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axial part of the fold it may be that ore also occurs somewhere along the
limb and might be found by extending No. 1 adit. Ore may continue
along the axial part of the fold below the lowest or No. 4 adit, but to the
south of this level the dip of the strata changes within a distance of 100
to 200 feet and it is likely that the attitude of the vein also changes.

Falcon Group (Locality 169)
Reference: Annual Report of the Minister of Mines, British Columbia, 1930.

The Falcon group of two mineral claims is west of Illiance river near
its head. There are three parallel shear zones on the property from 2 to
5 feet wide mineralized with quartz, calcite, galena, sphalerite, and
tetrahedrite.

Fox Claim (Locality 125)

erences: prea Report of the Minister of Mines, British Columbia, 1918, 1925,
and 1927.

The Fox mineral claim adjoins and lies south of the Tip Top claim.
It is at an elevation of 4,000 feet on the west side of Kitsault river near
its head. Access is furnished by a foot trail from the end of the Vanguard
trail. The deposit is a quartz-chlorite-pyrite vein containing some chal-
copyrite and a little galena and sphalerite. The vein strikes southwest
and dips northwest, is up to 4 feet wide, and lies in massive rocks of the
Hazelton group.

Fox Group (Locality 162)

Reference: Annual Report of the Minister of Mines, British Columbia, 1929.

The Fox group of seven mineral claims is on the ridge west of
Washout creek. The workings are at an elevation of 1,600 feet. Access
is by a trail branching from the Dak River trail near Washout creek.

The mineral deposit is a body of quartz and barite containing pyrite,
chalcopyrite, sphalerite, galena, and fragments of country rock. The size
and shape of the body have not been determined. It is probably a
replacement in a brecciated zone. The deposit may be of considerable
size.

Glacier Claim (Locality 167)

Reference: Annual Report of the Minister of Mines, British Columbia, 1918.

The Glacier claim is on Tchitin river north of the head of Llliance
river. The deposit is a quartz vein up to 1 foot wide containing silver
ore of good grade.

Golden Crest Group (Locality 173)
References: Annual Report of the Minister of Mines, British Columbia, 1916 and 1918.

The Golden Crest group is east of Illiance river near the 11-mile
bridge. The mineral showing consists of quartz stringers with pyrite and
chalcopyrite in altered tuffaceous rock. A body of massive pyrite several
feet wide is visible in one open-cut.