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('. KKKFFH, ('.M.(i President. •'rULISHED. BY OHDEU OF TIIK SOCIKTV. IN ADVANCK OK ITS ANNUAL VOLUME OF TRANSA(rriONS. ON ACCOUNT OF THE GENERAL INTEREST IN THE SUBJECT. Ill h< 111 til III "i; n.: I,v !ir •Ik J- M I iipi is J ['li« its irif.f the Uf)V m\\ I'lor siri] I'KKSIDKNTIAl. ADDKKSS (anadii with a. small |i(>|tiilat ion and insuHicicMt ('.apital hii< riovorthe- ly!«s lu'ld a loivinost position in the products of t\u\ Korcst. and the Fish- ( ri<'S. as well as in tlir (piality of those cereals and I'rnils which attain their hif,diest dev<'lopinent in a northern latitude. In live stock she has not suirered hy comparison with any other portion of this continent, while in dairy products she is })rc-eniincnt. If she has not, until re- cently, nuule much pro^M-ess in mineral development, it has heen more Irom want of money than of mines. If ^hc has hecn lonjr in attaininettle(l country, the smallness of a iiome market, and the competition of ^xrcattr capital and out-put, and therefore cheaper |>ro(iucti(Ui elsewhere. Amongst the many partially developed resources of Canada, perluqts there is none more widespread or iimre fai' reaching in future results than her unsurpassed Water I'ower. The \alue of this has Ix'cn enorm- eiisly eidianced, first iiy 'he expansinn oi' the Wood Pulp manufat't lire, ■..n.\ the introduction of eh ctro-elieniiral and metallurgical industries for which this country jtossesses the I'aw material: and, more recently, !iV the revolution which has heen liroiight ahout hy success in transmit- !ing the energy of water falls, from rem ite and inconvenient positions to 'li(>se where the work is to he done. {electrical transmission itrings the power to the W(uk, and when the [Time mover is water, we have the cheapest power, and perhaps nearest a|>proach to perpetual motion uliieh it is possihle to ohtain; — one which IS always " oji tap."" and, like gravity, maintained without cost and aj)- plied without ors. The frontier, where nui already occupied liy the l-'reuch, Wius neces .sarily rapidly >ettled in the tirst place hy the jioyalists of lll»i, whn could mil >taud upon the urdei' of their departun? aftt'r their honie-- were rontiscated. These found ihe rivers their earliest friends from whence they obtained the liieans of t;lielter and of eiuploymont in th ■ (»nly industry l»y which uimiey coidd then l)e obtained, viz, the tloatin<; of tindx'r and potash to Montreal and (Quebec. Over a leuiitli of seviM'al thousand miles hetwi'en Lalirador and Alaska and over a width of sevei-al hundretl miles, there is an almost continuous t;e of their Hood waters. 'i'hi> power of storajre has been larp'ly taken advantaire (tf by luud)ermen to retain the needed suppl\ foi' their SpiMuji" "drive" into the main stream. In many |)laces th outlet from the lake, or the connection between a chain of lakes, i» a narrow cleft in rock where an inexpensive vhile the former are navijiable for thousands of nules ami are thereforf witlunn. water j)ower. Those ^n'eat wi'stern rivers How upon a uearl\ uniform ;frade of a few inches per mile, whilst the St. Lawrence an I its tributaries art' interrupted by Kapids, Chutes and Cataracts, airordin.: a ;rrcat variety, (juantity and (juality of Water I'ower. in the I'nited States, between the Atlantic coa.st ami the l{ock\ ]\lountains, as far south as the Gulf of Mexico, and as far north as th ■ Bakota.s, (with the exception of ])art of ^!ew Y'ork and New I'jijj^landi there is an entire absence of lakes; while throughout Canada, north e! the St. Lawrence and stretching northwest toward the Mackenzie Uivei Basin, these are innumerable, in fact have never been numbered, ani thousands of the smaller ones have never been represented on any map The upper sections or sources of most of the Canadian Kivers ar^ chains of lakes, occu|)ying in many instances the greater portion of th • water course. These head waters are often upon nearly t'»e same eleva ictors ill till" of iipitroiU'li r tlic oxi)loi ami till' fill IS ()|)OIlt't" r. Iti, wli" tluMI" llOUlf- rriends from ^iniMit ill til-' . the tloatin- ►r and .\lasl<;i st contimiou- Tied outliiu'>. isui;^ I'acilitif^ •aixo lias hciMi leedi'd supplv iiy places til II of lakes, i> ai'k the watei aiiatla ditVe' their tril)U- iths, orahov ■ led tiei'tion> are therefor' •oil a iiearl\ iawreiice an I •Is, atfonliii^ the I{oek\ north as tli' ew Hnjjlandi (la, north i>t ikenzie Kivei imbered, anl on any map n Uivei'8 ai- ortion of th ■ i same eleva lion and interlocked uitli the suiinrs ,,r ,,(hei- rivcr> flowiii^' ia opposite or ditVeieiil directions, and separated hy narrows necks of land at a low e(tions, of ice covered lakes and of broken water in rapids, which may cover miles in extent, as well as at chutes or cataracts with more or le>s open water ahovi' and below them. it is an interesting (piestion for s})ecialists to determine what ell'ect. if any, this often large percentage and almost general distribution of ojien water during the coldest weather ( of which every stream large or small has a portion) may have in modifying the extremes of tempeniture in tlie-e northern latitudes. When all the ground is frozen solid and covered with a deep mantle of snow, extending over the lakes and check- ing increasing thickness of their ice covering, large bodies of water are impounded and maintained at a temperature above the freezing point, although there may be lifty degrees of frost in the air, and are constantly poured forth into this frigid atmosphere. It is concer vent to lier siij>|iresfc;t'ceiid. tlirou<:h the Laurentian rejrion. from t'lexations of ISOO to lOdO fee' ahove tide, and deltoiiche within a (rw miles of e:ich other excep' immediately ahoiit the Sa^'uenay. In many cases they hriii^- their prin (ipal cataracts very near their outfall, notably in the case of the fanioii- l-'alls of .Montmorency, which. lea|iin^- directly into the St. Lawreiic' from a heifzht of '.TiO feet, are utilized to li^dit the strtM'ts and drive tin tram cars of Quebet'. Somewiiat similar condititms exist on the soiitli shore of the St. Law ronco until the K'iclielien river (the outlet of Jjake Champlain) i- rcaclu'd. where at Chambly. water ^lower is about to bu used to send lb' electric current into Montreal, in comiietition with steam, and with .i similar water power from the Lachiiie Kapids. The divide between the St. Lawrence and the Ottawa is studded with lakes west of the liideau Canal, a ]M-incipal outlet for which. — on lb' ^,),,th, — is tbe Kiver Trent dischar<:iiig into the Bay of (^)uinte. w ith lar<:' mills and much undeveloped water power at its nnuitb: and on tie north, some balf a dozen important tributaries discharging into th' Ottawa. At Sault St. Marie, a water jwwer canal fed from Lake Superior sup plies the largest pulp mill yet erected in Ontario, and a similar work a' tlie Lake of the Woods (which lake is 1000 feet above tide) gives powef to the lar<'est flour mill in the Dominion. The waters of the Wiunipe,: (•«'/('S, wlllli s littld upon (I ice liflitw. . 'I'lif latt'Hi ciirs M> ti'i' 1 the iiliiHt- ■ the cast' in ill •• illU'luM - •li is said til (•(tlllC t'l'l»/.*'Il. thfin to il- • imiii»uii(U') dexMiid ahnill .'KIO feet, lUl- iiscd. into W'iniiipe;,^ Lake, adjoininir J.ake Maniloha, Ironi whence the water system extends In the Saskalehewan, and thence via Athahasca, the (ireat Shivc and the (Jreat Bear Lakes, to tl»e Arctic circle. No ret'erence has he«'n made to the hmg estal)lish(H| water power in the older districts, on the Sa^Mienay. or those hetween Montreal and l^uehei;, and upon the Ottawa, nor to the more recent and extensive pidp and jiapei- estahlishmcnts; — it l)eini al the Lake of the Woods. 'I'his province is hy no means delicient in water |»ower, although it has heen little used as yet where iiunes are on high levels, and hecanse steam could he more n^adily api)lied. On the i'llicr hand, it is the only Province m which Hydraulic Mining is in operation: and where g(»ld is found in ipiantity sutlicient to warrant the -real Ko(»tenay, water wheels, with or without electrical transmis- --ion. ;irc necessary foi- water power, in order to mine, pumj). and crush I lie Liold hearini.;- rock>; hut in the Carilioo district, water j)ower i.s aj)- ;ilicd in the simplest form, without wheels or wires, hy direct pressure from a no/zle. as is done in Ottawa from a lire hydrant. \\ idle the mountains south of the Canadian racilic- Railway are rich 1 metallic Vein- the region north of this Kailway extending into the Arctic Circle, .ippears to he a vcritahle land of llavilah. a conlinuou-; " I'huer " gold fudd, in which much of the precions melal is to he oblain- <'l hy Hydraulic mining, wherever that is practicable. 'rhi< gold field, over a thousand niiies in extent l)etween the Fraser and Yukon KMvers. and of nmuscertained width, has heen exj)l<>ited at (arihoo. (from whenc(> lifty million dollars ha.>« heen taken), at Ca.ssiar and Omeinca. and recently at Atlin, all in British Columbia; — a.s well a- in the far famed Klondike, in the Yukon district, said to he the richest gold field in the world. Water, in whatever way it is used, i.s necessary to the recovery of this L'dd. hut in many places water power alone will profitably unearth it tmm its hitlden recesses. This is collected in quantity from lakes, and II sevoirs on the high levels, and carried for miles hy ditches, aqueducts and Humes, to the banks of a prinu'val, dc^serted river channel, at the bottom of which, under forest covered clav hanks, lies the auriferous ■r?' 'I i->^ ?* A. I i J J vi ( --» pravrl stiuMrd \\'\\h lunildrrs jiiid rest ill;: <>i> the bed rock, rnd*'!' ii head (if iil»(»iit .■?(•(» fret "six inch nipid fire" hydianlic puns arc pointi'd i>;:iiiiist tlic l);ink. Itrcakiii;; dnwii llic earth, uproot in;.' trees, scattt'nii;.' l>oid»h'rs and wa^hiii;: out the gold— which reinuijis in the traps >et for it ill th«' Itottoiu of the sluices after all clsu has been carried oil' bv the power iif tile water. 'i'hese "machine ;:iiiis ". called *';,Mants" and " ...»>nitors ". arc models of -implicitv as well as of ingenuity and elliciencv. While work- in;: tlicv ari' ;:i'eat roii'^inncr- of Wiitcr,- and can only be used when llie ;ii'oiind i> unfrozen, but this season is p-nerally suHicient to u-e up all the w.itcr which can be collected at the necessary elevation. It ri'tpiirc^ at bust two nu'ii to hold and direct the force of the is- suin;: stream from an Ottawa lire hydrant, but a boy can direct the movement of a stream, twenty times ;:reater in ([uantity and lifty percent i«tron;:er in pressure, as it rushes forth from the no/zle of one of these '* ;:iants ". — which is li\<'d to a loaded jdatfonn, and moved forward as the bank in front of it melts away. A thin shoi't tube, of lar;:er diameter. pr(»jects bey(»nd the no//,le ti> which it i> fixed by trunnions, sd tjuit the inbe can i»e moved indepeiul- ently, bdili li(iri/ontally and vertically, to t<»uch the issuin;;: sti-eam. which immediately recoils from the obstruction, movin;: the ";'iant's" no/./lc in the oppdsite direction. 'IMius a boy " behiml the ;:un " can (oiitrol its m>'Vement and compel the " ;:iant " to fall back upon his ('wn resources for motive power. li()!;sK iM)Wi:«. It is impossible t(» ;:ive anythin;: but an approximate estimate either of (|uantity or value (»f the available water ])u\ver over so vast an area, because the first would involve the survey of every power site; and, as 1() the second, the value be;:ins when the power is wanted. All which now »an l»e done is to state tiie conditions and eiubnivour to estinuiti' the (piant ity. hypothetically. What is needed for an e-tiimit'' is tlie (| uantity of water a.'id the amount of fall wliich can be relied upon at the site for each |»ower. To ;:et the first, a nieasiirement of the mini- mum flow at each p(»int wiuild be necessary in low water years, and fo' the second, sonu' local knowled;:e as t(> river levels, back wafer, etc. In the absence of such surveys we must fall back uj>on the averaj:- rainfall of the whole re;:i()n as far as that can be procured for any time, and assume the proportion of this precipitation ( ()f rain and snow i which, after de(lucti(»ns for evaporation, the demand.s of vegetation, or infiltrati(»n. would reach the wheels. An allowance nnist also be mad ' for that porti(jn of the rainfall which may he carried off in floods. I n(l«'i' ii III'. Ill arc |»i»intiM| 8, scat t frill;; traps M't fur •d olV by till- [lilurs ". lU'i' Wliili' wi>rk- .' usi'tl uhfii nt t(» u-e tip atioii. CO of till' i>- n dirt't't tin- lifty |>iMT.'nt one of tht'Sf (1 forwiinl ii> tlu' lli>/zli' ti^ ('(I in(l.'})tMi(l- ;uiii^' .-IrtMin. \\v " tr'iiiiit's ■■ H' fiuii " I'iin k upKii \u^ iiimtc either vast an area. site; and, a.* \<1 ('iidt-aviiu:- r an (■■itiiniit'' rclii'il upon of thf mini- ciirs, and fu" iter. etc. [ho avi'raiz or any tinn'. and snow ) |('^C'tatii)n, or Ibo l)e mad 1 floods. Tlir iirra o\cr wliiiji fjiis prrcipilalicdi would lir in iciK li lor water ()0\vrr purposes, wi.nlil »iiil»ra(e nil the main land of ('iiiinda suutli uf the St. Law rente, as well as all n(U-(li of it in the Ht. Lawreneo valley, and !-" iiiiieli (if the llirdson hay watrrshed as ran hr utili/ed, oi' inipui'trd liy I ran>inissiun. As re;.i-ards the powi r of the water thus est iniatt'ccrtain- et» feet, a* in the (ase id' the I'Vench river wlii(h has Lake Nipissins.' for a mill p(Uid. >m* riso to |."i(Mt feet or more as at the riveis nelow .Ant n "stj. In the case of tin- Kreneh river (which is the lower part of a. lon.j(r stream) we have surveys, and know that its whole fall can he utili/rd, as would he done if it is made navipdd ■ hy locks and dai.is. In the others (wIk" ' ' surveys have heen made) some will il»c more or less like I-'rciich river, while at others (uily a |»<»r ion of t'le total fall upon tlieni may he pi-olitahly nlili/ed. The most valuahle will he liM»se which, liko M(udni ^'reat an extent of unoccupied territory. .Assuming' therefore an averap' annual pn'oipitation of twenty-four iiiches and takin^^ o!ie-half (d' this as available for water power, every ten sipiare miles would yield an average of nearly one horse power for (very foot of fall. .\ million sq\iare miles (and there is mnch more) wonld give nearly 100.000 Horse Tower for every foot of fall: As there vv<»uld be s»veral hundred feet of fall whieh oouhl be utilized our water power nuist be immense, — and eommen- urate with this conntr}' in other respects. The above applies oidy to the tributaries of the St. I^siwrenee and the Ottawa. anlt; foot, in not incliulod, iK'iii^ holow the level of the trilmlaries. We have mea-sureineuts of the tlow in hoth the St. Ijjiwrence and the Ottawa in cul)ic feet per soeond, tis follows: c. ft. per .see. Tn St. Clary's river, outlet of Fiake Superior SO.OOO ]n St. Clair river, outlet of Lake Huron "i'i.^.OOO In Xiajjfara river, aliov(> the falls "^.MJ.'t.OOO In St. Lawrence river ahove the rapids.... .'JUO.OOD In Ottawa river, ahove Lake of Two ^lountains ;{.*>.()()() Catiada's share of the St. Tjawronce water power from Tiake Superior to Montrciil would he about ten million horse j)ower. Canada has half the water of the St. Lawrence from Lake SujK'rior to Cornwall, and all of it between T^ake St. Francis and Montreal; hut only a ]»ortitm of this half could i)e utilized, — and this would ap))ly more or less to the Ottawa and other rivers, when? all the power could not be utilized without an expenditure probably beyond its value. The power at Nia«jara has been ostimatiMl at seven million horse power, from less than half of the fall between Likes Krie and Ontario, Imt the How of the \iat bound craft, tlnis incidentally compen>atinir for a vi(»lation of canal maxims. I While \vat''r power was at lii->t the only substitute for tin* windmill in new (onntries. and its economy as well as superiority has always been reco>;iii/.cd. several causes have contributed to limit its more ^eiienil ap- plication. Kebd'c the invention of the turbine in the llrst half of the present centui'y heads exceedin<; about seventy feet could not be utilized on account of the comparative weakness and excessive cost of wheels of lar;ie diameter, in these days of structural steel, and *' l'\'rris " wheels, this ditliculty could he overcome", but. with the turbine, the conditions ai'e I'eversed, tile higher the head the less tliosize and cost of wheels, so thai the most valuable water powers were the nu>st cheaply utilized in this l'esn(!ct. 11 Mici' and t.lie •MUil'l'IlHMlt luM'tt), on ac- currcMt ('>- wintliuill III lilwavri l)('< economical power is tra.nsf«'rred to tlu^ work, ovi^r many miles of distanc(\ upon a single wire. AVithin the last, ten years high voltage electricity has been firmly es- tal»lish('d with annually increju^ing power of exten.sion, and this has brought Canada into the tirst rank of economical power producing coun- tries. Water is thus represented by a power to which it can give birth, but which is superior to its own, in that, where ever transplanted, it can do nearly all the parent j>ower conld do, as well a.s give light, heat and greater speed: moreover it has given rise to industries only possilde with abundant cheai) electricity. What is more important to ns is that such industries are those for which Canada possesses the raw material, but wliich, without water power, she could not engage in. There are important industries in which we have for some time utiUzed Matei" power, for which eh>ctricity is not indispensiblo; but which e(|ually re(|uire large amounts of eheaj) p.iw«M'. and are capable of indefinite ex- tension: but while tlieion of inestimable value in many situati<»ns; while, for lighting and lieiiiing |iiii'poses, water power is invaluable to ail. lleretotbre we have cut our spruce into deals and expi»rted it t) I'lurope. and more recently into pulp wood and exported that to the I . S.; hut, manufactured by our water power into pa[)er, the raw ma- terial would yield this country ten tiiiu's the value it is now exporter which has hap|)ily been described a.s " the most inniantic form of energy" by Win. Henry Pr«'ece, C. l\. F. K. S., in his iccent address a.s I'resideiit of the Institution of Civil Mngineers. ^ i :l p ' ! ) J Vil 1 12 Tnnstmu'li as tlio cost of production of electrical oikm-^'v «lc|ien(ls upon continuity of (Uilput. water power nnist ])e the ideal ono for tills purpose, at least until souu' cheaper j>o\ver is discovered. In some places when^ steam is now used for electric li<:ht other industries have hecn added to seeui-e the nu)re continuous use of the j)ower in daylij^ht hours. The oidy (piality in which any deticiemy has been exhibited by elec- tricity is for li<:ht house })urposes. a hsser ])o\ver of penetration in fofrs. in which n'spect it is iufi'iior to oil or rcsent year, been more than compensated for by the successful appli- catioji of •' wireless tele;:raphy ". by which, in any weather, communi- cation between the ship and the shore can be established. The shores of the St. Lawrence from tlu' Atlantic to the Ivakcs are liiu'd with water ])ower which can l»e used t() lifrht. in fair, or protect, in foul weather, the passiufi vessel; to ring the bell or blow the honi. When water is applied for light and })ower i)urposes its economy is always the important factor; but it is chiefly to its value for electro- chemical industries that Canada will look to reap the greatest benetits. because, in these it is not merely a question of competition of ]tower producers. Imt one in which intense electricity has the monopoly, and in the eajie of some of them, as in the prodiution of aluminium, calcium carbide, carborundum, etc.. their existence de|»ends upon ample supplies of an intense electric current. f(»r the generation of which abundant and cheap wati'r ]tower is indis|tensible. Touching electro metallurgical proces.ses Mr. I'recce says : '* Every electrolyte re(]uir<'s a certain voltage to overcome the atliuity between its atoms, and then the nuuis di'composed. per minute or per hour, depends solely upon the current ])assing. The j)r(»ccss is a iheap (me and has become general. Three electrical 11. 1*., continuou>ly ap- plied, deposits !(► lbs. of ])ure cop])er every hour, from copper sulphates, at the cost of one penny. All the cojtper used for telegraphy is thus ob- tained. Zinc in a very pure form is extracted, elect rolytieally, from (hloride of zinc produced from zinc blemle, in large quantities. Caustic soda and chh rine are ])roduced by similar means from common salt. The |)assage of electricity through certain gsu.tit' eoiiunon salt. inie«l by their enee the ari' luxitt'. IMios- sphates. Cal- )ortaut iiidus- eoal, of jj^ood cheaper than Eastern arul Western Canadian coal fields arc separated by thousands of niilcs, but water power is abunorhood, they may ^dve rise to electro-chem- ical and electro nictalliM-^dcal industries without the intervention of water power. The comnuTcial product i(»n of calcic carbide (acetylene ga»s), by elec- trolysis, is the discovery of Mr. T. L. Wilson, (a graiulson of the late Jlon. .1. ^r. Wilson of Salttleet, Ontario,) who has established works on the water ptuvers of the Welland Canal and has shipp<'d this product all round the world. The electric prodiu*i,ther field nearly as widespread a> our water power in whidi electricity is destined to play a most impoHant role, and this is Mining, which is now spreading over the Dominion with the same rap- idity as the utilization of our forests for pulp and paper i)urposes. Over this area minerals have been discovcn-d and in many cases tested and succcssfidly worked, and from recent results we appear to be on the threshold of r<'nuirkal)le developuu'nts in this directi(»n, especially as so snuUl a poll ion of so great an area has been j)rospect«'d sutriciently for mining ptirposes. F(»r power purposes alone, electricity is invaliuiblo in mines, and its ninlfifarious uses (as enumerated by Mr. I'rwce) ar<' " for moving trams and for working hoists: it lights up and ventilates the galleries, and, by fium|>ing, keeps them free from water. It operates the drills, picks, stamps, crushers. c<»mpressors. and all kinds of machinery. The modem type of induct i«»n motor, having neither brushes nor sliding contacts, is free from sparks and free from dust. Klectric energy is safe, clean, con- venient, chea|», and produces neither refuse nor side products." The Canadian mining districts are well supplied with water power, and all the wonderfid effects of electricity are available for us upon a larger annore <'cononucal scale than elsi'where. In connection with this abundance of water power, and from the fact that a large ]>roportion is at present situated remote from present rail- ways and present setth'Uients, the (piestion of pn)fitahle limit of elec- ^ 1 . ■ I mi ^%M I r J U Irionl transmission is most imj^ortant, — if in(1o(Ml it ho now possilbe to jmt a limit on anything eonnoctod with oh;ctri(;ity, with or withont the nid of a win*. It', as ro))ort(' t.he greater part of the water ])ower npon the two watei-sheds north of the St. Jjawrence River. Professor l''lihn Thomson says " I'p to the present time it was prac- ticable to transmit high })ressure currents a distance of 8;3 miles using a pressure of r)0,00() volts. If a voltage higher than that were used the electricity would eseape from the wires into the air in the form of small luminous blue flames." As showing how far we are yet behind nature. Prof. Thomson says the estimated voltage from a lightening discharge ranges from twenty to tifty million volts. Wherever tlu> raw material for electro-chemical, electro-metallur- gical, or other industries, affords sutlieient inducement, and the water ])ower is at hand, the forest will he penetrated much more rapidly than heretofore, and settlements advanced in new directions. What can he done in this direction is best illustrated by the develop- ment of a single industry in tlu' wilds of Minnesota north of Lake Superior, and adjoining Canadian territory. Over four hundred mihs of standard gauge railways have been built, through what wa.s a track- less wilderness in IMS,"), to reach iron ore beds, the ore from which is shi))])ed to T^ake Krie and thence again railroad to as low a rate, by water, as 1 cent jkt bushel for wlicat between Chicago and Buffalo, and "^(t cents per ton for coal from Lake Krie to Duluth, nearly 100(» milt One-half of tlie charcoal iron, and nu)re than half of tlu ])ig iron made m the r is s melted from Lai ke Superior ore. KLKCTRir RAILWAYS. The substitution of electricity for steam as the motive power for rail- ways on many roads is regardecl ax inevitaltle sooner or later. It has al- ready taken ])lace as regards sul)iirban railways, notably in the case of the Charlevoi.x road and ILill and Alymer railway, where water is doing Ihe work which has heretofore been done by coal. The chief ob.stach^s to an early change on the larger roads are the Inuidreds of millions in- vested in locomotives, and the very large outlay required to ecjuip exist- ing steam roads with the electric system. The principal inducement would be the pas.senger service, owing to the increased speed ])ossible, — it being confidently .stated tliat. with electricity, a speed considerably over one hundred miles ju'r hour could be attained. Moreover there possilhe to rithout tlu' ' profitable )art of the ence River. t was prac- inilos iHJug re used the :m of small omson says roiii twenty ro-inetallur- 1 tlie water apidly than he (l(!velo[)- h of Lako iidred miles va.s a traek- m which i-^ into Penn- d fleets of 1 to as low \icaifo anil tith, nearly lalf of the ore. •er for rail- It has al- ihe case of er is doinj; •f ohstacles nillions in- '(jui]) exist- Inducemeut j)Ossil)le, — l)nsiderahly lover there 15 would l»c entire ahnlition of the poisonous smoke wiii< h drops upon the I'ulUuan in preference to any c(tach ahead of it. While the (Muiversion of trunk lines would be attended with a. cost which is for the present pi'oliil»it(uy, this oljjeeti(»n does not apply to ricw lines which nuiy be work«Ml independently, or in connection with electric ones. When the time arrives for such railways, water power will have a field of usefulness of which we can at present form little con- (cption. Water wiieels and wires would displace the coal docks, the (cal laden vessels, the hu^fe coal yards, and the trains re<[uircd for dis- tributing' their contents over jiundre, for maun fact urin,i; and mining pur|)os('s. especially for tiie electro-chem- ical and nietallnrgical pi-oduetions. naturally leads to the consideration (d the character of the output, especially with regard to markets, and trans|)ortation )wol>lems generally. 'rrans|)orfati(m, next to pro(lncti it — ami await results. The (|uestion (»f transportation deterndnes, to a great extent, the ex- istence, or otherwise, (d" a |)ossible imlustry, and enhances or diminishes the value of every article of export just in proportion to its efVu'iency and economy. On the other hatul, where transportation is necessarily cxjK'nsive, cheap production may nudidain an industi'y; — and here is where our abumlant water power nuiy come in. The geographical position of Canada in relation to the commercial centre of gravitv of the North American continent is at least noteworthy. This centre is very near T^ake Erie. From the western end of this lake the water ro\de to the Atlantic, at the Straits of Belle Isle, follows the general direction of a great circle wliich cuts the commercial heart of '^ 16 i-l ^ % , 1 J SI Kiiropo, aiKl is tlieroforo upon the sliorto^t routo, or " air liiu' ". Our two ])oninsiilas, Sarnia-Dctroit and Sault Stc. Marie. wlii(;li are tin- railway gates of the Ijnke ref^ion, alFonl the most direet routes to the Athmtic for all the North Western States, and are traversed by the trunk lines of railway. From liake Erie water ecMumunieation on the largest scale extends thr()U«]fh Lake Huron to the extremities of iiakes Michici- day. i-'or this the St. Lawrence is the mitural route for cxj)ortation, and to it this heavy tonnaije is of tlie greatest importance a.s a means of attracting '' tramps " as well as liners during the oj)en season. Increase of sea tonnage into the St. Lawrence is essential to our inland commerce: hy it only can sutUcient west hound freights he secured to at- tract a j)roper share of the commerce of the Lakes, after all has heen done to give to the latter (piick despatch at Montreal «)r Quebec. There is probal)ly no place in the world wln-re inland transportation is carried on with greater expedition and economy than in the valley of the St. Lawrence. This is due to the character of the inland naviga- tion, mieciualled elsewlu're, and t(» the intluence which this exerts u]>on the Railways comj)eting with it: and also, because the valley of the St. Lawrence is not (udy the greatest highway for agricultural products, but of mineral ones, as well as of the products of the Forest and the Fish- eries. ]^Iorethan half of the iron ore prodiued in the United States is mined around T^ake Superior. lnt<> this Lake an increasing number of railways are pouring the produce of the vast wheat fiehls l)etween it and the Kocky ^Mountains, and thus placing this grain within a thousand miles of Montreal, which is the nearest seaport, hy hundreds of miles, and the onlv one which can be reached by vessels capable of navigating the lakes. Wheat grown in the foot hills of the Canadian Kockies has already reached Lake Superior by an all rail haul of fifteen hundred miles, a (Mi(l- . and wholly tl'S. \u\ Mitliin a aimed to l)t' ) the largi'si 'tro-clu'inical ilditions may . the output Kor this the it this iu'avy liT "" tramps " to our iidand ;c'euri'd to at- all has hi'cu uohec. aiisportatiou n till' valley land navifjja- exerts ujHm n' of the St. )n)du('ts. hut id the Kish- The lateness of harvest in our Northwest, and the earlv ih^inu of navigation in the St. liawronee. will soon over-tax all our means of trans- port, hoth watei- and rail. durin;j; the interval between Septeml>er and Decemher. 'I'he Welland and St. Lawrence canals and the portaj^e rail- ways hetween Montreal and Iials is the demonstration, that, in spite of climatic drawbaiks. or inferiority in other respects, the St. liawrence is the route towards which northern exports will gravitate