186 Tonnage Estimate Proved Ore: The only part of the deposit that can in any sense be classified as proved ore (developed on three sides) is the double pyramid of magnetite, whose common base is the triangular section shown in the section on line A-B (Figure 30), and whose heights are represented by the lengths of the lines from this section to the two opposite ends of the exposure. 2,800 (square feet, area of triangular section) X 320 (feet, height of double pyramid) + 3 (for volume of pyramid) + 8 (for cubic feet per ton) = 37,300 tons. Probable Ore: Included within a volume outlined by the present slope area of exposure, and a depth along the dip of 60 feet (to the breasts of the two tunnels), less the tonnage of proved ore. 13,200 (square feet, slope area of exposure) X 60 (feet, depth) + 8 (cubic feet per ton) —37,300 (tons, proved ore) = 61,700 tons. Possible Ore: No estimate can be made, but it might be stated ap- proximately, that for every 100 fect of additional depth along the dip, below the limit of probable ore, with the same cross-sectional area as is exposed, there would be included 165,000 tons. This tonnage is not as speculative as the corresponding figures for the Sirdar deposit. Value of Deposit As far as can be judged from present exposure and development, the Little Bobs-Baden Powell deposit is not of sufficient magnitude to become by itself a commercial iron mine. Its economic possibilities, however, should be considered in its relation to the other Bugaboo Creek deposits (See below). Bibliography See page 158 for further details 6. Carmichael, H., p. 219. 16. Lindeman, E., p. 10. 17. Clapp, C. H., pp. 189-193. 20. Lindeman, E., and Bolton, L. L., p. 5. 21. Brewer, W.M., p. 14. 22. Whittier, W. H. (46 f) General French and General Warren Claims Magnetite occurs on these claims (See Figure 27), more particularly on the General French, about 1,200 feet east of the Baden Powell-Little Bobs deposit and 200 feet lower in elevation. No published or previously reported description of this occurrence is available. Present exposures reveal only a small deposit. Magnetite is exposed in a stripping showing a bluff of ore 20 feet high and 15 feet wide. The deposit is bounded on one side by crystalline limestone, and on the other by a mass of fine- grained diorite or andesite, which is in dyke form, having limestone on its other side. Considerable stripping had been done years ago around this occurrence, and a tunnel, now caved, had been driven into it. No magnetite float was visible above this exposure. The magnetite is of fairly good quality with only small amounts of intermixed pyrite.