~106-

Thus it appears probable that the deposits are confined to a
narrow zone which originally lay just below the sediments. The
nature of the mineralization is similar to that of the group of
deposits on the southwestern slope. Variations from place to
place may be due to changes in the composition and courses of
mineralizing solutions, Shearing of galena in the E.pire shows
very late movement along the veins. There is no evidence of
zoning. The fractures, like those to the west, strike toward the
peak, but unlike them dip southwest instead of being nearly
vertical.

References to published descriptions of properties in
this area are as follows: Yukon, 12%yukon,3(1929, pege 164; 1928,
page 162; 1925, page 136); Empire? (1929, page 164; 1928, page
160); Lone Star3 (1916, pege 122); Dorothy (Wade); Cascade? (1923,
page 10); Vancouver (1926, page 132); Heather’ (1931, page 73);
Snowshoe® (1929, page 163; 1928, page 162); Jessic® (1933, page 97;

1928, page 162).

SOUTHEASTERN SLOPE OF HUDSON BAY MOUNTAIN. Several deposits occur
low on the southeastern slope of the mountain in zones trending
toward the peak: Zobnic,= Smithers Copper ,2 and Canadian Citizen.&
Values are mainly in silver and copper, but lead and zinc are also

present in some of the deposits.

z Geol. Surv., Canada, Sum, Rept. 1925, pt. A, p. 137.

S Jones, R.H.B.: Geol. Surv., Canada, Sum. Rept. 1925, p. 137.
Suive ORSee | amiewe GF oa) BC.

Ann. Rept. inter of Mines, BeaC., L927, pe. Lor.

lipaldencl O50, pe U4Os 8929, pie Loo.

6 jones, R.H.B.: Geol. Surv., Canada, Sum. Rept. 1925; Ann. Rept.
Minister of Mines, B.C., 1929, p. 136.

a