smaller pan fish; and the forest affords game in the caribou, a species of large deer.
Kootenai Lake mining district lies on both sides of the lake about fifteen miles north of the outlet. The Blue Bell Mine, on the east side, is on Galena Bay, and owned by the Kootenai Mining and Smelting Company, which has its office at Kootenai Station, on the Northern Pacific. It is a ten-foot vein of lowgrade galena in lime, extending north and south, assaying eight ounces in silver, with eighty per cent, of lead, and opened by a one-hundred-foot incline. The Blue Bell was discovered and to some extent developed previous to 1885, when, owing to a contest over rights, work was suspended until the present company acquired the property. The Kootenai Chief, an extension of the Blue Bell, is owned in San Francisco, but not at present worked. On the opposite side of the lake are numerous locations, among which are the Highland, owned in Spokane, a three-foot vein of clear galena, assaying, from forty to two hundred and eighty ounces silver and sixty per cent, lead, opened by a sixty-foot tunnel at a depth of one hundred and ten feet; the Jim Blaine, a narrow vein, owned in Butte City, Montana, which shipped to the Wicks Smelter three thousand five hundred pounds of gray carbonate ore that netted over two hundred and eighty-three ounces of silver, the vein being in a basin on top of a mountain, and difficult to reach or work. Out of a large number of claims, a dozen or more show a good grade of galena. There are hot springs among this group of mines, which continually deposit lime.
The Bonanza district is situated six miles south of the Kootenai Lake outlet, on Cottonwood Creek, which comes into the outlet from the south at a point twenty-two miles southeast and down from the main Kootenai Lake. The principal locations are at an altitude of five thousand four hundred feet, and two thousand seven hundred feet above the lake, cutting at right angles through a timbered ridge running northeast and southwest, which slopes uniformly down to the outlet. The district was discovered in 1886 by parties from Colville, and located the following year. There are three parallel veins, about six hundred feet apart, ranging from thirty to eighty feet in width, and running in an east-and-west direction, with a dip
