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Tous les autres exemplaires originaux sont filmds en commenpant par la premiere page qui comporte une empreinte d'impression ou d'illustration et en terminant par la dernidre page qui comporte une telle empreinte. Un des symboles suivants apparaitra sur la dernidre image de cheque microfiche, selon le cas: le symbole —^- signifie "A SUIVRE", le symbols V signifie "FIN". Les cartes, planches, tableaux, etc., peuvent §tre film6s it des taux de reduction diffirents. Lorsque le document est trop grand pour dtre reproduit en un seul clich6, il est film6 d partir de Tangle sup^rieur gauche, de gauche d droite, et de haut en bas, en prenant le nombre d'images ndcessaire. Les diagrammes suivants illustrent la m^thode. 1 2 3 32X 1 2 3 4 5 6 /d REPOETS RELATIMO TO (r-y-^ The Albert Cannel Mines, th) i'hert Eailway, Shepody Harbour, and Mary's Point, New Brunswick. 'f^mmmm^' iwmmmmmmmimmm mw I III ipiip ■PlWPliP 1/ r ^ II / r l j ' * 1 i I, i - 1 1 ^j K^' ^^^^ illap or THE INTERCOLONIAL RAILWAYS, SHOWING THEIR CONNKCTION WITH 7TIE RAILWAYS OF CANADA AND or THE UNITED STATES OF AMERICA , AND WITH THE ALBERT RAILWAY & SHEPODY HARBOUR . ^ I i V f { li -IB I / z' TJEPOl^TS, &c., rchd'ing to (he \\a\va\x Cannel Mines, the Albert Hailway, Siiepody IIar- noiJii, and Mary's J'oint, New ]3ri nswtck. SIIKl'ODV lIAliBOUll, Insidp of GrindstoiK' Island, is capacious and safe, liavinir, from its southern cxtrrnnty at Mary'> I'oint to flu- UKUith of ftlu'pody Uivi-r, a harbour lim- of two uiili-s in lenuth 1)V up- wards of lialf a niilo wide", with from two and a half f<) full five fathoms water at huvest sprin/j tides. Insidi- tht' I.iiiht- house and IMary's rivf it is })r<)tecti(l from all winds except due S.W., which, howi'Ver, causes no stre//y (he reef hcnflnt/ doicn the yowjticst sed. The onlv suill in the harbour is from S.E., but is never suflicicnl to be cau>e of danger to the smallest craft. A lighter laden with deals has been known to ride out the severest <;ale in perfect safety. Shepody is the only low w.iter harl)our and place of refuije above St. John, 'i'he anchorage is exceiUnt. There is but little nu> of tide or drift ice in the harbour ; the strength of tide and run of ice bein<ij outside Grindstone Island into and out of the l*etitcodiac and Memramcook rivers. All persons acquainted with the navin;ation of the bay are of opinion that the erection of tlie wharves and piers necessary for the business of the Albert Uailway will reiidir SliejHjdy Harbour perfectly safe and free from ice at all seasons. N'essels lie safely at the wharves at Mary's Point, and depart thence durinfr all months of the year. The facilities which ShejKxIv Harbour ])resents as an orenu outlet of the railway system of the Ihnni/uon of Cdiinda and as an cntrefjot for the l)usiness of the vast interior, for manufacturinf; (beintr in the in)mediate vicinity of large eoaf- feld.s), for .stiiphui/dififf, for .s/tippin'j; ; for buildini; break- waters, piers, wharves, &c,, cannot be surpassed, jf (quailed, ji 1 1 at jniy oilur port in tlic Hav of Fimdv. 'I lie supply <>f w«>»i() jukI stoiu' on till' spot iiiul ill till' viiinity in praitii-iiiiy uiiliiiiitcd. Slirpody is tilt' fif'ftn sf (ii'ftiftifi/r on f let tit Ifir /Jlmitir for nil tlu' \ast iiit( rior travirsid by tin- (iraiid 'I'nmk and Intiiidldiiial railw.iVN, It is ncait r to <^;in lu c and ail ( anada l)y I K) iiiiIrN than liaiit'ax. and i>y /)() or (iO niiUs than St. John ; nnd is nothiiii; inlrrior to cither as a point of de- ])aitnri' or iniportaiion to or from any part of thr woild. As a naval and niilitary station for the Dominion of Canada, Shcpody pns>('SMs spriial ail vanta<r«. s. It is wrll in tlu; intt'ii<ir, and, havinj; hut om- narrow riitrart'c, tlu- haihonr can hi' compK't "ly fortilird at littli' co'^t hy difrnsivi' uorks on Mary's Point and (Jrindstonr Island. /\s an tini^rant port it is piohahly w itiioiit its ((inal in ."11 thr Dominion. It is in the inmu'diati' nriiihhonrhood of thi' rirli -iiii ii\iltiiral ronimiiiilliis wiiiih sunound thr Hay of ]''nndy and lis trihntaiirs ; and the lisht'rirs. ship-hnildiii;^, niininii;, (piarryin;:;, himhi'rinii'. and otiur indiistrirs whirh floiirish in all this riM-ion, oll'cr a yarirty of pursuits and ct-rtainty of i'm])loynu'nt to all classis ()f inii^rants froi • 'lu' nionifnt ol' thur arrival. Stafi'mviit o/' C'ai'tatn' ItoiiriiT Hissfi.t.. 1 nm a nntivc of Slicjiody, County of Alhirt, niiit now in my sixtieth year. I liavr t'tillowcd tlic sea siiu'i' 1 wns twelve yeiii's (if ime. 1 ('(ininiaiidetl a Nt-sscl tor twenty jeai> in the (•iiislinif trade in tlie \\',\\ ol Fiiiwly, ami have tor many years lieen a jdlot in tlie lu iid-wut«rs of the Hay. I am tlioroui/ldy well a<'- (jiiaintcd with the harlimii' ;it Miry's I'oiiit, and cdn^ider it the hot and safest in the i5:iy. 1 liave frecpn uted it at all tiines and seasons, and never lost ;> rope yarn. It is the only low water harlxmr and plaee of relive ahove St. .jolm, and it possesses all the aiKantagi's an<l re(|uisite.s for a lar^t! trade and hhipiiinj;. August 2Hth, IHCr. RoilKIlT Rt'SSKM,. Cai'Taix Gko. Wood, nf Shvpody. I have been for twmty-fivo years engaged in the eoastinsr trade in tlie Ray of Fundy, and am well accjuaintod v\ith the harbour railed Five Fathom Hole at the mouth of Shepody river. This is a safe and commodious Iniriiour formed by Mary's Point and Grind- stone Island. 1 have been for si.\teen years a Master Mariner, and durinji that period, and at all seasoTis of the year, 1 have fretjuented this harbour, and know the soundings as laiil down in the Atlmiralty chart to be correct. There are five fathoms at dead low water, immediately off the end of the reef running out 8 ipply of iutiiMlly "fifir for ink .'ind I ( '.-inadii lll.lM St. of (K'- •1(1. C'mi);i<I.'i, I ill the li;irl)()ur I' works liom MuiyN I'liiiit, iit llic v»>ry lowest tidw ; iind tlii' luii-horHKtt In in'ifirtly i»ft' fiiHii Jill tMiiclx, 'r.iKiin; till' rn'f /iH a tiMimliitiiiii, ii tiriiikwiiicr or pier I'oilld .'iiojly III' I'oiistrucli'il ut wliicli vt'^iilit iil' lurgu tuiiiittgi! I'lmlil loud mid diti'liiirgu Ut low WrttiT. I'lii' iiiii!iori»if«' (rrnnnd in di'i'p wnfrr in (if i«m|>lf rxb-iil for u lurn*' lli'i-f of v«'!<"«'l>i, ami I cim >.|m ik witli r"iitiil(iiri of itn urtiit i«iifi'ty. I 1/iy tlnrrwilti Tiiy M ■^'^rl ciilltd i| Aiiilurtt " durinx tlir i{ul(t of tlit- Jiid Aiiuuitt iiutiint, « Inch wiiM till- iiiot( m-verf within my ici-oll. rtimi. I wan hound in St. J. dm, hilt Iniiitj overtHkni hy the itiiU* 1 ran in tlii'rc for «hrltfr. Tlii' wind wim from till' iii(i'«t ix|H))*td ((ii.irtir, hilt I fouk ik injury; and othiT vi-jisrU lii*iivily ludrn riiili- out tiic ifm in itfrfci't M.iii'ty. I (-(iiisid'r ilii« harliour tlic hcHt in the Day of Fiiady. und motit i-oiivuuicnt for ihi" |iiir!'o*< 1 i(f f.\ti'ii>ivr tru li*. August 20i:., 1HIJ7. Ctf.o. WooiJ, lal in ."U (! of the Hay of )iiil(lin(r, •s wliiili nits and fioi ' the Cai'taiv W.m. Wood. 1 have bci-n for cijrhti'cn yean onin/cd in the. coast'nj^ trade in the Bay of Futiily, and am wi-ll a<'i|iiuini" ' with l-'ivi' l''ath'>:'.is hailiuur Sli»'|io(ly) I contirm tlu- lori'i.'o-iii; !<taliiiier i all juirlii'uli ■'. I havf laid liifu during a storm with niiwurds of tweii'y vessi'ls, i oni' oi which took any injury. William Wood. ■th yonr. I Iril a vessel e tor many ily well ae- and safest lost a rope .lolin, and Slalement c/ Captain' i\ A. Scott, of !f>'r Majesfifs Navy. I fully airn-e with Ciptiiin'- Rus-<ell and Wnod in thrir stati'iiicnts as to the oajialMlitics of iM^'e Fathoms llarhiiur. at llic mnutli of Shejmdy Hivor. My knowledge of the anehoraffe is iXtTWudUnnx the ncfiial siirreti ^)\ it, and from having: u>ed it for year?-, while pruM-eutiiiu llu' llydni.'raihic Siirvry id' that purl of the eou-st. It is, in laet. the only sufr aiiehora;;i' iii llial part of the Buy of Fuiidy uvuiluble at low ivatfr, and is much frei|Ueiiled in bud weather. P. A. Scott. .UHSKLL. the I?ay of nn Hole at mid Grind- ilurinjj that , and know ere are five unninc; out • lieport of ^\\\ CiiAULEs Komi, Civil and Mininii' Eii^^intHT, on Mincr.il Lands belonoino- to ('. J). Auciiiijai-u, Ksq., F.U.S,. \\\ Albert County, New Hucxswick. Tlie propi'rfy to whieh my attention was more partieularly directed consists of about (i.O'MI acr»;s of land, situated in a rich mineral district. It is further, for the must part, covered with a heavy growth of valuable timber of various kind.s ; and, when cle.nred, will constitute excellent farming land. It possesses, niore- over, jieeuliur facilities and advantages as regards accessibility and transportation of produce both by land and sea. Till most remark'ible and valuable products which characterize this part of your property consist in vast deposits of a highly bituminous mineral '•e>embling Ca.snil (,'()al, or more nearly allied to the Hoohkad mineral of Scotland, by v^'liich it is undoilaiil, and wliicli has been proved to be a most valuable niatfrial tor the production of iil'iniinatinL; and othiT oii.s an<! gas. You have already reieived iVmn various lonipetent, scientitic, and practical auiiioritits, ample rcjiorts, l)otli in regard to tlie quantity, ipiaHty, geological condiliiius, and econonut: value of ihis mineral product. These reports have been sul)niitted to me, aud iiaving visited the various out-croppings, and examined all the pits, shafts, drifts, and other openings, as well as the general geological structure of the region, I am enabled from personal (d)servation fully to verify and corroborate these slatenuuts. insofar as regards trie ijuantity, mode of occurrence aud facilities for uiinint;. 'J'heso observations, which include sonu' ini})ortant discoveries made subsequent to the i)revious reports, place it beyond a doubt that over a S])ace of at least three miles in length, by a quarter of a mile in 'average breadth, you have on your property an aggregate thickness of at least 'M) feet of the l/pst i/tinli/_i/ of rtnuirlitc, such as that submitted for ex- perimental examination by the various clieniists aiul manufacturers, aud reported to yield, according to the samj)les tested, from 45 to C'J imperial gallons of crude oil per ton. The country is undulating, and is intersected by numerous ravines, in which the beds or veins are found cnit -cropping several hundred leet above the natural drainage levels, thus atlbrding access and convenience for the extraction of the mineral by the cheapest system of miniiuj. The pits and other vipeidii^s nuule, although not prosecuted to any consider- able depth, are amply sutlicient to enable me also fully to verify the statements made in regard to the increasi/ii/ fhic^npus aud richness of the deposits, which may tlu'refore be considered practically inexhaustible. Although the structure of the formation on the whole is sufficiently regular to atl'Mrd amjile assurance that the veins will prove ti) be persistent, I found, oti some parts of the ]iroperty, indications of slight local disturbance, such as occur at the celebrated Albert Minus, situated a few miles to the east, aiul nearly in the same geological position, aiul which, in conjunction with other sigmticant circumstances, lead to the exjiecration that similar rich and valuable de|)iisit8 may, on nufe minute e\a'iiinatit)ii, be found on yiuir jiroperty. ConsiiU'ring the slight indications which led to the discovery of the Albert Mines and the similarity of conditio is here, as well as the actual ociiurrence of Albert coal, although in a more dill'used form, on your prcjierty, such an expectation seeni3 reasonable. A considerable proportion of the territory comprised within the property is underlaid by rocks of the Metaniorphic Devonian age, which, in New Brunswick are rich in ores of copper, manganese, and other valuable metals. Rich indica- ti(uis of cooper ores have been actually found in a vein on your property, and niani.:ani'se has been mined in the ueiiihbourliood. Of late years the abundant sujiply of petroleum from natural springs has greatly restricted the production of oils by the distillation of solid materials. There are, however, in view of the prol)able largely increased demand for crude il as iiji'inl f'li.el, and iov (/as manufacture, iS:e., many reasons for bidieving that, with so rich a material and in a district so favourably situated as yours, this branch of manufacture, if extensively, systematically, and economically carried out, will com|)ete successfully even with the natural sources of supply, which are at the hot jireearious and generally involve much expensive transportation. For the nianulaciure of illuniinalin;/ f/a.s, the better qualities of ytnir cannel appear, from the reports and from careful estimates of the cost of mining and shipping, to he fully capable of bearing the expense of transportation to the great cities on both sides of the Atlantic, while still yielding a very handsome ])rofit upon the optTation. The tuuber with which this property is densely covered consists of maple, heach, and birch for barrel-making, and fuel ; spruce, hemlock, tir, })itch, j'lie, aud li:i<;mata<- for ship -building and ordinary building jnirposes, railway ties, bridges, \c. The fore.-ts have been for the most part untouched, and many of the trees ha\e consequently attained a very great size. 6 )st valuable id practical , gt'ological •|iorts have )ltiiigs, and the general vation fully ic (juantity» liich include ts, jilaco it jy a quarter thickness of ttfd for ex- nd reported JUS of crude Ls, in which the natural :tion of the ly consider- l; statements osits, which y regular to I found, on Lich as occur ul nearly in r signiticant ible deposita ConsiiU'ring ini'S and the Albert coal, tation seems ; jiroperty is !v Brunswick Rich indica- roperty, and springs has d nuiterials. id for crude lieving that, s yours, this cally carried ly, which are rtation. your cannel f mining and tation to the ry handsome ts of maple, , pitch, 1 ne, railway ties, and many of THE ALBERT RAILWAY AND SKEPODY HARBOUR. The value of these various propi^rties will be very niateriully enhanced by the construction of the Ai.hkrt Cuuntv Railway, designed to run from a l)i)int on tlie European and North Aniericim Railway to the lieat and most con- venient harbour on tlie Bay of Fuiidy in Albert County, such harbour being undoubtedly that formed by Mary's Point and Grindstone Island (Shei'ody) at the mouth of the Petiteudiac and Slu'poily rivers. This Railway wil! intersect tiie rich nimenil districts seme of the features and resources of wiiich 1 iiiive endeavoured to describe ; and, besules opening up a rich agricultural district, will connect by short branches with the Albert Mnies, Ililsborough Plaister works, &c. It will prove a uio.-t valuable adjunct to tiiu European and North American, and especially to the Intercolonial RaUway, which wid be tapped at its northern terminus by the All)ert Railway, the whole length of which to Siiejiody Harbour will be about thirty or thiriy-tive miles. Tue Harbour of Mary's Point (^Shepody) will artbrd a safe anchorage for a large fleet of vessels with at least twenty-hve feet of water at the lowest tides, and IS said to bf o\)fi\ at all seasons; wlnlv the adjacent sliore is highly favour- able for the estat)lishment and growtii of a large town or city. The advantages of such a harbour, in immediate connectiou with the Inter- colonial Railway can scarcely be overestimated, affordnig as it does th(> most direct point of shipment tor the rich products of the western and central parts of the Dominion of Canuda, and for the exiensivc lumbermg districts of New Brunswick. At the same tunc tlie peculiar mmeral and other resources of the district, for which an extensive demand will probably spring up in the western cities, must contriLiute largely to the return freights. Tiie construction of the Bay Verte Caiud, between the Gulf of St. Lawrencj and the Bay of Innidy, is only a question of time, and when eft'.cted will add immensely to the importance of the proposed new harbour and railway as the nearest available point of shipment from the intercolonial Railway and New Brunswick to iLurojie. Tiu! Albrrt Railway, Tor about two thirds of the distance, will pass through a country peculiarly (av( urable for the construction of such a work. The remain- ing tiiird — being the central division — although it must traverse an elevated and undulating region, presents no unusual engineering dithculties. The steepest grade will mii exceed sevenry feet to a mile. It is conridently anticijiated that the Government subsidy of ;. lO.d';-) (ten thousand dollars; per mile wdl amply sutlice to defray at least one half of the cost of construction and equipment of the whole line. CHARLE.S ROBB, Civil aud Mining Engineer, St. John, N. B., 21th September, 18G7. Ao/p. — In view of the great discoveries made since the date of previous reports, it maybe thought that I under-cstimate (juantity ; but it should be borne in mind tliat I only take into account the very best No, 1 quahty— C. R. Sir William Logan-, tlic chief of tlie Geological Survey of Canada, savs: — I consider Mr. Cliarlcs Rol)l) a iv iblo milling engineer. He is nircful in ascertaiiiiiii; his lactn, gives tiiem ucci, lely, and stutes his coiioUisions con- scientiously. Report of Kdwakd Wadham, Lsq., C.E. I am well ac(|iminted with Mr. Archibald's property called ]Mary's Point in the Albert County, New L?runswick.whii:li 1 visited on two occasions, and care- fully examined and surveyed. It is a ju'onioiiiory, jutting out into the Bay of Fundy. and, with (grindstone Island, forms, as I was well assured, the best and safest harbour in the Bay of Fundy. My attention was particularly direi-ted to the valuable Quarries of Freestone whicii this ]iropprty contains. Tiiey consist of various beds of sandstone of uniform texture, and very durable. There are two colours, olive and light red, very ple^ising to the eye, and much prized tor statuary and monumental purposes, as well as a building material — I saw several buildings in New York, Phdadelphia and other cities of the United States and tlie Provinces built of stone from the>e Quarries, an<l heard but one ii|)inion of its excellent quality. At the time of uiy visit, there were about <Mie hundred men eni'doyed, and the Quarries were well furnished with the needful appliances for shipping from ten to tifteoii chou>and tons [ler annum, and the cpiantity might easily be largely mcreased. The protits, as estimated by the manager and others, were f3'H0 |)fr ton, and my inquiries at the time led me to believe that they were not exaggerated. Mary's Point, moreover, holds a commanding geographical jiosition with reference' to the general trade and navigation of the Bay of Fundy, and 1 have never seen a place better calculated for the sea terniinm of a large system of railways. The great extent of the "foreshores," owing to the exirai'idinary rise of the tide, make it most eligible for ship-building nd extensive manufacturing operations ; and the Quarries on the spot, and cheap timlier and wood in tiie neighbouriiooil, would render the building of wluirvcs, piers, warehouses, &c., a matter of trifling cost, compared with other localities whicli do not possess these advantages. The excellence of the harbour and the i/njie(as given to the trade when Mary's Point siiall be connecteil with the railway system of the Dominion of Canada by means of the Albert Railway, will necessarily attract population and enter])rise ; a<id a more convenient xiie for « larfje .^cajwrt tuicu with all needful accessories could not easily be found in any country. Dalton-in-Furness, February, 1SG8. EDWARD WADHAM, C.E. /• Dr. a. a. Hayfs, Slate Aasai/er, Boston, Mass. In former Reports on the Cannelite of New Brunswick, there was an omis- sion, to which 1 will now call attention. 1st. Cannelite contains 55 per cent, of jiure dry Albertite, and, on an average, 55 per cent, of Albertite aflords G2 gallons of Oil as it is worked in the uianufuetory. cal Survey e is rarcful in iclusions con- 2iul. Wlioii Cannelito is distilled by t.lie side of Albertite, in the same wa)', ('Hiuielito will yield CO standard gallons per ton, while Albertite produees lOo gallons. 3rd. I found by comparing statements made by two Companies working Cainielite that the yield exceeded GO gallons per ton. 3Qth January, 18CG ,E. lary's Point in on.f, and care- ito the Bay of d, the best and s of Freestone af sandstone of live and light d monumental in New York, vinces built of lent quality, it-n eni'doyed, ■s for shipping ily might easily ml others, were that they were 1 ])Osition with Fundy, and 1 ms of a large owing to the p-buildiug nd the spot, and. the building of )ared with other the trade when he Dominion of t popvilalion and ! town with all Dii. AxDKKsnx', rrofcsM)!- of Clieniistry in thi' I'nivorsity of Glasgow, reports as follows : — The Brown Sample, when heated in close vessels, gave : — Volatile Matter IG-.")G ^ r Fixed Carbon -l^S ^°'^''' \kA\ 48i)G In the experimental Gas Retort it yielded 10-1\10 cubic feet. Illuminating power, when burned in the Standard Burner, consuming ') cubic feet per hour 30 candles. Absorption l)y Bromine -'"' pcr cent. Specitic gravity of Gas O'G.'jH. This INlineral is of a remarkably high cpiality, and gives a Gas equal in Illuminating I'owcr to that obtainetl from the best qualities of Cannei Coal. Thomas Anokrison. Uuivcrxifj/ of (tlasf/ow, ?.Qth Xovcmbcr, IHGT Cannei of the " Brown Sample " above referred to exists in immen«p quan- tities, and the resident agent states, that " the whole hill from the bottom of ravines on its eastern and western slopes to its summit, an elevation of -100 to .•jOO feet and a miie or more in length, appears to be a solid body of Shales and Canncls. The veins rise regula- ly with the slopes of the lull on either side, and have precisely the same surt^ce indications at the top as at the bottom " — and further, that the mineral rapidly improves as it is sunk upon both m quality and thickness of vein. 3IIAM, C.E. , Mass. ere was an omis- d, on an average, ; is worked in the Mr. Ev.\xs, of the CHAUTERi-.n (iA> Company, experimented with two varieties of the Cannemtk, and reports that he found them both v.ry good. One sample gave an illuminating power of 29 candles. Th.' other gave ;i7'7<i. candles. Condensation by Bromine 2'J per cent. Mr. Evans reeommeni.s the conversion of Shale into Oil on the spot as the most convenient and economical i)lan of supi)lying for Gas purposes. Dr. Franklano, F.Il.S., in his conchnlins; lecture on Coal Gas, delivered at the Rc.al Institution, on the 2;ird March, 1SG7, referred to the New Brunswick C a NNKi.iTE as a very valuable Gas material, yielding Gas exceeduig 'M candles illuminating power. I'* Mr. Joshua Merrill, Superintendent of the Downer Kerosene Oil Company of lioston, Massachusnetts, reports: — A sample of Albert Cannelitc, placed in my hands for analysis, contained : — Volatile Matter 4G-60 Fixed Carbon and Ash 53'40 10000 The above gives a very large luminous flame, and abundance of Carbon in burning. It yields of oily liquids 835 lbs., and, making all allowances, I have no hesita- tion in stating it safe to depend on a yield of 75 gallons per ton of crude oil of excellent quality. See also, elsewhere, reports of Vernon Smith, C.E. ; Dr. A. A. Hayes, State Assayer, Mass. ; Professor Hind ; Dr. Doremus, of New York ; M, Cogniet, of Paris ; and others. ■# I Downer reports: — nntained : — ;-60 •00 of Carbon in ivc no hesita- i crude oil of :.E.; Dr. [ind ; Dr. id others.