A few miles below Tête Jaune Cache the Fraser, after running almost due west from Moose Lake, receives a tributary from the south-east, then suddenly turns almost due north; and, according to Indian report, is joined a little lower down by an important branch from the north-east. The Cache is situated in a valley of triangular form, with the apex to the south, and enclosed by lofty mountains. The valley is some fifteen miles in length, and not more than five in width at the broadest part. Across the base runs the Fraser, from east to west, turning north, when it meets the range of hills which forms the western side. The commencement of a bold range of mountains, running nearly north and south, and dividing the watershed of the Columbia from that of the Thompson, closes up the point of the valley. The main chain of the Rocky Mountains forms the eastern boundary. Part of the valley of The Cache appears to be rich; but immediately to the south is a stretch of sandy, undulating country, partially covered by small spruce, and terminated by the range of hills mentioned as dividing the watersheds. Then commence the dense forests of the North Thompson. The view from The Cache looking westward is, we imagine, one of the most wonderful in the world. Away as far as the eye can reach, north, south, and west, are mountains packed behind mountains, separated only by the narrowest valleys, most of them snow-clad, and apparently stretching away to the Pacific. Although we had crossed the main chain of the Rocky Mountains, and were now in British Columbia, we were surprised to find we were still really in the midst of Rocky Mountains. For, in truth, the mountains which rise like a wall from the prairies of the eastern side extend to the western ocean. The exact reverse of this view may be seen from the Bald Mountain in Cariboo, and we were assured by Mr. Fraser, of Victoria, who had visited both the Andes and Himalayas, that nothing there could compare with these hundreds of miles of mountains in British Columbia.