The Conquest of Canada, Vol. 1. George Warburton
at the bow, two on each side, thrust their poles into the channel, and grasping successively the wooden bars, work their way toward the stern, thus pushing on the vessel in that direction. At other times, by the brisk and vigorous use of the oar, they catch and dash through the most favorable lines of current. In this exhausting struggle, however, it is needful to have frequent pauses for rest, and in the most difficult passages there are certain positions fixed for this purpose, which the Canadians call
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"From the sea to Montreal, this superb river is called the St. Lawrence; from thence to Kingston, in Upper Canada, the Cataraqui or Iroquois; between Lakes Ontario and Erie, the Niagara; between Lakes Erie and St. Clair, the Detroit; between Lakes St. Clair and Huron, the St. Clair; and between Lakes Huron and Superior, the distance is called the Narrows, or Falls of St. Mary. The St. Lawrence discharges to the ocean annually about 4,277,880 millions of tons of fresh water, of which 2,112,120 millions of tons may be reckoned melted snow; the quantity discharged before the thaw comes on, being 4512 millions of tons per day for 240 days, and the quantity after the thaw begins, being 25,560 millions per day for 125 days, the depths and velocity when in and out of flood being duly considered: hence a ton of water being nearly equal to 55 cubic yards of pure snow, the St. Lawrence frees a country of more than 2000 miles square, covered to the depth of three feet. The embouchure of this first-class stream is that part of the Gulf of St. Lawrence where the island of Anticosti divides the mouth of the river into two branches. According to Mr. M'Taggart, a shrewd and humorous writer, the solid contents in cubic feet of the St. Lawrence, embracing Lakes Superior, Huron, Michigan, Erie, and Ontario, is estimated at 1,547,792,360,000 cubic feet, and the superficial area being 72,930 square miles, the water therein would form a cubic column of nearly 22 miles on each side!"—Montgomery Martin's
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"Kinnel Lodge, the residence of the celebrated Highland chieftain M'Nab, is romantically situated on the south bank of the lake, about five miles above the head of the Chats Rapids, which are three miles long, and pass amid a labyrinth of varied islands, until the waters of the Ottawa are suddenly precipitated over the Falls of the Chats, which, to the number of fifteen or sixteen, form a curved line across the river, regularly divided by woody islands, the falls being in depth from sixteen to twenty feet."—M. Martin's
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See Appendix, No. XIX. (vol. II.)
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"At Quebec, the River St. Lawrence narrows to 1314 yards; yet the navigation is completely unobstructed, while there is formed near the city a capacious harbor. About twenty-one miles lower, its waters, beginning to mingle with those of the sea, acquire a saline taste, which increases till, at Kamauraska, seventy-five miles nearer its mouth, they become completely salt. Yet custom, with somewhat doubtful propriety, considers the river as continued down to the island of Anticosti, and bounded by Cape Rosier on the southern, and Mingau settlement on the northern shore."—Bouchette's
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See Appendix, No. XX. (vol. II.)
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"The Falls of the Rideau are about fifty feet in height and 300 in breadth, being, at the time we saw them, more magnificent than usual, by reason of the high state of the waters. It is from their resemblance to a curtain that they are distinguished by the name of Rideau, and they also give this name to the river that feeds them, which again lends the same appellation to the canal that connects the Ottawa with Lake Ontario."—Simpson, vol. i., p. 16.
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Modern alluvial accumulations are rapidly increasing on some points of this coast, owing to the enormous mass of fresh water, charged with earthy matter, that here mingles with the sea. The surface of the water at the mouth of the St. Lawrence, where the depth is 100 fathoms, is stated by Bayfield to be turbid from this cause: yet that this discoloration is superficial is evident, for in the wake of a ship moving through the turbid surface, the clear blue waters of the sea are seen below.
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"The neighborhood of Quebec, as well as Canada in general, is much characterized by bowlders, and the size and position of some of them is very striking. There are two crowning the height which overlooks the domain farm at Beauport, whose collective weight is little short, by computation, of forty tons. The Heights of Abraham also are, or rather were, crowded with them; and it should never be forgotten that it was upon one of these hoary symbols, the debâcles of the deluge, as they are supposed to be, that the immortal and mortal parts of two heroes separated from each other. It has often occurred to us, that one of the most suitable monuments to the memory of Wolfe and Montcalm might have been erected with these masses, in the form of a pyramid or pile of shot, instead of burying them, as in many instances has been done, in order to clear the ground."—
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Gray says, in 1809, that "no coal has ever yet been found in Canada, probably because it has never been thought worth searching after. It is supposed that coal exists in the neighborhood of Quebec; at any rate, there can be no doubt that it exists in great abundance in the island of Cape Breton, which may one day become the Newcastle of Canada."—P. 287.
"No idea can be formed of the importance of the American coal seams until we reflect on the prodigious area over which they are continuous. The elliptical area occupied by the Pittsburg seam is 225 miles in its largest diameter, while its maximum breadth is about 100 miles, its superficial extent being about 14,000 square miles.
"The Apalachian coal-field extends for a distance of 720 miles from northeast to southwest, its greatest width being about 180 miles.
"The Illinois coal-field is not much inferior in dimensions to the whole of England."—Lyell's
"It was the first time I had seen the true coal in America, and I was much struck with its surprising analogy in mineral and fossil characters to that of Europe; … the whole series resting on a coarse grit and conglomerate, containing quartz pebbles, very like our millstone grit, and often called by the Americans, as well as the English miners, the 'Farewell Rock,' because, when they have reached it in their borings, they take leave of all valuable fuel."—
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See Appendix, No. XXI. (vol. II.)
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Professor Kalm visited the iron-works of St. Maurice in 1748, eleven or twelve years after their first establishment. "The iron-work, which is the only one in the country, lies three miles to the west of Trois Rivières. Here are two great forges, besides two lesser ones to each of the great ones, and under the same roof with them. The bellows were made of wood, and every thing else as in the Swedish forges. The ore is got two and a half miles from the iron-works, and is carried thither on sledges. It is a kind of moor-ore (Tophus Tubalcaini: