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       BY HEW CROMARTIE, M.A. 
		N the raw materials which 
		constitute the basis of industrial greatness, the Province of Ontario is 
		singularly rich. Her temperate climate and fertile soil not only assure 
		abundance of food for man and beast, but provide the necessary 
		conditions for rearing the domestic animals in the greatest vigour and 
		excellence; her forests of pine, spruce and hardwood maintain a great 
		industry in the manufacture of sawn lumber, square timber, pulp wood and 
		furniture; and to the patient fisherman her great lakes and inland 
		waters yield a bountiful return. But it is not so generally known that 
		in her mineral wealth Ontario possesses resources quite as needful to 
		the upbuilding of a nation as those contained in her fields, her forests 
		or her fisheries. The fact remains that with one or two important 
		exceptions all the commoner minerals are found in great profusion within 
		her borders, and many other substances of less frequent occurrence but 
		great usefulness in the arts and industries. 
		The geology of Ontario is 
		confined for the most part to the formations of the azoic and palaozoic 
		ages, and there is therefore not the great variety of rocks found in 
		some other countries; but the Huronian series, which is pre-eminently 
		the mineral-bearing formation, is extensively developed north of the 
		great lakes, and there furnishes deposits of iron, nickel, gold, copper, 
		silver and zinc, etc., while in eastern Ontario related rocks supply 
		gold, arsenic, corundum, mica, felspar, apatite, talc, graphite, iron 
		pyrites and lead. In the south-western peninsula the Devonian and 
		Silurian formations yield petroleum, natural gas, salt and gypsum. 
		Granite, trap, limestone and sandstone are quarried from the earlier 
		formations for building and other purposes; shell marl of more recent 
		geological date, found in the beds of dried-up lakes, is used in the 
		manufacture of cement; clays of various origin are used extensively in 
		the making of bricks and pottery, and an Old World industry in the 
		utilization of peat for fuel purposes bids fair to establish itself in a 
		new form on the bogs of Ontario. 
		Probably the most 
		important of all minerals is iron, and it has long been known that 
		Ontario has large stores of magnetite and hematite in the eastern 
		counties and also in the territory north and west of the great lakes. 
		For years the operation of various causes, including a hostile tariff in 
		the United States, retarded the development of the iron mines of Ontario 
		and the establishment of an iron- making industry. Until lately the pig 
		iron requirements of our manufacturers had to be met by importations, 
		which formerly came mainly from Great Britain, but of late years mostly 
		from the United States. All this is now rapidly being changed. There are 
		three blast furnaces in operation, one at Hamilton, one at Deseronto, 
		and a third at Midland, while five more are in course of 
		construction—four at Sault Ste. Marie and one at Collingwood. Two of the 
		existing furnaces and three of those under construction are designed to 
		use coke as fuel, while one of those now in operation and two being 
		built are for the manufacture of charcoal iron. The output of pig iron 
		in 1900 was 62,386 tons, valued at $936,066; for 1901 it was 116,370 
		tons, worth about $1,701,703. 
		When the furnaces began 
		work most of the ore they used came from the American side of lake 
		Superior, but the discovery of the great Helen mine on the east shore of 
		that lake in 1898, and its development by the Clergue syndicate, soon 
		furnished the coke furnaces of Ontario with ample supplies of native 
		hematite ore of good quality. The establishment of a bounty on iron ore 
		by the Provincial Government, and on pig iron and steel by the 
		Government of the Dominion, have played a material part in the growth 
		and prosperity of the iron business of Ontario. 
		During the past season 
		there has been great activity in searching for iron ores, and many miles 
		of "iron ranges" have been located in the neighbourhood of lake Temagami 
		and north and west of lake Superior, very similar in their geological 
		conditions to the famous Mesabi and Vermilion ranges of the American 
		side of the latter lake, which, it is not too much to say, have 
		revolutionized the iron business of the world, and transferred the 
		supremacy in iron and steel from Europe to the United States. Strong 
		hopes are entertained that careful investigations will discover similar 
		ore bodies on the Ontario side. The output of iron ore in this Province 
		in 1895 was nil; for 1901, the production will be about 300,000 tons, 
		valued at the pit's mouth at about $325,000. 
		In the deposits of nickel 
		ore situated in the Sudbury region north of lake Huron, Ontario 
		possesses one of the two sources of the world's supply of this important 
		metal. It occurs here in pyrrhotite in which part of the iron has been 
		replaced by nickel, the ore usually carrying copper as well as nickel in 
		varying proportions, but as a rule about two per cent. of each. The ore 
		bodies do not exist as regular veins with well-defined walls, but rather 
		as lenticular masses at or near the contact line of the granite and 
		diorite, or in the diorite itself, some of these masses being of great 
		size. A find recently uncovered by the Canadian Copper Company, called 
		the Creighton mine, bids fair to develop into the largest body of nickel 
		ore yet opened up in the district. In the Copper Cliff, one of the first 
		and most extensively developed of Ontario nickel mines, a depth of about 
		1,000 feet on the incline has been reached. Mining began about fifteen 
		years ago. The ores were at first worked for their copper contents, but 
		difficulties experienced in their treatment led to the discovery that 
		they carried nickel as well. 
		The Canadian Copper 
		Company, of Cleveland, Ohio, at Copper Cliff, and the Mond Nickel 
		Company, an English concern at Victoria Mines, are the chief producers 
		of nickel. Both companies bring the ore to a rich matte, containing 
		about eighty per cent. of nickel and copper, at their works in Ontario. 
		The final separation of the metals is effected in the one case in the 
		United States and in the other in England. Recently the Lake Superior 
		Power Company, whose president is Mr. F. H. Clergue, has entered the 
		field, and is vigorously developing the Gertrude and Elsie mines. Roast 
		heaps and smelting works to treat the ores from both properties are 
		being erected at the Gertrude mine, from which, also, selected ore rich 
		in nickel and carrying little or no copper is shipped to Sault Ste. 
		Marie for the manufacture of ferro-nickel. The nickel industry is 
		rapidly expanding, and under the stimulus of an active demand and high 
		prices, business during the past year was unusally brisk. In 1900, the 
		output of nickel-copper matte was 23,448 tons, equal to 3,540 tons of 
		nickel and 3,364 tons of copper. For 1901 the production will be 
		considerably larger. 
		The gold-producing areas 
		of Ontario are in the east and west portions of the Province. The 
		eastern field lies mainly in the County of Hastings, where there are 
		both free-milling and refractory ores. The latter owe their 
		rebelliousness to the presence of arsenic; indeed, this constituent 
		predominates to such an extent as to make some of the deposits more 
		valuable for arsenic than for gold. The difficulty formerly experienced 
		in treating these mispickel ores has now entirely disappeared, and 
		arsenic is being produced in Hastings county, of first-rate quality, at 
		the rate of about eighty tons per month. In western Ontariothe gold is 
		found principally in quartz veins carrying variable proportions of 
		pyrites and other concentrating minerals. For the most part the ores are 
		low in grade, but many of the deposits are of unusual size, and the 
		abundance of water and wood and other facilities for treating them 
		bespeak for the gold industry in this part of Ontario a notable future. 
		The yield for the Province in 1900 was 18,767 ounces, valued at 
		$297,861, and for 1901 it will be about the same. 
		Copper was one of the 
		first of Ontario minerals to be won on a large scale. The old Bruce 
		Mines on the north shore of lake Huron forty years ago were worked 
		extensively, and yielded several million dollars' worth of metal. A 
		revival of copper mining in this and other districts is now in progress. 
		The Bruce Mines themselves have been put in commission, though work has 
		again been temporarily suspended, and at Rock Lake, thirteen or fourteen 
		miles distant, Massey Station and Desbarats on the C.P.R., at points 
		near Sault Ste. Marie and elsewhere, deposits of purely copper ore are 
		being opened up. 
		The famous Silver Islet 
		mine, situated on a tiny island in Lake Superior, not larger than a 
		good- sized ball-room, yielded in its day many million dollars' worth of 
		silver, but has now been under water for years. Deposits on the mainland 
		were worked with much vigour until a fall in the price of silver 
		rendered mining unprofitable. In recent years work has been resumed on 
		some of the properties near Port Arthur, with satisfactory results to 
		the owners. The silver occurs in quartz and calcite veins in slate rocks 
		of the Animikie formation in the form of native silver and sulphides, 
		chiefly argentite. The rich ore is sacked and shipped as it comes from 
		the mine, while the leaner ores are stamped and concentrated before 
		being sent away. The yield of silver in Ontario for 1900 was 160,612 
		ounces, worth $96,367. 
		In eastern Ontario is 
		found mica, both phlogopite and muscovite, but chiefly the former. 
		Demand from makers of electrical machinery has led to considerable 
		production, which fluctuates from year to year according as prices go up 
		and down. North of Kingston, and in the neighbourhood of the town of 
		Perth, are fields from which a large yield of mica would come steadily 
		if the market called for it at remunerative prices. The deposits are 
		pockety and irregular, like those of mica in whatever part of the world 
		it is found. The production in 1900 was 643 tons, worth $91,750. 
		A new substance has 
		recently been added to the list of Ontario's mineral products. As an 
		abrasive, corundum has long enjoyed high repute, but its existence in 
		Ontario in commercial quantities was not suspected till 1896. A 
		mislabelled crystal in a collection of specimens purchased by a member 
		of the geological survey staff at Ottawa, led to the discovery of 
		immense bodies of corundum-bearing rock in the counties of Renfrew and 
		Hastings- doubtless the largest yet made known in the world. Tests 
		proved the mineral to be of first-rate quality, and its exploitation has 
		been entered on with energy. Crushed and graded corundum is being put on 
		the market in all the required sizes of grains, well cleaned and free 
		from injurious ingredients, and the manufacture of corundum wheels has 
		been begun. The crystals occur in all sizes, from that of a thimble or 
		cruet-bottle stopper to a sledgehammer, in a pegmatite or syenite matrix 
		accompanied by a small percentage of magnetite. In the county of 
		Peterborough, corundum is also found, and specimens have been picked up 
		of an ultra-marine blue tint, which encourages the hope that sapphires 
		or rubies like those of Burmah may yet be discovered. 
		Graphite is being 
		produced from the Black Donald mine, a deposit in Renfrew county, 
		felspar from Frontenac, talc from deposits near Madoc, while apatite, or 
		phosphate of lime, though found in eastern Ontario of first-rate 
		quality, has been put out of production by the more cheaply-mined 
		phosphates of the southern States. 
		The agricultural 
		districts of older Ontario are not usually associated with mineral 
		deposits or products, yet the yearly output of petroleum from the oil 
		fields of Lambton County approaches in value to that of pig iron at the 
		present rate of production, and forms the basis of a very important 
		industry. 
		The wells are mostly of 
		small capacity, yielding not more than one-quarter or one-third of a 
		barrel of crude per day; but they are very numerous, perhaps ten 
		thousand in all, and are economically worked by means of a "jerker" 
		system of pumps. The oil is obtained from the Corniferous limestones at 
		a depth of 460 or 470 feet, and though containing a greater proportion 
		of sulphur than the Pennsylvania petroleum, yet yields, under modern 
		methods of treatment, an illuminating fluid equal to the best. 
		The counties of Essex and 
		Welland contain two natural gas fields, from which large quantities of 
		gas are yearly taken, the yield in 1900 being valued at $392,823. In 
		both fields the flow comes from the Silurian rocks—in Essex from the 
		Guelph dolomite, and in Welland from the Guelph dolomite, Clinton 
		limestone, Medina sandstone and Trenton limestone. 
		A large part of the gas 
		from both localities has, in the past, been piped across the border line 
		and consumed in Buffalo and Detroit, but the Ontario Government has 
		within the past few months revoked the license of occupation of part of 
		the Detroit river-bed, under authority of which the gas was sent over to 
		Detroit, and has thus brought the exportation from the Essex field to an 
		end. 
		That the counties 
		bordering on the eastern shore of lake Huron —Bruce, Huron and Lambton 
		were once at the bottom of a salt lake or sea is proven by the great 
		beds of chloride of sodium, otherwise common salt, which are found in 
		the lower part of the Onondaga formation at a distance of about one 
		thousand feet from the surface. This process of deposition may be seen 
		going on at the present time in many parts of the world, notably at Salt 
		Lake, Utah, which receives the waters of four large rivers but 
		discharges none, the equilibrium being maintained by evaporation, which 
		leaves the solid constituents behind. The principal of these is salt, 
		and the water having become saturated with this mineral, the excess is 
		deposited at the bottom and in shallow places at the sides of the lake. 
		From the Ontario wells the salt is pumped in the form of brine, which is 
		led into pans and there evaporated. The resulting article is of 
		excellent quality, and in the beds of the lake Huron district there is 
		ample supply for all the needs of the country for many thousands of 
		years. 
		The Government of Ontario 
		recognizing the importance of the mineral industry to the Province has 
		adopted a policy of lending it every legitimate assistance and 
		encouragement. The mining laws are acknowledged to be fair and even 
		liberal. No royalties of any kind are exacted, and the prices of mining 
		lands are very low, the highest rate being $3.50 per acre. On the other 
		hand, development being the object aimed at, the law requires that 
		certain expenditures be made upon the land—at least $6.00 per acre 
		during the first seven years after title is issued. The prevailing form 
		of tenure is leasehold, payment of $i.00 per acre being required for the 
		first year, and from 15 to 30 cents per acre for subsequent years, 
		according to distance from a railway. The lease is for ten years, on the 
		expiry of which time the lessee is entitled to a grant of the land 
		without payment if he has complied with the law. 
		Direct aid is given to 
		the iron mining industry in the form of a bounty on: iron ore raised and 
		smelted within the Province, the rate of bounty varying from year to 
		year according to the quantity of ore mined and smelted, but not 
		exceeding $1.00 per ton of the pig iron product of the ore. A fund of 
		$125,000, called the Iron Mining Fund, has been created by the 
		Legislature for purposes of these payments, out of which aid to the 
		extent of $25,000 may be disbursed annually. 
		Indirectly the Government 
		aids the mining industry in many ways. The Bureau of Mines was 
		established in 1891 to promote the development of the mineral resources 
		of the Province, and it has since been actively engaged in collecting 
		and disseminating information respecting the mineral wealth of Ontario 
		and the output of minerals, in examining and mapping promising fields of 
		discovery, and in drawing the attention of capitalists and others to the 
		opportunities afforded for investment in mines and mining properties. 
		The yearly reports of the Bureau are in strong demand, and have proven 
		very useful in promoting the development of mining in the Province. 
		Another practical step was the establishment of an Assay office, located 
		at Belleville, where prospectors and others may have samples assayed and 
		examined at very moderate charges. In the chief mining districts local 
		agents have been appointed for the purpose of supplying information as 
		to granted and ungranted lands and otherwise assisting prospectors in 
		their work. 
		In the Sault Ste. Marie 
		and Michipicoton regions great results have followed the policy of the 
		Government towards the newer portions of the Province, in increased 
		activity in mining as well as in other industries. The opening up of the 
		great deposits of hematite at Michipicoton by Mr. Clergue and his 
		associates has led directly to the building of four blast furnaces (now 
		under erection) at Sault Ste. Marie where the ores are to be smelted, 
		and to the construction of an immense steel plant at the same place, 
		which is almost ready to begin operations. Ferro- nickel is also being 
		made there from nickel ore brought from the Gertrude mine, the sulphur 
		contents of which are used in the manufacture of sulphide wood pulp. 
		Charcoal and coke ovens form part of the Sault Ste. Marie programme, and 
		will convert the wood and coal respectively into fuel for use in the 
		furnaces on the spot. A large plant for the pro duction of bleaching 
		powder and caustic soda from salt brought thither from Windsor is 
		running very successfully. All these industries derive their motive and 
		electric power from the falls of the St. Mary river, which forms the 
		outlet of lake Superior, the energy already developed and in process of 
		development being about 95,000 horse-power. 
		The opening up of 
		northern Ontario is a task to which the Government of the Province has 
		definitely committed itself, and useful minerals form no small share of 
		the dormant wealth of the Crown domain. To bring about their 
		development, to convert the uninhabited wilderness into scenes of busy 
		industry, and to found in new Ontario communities which in their 
		solidity and progressiveness will equal those of the old, is an ambition 
		worthy of any government, and all patriots will wish it a successful 
		issue.  |