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into the great waters of Canada; of those eastward of the Saguenay little is known beyond their entrance; they flow through cliffs of light-colored sand, rocky, wooded knolls, or, in some places, deep, swampy moss-beds nearly three feet in depth. From the Saguenay to Quebec the mountain ridge along the shore of the St. Lawrence is unbroken, save where streams find their way to the Great River, but beyond this coast-border the country is in some places level, in others undulating, with hills of moderate height, and well-watered valleys. From Quebec westward to the St. Maurice, which joins the St. Lawrence at Three Rivers, the land rises in a gentle ascent from the banks of the Great River, and presents a rich tract of fertile plains and slopes: in the distance, a lofty chain of mountains protects this favored district from the bitter northern blast. Along the north bank of the St. Lawrence, from the St. Maurice, the country toward the Ottawa is slightly elevated into table ridges, with occasional abrupt declivities and some extensive plains. In this portion of Canada are included the islands of Montreal, Jesus, and Perrot, formed by the various branches of the Great River and the Ottawa, where their waters unite. Montreal is the largest and most fertile of these islands; its length is thirty-two miles and breadth ten; the general shape is triangular. Isle Jesus is twenty-one miles by six in extent, and also very rich; there are, besides, several other smaller islands of considerable fertility. Isle Perrot is poor and sandy. The remote country to the north of the Ottawa is but little known.

      FOOTNOTES:

      [118] "The sea (if it may be so termed) on Lake Ontario is so high during a sharp gale, that it was at first thought the smaller class steamboats could not live on it; and on Lake Superior, the waves almost rival those of the far-famed Cape of Storms, while the ground-swell, owing to the comparative shallowness, or little specific gravity of the fresh water, is such as to make the oldest sailor sick. Whether the water in the lowest depths of Lakes Superior and Ontario be salt or fresh, we can not ascertain; for the greater density of the former may keep it always below, or there may be a communication with the fathomless abysses of the ocean."—Montgomery Martin, p. 181.

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