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This item is filmed at :he reduction ratio checked below/ Ce document est film* au taux de reduction indiqu* ci-dessous. lUA ^^j^^ 14X 18X 22X 26X 30X 1 12X 16X 20X 24X 28X 32X The copy filmad bar* hat baan raproducad tbanka to tba ganaroaity of: L^islature du Quebec Qu6bec L'axamplaira film* fut raproduit grica A la g4n4roaitA da: Legislature du Quebec Quebec Tha imagaa appaaring hara ara tha baat quality poaaibia considaring tha condition and laglbility of tha original copy and in icaaping with tha filming contract apacificationa. Original copiaa in printad papar eovara ara fllmad baginning with tha front covar and anding on tha laat paga with a printad or illuatratad impraa- sion, or tha bacic covar whan appropriata. All othar original copiaa ara filmad baginning on tha firat paga with a printad or illuatratad impraa- aion, and anding on tha laat paga with a printad or illuatratad impraaaion. 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A.jr * 'I QUEBEC: PRINTED AT "LE CANADIEN" OFFICE, 21, Mountain Hill, Lower Town. 1866. — 4 — basin an area of 400,000 square miles, of which ab-)ut 70,000 belong to the United States. The re- maining 330,000 square miles constitute the pro- vince of Canada. With the exception of about 50,000 square miles belonging to Lower Canada, and extend- ing from the line of New York to Gasp6, the whole of this territory lies on the north side of the St. Lawrence and the great lakes. On either side of the valley of the lower St. Lawrence is a range of mountainous country. These ranges keep close to the shores for a considerable distance up the river ; but about 100 miles below Quebec where the river is fifteen miles wide, the southern range begins to leave the margin, and opposite to Quebec is thirty miles distant. From this point it runs in a more southwestern direction than the river valley, and opposite Montreal is met with about fifty miles to the southeast, where i^ enters Vermont, And is there known as the Green Moun- tain range, which forms the eastern limit of the valley of Lake Champlain. In Canada, this range, stretching from the parallel of 450 north latitude to the Gulf, is known as the Notre-Darae Mountains, but to its northeastern portion, the name of th.e Shickshock Mountains is often given. The flank of the northern hills, known as the Laurentides, forms the north shore of the river and gulf, until within twenty miles of Quebec. It then recedes, and at the latter city is already about twenty miles distant from the St. Lawrence. At Montreal the base of the hills is thirty mileS in the rear, and to the westward of this it stretches along the north side of the Ottawa River for about 100 miles, and then runs southward across both the Ottawa and the St. Lawrence, crossing the latter river a littic below Kingston, at the Thousand 5 — ;^3larlds, and entering New- York. Here the Laucen- tides spread out into an area of aboiit 10,000 square miles of high lands, known as the Adirondack country, and lying between the Lakes Ghamplain. and Ontario. The narrow belt of hill-country which connects the Adirondacks with the Laurentides north of the Ottawa, divides the valley of the St. Lawrence proper from that of the great lakes, which is still bounded to the north by a continuation of the Laurentides. The base of these from near Kingston •runs in a western direction, at some distance in the rear of Lake Ontario, until it reaches the southwest extremity of Georgian Bay on Lake Huron ; after which it skirts this lake, and Lake Superior, and runs northwestward into tlie Hudson Bay Terri- tory. This great northern hill-region consists of the oldest known rock-formation of the globe, to which the name of the Laurentian system has been given, and occupies, with some small exceptions, the whole of the province northward of the limits just assigned. We shall designate it as the Laure;nt.ian Region. Over a amail portion of this area, along Lakes Huron and Superior, and farther eastward on Lake Temis- caming is another series of rocks, to which the name of the HHronian system is ^iven. But as the country occupied by these rocks is^eographically similar to the Laurentian, it is for convenience here inclu(led with it. To the south of this region the whole of Canada west of Montreal, with the exception of the narrow belt of Laurentian country described as running southward across the Ottawa and St. Lawrence Bivers, is very level. The same is true to the east- ward of Montreal until we reach the Notre-D^me range of jjiiils, already described |is passirig sputh- ward ifltp yermont, and in its north-eastern exten- — 6 — sion as bounding the lower St. Lawrence valley to tlie south. This valley may be regarded geographic ally as an extension of the great plains of western Canada and central New-York, with which it is connected through the valley of Lake Champlain. This level country to the south of the Laurentides in the two parts of the province is occupied by sim- ilar rock formations, and constitutes the Champaign RECiON of Canada, the surface of which is scarcely broken, except by a few isolated hills in the vicinity of Montreal, and by occasional escarpments, ravines,* and gravel ridges farther westward. The next area to be distinguished consists of the No tie-Dame range on the south side of the St. Law- rence which forms the belt whose course has just been described, with an average breadth of from thirty to forty miles. To the south and east of this, is a district of undulating land, which extends to the boundaries of the province in that direction. These two districts may for convenience in farther descrip- tion be classed together, and they embrace the re- gion which is generally known as the Eastern Townships. By this term they are distinguished from the Sei&nioiues, which bound them to the north and west. To the north-east however, along the ChaudiereRivei, some few seigniories are fou«d within the geographical limits of this third region. The whole' of the province is well watered witJi TAimerous large and small rivers, and in the moun- tainous districts there are great numbers of small lakes, more thar 1,000 of which are represented on the maps. We have in the preceding descriptions divided the country into three distinct regions, and have next to consider the geological structure of these as re- lated to the soil and to agricultural capabilities. — 7 I. THE LAUBENTIAN BEGION. The great tract of country occupied l)y the Lau- ren tian rocks has for its southern boundary the limits already assigned, and stretclies northward to the boundary of the province, which is the heiglit of land dividing the waters of the St. Lawrence basin from those of Hudson Bay. Its area is about 200,000 square miles, or six tenths of the whole land of the province. This region is composed exclusively of crystalline rocks, for the most part silicious, or gra- nite-like in character, consisting of quartzite, sye- nite, gneiss and other related rocks. These are broken up into ridges and mountain peaks, gene- rally rounded in outline and covered with vegeta- tion. The summits in the neighbourhood of Quebec are some of them from 2,000 to 2,500 feet in height, and in other parts attain 4,000 feet o"r more ; but the general level of this region may be taken at about 1 ,500 feet above the sea, although it is much less in the narrow belt which crosses the province east of Kingston. Through the hard rocks of this region run numerous bands of crystalline limestone or marble, which from their softness give rise to val- leys, often with a fertile soil. The hill-sides are generally covered with little else than vegetable mould, which sustains a growth of small trees, giving them an aspect of luxuriant vegetation. But when fire has passed over these hills, the soil is in great part destroyed, and the rock is soon laid bare. In the valleys and lower parts of this region how- ever, there are considerable areas of good land, having a deep soil, and bearing heavy timber. These are the great lumbering districts of the couitry, — 8 — tL'om wlii.-li vast (l"a"'ili'» »f 'i">b»'-' '='"*'''^ P'""' are auuually oxporlod, and coiistitalo a great s»u,-co woaltU to the pvovi"ce. Tl.e,., valleys ave w. most cases alou? tUo line of the bands ot limestouo wlioso runt contribute umcU to the tort.lity of the »0,1. Lines o! settled .'onutry fuuning many mtlos .uto «,e wilderness are fotuid to follow these beta of soft calcareous rock. The settlements in tl-.is region are along Us =outh. ern border, and at no great altitude above the sea. n the higher parlo, the rigor of the chmate scarcely p rnUs the cultivation of cc-eals. It is probable that To great portion of this immense region w.ll ever bo colonized! but that it will remain tor ages to como o«>red with forests. These, j£ husbanded wj^. due care will remain a perpetual source of timber for ZVe of the country and tor exportation ; besides a^orf ng, with proper facilities tor transportation, arabundaut supply ot fuel to the more thickly seU tied districts, where the forests have nearly disa^ Beared, and where from the severity of the long wU ter^, an abundant supply ot fuel is o the firs Te essi Y There are other reasons why this great Cstregion should be protected. The vegetation, andtlesoil which now cover the hillsides play a most important part in retaining the watei.wluc here fall in the shape ot ram or snow. But .ui uo^s covering ot soil, the rivers and mllUtreams which hTe take thei rise, would like the streams of so" hem France, and of the north ot Italy, be destruc- tive torrents at certain seasons and almost dried^up hLnels at othei.. The effect ot this S-at wood d area in tempering the northern winds, and modeiat ing the extremes of climate is not to be overlooked in estimating the value ot the Lau'^"''^" "«'»"' which moreover as will be shown farther on, con- ? -0- lams iiiexhaustibl.i minen of rioh .ron ovcft, bosides copper, lead, marble^ and oUior mineral substances of economic importaiictv n. THE EASTERN TOWNSilU'S. Under this bead, as already explalnod, Is incliid.?d the belt of hill-comitry south of the St. Lawrence, with the region on its southeast side extending to tho frontier, and forming a succession of valleys, which may be tiaced from tho head-waters of tho Connecti- cut northeastward to the Bay of Chaleuts. Tt ,, true that the Eastern Townships, as now known, do not embrace this northeastern extension ; but as it belongs to them both geographically and geologically it may be conveniently included with them. The area whose limits are thus det\ned forms about one-tenth of the province. The hills of the range which traverses it are composed, like those of the Laurentian region, of crystalline rocks; but these are softer than the greater part of the rocks on the north shore, and yield by their wearing-down a more abundant soil. Some of tho hills in this range .attain an elevation of 4,000 feet above the sea, and the principal lakes in the valley on the southeastern Bide^Memphremagog, Aylmer, and St. Francis^^ from 750 to about 900 feet above the sea-level, llu. region is well wooded, and when cleared is ound in most parts to have an abundant soil, generally sandy and loamy in character, and well fitted for grazing and for the cultivation of Indian corn and other grains. Great attention is now paid to the raising of cattle, and the growing of .Jool, and within the last few years the best breeds of sheep have been sue- — 10 — cessmlly introduced from England and from Ver- mont. Draining and improved methods of farming are in many parts practised, and the agricultural importance of the sout'^orn portions of this region is yearly increasing. The Eastern Townships moreover abound in metallic ores, marbl6s, slates, etc., v/hicli will be noticed in their place. I \- in. I » THE CHAMPAIGN REGION. The limits of the great plains ul Canada have al- ready been defined in describing those of the two proceediiig regions. These plains, which may be cal- led the champaign region, occupy about three tenths of the province, and are, as we have seen, diNidf "• into two parts by a low and narrow isthmus of Lau- rentian country, which runs from the Ottawa to the Adirondacks of New-York. To the eastward of this division, the present region includes the country between that river and the St. Lawrence, and all be- tween the Laurentides on the north and the Notre- Dame hills on the eoutheast ; while to the west- vvard it embraces the whole of ihe province south of ^le Laurenlian region, including th. great area lying between the Lakes Ontario, Erie and Huron, gene- rally known as the southv/estern peninsula of Canada^ The whole of this region from east to west is essen- tially a vast piai.i, with a suficient slope to allow of easy drainage. The distance from Quebec to the west end of Lake Superior is about 1,200 miles, yet ■this lake is only 600 feet above the sea-level, while Lake Erie is 565 fe?t, arfd Lake Ontario 232 feet v. hove the sea. The land on the banks of the St. Law- rence and its kkee, either near the margin, or not - 11 -^ very fai* removed, generally rises to a height of front fifty to one hundred and fifty feet, and from this 16vel very gradually-ascends to the base of the hills which bound the region. Unlike the two regions already described, these great plains are underlaid by beds of unaltered Silu- rian and Devonian rocks, consisting of sandstones, limestones, and shales. These are but little disturbed, and are generally nearly horizontal ; but over by far the greater part of the region they are overlaid by beds of clay, occasionally interstratified with or over- laid by sand and gravel. These superficial strata, which are in some parts several hundred feet in thickness, are throughout the eastern division, in great part of marine origin, and date from a time when this champaign region was covered by the waters of the ocean ; while throughout the western division the clays are more probably of fresh-water origin. ■ It results from the distribution of these superficial postrterii^ry strata, that the soil over the greater part of the region consists of strong and heavy clays, which in the newly cleared portions are overlaid by a considerable thickness of vegetable mould. In the eastern division, a line drawn from Quebec to Ottawa, and two others from these points, converging at the outlet of Lak<^ Ghamplain, will enclose a triangular area of about 9000 square miles, which is very nearly that^ occupied by the marine clays. These are over- laid, chiefly around the borders of this space, by more sandy deposits, which are well seen near Three Ri- vers, and abciit Borel. They form a warm but light soil, which yields good crops when well manured, but is not of lasting fertility. The greater part of this area however is covered by a tenacious blue clay, often more or less calcareous, and of great depth, which constitutes a strong and rich soil bearing in I' — 12 — abundance crops of all kinds, but particularly adapt- ed for wheat, and was in former times noted for its areat fertility. These clay lands of Lower-Canada,, have been for a long time under cultivation, and by repeated cropping with wheat, without fallow, rota- tion, deep plowing, or manure, are now in a great many cases unproductive, and are looked upon as worn out or exhausted. A scientific system of cul- ture which should make use of deep or sub-soil ploughing, a proper rotation of crops, and a judicious appUcation of manures, would however soon restore these lands to their original fertility. The few trials which within the last few years have been made m tbe vicinity of Montreal, and elsewhere, have sufficed to show that an enlightened system of tillage, with sub-soil draining, is eminently successful in r^stormg these lands, which offer at their present prices good inducements to skilled farmer*. Besides grain and green crops, these soils are well fitted for the culture of tobacco, which is grown to some extent in the vici- nity of Montreal. Notwithstanding the length of the winter season in Canada, the great heat and light of the summer, and the clearness of the atm^ospjiere enable vegetation to make very rapid progress. The mineral resources of this champaign region of Eastern Cknada are chiefly confined to stones for building, paving, lime and cement, stone for glass- making, and peat. Large peat-bogs are very nume- rous in various parts of this re-ion, and may be .nTade to furtish an abundant supply of fuel. This part pf the countr/ 1-. also remarkable for the great number and variety of its mineral springs. To the northeast of Quebec, besides the plams which border the river, there is a considerable area of low-lying clay land, cut off from t^e great St. Lawrence basin by Laurentian hills, and occupying ^13 — the valley of Lake St. John and of a pbi^tion of the Sa- guenay. Here is a small outlying basin of Lower Silurian rocks, Uke those ahout Montrea , and over- laid in like manner by strong and deep clays, which extent over the adjacent and little elevated por^on of the Laurentian rocks, and form a soil as well fitted for cultivation as any part of the lower St. Lawrence valley The valley of this lake is probably not more than 300 feet above the sea ; and from tbe sheltered position the climate is not more rigorous than that of Quebec. Several townships have within a few years been late out in this valley, and have attracted large members of French Canadians from the older parishes in the valley of St. Lawrence. The western part of the champaign region, com- mencing near Kingston and including all the south- ern portion of the western province is the most fertile and productive part Canada. Like the plains further eastward, its soils consists chielly of strJiig clays, overlaid here and there by loam, sand, and gravel. In the natural state nearly the whole of this region sup- ported a fine growth of timber, in great part of broad- kaved species, but presented however various local peculiarities. Thus, the banks of the Grand River from Gait to Brantford were remarkable for a sparse growth of oaks, free from underwood, and known as oak openings. These are said to have been pasture .rounds of the Indians, brought to this condition and kept in it by partial clearing, aad by the annual burn- in- of the grass. The object of this was to attract the d/erwho Ue to feed upon tbe herbage ^See on this point. Marsh's Man and Nature, page l37).The sml of these plains is a light sandy loam, very uniform in Character, and generally underlaid by coarse gravel. Though fertile, and of an easy tillage, this !nd similar soils will not support the long continued — 14 — cropping without manure, which is often practiced on the clay lands of both Upper and Lower Canada. The valley of the Thames, together with the rich alluvial flats which extend from it northwArd to the North Branch of Bear Creek, and southward nearly to the shore of Lake Erie, is remarkable for its great fertility, and its luxuriant forest growth. The soil is generally clay, with a covering of rich vegetable mould, and is covered in the natural state with oak, elm, black-walnut and white-wood [liriodmdron tulipifera) trees of large size, together with fine groves of sugar-maple. Towards the mouth of the Thames, and on the borders of Lake St. Glair is an area of natu- ral prairie of about 30,000 acres. It lies but little above the level of the lake, and is in large part overflowed in the time of the spring floods. The soil of this prairie is a deep unctuous mould, covered chiefly with grass, with here and there^ copses of maple, walnut and elm, and with willows dotting the surface of the plain. Numbers of half-wild horses are pas- tured here, and doubtless help to keep down the forest growth. The characters of the surface are such as to suggest that it had been at no distant period reclaimed from* the waters of the adjacent lake. In no part of the province have skilled labour and capital been so extensively applied to agriculture as m western Canada, and the result is seen in a gene • ral high degree of cultivation, and in the great quan- tities of wheat and other grains which the region annually furnishes for exportation ; as well as in the excellent grazing farms, and the quantity and quality of the dairy produce which the region affords. This western portion of the province, from its more southern latitude, and from the proximity of the great lakes, enjoys a much milder climate than the pther parts of Canada. The winters are compara- r :r r - r.T.— siaaK — 15 — lively short, and in the more southern sections the peach is successfully cultivated, and the chesnut grows spontaneously. The mineral resources of this region, like those of the eastern portion of the champaign district, are comparatively few. Besides building-stones, limej and cements, however, may be added gypsum and petroleum, both of which will be mentioned in Iheir proper places. It being the plan of this essay to notice in the first place those points in the natural liistory of the country which are connected with its agricultural interests, the supplies of artificial manures for the soil, and of peat for fuel may be here described. The building materials of the country will next be noticed, and finally the various ores and other mine- ral products which are the subjects of mining and manufacturing industry. ARTIFICIAL MANURES. In addition to the manures which are the produce of the farm, modern agriculture avails itself of various other materials which are capable of restor- ring to the soil the elements removed by tillage, or in other ways of promoting the growth of vegeta- tion. Of the more common of these materials, lime and gypsum, Canada contains an abundant supply. The further notice of locahties of lime, which is found almost everywhere through the province, is reserved for a subsequent page, under the head of Building Materials ; but mention may here be made of the deposits of white calcareous marl, which abound in a great many lakes and marshy grounds throughout Canada, and being pure carbonat'; of lime, constitute a valuable manure for soils la-^K ag this element. — 16 — OVPSUM. Gypsum is found in great abundance for a distance of about thirty-five miles along the Grand River in western Canada, and large beds of it are opened at Cayuga, York, Seneca, Brantford, and Paris, About 14,000 tons of gypsum are annually raised from these quarries, and are for the most part consumed in that portion of the province, as a dressing for the soil. It is chiefly ground at mills in the neighbour- hood, and sold in that state at from three dollars and a half to four dollars the ton, ( fourteen to sixteen shillings sterling). Some of this gypsum is however pure and white, and being fitted for use as stucco, commands a higher price. These quarries are si- tuated in the immediate vicinity of railways, which afford facilities for transportation. The gypsum con- sumed in Lower-Canada is chiefly brought from th(e Magdalene Islands in the gulf of St. Lavvre.ice. These contain abundant deposits of this mincri-l, which is brought by water to Quebec and Monireal The consumption of gypsum for agricultural pur- poses in Lower-Canada is however less than m the west, and might be increased with advantage. PHOSPHATE OF LIME. Among the most important discoveries of mocern scientific agriculture is that of the value of phos- phates as a manure. The beneficial effects of ground bones, and of Peruvif^n guano, of which last about 300,000 tons are annually brought to Great Britain, are in a great measure due to the phosphates which these manures yield to the soil ; and within a few years, the use of a soluble phosphate, or superphos- phate of lime as an application to the soil, has been so much extended, that its manufacture has become ( \ '! ( \ — 17 — a very important industry in Great Britain, France, Germany, and the United States, and has within the last few years been successfully attempted at Mon- treal. The phosphates employed for this purpose are bones, certain kinds of guano, and coprolites, the .lattei" a fossil form of phosphate of lime abun- dant in some parts of England and France. But the supplies of these materials being limited, and the sources in many cases remote, attention has been turned to the deposits of crystalline mineral phos- phate of lime (called by minoralogists apatite.) This substance is found to some extent in Norway and in Spain, and the investigations of the Geological Sur- vey have shown that it exists in abundance among the Laurentian rocks of Canada, forming veins, which have been met with in several places along the Ottawa, and more abundantly near Perth, upon the line of the Rideau Canal. Here, over an area of many square miles, phosphate of lime has been found in a great number of localities, several of which promise to yield abundant supplies of this mineral. The attention of speculators has been turn- ed to these deposits, which are in a locality favorable for working, and for exportation, and during the last year a New York company has expended a large sum of money in opening several veins of the phos- phate, with a view to extended mining operations. This mineral phosphate is richer than the coprolites so much used in England, and contains from thirty- five to foiHy per cent of phosphoric acid. The work- ing of these deposits is however undertaken solely with a view to exportation. In order to convert this mineral into superphosphate there is required a large quantity of sulphuric acid, a material which is not manufactured in the country, and can only be imported at a very considerable expense. As yet, the 2 4* ■*• value of the superphosphate as a manure is but UtUe known in this country^ Small quantities of it are however now manufactured at Montreal from bones, and the farmers of the country are beginnmg \o learn its importance. It is to be hoped that more enlightened notions of agriculture will soon so ^ciuch increase the demand for this article as to warrant the establishment of a sulphuric-acid manufactory, and the conversion into superphosphate for domestic use of a large portion of the mineral phosphates to be obtained in the province. Us employment will be one of the most efficient means of restoring the apparently exhausted wheat lands of Lower .Canada. FISH MANURE. A most important and hitherto neglected sour»e if valuahle manure is to be found in the great flshenes o£ the GultotSt-Lawrcncc. The use ot fisl for a manure is known in many parts ot tlie world, and Tre are small and mrerior kinds offish wh.chon the coast of the United P'ates are taken u. great quantities expressly tor *« P"'^!"'^''' *"*;,f f *^" nlled directly to the fields, or converted mto a con- t:fratd m/nure nearly equal inline to P-ma« «uano For this purpose they are cooked by steam, presto remove the water, and in the case of some Crot fish, a large quantity of valuable Oil, and flnallY dried and ground to powder. According to Payen, an eminent French authorUy the total yearly P™*"^* »' f « 7* ''"oO *, North American coast is not less than 1,500,000 tons ot fresh flsh. Ot this, the head and entraiU, equal to one halt the entire weight, are left to decay or are Town into the sea ; but it dried would yield more ,ni,i4a»tiai>iyv5g»Bi — 19- , but UtUe of it are om bones, inning \o ,hat more" a 30 ifiuch ;o wanant nufactory, r domestic >sphates to ment will : restoring of Lower ;d source t f cat fisheries f fisli for a w^orld, and h which on en in great id either ap- l into a con- to Peruvian d by steam, case of some lable oil, and ich authority, iheries on the 1,500,000 tons rails, equal to decay, or are Id yield more than 150,000 tons of a most valuable manure. The French fishermen have for several years had an esta- blishment for this manufacture at Kerpon, on the coast of Newfoundland, and export the product to France. The quantity of manure of this kind which might be manufactured in Canada and the Mari- time Provinces from the refuse of the fisheries, and from inferior kinds of fish which are now neglected, is very great, and this material might become a pre- cious resource both for exportation and for the en- riching of our own soils. PEAT The Eastern division of the champaign region of Canada abounds in peat bogs, which are generally distributed, and cover an area approximately esti- mated at from 120 to 150 square miles. In addition to this the island of Anticosti contains a still greater area. In many of these bogs on the main-land the peat attains a depth of ten to twenty feet, and even more; and, especially in their deeper parts, is often so compact as to sink in water when dried ; while it is at the same time very pure, yielding from four to six per cent of ash. No systematic attempts have hitherto been made to turn this material to use : but v/ithin the last few months proper arrangements have been made by an Englisfi. capitalist to compress, with the aid of proper machinery, the peat of an ex- tensive bog in Bulstrode, on the line of the Artha- baska Railway.— The success of this experiment will be a matter of very great im;>ortance for Canada. The wanton destruction of the forest in the older settled regions has made fire-wood scarce in a coun- try whose climate renders an abundant supply of fuel indispensable, and which contains no coal- mines within its limits. — 20 — ene of ths chief difficulties in the extensive work- ing of peat, arises from the obstinacy with which it retains a great amount of water. A large propor- tion of this must be removed by spontaneous drying, a process to which the summer climate of Canada is peculiarly favourable. According to Dr. B. H. Paul's late inquiries, it appears, that the heatrproducing power of good peat is about one half that of the weight of coal. It is claimed that by proper treat- ment peat -can be brought to the same density as coal itself ; and Dr. Paul concludes that where such peat can be furnished at four shillings sterling the ton, it may advantageously replace coal at ten shil- lings, as a fuel for generating steam, burning bricks, , etc. The price of coal in our markets is more than twice this, and it remains to be seen whether properly dried and compressed peat can be produced at two fifths the market price of coal ; in which case it may replace it with advantage on our inland steamers and railways, as well as for household use. It is said to have lately been employed with success as a fuel for the locomotives on the New York Central Rail- j way, and it is well known that peat is now largely employed for smelting iron in some parts of Ger- many. Viewed in the light of the foregoing conside- rations it can scarcely be doubted that the extensive deposits of peat which Canada contains are destined soon to become very important resources for the province. BUILDING MATERIALS. « Among the materials of first importance to a country are those required for the purposes of build- ing. Of these, besides the wood of the forests, may be mentioned clay for bricks, lime for mortar and cements, granites, sandstones, limestones, marbles, — 21 — and rooflng-8late9. Th*? principal sources of these materials in Canada may be briefly noticed. BRICK CLAV. Brick clay is met with abundantly in almost every part of the great champaign region of Canada, where there are few towns of any size in the vicinity of which bricks are not manufactured. That they are not more generally used for building is due to the fact that quarries of excellent and easily wrought stone are common throughout the province. Through the western division of the cliampaign country, and in the westernmost parts of the eastern division, as near Brockville, there is found a clay which yields white, yel'.owish or cream-colored bricks, which are much esteemed for building, and are carried to Montreal and Quebec. This clay is in many parts overlaid by another, which gives red bricks. From eight to ten million are yearly made at Toronto, of which perhaps one half are white bricks. These are sold at the kilns at from $5.50 to $6.00 the thousand, (twenty-two to twenty-four shillings sterling,) while the red bricks are worth from $3.00 to $4.00. At Mon- treal there are several brick makers, of which the two principal ones manufacture together about 12,000,000 of red bricks, the ordinary price of which is about $5.00 the thousand. Many of these clays are fit for coarse pottery and for tiles for agricultural draining, both of which are manufactured at numerous places throughout the province; while at Quebec glared earthenware pipes are extensively made for street and house drains. — 22 — LIMB. Limestone fitted for burning is found in great abundance in most parts of the champaign region, as will be seen when we come to speak of building siones. The use of lime as a ferlihzer for many soils is well known, and for this purpose the greater part of the limrs in the province, on account of their freedom from magnesia, are well fitted. About 270,000 bushels of lime are annually burned at Mon- treal, where its price is about seventeen cents (eight pence half-penny sterling) the bushel. Limestone is less abundantly distributed in the mountainous districts of Canada, where however geological research has shown its presence in very many loca- lities, e^cially in the Laurenlian country, where bands of limestone have been already mentioned as marking the course of numerous fertile valleys. Limestones are also found in many parts of the Eastern Townships. The property of forming a mortar which will harden under water, which belongs to hydraulic cements and water-limes, is possessed by the lime .yielded by many limestones in the country, as at Quebec, at Hull on the Ottawa, at Thorold near Nia- gara, and at various other places in the western peninsula. Materials from these sources have been used in the construction of the extensive hydraulic works of the province. ' BUILDING STONES. The abundance of good building stones in Canada is so great that it i;> easier to say where they are not found than to iiiU'-'inte tlieir various localities. Quebec, Montreal, Ott iv/a and Kingston are built of a grey limestone, wMch is quarried in their imme- t f T I ft I -28- diate vicinity, and ai*0«nds in a great many intfirme- diate localities, from which materials have been obtained for the canals and other public works. The stone required lor the great Victor.. i Bridge at Mon- treal was in a large part procured from Pointe Claire, a few miles above the city. Limestones and dolomites of euperior qualities for building purposes are met within agrentmany places in the region to the west of Lalift Ontario; which also yields in numerous lo- calitifis a ■superior sandstone, of which University College, Toronto, and many other of the public buildings of that city and of Hamilton are con^ Btructed. Good sandstones for building purposes are also met with among other places at several points on the Ottawa, at Sillery near Quebec, and in the more eastern parts of the* province. In the Eastern Townships, to the east of the Notre- Dame range, there are great quantities of granite of a superior quality for building purposes, and in many parts of the Laurentian region, granite, sye- nite, and syenitic-gneiss rocks abound, both red and gray in colour. Some of these materials are equal to the granites of Cornwall and of Aberdeen, and would yield materials for building and for decoration of great beauty and durability; but as they are both more costly to work than the abundant limestones and sandstones, and generally more remote from the great centres of consumption, they are as yet scar- cely made use of. MARBLES. The rocks of Canada afford a great variety of mar- bles. Some of the limestones of the Laurentian region afford a good white marble for building pur- poses and for tombstones, as at the Calumet, Por- tage du Fort, and Filzroy Harbour ; from which last — 24 — place marble has been obtained for the new Parlia- ment Buildings at Ottawa. Similar white marbles are also found in Beverley, Elzevir, and Marmora. These marbles are seldom very fine grained, but from the township of Barrie, marble'^ of a very fine texture, both white, and colored and variegated have been obtained, through from the remoteness of the locahly they have not yet been wrought. A bluish- grey veined marble, which like the preceeding is from the Laurentian region, is quarried near Arn- prior on the Ottawa, and another at Grenville of mingled green and white, containing serpentine, and: resembling the Gonnemara marble of Ireland. Simi- lar marbles abound in many other parts of the Lau- rentian country, but little has as yet been done to bring these and the other marbles of the country into use. The hills of the Eastern Townships afford many marbles of considerable beauty, as at St. Joseph and at Dudswell, the former red veined with white. At the latter place are beds of a cream colour and of grey, veined and mottled with yellow, and some- times with black. The serpentines of the Eastern Townships are also many of them of considerable beauty, being generally dark green, often veined with lighter green and white, and resembling in some cases the famous vcrd aiUtque, or some of the serpentines of Corsica and Cornwall. None of these materials, which abound in Melbourne, Orford, St. Joseph, and many other parts of this region, have as yet been cut, except for the purpose of exhibition ; although the same serpentines are extensively quar- ried in the neighbouring state of Vermont, and are highly esteemed. Many of the secondary limestones of the cham- paign country of Eastern Canada are susceptible of •? li t I \ \ ■r •,^ — 25 — a good polish, and present pleasing varieties of color. Good marbles, red, black, and various shades of brov^rn and grey, often agreeably variegated, may be obtained from them in a great many places in the vicinity of Montreal, but are as yet scarcely known, although well suited for internal decoration. Stones well fitted for flagging and paving are found in places too numerous to mention, throughout the province, but brick, and from its cheapness wood, is still to a great extent used for pavements in our towns. Paving-stones are however brought from the state of New-York and even from Scot- land, while materials probably in no way inferior are to be met with in many parts of the country. ROOFING-SLATES. Slates for the roofmg of houses have until recently been very little used in Canada, but extensive quar- ries in no way inferior to the best Welsh slates have within the lasf few years been opened in the Eastern Townships, on the line of the Grand Trunk Railway. Plates of great size cmd of excellent quality are here readily obtained. Similar slates are found in several other parts of the same region, and good roofmg-slates have also been obtained on the north shore of lake Superior. IRON ORES. The ores of iron are found in very large quan- tities in the Laurentian rocks of Canada at several localities on the Ottawa, along the Rideau Canal, and in the vicinity of Marmora. These deposits are of the magnetic species, and less frequently, of red hematite, both of which are very rich ores, con- taining about 70 per cent, of metal. They are similar to those which yield the fhie iron of Sweden, and W tliii)^ wbich are min^d oii this shores of Lake Ghamplain in New York. The ahseftce of mineral coal in Canada would render it necessary to use wood^charcoal for the smelting, of these ores, unless as before suggested, peat be employed for the pur- pose. The price of labor in most parts of the country so augments the cost of charcoal that the iron smel- ter here finds it diflficult to compete with foreign iron, and to this cause is to be attribnted the fact that the ores of Canada are not more extensively worked. The state of Michigan possesses on the southern shore of Lake Superior great deposits of red hematite ore, not unlike those of Canada, and within the last few years has exported large quan- tities of this ore to the vicinity of the coal mines of western Pennsylvania, where it is smelted. The value of the iron ore thus shipped is said to be at present about $2,000,000 annually, and the amount is increasing. A similar ore has lately been found in Canada, on the north shore of Lake Superior, and is about being mined by an American company for exportation to the United States. It has been at- tempted to send the rich ores from the Laurentian region of Canada to the American market, and it is probable that the plan may be successful, especially as some of these deposits are very adA antageously placed for transportation by water. Extensive beds of good iron ore occur in the Eas- tern Townships. They are iron-slates, consisting in a large part of red hematite, and although less rich than the ores already mentioned, might under favo- rable conditions be smelted with advantage, as has already been the case to a limited extent, the ore having been taken to Vermont. At various localities in the champaign region of Canada considerable quantities of bog-iron ore are Ww — Mw i i. ^ais^; •^^'^^i^.'-xam^jiima^^:-. — 27 — Matt t6 Thr^ RiVefrs thre 6re was siiielted f«r rhdi^lhkia century, and allhn ore is ^no- .erable qu*n- wnships, ai?d ite of potash, e arts for the i in various ^31 — glaaa-factory aow in suocessful pperation near Vau- dreuil, a few miles west of Montreal. The various refractory materials required for the construction of furnaces, and for smelting metals are not wanting in Canada. In many parts of the Laurentian region plumbago or black lead is found of a superior quality for the manufacture of cru- cibles. jars attracted • its supposed as moreover n the arts, is ly inexhaust- ron ore, both istern Town- ioned ores of carbonate of lications in a are pursued. id of various 'oral parts of or the New- ;e of barytes, 1 of pigments, several parts iss-making is le in several 1 in a large SOAP STONE. Soapstone which is used not only as a lining for furnaces, but in the United States for the construc- tion of stoves for domestic purposes, abounds in the Eastern Townships ; while sandstone for the hearths of furnaces, fire-clay, and moulding-sand are found in many parts of the province. MICA. Mica, which now finds so many applications in the arts, exists in the Laurentian region of Canada in abundance, and of an excellent quality. Thin shpots of tlip mineral of very large sizes are obtained, and it is already an article of export. As materials for •millstones, varieties of granite, and of hard quartzite rocks are made use of in va- rious parts of the province ; and in Grenville on the Ottawa a variety of silex precisely resembling the French buhrstone is found. Grindstones are made in many parts of western Canada from a sandstone well fitted for the purpose, while whetstones and honestones, some of them of superior quality, are found in a great many parts of the country. Superior stones for the purpose of lithography have been found in several localities in western Canada ; but although trials have shown them to be of an excellent quality, they have not yet been brouoht into use. :u -^ 32 — Among materiala for ornamental pui-poses may I)e mentioned agates, jaBpers, labrador feldspar, and por- phyries. In Grenville and in Chatham are found in great abundtince porphyries of fine texture, suscepti- ble of a high polish, and of various colors, rivalling in beauty the porphyries of the old world. PETROLEUM. Springs of petroleum or mineral oil occur in seve- ral localities in the southwestern part of Canada ; and from numerous wells sunk in Enniskillen, near Lake St. Clair, several millions of gallons were ob- tained in 1861-2. Since that time however the supply »f oil from the wells has greatly diminished. In other localities in this region, as at Bothwell, the existence of natural springs yielding a little petro- leum has led to the sinking of wells, which are yield- ing moderate supplies of oil. The part of the country he" e underlaid by the oil-bearing rock is very large, and it is not improbable that from some portions of it considerable quantities of petroleum may yet be obtained. At the other extremity of the province, in Gaspe, na- tural springs yielding small amounts of petroleum are found over a considerable area, and wells are being sunk in the hopes of obtaining it in available quan- tities. The oil in this region occurs in Upper Silurian rocks, while in southwestern Canada it belongs to the Lower Devonian limestones. These are supposed to be the source of the wonderfully productive wells of western Pennsylvania and the adjacent regions ; the estimated value of whose produce of petroleum for the current year is stated at not less than $75,- 000,000. Although the geological conditions have there been more favorable to the preservation and accumulation of the oil than in Canada, jt is pro- bable from the results lately obtained in Bothwell, — 33 — that wolls in this region may bo made to yield satis- factory rotiims. The narrow lirr its assigned to the writer of this essay, which he has prepared at the request of the Minister of Agriculture, have permitted nothing more than a notice of some of the more important mineral resources of the province ; and the reader who may be desirous of farther information upon these sub- jects, and also of more detailed chemical descriptions and analyses of the soils of the country, is referred to the work already indicated as the source of the information here given, viz the Geology of Canada. T. STERRY HUNT. + , I ' ' U.iM.-iint-Mt-.mt ' .i ' mnf ' ni mm CONTENTS I I Pares. GtooRAPHicAL Description.... 4 Laure.vtian Reqion.— Soil, Climate, Forests 7 Eastern Townships — Soil, Climate, Agriculturo 9 CiiAMPAioN Region kj Eastern Division: Soil, Agriculturti, &c n Lake St. John aHtl Saguenuy DiHtrict (o Westbrn Division : Soil, Agricalturc, &c 13 Artificiai, Manures , jg Gypsum , _ jg Pliosphato of Lime , "" ^g Fish Manures jo Peat.— Its application jg Building Materials , oq Brick-Clay 2j Lime 22- Building Stones 53 Mai-bles " qo Serpentine , ^^ 04 Roofing Slates 05 Metallic Ores, &c or. Iron Ores....; ^,^ 05 Copper Ores ^^^ ^ _ 07 Lead Ores,, , _ „g ' Gold ,^ 2g Iron Pyrites ^ , ^ <,n Chromium ,.,_, on Titanium , ^q Ochres on Quartz for Glass-making ^Q Plumbago , g. Soapstone , 01 Millstones ,.. ..' 31 Lithographic Stone ■ 3^ Porphyries, &c „.. 32 Petroleum , «..»,»..... 30