Field Notebook: New Bruswick, Quebec, Nova Scotia, Ontario 1900, 1927

Schuchert, Charles

1900

Yale Peabody Museum of Natural History

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paleontology stratigraphy fossils

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84 Pages

doc. 83 Trip of 1900 with Dr. Clarke to Nova Scotia, New Brunswick and Gaspe, Canada. Also trip of 1927

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doc. 83 Property of Chas. Huchert U.S. National Museum Washington D.C. U.S. America. ontario, New Brunswick Nova Scotia, Quebec 7969 Jul.1- Aug.16,1900 quebec Aug 4-Sep.2,1927 3891

July 1 - 1900 Left Washington on Federal Expy. 4.30 P.M. Made the company to Boston of Mrs Patterson and son. July 2-1900 Arrived on time in Bostm at 7 A.M. Had breakfast at the R.R. terminal. Called at Mss. Gmg Jory, saw no one but left cards for Jackson & Eastman. Also left a card at Prof. Dr. Mat this for Orgatt. Did not get into Public lit, had lunch called them at 1 P.M. after which the steamers Boston, had left 63. Many of the Cuban traders had arrived at Stamford, then is great discrepancy of say among them but many arriving from the Spanish location then at Washington. Left Boston at 2.15 P.M. on steamer ship Boston for Yarmouth. Wind very light with no sun or fog on. July 3-1900 Arrived at Yarmouth about 7 A.M. Left at 9.30 arriving after a very slow journey about 6 P.M. at Portland, shortly after I registered at the Victoria Hotel. Mrs Russell also registered on this trip.

"Here and there" During the evening had a long talk with Russell. July 4 - 1900 Started out early at 6 My with Russell to see Prof. Kennedy Prof of the Geology at King College The latter took us to the two main Windsor post localities. Collected the entire day at Maxner Point on the Argo estuary which is about one mile south for the two bridges, and on the left bank. July 5 - 1900 Spent the morning at Maxner Point and finished the life study. In the afternoon collected between the bridge up to Miller quarry.

Brinsea ayne bidge 1 2 Green Bridge location. A point, Brinsea between bridge, finds in this page. 1, 2, 3 Barnum Shales Procheste form Thin bedded blue clay Jellyfish shell etc Red shale Pecorine zone. Corral zone. Dominion Atlantic R.R. bridge 4 3 2 in

"In the region of the bridge, there is the appearance of an art dome. -- On one's direct a short distance south along the town street, the kids are again seen to stand or arc. Def by for long, some of my sketched repeated but not the high rise. At the second fault the kids are gone going horizontal and here plaster kids appear. The structure seems like this: -- Bridge bridge Gruyere dip's M.E. gross grasse 100 ft Fault 3 5 3 dpp ? Fault Carmel Graves area on Bridge R. dip off S side 30 -40 for use: maximum find 2 bypm Corral cave, Rath. -- miles Corral cave and then than stairs is Jutian distances from bridge to Onexian four about 3/4 miles in a straight line.

July 6 Friday. Kindson Collected during the morning at Millers quarry. The fossils here are much like those of the Maxneso joint although a lower band of limestone. Bryony and her attendant essentially Fernstall and Churhfora are of which we only about at Maxmes Point. Picked two trees and shipped this afternoon. To me has are the material from Maxmes Point, the other has smelted jackjags and some material from Millen quarry left in the evening for Halifax. In looking over the above section it seems to be certain that taking the Railroad bridge as a center the strata dip or recede right fit in opposite directions. There is a fault or line but apparently only a slight dislocation. The beds to the south are also slightly twisted out of the strike of those to the north of the body. The second fault cuts out zones 1 and 2 and the sandy limestone appears next in quite another way ! So therefore impossible to say withy the Windsor limestone is higher or lower than the Arm bridge limestone. According to the records the Windsor limestones are higher than the Arm Bridge limestone.

July 7 - Halifax Philed around town in the morning and visited the Provincial Museum to see the Honeyman Collection. There is almost nothing due of Honeyman excepting a lot of Jaffray's plants and a very small collection of Canadian mosses. Honeyman dies suddenly and left much of his collection unlabeled. On moving this collection from the Post Office, thirty present shared the enormous material now with careful array in boxes or dis- dtributed among the higher schools of N.S. The best feature of this Museum is its bird collection and this is small. In the evening read the history of the Academy. July 8 - Halifax Wrote letter in the morning. Also visited the citadel. Visited with Clarke during the late afternoon on corner. He remained in the citadel while drove far by rail.

July 9 - 1900 In the [illegible] Artin Institute there is a tooth of Mastodon shir[illegible] found at Address Cape Breton in 1859. Also, a fiver from Dales farm Middle Rive, Cape Breton. Length 3' 10". The "Giants are Pygmies." The tooth is a fragment with three decided tusks. Left Halifax on the 12:30 train for Antigonish. Telegraphed to Mrs Donald that Clark and I were together in Antigonish to morning. Mrs David Stonegman, Cnr of Mr Stanley, New Glasgow, N.S. Harry Piers Prov Museum, Halifax, Secretary Provincial Museum, Left Halifax at 12:30 and arrived at Antigo- inish by 5:30 p.m.

July 10 Antigoniola, Tuesday A bright sunny morning and waiting for Clarke. He arrived at 1.30 and by 2.50 we started for Arisay were be arriving after 18 miles driving at 6.0 P.M. Ami and Russell called in the country. July 11 Arisay, Wednesday. Collected all day in the uppermost Arigayi series near Storehouse brook. Not yet came 2.5 foot from top. July 12 Arisay Thursday Collected most of the day in a high 40 feet from the top of the Arigayi series. This locality is individualized by the great numbers of Pelecyptera. Also collected material 70 feet from the top holding Extinctiones and Glonites. In fact one can see our Helduby in any zone of the E.6. Not a single character- tising species turns up and what is more to deplore the species are are reminder of the Arigayi fauna. Stopping at Alex. J. MacDonald's

July 13 Arisaig. Friday It rained early in the morning so we collected along the road. In the after- noon collected along the shore from the "Red Hill" to Stonehouse Brook. Also for a short distance into series C. July 14 Arisaig. Saturday Collected all day along Dr. Chasms brook and in the fields to the N.E. A thunder storm with mixed rain came up at 3 P.M. Then called on Dr. Ami at Johnny Joe MacDonald's. Yesterday I had a talk with Dr. Ami on the 2 Dr aspect of the Arisaig but could not get him to commit himself. To- day Clarke had a talk with him on the same subject and he admitted the Arisaig to be the equivalent of the Ludlars but only the Lower Felders grp. He repeated this again in my leaving. Yesterday he appeared to think that the Upper Ludlars are more Felders- by some effervescent deposits. For the teleports which give the Aris- ai grp D its peculiar falmler aspect. They are the common fossils but the species are quite numerous.

July 15 - 1900 Sunday. Went to the Catholic church with Mr. O'sheafoul. In the afternoon collected fossils Arisaig brook along the shore. The fossils here are quite different than those of Gore D and C. This group is but 20 ft Fletcher an Fairbault of Gore B. July 16 - 1900 Arisaig Monday Spent the day in the region of the Pharos brook. July 17 - 1900 Tuesday Arisaig. Collected a few fossils along Arisaig brook and shore system to Grafton factory. Also examined shore extension to Harold Mans farm and the Brown road. The fossils are Gore B. Light rain all the afternoon.

July 18 Wednesday Arisaig. Rained all night and continues on this morning. Staid in the house wrote letter and read all the morning. Note to Rothburn, Drilliard and Mrs. Otmy- onan Rained all day July 19 Thursday Arisaig. Collected in the morning along the shore east in Division C and B'. Division B is a soft shaly gray white B' in a harder shaly gray but more than hundreds of limestone. Collected in the afternoon from the red stratum N.E. to Mr. Adams house in division C. The fossils gathered in the morning from the lower limestone probably in Div. C instead of Div. B'. I have now seen all of the gray limestone from B to D. Palaeontologically it is one series and forms part of a district basin from that of the United States. Approximately the Linnay conforms with the Clinton and Niagara. If any portion correlates with the Medina it

Dalhousie N.B. Section. Facing Stuarts (Charles) Cove, slip about 70° North. Are greenish-grey beds, and argillaceous. Otherwise a whole series excepting near base where they are apparently hardened by contact with eruptive. Supposed to be ascending Eruptive Bedded sandstone Beds of coral reefs etc. 7 ft Brecciated cherty lamine Dolomite Coral zone At least 25 feet. Coral thinning out. Cracihorbed mainly below the catum. Reds 4 [F] Sea level. 10ft. 27ft. 25 ft 7 ft Eruptive [illegible] beds Aulc.3 Coral reef 450 feet, Talus of sea beach [illegible] Coral reef 16m. [illegible] [illegible] 25' 25' 9 [F] 4 7 25 25 27 17.6 58 204.6 ft thien.

MURPHY'S HOTEL DALHOUSIE, N.B. THOS. MURPHY, PROP'R doc. 83 Dalhousie, N.B. 189

is more or less apparent. The divisions B, B', C, and D, have little value lithologically and certainly none paleontologically. A separation is properly made included by placing together B, B' and Clark D. The Leptreedia Anatria (immoglyphus Peter) Fictum and ? Hyzastella contrast sharply with the fauna of C and D. The latter is the first Pelecyprid horizon although they are also fairly abundant in spots in C. All of the characteristic fossils identified by Army at any of Maysara and none of the Heldebury species I hast to find. There is no Pentlandia, Hogs, P. thwitei, R. cuneata, and none of the so-called 'low' Heldebury species. If your works as I see it had been failed very, very badly. July 20 Friday Arisaig In the morning visited Doctors Brook but found nothing. Then looked over the shore at Pelecy Cove but saw little of any value. In the afternoon pocketed the final box, looked at the so-called 'low'

"I hope you will be in the city next week and finish the Arisay region. Brookes thinks we'll get 32 stands which Mr. Mac Donald with both to rail on. July 21 Saturday en route for Dalh. Left Arisay by stage in time amid at 8 where we arrived at 11. A.M. Here we adjusted the shipping papers for Mr. Mac Donald and had that attested by a Justice of the Peace. I took the 1.15 P.M. train for New glasgow to see Mrs. Strongman. Saw Mrs. Harley, daughter of Dr. Strongman. Found that Dr. and lady have been her two days ago. She said they would be willing to part with the Arisay collection in $250. This is practically Dr. Strongman's life work in geology. She says the collection is completely labeled and that it is the most complete in England. Mrs. Harley is sister of Mrs. because for several years she was the attendant in the New Berlin Institute. Further she was much with her father when he made it. Left New Glasgow to take the

"Maritime Express" from Dalhousie had a berth. July 22 - Sunday Dalhousie Arrived at Dalhousie at 4.20 Eastern standard time. Retired and had breakfast at 9. After that spent the day on the shore at Mr. Stewart's house collecting fossils. Later in the day very cloudy off the horizon and to be taken from Dal - down by but a time. Cumulus gone and I saw Hildreth reminds of the fame is propounded in crests of Farritas. The magnitude of possible remind of Middle Cumbria.

July 23 - Dalhousie, Monday. Spent the entire day at Charles Stuart's Cove. Had a grand sleep in the morning. A section is given beyond. Estimated at 204 feet. Dip about 75 deg. north. The highest second coral zone is seen only at two or three and had apparently the same species as in the lower series. I dare not say precisely from it. [illegible] These beds indicate geologic ac- tion during deposition and these beds have affected unlike those lower. Arenues are seen here. Steepen up, the corals reappear. The first masses of eruptive matter is subsequent and broke through and injurious stage of the Dalhousie beds. It may be been the case of the tilting or may have no other thing after the tilting. All my fossils are marked according to the numbers of the section, 1-6. See section on next page.

July 24 Tuesday Dalhousie. Pork boxes etc on a wagon this morning and finished collecting at Charles Stuart Cove. Shipped 3 boxes, 250 lbs. The large packages unmarked are all from the Coral Grove, which is 4. The second outcrop farther south we did not see again after Sunday. If Dan can only but otherwise may be another series. I hope so for fossils, a smart Pentamerus on the bottom beds. Left the hotel after supper and went aboard the steamer to save ourselves the trouble of getting up at 4 A.M. Tomorrow. Route $1/22$. Earthquake, 3.50 For more at my Dalhousie see after Aug. 6-1900. July 25 Wednesday Left or tried to sleep aboard this Admiral last night. The French passengers, and they are one friend, left of a cricket all night and with rain and thunder there was little chance to sleep well. The very idea that I am abroad in a vessel seems to unsettle my stomach. While I am not sick yet feel uneasy. The Admiral alone, it stops in its

may to Baspe: Only at four is it possible To have wraps. At one other place, alike boats and barges come out to the ship and transfers passengers up freight. The language most generally spoken in this country is French. There are no less than three priests aboard. The old fellow is about got through as he can be and is attended by four or women. July 26th Thursday Baspe Fog and rain all day aboard the ships. Pass little of the Oland and arrive at Baspe about four o'clock, P.M. Peace in sight good on the fog also Comanche Island but hardly to give one a distinct idea of these landmarks and Peace. July 26th Thursday Baspe. The morning is bright and all the storm appears to have blown away. Baspe is a very pretty place and well adapted to watering. Dr. Kakeham is in Town with his vessel. Dr. Dr. Kakeham who once in a steam launch takes us to Peninsular, there we can talk again to Island

"Dr. Gralcham says that only further instructions for the Smithsonian service are as in the prominent vessel to Anticosti. He advises taking the necessary help from him at $1. to $2.00 per day. Arrangements can be made also in Anticosti. At the Jefferson are fixed. The agent at East Point will get the necessary permit to collect. Best season The middle of July, later and first 2 weeks in October after the Hare flies an about five. Camping out- necessary. The foods can be shipped at the various post offices and telegraph stations and can be picked up by Dr. Gralcham. Canoes he thinks will be the most serviceable boats. A trip to the head of Fichersigh Bay can be made from Capt. John. Blandford, St. John's, New Brunswick or a station if makes trip to Cape Chidley. Choosing for coal first go to this point. Capt. Blandford in the Ocean would take us to Saguenay a schooner could be hired for the entire trip and to cost $1000. A schooner leaving regularly from goes to Anticosti the first day of fifteenth of each month. Passage can also be secured in this way. From Dr. Gralcham would bring

to take us on if the necessary time in advance can be furnished this. Dr. Brakehart had us taken over to Clemencia by the steam launch of the La Canada which he commands. Late in the day had two vehicles take us to Brand Tree where we arrived at 6:30, P.M. Our care. Hotel at the house of Orbel July 27 - 1900 Friday, Brand tree. Started out with lunch and spent the day in Creek Rover Cave. They kids 1 and 2 came down to the stage. Pejos are most prolific in kinds of grapes grapes are the common fruit, Alphonse fruit are not common nor in fine con dition. No delicious fruits type up yet by disappointing fruits are thrown upon the party by affluents or species. The housing of their beds is about that of the down Weldbury. Our soil but Clarke seems to think the Creek Rover kids and the Alphonse go together. Both have similar cords but otherwise the various are altogether inharmonious

"North Britain and of Cape Breton Ore, When the earth's surface is one line, the difference in heat between two points in the same latitude is proportional to their distance apart. John Gould having his a ship hit by its fault.

July 28 Saturday Grand Bravo Started out for Cafe Don Amis but before half way there lit began to rain and with the muddy roads we had to cross through Clarke thought it best to give up the trip de then returns for dry clothes. Late collected along the road to Tyndal Grand Bravo to Ledyon Cove. Found an- ecdote Orient any fruits. July 29 Sunday Grand Bravo. Spent the morning at the English Garden. In the afternoon walked to the "high hill" and looked over the bay towards Cape Rosier light. July 30 - Monday, Spent the morning collecting in the little reef coming down- (Barnes other are coming) through the Facing (Dolbel) Fish houses. This is the Shipgriggy Bahua. Have quite a number of these but could secure but after fair specimens.

This horizon seems to be with the dawn of July 8. In the afternoon collected along the shore east of the Farrier fish houses to about half way to the Island Grove P.O. These fossils are mainly characterized by Rhynchonella philippina. July 3, Tuesday Grand Bayou Spend part of the morning on the M.E. shoals where called "Quay" type bits of the Basque can be seen. Also the conjugated beds. Fossils are exceedingly scarce. The conjugated beds appear as if fiddled much had been pushed causing it to curl and distort. The limestone bands are nodular. In the afternoon collected at the shore below Grand Bayou Grove house. Here there is still an Eotonia strong. Late collected at Little Basque but found very little. The contact of the Basque limestones and Basque sandstones are seen on the shore east of the little stream flowing through Little Basque.

"Our work indicates that the base limestone series had best be divided into three zones with distinct names. The upper lagers beds 8 can be termed the Brandy Grove series because they are well shown and are most fossiliferous at Brandy Grove to Indian Cove. The middle series, Lagers beds 3-7 are practically unfossiliferous and may be called the St. Albans series because all these beds are seen in St. Albans Cliff down to the shore on the road to Coke Springs Lytt house. The lower series includes Lagers beds 1 and 2 and may be called Rosed Cove beds. These lower beds make a good contrast to upper lagers. Beds 3 are soft and break down while the balance of the series again stand in vertical cliffs.

August 1 - Wednesday, Grand Grove. Spent the day at Ship Street. The Keefut as present by the brother to Mrs Owen Moore at whose house we are staying. The section giving the place at this head beneath the cliff house is as follows: | Rock 8 | Lean Line | |---------|------------| | Oyster | Bad 7 and Bedding: Joddy 6 | | Cavity and Hole 8 = 200 ft. | Thin hard chalky limestone grit Land shelly flinty Triad Beds x 20 of feet. under) can't fall in Indistinct thin coat. Shelly sandstone shells green col. shale etc. with some limestone bands Shattips out easily. 150 ft. thick, the small sands at the top. This red dolomite limestone x 2 feet. Flinty shelly with thin bands of blue stone. Has large & flinty shells at the bottom and a few flints over 17.5 feet.

"This valley goes to Grand River at three stops." Cape Cod. The archs in the bottom of the "valley" have Chromites, cancrusis and there are a little lower than the large L. Hellebals along the shore. All are dependent on Bed 8. They are given the region of Dolthi creek collected on Monday. In this case the top of Cape Cod is capable by bed 7 and which one appear to have and most now have we sent the beds, except at the bottom of Atchison City. Further at Ship Head Bed 8 is 300 feet thick and 150 feet where merging which partly are banks along the shore at Grand River. Among the same personal combination appear to throw together all the Ship's head Presidio type beds which in that region only happened bed 8 at Ship's Head about 700 feet. There is no telling however that the beds at Grand River and not quite higher than any of Ship's Head. In that event it may judge that Bed 8 is considerably thicker than 500 feet.

Both yards & an hill slopes down to Brandt farm on Burke Bay. R.R. Bldg 300' Bldg 5-380' Taken after Two acres in clumps. from A barn - C.P. River Farm.

Grand River - from Rock at high est point looking at St. Albans City and towards Grand River Gne. Aug. 2 - 1900 Oct. 7, h. 240 R. d. 4. 200 ft. R. d. 3 170 ft R. d. 2 90 feet R. d. 1- 70 ft. Cape River Line One River Two Creek Three Creek

Aug. 2 Thursday, Grand Mere. Spent most of the day at Rosier Cove and seemed many large field bury fos. There are mainly from Bed 1. Hardover beds 1 and 2 hold as the greatest some many of the fossils seem to be common to both did further get an collected fine bone and for this bed. In the afternoon packed the fossils into one barrel and made it ready for shipping. In talking with Clarke over the Colhoun horizon, he is rather of the opinion that it is most closely related to the Chapman fauna. Also that it seems best to fit into the Saspe beds 1 and 2. My own impression is that this Col-housed fauna is probably a thousand, unlike any bed of the Saspe series. The good aspect seems to connect it with the Saspe beds 1 and 2 but then more the fauna's are different. Is it possible that the Colhoun fauna may fit into the Saspe above 2 and beneath 3? This point may be determined after we return to Colhouster to visit the town beds.

Aug 3. Friday, Grand Z. - Basque Basin Left Grand River at 7.30 and by ten was at the Ariscon de la Gran Obiense. Found the place practically inaccessible, the streams high & rain, all the works almost imperceptible. Under these cir- cumstances we seemed but for fossils. Arrived at Bakers hotel for dinner at 2 P.M. Then started out along the Dart- mouth River road to the Pear Mill and then along the Postage Road to reach its end where in the road I secured a number of sandstone fossils. This locality is desired for a fossil, plentiful out of the hills in situ. This is the first sandstone zone 1100 feet above the river- line. Aug 4. Sat. Basque' Spent the morning opposite Basque and found one lone rock filled with Cephalocinina and Chonetes. Did not find the fossil ledge mentioned by Logan. Collected in the afternoon on the Postage road. This time east of York Ave road which is at about 2 miles from Basque village to Postage road locality.

Aug 5 Sunday Basque. Spent the day along the Griffin Cove road about the Grand Cave streams. On the Geological map this stream is named the Grand Carierre. The springs here are difficult to secure and the few seen seem to indicate the Basque proprietors held lands. Clarence admits this. He found Rhynchosmia milare. He sent me to take me to this bro. in Mr. Colomitz. The agent of Basque in the Anticosti school is in Mr. Dief. The limestone and shale of the Grand Cave crop out about 1/2 mile further on the stream towards Griffin Cove. Then follow huge blocks for coarse conglomerate with a pebble matrix. This may be a part of the Quebec series. From the Grand Cave towards Pen- insula the Basque limestone again continues for nearly two miles. This shows further that the beds of the Grand Cave are now down in the series.

Aug. 6 Monday Steamer Admiral. Came aboard the steamer Admiral last night and this morning on a little sea sickly. Did not get off for breakfast. Charles suggests for Bersey longstons beds 1 and 2 Rising Cove beds; for 3-6 in Ami beds; in 6 and 7 Stand Bure linestones. For Ben Ami it might best to care them at Calhous beds. This will avoid the Cape Ann Ami or Ben Ami reals near Dalhousie. The latter are best named Dalhousie beds. Arrival in Dalhousie by 4.30 P.M. See further remarks under date of Aug. 7-1900.

2/2 240 /6 18 A [illegible] [illegible] along [illegible] (? tuba niter cave) see specimen (Later. Dipped from above.) S.P. or second Wachmans & th infelip. Aug 7. [illegible] Oamaru Bluff left country Oamaru layer mass 30° dip M N E about 70° B Penetrating and dip. Blue grey slate to phyllite Grey to blackish shale and the bands of leaping into black compacted impure limestone. About 125 feet. country which had [illegible] two around [illegible] dip M = E. dip rising around but to North k dip. about 70°

tu Crad modular Left Sculpture. Right stria and radial ridulae Anterior, Chief of my (160 yards in a dotted) man. & I will separate, as much as possible, from the rest of the art. [illegible] other section type here this part. strata stream.

Aug. 7. Dalhousie Tuesday. Spent the morning in the cave beyond the high trap ridge. D.D. & Sturges Cave are next on page before this. Had very little time to collect or descend at all today. Clarke has most of the fossil points collected while I made the section. After pocketing and shuffling the single box completed to assist the elder of the morning. The tide was out and terrible for anywhere. On the Portamurus bed I found a number of Leptaena? or Pineaora. These came in just a few feet above the Portamurus. All my proofs are regarded to agree with the section on the page before this. I am more satisfied that the Dalhousie beds are true Devon, Holdbury but that the fauna is unlike that of New York and belong to another province. Further, that the Dalhousie beds in a general way correlate with the Cape Byron Cave beds which are away in a straight line 140 miles away. Clarke thinks about the same and finds that the Cornforth fauna is either the same or nearly of the age of the Dalhousian series. The Dalhousian beds must be the key to the base of the Cape limestone series. In Portley very a page and detail map of this region in Murphys hotel I saw there

October 2d. small maceoas as far west. Cuphins. about 8 fath. off about. Cuphins. over line. Abund. [illegible] about the eastern side all in depths. and being a maceoas.

Cape Bon Ami is on the north side of the Skepe promontory. It is not given as an Orthosie. The nobls however just called Strats Cove, are called Bon Ami rocks but it is easy to name the Orthosiy hills in Strats Cove as Bon Ami. The latter name should be restricted to its original credit. On the same map I see that St. Albans is a village near Cape Race light house. Therefoe I think we had best use in the middle Skepe limestone series Bon Ami beds instead of St. Albans. Aug 8, Wednesday, Ennorets, Quebec. Set off at 2.30 to take the 3.10 train for Quebec. Had to go without breakfast til 7.30. Arrived in Quebec at 2.30. My ailing and has been doing so for the last month - your mind of this curious turn but no distant wing. There is not a regular bookshop in Quebec. All are dealers in station- ary and magazines. My little English is spoken here and many of the street car conductors of the urban Tram can't do it. The streets are narrow, some paved with granite blocks, after most asphalt but the

"majority are asphelted. The side walls are very narrow and are usually paved with bricks plant[?] offer at the Victoria before come in in the Annex. Augt 9 Thursday Quebec. The French are a noisy set. A couple of men on one floor had a celebration with gaywomen and made noise until mid-night the way of again etc. The dear in a fire one am[?]. I start out alone. First walk in midst of the "Lower Town" and then the "Upper Town". The former con- sists of many small one story houses with gay little festival roofs in distinct quieted rooms. In many respects the section of Duplex reminds of the French Quarter in New Orleans. Walled around the walls of the Citadel and then through the gardens. Had a fine view of this country. The St. Charles river here joining the Old Lawrence. At the junction of these rivers the impression from the citadel in this here there are from right at right/ corner. The factor showing that one of the largest land masses in the Island of Orleans. To the [? North] are the Laurentide mountains, some quite rugged. Try five

"the impression of terror felt in one higher Beyond Point Levis the country is stilling. In some things the offer I get to me continued climb, climb up to Dufferin matters, the magical Belleisle fortumae, the fine monument to Charle plain, along Dufferin collapse to that club and then hill all of to the tops of the citadel. From that Citadel one passes directly through the St. Louis gate to the Parliament building. In this region along Grand Allers are the grand some residences. Left Quebec at 2:20 pm Montreal way are arriving at 9.30. Took a room at the Bolmont Castle Hotel.

Mrs Bill University City Redpath Museum. There a large and fine exhibit of Eogon and the associates fossils. Their general ap- pearance is certainly most like the ostraca- topsides. The Little Metes spray on blood slate show an abdominal with white over the specie. Has a fine specimen of Stereaster sal- tum (two easy felt tips) Also a Palaeotryma musa from the Hud. Riv p. of Anticosti (Alwood case 2sh) It is a very good specimen. Of Palaeaster giant he has two fine specimens, from Grant of the Clinton at Hamilton Lower Red. Case Phacops striatus is a head of Delmanites East River Pictou seems to be a good locality for fossils of about the same age as Anticosti. Homol- ites Dawson grey in an estate. Sutherland River is also a good Anticosti locality. The first even a clean fossil skull or cast. Dawson makes no distinction and calls all from Hudson Bay, Anticosti, East River Pictou, Sutherland River, Eyound Shore, all Delmerian

Leptocelia intermedia East River Picton are very much like L. haematites. Dutchland River has a large Rhynchocladi mega metatibae. This requires much of the Large deltahy. Trematoscelis acutice is - spicifer. In pic East River Picton, All the frisks for Coke Bay Annie are from Dalhousie. I have nothing to do with the Coke Bay Annie in Blake. Many of the frisks from Dutchland River and East River Picton remain strong of Dalhousie. They may probably prove a distinct form the Arboretum series. Spicifer coming from Dutchland River looks like the same Spicifer from Dalhousie. The large called erect corns in true latellite F. haematites. The hemispheric menne with small cells F. hemispheric. That flat Scindia from Dalhousie is H. nicholami. There is a particle in this collection with Stolzity stage maybe one with small cells give a fine base? This particle is not in place. Palaeocin parvusculus is a mold in a large particle with enormous costs of crinoid stem.

Looking at the Saint Helena Island birds it seems after all that they are of some Melanesian type. The Thicklandia suspensa seems to be a Rhynchonellus grandis. A very common in one little colony, The species near menors is of that type but not that species. The Saint Helena Island birds and the ones off of a different country than those here are Melanesian parsons. Certain all of those are of some Melanesian by aspects. Danson has all the Dictan from or Guiana. Danson prefers to use Erion or Geormia. All the labels have it. On the outside of the case it is "Erion or Geornia". For the forest series he has "Dilurus = Candrian". The Peter Redpath Museum is one of the best American Museum fields. The birds are good. The mammals are narrow but high, apart of all of the fatter cases with dramatic undertone. Between the wings are glacier cages just like those of the Zoo. Mr. M. W. in the middle of the formal films are the large exhibits and draws of both coven or lepor. One wall is given to large sloth, and beards. The second floor is a gallery with

the agreement as in the Plan. The forms are exhibited, once & trays, shelved to paper boards or plain in plan large bill boxes or paper stands. The forms an alternate with an case can be seen. The details lie in often partly a basket, or Rostymore River on Arden Ontario. Everything is labeled but not in my case recorded. Sometimes there are very bad errors. The animals are shown together casts found and pictures large plants are also exported. The gallery is occupied by the Geological department whose pieces ride underneath. The Carpenter collection of Mollusca any fine. All laid out on plain with a dead black background. The name in written on the plan in white ink to do. Palaeotermia rugosa is of the same genus as P. pincumbra. The plate appears less squeezing than Bellini type but otherwise it's a little green. It must belong to There is a Helms Island list by Dr. Deeks in the Record of Science I mentioned about 10 years ago. De Martins (not this one) Dr. Deeks, The L.H. Jos. of St. Helens Island.

"St Helena Island Shirifu concerning appear to be correct. Rhyn. prumoa, R. mutabile, R. vestitus. Then there is a Shirifu which smells in much like what the Cylp I. emeemia but the thollare unda plicatus trans orantus. Mastipynchus radiata in part a large Orthos, Plagip.Delophythus hae. Q. Maly may be Deligifayria ~ Q. tubulostriata has two species, one a small Orthoderonto like paphana the other a Orthoderonto affants nua variestriata. Shirifu cylpeterus. Stricklandina gascensis is a hy Rhynchus near Taranandui.] Orthos near Allet, the other a Strickherdntu with alternate striae, near variestriata. Strickalleo near the little Cembrulae species Pult pseudo-galeatus maybe a par. of galeatus. It maybe the same as the one from Calthrusin. Ryb. agremuli is a Sp. emeemia, sp. chroidalis Platysternus Chamity like Ploe. sericua, Avreelfield. for point to club. Stictopon Demitypon & Farvotille the Delisletes? in a branching Tarriter

"Jot. Roth. striat. spora. Sphagnum spora /29p. Day: new hemisphere J. Delhoussie This fauna identified by Dawson and small nud, yeasins. Ask Dr. Adams to have Mr. Andley dr some collection. Permit only have to come from the C.I. authorities. My Bell's Arisay collection has some good things but taken in all I think my collection will compare favourably. At least I have many species polypods they have not. East River Picton should be collected in the hemisphere are better and more Gymnosperms. They also have a more decided Lone Helderby aspect. Dawson has Philadelphia prince from Cape Bon Ami, Abr. Prototaxites Morganii, Pachythreen. The castings of Hypotyodendron Eatonian but much better at Lepidodendron. I can't see how it can be the making for Bryozoa. There are some splendid ferns here marked Delhoussie. They have in say sandstone. Others of the same

natum an lobeli Lcaminae, Ivotan M.D. is a good & Cast, flat locality. Diggins, Sydney and Picton are the best Coal Meas plant localities, Many of the first Botrisidpes are marked Niffer Ericæ Dalhousii; this type must opposite Dalhouziii new Lauginae. Lower Erica frith seem to be abundant at Campbelfton, Le Brown edite of Events, The leaves sometime fruit skins are in a coarse yellow to greenish matiny. Usually there is only a Cast. Nictanx M.D. is placed here as Disth- an. The fruit are very poor and badly distincted. Ostys hipparinyx is for some time ideal, & of arenæ or of that type but hardly that of Ostys Dick Philocalus. Aen. croodes dam shurg out from Dun. D. arenan may be that species but the almost flat condition of the fruit lead to the impression that this is a mistake in the range. It and O. nictaurens are the commonest fruits.

E. Ardley Redpath Museum Montreal Left Montreal a little after 7 p.m. and arrived in Ottawa at 11.

Aug 11 Saturday. Ottawa. The Geological Survey Museum is in a temporary square structure of quarry struck stone. Inside, the large labels are seen upon the ends painted on the top side and outside of the cases (made of white paper) which inside on the engraved surface the effect is good. The numbers on all the specimens are probably slips pasted on the material. "Cape Bon Amie M.B." is used very often for the Dalhousie locality. "Cape Bon Amie Bay" for the others. The common species from Dalhousie is Lab. S. cyclostoma. Cypra asparreta from C.S.A.M.B. The matrix is quite different, seems like fm 2 loc. "Ss. Miculites (S. radiata)" for Dalhousie looks good, like a Retro-lance. Not proper in some cases, indicates Phys. shells from Dalhousie lot. R. modestula. "Ss. crista" from Dalhousie appear like smooth S. cyclostoma little shells. Iodospila cast from "Cape Bon Amie M.B." but the specimen is wet here. "Amisay" fossil case in marble, E.-2,3 & 6". On each with two.

Cases are Lot 2. Held, The Whitlow series in fine but allow me Case 3 x 2 feet. Port Daniel is fine and good in a course marked E. 6" for the lands of Chalen [illegible] Oct. 2. See another note Aug 13? Between E. Boske & A. Rozier J. and "Cape Gm Ameli N. B." all are referred to Lowe Held. Buelph in "E. 4" The best Antiquati fossils are fine Dec. 1. While the others have good material it is apt to be fragmentary and in rock. The Bullen Riber fossil goes also good. The stratification with Egyptian are also referred to the A. Held. Looked the name Chalen- foss. The fossils are all glued to the painted blocks. Each row or column is separated by block sticks.

The Beaumne Bay fishes collected by Ford and Preston in 1879-80 are very fine. Our Union Oysterman, some say is hardly other or slabs. The plants for the same region are also very good. Indian Cove, Brand Grove and Little Saspe harbor furnishes us the best "Crabapple" apples. While some of the materials in better than again get our John aligned will be the equal if these. The Saspe co. forms are not so good as ours. The Campbellton fishes do not appear to be a good as those of the sea. In the vicinity of Caguya they are forms I have well seen before. They may pay to look up. The large slabs of Chimtichmitz caboni make good shoe material. From the Lake Desir/Pepins region thereupon a Atypon of about 19" in length, almost by appearance nearly 2½ in width. Across the lake the future Green measures near 4 inches.

"Phillipsia" (or similar) "hannachi" for the St. Lucia region seems to be the same as for the Red Pond area regions. Since this afternoon showed me the Moscov Collection de identified 14 years ago, The specimens are quite ungrateful, and have been identified just as found. I am going on and on the materials! This Pent. Knighti u two dorsal valves superposed of Clytona articulares. The Orthoceras longicamentum seems to me to taper too rapidly but above all it has too many septa. If I remember the species correctly the Musicy specimen has 3 septa to one very few just species. Orthus pereydon is a small chree and seems to be identical or near O. hybridis. The other 2 field species I could not find. The Lignula in nodules occur at Meryland Made a good many notes on the starfishes. Found Reilings accurate, or nearly so, or far as it goes. In some cases Le could have gone further. Called on Dr Amie after tea.

Aug 12 Sunday, Ottawa. Spend the morning with Dallas R. Billings. He showed me a number of fossils. Among others a Cybceratoidy which that this fossil was a free animal. The plates both sides are granular but different granules. The lower side has the radially plate mate markups, pointed by Billings. The upper has small close adjoining plates. The lower side has a central opening which may have been formed as protruding above the upper plates surface. He is willing to exchange us Trector and California fossils. See to send him first class Illinois crinoids and then other fossils. Billings thanks very little of Dr. Ami by a word dear favor from Prof. Whitcaves. He remarks that the latter is so difficult to get his doggin nights or to walk at the home. He thanks him again. Billings family are Boston logalists. They settle near Ottawa at "Billings Bridge" on a lumbering camp. Although Billings was from several miles away from here, was a fine looking smart broad shouldered man given tall. Studied law and practiced it for a time and then after a literary turn of mind enjoyed his out with the

'[illegible]' and having a good time, his grand family but never press after to make a comparison of same problem. This portion led to his engaging outright distractings. E. Billings did not believe in the organic nature of Coprinus comatus. Logan was the first to state it up, but Dawson thought of other Carpette, and his support. Dawson also took more the credit. She said that Billings wrote and that there is no reply in the Survey Office a letter calling for be allowed to give his opinions. And Logan would not allow. E. Billings did not consider Lu Dillon, Dawson much of a geologist. Walter R. Billing relates that his aunt is speaking favorably of Dr. Billigan had a reprimand from E. Billings as follows: "Oh, it's no geologist at all. He sees fossils in any carpet pattern!" Walter R. Billings speaks very freely of J. C. Weston and made some funny comments on his book "Reminiscences about the Devils." She has some friend in Ottawa, a publisher who undertook to make the book presentable. Weston was my timid man and had many adventures more others would have been mine. Ami is graduate of Mr. Bill and

a protop. of Sir Franq. Egerton. I cannot help thinking but others that Dr. Ami is not much of a Palentotogist. Certainly to see Pentemeros Knight as an identifying based on two cup and bowl colves of City in Cathedral is enough to condemn any one. I cannot help thinking that Dr. Ami lost of 10 years ago (Friday last) is more than just guessing.

Aug 13 Monday Ottawa The type Taeniaeii cylindricus is on a large slab in an empty case. The Eggen collection here is some more interesting than at the Bell. Distinctly particular and in the long manner. Ami has one in a little oval bottle, with roots. Port Daniel is a fine locality for fine Megarian fossils. They come out good and are very creditable to your col. The following are some of the Megarian species: Or 2 Choleus pl. Biffieldia timida Chy. milomi Gonia expansa Geoceras sp? Imago Pentanum? like the Gounne P. algetra, Rhys. stricklandi, P. cripta O. flutello O. elegantus. A. articulans Other species do not compare with those of America. Division of the Choleus group is mainly characterized by cords, which is

than is quite - rare. L'Anse au Basen [?] and L'Anse a la Barre L. host loc. Another in L'Anse a la Vielle ? Spirophyta Caulusalle in E Candela ha no strotysophi value. It found it at Colborsit but man Part of Scope. There is a specimen for the Chalem [?] I which in Michigan. Baspe collection now made by Curry, Logan, Reil, Weston and Fohrd & D. Peter. But Dr Whitman and others might of the morning meet him. He agrees that the Chalem [?] and Smith regarded as a man field in 1863 and it Michigan age. They are retained up that place in your possession or Belfor's left them because the strike has not been removed since. Just methods of proof reflect no credit on the survey. If their collection is lost, it should thank a pupil not impress by an one. And this knowing by the poll, Enttlypt in chief. Whitewas is the most original Paleontologists know to me. In a letter he in colour and opals represents a division. In conversation he declares right and left. Paleontologist

"de agree into the schools are only on the living side (general) who may be called "luddites" and those on the "doleful" side usually "agri flattons" which he thinks belong to the latter school and thereby does not know his own forms. Dezatti's philosophy is all rot and he charges that in "this world" we cannot know the times & descent. It left he puts no value in Dezatti's own philosophy. Ami he thinks very little of and says as at variance with are the men of the party. He does not care to give his opinion regarding any of the contemporary did get the facts as he selects them are all in favor of Amij. For instance he says that Flitch he worked for 20 years in Nova Scotia and has paid his attention to fruits. Certain a horseman for any such girlgirl. Then Dr Lawson on "The Times" of certain parts calls cutar by Dermia (which Huston ad David White said perhaps say are Calomining. Further he places great value on the determination of the latter and yet he will go into the Amij's as to the age of the beds, because he is no paleo botanist. Under such critical stages Ami is left alone to put the palaeo tigraphed stratigraphy without the support

"of Dr Whitcam. The latter in the chief the division of Pol. and yet he could not legal. Peter Amis. The greatest factor against the latter is that he is an erratic and even quite dog crazy in a problem to settle it. Further he is a poor paleontologist but while he makes many trips he in most cases will aggravate the work of the Lymph better than Dr Whitcam. The books of Dr Whitcam is no doubts good but his reluctance to an effort in joint officially is a detriment to the Canadian Army difficult to counterbalance. Sandy Carrion Brook Styphell punctulifera Atypa actylara Sk Phrodonto (arata lily) Orthus (? Photo) Rhyniophyton (lil 24) n? Orthotheca keki Pterophyllon manno ad lug and mud on from him. Suffit River There are tails of a Durostros or Dlamun from different matter. The L. gleaming is for notty (?) Chest) with the point of the tail. But away gave another small tail for one rock to form to ides; joint of that imperfects.

"Dalhousie The Cyrtia exspicata is our Cyrtium from Ramillies (This sp. is an Ami form). Cape Ann, Amis N & C. entum Calymmer (Helmuthi). Sp radiate in the pentagonal, not quite this species but pretty close. C. exspicata 3 Sp ident with Rhynchomella modesticula is a gory coarse albus A reticularis (not a true A reticularis). Spiriferma criopa is a speci near this one. Spent the day at the Luxury and left on the 7 P.M. train for Montreal. It was said that Mr Terry Hunt was hard after the crewmen. Also that he carried the north gang on in the Canadian Luxury to Stale. I take it this man there been going on during Billings time and that Stale in this way knew what he was doing. Elchanah Billings had a brother in Ottawa - Charles Billings, I saw #200 towards Billings

"portrait to be hung amongst the prints. Dr. Whiteages will lend one of his starfishes at once, from Louis Nul. Halter Billings may let me have eight or twenty are of his Tabulae starfishae if he can send them from another place. Whiteage also does not believe in the tyranic action of Cozyon.

Aug 14 Tuesday, Montreal. [illegible] All [illegible] Island, floods killed calves & animals and dam stream girdle. off [illegible] off [illegible] all kinds of fish swimming by a thick bush from old days. off [illegible] Cuts back at D. s Approaching (1) Trap (have a press) 2. Hill. about 40 per Trap about 30 and 2 about 30 but large slow then or from and marked of water of [illegible] So many.

On the up stream and facing the city of Montreal (170 miles) St Helen's Island Block. Chole in shorin. Thin is cut and corned different by drops. It is strong in ground layer faiths different and away from Montreal. The salma of the island is made up of the agglomerate and carries limestone fragments in which I have Plie, Seneca Anthomerna filitexta and striptylesian. Also a flack full (minutely). The lower Hellulwy is part of a large mass of limestone broken up by decompose action and embedded in the middle of the agglomerate. This limestone seems to be an ancient limestone. The up stream end of the island appears to have the agglomerate in smaller fragments. The Downstream side has often fragments a foot or more in dimension. These roots are about 20 miles for Mount Royal in an air line. The agglomerate is composed of Trentonian limestone, Otician shale, sandstone with Pitsdas or Freeling and Lower Hellulwy. Also old crystal. The Lower Hellulwy may be a man in open and most of it broken up and mixed with the agglomerate. Part are cut by the two sides. The Upper Hellulwy may be hard blocks involved in the agglomerate. It has its own that way. It certainly is rough cracked at these spaces quite complete and the agglomerate. Being very difficult to make out the folding.

"Mr. Lill, U.S.N. Of this Arthur's fill [illegible] five specimens by Sellers there are specimens for Price. These are described Avicel species, Arthur Lill must the army. In association with the St Helens Island group (Seldenby) there is also an outcrop of Middle Oomian rocks. Mr. Liddell showed me a fine specimen with several quite characteristic Spirifer designata. In the case there are three other species with quite a different spiral (named like S.— [illegible] from the [illegible] Rock Island). It has fine striae in the dorsal fold. The specimens are for not separately by various forms. This material is in quite a different matrix and some of the fossils are as casts. It is in this matrix that the shells are which I found of Prof. Whiteways. Is it that they [illegible] occur in the past? In agglomerate? The once probably edge in that it is another involved shell. But that exactly the agglomerate is post-Middle Oomian. went back the same time to as the Middle Oyr. Rock but failed to make clue of it. I think I saw a D. [illegible]. If I did it in an involved Shell rather perfect removed from the Lower Seldenby.

Helms Island Office Creek and cyclamut hills about 10 ft. about office 12" Sentenced to 30" (June & July) office about flat mouth dam to about 2ft. little fault here. plain

Aug. 15 Wednesday. Left Montreal at 10 A.M. in Albany. At 11:30 on an Express train to Saratoga County. At 4 at Saratoga and after that Keeler Hotel, Albany. Spent the evening with Mrs. Drake very sorry to learn of this shameful traitor by Clarke. Aug. 16 Thursday. Spent the morning at the State Museum with Clarke of Hildreman. Clarke showed me to my German friends (a group of friends) who had come town. At the game where as I have been of this other man in the State Museum under Merrill. He also showed me his Chapman fauna material. The natural part, [illegible] it is going to be very large a fact to the god back at Polk County, it may give belief to that region. The Chapman fauna does not remind strongly of any fauna known it in Lower Wisconsin and nearest to Polk County.

Left Albany at 2.30 P.M. for N.Y. 1927. New Haven Aug 4-1927. Left at night for Port Daniel, Quebec to cord after the July visit of Studebaur Northrup. Aug 5 left Montreal for Quebec about 8 jar at 2.30 P.M. Left that night from Leris for Matepecdia Aug 6 left Matepédia and at 10.05 P.M. for to Port Daniel where Mr. Northrup was waiting for me. Put up again at Mr. Sweetmans home

Aug. 7 - 14 camping around Portland and Sascus. Aug 14 - 26 camping around Pierce. Staying at Pierce Creek Hotel until Mr. Bisson. Monday Aug 22-1927. Met on the road last evening Professor Perkins of Colby College. Today we saw with two ladies and a student were off for Sacs' Basin. Met Mr. Piterson a local streetcar man who knew Mr. Clarke. He took us to a ford [Richmond]

"locality in Barke sandstone fossils. It is one mile from the Baker Hotel up the Fork River trail to a fence north having a trail up the eastern side, and then north about four miles, and from there into the woods to the fork. Here occur loose blocks of the Barke sandstone reflect rock forms. Took away a few slabs. Attempted to make a collection from one, and I guard to try for $25-35 per t. Aug. 25-1927. Spent the day collecting along the Priest's Road to near Corner on the Beach. Got many of fossils at some place collected only Guthrop. A slab and Favorsites came beyond the school house at the fork of the roads. All Richmond

August 26-1927. Trolling at Bonaventure formation to smiths Perce. clay sea-fink. All the well rounded pebbles, as if stream rocks, vein-quartz, and very rarely one sees a small red Granite pebble, Jasper pebble, fairly common and some are rich in tin. Some of these hard pebbles exceed 4 meters in dia. All other and softer pebbles are sub-rounded, of older limestones and muddy sandstone. Saw many Perce Rock. Those of the rolls up to 8 meters across ad maybe layers. Many Bonaventure and red mica- ceres mixed with some cream-baked stream sandstones. The latter and Grey formation are not quite. Saw some current action but are lim

summer direction. All is clear of that nature origin. At a tree ornd a plant was seen. Color all a fire brick red. Aug. 27-1927 returned to Port Daniel and left for home on Sep 1-1927. Set to Raw Haven Sep 2 at ten at night.

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Aug 10 R.R. to Ottawa & Reti / 5.85 13 Hotel at Ottawa / 6.00 13 Portage .25 14 Ferry & street car .25 15 Hotel at Montreal / 3.00 15 R.R. to Albany / 7.65 15 Hotel at Montreal 3.00 15 Dinner in cars 1.00 15 Supper in Albany .50 16 Breakfast . 1.00 16 Room 16 Lunch - 1.50 16 Albany to N.Y. 3.60 16 Portage .25 16 Supper .75 17 Breakfast .50 17 Transfer to Depot .25 17 Hotel 1.50 17 R.R. to Washington 6.00 182.19 Standed in a bil Aug 25-190 for 171.57. Agreed to take two, as per instructions.

Balance 82.39 July 24 Lunch .50 " 24 Regular dinner to defray .50 " 24 Hotel at Dalhousie ✓ 5.25 " 24 Steamer to Gaspe' ✓ 4.50 " 25 3 meals on steamer ✓ 1.75 " 26 Hotel at Gaspe ✓ 1.50 " 26 Transportation Gaspe to St. Bernard. ✓ 2.00 Aug 1 Rugby transportation .25 " 3 Exp. of Grand Mere ✓ 9.25 " 3 Transporting to Gaspe' 109 ✓ 2.00 " 4 Ferry at Roque .10 " 5 Dragon hire to Grand Care 1.00 " 5 Portage .25 " 5 Hotel at Gaspe Basin ✓ 3.75- " 5 Farty Dalhousie ✓ 4.50 " 6 Breakfast & dinner on Admiral ✓ 1.00 " 6 Portage .25 " 8 Hotel Murphy Dalhousie ✓ 2.25- " 8 Dalh. to Quebec Montreal. ✓ 10.50 " 8 Portage .25 " 8 Breakfast on cars ✓ .85 " 8 dinner on cars ✓ .75 " 8 Stage of Quebec .25 " 9 Hotel Victoria Quebec ✓ 2.00 " 9 Shack & Portage .25 " 9 Luffer on cars ✓ .75 " 10 Breakfast in Mont. ✓ .50 " 10 Dinner & Luffer ? ✓ 1.00 " 10 Room ✓ 1.00 139.84

Expense account July 1 R.R. to Boston ✓ 12.25 1 Transfer baggage .25 1 Quebec to Boston ✓ 3.00 1 Dinner on train 1.00 2 Portage fee .50 2 Boston to Windsor ✓ 8.50 2 Berth to Garmouth ✓ 1.50 2 Dinner on steamer ✓ .50 3 Breakfast at Garmouth ✓ .50 6 Hotel at Windsor ✓ 9.00 6 Packing boxes (2) .10 6 Freight by N.Y. mails ✓ 1.00 6 Windsor to Halifax ✓ 1.38 6 Transfer in Halifax .50 9 Telegrams to McDonald .27 9 Queen Hotel at Halifax ✓ 6.75- 9 Transfer to R.R. depot .50 9 Ticket to Antigonish ✓ 4.52 10 Hotel at Antigonish Bros. ✓ 2.10 21 Expenses at Arisaig ✓ 15.55 21 Stage to Merigomish ✓ 1.00 21 R.R. to New Glasgow ✓ .42 21 J.P. for shifting bill .25 21 Dinner at Merigomish ✓ .50 21 New Glasgow to Dalhousie ✓ 7.30 21 Dinner in cars ✓ .75 21 Keeper ✓ 2.00 22 Return .25 24 Boxes, mails & papers .30 82.39 9.

195 cash 12 ticket. 197. 1/2 1/4 Expense account July 1 R.R. to Boston / 12.25 " " Hampton to Boston .25 " " Depart to Boston / 3.00

for instruction regarded to take into 27th April in the night showed me in first day after

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