30 veins. In 1933 the company continued the adit, but encountered only harrow quartz stringers. These stringers strike north-northeast and dip 70 degrees west. Cube pyrite is very plentiful in the rocks near the veins. About 1,500 feet north are other old workings tracing a quartz vein uphill for a distance of 500 feet. The lower part of this vein strikes east- northeast and the upper part north-northeast. This vein, also, was mined, but no recent work has been done on it. About 500 feet east of the camp is a quartz-ankerite vein, 1 to 3 feet wide, striking northeast. The ankerite appears to oceur chiefly near the walls of the vein. About 2,000 feet southeast and 300 feet below the camp, the com- pany drove a crosscut adit northwest. This tunnel is 1,370 feet long, and cuts several narrow, northeasterly striking quartz stringers. Mining on a small scale was carried on at the property for several years after 1878. Good ore is reported to have assayed $30 to $120 in gold. CANADA GOLD LODE MINING COMPANY Four groups of claims were being prospected in the summer of 1933 for the Canada Gold Lode Mining Company. These groups are the Eagle Mountain Gold Quartz, Dragon Mountain Gold Quartz, Jawbone Gold Quartz, and Tiger Gold Quartz. The properties are north of the Barker- ville road 2 to 4 miles east of Beaver Pass House. The country rock is mainly quartz-sericite schist of the Cariboo series striking northwest to northeast and dipping at various angles to the west. The location is approximately on the crest of the main anticline of the Cariboo series. At an elevation of 4,800 feet on the east side of Timon creek, two open- cuts, 100 feet apart on the Eagle Mountain Gold Quartz group, expose a 2-foot quartz vein striking northeast, dipping 45 degrees northwest, and lying parallel to the shear planes of the rocks. The quartz contains some pyrite and sericite. Low assays in gold are reported. Another open-cut, 150 feet away, discloses another body of quartz 3 feet wide and 8 feet long containing some pyrite and sericite. On the west side of Timon creek, on the Dragon Mountain Gold Quartz group, an open-cut at an elevation of 4,200 feet exposes a vertical quartz vein varying in width up to 2 feet and striking east. It is parallel, or nearly so, with the shear planes of the rock and contains some pyrite and sericite. Another open-cut, 200 feet higher and about + mile farther north, exposes another 2-foot quartz vein striking east and containing some sericite. At an elevation of 3,900 feet on the east branch of Jawbone creek, on the Jawbone Gold Quartz group, a short adit exposes a quartz vein varying in width up to 6 feet. The rock and vein are so shattered that neither the strike of the rock nor that of the vein could be determined accurately. The vein appears to strike east and to dip gently south. The quartz is mineral- ized with some pyrite and a little galena. At an elevation of 3,800 feet, 4 mile west of Jawbone creek, a short adit on the Tiger Gold Quartz group exposes a quartz vein 3 feet or more