[135] "The mouth of the whirlpool is more than 1000 feet wide, and in length about 2000. Mr. Howison, in his sketches of Upper Canada, says that the current of the river has formed a circular excavation in the high and perpendicular banks, resembling a bay. The current, which is extremely rapid, whenever it reaches the upper point of this bay, forsakes the direct channel, and sweeps wildly round the sides of it; when, having made this extraordinary circuit, it regains its proper course, and rushes with perturbed velocity between two perpendicular precipices, which are not more than 400 feet asunder. The surface of the whirlpool is in a state of continual agitation. The water boils, mantles up, and wreaths in a manner that proves its fearful depth, and the confinement it suffers; the trees that come within the sphere of the current are swept along with a quivering, zigzag motion, which it is difficult to describe. This singular body of water must be several hundred feel deep, and has not hitherto been frozen over, although in spring the broken ice that descends from Lake Erie descends in such quantities upon its surface, and becomes so closely wedged together, that it resists the current, and remains till warm weather breaks it up. The whirlpool is one of the greatest natural curiosities in the Upper Province, and its formation can not be rationally accounted for."—Martin's History of Canada, p. 139.
[136] "This inland sea, though the smallest of the great chain with which it is connected, is of such extent, that vessels in crossing it lose sight of land, and must steer their way by the compass; and the swell is often equal to that of the ocean. During the winter, the northeast part of Ontario, from the Bay of Quinté to Sacket's Harbor, is frozen across; but the wider part of the lake is frozen only to a short distance from the shore. Lake Erie is frozen still less; the northern parts of Huron and Michigan more; and Superior is said to be frozen to a distance of seventy miles from its coasts. The navigation of Ontario closes in October; ice-boats are sometimes used when the ice is glare (smooth). One, mentioned by Lieutenant de Roos, was twenty-three feet in length, resting on three skates of iron, one attached to each end of a strong cross-bar, fixed under the fore-feet, the remaining one to the stern, from the bottom of the rudder; the mast and sail those of a common boat: when brought into play on the ice, she could sail (if it may be so termed) with fearful rapidity, nearly twenty-three miles an hour. One has been known to cross from Toronto to Fort George or Niagara, a distance of forty miles, in little more than three quarters of an hour; but, in addition to her speed before the wind, she is also capable of beating well up to windward, requiring, however, an experienced hand to manage her, in consequence of her extreme sensibility of the rudder during her quick motion."—Martin's History of Canada.
"The great earthquake that destroyed Lisbon happened on the 1st of November, 1755, and on Lake Ontario strong agitations of the water were observed from the month of October, 1755."—Lettera Rarissima data nelle Indie nella Isola di Jamaica a 7 Julio del 1503 (Bassano, 1810, p. 29).
"From some submarine center in the Atlantic, this earthquake spread one enormous convulsion over an area of 700,000 square miles, agitating, by a single impulse, the lakes of Scotland and Sweden, and the islands of the West Indian Sea. Not, however, by a simultaneous shock, for the element of time comes in with the distance of undulation; and, together with this, another complexity of action in the transmission of earthquake movements through the sea, arising from the different rate of progression at different depths. In the fact that the wave of the Lisbon earthquake reached Plymouth at the rate of 2.1 miles per minute, and Barbadoes at 7.3 miles per minute, there is illustration of the law that the velocity of a wave is proportional to the square root of its depth, and becomes a substitute for the sounding line in fixing the mean proportional depth of different parts of this great ocean."—Humboldt.
[137] "There are two lakes in Lower Canada, Matapediac and Memphremagog. The former is about 16 miles long, and three broad in its greatest breadth, about 21 miles distant from the St. Lawrence River, in the county of Rimouski; amid the islands that separate the waters running into the St. Lawrence from those that run to the Bay of Chaleurs, it is navigable for rafts of all kinds of timber, with which the banks of the noble River Matapediac are thickly covered. Memphremagog Lake, in the county of Stanstead, stretching its south extremity into the State of Vermont, is of a semi-circular shape, 30 miles long, and very narrow. It empties itself into the fine river St. Francis, by means of the River Magog, which runs through Lake Scaswaninepus. The Memphremagog Lake is said to be navigable for ships of 500 tons burden."—Martin's History of Canada, p. 102.
[138] "It is worthy of remark, that the great lakes of Upper Canada are liable to the formation of the Prester or water-spout, and that several instances are recorded of the occurrence of that truly extraordinary phenomenon, the theory of which, however, is well known. Whether electricity be a cause or a consequence of this formidable meteor, appears, nevertheless, to be a question of some doubt among natural philosophers; Gassendi being disposed to favor the former opinion, while Cavallo espouses the latter."—Bouchette's Topographical and Statistical Description of Upper and Lower Canada, vol. i., p. 346.
[139] "The most considerable harbors on the English side are Toronto (York, the former name, has recently been changed to the Indian name of the place, Toronto) and Kingston. Toronto is situated near the head of Lake Ontario, on the north side of an excellent harbor or elliptical basin, of an area of eight or nine miles, formed by a long, low, sandy peninsula or island, stretching from the land east of the town to Gibraltar Point, abreast of a good fort. The town of Toronto, at that period York, was twice captured by the Americans, in April and August, 1813, owing to its defenseless state, and a large ship of war on the stocks burned. The Americans would not now find its capture such an easy task. Little more than forty years ago, the site whereon Toronto now stands, and the whole country to the north and west of it, was a perfect wilderness; the land is now fast clearing—thickly settled by a robust and industrious European-descended population, blessed with health and competence, and on all sides indicating the rapid progress of civilization. The other British town of importance on this shore is Kingston, formerly Cataraqui or Frontenac, distant from Toronto 184 miles, and from Montreal 180 miles. It is, next to Quebec and Halifax, the strongest British post in America, and, next to Quebec and Montreal, the first in commercial importance. It is advantageously situated on the north bank of Lake Ontario, at the head of the River St. Lawrence, and is separated from Points Frederic and Henry by a bay, which extends a considerable distance to the northwest beyond the town, where it receives the water of a river flowing from the interior. Point Frederic is a long, narrow peninsula, extending about half a mile into the lake, distant from Kingston about three quarters of a mile on the opposite side of its bay. This peninsula forms the west side of a narrow and deep inlet called Navy Bay, from its being our chief naval dépôt on Lake Ontario."—Martin's History of Canada.
[140] "The channel of the St. Lawrence is here so spacious that it is called the Lake of the Thousand Islands. The vast number implied in this name was considered a vague exaggeration, till the commissioners employed in fixing the boundary with the United States actually counted them, and found that they amounted to 1692. They are of every imaginable size, shape, and appearance; some barely visible, others covering fifteen acres; but, in general, their broken outline presents the most picturesque combinations of wood and rock. The navigator, in steering through them, sees an ever-changing scene: sometimes he is inclosed in a narrow channel; then he discovers before him twelve openings, like so many noble rivers; and, soon after, a spacious lake seems to surround him on every side."—Bouchette, vol. i., p. 156; Howison's Sketches of Canada, p. 46.
[141] "The St. Lawrence traverses the whole extent of Lower Canada, as the lakes every where border and inclose Upper Canada. There is a difficulty in tracing its origin, or, at least, which of the tributaries of