Ln 33 north and south, the surface of the country slopes rapidly northward towards a low, level horizon. The ridges, which do not here appear to have any very definite direction, are composed of well-rounded shingle, and the hollows intervening become larger in proportion, with a clayey soil, and support a dense growth of black spruce, with occa- sional large birches, balsam poplars and Douglas firs. There is coatinued evidence of approach to a region with greater rainfall in passing from Blackwater to Fort George. ° Mosses and various species of Lycopodium begin to grow abundantly in the woods, and a few miles before reaching Fort George specimens of Ledum latifolium were seen for the first time. ‘Surrounding Fort George is an area of probably from 2,000 to 3,000 acres, elevated only about thirty feet above the Fraser River, and bounded to tht south and west by the escarpment of the high-level plain above. Such crops as have been tried succeed well. , “VALLEY OF THE BLACKWATER NorrH oF THE CLuscus LAKE. “This part of the Blackwater Valley, like most of its length between this place and the bridge at the Lower Canyon, has much resemblance to that of the Eu-chan-i-ko above described, but is on a larger scale. The north slope is generally bare, or but lightly tree-clad, with. bunch-grass, wild onions, bearberry, vetch, strawberry and Galium borealis, while thickets of willow and dwarf birch (Betula glandulosa) fringe the stream. The south bank presents a somewhat similar assemblage of plants, but is much more thickly timbered with serub pine and poplar and ocedsional groves of black spruce. The appearance of the river valley is pleasing, and there is abundance of good grazing for animals, which the winter snows can not be deep enough entirely to cover, as the Indians of Cluscus Lake own a number of horses which are allowed to live as best they can at all seasons. The sloping sides of the valley are generally steep, but show little rock, being covered with terraced drift material. At this place a very conspicuous bench may be traced running for miles along the valley at an elevation (at Cush-va, sometimes called Upper Eu-chen-i-ko Lake) of 296 feet above the river, or 3,476 feet above the sea. The river itself flows rather rapidly between the long lake-like expansions which here characterise it and add greatly to the beauty of the landscape. Whether these lakes are held in by rocky barriers or dammed merely by drift material, I have been unable to satisfy myself. “