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tures veinle the qi reddis made under optiOon to the Agaura Syndicate; the Woodâ€"Brown claims, which are beâ€" ing developed under the direction of the Coniagas Mines, Limited; and the Brennanâ€"Kenty claims. Brookbank Claims (Connell) On the Brookbank claims the rocks are massive greenstones. Along the top of a ridge extending in an eastâ€" west direction there is a fractured zone 6 to 12 feet in width. At the west end the strike is N. 85° E., but towards the rast it swings to N. 535° E. The fracâ€" ures cOontain a net work of quartz veinlets, and in places the rock along ately south of Cl Windigokan lake The Brookbank g tyâ€"four claims:; â€" in two groups cor to the east and n of the Brookbank western Knox cl claims staked by Syndicate. Abo north in the va. river are the B under ontion t» t PQur Cf by the wri vincial Ge area nori Name wam Windigoka bearing qu area durir number of visits wer Knox, Spri Brown, an claims. * Springer ( Department of Mines Issues Timely Review of the Jellicoe and Other New Gold Sections in the Thunder Bay District. Report of Geologist on Number of Leading Claims in New Gold Area. Preliminary Report on New : Sturgeon River Gold District : If the first bottle of BonKora does not bring you the druggist will refund your money. Try it today. BonKora has also shown its effectiveness as a splendic tion, constipation, Ratulency, biliousness, in fact a c ailments as well as a general health builder and tonic and digestion are the foundation of perfect health. the reason why F â€"â€"harmless and pleasant to takeeâ€" enjoys such im mense sales, the F you cannot find dresses to fit you because you are too stout, if your friends and neighbors make fun of your figureâ€"try BonKora, the sane and safe way to reduce and to better health. No starvation diet, no vielent exercises, no harm» ful, habitâ€"forming drugs, nothing that will interfere with your daily duties or social pleasures. That is cuontain a net work of c ts, and in places the rock lartzâ€"filed cracks is altered h material, which seems up mainly of feldspars. Inâ€" E DOES MAKE EVERYTHING / l IAST E BETTER. â€" ’\ 2e Z.GUK EUH THE WATTHAUIVE M WORLDS STANDARD OF QuALiTty _A WOULDN‘T USE \ ANYTHING ELSE Now, SINCE TVE DISCOVERED NEX TLETE.ITS 50o HANDY AND REALLY IT DOES MAKE EVERYTHING TASTE BETTER: . (E. L. Bruce) places there ar days in September were spent | there are no qua vriter in company with the Proâ€" ation extending H. C. Rickaby, in the the central fissu rth of Jellicce between the | both of the qua minikan (Sturgeon} river and reddish zones, kan lake. Discoveries of goldâ€" | abundantly in cu quartz veins were made in that | to oneâ€"eighth of ring the summer, and a large | Gold can be pan of claims were staked. Brief ca material ahav WHV NOT USE NESTLE‘s MARY ? 1T‘s DOUBLY RICH, BECAUSE Most OF THE WaAter Has [ BEEN EVAPORATED. An kbank laims:; oups c nox clalms is a group o ked by the Karl Springe About two miles farthe the valley of the Sturgeor the Barnumâ€"Green claims V a rt MR CANADIANS, onCcE Fat why BonKora a CBUILS, LDA wW. SCOLLON, Suskatoon, Sask. tle of BonKora does not bring efund your money. Try it today AI J,. H. CLARKE, Port Alberni, B. C NOVEMBER 15TH, 1934 ri “‘in. I !I sults with ‘ards the | the Broo ‘he fracâ€" | work has ~â€" quartz | continuity ck along | zone there red to a | acter fron s to be|on the B: In many vein on t se 10 treatment. Ins, | {Nhe points o ite; | rock is congl beâ€" | (Timiskamia weight and muy edies, also rig results."** . PRaist BONKORA "I think BonKora ever used to reduce,‘ MRS. F 6721 Borde MRS. L. WILSON, 19 Price Street, Taronto. bring you the desired results, your near t the sediments is much less p merate on the north side of conglomerate | quartz vein in be in line wit as a splendid remedy for indigesâ€" , in fact a corrective of stomach s1dGe of es at the locally kno north side « places there are reddish zones where }ot‘l there are no quartz stringers, the alterâ€" | It ation extending outward merely from | mu the central fissure. Along the margins | ave both of the quartz veinlets and of the | is : reddish zones, pyrite occurs rather| side abundantly in cubes from oneâ€"sixteenth | by â€" to oneâ€"eighth of an inch in diameter. | fiea nd tonic. Proper elimination health. Try it! I lIne with Br0o0Okbank rom an i1 Brcookba i the Kn he JOS1 Claims (K. L. Exp Company Limited) stern group of Kyr eâ€"east end of a : Own as Knox lake T1 r o of Aan Intch in panned from the ribove the lode:; â€" m unweathered LK € The sheari ronounced in south shore he roc 16 bet VITCH x St., Montre im snore ike. _ ut ~CL0i0g snear zone hern boundary of shearing, however. frac )€ 3e lak ind C Exploration side Of i ie Windig it seems to L he appearanc which sample nd which ar work will hav rty before an s to the valu Knox claims a small lake ike. On the VAIY Zones where rs, the alterâ€" merely from the margins XJ rible WE n the me of an y ilue but Di | fied zone, which c râ€" | amount of sphals re j and pyrite. The il. Har variety, coffee done tanc has due is said to indica gold values. T the quartz vein fied zone, which end of the worki side. The quart has a ribbconed juartz, th [t cuts ac OoI the claim n It consists of ; mum width of average width is nearly vert acrosg of th re staked by Wood a not included in the t mentioned. Woodâ€"Brown Claims ‘his group of claims li A VE No out in On tember ‘lhey Along the sot is a mass of of which exte out in a shotr Un The Cclaims when visitec ember, considerable trench tripping had been accomplis our veins had been discovered hese are roughly parallel with raced ists 0 e 2enCo ed n T‘he vVeIr Ti@d@ Irom sampies assaved. Claims South of the Sturgeon River e width â€" vein has b distance C ilm ulp VIS1teG. irnumâ€"Green Claims (Agaura > Barnumâ€"Green claims are w y strik orner 1¢ 11 hi o determint Woodâ€"Brown nair Ma ide â€" ‘al t e of ~T.B.~13,398 S. 30° W B. 13,399 nearly to the centre im next southwest, T.B. 13,395. s of a quartz vein, the maxiâ€" th of which is 7 feet and the vidth about 2 feet. The dip vertical. On the northwest is vein and separated from it t of chlorite schist is a siliciâ€" which contains a considerable F sphalerite and some galena . The sphalerite is a granuâ€" ‘, coffeeâ€"brown n colour, and indicate the presence of fair Irom much 1] n som samplin vein is of ha outh side of quart: T‘€ 400 M il jpre ike 16 springer Claims 70L Hen« drift Te hev s al vidth ake 1¢ of 1( irds t throu n that is on | the ( earan{ 18 it thi inC 1 m traced 300 fe DDO ralf discovered. All « rallel with a nort!] 1 vein in the sout} . 12,399 has bee 1} C Syvndicatd trenching iccomplished m M her s Coniagas) i Synd a} I‘l1€ al greenston?>y T.B. 13,403 there rphyry., tongues e eIn d ( Pach w in one ib the r9rt dis h end C rtheant nch sampl > quar ith end THE PORCUPINE ADVANCE, TTMMIN3, ONTARIO 11 [(eBBDi but 1A the inch 11 1€ 1@Ay? ) VC VC ON alil C%f Thnem, diliamond â€" dr Samphng has Niagara Falls Review:â€"No longer is l a quartz vein a leftâ€"handed boy or girl compelled to and which h use the right hand in most Canadian | short distanc schools, and it has been found that the | Obtained acro: leftâ€"handers are not behind their conâ€" | alized syenite temporaries who use the more normal| The geology hand. In the Caledonia‘ public school | dike of syenit it has been found that the 18 leftâ€"hand~â€"| the property ed pupils all are among the leaders in with sulphide their classes,.. Fortunately, nowadays, ments are loc no effort is made to force children to|and granite t use the hand found least natural and is in the sye the results are all to the good. have been ma ind en All T rower toward the nor southwestern end it is placed by a fault which vein to the stutheast. tion uncovered in a t the part where it is transverse to the foliation, quartz stringers tongue out along planes of the schist. The quartz is white with a banded and brecciated structure, marked by chloritic streaks. It contains considerable quantities of a buffâ€"coloured carbonate, probably sideâ€" rits. The metallic minerals present are galena, chalcopyrite, and pyrite, all of which occur in small quantities. The maximum width of the vein is one foot, and in places it narrows to a couple of inches. Gold in visible quanâ€" tities is reported to have been found in this vein; assays of grab samples iffi rOWw Brennanâ€"Kenty Claims (Sturgeon Reserve) The Brennanâ€"Kenty claims lie west of the Coniagas group separated from them by the McDonough (Macjoe) claims, whith were not visited. On the Brennanâ€"Kenty claims the rock ds greenstone intruded by some masses of granite or granodiorite. At the originâ€" al discovery there is a lens of quartz 5 fect in width exposed on the side of a hill for a length of 15 feet. It appears to strike N. 25° E. and to become narâ€" rower toward the northeast. At the General Character c The geological condit CaAabVICILICIY UuIliliClUlL LOQ AITIVE aAt an atcâ€" curate estimate of the value by chanâ€" nel sampling. On account of the narâ€" rowness Of the vein and the apparent lack of mineralization in the wall rock the gold content of the quartz will have to be high to make the deposit workâ€" | L.B. 13,642. It strikes N. 42° E. and |dips 60° N.W. At the point where it disappears beneath overburden to the north it is 100 feet west of No. 3 vein ’ and, if continuous, should intersect that vein 200 feet farther north. No. 2 vein has been traced for a disâ€" tance of only 200 feet. It shows a width of two feet at a point 250 feet west of the east boundary of T.B. 13,643. The strike is somewhat irregular but the general trend is northerly. The large number of occurrences of gold in visible quantities in No. 3 vein is the most promising feature of this group Oof claims. It will, however, be extremely difficult to arrive at an acâ€" curate estimate of the value by chan-! nel sampling. On account of the narâ€" iD uthnwestern end it is apparently disâ€" aced by a fault which has shifted the ‘in to the stutheast. The continuaâ€" n uncovered in a trench in that rection is, however, considerably narâ€" wer and has a somewhat different rike. FaArther east a narrow and very regular vein in strongly schistose lorite schist cuts across the schistosâ€" ‘ for a distance of 60 ft. and for some stance farther is parallel to it. In e part where it is transverse to the tanceg of width of : west of the The strike ha er and has ke. Farther c gular vein ; rite schist cu for a distance ance farther h f which occur i: maximum width and in places ty are vere cold. 1 tried several remedies without deriving any benefit. At a friend‘s suggestion I tried BUCKâ€" LEY‘S MIXTURE. It is wonderful how it can help a cold so quickly." Whether your cold is merely in the sneezing, sniffing stage, or away deep down, Buckley‘s will bring you prompt, sure, safe relief. It acts like a flashâ€"A single sin one who tak es BUGKLE Y ‘S for the first time. Accustomedâ€" t o ordinary c o ug h remedies t he y don‘t expect any benefit for severâ€" al days, and often don‘t get relief then, and are astounded to fin first dose of BV TURE gives unn t WO mine K6 NC A}l IT‘S WONDERFUL HOW V BUCKLEY‘S CAN FIX _ _A COLD $O QUICKLY /.. rnd Irom a he Barnum O irpri ima lake. So far as exploraâ€" zone the veins in which gold to the found in visible quantities are [t seems possible, however.' A small cre me there may be a sufficient | surface explor to make them workable in | the Brydges G he narrow widths of quartz.| east of Consol work has not been done yet | about 15 mile: ine the value of any Oof the Several inter , and thorough sampling will | been opened â€" ‘ done on all of them. diamond â€" dri\ Ves ito Other Discoveries few | he properties in the Sturgeon | with already described a number | little | iscoveries have been made:; |can v _not visited. _ These disâ€"| went _ along the Sturgeon river| load nOst @_gives unmistakal Miss Mary Rysary, ftor inst Winter zing, sniffin ip down, Bi _prompt, sure like a flashâ€" a point abcut 4 miles imâ€"Green claims for a proximately 20 miles to Lake Nipigon. On veins have been found values have been reâ€" acter of the Area conditions seem fayâ€" currence of goldâ€"bearâ€" basic voilcanics have jleal of shearing and > the northeast there Tranite or granodiorite y related to the inâ€" t occur in the vicinity . So far as exploraâ€" in which gold old nstance â€"â€" } ter I caught I tried sever ion in the wall ro that the greater part in the auartz. n MuC find that the very BUCKLEY‘S MIX. difficul e avera t of No. 3 and n T.B. 13,643 and 5 N. 42° E. and pearandC movem h JZIUE._ Lh wall rock quartz. In tinvy flakes slenside, writes :â€" very seâ€" remedies rtion of arrive at 1 gold in at many #old is in and both @bundant nt and. mewhat relic AinNe geoiliogy consists dike of syenite porphy the property and whic with sulphides and vi: ments are located nor and granite to the sou is in the syenite tha have been made to da The vein some few days about 4 feet in width gold in the core. Th aging. The company of about 40 men wor The Alscheback Gol toward China at the feet per day. They about 25 men and are fine. Their object depth of 500 feet. Work at Brydges Mines to the East of Matheson On The Kirkland diamond drilling vein some few . cow. Mr. Young y few hours and deli~ with neatness and d little hard on the T. can we do about it. went down to Heaslip Some News and Views from ! the Goldthorpe Gold Area We hear ‘that the at Bourkes, has bee of mining men from that they will pump once more give the trial. We hope this dent mce more give the o rial. We hope this tand up to ‘the test a lucer. J. R. Young went c ast week and broug | W4i€LE, and Is uUunder no restrictions. PHere are no tafiffts With which to 'contend, and it is not necessary to keep a trade commission or sales staff. It is unfortunate, said the speaker that the public comes into contact with the mining industry through unscrupâ€" ulous promoters, An industry that can carry on with those parasites and hangersâ€"on clinging to it must be fundamentally honest. Avoid tipster sheets, was the warning given the audience. "If the parties who write these tip-' ster sheets knew half as much as they thought EFhey did they would have owned all the mines in Ontario ten | years ago." The losses made by the‘ public because they do not investigate before investing were unfortunate for the whole mining industry. nearly _ every ‘com tional Nickel, for ex 000 cheques when ; clared. Mining does no{ any other ‘industry. where, and is unde There are no tarifi contend, and «it is keep a trade commis: were Cani Another wealth g« power. of supplie; be taken ; The following paragraphs e last issue of The Speak it in by the Goldthorpe c that men presen few ve and executi Kirkland L depression, sard ithat t advantage ( blem to pay remained th The wages ( are slightly went produ years mines WeE ple chief Onta of H addre Orilli cond in gold art pper and fourth It «s expected t ice _ $105,000,000 in 1935, M ust SsSOlidated > miles east M 1 ‘alue of the Mining | Industry to Canada. The impot id uced sicent of Howey Mines Shows Wh Mining is Doing to Help Canada‘s Stability and Prbogress. Great Wealth Produced. dIians, an he could employed and id _ ind Lak ssion, stat hat the m placed ndustr ) prodi d _ $195,000,000 Wealth â€" prod 11 oyed in the minin idians for two gene ‘ channel into whi es is that of sutr old Mir befort Mr. orpt 1€ Dauced 2 $350 . 000 1( im mnsolidat The drill ver, no mine has ever| U xes. Mines dispensed | P s year $45,000,000 and | P® rey finds its way into j 1P community. Internaâ€" | Y« r example, writes 90,â€" n a dividend is deâ€" | wl desp sibl th « 1i U l1d Bourk pioneer f nd soon 1 )] Ma Mit Cold i Mr. Birks th least half C mineralized 108 fr ind th mpiloyn P 16 I¢ mecessary r sales staff. the speaker contact with Me: m l 1X ire from ‘r, being rrespon â€" ch mining | plies and| old fTC pl day in fits 1 ind ind with anyâ€" ib 11 e : F. J. Sullivan, mine manager, for Lake Caswell Mines, in the West Shining Tree gold area, reports that surface exploration work is being conâ€" tinued, angqg a series of shear zones are being examined and mapped. A numâ€" ber of these shearings recently were located and ‘there are 17 in this area as well as several others to the east. 1evelo} Shinin camp:s would ‘r of these shearings recently were cated and ‘there are 17 in this area as l1 as several others to the east. The No. 109 vein is being blasted, and iere opened up free gold is in eviâ€" nce in a number of places. It is the Exploration Work in the West Shining Tree Are; iA C 1l A 1 1€ * prop )pmen HEAD QOFFICE â€"TOR.ONTO BRANCHES THROUGHOUT CANADA 1l 17 m h l The Twentieth Century is still Canada‘s. In this brief series we have told in some small part of the Bank‘s activities in Canadian development, and of the abiding faith in Canada‘s destiny, We look for a return to reasonably general prosperity. A new head office building for this Bank is to be erected in Toronto during the next year at King and Bay Streets, where the executive offices will move after nearly sixty years at Wellington and Leader Lane. 1 Throughout the trying times of boom and depression Canada‘s financial structure has stood firm. The banks and the system of bankâ€" ing have grown up with Canada. The roots are deep in native soil. They stand all tests of comparison. This Bank, by virtue of sound principles and faith, stands today in a favourable position for serving its clients. For sixty years the Bank‘s shareholders have received a fair return on their capital. Hundreds of thousands of people have used the Bank as a savings depository and the Bank has been ever thoughtful of their interests and of growing industry and newer developments in the Western and Northern areas. and the world is ready to supply it. OL;I‘ ral:il- road problem and the drag of interest payâ€" ments on borrowed capital will grow less in the natural course of events as the country fills. Institutions the world over, both political and economic, have been shaken to their foundaâ€" tions during this decade and, as would be expected, some have not stood the test. Forâ€" tunately, Canada was faced with no such major problems as overâ€"crowding population, famine and disease, or, unfriendly neighbours. Until the present century our growth was slow but sound from the roots and we have an enorâ€" mous territory that to a large extent is still undeveloped. Our only need is more people 3. .‘% % SWih ie a â€" ul i on o 2s P ces e o e these car _ and de istification needed : of the Oot i} and development ha: tification for the advo needed road. Develop f the Oother gold field: ould seem to add weigh _for the new road. Th« f any properties a or West Shining Tre ken as further evidenc usefulne onnect u id bury The Twentieth Century Is Still (anada‘s CAFPOU Shni DECADES OF PROGRESS CowarposBsurc camp pit ~Of, thk. Sudbut The 1M mm th i the de Matache he road ind Por min.n The famous energyvâ€"producin sweetâ€"an casily digested foo invaluable for infants, rowing children, and enjoyed‘ by the whole familv. trip and h it The Canada S‘tarch € and as he grew old to become a railr ‘stead. he became : retirement on his lyme, Conn., his 1 has come true. built a miniature | long with trestles o nels through hills. of his sturdy little to a string of cars be seen almnst 4n Ove dre iNoted Actor Has (‘Omplete Railroad Trains and Tracks Ite (Huntingdon In his boyhood William Gillette, 79 actor, like railroad t W 5 w©umeâ€"true. â€"C It a miniature g with trestles s through hills his sturdy little a string of car seen almost r his railroad ims realized nC In ‘â€"@ IRGUWUIIAL T( A new head to be erected , according to figu Ontario Departmen o is the intention grew older his ambi ‘ _ A railroad enginee became an actor but _ _ estate his longâ€"defe . ~Om this f ure railroad l oug} i1 expic ngtlhi 5¢ men V WO h m 11 mited ree} mad hing thrilled d American His favorâ€" adlong vhood ‘es gol uppli Mines, ap th ie lak ag in ns ) shore io Deâ€" ill bel whnclr aVvoreâ€" train . wWAaSs In=â€" t ars star earl con~â€" nuwty