Of these useful animals no care whatever is taken, as when they are no longer employed, they are turned loose winter and summer to provide for themselves. Here, it is to be observed, that the country, in general, on the West and North side of this great river, is broken by the lakes and rivers with small intervening plains, where the soil is good, and the grass grows to some length. To these the male buffaloes resort for the winter, and if it be very severe, the females also are obliged to leave the plains.
But to return to the route by which the progress West and North is made through this continent.
We leave the Saskatchiwine[10] by entering the river which forms the discharge of the Sturgeon Lake, on whose East bank is situated Cumberland house, in latitude 53. 56. North, longitude 102. 15. The distance between the entrance and Cumberland house is estimated at twenty miles.
It is very evident that the mud which is carried down by the Saskatchiwine River, has formed the land that lies between it and the lake, for the distance of upwards of twenty miles in the line of the river, which is inundated during one half of the summer, though covered with wood. This lake forms an irregular horse-shoe, one side of which runs to the North-West, and bears the name of Pine-Island Lake, and the other, known by the name already mentioned, runs to the East of North, and is the largest: its length is about twenty-seven miles, and its greatest breadth about six miles. The North side of the latter is the same kind of rock as that described in Lake Winipic, on the West shore. In latitude 54. 16. North, the Sturgeon-Weir River discharges itself into this lake, and its bed appears to be of the same kind of rock, and is almost a continual rapid. Its direct course is about West by North, and with its windings, is about thirty miles. It takes its waters into the Beaver Lake the South-West side of which consists of the same rock lying in thin stratas: the route then proceeds from island to island for about twelve miles, and along the North shore, for four miles more, the whole being a North-West course to the entrance of a river, in latitude 54. 32. North. The lake, for this distance, is about four or five miles wide, and abounds with fish common to the country. The part of it upon the right of that which has been described, appears more considerable. The islands are rocky, and the lake itself surrounded by rocks. The communication from hence to the Bouleau Lake, alternately narrows into rivers and spreads into small lakes. The interruptions are, the Pente Portage, which is succeeded by the Grand Rapid, where there is a Decharge, the Carp Portage, the Bouleau Portage in latitude 54. 50. North, including a distance, together with the windings, of thirty-four miles, in a Westerly direction. The Lake de Bouleau then follows. This lake might with greater propriety be denominated a canal, as it is not more than a mile in breadth. Its course is rather to the East of North for twelve miles to Portage de L'Isle. From thence there is still water to Portage d'Epinettes, except an adjoining rapid. The distance is not more than four miles Westerly. After crossing this Portage, it is not more than two miles to Lake Miron, which is in latitude 55. 7. North. Its length is about twelve miles, and its breadth irregular, from two to ten miles. It is only separated from Lake du Chitique, or Pelican Lake, by a short, narrow, and small strait. That lake is not more than seven miles long, and its course about North-West. The Lake des Bois then succeeds, the passage to which is through small lakes, separated by falls and rapids. The first is a Decharge: then follow the three galets, in immediate succession. From hence Lake des Bois runs about twenty-one miles. Its course is South-South-East, and North-North-West, and is full of islands. The passage continues through an intricate, narrow, winding, and shallow channel for eight miles. The interruptions in this distance are frequent, but depend much on the state of the waters. Having passed them, it is necessary to cross the Portage de Traite, or, as it is called by the Indians, Athiquisipichigan Ouinigam, or the Portage of the Stretched Frog Skin, to the Missinipi. The waters already described discharge themselves into Lake Winipic, and augment those of the river Nelson. These which we are now entering are called the Missinipi, or great Churchill River.