106 NORTH BEND OF FRASER RIVER. A prospect owned by Oscar Eden, of Prince George, and others, situated just north of the most northerly bend of Fraser river (Figure 1, locality 1), carries values in silver, lead, and gold. The property is con- nected by steamer channel up the Fraser with Hudson Spur near Hansard about 24 miles east, on the Grand Trunk Pacific railway, and to Prince George about 50 miles down the river to the southwest. The route to Hudson Spur is in quiet water all the way, but there are several long rapids down the river toward Prince George. Developments on this property include a tunnel and shallow shaft. The tunnel, within 100 feet of the north bank of the river, is about 95 feet long trending about north 40 degrees west. The country rock is a quartz muscovite chlorite schist carrying some carbonate. A sheared zone about 3 feet wide and dipping east, carries quartz with pyrite. In places in the tunnel it lies between fairly solid walls, the easterly wall being apparently more schistose, but other- wise of the same character as the wall on the west side. There has been much faulting and silicification of the country rock. The shaft lies 300 feet in elevation over the river, about 1,800 feet north of it, and about 750 feet east by south of the northeast corner of Eden’s homestead lot. Galena occurs in quartz that is from 5 to 6 feet in width lying between well-defined walls of schist. The walls strike 285 degrees magnetic north (46 degrees true north) and dip 60 degrees to 65 degrees to the northeast. Faulting on the foot-wall is represented by 8 inches of black and red gouge. About - 20 feet of the length of the ore-body has been exposed. If the strike of the ore zone be followed in an easterly direction for 550 feet along the side hill a gulch is crossed running south 67 degrees west toward the Fraser. Two hundred feet down the gulch from where the strike of the ore zone would cross the gulch are boulders of quartz, some of them 2 feet across, with much galena. They must have moved downhill from their outcrop and are a very excellent indication that the ore zone has a length of from 500 to 600 feet at least. Samples taken from various places in the tunnel and in the foot-wall of the ore zone at the shaft are said to have carried radium. The writer took samples from the gouge in the shaft and from points in the tunnel, as near as possible to the pomts from which the original samples are said to have come from, but a test on these samples by H. V. Ellsworth of the Geological Survey, did not indicate any trace of radium. According to Mr. Eden samples taken by him across the outcrop near the top of the shaft gave 13 ounces of silver and 15 per cent of lead to the ton, whereas a sample across the ore at the bottom of the shaft yielded 25-8 ounces of silver, 42 per cent of lead, and a trace of gold. The writer did not sample this ore- body, but galena is plentiful through the quartz. | Assays made from samples 30 feet and 60 feet from the mouth of the tunnel are said to have yielded respectively 3 ounces silver, 50 cents in gold, with some lead; and $4.80 in gold. A company known as the North Point Mining Company, of which Oscar Eden is president, has been formed to develop this property. Surface trenching should be done to prove the outcrop over as long a distance as possible so as to determine its dip and strike and whether