NORTHERN INTERIOR OF BRITISH COLUMBIA north, where lines of snow-capped peaks intersect the whole country between the two main ranges. Endless forests, mostly of coniferous trees, and deep lakes, whose length generally exceeds considerably their breadth, cover such spaces as are not taken up by mountains. The only level or meadow lands of any extent within that district lie on either side of the Chilcotin River, where excellent bunch grass affords lasting pasturage to large herds of cattle and horses. The Douglas fir preponderates in the southern half of the country, but cannot stand the cold prevalent north of 54°40, while the three different species of spruce which cover the northern part of the district hardly appear within its more temperate zone. The black pine is fairly common all over the country, and it is always indicative of a dry, sandy, and usually level ground, just as the poplar and the aspen betoken a moist and rather rich soil. Apart from the animals to which they give shelter, these woods afford but very meagre resources adapted to the wants of man. These are reduced to some varieties of berries, prominent among which is the service berry, the fruit of the Aelan- chier alnifolia, which the aborigines compress into flat cakes and keep in their larder for use in any emergency. Lakes and rivers are practically numberless. The most important among the former are: Lake Stuart, with its tributaries Lakes Rey, Soullier, Tremblé and Tatla; Lakes Babine and Augier ; Lakes Morice, Dawson, and Emerald, 1. H. H. Bancroft, in his ‘‘ History of British Columbia,” asserts that “the lake country from Chilcotin to Fort Fraser and beyond is generally open” (p. 37), a statement which is far too comprehensive. The lakes of that country, and those immediately to the north of it, R. Greenhow gravely declares to be ‘‘ frozen over more than two-thirds of the year” (‘* History of Oregon and California,” p. 29), which assertion will seem strange to people who, like the present writer, have annually navigated their waters from the middle of May to the middle of December, practically ever since the year 1885. 2