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/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 
 
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 ^ 
 
 
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^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.