-9]-

different mineral association from that of. other deposits described,
but is similar in most other respects. One deposit 3 feet wide is
opened up for 100 feet. t does not continue up the slope but may
continue dovm. It contains mostly pyrrhotite with sphalerite and
pyrite. Lay describes three veins; one is 18 inches wide and is
mineralized with pyrrhotite, galena, arsenopyrite, pyrite, and
some chalcopyrite, assaying gold, 0.02 ounce, and silver, 5 ounces,
a ton. Two hundred feet east is a vein sparsely mineralized with
pyrrhotite and pyrite and 500 feet southeast one 4 feet wide with
18 inches of solid pyrrhotite assaying 0.04 ounce gold 1.7 ounces
silver a ton.

The Cenary, Humming Bird,l King Tut,2 Neepawa,5and

White Swan® are in the main smaller or lower grade deposits of the

Ann. Rept. Minister of Mines, B.C., 1929, p. 161; Jones, R.H.B.,
Geol. Surv., Canada, Sum. Rept. 1925, p. 150.

Poa-dign POLS. pis 132).

Jer oo

Ann. Rept. Geol. Surv., Canada, Sum. Rept., 1929, p. 163.

[>

fad, 1994, p. 215.

same types as the others on the southwestern slope.

GLACIER GULCH AREA, HUDSON BAY MOUNTAIN 2 The Glacier Gulch area

i

2 txamined by the writer

has attracted much attention because of a small production from a
number of pockets of very high-grade gold-bismuth ore of a unique
type. There are also a number of other deposits, some of which
have been developed, of the common types, containing, mainly, gold,
silver, lead, zinc, and copper. With the exception of one vein
under development in 1934 most of these are very small and lie in
irregular fractures.

The dominating feature of the area is the great gash

which the glacier has cut in the mountain. The location of the