bangor and then up to Penobscot Valley to Lin- coln where we put up at the Lincoln House for the night. Came 241 miles today. I was here three years ago with Dr. Keith on his earthquake investigation trip throughout Maine.

Fredericton, New Brunswick July 12-1929 Left Lincoln Maine at 8 A.M. drove to Houl- ton. Looked at several supposed

Before we saw these red hib are came acm cream-teddd layjntid whnie ss onth the eridnce of Plants, These are of the Carboniforus series, but whether have a upper Jdr on thurs.

Frederickton July 12-1929 Just north of the railroad station Anandale in a mountain stream that falls over granite. There are peined specimen, [illegible] above in the stream bed and it is more common than the coarse grained example associated with it. The fine grained material appeared [illegible] deformed. Evidently this granite cuts the the Ordovician. One sees much of this granite along the creek for many miles, at least 10 and joining as much as 20 miles. Are these Devonian granites? At a turn in the road near a farm house about [illegible] from Frederickton one sees horizontal red beds with caliche nodules grows. Some of the shells are a copper green color. Going into Fredericton one sees more of it and that it seems primarily overlies the upended Ordovician. One also sees in the dip slope hills on the opposite side of the river. Evidently it is either the Windsor or the Horton beds of the Oant sequence. Part way up the night at the Windsor Hotel. Came about 180 miles today. One tire was punctured by a nail and another blew out due to an imperfect valve.

Had another hour out in the first 20 miles. Then no more for the day. The country up to Newcastle appears to be settled thinly out along the river bottoms - first in the stream that flows into the St John - then almost no homes across the divide, and none of them along the Miri- michie that flows into Newcastle Bay. From Newcastle to Bathurst the short road of 45 miles is all through the forest and one sees no clearing until within ten miles of Bathurst.

Bathurst, N. B. July 13 - 1929 Coppen had the garage fix the two flats yester- day and so we did not job started from Friday 1pm until 9 p.m. It was an uninteresting drive to Newcastle where we put at 2 p.m., on sandy dusty roads. For Tuesday travel was light. Had a Palmer funnel here. Every now and then we saw the horizontal muddy gray-brown heavy bedded SS that would weather into thin flakes a few inches thick. Holes are practically absent. All are of muddy coarse and fine sandstone with irregular grains of coarse crysmic in which the layers fuses are quartz pebbles. It is all more a less cross bedded and the angle have long pieces of gravel. It in my layers an ochre. From Newcastle to Bathurst it is 45 miles through the woods. We arriving at 6 p.m., at the Gloucester Hotel. In places we saw the same Carboniferous SS and at the sea side as Newcastle. The river banks at Bathurst opposite the Paper Pulp Mills on the red Bathurst formation, the basal part of the Pennsylvanian. It is a brick red not quite so dark red as our Triassic. Anthracite coal, smother up about 1/3 of the whole with surrounded quartz pebbles up to

See the Tetagruche paptolite fm the Teta- Grucho formation. Leta sent them to Ruedemann and asked him to name them for Northrop. He did so and made the horizon typical Normanskill. It's therefore older than Northrop's Trenton series of the Pat Daniel area.

Bathurst, B. B. July 13-1929 one m[illegible] area[s], it might as well be called Bravens. true formation. See the sample from the type locality on the bank of the [illegible] River. Tried to telephone to Albrecht Alers, but could not find him, so Tom on our way will go to Jacquet River where we hope to connect with him. Jacquet River, July 14-1929 Sunday morning and no breakfast until 8 A.M. Left Bathurst at 9 A.M. and then drove north about 3 miles and [illegible] mile more north on the Intercolonial Railway to the bridge over the Tétamouche River. From the bridge one sees low exposures for about 1/8 mile along the north bank of the river. The Haall Shales, with some calcarenites, hard shales, and an occasional green shale beds, of the series, may be 100 to 150 feet thick, and all of it is more or less profitable for fossils, but some of the specimens are fod. [illegible] stand on end and are once a lot twisted and are frequently slicen-sliced. The gap thus make a loss of not on reflection and distortion.

As the truffles of the Tufjan area as a rule will surround this engl. Should be a marine deposit. [illegible] The thickness of certain may hinder. [illegible] is supposed to be a stray marine deposit. I am not sure that we saw any granite pebbles, and if such are present the pieces are small and do not attract attention. Where this mass of volcanic truffles came from is a problem not easily to be answered. One looks first for the present dry land of N.B. See the finds only the Tufjan, and the sample of Tufjan engl.

Jacquet Rivu, July 14, 1929 (continued) Then drove north to Turgeon P.Q. and on the sea shore to the north of the cemetery one sees muddy sandstone dipping about 20° N.W. and then rising to about 40°. Then a core to the north with Bonaventure that at the north end flints rules the Turgeon boulders in the Turgeon crag, and the igneous boulders up to fifty acres. Part- alley three-quarters of it is igneous boulders, the rest is of diluvian limestone, jasper, quartz, etc. Of fruits for Shmatipora, Farreze 2013 species, small alfrido, small Gephyrites, Leftaera rhomboidal, Del- cranella Meyantula, de. Also saw two large angular flints 12 and 18 inches across of the diluvian limestone (>60ft ces) These have some true sharp distance derethly This crag is folded like the rest of the diluvian. To me the diluvian is underlain by the Turgeon crag, and it is clear not basal Diluvian as far as for it. It probably makes the base of the Lower devonian. Its upper probably underlain by the Bona- aventure crag., a different folding crag though made of of the same kinds of rocks but in different quantities with more long jasper. The Bonaventure is undisturbed. The Bonaventure is not so consolidated and has far more lime in it, and pieces of the Devonian sandstone.

Is this "Basom" = Barbe ss? overlying and apparently conformably occurs the Turgeon Congl, like what we saw yesterday. In some hundreds after this, but here the breccias are smaller and thin maybe less variety of the igneous rocks. Here it also has Diluvian ends, and Cooper found one small granite pebble. Alevell is inclined to regard it as Devonian. At the east end of the Turgeon Congl, saw at least one large block of Heldbergian (but I do not very much), between which are also included in the place a clay drift.

Jacquet River, N.B. Monday, July 15-1929 a.m. Dr. Aleroll came in his car at 8:30 and we then sat down and talked over the Lillurian section and places to be visited. After an hour or so drove east 2 miles from Belladune [illegible] to see the top of the Lillurian section. Where we saw what may be the "Lacoun" formation though there was nothing to remind one of the Port Daniel rocks. Saw many of the worm trails running Taurus in ethul ports. Accordingly saw nothing to prove the presence of the Lacouns and certainly nothing at once of the Bouleaux formation. Can this be do to Gorge's After lunch studied the remainder of the Lillurian section, drove over to new Barclay Street. Began in the La Vaille formation with many beds of stromatopora and corals and a gone about 40' thick with many Stricklandinia perpicua (small). Farther on we saw the Clemville with Cordiparia tenuis-plicata, etc. This series is faulted and just all to the base of the visible Lillurian appears to be Clemville. It is complete with tuffs; maybe one half of its thickness. How thick the Clemville in Hole and Illume but may extend 300' feet. Some fossils are found throughout, but I saw nothing characteristic in these lower Clemville beds, nor did I see anything to indicate the higher Lillurian like the Bouleaux and high formations. The Lillurian ends with a large flora. The car that left 7 miles east of Barravante.

These foraminifera of Clarke only the true Bonarentine are here Byrga. If Cutaeros a Neogenic try should on the of Corticaliform as I think they are, Being out of the clusts of the B. try-mundoc of lay Paleogric age.

Jacquet River, Monday July 15=1929 (cont.) Nearly everywhere the upended Silurian is unmem- formatively retained by the Bromavertine implements. It always overlies directly half the Silurian. It does not in any one case than 1/2 miles, and its thickness is not great. At the west end of the section it runs north to the Silurian but hits against a vertical cliff of it. Allrock is displaced or grames physiographically from if the Bromavertine was not laid down in Cretaceous time. He thinks he who has some support in the Foraminifera found by Clarke and determined by Chapman. This evidence is almost worthless. To me all of it is best called Pennsylvanian and certainly isn't older than Drinker = dip Mississippian.

This series in the same one saw yesterday on the coast strolling through the level from the sea to the railway.

Jacquet River, Tuesday July 16, 1929 It was nine A.M. when Dr. [illegible] arrived. He then took us east three miles and then south to the International R.R. at Culligan Station. We then walked east about one mile to the outcrops of Stricklandinia tuffs of La Vielle. There are one large shale and a coal. There are small quartz veins inside the tuff in the Stricklandinia zone. About 85 to 100 yards east are beds with the Steffrochetus like algonids that were seen on Sunday in the Tufjen cycle. La Vielle is as here as at Mrs. Port Daniel and transitions into a transition zone - alternating of ls and red brecciated shales. Then comes the 'Basen' premist ss that weathered, trails are scarce, and here one sees more of lended tracks, not if the Taconites or common at Port Daniel Drift. The 'Basen' is here much thinner than on the north side. Further east and lying directly on the 'Basen' sh are the Tufjen cycle. Saw one small cup coal in it. In the afternoon went back to Belle Dame River and then south to the International Railway. Walked over about 1/2 mile to the cuts in conglomeratic sandstones interbedded with joints of what may be tuffs or ark beds. In the paste of the cycle, got a number of poor casts of forms and of which appear to indicate did Christians or even early Ordovician, but

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Jacquet Rivin July 16-1924 (continued). a large Diaphorostoma, Eatonio singularis, Oristella lata, Orthrenus with septa far apart, one firelace, several scotiripods, Steptilaasma, small Furrosits and other things. These prove the beds to be deep Ordovician or even Cambrian time. Then collected on either side of the Belle dune Rivin at the trumpile near sea shore. Here Steptilasma and small Furroisits are common, and also a small Rhiz'dmella and other look like Pennacaria stuaroti but very small. Also saw a Lep. rhombor dali. These are on the west side of rivin. On the east side of rivin these same things occur but here also Leptrocelia flabellita, and L. planocum crepa. The strata are brownish-grey fine grained muddy sand-stones with some grey thin ls from 1 to 6 inches thick. All in all to age in lower Ordovician, and maybe higher than any part of Stuart Cove at Dalkousie, N.B. Kindle has been wanting to make these strata Silurian but I did not see a single Silurian species, of the small Steptilasma and Furrosits do support Silurian, but just such things occur in the Heldutropia and Ordovician.

Cooper and I again visited Black Point on morning of July 23 to collect more fossils but got very few good ones. The section here in atwhas follows: Beginning E and going W. Volcanic lava flow seen at low tide about 30' thick. Long beach to E shows our arches. Pontanerus Almyrus beds about 35 yards across. Dip 45° N.W. This fossil goes through central 50'. Overlaid Leporiditia Crelaspin etc. See small list of fossils. These volcanic flow making Black Point to heart of which is Dickie Cove with its Dilenian (two grms). Black Point. These brittle l's reminded of ocratalimestone and when they belong is hard to say. Certainly Diluvian and apparently early rather than late. Look this up on Aleredo map. I did and they are the farthest E beds of Black Point. Can these beds be the regularly bedded ones out in Laper- ditia that occur on the eastern limit of the Belle dune Gray section. See beds 2-3-4 of July 20-1929. Aleredo thinks not, but I would place them life in the Clemville rather than elsewhere. And and he has large collections of these black l's.

Jacquet Rivu, Wednesday, July 17 - 1929 Drift Alcock started out over for Black Point P.O. to see what he expected as the Stricklandinia gaspiciens zone. A little collecting revealed some smooth and striated forms. Somethng like to put hida was a zone of Pentameus Hogus (small Clinton var.) and mac rare Colypina hemispherica. A little higher the latter shells were common. The large specimens of Stricklandinia over the hard at times distinguished from the young S. gaspiensis, but the association with the forms of C. hemispherica and Pentameus over show that the region in Lemsville and mt La Vielle. I'm also here me specimen of P. radiatus and several Tax of the Pentamens Hous (smally Black Point, To the over is a great many of Lasa flows, and to the east of the Pentameus Hous are then redded clust flue ls, hard and fracture emchridals, very thin interbedded Hard sh. The common forms were several species of Ruthstrafhi, and more here we saw two Tautacu-lits, and a dol manella with fragments of Colymone. These led's dip to the E. while the Pentameus was dip to the W. and to near stream Farther west at Dickie Cove, we again saw the Pentam- erus Hogus beds. Here C. hemispherica is very common and Ruthstrafhi. We also saw the striated Stricklandinia, A. articulata, Ortho: Flabellita, and a Niagaraan large Bucania with flaring mouth.

The Bonaventure formation is well developed on this coast, from west of Bathurst to (Campbelltown). It is here more light hick shaled than on morne in the Lake Crock. The pettles and especially the laye plies are angular cut off the sharp corners removed. The deposition is irregular as in iron deposits, the crop grows pinch in and out, and that in one calm irregular can bedding. It is more found inland more than 1/2 miles, and above the sea not more than 700 feet. Off north west of Lickie Cove there is an island all of Bonaventure formation.

Jacquet River, July 17-1929 (Continued) We then entered inland to Jack River and on its land Copin and Alcock collected some large cup corals with very large twisted centers, always branching favorites Pentamerella and L. chmaitidali. This appears to me true to his Permian sea and maybe of Ordovician time. These fossils came in a sandy shale at least 10' thick. Be the small lot collected. We next visited an outcrop on the road side about 3/4 mile south of the Barclay House and it turned out to be regulatini New Zealand fauna. Here we collected L. chmaitidali, Leptostrophia pyflana, L. teatei, Spirifer belamellus, Cretospina disparilis, Dalmanites, Rhacops, several tirabres, Philodips, Camartozchia Rhipidomella flata These beds must come in near the Tuncom coal, and get then maybe hundreds of feet I struck between the two horizons. In any event is in the oldest frondiferos Permian so far seen. It is a very hot day and we stopped working at 4 P.M.

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Jaquet River, Thursday, July 18 - 1929. Doctor Alecott told us in his car into the area of the Bathurst sheet. First to the one at Turgeon Village and then rested for about 1/4 miles. When the road from the church to the one ends one comes upon what looks like the "Basen" (Later made it out as Barbe's S). sheer. These are here muddy SS, greenish, creamy red. As a rule the strata are banded films with zones of shallow ripples and an occasional zone of sun-cracked surfaces. One of the latter ones have been rain pitted. As one goes up in the series the surfaces of separation between the beds become more and more often arthritic (the grains are small), and in places that are crypt, with the fossils, up to 1/2 inch. Towards the top once and more crypt. zones are introduced and now some of the fossils are of the Bas- (=surface) en itself. Here beds are decidedly cryptic. Then follows more gneiss SS like those below, followed by an area 600' across or once with no rock exposure. Average dip 45° to W. Just resting headland exposures Basen, also banded with zones of collars, and now all are more crypt-bedded. They are to be seen along the south shore of the estuary that I have, Back if ever exposes Baraventine. Last headland across at least 300' of "Basen", and the full way over into the exposures no Silurian. The "Basen" must continue from where first seen up to the Turgeon crypt, and for a thickness of around 1000 feet. Alecott will measure it with chain.

We found this same sort of large Palaeocclus on the shore west of Belladuna front on July 19. See note about it.

Jacquet Riou, July 18, 1929 (continued) We must be able to overtop the great Turgen horizon and bore east, for which at least two-thirds is a sign of success that Alcora thinks looks like what he really believes in flora. If we try any path with it. See unimportantly. The Turgen is plainly overlying the horizontal Bonaventure and in places fills hollows in the Turgen. This angle, from our work for a long distance, to a little dead end employed by Lara flora. Then to us, more angle, and then a very thin line flora. Together they must be here 2000' of Turgen angle or even more. We then continued south to Turgen R.R. station, and half-way back came upon a Lilian exposure of young "Bella clune formation". The ds stand near on edge and other beds has been disturbed away it leaves behind semi-siliceous fossils the most interesting of which are small and very large Palaeocycalus mist. Other fossils are cupenae, Ortha, Flabellites. Fossils are scarce. The design appears to be about higher Clenoile or even La Vielle. We then continued east across Hendry Brook to see the Elm tree slate, but instead encountered the dead angle, as seen yesterday in the intersection of R.R. road. Further east one came upon an apillite suggesting the Leptocaelia flabellites beds seen yesterday. Accordingly the Elm Tree formation is new.

This emyl is composed of smaller pellets and in fallen variety than the true Turjem. It has much reincrusty, some jaspen and other many pieces if he so wills the Basan, but these may also be joined. Of its pieces there came also fallen. At the top it had a broken Stimulypora; and a worn ends.

Jacquet Ruin, July 18-1929 (Continued) Then mistored east to Limestone Point about one-half mile west of the post at Mrs. 3/4 mile away from Looming Point. mile over by Elm tree Village. At the shore to the east of the Point there is a greenish greens arell, and next near a zone some ten feet or if ss much like the "Sason". Then follows to be as a series of ls. Some thick reddish, red- did crinoidal ls, 10-20 feet thick, that may have furnished the red Crystalline ferric in the Tujam karys backshiffs. On top of the ls here is a thin reddish layer of some ls al- alternating with con pure zones, but to visible in my mud there are from 30-40 feet thick squiggled and more a con metamorphosed. Good fossils anyway scarce and none can be easily extracted. Just what the age of these groups is we could not make out. Further over the lower ls dare ends, Shima- tipora, and small Sticellandinias. Evidently the latter beds are at the top of the Clamville. For the upper ones maybe La Reille. Below these ls comes ss (Sason hills) that have cones at base, the whole may be 1000' thick. Next down is a red coal zone much like the Tujem, 200-240' thick. Next red agillite that shows our bedding 200-240' thick. Then ss (Sason hills) with coals 30-10' thick. Then a core without reef followed by an androic ss. Another core followed by a great thickness of gypsum material, that we dig for harase.

Strickland's gone there about 40' this.

Jacquet River, Friday July 19, 1929 dark cool morning with rain in the air. On the shore a strong current off the water and collecting disappearles. Started with Carpen Lake [at mt 2 miles] tr owest of the Belledune group. Started in to collect in te La Picelle ls. Through the lorn 140 fur west many small and very large Palae-ocpulus, and again 40 fur Nthen at the top of the Stricklandimia galbiansis gme. At the base of this scain saw one Cocliospira hemi[illegible]cus and a little higher Carpen for others looks like Dzyotella. Also Chinito (common) Spirifur radiata and J. Niagaraensis and other things. St Ryan to rain at 11:30 and or we returned to the Baroley House. Stayed in te hotel the rest of the day. Will again go on te section and determine it in more detail.

lee. Does this indicate movement from the N? Dury it cannot be from the Atlantic, What I am describing is a syncline with the W limit vertical to overturned to as much as 40°, and the eastern limit flattening down to 20°. Nor anything of the Shieland in a gone because it is covered by the Bonaventure coal. on the eastern limb,

Jacquet Riva, Saturday, July 20-1959 It is an at normally cool morning and as testy in dark. Put on extra clothing before starting out. We motored early to the same farmhouse as yes- terday, and then walked along shore almost east of the long Belladune Raup. Here the Benarantine eml. goes out into the sea and crosses the Lulurian only eight. 1. The first Lulurian is the area of the Benarantine dip 20° N.W., and in the Palaeocyalus gore. Here also can may occur the large ring like erinid Clamulus or other actinotic of the Ohio Clinton, We may also have collected Hyattidina but not they are Esprificue. It is 125 yards to the next gore but we saw the Palaeocyalus out in the lown strata. 2-3-4. Lepeditia beds, 25 yards; 2, beds of Lepa- ditia only small ostracods, 3, at ten fur kips has Ostr- kerdonta, 4, at further kips has small Rhynchomella in nests, Bryozoa lagen at tips. 5. 50 yards later a Stomatipora gore with Favosites having forids 1/8 inch in diameter. 6. Ten fur kips a gore of nodular or irregularly forming favosite, Dip 30° N.W. 7. Stimmer WS sands to the last ordula is seen. Same dips as before.

= Barbed Basem series at least 570 yards acrn = ? 1300' how much is Basem in numbers 10-8 cannot be seen, scale it "Basem" on the basis of geological position beneath the Turfem series (= Klevonian) and the lithology is not opposed to this view. This "Turfem series" appears to be last of eastern limit of syncline. The Basem series is the first of western and much steeper limit. The Turfcon has here a width of 575 feet, but as it is drilled up in the center of the syncline this cannot be the true depth.

Jacquet Rwn, July 20 -1929 (continued) 8. Cornuel gone to Belle dune cray?, about 300 yards acrm. Belle dune way. 9. Crwud gone 150 yards w'to brock. 10. " " " 150 " to first exposed "Basem?" Green annady ss tr sandy sl orathering red, Dip 43° N.W., basem is apparent to last of E. limit. 11. Basem series seen 100 fends acrm. 12 Cornud gone 410 yards to what Alcoch calls Tujcm. Brock lare. Dip 75° E, 13. "Tujcem series" a, eastum red orathering sl with one gore of fine emyl, 4' thick, 13 yards acrm. b. Red truldn emyl, 4 yards acrm c. Gry anthric emyl. ontlo pettles 3½ yards d. Well ldded truldn emyl. 6 yards e. Grey anthric small pettled emyl. 3 yards f. Red orathering sl 4 yards g. Red crasse emyl. with red sl, gry anthre and gnes of trulden beds, 40 yards acrm, h. Red sl and emerald area 10 yards. i. Crarse red emyl. 5 yards j. Red sl 9 yards k. Crarse cmgl. 17 yards

Here about one sees no fms in basem series. If all this space (242 sqs.) be basem'd, it is 725' thick. On the eastern limit is at least 1300' thick. Observed July 21-1939. This La Picelle is about 300 sqs. across, and the thickness must be 600-700' thick, a far greater depth than that of the north coast of the Bay de Chaleur. Alcock has of La Ville here over 1000 ft. 85 13 38 31 8 4 9 25 ------------------ 213 27 24

Jacquet River, July 20-21, 1929 (Continued) l. Red sl & yards m. Crasse emyl. 31 yards, Red n. Red sl 12 yards o. Crasse emyl. Red 3 yards p. Red sl and emyl. 3 yards. fault contact [Alcock] 14 Bascon green ss and sl or attaining red, strata almost vertical but lean sloping to W. 33 yards to fishermen house road, 80 yards more on other side of road. 15. Bonaventure over and green 200 yards across 16. La Vielle modular ls seen at low tide, 85 yards. Has Halysites, Favosites, Stromatopora, and the rther things cannot be seen in the dirt, sea weeds and the cliffs of the strata. Strata more than vertical, slightly overturned. 17. Even bedded then and thin ls separately by very thin sl zones. Saw no fossils because of the sea ocean, but appear to be the Lefevre dition beds of the eastern limit. Overturned almost 10°. 13 yards across 18. Corneal green of beach and core, 38 yards across 19. Thin bedded granitic ls seen under Bonaventure emyl. Cannot be collected from, 31 yards across. 20. Thiers bedded ls, 8 yards 21. Thin and thick bedded modular ls eroded with small hemispheric and branching Favosites. 4 yards thick. 22. Modular blue ls without fossils, 9 yards across

Turgeon enl. atnr 250 feet "Bacon series 725 feet, Cleared on line of 250, At nr 600' La Vieille " 600 " (maybe 1000' [area]) " " transition 300 " Clemville series 775 " Cleared has strnr 3000'-4000' " atl. 800 " 3200 " for Lilerian and its orleans, Noted with Alcroa July 24-1929. La Ville Transition of 200m to La Vieille, 138 ? ? Clemville 365 yards to fault, Monday July 22-1929

Jacques Riru, July 21-22, 1929. Monday 23. Rhynchotreta gone at top with Oenite etc. Lower Atrypa, Leptaena and [illegible]. Ordulals 27 yards. 24. Ordularls. Palaeocylus gone, specimens common and large. Ohio Clinton crinoidal stumulus, etc. Shale own turned atmt 20°-30°. Thickness 27 yards. 25. Green sh with gones of ls and ordularls, becoming more sh helm. Has Stricklandinia gaspensis through bogues. Palaeocylus also from throughout this zone. 26. Covered gone, 33 yards 27. Green sh with thin ss, 105 yards 28. Red and green sh to fiddermans road th three, 100 ofjus 29. Greenish cyml with small pertles, coarse ss, and tuff gones. About 190 yards across. 30. Covered gone with brook, 20 yards, 31. Green sh with red sh gones and fine cyml. Dip var- iation, 50° to 70° E. 18 yards across 32 Covered gone 38 yards. Section continues great Sharp fold and syncline to w looks like fault with dip. Covered gone 32 = 3 & etc. 15' ss & [illegible] came as ① repeated ② fine cyml, 15' thick ③ Red sh. G. thinnin. ④ Red fine Cyml. 17 yards

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Jacquet Rim Monday July 22-1939 1. Green and red sl with thin ss 35 yards. Dip 15° S.E. About 50 feet thick. 2. Quartz cmpl., small pebbles, with thin ss, 1/2' thick 3. Red sandy sl 6' thick. Atwt 70' re- peated to W. 4. Red weathering fine cmpl., 17 yards 5. Green and red sandy sl 5 yards 6. Corred space and Bonaventura corn) 31 yards Dip S.E. 7. Section now reverses and repeats 4, 3, 2 and 1. Dip 40° N.W. Then come three dipfer beds. a. Green and red sl, grey and red cmpl., with thin beds of ss, about 50' thick, or atwt 18 yards across with dip 50° W. b. Red weathering and green ss and sandy sl, 72 yards. Dip 50° N.W. c. Green and red sandy sl and ss, 50 yards across d. Intraformational sl cmpl., tumbles of sl 5 feet thick e. Same as c 20' thick f. Same as d 18 inches thick g. Green and red ss with intraf cmpl. green, 30' thick h. Forest intraf. cmpl. gone with sl parting, 30 yards. Dip 60° N.W. i. Green and red ss, sl, pebble cmpl. 32 yards. Shows fine of terridal weathering j. Thin bedded green and red sl, ss, 50 yards. Rippled beds. Dip 60° N.W.

900' 10 40 7 2 4 7 5 6 88 120 33 6 13 10 70 60 49.9 149.7 = 1200 Alternaology 900'. am Strick.

Jacques Rinn, July 22, 1929 (continued) K. Yellowish streaking sh grit calcareous nodular layers having Phacodermella, 57 yards tr center of syncline. Dip flattens from 60° to 30 going W. Also has O. flabelloides Platystrophia, corals, small Palaeospolus Grit going down 150 yards (fibs not seen) appears to be 10. Coeloparia hemispherica gone. Arctid bedded ls tectonizing shaly and sandy felsm. 10 yards. Dip 70-75° E. 11. Thick bedded grain ss with sandy sl and stone and below pettles cmpl, grms. 45 yards. Dip 75-80° E. 12. Small quartz pettle cmpl. 5 yards 13. Green sl 2 yards 14. Stomatipora - Favrite (layer) in sandy sl, 4 yards. 15. SS and sandy sl with one cmpl, bed, 7 yards. 16. Small quartz pettle cmpl, streaking yellowish, 5 yards. 17. Corund by Bmarantine, 15 yards 18. Same as 16, 6 yards 19. Core. Corund gone, 88 yards across. 20. Purple streaking pettle cmpl. and sandy sl making joint; absence of zone pettles fall kinds up to 2 inches across. 120 yards. Dip 78° E. 21. Red and green sandy and cmpl sh, 33 yards 22. Cmple like 20. 6 yards. 23. Corund gone, 13 yards. Probably like 21.

From the fault zone in the Clamville is according to Allen on 1800' thirty including the mechanics, or 1200 for the sediments. This takes us to the next fault zone and the the films are repeated to Dr.

Jacquet Cirn July 22, 1929 (Continued). 24. Green ss and cmfl, offt. 10 yards. 25. Same as 21, 70 yards to break, 8 yards mnet W Dip flattens from 75° to 35° E. 26. Yellowish gray being soft cmfl. Dip 35°E. At mt 60 yards across, Some much crumpled T? fault gore that dips W at mt +45° Across has fault gone here Then a tuff-like purplish gore on the volcanic flow. Offs or bedding. 35 yards at contact with dip 45°W. Volcanic flow 15 yards, dips W at mt 45° Tuff gore 53 yards across Volcanic flow, amygdaloidal, about 10' thick Tuff gore about 10' thick. Dip 35°W. Volcanic flow, amygdaloidal, about 100' thick. Tuff gore 15 yards and volcanic flow 10' thick. Fisher- man road to three ermes both gors. Tufts showing our bedding, about 160 yards across. Actual thickener less because measuring around deadland. 27. Muddy ss and s? grits intert enyl ? tuff at base. Dip 45°W, +9 yards. Section now again rises. 28. Interformational cmfl. 6 yards. 29. SS and S? much disturbed, 15 yards 30. Same as 28. 3 yards Dip 50° W 31. Regular bedded ss and s? green and red, 17 yards.

44 Another cave with Diluvian beneath, near the end of which the Dil. again dips to earth. This cave is several hundred feet across. 45 Headland of volcanic flow with a thickness of about 100 feet. Then Bonarentino makes a crash and crosses Diluvian for about 7 miles to W.

Jacquet River, July 22, 1929 (continued) 32. Green sandy s7 and ss, even bedded and much ripped. 15 yards across. July 23 collected some from here. 33. Same as 32 with large Tarrots near base. Also much ripped. 44 yards. Dip 45° W. 34. Red soft s7 45 yards 35. Interbedded ss and s7, 9 yards 36. Regularly bedded ss with flinty veins, see collection. Also ripped, 16 yards 37. Soft red s7, 22 yards 38. SS, 9 yards 39. Green s7 with some ss, 87 yards, dip flat- tow down to 30° W. 40. Soft s7, 20 yards. Dip 30° W. 41. Corund gone 19 yards. Then Bonaventure to Fidderman road to shore, 70 yards and 18 yards more on w side of road. 42. Soft weathering purple s7, 94 yards to core with tiny brook. Dip 43° W flattening w. To 22° and then for a long distance practically flat. It is 310 yards more to where Lelurian grestoneath beach and a point of Bonaventure. 43. Bonaventure across Lelurian to little headland 25 yards. Around the point there is 70 yards more

44 form sk creating purple, continue no 42. Here it has any thin s.s. dip variable from 10° to 30 N.W., 35 yards then lose same and beneath the Bonaventure begins to rise to northeast and dip finally from 40 to 50 E. and turns up against the red floor. 45 My third volcanic flow creating several small points, seen on a horizontal distance of about 1000 feet. 46. Bonaventure and head-guards make the shore fast Armstrong Brook, Jacquet River, etc for about seven miles to the Lilenian just east of Black Point Jacquet River July 23-1929 Casper shipped two boxes by freight weighing 220 pounds. By Ephron prepaid a small trip to Reedemann carrying the Teta prochoe grafts/lots. In the morning collected more mme at Black Point in the Pentamerus beds. In the afternoon looked up a few points in the Lower part of the Belle dame Gray section.

Dalkousie, N.B., July 24-1929, Wednesday Left Jacquet Rim at 8 A.M. and at 8:45 we called Dr. John Alcock at Charlottetown to tell him what we learned about the Silurian since last Friday. Then motored to Dalkousie and put up at the Queens Hotel at 3 dollars per day, we got here at 11 A.M. After lunch we collected all afternoon in Stewart Cove in the Upper Dalkousie beds. Collected less than one half the beds, and will go at it again to morrow morning. Cooper is delighted at the good collecting and therefore joins. It must remind him much of his Hamil- ton collecting, since we here have calcareous shales. Some of the Dalkousie beds are one turn or flared and others all stand at high angles get the disturbance, far less than in the Silurian series. Maybe the latter is due to the greater load on the top of them. Cooper got a fine lot of fragments and pieces of a large Lichas in the area of the Stewart brook = Clarkes arj. I collected most of the time in the ark beds with Renweldae rida stewartii having other fossils common to the long spiral gastropods, brachiopods and helms.

The Rensselaer's of this lorn zone appear to me be eraser plicated. Also see if they are smaller below in the older beds. Bivalves appear to be the most persistent forms of the Upper Dalhousie beds and many of the species may go through most of these beds.

Dalkousie, N.B., Thursday, July 25, 1929. Collected all morning in the Upper Dalkousie beds of Stewarts Cove. I worked all morning in the Coelidium zone next below the Renosalaria beds. Got a large lot of Hirulves to which I added the same forms from the top of the next zone, Birulves dominate these beds and all else is much rarer. Some Renosalaria occur in the Coelidium zone and somewhat lower--[illegible]-- Cohen collected the lower beds down to the Stewart Brook. He also got a lot of Hirulves but here Machildae and endis are far more common. His collection is from the 10 foot zone. In the afternoon we collected a small Heldu--[illegible]--terrigen fauna from the basal blue sandy and calcareous strata that improve us. Spirifer emacius is the commonest frond along with Schuchertella and orthothona Cohen got some Dalamanites and a load of Calpinea while I got some tails of the last named form, Phactis also occurs here. These strata are fine grained for their mud directly underlies the tuff. Further southeast is a wide marsh exposing no beds. There can be no doubt that these older beds are also Helderbigerian and not older than the New York Creemans.

Hyd Miller Cliffs at Mt Maguasha. In the crest towards Flemons Point the light greenist Devonian ss and sandy sl are very horizontal but begin to arch having dips to the crest from 2° to 10° and dip to the north at about 5°. The centre of the arch is to the east of the Maguasha draft, to the east of which for some hundreds of yards one again sees no outcrops. Then seen they dip at about 5° and further cast steepen to about 15° or from there and here they are stated upon the Devonian flanges under the sea. red to the crest from the nearby Bonaventure. Saw a few Heliptychius scales, me for first tail, two small Archae- pitys, and considerable plant fragments. All the Ordov ss are lim- amons shipped and in one place saw a little lim dredging. The Devonian goes far to the crest, two miles east of Gino Point. The Compston Drw is opposite the farm and to the cast of this lumbering town. Paid close attention to the conglomerate bed 10' thick to the cast of the little stream west of the draft, it was Boulder conglomer with gray granite and igneous ones and in signs up to one foot across, All are well rounded and most of them are of own quantity and the granite. Some of the are striated. Got me five boulders of Walpits and another dilemia one with a coal. Near the stream saw two large boulders (18" across) that cleaved once are a chalybite, weather a dim time. striated, but these were loose. All about this stream and up it are many loose large boulders and partly are of Pleistocene scratching. There is then no evidence of glacial action in (See second page to right)

Dalhousie, N.B., Friday July 26, 1929 Collected most of the bees in the lawn and upon Dalhousie Bells. It is almost impossible in bed not to get good Licherella pseudopulcata, but one good one and a lot of poor things came to identify the fauna. Trimbed 2 acres of grass mecca fauna. Bees 3-5 yield no fms and had 6 lies between tuffa and orleanie rocks. Most of our fm's come from the diffen Dalhousie bees or those of Stewart's Core. Corpus shipped three large boxes of fm's. The last one came fm June 7. Did not take any of the large cards. Dalhousie, Saturday July 27, 1929 Took the 7:30 A.M. ferry across the Restigouche to Maguasha to visit the Hyld Miller cliffs of Sguamenes Bay. First called on Anthony Plomde but he was out collect ing. In the late afternoon he found us in the shore and then went to his home to see what he had in fishes. He had one good fish but Stindle had already bought it. The rest were from Bothriolopis or worthless stuff. Bought them aforn for $1.00 that is worth 50 cents. See jagets left in continuance.

"Huge Drilled Cliffs" in the Tordel bed. The tordel lie in a anticlinal cement of the same general color as the Oerrman ss and are more indurated by the same kind of ss. I am much better on less films most in view in northern. In places the tordel bed has short beds of ss with our tordels = filled in places between the tordels. The mistake was first made by Ellis in saying that he first came to see it (I think) long ago from the Germanian folded bed, the Bonarantine to the east appears to lie conformably up on the Germanian and to have the same amount and kind of deformation. The contact between the two formations now main surface with irregularities for far feet included. Large slabs of the Oer. lie in reverse of the Bonarantine. According me sees here no unconformable contact and the Bonarantine is more folded here than in usual further east. To the west of the way the B. under by the Germanian and makes a high critical red cliff, the top of the one being about 400 to 500 above sea level. Maybe me half of this hill in Oer. The rest Bonarantine. The Oer. directly beneath the B. as seen mostly on the west face of the outside that is or colored, inside all is green. There is no transition here from the Oer. to the B., many irregular in places are lines of cryl in the B., but none are prominent and than a few rounded jut.

"Hugh Miller Cliffs" The bedding is so regular and coars e or wide an area that one must conclude that the Devonian is not of fine definition, but in a sort of delta deposit at the inner end of an estuary. No one has ever reported in the higher Der any marine fossils, but the beds over y Campbeltown have ostracoda (Rhodania) and reptiles are different. These lower strata may be typical estuarine, while those of Hugh Miller cliffs are of fresh water delta. Britholepis and Archaeopterus indicate Upper Devonian time but it cannot be of the later Der. The apparent conformability of the Bonarenture on the Devonian perplexes me as the Acadian folding came long before the time of the Bonarenture. Can it be that the Der in this area lay almost flat after the B, over laid on it, and that the deformation present is post B? I am puzzled today as much as I was in 1913 when I wanted to include these "Bonarenture" strata in the Salpe series. I can present a good argument that the "B maranture" is not the true one of the eastern end of Salpe, but upon the whole the upper red series had better be regarded as of the Bonarenture.

July 28 continued. Further east near 3/4 mile Held again occurs inter- twiddled with Orleanica and here we get Spirifer emcinnus, L. chmtrideli, small Creistella and on certain beds an abundance of plant fragments. Above these jossy frondifurus beds is a third zone of the same blue muddy ls that has scattering well rounded petels, if the Oratapedia ls [?] kil. These petles are up to four inches long. A little further east at about 6 miles pm Oratopedia occurs the same ls intertwined with loras. Here we get the Dietrella, A. reticularis and L. chmtrideli, A little further is a mt arnt 1000 feet high of lara. The Held first seen is cut by several besader-like dikes from a few far thick to one gone much thicker, All if the strata seen are Heldutayian and I should say = Lourdalkousic. At least we did not encounter the Rensselavia stewarti horizon.

7080 Matapedia, Quebec, July 28, 1929. Sunday. It rained hard early this morning and we did not leave Dalhousie until 9.30 A.M. The roads were good 17 miles to Campbellton and then on to Matapedia, where we arrived at 11.30. Crickmay was waiting for us and soon he had his maps and explained what he had done hereabouts during the past three weeks. He has to survey in the roads and houses besides doing his geological progress goes slow. After lunch we continued four miles to the east down the N. side of the Restigouche river to about 1/4 mile west of the first covered bridge. Here we saw the Helderbergian dipping W and or in suring as the section rises into higher beds through about 1000 feet in thickness, All in a blue l's with considerable mud impurities. We saw the strata along the auto road, the Oriental R.R., and finally at the river level once occurs the best exposures. At the base are spiriferella smooth and fairly plicate, also Athyrisa reticularis, Spirifera and small Favosites. Hidden came Delthyra sculptile; and it thrives through the section. Much hidden occur common of Strophomena punctulifera, Spiriferonta keelii and small Orissistella. In this zone also occur groups broken and displaced Stromatoporae and large Favosites sites along with smaller branching form, Lechstromtrideli is com- mon through out, and in places Hirudis. Hidden are spirate Eatinia medialis (see page to left)

July 29 continued. On another road found a dorsal valve from undoubted Dictyella crugmanensis. On the Bosalquick road two miles E. of Dawsonville are collected macradial cutting. Here a small called Fa- rosites is common, a small branching form, Halgites and many small Helipora and cup corals. Of hashidros we fit one Dithes tonchardi, Ottes; fewista like Rhynchomella whitii like, (Merista and Onistilla.) The surprise was two large heads of Calymene camerata. He did not see a single Heldukujian guide found and Helio's this gave T.T. to say Kazan because of its more Silurian aspect than Lorn Derman. Further towards the Restiforche valley we found another road cutting, limestone with the same cyl montagne y ls pottles that we saw yesterday. Here the ls pottles are all larger than those seen before. This is in the Heldukujian series and Gridway has other fossils.

Matapedia, July 29-1929. Monday. Started out at 8 A.M. with Cope and Crickmay To see the remainder of the fossil bearing rocks he had discovered. The Matapedia series well exposed all about Matapedia consist of dark blue consolidated sl and alternations of the same sl with thin rounded ls and some thick seams of quartzites. In the sl at 5 ½ miles up the Restigouche river from Matapedia on the New Brunswick side beside the road are high exposures of these sl that are constantly breaching down. Here finds occur but extremely rarely. One for now Cyclospina tricaudata, the platella of Pomo flexilis, a large Cystroneas, and Atronsaw Bruthrophis. This then proves the superiority of Matam time and to equal the Tetragouche series of the Battourist shut. These ls are a dense conchidally featuring oral and about earrid free life. One sees not a trace of organisms other than an occasional Bruthrophis. It has generally been supposed that these strata must be Diluvian because of their proximity to the lower Devonian. The lithology is also far more that of the Ordovician than the Diluvian. The Matapedia series is said to continue up probably the Matapedia river. For continuation see page to left.

July 30 continued. Then fell on a huge calcareous shale with crabs and fragments collected some prod cup crabs some years ago. Then begin the first and weathering shales of the season, they go to Ferricco creek. For see see my paper of 1946. Between the two nodular zones of Bouleaux there is much of semi-cracking. Corpen took a photo of it. There are several groves of it. The prisms break out to a foot in depth. About 1/3 of the distance between the two nodular zones is semi-cracked. Stopping at Bag View Inn, near to Mr. Cyr, at New Richmond. The old Robinson Hotel turned down at my 5 years ago.

"New Richmond, Tuesday July 30-1929 Left Matapedia at 8:15 A.M. going E along N shore of B. T. Channel. Shortly west of Oatway we saw Devonian pebble and brindle engl. along the road side. It had a strong dip to the S-E. General goes in a coarse sandstone. One miles east the same Devon Engl. as exposed along the road side. Black Crape Section. Coelospira hemispherica, Chmites etc occur in lawn part of section. Dip about 60° S-E. Shortly above came in Stricklandinia gaspiciens and they detained layer size trends to top. Are estimated that they ranged through 150 feet. With them occurred an occasional small Palaeocyclos, Clorinda and many corals. Then followed strata 100' thick at the top of which occur large Palaeocyclos, Rafinesquina, Leptaena and by Rhypidomella. 150' Apparently all of the lawn if any 1926 Japan went/Out should go into Oatmville. At several places in this thickener we saw the Crust (sp) The next 70 I did not make what forms occur here. Then comes the Stricklandinia gone 150' thick and the series terminates with large Palaeocyclos. The arndular layers = La Villed cause about 200 there- [illegible] cued far east of prominent modern's headland, around which we can not get at any certainty. Continuing west by auto road.

July 31 continued. There are also beds of sandy ls separated by red weathering of Corbin and I concluded that the whole could well be interpreted as a reef deposit formed in the lava flow and cml. accumulation. It is rather a local affair than a wide spread formation, but the time in West Point Is or higher in the same series. See the print collected. Got to Port Daniel at 4.30 P.M. and put up at the home of Mrs Claude Sweetman. Then called on the Orcels family stopping at the Jureaus = Chaleur Bay House, next to Mrs Herbert Sweetman's. Finally after supper we all motored down to the West Point Light House. Before getting to West Point Ridge we turned to the sea shore to see the Lulberian at the road going in at the Butler Factory. It is the Indian Point series. Looks much like the Bas- em series with Turnums and worm tunnels.

New Richmond, bred day, July 31-1929. Started out at 8 A.M. for the Black Cape section. Went to the mine by the Fidermano road east of the station under the trestle. Saw little of note in the Boulcaux. The oolcanic series appears to begin with a thick tuff zone and then came engl. of ooleanics and oolcanic breccias. The engl had many boulders of oolcanics but also were pieces of the older strata. The following ls are also a compl. of the Oost Point Crs. Talcraious, we collected some of the fossils, but there is little of any great value. Then came a long series of flows and engl, the latter composed as before of ooleanics, older strata and pieces of the Cristolcrinious ls. This took us to a point around which we could not get. Finally we found a place from the railway from the grounds to the mine where we saw ls cast of the point around which we could not get. Here the ls are actually beds of agulaton ls replated onto Lependita, Cordo Frederics of stratiforma ends and pieces of ls, and end breccias lying in a mass of Coenites. Cristolcrinious stems are common here. See pages left for continuance.

Baell of Campbells stand a high iprems man and seeing it across the Rostfrockle it makes a conspicuous isolated man - a monad-nroll-like man isolated in a map topography.

Centu, Port Daniel Thursday August 11-1929 Yesterday in motorring E. and after getting to the east of New Carlisle and while on the low coastal land I was impressed with a mountain to the south that at first I did not know. I said there is a hump in the land that I do not know, and it stood across our path. Finally it dawned on me that it was the Drill Point Ridge. In other words here is a- mother mountain range striking through Macguarvan Point out into the sea - Bay Chaleur. From Matapedia to beyond Renouville we are all too way close to the igneous crasses that hroke into the surf Paleognics in late Devonian time. Farther south they join farther into the land. Above get towards New Richmond they make an impressive dight leading back to the crest. The next high land is just east of New Richmond and lying Black Capes. Beyond all the way to the Drill Point Ridge the shore is all Bonaventure. In the morning Dr. Wells took us in his car to La Vielle to collect the long main part of the La Vielle formation along railway track. But a fair collection for this tree.

One Stricklandia was about 6 inches long (Jim hills) has it) and Coflen got one nearly 8 inches long. This duration for gale.

"Port Daniel Continued and Mount Holyoke College. The last things collected were a fine Amphrycus, three Harania one of which showed to Hambard and there after one FORT LIG (collected by Mrs Dells), one Stricklandinia about seven inches long, two good Omythgra, and several small but perfect Strick- landinias. Palaerophus are seen in the lower nodular beds below the Stricklandinia zone, and at least one small one was seen in the upper part of the Stricklandinia zone. Clorinda is common in the lower part of the same zone, and Cope says now we Eupisyn nadiata and E.nigraeensis. I gave most of the forms collected to Mrs Dells, and together with her a fair representation of the coats. In the afternoon we collected on top of Red Point in the lower beds of the Red Point or the point Cristalreinus beds. But the usual run of things and upon the whole Mrs Dells has a fair collection. Dr Dells collected one large Rhynchonella Stricklandi, and most of a small Brontes. Cope also saw a Hlaenus ochus, and I a tail for a small Brontes with spines. Attached to Port Daniel with thanks shown."

"Port Daniel Centre, Friday, Aug. 2 1939 In the morning Dr. Wells took the four of us to Clemerville. First we went down the Little Port Daniel River over the transition mfs to La Vielle and all the trails are for once a few incisions. Then we went up to the river to the dam and the stand and saw miff to see La Vielle but got along our fins. It was then too late to go to the fruitful Clemerville with Hyattidine etc. In the afternoon Cohen and I went to Pointe L'Enfer to see the closed syncline, and then along the shore of One Binnis Cove across the Bonlaux series. Then to the last side of same area to see the fault bounded to E by the Cratalorinous As and the Bonleaux to the south crossing the steel here and striking along the shore to Hartingtons Cove. We then followed the fault line to Hartingtons Cove, looked at the Bmaranture filling and old valley here with Cratalorinous Herces up to N-faulting. Then walked back to our car left at L'Enfer group."

Port Daniel Centu, Aug. 3 - 1929 Collected all morning in the low part of the Indian Point ls on the land of Adam Graham. Before large Cheirurus showing all of the thoracic segments. A large Calymere and Adalmotus or ocean her besides two or three other thrilities. A large Zeppidula reminiding of S. Creymarencis in also here beside many kind of finch birds. Shipped the large box of fossils by freight. In the afternoon examined the bascum formation along the west side of Port Daniel Bay, up to the brachiod pod bed at the base of the Brouleaux at Adam Bebe's house. Said good-bye to Dr. Wells and his family and retired at 9:30 P.M. We have had three splendid days at our Port Daniel. Tomorrow morning are from to Pelee.

Perce, Quebec, Sunday August 4th - 1929 Stopping at The Havana near by Ernest Riard 3.50 p.m. day 21.00 a. night. This is the fourth Sunday out from New Haven and it is raining, he usual thing on all of them this year. Hovins are have breakfast at 8. and by 9 A.M. are away for Perce' others are arrive at 11.30. Corpus girl called to say good-bye and all the morning in the rain he has the blue-devils and finally I had to scold him and told him that if he kept on crying in the cabin among his scattering the church-going people, that he could go to the devil. He took it properly and straightened out but died down in his deck chair soon as he got pains - the loss of his sweet heart and the fame of the Professor. In the evening are best uprest again. We are get there from one we on the Macquarie rocks and appear to remain on them to ocean Anse du Cap. While cross- ing this region the thought came to me can this area be an old axis of sea separation running to the south the Lil and Olev, and to the north the Richmond and the Oler. If so the axis came into being after the Trenton series and before the Richmond. There will then be two sea ways in the St. Lawrence gorge - cline, (1) a northern or Salpe trough and (2) a southern Port- Daniel-Dalhousie-Jacquet River Trough. The Richmond then is restricted to the northern trough followed by the Olev, while the Lil, Held. and modified later Olev. is confined to the southern trough. This all is very much worth while looking into.

Perce, Quebec, Monday, August 5-1939 The day started in bright but soon became squally with light rains. It is cold and windy also. In the morning examined the rocks of Mt. Joli and around to Cap Cameron. itself was between marl and the Split Rock The Weld, dips about 70° N. and strikes N. 80° W. Further southmar the dip is 73° N. and he strike N. 60-70° W. The Mt. Joli formation consists of dark blue sh and hardulring-sandy beds from 2 to 10 mick's thick. Below the said exposure were some sandstones in beds 4-18" thick. About half way trans the Red are found two & gone, small nodules or small interformational jettles having join forms. Have are got Chyplimella Meta, Lepidodendralis, Oristella Spirifa flamellous, Phacops, etc. On one of the SS surfaces got Favosites effervescus and a branching Fan. At the very base a large branching Favosits with a Japhra-tis in commm. These forms show that the design is Welden-tayian. Then follows the Richmondion and all seem mistake pieces of an Illaeus. Captain called on Peter to the Perce Rock and got some Chitlany fossils. The Cape Cameron series has much of the lithology

"August 5th continued. Like Richmondian and maybe of the same formation. Saw out a trace of a print. The series consists of thin red clay that is separated by black shale and the whole is decidedly squeezed and rolled into one another. In the afternoon we went to Cape Jane and found the dip Tbd 50° N-E. and the strike N-65° W. Here occurs Taonurus, and also very small Lingula. On the Prieto road the "Ovis" like sandgels cross the road with a steep dip and a strike of N-70° W. It is too cold, windy and going to continue outdoors.

Perce', Quebec, August 6 1929, Tuesday Started our tope 8A.M. tr investigate the Priests road tr locate on Clarke's Map of 1917 the various geological formations, and tr take dips and strikes. Crossing the front - Tron au chat - one soon saw that all of Clarke's Hog is Ordovician like Perce' Rock. It stands very vertical = dip 75° S-E, strike N.85° W, and is cut by pink orthal. jdg mns near at right angles to the strike. Where the Ordovian comes to the Priests road the dip is 70° S.E. and strike N. 70° W. This strike leads into Tron au Chat puleh where the Ordovician is outcrop by the Bonarentine. The Ordovician or the road crosses a wide gneis. In the gutter saw a little fluctuated Ord. outcrop. Then follows the Bonarentine crop, about as Clarke has it, only it appears to be continuous with the Bonarentine of the Pic d'auron and in the criele. It appears to lie nearly horizontal, and mostly the pettles are of the Ordovician. At the Grand Coupe the Bonarentine trace of St. Anne comes down all the way to the stream. here crossing the road and even below. How the strata appear to be horizontal all the way to the top. At the mouth of this brook in the Richmondian and I judge it comes up all the crees, and is outcrop by the Bon- arentine and notes Clarke has it north a litt of the Heldetley in 2 morg; his notes should come up to enclose by the Bonar.

August 6 continued The first Richmond comes in to the N.E of the Coupe on the sharp rise of the road marked on map. Here the dip is 40° N. with the strike N.80° W. The Richmond then continues all the way N.W. to the school house and beyond, or where the mountain road unites with the Pickets road. Are all of these strata overturned? Further on the Richmond stands nearly vertical and has a strike of N.67°W. At north west of School the Richmond strikes N.70°W., but the dip may critical. At the Colmona bro. the dip is steeply to the S.W. In the afternoon studied the Richmond enters into Mountain Road. All in Bonaventure in place to the big bend north of the Lay Out. Here occurs the highest Richmond marked by Plestommites serieus. It outcrops down to grad forms the Amphitheater and before descending into it intersects the Rapnro- guina ledn - Catogyga anti criot'suei beds having a steep S-W dip and striking N.60° W. Cecil Kindle met us here and told us of another Richmondian exposure, or one near to it. It in the first gulch the stream of wh, at comes, the road to Irish Town. Here are collecting Halgaites, two others species Tarraites, Helidona Atropa majiscalis, any large Plestommites, Coscorus etc. We work so again and make a large collection.

Perce, Quebec, August 7, 1929. Wednesday Cecil Kindle called at 8 A.M. to show me his maps and found he had mapped the coast from Macguireau Point (We is about to take in Perce county.) to about Cape Cove. He has no farther than to map the beaches and does not want out the formations and accordingly cannot determine the structure. He says he has Silurian east of Chandler and over of Cape Cove. Until I see the finds tomorrow I do not know what he has. All in all I was not much impressed with his knowledge of the geology and as for the stratigraphy he knows, at all, on the basis of fossils his unreliable basis. I then explained to him what the formations are here about Perce. Explained to him my journal lists of the Richmondian, and then pointed out in the field the various formations. He then took me in hand up the hill overlooking the Grand Coupe and we then walked to the place where we yesterday saw the blue shells before meeting with the Richmondian. In these shells he got extra-erda and so are collected once. They are rare and scattered in the rock, and can be turned up this specious of Ambyx (ammonites) apparently like the one I got on the eastern side of Mt. Joli. Cecil Kindle traveled to Pied d'Aurore and when he returned said

August 7 entered that at the top the strata near vertical dipped seaward and inwards Malta, and that on the inner side of the Pie they dipped in the opposite direction. He brought back some crystalline ls that also had Ferustella, and these to me looked like Devonian jems = Crickley. Herd Middletons lumb at "The Haven". [19ab25] After lunch Cribben and I walked back to the Pie and he climbed to the top while I got up my half way. Here he saw about 50-75 feet of near vertical Crickley dipping into the earth, but on the land side were more in place. The upper part of the inner land side of the Pie is covered with the Bonaventure dipping at about 465° to the south. It is composed of blocks of the Crickly in all sizes up to ten feet across, a jiggedy-jiggedy mass accreted by lime. It is the material of an Crickley cliff dropped down a steep talus slope with the bedding of the slope of the hill down which the talus rolled. It is very nice that one gets an Cricklay print in this Bonaventure but I got some Leptrevelia flatellite, Chmites emplanata (small) and saw much of Ferustella and some Polygona, and no Odoranites tail. Grogal the top out of the Cricklay in place Cribben got Diaphorostoma, Odoranites tail and mrides, Leptrevelia flatellite, and other thmp. The strike of the Cricklay at the outer tops out of the Pie is N. 70° W, with the dip 65° E into Malta.

are then cross to the or the Crule Trom an cliff, here the Bonarenture fills an old valley with the Mt Joli making the western slope of the stream, while on the eastern side is highly more Mt Joli (weathered) overlain near the Bonarenture contact by the Oriolay, or Pierce formation. The Oriolay in the bottom of the gorge and beneath the water fall stands at N 60 W and strikes N. 60 W, on the cliff B E. The Mt Joli on the west side has the same strike, but here the beds have slumped and are creeing down the hill. In the Mt Joli (weathered) should see no fossils at all. But the bedding surfaces are marked by "facies" that are identical in character with those of Mt. Joli. The vertical Oriolay yielded Leptoraelis and is some where seen in the unconformable Bona- venture. Continuity to Tof Mt at canoe Bmaranture In an cliff from a page slope of same valley Bonarenture Oriolay Mt Joli lies weathered red strike N.60 W weathered red The Oriolay again definitely observed. This contact was not definitely established on the Mt. Joli age because in the absence of fossils. On have we seen elsewhere the Mt. Joli weathered red. Storms ac- ccepted on the terms of wind Joli and full on Borel

August 7 continued The tide was unusually low this morning and one could easily walk across the rocky bar uniting Mt Joli and Pierce Rock. Cooper made it as 150 feet across. To the E of Mt Joli he saw 135' more of the same Mt. Joli formation, that is all covered by high tide. To the Pierce Rock series must be added about 200-225' feet more distal aug. At low tide this morning Cooper collected some fossils in the "Dipterus" beds beside the Pierce cove. The strike is N.40 W., dip 55 S.E. This is at or near the strike of Mt Joli and Cape Barre beds. I think he has Spirifer eminens but appears to have fewer plications. These fossils are Helderbergian. The crasis are the same as occur at the base of the Joli series. asked and Cecil Kindle showed us a very large Stormotoma (about 7 or 8 inches lay) he collected in the Richmondian of the gorge visited yesterday. He also had Catagysa leadi from another locality than he one on the mountain road.

Perce, Quebec, August 8-1929, Thursday. Cecil Kindle called to show me what he called Lil- to omit urian forms from Little River East. All minute material and very poor in a limy shale. Nothing that served identify, and yet the abundance of mutilated ipoid and fiplicate hypra with anecce Odmanella suggested for me Ordovician than Lulian, and rather Middle Ord. than Upper Ordovician. There was also an abundance of crinoidal pieces. He says his "Lilurian" occurs between Chandler and Little River East. He has some material at Prince- ton. At nine A.M. we started for the Gulch at the base of the White Cliffs, inland from the roads and mouthing in the Bay at the west end of Lenfesty Cliffs. Here Richmond ls makes large talus slopes but the forms while not rare are next to impossible to get good material. The commoner fins is a very large Pleotammites. Due to remarks of this place made date of August 6, here occurs a very large Hormitoma, and what we get are all small. It is not clear where in the Ridge. there belonging, but on a guess I should say my Lophag. Capricorn. Then climbed down the mountain to the Richmon road and over on it to the second break to the crest of the Cap Blanc Lighthouse. Here to the east of the break and bridge the Pleo- tammites beds of the Mountain road outcrops, but a lot of forms and less are the Bryozoa.

August 8 Continued On the rise to the over of the broad and bridge there enters an infraformational cr/monite outcroping this appears to be the same as occurs in Logan Park and on the new road to the east of the Cap Blanc Lighthouse, the dips is nearly vertical and to strike N, 40 W. In the afternoon searched around the Cap Blanc Lighthouse but for no trace of forms. The new automobile road exposes an infraformational cr/monite like to me are our further north this morning, and probably the same as the Logan Park exposures. He then searched the Richmond strata to the west of Port Joli for forms, and here Corpen relocated the zone with Tretadon and Ambyx. He got a number of them and once collect more before one leave. See Aug ninth, Jem tried out and listen in collecting!

Perce, Quebec, August 9-1929, Friday Rest at The Haven on end of the morning. Walked along the sea front trying to solve the geological structure. Haven't found it out. It is plain that the Alpterus beds just carry the Perce away out into a fault of the Ont. Joli formation and seem initially so far or more hidden in the formation than my fault in the cliff facing Perce Road. Copper for some time here and down the gone from which they came; they are the youngest golf defined here at Low Oratu. (Low Mountain Perce Massif) It is also plain that the lower third of Cape Barre is of the Ont. Joli series and the very highest of this formation. I am not sure if it is then Taonurus but out of it Clarke got the third site with the fault folded planes. According all of the Ont. Joli beds can be seen on either side of the North Beach, i.e. at Cape Barre, the mount, and Mt. Joli. The strike crattles once or low due to squeezing of the beds into one another. certainly The upper two thirds of Cape Barre in the Perce formation = Upper Ordovician. The low dip of Cape Barre appears to me to be due to rising on the north the country which lies to the west of the Prior Road, towards the sea or Malta; the dip quickly steepens and seems nearly vertical. As one goes north

August 9, continued. appears to along the shore of Malta as the coast line cut across to Stride and at Cape Barre first cuts out the little of Mt. Joli formation, then all of the Oriskany, all of the Mt. Joli and at the stream of the Grand Couper is contact between the Mt. Joli and the Richmondian. In the afternoon climbed Mt. St. Anne and then to the Knitter. At the latter place a small brook falls over 100 feet of Comarantine conglomerate. In the morning Copan made at his stride in getting hundreds of Tetrapsis, some Ampyze, three other trilobites and a small Refinoguina. He is going to try to describe this fauna for me, or that I can use the information in my stratigraphic paper. The paleontology is to be his. The Tetrapsis stratum is about 140 feet beneath the Mt. Joli faunet contact. They are not common in a zone of about 5 feet but range about 20 feet down. It maybe how- ever that the actual range is much greater since we now know them at Mt. Pierce in several places.

7080 Perce, Quebec, August 10-1929. Saturday A middle called to show me a few more Richimmel fossils from another locality he said were in the lower beds. Had several Platystrophia, Otospha marginalis, Catazgya antiquiorans and other minute material. All poor material. Then Biard provided us with a tozand a new boat to take us to the Grand Coupee. A very quiet sea. As we rounded Cape Barne we see no evidence of the fault line here by Clarke separating the Barne beds from the Perce-Oriolany. There is here a sheer gone now nearly all fallen away, and it should be in the large Oriolany. Later, it occurred to me that the fault is laid some 500 yards or so more inland along its course. The face of the Three Testes maybe all Oriolany in very critical but highly crumpled thin-bedded material, = Perceuls. The low hill south of the Pic d'Aurore appears to be all sandstone in critical beds. At the top begins the Bonarenture descending to the north and filling an old valley. There s Pic d' Aurore ss sperric kens then must the basal, 200 yds or tar Sea level can split them Bonarenture 300-400yds. Mt. Hill = steel blue grime Grand Coupee Richmond red and pink About 1/3 mile north of Coupee stands red oreathing beds of interbedded gnes of sandstone or fine Congl, seldom seen-cracked shales and gnes of nodular kumps. It is in a cruddy tone. It stands from about 450 to near critical and all dips

August 10, 1929 continued. W.E trans Malta. They appear to unconformably overlie the Richmond. Towards the Coupe appears the Richmondian, which dips in reverse direction = inland towards the south and in this direction the Rich. becomes one and one third bedded ls. As the syncline is returned one descends into the Richmondian in accordance with Coupe. At the broad if te Coupe the Rich. dips stuff inland and it is from here up the brook that Corpen collected most of the Rich. forms. To the east of the brook along the shore of Malta, he at Tottel's Cyclorama and maybe a few other things. From the ls become very thin and most of the strata are shales of light grey etc. [314/18] The cliff just south of te Coupe brook has the result Joli shale with the same coals that seem early the fault n slip gone there the small bit of eras and add them to the list 1905 or 1906. Along Malta into Joli hills B14/19 Far the east, or about so far this occurs a coal breech of Ladoga with Turozites and the Bliths Nellen like cup coals. That led is about four feet thick. These last two gns lie to the N. of te Richmond, and on faulted the contact between the Rich. and the Joli seems here as was determined in 1906. Malta Still further E along come in crumpled thin redder sandstones, striking the N 70 W. Stuff great thickness and yields no fossils. Then interbedded with sl gns and loths differ from the typical Joli beds. ? There are few Pic d'Amu SS. of that area

"August 10, continued Faith E., at about beneath the Pic occurs a crane sometime of considerable thickness. See [illegible]. These SS strike N. 30 W. and dip from 45° to 60° S. and somewhat. All of them constitute what I call an arc rising to Peruano. He decided for awhile at the Three Sisters, where the beds are as usual very critical and troubling in dip and strike. I assume it is more [illegible] up to the cliffs gone at the north end of Cape Barre. The irregularity in deformation all along the Buraille saves me the impression that the structure is a closed syncline in more or less incompetent beds. Or this is an overthrust favour given here cutting out many folds just to Peruano Barre. Once around Cape Barre at low tide one can walk [illegible] all along this coast, but there is no way to getting here except by our boat, or coming from the north by walking. It will take many days to travel and surround the structure and determine the delimitations of the formations. The above interpretation is very different from Clarke's interpretation. I did not at once see the anticline under the Pic as he has it and the syncline to the north. Those structures as he has it are transverse to the actual structure which appears like a faulted or thrustled broken syncline or anticline. Which he cannot make out as yet. The whole Pic d'Amore is either parallel to Peruano ls, but as Clarke says, of they underlie them, then there must be a fault between Peruano Rock and Ant. Joli and the Coûte to the south of the Three Sisters. I am disposed to regard them as younger than the Peruano ls.

Perce, Quebec, Sunday August 11-1929 A dull Sunday with light rains, fast successione. Corfu and I went to lipomen in the Old Redstone Catholic church of Perce. The Church maybe the most beautiful in all Quebec outside of Quebec City. After dinner Corfu and I discussed the sequence here and than the profile structures. In regard to the latter are for certainty. The succession as far as it was follows: Bonaventure overlies a proto-Devonian graph tippography, and acrim are the formations here. Total thickness have been said up 200 of tub. Unconformable to our older archs. Late Devonian argyle. In 1930 I made two surfaces Middle Devonian old red sandstone @ Gray = Pic d'Aure Late Zorn Devonian Perce limestone In 1930 = 2 surfaces {Crisis} Devonian Pic d'Aure sandstone, shale and siltstone Cape Bare'ss and sh Ant. foli series - Heelutayian New Great, Or Silurian lie. Cape Blanc ls and sh = Richmondian Cape Canon ls and sh = ? Richmondian. If the last two formations are in succession the rid must be at least 100 of feet thick, but the formal sequence is not established. If the Cape Gygza beds are the older, than beneath them is a great thickness of shale. (In 1930 te Ogolmann has an older, thin blue sh, Cate siltstone)

Percé-Basque, Monday, August 12-1929 It rained hard all night and up to 8 A.M. Did not get started until 10 A.M. By 11 A.M. it began clearing and the afternoon was fine and sunny. I determined to see what Drin (fading) called the transition from the Basque ss into the Bonaventure, and what Clarke in 1908 in the days of Logan and Ellis now all called Basque ss. We first began to examine the e.g.l. at Belle Anse on the shore of Mulhag, a In the distance it appeared as if the Bonaverture overlapped the Basque ss. A close examination showed all to be confirmation and with decided meeting. Thus [illegible] [illegible] It was all a very erose pettle and broken e.g.l. (pieces rounded) with interlaced irregular grooves of crasse's or mudiness. Redip is outwardly towards Mulhag. Next we went out to Point St. Peter opposite Plateau Island and found the same kind of e.g.l. but interlaced with red meeting and decided even redder ss. There are more prevalents less than farther over at Belle Anse. Here again the dip is not around towards the south (must be stone) [illegible] After we had lunch (must be done) [illegible] caters 2 1/2 miles W) About one drove to Chien Blame, and then down to the shore of Basque Bay near the Church. Here the Basque ss dip 15°-20° S and E. Towards Red Head to the north we noticed a sharp flexure within in the dip but after all it amounts to little. Towards the south the dip steepens and before arriving at Whale Head appears a small

"August 12 continued" Twr decided syncline with the SS again running to the south this usual dip, then Further S the dip steepens to 60°E and the strike at N, and S in the same direction there soon appears a little fault but the throw is very small. This is about like this This dip from steepens to 20° to the S. Faults? The dip goes This is probably Goldring's fault, but it is not of importance. And the SS are decidedly arkosic and granite pebbles occur as large as one inch across on the surface of the bedding planes. The second point S of Red Head or the next one S of Chian Blanca is made of a truldu conglomer, 15-20 feet thick, and is confined able to be so far north. This truldu bed is like those of Point Point and Belle Ounce. The dip here is about 20°. Folding adds it to. To the S and E the shore is now very straight about 1/3 mile to Whole Head, made of the same kind of green SS where another conglomerate or more. little formation appears. The dips all along here is about 20°. I am now convinced that all the strata from Belle Ounce around Point Peter to Chian Blanca are Susquehannock Sandstones and Pailkypton material is not rare. The sandstones are an olive been green with thin beds of a finer makes thicker than have pebbles 1/2 naturally and SS. When these SS are red this coloring is due to oxid iron from above. The SS are often current rippled, and more or less firm bedded and sometimes decidedly dr. Some of the shale layers are much cracked and some SS surfaces other filling up into them. The conglomerate are cemented

August 12 continue and sand to the same green argillic sands and never to hematite, as in the Bonaventure. The ss on their surfaces include many small falls and small pebbles, and sometimes one sees clear overstream agate. evidence of growth in one direction; perhaps all is of the freshwatery side of a delta - activity of the geomorphology. Out of this engl we collected a poor shellfish (appears to be an Ostracod), and in another ls are small forms, not looks like a Pleistocene. forms. Many pebbles are of a bright-white crystalline ls, but most of the pieces are of a light grey ls, and some are crinoidal. Rarely some quartz paths and rarely a granite pebble. All found together by arkose a coarse quartz sand. The pebbles are nearly all well-rounded. This material could not have been rolled far. Creates the impres- sion that there was a delta from a mountain area formed out into at sea not far until, the present Bay de Chaleurs. Onkake did one see a true Bonaventure in which the current is a hematite, and all the pebbles and fragments attain and angularity to large sizes, seen in the Bonaventure. ocean in the Bonaventure After Belle Anne Crispen saw some jasper pebbles. Therefore The same sands sometimes have some red grains but these are more or brilliant red as in the Bonaventure. More of the red coloring of the lower ss relate to oxid work from above or due to weathering. from chim Blanche to Point St. Peter. All along one came up in the section, and where the ferric engl. comes in, Mind folding calls it Bonaventure, but unfortunately to see darkness under all these basse ss engl. Put up again at the Baker Hotel, but roomed in Captain on him my first trip down east clearly. Bakerham's Old Red Sandstone home, the same grand home I called A

August 12 Continued. Clarke in the 18th Rep. of the Directors of the State Mus. 1924 says this: "The critical region for the precise determination of the stratigraphy of the Basque sandstone, and the incoming stages of the Bonaventure formation, is the extremity of the St. Peter peninsula" (125). The Upper Basque sandstone in the St. Peter region "is gradually replaced by the Bonaventure sediment" (125). South and east of the faults near Chim Blance the green-pig Basque sandstone are followed by "at least four beds of conglomerate separated by by broad intervals of red to brown shales, the first of these, of lighter shale than the rest carrying plant remains of the same character as those in the Basque sandstone. The entire series on this north shore is terminated at St Peter point by a very heavy bed of conglomerate which is continued out ward to Plats island" (129). Clarke caps me and concludes that these congls. are all of the Bonaventure being the transition to the true Bonaventures. To me all of those congls. are but beds in the Basque ss and that they have nothing at all to do with the Bonaventures. The "Bonaventures" to the N. of Grand Crique shore and that under the Richmond area are not Bonaventures, but some part of the Basque ss. The B. j. St. Anne and the Pic is true Bonaventure and so would that of Bonaventure Island. The "Bonaventures" on the top of the Beaumenne cliffs is also not true B, but a part of the Basque series. In other words the Basque ss becomes more and more congls. and red towards the top of the series.

Gaspe, Quebec Tuesday, August 13, 1929. Paid a short visit to the locality and my Gaspe at twelve miles gaily from Kirkay Jones in the Gaspe ss. Sota fur good fons. Shortly after lunch jacked up and we started on our Ford for Grand Soree. It was nearly 1:30 P.M. when we left Gaspe and headed around the peninsula of the Quorn with a valley and finally across the river to the Forillon. This is 8 miles N.W. of Gaspe. It was about 15 miles away east to Grand Soree over very bad road full of holes and steep bumps hills. Copper had to exercise all his ingenuity to get the car to Grand Soree when we arrived at 3:45 P.M. We are stopping at Joe & Dave's home who re- gularly take in guests. At 4:30 P.M. we started up the King's road to see the St. Albans Cliffs. They looked as if old - grand, hip and white.

Grand Greere, Wednesday Aug 14-1959 At 7:45 we are off on foot for the St. Albans side of Cape Rain Core. Worked until 3 P.M., gathering Diom Weldbury fruits. But a few lot of them quite rarity in all part nor all the fruit good, A. galatea and cores are most common in Logans Div. 1. This division is the A. galatea cores and stimatophorics recalls the W.Y. Crepmous. Div. 2 is mostly shale and has a great variety of fruits but when one has a good feel of material that is off the edge to look on. The upper part of Div. 2 has red beds as noted by Logan. A group collects like Corpen working here several days could profit enrich the St. Albans fauna of Clarke. Returning to Grand Greere we collected a meager fauna in eminical ls along the fair rise out of the Rain Flat. What looks like Dictnella pseudo galatea occurs here with other species. The fauna is very small. It is in Logans Div. 3. fm which Clarke enters no fruits. The morning was bright but by 9:30 a fog covered from the sea and grew thicker all day.

[see doc. 90] Grand Mere, Thursday Aug 15-1929 [D9607] Collected all morning in a little quarry beside the road side after hundred feet east of the bare homes. It is in division 2 of Charles Grand Mere formation. Got a lot of things but all is fragmentary. As usual Coprinus for most of the fossils. [D9518] In the afternoon collected in Oltell Brook and in the arable lands to the east, in the upper ls of Charles division n°1. It is the regular Ordinary (Upper) fauna though hard to collect because of the thick reddish nature of the limestones. Saw one Eatonina eminens and all the species are as large as in N.Y. Arsenals in this limestone. If more oil lay upon the ls there would be more silicification, but the soil or is not stay moldses dipping 30 degrees or more. The strata dips north into Boston Bay but as one turns Oltell Brook. Another day I fog for till or three except today until in the afternoon.

Grand Prere, Friday, Aug. 16-1929 Started on my car for Shiphead and Cape dorpe. Copper started a little on the road and tore down this section of a rail fence, but otherwise we had no more bad luck. The road got so narrow that we finally crawled the last mile of the farm to the end of Gorpe Land. [3708] In the brook between the two mountains one gets fine things and a great lot of Plectrocyclus pleisphorus, some of which are very good whole ones. These are fine to about the same striking horizon as in Ooliel Brook. On the way back looked about in Indian Cove and would have gotten nothing if a local fisher man had not given one for a dollar six tails of Dolomanites. This man is Mr. Wilson Roberts and I told him I would try to get him to call out more. When I gave him the dollars he said it was as much as the value of his whole creek fishing. Poor man! Back to the care home at 3 P.M. I am tired and tried out to make a success of collecting fossils. Copper has two boxes of fossils to ship.

Grand Greve, Saturday Aug. 17- 1929 [19608] Spent the morning at the shore of Little Basse about 1/2 miles north of Grand Greve. Here occurs the hardest ls of the Basse series and they strike along the shore east for about 1/3 mile with the same 20 feet of strata. Man fork fels is too hard to handle but above it weathers it heats up into an irregular bedding showing many kinds of joints, all of which remain unexploited. The fauna remains most of the Boshani sort with a few Ordovician holdovers. It is most a backis- pred fauna in which one sees not a trace of cephalopods and only some Tetraconuls. The contact of the Basse ss with the ls is shown to within three feet of me an other. It appears to be a sharp contact and there certainly is no transition zone. Evidently there was a hard here, emergence of the sea bottom to land followed by a long time of delta submergence. The sandstone is distinctly fine set through Basse Bay; is fine grained and without coarse emp. Of the ss one sees not a few tens of feet and then a long reach over to the Basse ss continuation up the bay to Basse and far around. Stayed all afternoon at the Greve home reading the novel Madame X, a good story with a fine moral. It raised some.

Grand Breere, Sunday Aug. 18-1929. A cloudy morning until the sun heading through by nine A.M. Evidently it is not going to rain this Sunday, the first one while in Canada. Coffin purchased of Mrs. Joseph Bore two rag rugs, one a beauty with a rose and elma leaf design for six dollars. I purchased three small ones, one a three-star design made by Mrs. Daniel Bore, a sister of Mrs. Joseph Bore. The first cost $6.50. At 1.15 P.M., we started on our return trip and got to the Balers Hotel at Sappe at 3.45 P.M., considering the very poor road from Grand Breere to Quebec Balereville or quite to this was dry fair week. In the evening called on Frederick Richmond, the local erleeth and philosopher. He knows much about the oil well country of the year River, and from his account that should be discovered here coming wells. To Monday we start back to Sappe, but first to help out Christmas in the Metapedia Valley.

New Richmond, Monday Aug. 19, 1929. A splendid bright morning and we leave for the Bakers Hotel west by 8.15 A.M. We have many views of the Fossil on all the way from Conflantown East to about Blanche Chien. Just after leaving St Peter Point we have the first clear view of the Peace Ranges so far seen. To see them here to advantage one must do so before 10 A.M. in the early morn- ing sun since after ten o'clock they are in shadow, in the sun all the rock forms show in relief and other is more beau- tiful in the flood red colors of the top of St. Anne, the Pic d'Anne and the Sable ss to the north of the Grand Croupe Brook. To the north of the Pic are the green tops of the Out Joli, and ls than the front, followed by the peaks of New Richmond. Further north are the two flood red faces of the great vertical Dorman that Clout calls 'the dawn theme Bonaventure'. Then more gen- eral rock exposures (are those Rich?) followed by a long wooded area when once flood red and green cliffs appear sharply to the corner. The latter are some of the Sable ss. What an interesting lot of geology could be worked out here in de- tail by a young man with enthusiasm and the necessary time. [In 1930 I found this coast easy to interpret.] more Northward of Belle Cause are again great down to the shore to see the so-called Bonaventure transition of Gilding

August 19-1929 continued. In 1930 we saw that there are austral Bonaventure Here the Barke cnyl. are practically horizontal, mostly CNYL. on the gentle inner low angular and could be called a brecia. The sandstones that are tinted did are irregular in deposition, and have much caliche-like gives the equivalent of what we saw to the north of the Grand Coupee along Calvary that is called the circular beds also having some Venetian. Have a piece of the caliche, a red ss piece and a cnyl example. These types of strata continue NW to Barachois and traverse the railroad bridge over the creek. Farther NW along to Boileraud one sees lots of the regulating barke SS, green and red marls, and some cnyl. grss. Have four samples taken in front of the Post Office of Barachois Parish. As that is here no other kind of Bona- venture and as these cnyl. fan into barke ss here as on the castom side of St. Peter peninsula, it is clear that all of these strata are nothing other than the lighter Barke SS series. The fault folding indicates we did not see, but small meccyffe present in the area or t'harred by us. On to Boileraud 3-4 miles (north) of the Carre we saw Richmond ls very crystalline and with my smacoclite. It had no lons but clear felsp in the Richmond series. [This is the splitting middle kind if or tel. mmpy from cnyl carr. 1938] At about noon are stopped at Miss Couture Trading house at Cape Core to see young Cecil Kindle. Here we also had lunch.

Aug 19 - continued Since we left our Kindle de explodé down to Grand Coupe Brook, from the Priets road down to the north some distance occurs the Bornaventure. Then came Hue d'Als like to one he should see on the road having extra rods and emptyy. In those of he again found emptyy. Then came to a series with good free forms none which did see, but he said he had six capal rods. In this series of it he saw clear a syncline. Can this then be the bottom of the syncline all along the Ouraillès and Pic? To me it seems to be or because along the shore outside there is are the blue green of and granite which not the flood any green red Barke ss. Those some Barke ss red and green are again seen in vertical cliffs from the Corner on the beach. Regular vertical but dip towards Malta.

Aug 19, continued. on the mountain road, where the dip is towards the O.W. This agrees with the faunal evidence. Hindle has explored much along the banks to the north of White Dot, and here he has turned three places with Cataggyga antiquatissima. Only a shale series here and says several small arches are shown. This seems to indicate that the area between the Priests Road and the Cape Blanc exposures is a sort of anti-climorium trying as the Richmond in the same sequence as in both Isle-Cape Cannon. After lunch Hindle, Corbin and I went to the north of Little River Ear to see his so-called Silurian. Here on the east side of the stream is a point exposing nicely a lot of nearly vertical shales that dips inland. They are sandy slates, banded SS and sandy shell limestones all in very thin beds. Our finds are few even excepting in the shell limestones and here if often the calcareous matter has been leached out leaving behind an ochreous reticulation. Orinidial stromatones are frequent (all very small) and tiny hackis forbesi, Dalmarella is common. Also fragments of little a small Rhynchonella or ? Elyaspiria. Darne my small Plectambonites, Rictoliate hydra and several non-identified brachiopods. The whole place are future impression, namely middle Ordovician and probably Northrops Trenton series.

Aug. 15, continued. We then went to the first stream west of Little Brin East, about 2 or 3 miles, and east of Grand Brin Village. It is the place from the train four years ago. It is the southern point along the sea shore and almost beneath the railroad trestle. The strata stand nearly vertical but dip slightly inland and are far more muddy slate than those of Little Brin E., and devoid of fossil beds. Now out a trace of a trail. At this place these strata show far more meta- morphism than at the Port Joli and the Dileuvian. Hinde says they have been mapped as Devonian. To me these this place must be referred to the Ordovician, and clearly older than the Richmond. If this is true then the Taemic orogeny made a new geanticline extending from Port Macquarane to about Cape Core. To the northeast of these are lie the Richmond and the Devonian, while to the southwest is the Dileuvian- and Lower Devonian district of the Barfoss. The Ord., sil. with kimberls and some the axis probably have the whole Louis. Dilly ser., (=Macquarane) and the Thetron, while the sw. tips lay above the Dogranolite (=Tateysmoke slate). Sht to the Bay View Inn at New Richmond at 6.20 P.M. We came to day from Gospe a distance of 150 miles.

Causapscal, Quebec, August 20 - 1929 We left New Richmond at 8.15 O., M., in a faultless cold morning. It cold last night that doors closed tight. Left to Metapedie at noon and had lunch due. Gick-ory telephoned yesterday for us to go on to the place where he is stopping at the Bellvue Hotel. We arrived at 2.15 O., M., but Gickmay was not on duty for the day, took rooms and will see him when he gets in. West of Carlton shoreward of the mountain is a high ridge over which the Boulder and farms. Here we sees flood red emyl, stand-onnealon ridge, and because of their attitude they must be if the Devonian Baske ss series. To the north again is a low crest. These rocks are probably not Bonarentine and then maybe no B, west of Carlton. The slope to from Devonian ss with inter bedded emyl, grass occur about 30 miles over of terrain to Gun Point, This is further nor than he Deer, to the west of Campbelltn. West of the Park Daniel folds all in low country until one comes to the Silurian lara ridge of Black Cape, Brown from miles aside. Between all a low land from New Richmond across Cossia- pedia Bay, each of which for about Maria towards the west are the high grass mountains, striking north past of Nouvelle and Eccuminiae, and other manes south of Dalhousie and Camp-telltn on the other side of the Restigouche Bay. These is from

"August 30, Continued muses out the Devonian and have partly deformed them more than. Several miles before getting to Matapeedia one sees much of the highly cleared dark blue l's and sh of the Mataford; a formation that we may know as Trenton age. They are well shown all around Matapeedia and we see them on the roadside at intervals for about 7 miles north. Everywhere the schist is very vertical but the bedding is at all angles from place to place. At Matapeedia and in about 40 miles of the stream the valley is narrow and the land rugged, but north to Causapscal it opens out widely and the country is low with rounded hills. At 12 miles up the Matafordia at the mouth of the Cusumet- quasam coming in from the east are fine exposures of the Orick- crag ss series or Crick may tells one. Walked around the village and came upon The Catholic Church built of l's in 1910. In the floors I saw an abundance of marine flora: istina, Orthids, Rhynchonella, Delthyra, Strophomella like goni- culata, Brachiopim? Plectammites & small Tetramoralls, Fa- vorites 2 sp., Stomatopora, hemispheric bryozoa, Platyceras and other trip. This is a Devonian combination before unlike any that I know. It appears to be well up in the Devonian. Where did this l's come from? Crick may had not looked at this church and so knew nothing of them then. Later I learn that it comes from near the south end of Matapeedia Lake, at Cal Brilliant."}

Causapsocal, Quebec, Wednesday Aug 21-29 Last night Crickmay showed me some fossils out of the Matapedia formation on the farm near the bridge on the Matapedia river near Causapsocal, as I thought I saw a small Alcyta marginalis and as this fauna is very different from the one found on July 29 on the Resti broche, I decided to walk back to Matapedia. Arrived there at noon and remained collected here for four hours. The crystalline hills are very limited and we got nothing more than Crickmay haul. Corkran found one of the detatable shells The Matapedia formation goes up the river for 70 or 80 miles when fine grained muds ss appear and it then continues along with sandy sh to within 7 miles of Causapsocal. We found our fossils in place, no has Crickmay but in a small boring pit in a very weak shale at the side of the road, or for a large Diamonites tail and an abundance of Lep. Helellites, etc. In a large quarry in the ss at about 6 miles south of Causapsocal Corkran found a loose orthocerid shell with a large Spirifer having the fold and suture visible. These fossils show that the ss-sh series is Devonian. If there is no repetition or faulting Crickmay says the series is about 14,000 feet thick. This is unbelievable.

Anthy the ss comes in a phyllite that occations fossile, but it rules no fossils. It is about one mile across. At about 6 miles S of Caucapecal Lan comes in a sandstone over that for north of Caucapecal. In the railway cut to the north of the sta- tion there has yielded Leftocerids flactellits and a large Chonetes, muren len diti melmicea = Oriskany time. Crudely most of the land between Onatekedia and Caucapecal is covered with Baspe ss and sh, but this first summary is as yet not proven excepting around Caucapecal. (This ss stands nearly vertical, in heavy beds, a coarse aridmic ss often rippled and dim cracked. It weathers to a dull red brown.)

"Causapscal, Thursday, August 22 - 1929 At 8 A.M. went about 1/2 mile S and then as much E up a steep rise. Due dark blue lining of are exposed and schistose as usual followed by the road and within 55, Dr. took got about ten species of what look to me like real Oristany. But Chacks Rennelacria n.A. (up to one inch long), Chmits like onelmica, dif- frent lines of Spirifus and the Anchisrevinus sort. Saw my Lep. flabellites but hardly L. emeara, nor any regular Oristany species. These ol may be terminal Heldburian. Then tried the large road side exposures about one mile south of Causapscal, but found it too dirty to see fossils. Colled for one flab Chmites. Then looked at the R.R. cut in ss to the north of the station and a layan me about 1/3 mile north of the former. Saw my fossils, but Crict may got in the first cut one Leptocrelia flabellites and two Chmits like onelmica. Time Oristany. In the afternoon visited H. to Angui on the Boulevard and then crossed the Matapedia and came S. along the north side. Ex- aminial a number of outcrops and at four places got either Lep, flabellites, Crelopina emeara, or Chmits like onelmica but flat. All is though Lower Devonian and as far as the fossils show all is upper Low. Dev. As far we see no fossil evidence of the Silurian.

Sagabec, Quebec, Friday, August 23-1929. One mile N. of Angui in a railroad cut occur sand ls dipping 60° N. Here one pt Leptrocoelia flabelloidea saw one Ordovay like Spirifer and ? Ontrocelia. We are therefore still in the Ordovay. Then fn at mt 5½ miles N. we saw no road outcrop, but at 2½ miles S of Val Brilliant we came upon a little ex-posure beside the road thus furnished Tenostella, Pleurodic-tium, tiny land plants and some obscure fossils. Bring down on the railroad we found a dull red cut with the Shista rational. These are said to be in a syncline and as far as could see one ate to last high out of the Shieldrock Range before we came on the flat land undulating by the very horizontal Silurian white quartzites. In the railroad cut we found a light pink arenaceous-pyrites ls having scatering fossils. Of this layer are two orocrenulate. It had Lep, Rhomtridals, Ametricularis, a small Chuchuckstella, orthids, Phynochonella, an Ordovay like Spir-ifer and other brachiopods. Also a Dentistypa that reminds one of the Devonian. It is a fauna unlike any known collages-gets younger than Lower Dev. a possibly early Med.Dev. Less than one mile N. of Val Brilliant, or a little N. of where the auto road crosses the railway in in the fields to the west of the R.R. occur white quartzites smetels of which are lining and have an abundance of Pentamerus flonguos, Shield-

August 23, continued Londinia, Otius or Omomorella, Palaeocyclos, Steph- telasma, Farrita, and quite a number of other forms. The bay is clear Clinton. The hills are seen on the lake shore about four miles south of Sagatec and they are replete with fossils here and there of Corals and Lingula some feet thick. It will be difficult to collect this material. The dip of these strata is inland at 5 degrees. About 13/4 miles south of the Catholic Church of Sagatec, the Boulder creek crosses a small stream flowing into the Lake Matapedia. Here the dip is also inland or W about 15°. Sagateck, Saturday August 24-1934 It rained all night and kept it up lightly all today. We staid at the Hotel (Hotel Sagatec @ $3.00 pr day) all the morning but in the afternoon one sawk north Toronto River. The dip does to the E of the road has much loose white quartzite lying upon it but the rocks are all of the "Cambrian" = Quebec-Lilly series. One crawls about 3 miles and then E to the P R, but all is "Cambrian". This range of hills continues down the east side of Lake Matapedia and to the south. Alcote has recently described an erasing Ord. series with volcanics. At some time these formations must have been related to the Silurian rising here at other angles than

August 24, continued. 5 to 70 degrees Pazatec lies about one mile to the north of Lake Mataedia and is a flat land not much elevated above the lake. It is all undulating by the Diluvian ls lying at low angles, mostly averaging five degrees. He then crossed south of the Catholic church of Ja- goteed about 3 miles and collected in the Diluvian l's quarries here for the Catholic churches. About ten feet is exposed, a dark blue, sandy, friable and banded ls, this may lie very near the white quartzite. He got about all the sections seen in the walls of the Causapsical church. The church at Angqui is partly of the quartzite and the other of Val Brilliante and Pazatec all of the Diluvian l's. If we are ever able to learn what relation the Dil. bears structurally to the Ortho Camen Onts, maybe they join underneath the Devonian? Nor have we learned the thickness of the Dil. other than that the quartzite is said to be 60' thick. In the quarry are seen or trace a Heldutepian fauna: thus Bailey reported Shifter-denta varistriata, O. tecki ? and Peristella. We have not yet seen the quarries in the ls situated by the Intercolonial R.R., unless they be the ones seen to day (Bailey says 6 miles N of Val Brilliante which would at once make it other one or here today).

Sagabeck, Sunday, August 25 1929 A fine bright day and we are off at 8.30 A.M. At about 1 1/2 miles N. of Val Brilliant one comes to fields to the shore of Lake Oraphedria. Here the Lulurian quartzites are exposed dipping at about 10° N.W. About 1/2 mile N. of Val Brilliant [illegible] beds changed to N 57° E, but farther S again over as usual N.W. We traced it all the way to in front of the saw mill and the R.R. station. Saw no fossils, rarest nippled bit in one place cross- budded bit near gravel of or. Toronto, the S the plain over main course. South of Val Brilliant one could discern no further on the lake shore, extends, but 1/2 miles south one could look across to the shore of an island during Albert's highland series (an adnate emph.). In all this distance the Lulurian is not fully involved in the fields of the Orthodome Outcrops that stand high to the SW of Val Brid. South of Val Brilliant about 1 1/2 mile we trot a W road up toward the Old P. out, and soon on the south side of road one came upon the Lul. quartzite dipping at about 85° N.E., Here the Lil. is clearly involved in the fields. A little farther W on same road in a tract to study dipping flyschmuds rocks (ls) furnished a few small fossils among which is an Ordo- aria suggesting Devonian here. There must be a fault has angry side at least 600 feet thick across the whole Lulurian. We then returned to Val Brilliant for dinner (Chateau F.B.) and later went N. to a masters gray sand and after a time came upon a ls conglomerate along the road. It dips 15° N.W. and in 2 1/5 sands across to another gray a thickness of about

August 25 continued 100 p.m. All of the pettles appear to be of the Diluvian and many have Diluvian forms of the species are collected in the quarries today. There are also other Dil. Species like Con-chidium Knighti, Favosites, Stomatopora, and cup ends and some back spores occur free but form as pettles in the cups. The foot of the Cnyl, is full of comminuted fossils some fire to impressions to be of the same species as in the Dil. pettles. Above a sandy soil is interbedded and other Favosites and small back spores. At another place there is a shale Receia is reflected with some Diluvian fossils. The pettles, [illegible] aunts to Cnyl. upto 6 metres deep all of which have the conus rounded. This ls Cnyl gives me the impression that it lies on top of the Diluvian series and makes the base of the Permian sequence (in Aug. 26 - was found to be an error). At the base of the Notre Dame Cut and other the Dilurian Harland deposits appear are from a little exposure in the road cutting and have Jpor [illegible]. Other 20 feet Cawn Crick may also for the caprolites and a small Dalmanella Nuculifera and a peculiar Lep. rhomboidal. These beds are clearest beneath the Ls Cnyl. These strata dip at about 12°. Still nearer the Cut in a road cutting and in the fields are found these same strata dipping at NW 45° W. For several days Amorgaptes while Conus and Crick may get a small lot of back spores. Near there we found the strata rising

August 25 - continued with an arch that farther south must be faulted with the Devonian farther south. The Silurian then lies unconformably on the various members of the Ordovician. It begins with the white and fine quartzites that are frondiforous toward the top, and about 60 feet thick. Then follows the ls that are terminated by the grapholite sandstone sk. How thick the Silurian above the quartzites in one could not determine but may exceed 100 feet. Then follows the ls caye, apparently introducing the Devonian, but as yet we do not know if the Heldeu- terian is present, but I rather think we may find it somewhere on Aug 26 - other the conclusion was found in me). I rather expect the Silurian to pinch out toward the south. It is not known at our Oratophelia and how far over the Por Daniel - Black Cape series are in my column. There is perhaps a land barrier between them. The Helderian if present goes across the entire person. Give since it is once developed to the early Orato- pedia. {all @ Devonian and / my Barless} The Lower Devonian is the dominant formation of the Oratophelia really, but how much of the Barke SS is pre- sent was yet unknown. I had a very successful day.

Sagatech, Monday August 26 1939 It began raining hard at 7 A.M. and the day looked lost, fully 8 o'clock it cleared up so that the day promised to have of showers, but it rained on us no more. We started south at 9 A.M. We first examined a little cut on the R.R. about 1 3/4 miles south of Pal Brilliant and found the same fossils are present in the layers cut 3/4 mile further south. The few fossils are better here and especially the hygroza but the species are the same. Shale stand at a high angle and dip N. At the south end is a fault apparently a small one like this. We then studied the big cut 2 1/2 miles S of Pal Brilliant. At the south end are thin and thick bedded ss with some sandy sh, all are much folded and obscured. To the N follow a long series of cleared sh and then come to cross bedded series of lining ss with an occasional arenaceous ls carrying the fossils. All of the beds are obscured and faulted, but I do not think much is cut out at one place. It looks more like accommodation movement on a syncline. The whole is done limit since here is no repetition of the beds. After lunch, at Pal Brilliant, we went south to the road up towards Arthur's Quarrel Cut and once came to the first Silurian quartzite seen yesterday are surveyed to begin and since the Devonian ls come into the N when Old.

August 26 continued should be exposed, it is plain that a major fault occurs between the two nearby places llying down the southern jar so that the Lil. Der. comes to lie against the fossil Lileuvian. As we were sorting into Les Enyl. and the Heldutug series with our prospect if it exposed anyther der, one autred to the Les enyl. locality found geo-terdes. While I looked for fossils in the enyl. Brickmay and Cion sorted around to see if they could find young or older beds. Young ones have all been recorded away while form was could not be seen. However they found a loose block with Ornograptus that had the lithology of the un-terfied der lies as found in places in the enyl., and so they tried to find graptolites in the rock in the place. And to Brickmay for some good ones. According to Les Enyl. is Lileuvian, and instead of it being one continuous bed of enyl. it is probably a series of enyl. gree, in a slaty series of sandstones having Ornograptus. There are at least 3 species of Ormo. and one dictyomena According there is no probability of finding in the area what lies on tops of this enyl. grees. Probably some-what faulting to our side Brickmay may find em-tact between the Lil. and Der. I now think that it is no Heldutug because much most of Oratapecia.

August 26 continued. I said good-bye to Gridley and Colput took him in his car until he front are collected back to Causapscal. I told him that now he had the quarry fairly well in hand, but much remains to be done in working out the fold and fault structure. At the cairn he has a well developed Heldebergian that appears to pinch out to the west and south in the first 20 miles N of Oratopedia. At the north end there is a fine Silurian sequence and it probably will not be found south of Dal Billiawr. Part of the Oratopedia Valley is occupied by the Ordovician and only it appears to be Lower Ordovician that some of the Sarbeos maybe included but all is marine uptr and including the Johnskarie grit. Beneath all is the Middle Ordovician Oratopedia series of Trentm age. The old ls quarry operated by the Intercolonial R.R. appears to be one N of Dal Billiawr about three miles where the auto road crosses the railway. They get out culvert and other great stone, not ballast material. The R.R. operates a much larger quarry in red sandstone (called Red Quarry) from miles S. of Causap-scal.

Bie, Quebec, Tuesday, Aug. 27-1924 More or less a dark day and we left Sagatec at 8 A.M. No dust today but hared smoke last night. On the road side about 5 miles NW of Onoise we looked at a ls engl like those of Bie, Its associated with the greenish greg quartzite. Dip 45 S. Blocks up to 3 feet across. A sand matrix. Passed Rimouski at 10:15 and got to Bie at 10:45 A.M. Put up at Canada Hotel. Spent the rest of the day studying the ls engl between Bie Village and the sea shore to the east of the estuary and the island during the afternoon group. These ls engls are in the dark blue sh series of the Loris-Lillery formation. They are here associated with a light greenish to white coarse quartzite that is more or less engl. with cream quartz pebbles. The matrix of the engl and the vitutddu [illegible] 90 are a very coarse greenish ss reptile with quartz pebbles usually less than 1/2 inch across and up to 2 inches. Of ls there are three kinds, most common is a dove colored brittle one and another like Lacdaese but miltar the Physisis - an arenaceous one without coarse sand grains, and the Glenellas piece. The quartzites are variable, but all appear true of the associated quartzite (= and remind of the Laysonges and engls, are informative). Large pieces of feldspar occur and we saw six green boulders up to one foot across. Corbin collected samples of all the kinds of pebbles seen. Large mano

August 29 continued If traps also occur and some are amygdaloidal, they may rein-quartz pebbles, and the feldspar pieces give the matrix an alkaline nature, but there is not enough feldspar to call it an alkali. The strata engl at the sea shore has blocks up to 8 feet across, but the vast majority of pieces are under six inches, and all are more or less out-rounded to rounded. The other rocks inland are often of smaller and more angular pieces. Even the quartz grits have more or less of this piece. The quartzites and conglomerates are mixed together. The Bric engl are regular strata engl, giving the majority of the loose pieces by the sea grinding against each other in what was formerly Lower Cambrian. Whether age of the former is in com- monly determined since the reef fossils collected are of Tedd C. The strata came off from a granite country bringing in much sand and rein-quartz pebbles, some feldspar and rarely a handful of grains. The shore rocks were cut by dikes or bad flows of trap. It would seem that the main mass of loose pieces are of the upper C or the Orgeonian, but if so it is curious that none have fossils. Probably most are of intraformational origin. The outer Bric engl goes in a broken anticline but near- thelands to the thickest area. The inner engl. goes are many ways from a few feet thick to may feet thick. Most have associated quartz grits layers varying in thickness about either the engl. All are interbedded with soft slate that can be cut not easily leaving the hard ones sticking up as difficult parts and producing the extraordinarily

August 27 continued shore shore of Bie. From the size of the out to the W of Bic the quartzites and engl are here in perfect form and one wonders how all that could have been gotten from cliffs. Probably 1/3 of the engl samples another third is of the intraformational broken quartzites, and the remainder is sand and rock quantity. Then there some of the sand in the quartzite zones. Even though these engl are found yet here at Bic they occupy the shore for a length yet least ten miles. The many ridges may be repetitions of narrow zones. But a great list of fossils from Lower Cambrian pieces some of which were 8 to 12 inches across. Could there have been a great tidal bore in this period dis tearing down and distributing far and wide the land derived material. Quebec City, August 28-1959 A cold raw windy morning. Started out before 8 A.M. south of Bic to see if we could find mac? Lemaire points near the Creamery found ten years ago. Failed to find a trace of any granition. Then monitored two miles more to the S, but all we saw were slates that might once have been the Lewis-Dalley series, dark, green and red sh with bands and this else, lie from way on the quartzite underlying date of August 29-1929. At 10.30 we started for Lewis. Had a puncture both tires at 6.30 P.M. Put up at Orleans Hotel at Lewis.

Quebec City, Thursday Aug 29-1929. After supper last night we crossed over to Quebec City for some sight seeing. Spent all the morning around Quebec looking at the city and the rocks. After lunch went via the electric train to Montmorenci Falls. We saw the downtown trains, Is and ok to the S of the Gichenan grein, and above the falls the contact of the Trenton on the Chicohan. The extent of the Chicohan is very ample with irregularities up to 10 feet seen at the falls and the woods to the north to the road to Beaufore. The Trenton Is clearly clean on the Chicohan with the fur dollars filled with disordered Holendronas (up to 10" across). Some of the Holendronas are lying directly in the grein (I have a harel with two of them and one was attached to the grein - the whole piece I have lay directly in the grein separately from some from me-light met if lying mud. The other heels also lay directly on the grein. Many Trenton fins could be collected, but we still no ham-mers with us. Coppen was glad to see this famous old place made or by Logan and others. So back to the hotel at 5 P.M. Coppen wanted to take his car to the Garage for repairs and tube mending.

August 29 continued. Bros on the Bio. Yesterday in motor way from Bie one saw that the quartz ridges are continuous for 5 miles to the north of Bio and for about 23 miles to the east, farther east if present one can more from Rimouski to near Bio. These quartzite ridges are again continuous to the north Rivere du Loup and start all the way to within 20 miles of Levi's when they die down to far less significance. These quartzite ridges are all close to the present shore line and form large long islands out in the Gulf. They are associated with the green and red slates and the whole are in the lower part of the Silley-Lanym series, the base of the "Cambro- Ordovician". Order of Boletto Zonu Cambrian fossils came from these localities hinging with Bio and going west to St-Fatim and St. Limeron. All are very plentiful in the crests of the Cambro-Ordovician. He also got some on the island of Orleans near Quebec, and one of the Levi's crests also furnishes them. It is curious that these Bio ls engl. furnishes no fossils with the Ordovician fauna like those in the crests at Levi's. Does this mean that those deposits were not present or far closer as Bio? This matter should all be looked into in the Canadian reports (but very little work written), but more or if Copin could find a summer collecting on the Lewis -Silley series from Levi to Cape Rosier.

"Quebec City, Friday August 30 - 1929 Started out at 6:30 o'clock from an all day study of the Lapis conglomerate about to St. Joseph cemetery. First closely examined the large mass 60' along strike and 45 feet the other way. To one this mass may appear as a reef boss much larger in altitude to a long ls. It originally had an irregular surface, firstly a cauliflower like growth and maybe layers of talc or gypsum. In the hollows and finally over it lies a ls cusp. In a sandy paste that is replete with rounded large sand grains (cornithlum sand). One easily assumes that the whole ls is replete with rounded sand grain but an examination onto a close shows that weathering produces an angular or crystalline sandy like surface that is all celecite. Accordingly one is easily misled that weathering may be cephalopods makes them appear to lie in a sandy matrix. They are all in the reef ls without sand grains. The original nature of the reef ls has largely destroyed the joints and they are bombshells by weathering. In the sandy ls forms are much rarer. We have taken samples of the various kinds of ls and sands, along with some fossils other will help to explain the make up of the reef ls. Some of the hollows are filled up with finely broken ls making a cusp of small pieces. We next studied the abandoned quarry in the left ridge to the south and called locality M 15 Field. It has about

"August 30 continued to same dimensions as localiz'd. It's also a mg.ls. man and as it is long weathered shows almost no joints. It is much fractured by test tube movements. We now see no rounded sand grains or any sandy matrix - all in mg.l.s. If one notices, one either side and once particular to the east are junctions of various kinds of holds, small and large and all often long immersed in the green oh. To me it looks like a man of clay that has been rolled and pushed and squeezed about by the folding and thrusting movements. Then looked up the clay along the distal mine R.R. One comes at once below the rail up the lines into Earl Lewis, it is a flat pottle clay with the taste of the rounded quartz ss., and followed on by another angle of sandstone pieces in the same limit of quartz sand. Have a piece of it. This angle may be regarded as an introfomational angle, and may have no foreign rocks at all. Further east along the R.R. is a much thicker clay with flat pottles and the same rounded sand grains. Have a piece. It also appears to be an introfomational clay. A little further east is the famous Tetrapaptus - Philographus of locality. We made no attempts to get a good collection which can be done easily with tools. Only along some striking slabs. The A and B ls clay seen in the Lewis cliffs and up

August 30 continued The first strus on top of the hills, are real engl. with foreign jettes and onanes, but most of the pieces are of the Levis itself at least all the cephalopod pieces are of Beckman-town kind. Saw some Laugm os These Levis engl are of the same nature as those of Big with te addition ther of Levis the two laymans, are reefs in situie. Ice transportation has nothing to do with the phenomenon, nor Bailey's submarine land-slides. The St Lawrence geosyncline was folding at teh time of deposition causing fats to appear as islands and ridges above sea level, and Coasterine own-cratting lime mud flats furnishing the flint jettle pieces. Elsewhere cliffs were rising furnishing older rocks and from the inland came still older rocks and finally the round gained grind-flam sands and rein quartz pettles along with an occasional green toulder or pettle and some feldspar.

Quebec City, Saturday, August 31-1959. Started in street car from Lewis for the St. Lawrence disastrous bridge over the great river. There are two large cuts directly through the strike of two quartzite ridges of the Laurentian. They are separated by the Chaudiere river that has cut a gorge along the strike through alternations of shale and quartzite. The quartzite is definitely auriferous, we have two samples, one from the northern cut the other from the southern one. Have also taken some red shale (lilley) from the northern cut to use in analysis as to the red color. We then returned by street car and examined the Lilley red shale near the transition into the higher Lewis due to alternations of ls, smpl and green shales that are athyrellow. Concluded there is no fault here of any significance separating the two series, simply crumplings and squeezes. Then collected some raptrilites in the ls series of the Lewis. These are the youngest Lewis fm'ts and are above the Rhemardica ls. Then fasted up and 1:00 P.M. started went up the St. Lawrence river along the S. side. By 7:30 P.M. got to Three Rivers and put up at

August 31 - 1929 continued. the Balmeral Hotel. Have come 140 miles. At five miles E of St. Griv we saw a large road side cutting in grey-blue sl dipping steeply but not at all metamorphosed. Saw some small Electrum- Tonites scissus, and graptolite (few them). These strata are much grayer than the Lewis - Valley series and are mutilated or deformed. They are probably of the same age as the Tremadoc at Mont- morenci. This odder series we saw about 10 miles east of where we examined them. Farther west they flatten out to horizontality. At three Rivers occurs the Richmond series. Accordingly Logan's line must give into the southern Quebec Land within about 20 miles east of Lewis and gradually fan farther and farther south. The beautiful scenery of northern Quebec reminds at our 30 miles west of Lewis. The eastern boonies carry forest on a flat low terrace beneath which are Pleistocene clays and poor land. Tomorrow we are off to Phillipstown. Hope to secure Dr. One Belice (a student at Parker- tm.

Philipsturg, Quebec Sunday Sep 17 1929 Left Dorel at 8.30 and at about 11 A.M. we are in St. Lambert. Then started for Philipsturg where we arrived at 12.45. Put up again at the Champlain Hotel and found Mr. One Serifile here, and as well Dr. Clarke of the Rice, he having arrived last night. In the afternoon we examined the Loma Canadian (= Mallet) or thrusts on the Beclmantown. The surface of the latter is a very irregular one with ridges and hollows on which the Mallet moved and proceeded either apart of itself but more generally the Beclmantown as gone from one foot near in depth to about 20 feet. In places it looks as if one had an alternation of Beclmantown and Mallet, but the actual occurrence is that the Mallet lies in hollows of the Beclmantown or are outlines of the original sheet of the Mallet not yet eroded away. The contact plane can be followed over many hundreds of feet. Some of the surfaces of the Mallet look like a cleft, but this appearance is due to a cross deposit in the lumps every separated by a different material that on weathering is accentuated into a darker sandin color and nature. Then looked at the Minisoguri shore northeast of Becl- mantown or the Trenton shales having gullied along a formation

Sep 1 - 1929 continued. Farther east are Ordovician shales south of the Orallet. Then to the west comes the Orallet north of the Bellman town. Then the Bellman town over the Trenton shales. Finally the Trenton & maybe overthrusted on the ? Trenton ls. Phillipsburg, Monday Sep 2 - 1929. With Dr. Clark, Mac Gangle and Orpen, I started east to St. Armand across the fields and we celebrated Phifer- liftery section to see the sequence as described by Logan. Passed somewhat rapidly over division A that on the shore of Missisquoi Bay rests upon the Trenton shale. The same is all crngls and drf in thick not bedded beds and practically without joints. Logan reports a poor Pleuroto- maria and a Holopea. See Logan in Berl, J Canada 1863 pgs. 275 - 279, and again p. 844. Mac Gangle has also found two fossils which refers the beds to the Ogardian. Thickness 700 according to Logan. The Ogardian is thinner here and overlaid more than at Middleburg - via same from Matt on top of it, in the Gangles A 30 feet or less on the crngls with drf, plus other of the same age and thickness of the Olden beds in angular pieces sometimes in length. Evidently the sea bottom was in motion producing ridges from which the strata tore pieces and laid them in the dolomite mudling area. Dr. Clark

"Sep 2 -1929 continued" thinks the sea bottom during all or at least much of Phillipsony according to Hill times was filling, and these treats are of common recurrence. Logans A 2 is the mantle bed. Logans division B begins to introduce lons but it may be that which includes B1 = 120ft thick above the Ozarkian. Logan reports Pleurotomania and Ophileta. Logans B2 has in places a mass of comminuted lons. These lie in hollows of the bedding and the material is mashed together. At times such pockets are intraformational only. Logan makes division B 1040 ft thick, but Orc Shiple has it thicker - at least below the Phillipsony series at least 200 ft thick, against Logans 2060 feet. Division B shows clearly that the deposition was gradual, and that in places currents swept out channels up to one foot deep. In these deprenimo and hollows lies an oolitic breaching dol. In other places Clark holds that the sea bottom had risen into land and solution holes and even caves had been formed. All such are now filled with the rusty dol. and also lons. The lons occur in the upper lying surfaces of the doloms but not in the dol filling. These depressions and hollows are usually small but at times are more than ten feet across and cave fillings occur ten feet in depth. Crapan has a hint, near the base of division B Stork two small pieces, one a true crag, and the other a fabor one due to weather.

"One Serjio's bed B 4 is of the banded-reticulate (due to weather) character that I have often regarded as typical Reed mantown spheronin. It is a very peculiar deposit; the modules of me characters marked by anything that weathers into dolomite. Over the moraled some previous described comes a well bedded thin paired drl = One Serjio's B 3 1/2. Below is B 3 1/2. This then is an old erosion surface. For it has shallowed, followed by land and erosion and solution of holes and caves now filled with drl. of subsequent fills. The last interval is not thought to have been long. Another aerially eroded surface occurs between beds B 4 and B 5. In B 4 occurs Piloceras and we saw the old holes into which Bellings type came. Now our Piloceras in B 5. Bed B 5 has many once-eroded Cryptosorus, some in place and others fallen around smalling local empls. Another unconformity in B 5, higher up. The Phillipstony sheet is at not two miles across, fine here due to Challet interjps. The dips are much steeper in the W, as high as 70 (the stress side), but in the E flatten down to about 30. However there are also real thrusts in the sheet such since one may be seen in the road cutting about 1/2 mile E of Phill-lystony, and farther east the mantle bed is cut out in this section but present farther west and was much quarried for marble - here are the rolling marble smiles.

St. Albans, Vermont, Tuesday Sep. 3 1924 It was 8:30 AM when we left Philipstburgh and paid $50 by toll to Clarke and Orc Leagle. Two miles south we refuted out as "Burling Canada", and Orantin it ore answered the cus- toms question and orkorn south to be skinned is quary, Then on S to be road totates us north to our cnp, at the base of the eastern Beedmantown. The first place had be logathered oreaf surrounded by ls cnyl, but Corpus said it was a residual resting on the High gate of, and that the Bed mountain sea had caten into State and finally placing the cnpl. in little over into the under cut areas. The man is "trad-stuff" like while the cnpl, in the international character, To ore the residual is covered by a regular's cnyl. made up dominantly of High gate ls pieces. The Rockland great man is layer residual of the High gate, covered with by Beedmantown shale, or by the regula- tion ls cnyl. of many Highgate pice. Next we visited the Oriniqui page at Hyffpate Falls. How to their redded Oriniquari has much international cnpl. derminated by the great ls cnyl at the base of the Hyffgate. This cnyl, is dominantly of its descent from the upper Oriniquaric. Then we examined the sequence from near Champlain shae to St Albans - the southern sheet in the Beedmantown sle- encasing of Primovoli, some Mallet, Crickhartn, St Albans the trend ls Cnyl, at he base of the Highgate, and finally the Highgate slate - our Highgate ls is mostly laminated.

"To the east of St. Albans are the high cliffs of Porters grace, tremendous weathered fronts of the Potugonic sheet. It was a very hot sultry day and neither I nor had much energy to put into the drill and study. At 5 P. M. we went up for tea night at The Tannum where I stopped last year with Keith. Ludlow, Vermont, Wednesday Sep 4-29 A dense fog morning, sultry and hot. We leave St Albans at 8:15 and start S to see the high ls engl. terrmids S of St Albans. At the face along the outer side above the slates lie sandy cross-bedded normal grainy dolomite like sometimes that one fairly regular bedded. They have in them fair scattered pieces of dolomite and terraces the tips to ones. Against this S's lies a very large mass of white mg ls, and it looks like it lying on the slate as a residual. It is 20 ft across and about 10 feet high. Over the tops of the W end ls masses lie the regulatious ls engl. like the ones seem fortuity to the north, and the dip is to the east. This engl. mass appears to lie on the high slate slates, and it has of 10 white ls blocks up to 7 feet across. At the SE end lies another large mass that maybe a residual hill, it is at least 15 x 10 feet across and appears to lie on the High slate slate. Large pieces of the usual sandy dol occur as hills in the typical ls engl. Finally at the SE end we see the dark hue & this weathering hue or yellow only lying the engl. Evident the residual ls ridges over the cliff falls against which the den formed filling of local sand banks and healing up the ls and furnishing more kinds of ls to form the cast.

B&PN# 3458\n We than went S and under the R.R. to the second Cm and going N., or the first road to the Huff Hillards corners to see the large lentic, and the three small ones been last seen with Ilett. The large one looks little residual or a lentil, while the three to the east of the road may be all if not ls lagen. As one sees these three lenticles one is about 40s futacum, and the two others each 20s futacum. Each one surrounded to whole of the ? Hygate formation. Today or one or from here at all, and it is fortunate that none are round by the diagonal to my S and the adjacent. At 11:30 A.M we started fn home. Had dinner at Burlington, and was up North at 1:30 P.M. Through Jeffersons, Putland, Castleton, and finally got to Ludlow at 4 P.M. Put up at the Glenm Tabor. The afternoon was the hottest day of the trip. New Haven, Conn. Thursday Sep. 5 Left Ludlow Vermont at 8:15 A.M. and got to my rooms at 5 P.M. A dull day, foggy before again. It is still warm.

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JSTOR: Journal of Paleontology: Vol. 49, No. 1, p. 93 Page 2 of 3 Doc. 137 [illegible] DEVONIAN DALMANITACEAN TRILOBITES I. Saint-Léon and a. Grande Grève of Clarke (19[µ] older Formations and older authors II. York River and b. Grande Grève of National younger Formations Topographic Map 22 A/16 Cap-des-Rosiers Cove Cap Bon Ami GULF OF SAINT-LAWRENCE Dolbel Brook Cap Bon Ami Formation Grande a Grève Formation coulée II Cap Petit Gaspé Gave prépente b Indian Cove Cape Gaspe Shiphead GASPÉ BAY TEXT-FIG. 1--Map of the Forillon peninsula, Quebec. and bentonitic layers with an uppermost 1.5 m (5 ft) thick of "grass-green" beds (glau- conic shales and glauconitic calcarenites). Overlying this lower member is the Indian Cove Member, approximately 183 m (600 ft) thick of cherty limestones. A continuous sec- tion of the lower member is exposed, and fos- sils are therein easy to collect; no continuous section of the upper member has ever been followed, as its outcrop is largely parallel to the strike of the beds. Fossils in the Indian Cove Member, although plentiful, are difficult to extract, and silicified specimens are more easily collected. Problems facing the stratigraphy of the Grande Grève Formation are twofold. Firstly, the lithology of the Grande Grève Formation changes westward and, secondly, the faunas previously described from the type area of the Formation are assigned only with difficulty (if at all) to the present lithostratigraphic framework. The Grande Grève Formation extends some 225 km (140 miles) west of Cape Gaspé. In these areas away from the Forillon peninsula, the Grande Grève Formation is commonly dis- tinguished from the underlying Cap Bon Ami Cumming, 1959) are best assigned to Saint-Léon Formation. There is thus littl common between the Grande Grève Forma tion of the Forillon peninsula, and the strata ca by the same name farther west. The for tional names applied by those who map a particular area will be used here and ages of the trilobites from these beds will those ages obtained from the accompany brachiopods (identified by A. J. Boucot) Biostratigraphy.--The age assignment of the described fossils from the Forillon pe sula is a vexing problem. Sir W. E. Lo (Logan et al. 1863) named the strata of Forillon peninsula the "Gaspé Limeston and divided them into eight units (comm referred to as "members") (Text-fig. 2). U 8 corresponds exactly to the Indian Cove M er of L. S. Russell; unit 7 on the other h differs. The Shiphead Member is 39 m (128 thinner than Logan's unit 7, although the s upper contact of the "grass-green beds" Shiphead is used as a boundary between strata. Billings (1874) began a description the fossils of the Gaspé Limestones; the jority of the fossils described came from 8 and none is identified as coming from u http://www.jstor.org/view/00223360/ap040280/04a00070/2?frame=noframe&userID=82... 10/29/2007

doc. 137 PERCÉ A brief sketch of its geology BY JOHN M. CLARKE Advance sheets from Report of the New York State Paleontologist 1903 ALBANY UNIVERSITY OF THE STATE OF NEW YORK 1904

MAP OF REGION ABOUT PERCÉ 1 mile Isle de Bonaven Roche Peré Cap Canon Mr. Joll Perçé Mt. Ste Anne Three Sisters Cap Barre Anse du Nord Les Murailles Grande Coupe Rico Anse du Sud Cap Blanc Doc 137 the tide way, non, not, pens arly Len- th, the north mass south reply, thing train to rt to this pre-able. ly in ward comes is off barre shall tered , the

Doc. 137 Mt Ste Anne DV Three Sisters P Les Muralilles North Beach Blondale CB CB Cap Barre Limekiln F CC F J Mt Joli D Perce Rock P F 1 mile = 8 inches GEOLIGCAL MAP OF PERCE AND VICINITY P Limemkin beds L Cap Canon massive CC Devonian and Carboniferous conglomerate DV Drab Shale of North Beach D Cap Barre massive CB Mt Joli north flank J Mt Joli massive south flank JS Probable fault f Fault F

HOTEL ASPINWALL LENEX, MASS. JUNE TO OCTOBER PRINCESS HOTEL BERMUDA L. A. TWOROGER, MANAGER 3/16/29 minerals found in Bermuda fossil soil Augite Pervoskite Garnet Magnelite Titanite Quartz Ostrachno vol. blues Gisen (Dammaris) RW.S. DOCUMENT NO. 137 Invertebrate Paleontology Yale Peabody Museum

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Bermuda Formations Names Recent Dunes Recent Beach Rock Recent Bench Daly's 12(m) 5 ft Berl Southampton Eoliomite 5 - Mc Galls Soil Somerset Eoliomite 4 - Signal Hill Soil Warwick Eoliomite 3 - St. Georges Soil Royal Eoliomite (2- Elba Soil Devonshire (marine) 1 - Stokes Soil Walsingham R.W. Styles, 1929 Written March 14-1929 in Bermuda, DOCUMENT NO. 137 Invertebrate Paleontology Yale Peabody Museum

HOTEL ASPINWALL LENNOX, MASS. JUNE TO OCTOBER PRINCESS HOTEL BERMUDA L. A. TWOROGER, MANAGER

See doc. 439 Coopers notes

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doc. 137 Gespe pictures 1080

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Cap Gaspe', Lower & Middle Devonian Land's End. Photo Cripps 1929

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Grande Grève, Quebec Looking west to Little Gaspe village in middle distance Grand Greve is dipping into Gulf Photo Carpin 1929

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Contact of Sarpe ss on tip of Grand Greve ls. Atmt 1 1/2 miles ast of Grand Greve, Quebec Photo Carpen 1959

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"Interolated bed, Stewart's Cove, Igners Dalhousie Phdr Carken 1929

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Sillery - Cap. Ruziers, P.Q. Near Grand Preve Photo Cooper 1929

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/ re Cape Rosiers formation near Lighthouse at Cape Rosier, Quebec Photo Corbin 1929

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Cape Rosiers formation near Lighthouse at Cape Rosier, Quebec. Photo C. O. [illegible] 1929

Photo Postals of the Beautiful Percé District MADE BY H. V. HENDERSON, WEST BATHURST, N. B. doc. 137 Photos of Percé, Quebec FOR SALE BY CHAS. BIARD & CO. LTD., PERCÉ, C° GASPE, QUÉ. We carry a splendid assortment of enlarged Percé views from 5 x 7 to 12 x 20 especially suitable for framing, also Calendar views and a general assortment of over 200 different Postal views. DON'T FAIL TO LOOK OVER OUR COMPLETE LINE

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Perce' and St. Cune from North shore of Malbay Photo Cooper 1929

SIR WILLIAM ELIOT OSBORNE LOGAN 1807-1875 THE FATHER OF CANADIAN GEOLOGY AND FIRST DIRECTOR OF THE GEOLOGICAL SURVEY OF CANADA 1842-1869 ERECTED BY THE GEOLOGICAL SURVEY OF CANADA

Logan Memorial Tablet, Percé P.Q. On "Limerick Manue" Photo Corbin 1929

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Pie d'Aurore, Percé, P.Q. Priests' road in foreground Orist and vertical strata in Pie Photo Copin 1929

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Pie d'Aurore, Percé, P.Q. Photo Cooku 1929

Road to Gaspe from Top of Mt St Anne. [illegible] 351

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4548—PERCE ROCK AND VILLAGE, GASPE, QUEBEC CANADIAN NATIONAL RAILWAYS

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Bermuda photos by D[illegible] Dayles 1929

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(13) Hammer lying in Remnant of Stokes soil / Hungry Bay. The worst cases ever seen remind this soil Bermond, 929 P.M.I.

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12 and Ella Storks visit at Wilson's Island near Riddle's Bay, Stirl very kindly Hamilton Evansate. Bermuda. 1924 R.H.J.

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Walsingham strokes & Elba at Wilson's Island. Evil overlain by Hamilton? Whitecapping north. Shows erosion in Stokes time of horizontal Walsingham beds in left. The nucleus is erosional. Probably means Garnant erosion. Bernarda 1429 R.H.J.

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Walsingham formation at Hungry Bay. Bexmouth, 929. R.W.J.

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(15) Walsingham forester at Hungry Bay Bermuda 1929 R.M.D.

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Storks sail at Hamman Hammy Bay. Bernuda 1924 R.H.J.

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(18) Top Signal Hill? soil Semimus Beach, south shore. About 5 ft thick and gray in color and full of fossils. Bermuda 1929 R.M.I.

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Thunderclapping and falling of cliff on south shore. Nearly all the sand along here comes from the cliffs, and is already reduced to its present fine condition. Shells on the beaches are rare. Bernuda. 1924 R W.

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Mc Gulls Hill, Mc Gulls Bay It is overlain by Southampton Eubieite Bermuda 1924 R.H.S.

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(260) Prof. Schunkert at Paynters Valley Bermuda 1929 R.M.S.

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(6) Elba swill above bicycle at a locality at a place 5 minutes walk north of Princess Hotel Hamilton Bernards 1924 R.M.J.

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Deep red under cliff on east or south side of Pembroke Murch, Hamilton. Probably Elba. This same soil can be seen on a small island in the march showing deep erosion since its formation. Brenda. RPS.

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(8) Stone structure in granite in Cut just north of Pembroke Marsh Hamilton. Shows reset and freset beds Bennett. P.H.d.

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(9) Hamilton Evianite capped by undown soil. Quarry at R.R. supply locality. Brendon 1429 R.H.S.

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3 Deil m Ernst Elliott St. Hamilton. Bermuda 1424 R.M.A.

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the baths? soil at east end of Elliot St. Hamilton. Bermuda. 1924 R.W.

bermuda s.s. phatus Poecilognathus Nelsoni Bland Pagters Quarry

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Svil m east Ellintt St. at new cut. Bremuth. 1924 R.M.D.

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(17) Cliff on Scrimmers Beach showing fallen blocks R.M.Jr. Bernuda 1929 R.M.J.

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(20) Walsingham overwin by Drunskine at the Gull's Point Mrs Styles in Picture. Bernardo 1924

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(22) McGulls Bay Ella soil over-lain by Hamilton Evianite. Bermuda. Bermuda 1929 R. L.

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23 Segond Hill? soil at Summers Beach south shore. Miss D.W. and R.M. Taylor for Sunset avenue above. Bermuda. 1929 R.M.

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20 Prof. Schuchert collecting fossils in soil #5 on St. Georges golf course. Note transition beds above soil and dune or these. Bernuda, 1929 R.W.S.

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(25) Paynters Vale looking over Castle Harbor 63X Branwell 1924 RM.

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Palmetto holes at Spanish Rock locality. R.M.J. Jr. Bernuda 1929 R.M.J.

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(J) Princess Hotel locality Elba said in our cliff. Bermuda 1929 RMS

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Gerry in Hamilton sleeping method of cutting out blocks. I stepped on the block being cut. The next day the man sleeping cutting in the picture was killed as he was under- cutting the very block. Brenda 1929. RMS.

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(4) Scot m west Elliott St. Hamilton. Bernuda 1929 R.M.D.

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Wilson's Island. View shows Walsingham at left, St Johns & Elba Civil remains plane and over- tlying this Hamilton colouiste clipping north showing a Southern origin. I believe all these islands are original forms produced since the end of the I Glaciation stage of glaciation. Bernanda 1924 R.H.D.

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