NAME OF THE DENES AND THEIR HABITAT IN THE NORTH. 17 Geographical Features. As to the physical features of the northern land in general, it is but natural that most pronounced differences should result from such widely separated latitudes. The northernmost portion of it is, as a rule, as bleak, desolate and inhospitable as could be imagined. Almost immediately to the northwest of Fort Churchill, on Hudson Bay, and far into the interior, the eye wanders upon endless reaches of wastes silent as the grave, treeless as the great Canadian plains hundreds of miles away, but with no other soil than frozen mossy bogs, or barren tracts of land destitute of any vegetation Save, here and there, a few scrubby bushes and, almost everywhere, mono- tonous beds of lichens. These are the well known Barren Grounds of Canada, the Othel-néne, or Broad Lands, of the natives. Yet, while these apparently resourceless regions would certainly prove the death of the white man rash enough to venture through them alone, they are the granary or, if you will, the larder of the Déné huntsman, which a kind Providence keeps well filled with moving masses of reindeer, a noble animal which subsists mostly on the particular kind of lichen (Z. rangiferinus) which nature does not grudge that unfruitful soil. There also, but generally north of the reindeer herds, are to be found, sedulously segregated from every other living creature, the musk ox (Ovibos moschatus), that delight of the naturalist, which is so much the more prized as it is the rarer. In fact, it has no other habitat on the whole surface of the globe. Further west again, limitless forests of coniferous trees, interspersed with birch (Betula Papyracea), aspen (Populus tremuloides), poplar or liard (P. bal- samea) and the humbler willow (Salix longifolia), constitute the hunting ground of various tribes until 67° N. lat. is reached, where all important vegetation ceases again. Within Alaska low mountains alternate with tundras, rolling plains covered with moss and more or less marshy, when primeval woods do not extend as far as the eye can reach. South of these we have the sombre forests and snow-capped mountains of northern British Columbia, famous among which is the Cariboo group, of golden fame. The eastern and western Dénés are divided by the great orographic system of the American continent. I mean the Rocky Mountains (Tsé-thi, or Great Rocks) which, continuous in the south, except for a few gaps leaving passage to the Peace and Liard Rivers or without any stream of importance, become more or less broken as we go north, assuming at intervals an over- lapping or echelon-like arrangement. This is, according to the Indians, the backbone of the earth. Besides the few special kinds of game to which the range affords excellent retreats, its main object, in the economy of nature, seems to be to feed with its eternal snows numberless rivers which water the country and drain the multitude of lakes which dot it on either side. 2