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Structural Geology â€" The interpretation of the geolomcal structure in the area is impeded by lack of rock exposures and the uniformity of rock types over most of the country. The tracing of horizons of iron formaâ€" tion, however, is proving to be of conâ€" sidgerable use in showing the deformaâ€" tion of the region. By this method it has been found that the formation immediately north of the Pickle Crow mine has been folded into a syncline, the axis of which strikes about N. 45 degrees E. The axial plane is overâ€" to the north with a dip of about degrees. North and east of the mine lm'ync‘!lnenosesout and a series of measurements taken on nose ‘the folds indicates that it plunges to the northeast at an angle somewhere This rock assemblage is intruded by irregularly shaped bodies and dikes of granite, porphyry, and lamprophyre. two gdistinct types of porphyry occur, a sheared quartz porphyry and massive syenite or quartzâ€"feldspar porphyry. North of the Central Patricia mine are sillâ€"like bodits and dikes of quartz porâ€" phyry, which show various degrees of shearing and alteration to quartzâ€" sericite schist. An elongated body of massive quartg; porphyry occurs near the northwestern extremity of the Alâ€" bany River and Winoga Patricia claims. West of the Albany River shaft is a small stock of massive quartz feldspar porphyry. Small syenite porphyry dikes are occasionally found. The lamâ€" prophyre cuts the granite of the area, and a lamporphyre dike cuts the main vein at the Pickle Crow mine. A diaâ€" base dike runs southeastward across the Central Patricia claims east of. the mine and is presumably Keweenawan in age. > The bands of iron formstion range from tiny patches only a few inches wide lying between lava flows to bodies two or three hundred feet in width that may be traced for several miles. The traceable horizons may pinch and swell or even die out at various. places along the strike but are sufficiently continuous to provide marker horizons in the greenstone complex; they afford the only reliable clues to the details of structure in the rock formations.. Most of the area is underlain by Keeâ€" watin rocks, chiefly basic volcanics. Interbanded with these lavas are bands of iron formation, agglomerate, tuff, and volcanic breccia. The lavas are fairly massive and commonly show pilâ€" low structures, but may be locally sheared and dragâ€"folded. In a few places bands of diorite strike parallel to the general trend of the lavas and are probably sillâ€"like intrusives of about the same age and composition as the flows. (By Jas. E. Thomson) During the past sunmer, a detailed geological examination was made : of most of the properties being actively developed in the Pickleâ€"Crow area. These extend for about nine miles from the Gateway Patricia claims on the west to the Kaw Crow Patricia proâ€" perty on the east. Preliminary Report on Pickleâ€"Crow Gold Area Government (eologlcal Party Made Examination of Pickle Crow Area in the Patricia District During Past Summer. Preliminary Report Just Issued. PAGE TWO Doherty Roadhouse Co. Toronto 293 Bay Street Market Quotations broadcast each day at 12.20 noon and 5.20 p.m. Direct private wires for fast and accurâ€" ate quotations and executions in all Aceurate Markets and Executions in Commision basis only Local Phones 1200 and 1201 Members Toronto Stock Exchange Charlie Hallâ€"Manager Unlisted Stocks Mining Stocks Industrial and Public Utility Stocks Bonds with pyrite mineralization; the zone strikes N.30 deg.â€"35 deg. E., and dips 65 deg.â€"68 deg. NW. Seventy feet north of this lies No. 2 vein, which is said to have been traced 25 feet by diamond drilling and which contains gold values. Drilling at intervals over a distance of 800 feet to the southwest along the strike of No. 1 vein zone has indicated goild values in a number of places, but these intersections are difficult to corâ€" relate from drillinrg data, and only unâ€" derground work can establish their exact relationship. Gold seems to be associated with pyrite mineralization main vein but carry only low values. tion or entirely within the latter rock. 3. Silicified sheared zones in lavas Mine officials estimate that 80 to 85 or at the contact of lavas and tinylpel' ceéent. of the ore section liee in bands of iron formation:â€"These may | Sreenstone. It is said that, in general, be mineralized withn sulphides. Such | the part of the vein in iron formation sheared zones occur on the Albany| is wider and slightly lower in grade River claims, where gold is associated | than the part in greenstone. In limited with pyrite and, to a lesser extent, sections, where ore is being stoped in chalopyrite. At the Cohenâ€"McArthur| the iron formation, parallel fractures showing north of the Pickle Crow Mine,| filled with quartz veins and stringers quartz véins occur in silicified sheared ) occur across widths of 20 feet or more. zones, are mineralized with arsgnopy-‘Three prorounced arag folds occur rite, and contain native gold. | along the vein, and in the vicinity of Descriptions of Properties | these good ore widths are found. Albany River Mines:â€"During the l Typical vein material is banded white summer a vertical shaft was being sunk | quartz with chlorits or tourmaline ocâ€" in the vicinity of a gold showing preâ€"| Cupying narrow fracture planes. Sulâ€" viously exposed in surface testâ€"pits and | Phides are comparatively rare, and visâ€" intersected by diamond drilling. | ible gold is not abundant. Gold values The goldâ€"bearing zone lies in an area | are generally consistent along the vein. of basic lava flows containing many| Winoga Patricia Gold Mines:â€"The small bands of iron formatior and adâ€"| company owns a group of nine claims jJacent to a small stock of massive| located immediately east of the Pickle quartzâ€"feldspar porphyry. The shaft Crow. These are being actively develâ€" zone lies immediately off the nose of Oped by surfaceâ€"trenching and diaâ€" the main porphyry mass, where it finâ€"| mondâ€"drilling. Owing to the fact that geers out into small dikes and irreguâ€" most of the ground is covered by overâ€" larly shaped bodies. At the main surâ€" burden, a geophysical and electrical face showing (No. 1 vein), located 200| Ssurvey was made during the summer to feet northeast of the shaft, results of | and diamondâ€"drilling to a depth of 1838 feet are reported to show an average value of $23.64 a ton across 5.4 feet for a length of 20 feet. Here golid occurs in a silicified sheared zone with pyrite mineralization: the zone assist in the drilling campaign. The exposed rocks are largely basic lavas with minor amounts of volcanic fragmentals. A band of iron formation runs northeastward across the northâ€" west corner of the property. North of this, an elongated mass of porphyry 3. Silicified sheared zones in lavas or at the contact of lavas and tiny bands of iron formation:â€"These may be mineralized withn sulphides. Such sheared zones occur on the Albany River claims, where gold is associated with pyrite and, to a lesser extent, chalopyrite. At the Cohenâ€"McArthur showing north of the Pickle Crow Mine, quartz véeins occur in silicified sheared zones, are mineralized with arsenopyâ€" rite, and contain native gold. Descriptions of Properties Albany River Mines:â€"During the summer a vertical shaft was being sunk in the vicinity of a gold showing preâ€" viously exposed in surface testâ€"pits and intersected by diamond drilling. pasits in the area. | â€" Pickle Crow Gold Mines:â€"The main _ 1. Quartz veins occupying fractured | véein at the Pickle Crow mine has been zones in massive or slightly sheared | explored from six levels to a depth of lavas:â€"These veins are generally twistâ€"| 750 feet. The shaft has recently been ed, contorted, or dragâ€"folded. They conâ€" | sunk to 1200 feet, and three new leveis tain tourmaline, chlorite, and native| will be opened up. During the first nine gold, but sulphide mineralization lsl months of 1936 the mill treated an rather sparse. This group is representâ€" | average of 146 tons daily, with an avâ€" ed by quartz veirns on the Springer, erage recovery of $30.20 per ton. The (No. 2) operation of Central Patricia| mill is now being enlarged to handle and some of the veins on the Pickle| 400 tons daily. Crow, claims, including the main (Howâ€"| The vein has been explored underâ€" ell) vein. ground over a total length of 1500 2. Sulphide bodies occupying fracâ€"| feet. On the surface it extends 200 feet tures in iron formation or replacing| west of any undergrond exploration. certain parts of this rock:â€"In thisiThe vein strikes roughly N.65°â€" group belong the ore bodies at the| 75°E., but in places is much contorted Central Patricia mine. Here, pyrite,| by drag folds. The general dip is about chalcopyrite, pyrrhotite, and arsenopyâ€" | T3°N.W., but between certain levels is rite are the sulphides with which the|almost vertical. The vein angles across gold is associated, especially the latter|the enclosing rock formations, which two. On the Albany River claims gold ' have a general northeastâ€"southwest is also associated to some extent with | strike in its vicinity. The eastern and pyrite in iron formation. Sulphide] Wwestern parts lie in greenstone, and bodies occur at the Pickle Crow mine| the central section is either along the in the iron formation adjacent to the| contact of greenstone and iron formaâ€" main vein but carry only low values. | tion or entirely within the latter rock. In the vicinity of the Central Patricia mine a number of bands of iron formaâ€" tion have also been traced for some distance. Here there is evidence of faulting in an eastâ€"west direction along the Crow river and of crossâ€"faulting which has offset the iron formation. __ _ Veins and Mineralization _ Gold occurs in several types of deâ€" pasits in the area. ibe'w'een 45 and 70 degrees. Two horiâ€" zons of iron formation have been traced around both limbs of the syncline. A tb,i’rd and possibly lower horizon exâ€" ists on either side of the above strucâ€" ture but has not been traced around the nose of the syncline. The southâ€" eastern band, which may be a limb of the third and lowest prominent horizon of iron formation, has been traced from point near the Springer vein ‘of, the Central Patricia Mines across the Pickle Crow, the northern part of the ‘(Winoga Patricia, and the Albany River claims. That this horizon of iron formation was the locus of conâ€" siderable fracturing is shown by the fact that numerous veins and sheared zones, including the vein at the Pickle Crow mine and the main gold occurâ€" rences on the Albany River, Winoga, and Springer claims, are locatea either in or fairly near this band. Timmins 19 Pine St. North Kaw Crow Patricia Gold Minesâ€"This company owns a large block of claims that surround the Winoga on the south and east and adjoin the Albany River property on the North. The southwes. Crow. These are being actively develâ€" oped by surfaceâ€"trenching and diaâ€" mondâ€"drilling. Owing to the fact that most of the ground is covered by overâ€" burden, a geophysical and electrical survey was made during the summer to assist in the drilling campaign. The exposed rocks are largely basic lavas with minor amounts of volcanic fragmentals. A band of iron formation runs northeastward across the northâ€" west corner of the property. North of this, an elongated mass of porphyry and some smaller dikes cut the greenâ€" stones. A number of goldâ€"bearing veins and stringers have been intersected by diaâ€" mondâ€"drilling. The most interesting values to date have been obtained on the company‘s northwestern claim near the Pickle Crow boundary and north of the band of iron formation. | similar to the aboveâ€"mentioned ore bodies. The Springer (No. 2) operation is loâ€" lcat.ed about 4 miles east of the main | workings. A shaft was sunk 175 ft., and \lateral work was done at the 150â€"foot | level on the Springer vein. At present | this shaft is being deepened to 500 feet, ’and other levels will be opened. The goldâ€"bearing quartz vein, which occupies a fracture in fairly massive greenstone, has been traced about. 350 f feet on the surface, but disappears unâ€" \der swamp to the east. It has been dragâ€"folded and contorted, and the general strike swings around considâ€" The vein is generally narrow but local bulges show widths up to 8 feet. The vein filling consists of white quartz, black tourmaline, and traces of sulphides. Native gold occurs in conâ€" spicuous amounts in certain parts of the vein. On the 150â€"foot level four ore shoots, rarging in length from 25 feet to 90 feet, were found. These made a total ore length of 198 feet, averaging 2.35 ounces gold over a width of 14 inches. | both in the iron formation and the siliâ€" | cified sheared zones in lava. During the summer drifting westâ€" ward on the 375â€"foot level disclosed a new ore secton in a band of iron forâ€" mation with sulphide mineralization A number of ore shoots occur along the band of iron formation, the most productive to date being B and C ore bodies. All these have a definite easterâ€" ly rake, which averages about 53 deâ€" zrees. The localiz»ation of the oreâ€"shoots is thought to have been controlled by zones of crossâ€"fracturing in the iron formation. formation that have undergone fracâ€" turing, which has allowed the mineralâ€" ization solutions to penetrate these openings and replace certain parts of the iron formation. Gold values occur in bodies of sulphides and networks of quartz veinlets containing varying amounts of sulphides. The sulphides are pyrrhotite, arsenopyrite, pyrite, and chalcopyrite. Gold is found in close association with these, especially with pyrrhotite and arsenopyrite, and is scarcely ever seen in the visible state. The quartz does not contain much gold. tons daily with an sverage recovery of $19.00 per ton. The ore bodies oecur within a band of iron formation, which is bordered by Keewatin greenstone. The iron formaâ€" tion trerds about eastâ€"west and dips to the north at an angle of about 75 degrees. It ranges in width from 5 feet to about 75 feet and is revealed by surface trenching for 1800 feet. Ore bodies occur in those parts of the iron At the southwestern extremity of the property and about 200 feet from the Winoga Patricia boundary, a silicified sheared zone in greenstone near a small band of iron formation carriee gold values, especially where sulphides are present. Central Patricia Gold Minesâ€"At the main property the mine has been deâ€" veloped by 8 levels to a depth of 1.000 feet. Up to the present the ore mined has come from above the 500â€"foot level. Four new levels are now being opened up. During the first nine months of 1936 the mill treated an average of 155 THE PORCUPINE ADVANCE, TTMMINS, ONTARIO Globe and Mail:â€"In the House of Commons on Friday the fact was emâ€" phasized that the British people have a King because they want one. A moâ€" tion to establish a republican form of government mustered only five votes. Ottawa Journal:â€"Mr. Hepburn says he is proud to associate himself with President Roosevelt. We have yet to hear from the party of the second part. rorth. During the summer the claims were prospected and developed by surâ€" faceâ€"trenching. The rock exposures are largely altered agglomerate and tuff with lesser amounts of basic lavas. Some quartz veins were found. A siliâ€" cified sheared zone with pyrite minerâ€" alization was traced and explored on the surface. Roeanor Gold Minesâ€"The company holds a group of claims which adjoins the Central Patricia on their west boundary and the Kaw Crow on the The rocks on the claims are largely basic lavas. A siliceous carbonate body in the greenstone extends in an eastâ€" west direction across claims Pa.777 and 774. On the north side of this body sheared zones occur in the greenâ€" stone and contain irregularly located quartz veins and stringers. These are mineralized with arsenopyrite and conâ€" tain some native gold. Gold values have been obtained in the surface trenches over a length of about 150 feet. Twelve hundred feet to the northeéast of this, a series of discontinuous sheared zones contain some quartz stringers and a little arsenopyrite. A section across 85 inches in one trench is reported to asâ€" say $9.00 in gold. o Coniagas Minesâ€"During the summer two groups of claims were staked in the northeastern part of the Pickleâ€" Crow area by Jack Sutherland for Coâ€" niagas Mines. A band of iron formation was traced for a distane of 12.000 feet across the northeasten group of claims by a dipâ€"needle survey. A series of exâ€" ploratory diamond drill holes were put down to intersect the iron formation at intervals along the strike. Cohenâ€"MacArthur Claimsâ€"The Coâ€" henâ€"MacArthur claims lie immediately north of the Pickle Crow and west of the Albany River. A gold discovery was made on this group by Jack MacArthur and opened up by surfaceâ€"trenching in 1934. The showing was diamondâ€"drilled during the past summer. The rocks on the claims consist largeâ€" ly of Keewatin lavas, agglomerate, and tuff, which are intersected in places by porphyry and rhyolite dikes. Two outâ€" crops of altered sediments ind iron formation occur on the southwestern claim of the group. A drillâ€"hole 100 feet east of the Winâ€" oga boundary on claim Pa. 2122 cut a 4â€"foot ven, which assayed $8.40 per ton in gold. Gateway Patricia Gold Mines:â€"The company owns a group of 27 claims, which adjoin the Central Patricia on the west. These claims, which are unâ€" derlain by Keewatin greenstones, have been explored by an electrical survey, surfaceâ€"trenching, and systematic diaâ€" mondâ€"drilling in the driftâ€"covered secâ€" tions. tern claims tie on to Pickle Crow ground. A considerable part of these claims is covered by overburden, and geophysical and electrical surveys were made of the western part of the group. Development work has been carried on by surfaceâ€"trenching and diamondâ€" drilling. 11 Spruce 8. GOOD WOOD For Sale At Reasonable Prices NEW TRANSEER Timmins l | Adopting a somewhat different view of the conditions, the property of Minâ€" eral Estates, Ltd., was acquired on the expectation that the extension of the sediments continues westerly through the townships of Mountjoy, Godfrey and Turnbull, ard octhers to the southâ€" west. Taking the broad view of the exâ€" ploration possibilities, should such a _condition be proven, sponsors of Minerâ€" al Estates, Ltd., acquired more than 20 square miles of territory in the townâ€" ships of Mountjoy, Godfrey, Turnbull, Carscallen, Bristol and Ogden. Then came a programme which has emâ€" braced every modern prospecting pracâ€" tice, directed by an organization espeâ€" clally qualifiedâ€"the staff of Mining Research Corporation, Ltd. Where practicable, surface work was done, and some major vein occurrences were disclosed, in some of which very high gold returns were reported. At other sections of the holdingsâ€"which extend for some 14 miles west of Timâ€" minsâ€"the amount of overburden dicâ€" tated different methods. For structural information some diamond drilling was done, and this work definitely indicated that the sedimentary belt could be traced on the Mountjoy township claims. Then followed a geophysical survey, by which method large areas can be mapped and rock structures deâ€" fined without the costly work of trenchâ€" ing and sinking test pits through the overburder. This survey, as mentioned, is the largest contract ever undertaken in Canada and was carried out by Hans Lundberg, Ltd., recognized as the ‘eadâ€" ing organization offering such technical service. The geophysical survey has now a presumed strike somewhat to the southwest. A very large amount of deâ€" velopment fungs has been expended by some of the foremost operators on the continent along such a premise, and without any outstanding success. A review of the situation to date may be of assistance in interpreting the sigâ€" nificance of anticipated success. It has lorng been held that the belt of Timisâ€" kaming sedimentsâ€"with which are asâ€" sociated the major producers of the faâ€" mous Porcupine campâ€"would be found to extend westward from the present recognized productive area. There was among geologists and engineetrs a disâ€" position to seek such extension alonzg R (From Pinancial Review) With the announcement of plans for an immediate and comprehensive diaâ€" mond drilling campaizn for the holdâ€" ings of Mineral Estates, Ltd., in the Porcupine field, the operation reaches its most interesting stage to date. A contract for a minimum of 5000 feet of drilling is being negotiated by Minâ€" irg Research Corporation, Ltd., conâ€" sulting engineers, and the work is exâ€" pected to get urder way without delay. For months, Mineral Estates has been carrying on a very extensive proâ€" gramme of exploration on its large acreage to the west of Timmins, and results have been such that conditions indicate new history in the making for this premier gold camp. Probably not more ambitious mineâ€" making project has before occupied the attention of the investing public than the effort of Mineral Estates, Ltd., on its vast stretch of mineral ground west of the Mattagami River. The very acreage of the company‘s holdings is unique, and the magnitude of the posâ€" sibilities has aroused interest throughâ€" out the mining industry. The forthcomâ€" ing diamond drill campaign can be exâ€" pected to provide news of profound sigâ€" nificance to Ontario mining and may write a new chapter in the history of the leading gold province. For months a programme has been under way which has embraced surface work, a limited amount of diamond drilling, and the most extensive geoâ€" physical survey ever conducted in Canâ€" ada. The enterprise has thus reached the stage where it may be the fourdaâ€" tion for not only one mine, but several, if the results achieved to date can be taken as a criterion. Mineral Estates Let Drilling Contrac Property has Already Most Extensive Geophy s ic a| Survey Given Any Ground in Canada. "No," Huggins said, I‘ll go down to Toronto and pick up some real players." So a day or two later Huggins startâ€" ed for Toronto. At about the same time Conny Smythe of Toronto Maple Leafs and Coach Powers of the Stars joined their At the end of the season, the "boys" called in Al Huggins. "We want a good senior team next year. Better start making your plans now," they suggested. "How about trying Doran with the seniors," someone proposed. But Huggins turned thumbs down on this suggestion. ‘"Doran," he said scathingly, "why that gawky kid will never make the erade." Ssouth Porcupine with the mining industry booming, takes its sports serâ€" iously. The "boys" are not averse to digging up a nugget or two to help some of the "amateurs" along. Last year South Porcupine had only a fair senior hockey team. It had a crack junior outfit, however. Bummer Doran and Mike Miller of the Stars were members of the junior outfit. You really can‘t appreciate the story unless you get out your atlas and find South Porcupine. It‘s way up in the wilds of Ontario, in the heart of the goldâ€"mining country, where they play their hockey on natural ice rinks with the temperature anywhere from zero to 50 below. (By Louis Kosoff) Have a laugh, you hockey fans, with Bummer Doran, scintillating leftâ€"wing recruit of the Syracuse Stars, and Coach Eddie Powers. Yes, sir, have a real laugh. It‘s on Al Huggins, who not so long ago patâ€" rolled a leftâ€"wing berth for Coach Powers with these selfâ€"same Stars. Al Huggins quit the Stars at the beâ€" ginning of last season to take a posiâ€" tion as hockey and baseball coach of the South Porcupine, Ont., senior amateur teams. You really can‘t appreciate the story unless you get out your atlas and find traced the desired formation over seyâ€" eral thousard acres of the property of Mineral Estates, Ltd. Correlated with the surface data and close study of the geology, it is now possible to plan a diamond drilling campaign with conâ€" fidence that veih structures and ore results will be forthcoming. Hence, with every expectation of success, Minâ€" eral Estates, Ltd., now enters an adâ€" vanced stage of exploration and, conâ€" sidering the vast amount of favourable ground to be developed, places itself among the most absorbing mining ven. tures in Canada. The following is from a recent issue of The Postâ€"Standard, of Syvracuse, N. Doran‘s Great Play Costly for Huggins We‘ve searched for the best of the oldâ€"time recipes . . . added choice delicacies from far lands . . . and arranged a menu that the whole family will enjoy. The HUB‘S usual fine service and reasonable prices makes dinner here even more delightful. Pin e St. N 0 rt h Bring The Family Here For New Year‘s Dinner The Golden Hub MEET YOUR FRIENDSs HERE (From Northern: Miner) Working in Hoyle, in the eastern part of Porcupine area and beyond Pamour, Ventures Limited is getting good reâ€" sults which, while interesting and enâ€" couraging, are not yet quite conclusive. Two diamond drills are at work and the present plan is to continue exploration for two or three months more, then decide whether underground work at that time is justified. There might be a tonnage of $7 ore, if the good reâ€" sults in the good holes could be correâ€" lated. Ventures owns the ground outâ€" right and therafore is not under any optionâ€"term necessity of proceeding with shaft sinking. The company is carrying on quite a bit of exploration work across the north country, including the exploring of a couple of prospects between the Cadillac and Rouyn districts. wEpNESDAY, DEC ~\tas Howey CGold Mines Limited has deâ€" clared a dividend of 2¢ per share payâ€" able February 1, 1937, to shareholders of record December 31, 1936. The disâ€" tribution will make a total of 4c for this year, the previous payment having been on August 8. The aggregate since the commencement of dividends is thus 19¢c per share. The initial disbursement was 3c on February 20, 1934, and sucâ€" ceeding payments have been: 3¢, July 2, 1934; 4¢, December, 1934; 3¢c, May 1, 1935; 2¢, December 14, 1935; 2¢, August 8, 1936; 20 February 1, 1937. Highly effic¢ient methods mark the operation of the Howey Gold Mines, the company making profits of a very low grade of ore. For the nine months ended September 30, the total recovery was $958,831 from 394,0554 tons of ore, or an average gradeâ€"per ton of $2.44. The aggregate recovery for 1935 was $1,332,950, and the average grade $2.75 per ton. Interesting Results in Work in Hovle District Howey Gold Mines Declares Dividend 2 Cents a Share pair of skates when Doran raps in one of those trick shots of his. It also may explain why Doran always skated back to Powers after he scores and says: "That‘s just one more for Al Hugâ€" gins, coach." The season is now only one quarter gone, and Doran has already regisâ€" tered nine goals and is one of the leadâ€" ing scorers in the league. Doran reported at the Torontoâ€" Syracuse training (amp at the beginâ€" ning of the seasot and promtly won himself a place in the Twinks‘ first line. And with the first games, he began to pop goals and figute in scoring plays. The whole story of Huggins and his bet got back to Bummer and to Coach Powers, which may explain why Eddie is as tickled as a yvoungster with his first "How come, Al" they asked, "that Doran isn‘t good enofigh for our senior club, but is good enofgh to get a Maple Leaf Huggins was still tkept:ical. "Listen," he said, ‘that kid won‘t get 10 goals all year in the International League. I‘ve got you fome real players." One of these real players, it develâ€" oped, was Huggins‘ lrother. The discussion hectic. It wound up with Huggins offering to bet anyone in the house that Doran would not get 10 goals in Jw entire season if he managed to stay with the Stars in the International League. Huggins promtly Iound some takers, to the extent of qetfexal hundred dolâ€" Y‘ | Powers suggested Dpran, Miller and Wilf Hannebury of theaSouth Porecupine junior team. The ree youngsters thrilled by the invitiétion, responded. It takes two days to get from South Porcupine to Toronté but the boys were there just as fgt as the trains would take them. In that first pracâ€" tice session Doran rapped home no less than 10 goals, as Pow@‘s tells the story. Smythe and Powert looked at each other sigrlificantly. Afew minutes after the practice they hadDoran‘s name on a contract. } Bummer wasn‘t loathe to spread the news when he returnyed to South Porâ€" cupine. The "boys" Ifarned of his proâ€" motion in short ord@. They called a hasty meeting with 4Â¥ Huggins. forces for a series of dfills preliminary to a western exhibitiony trip at the end of the season. Smithe thought it would be a good idea to try out Some youngsters he had beesg watching. Timmins