A Yankee in Canada
by Henry D. Thoreau
Some falls should even be kept sacred from the intrusion of mills and factories, as water privileges in another than the mill-wrightes sense. This small river falls perpendicularly nearly two hundred and fifty feet at one pitch. The St. Lawrence falls only one hundred and sixty-four feet at Niagara. It is a very simple and noble fall, and leaves nothing to be desired; but the most that I could say of it would only have the force of one other testimony to assure the reader that it is there. We looked directly down on it from the point of a projecting rock, and saw far below us, on a low promontory, the grass kept fresh and green by the perpetual drizzle, looking like moss. The rock is a kind of slate, in the crevices of which grew ferns and golden-rods. The prevailing trees on the shores were spruce and arbor-vitae, the latter very large and now full of fruit; also aspens, alders, and the mountain ash with its berries. Every immigrant who arrives in this country by way of the St. Lawrence, as he opens a point of the Isle of Orleans sees the Montmorenci tumbling into the Great River thus magnificently in a vast white sheet, making its contribution with emphasis. Robervales Pilot, Jean Alphonse, saw this fall thus and described it in 1542. It is a splendid introduction to the scenery of Quebec. Instead of an artificial fountain in its squares, Quebec has this magnificent natural waterfall to adorn one side of its harbor. Within the mouth of the chasm below, which can be entered only at ebb tide, we had a grand view at once of Quebec and of the fall. Kalm says that the noise of the fall is sometimes heard at Quebec about eight miles distant, and is a sign of a north-east wind. The side of this chasm, of soft and crumbling slate too steep to climb, was among the memorable features of the scene. In the winter of 1829 the frozen spray of the fall descending on the ice of the St. Lawrence made a hill one hundred and twenty-six feet high. It is an annual phenomenon which some think may help explain the formation of glaciers.
In the vicinity of the fall we began to notice what looked like our red-fruited thorn bushes grown to the size of ordinary apple trees, very common and full of large red or yellow fruit which the inhabitants called pommettes, but I did not learn that they were put to any use.
Chapter III: St. Anne
By the middle of the forenoon, though it was a rainy day, we were once more on our way down the north bank of the St. Lawrence, in a north-easterly direction, toward the Falls of St. Anne, which are about thirty miles from Quebec. The settled, more level, and fertile portion of Canada East, may be described rudely as a triangle, with its apex slanting toward the north-east, about one hundred miles wide at its base, and from two to three, or even four hundred miles long, if you reckon its narrow north-eastern extremity; it being the immediate valley of the St. Lawrence and its tributaries, rising by a single or by successive terraces toward the mountains on either hand. Though the words Canada East on the map, stretch over many rivers and lakes and unexplored wildernesses, the actual Canada, which might be the colored portion of the map, is but a little clearing on the banks of the river, which one of those syllables would more than cover. The banks of the St. Lawrence are rather low from Montreal to the Richelieu Rapids, about forty miles above Quebec. Thence they rise gradually to Cape Diamond, or Quebec.