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Kalum Lake Mines.— On the Kalum Lako Mines property granodiorite is

1 am. Repts., Minister of Mines, B.C.; 1925, p.48; 1927, p.63;

1930, p.74.

cut by dykes of albite syenite(?). Small irregular quartz veins and
shear zones traversed by stringers cut these rocks and in turn are
cut by andesite or basalt dykes. One vein with an average width of

1 foot has been developed by a shaft. The vein is made up of
pyritized quartz with a little chalcopyrite and carries free gold.

i representative sample of 500 pounds of vein matter assayed 33
ounces of gold a ton, of which 3 ounces were free. Southwest of

the shaft a shear zone up to 2 feet wide, and holding stringers of
quartz carrying pyrite with rare specks of galena and chalcopyrite,
has been traced for about 200 fect. It carries little gold.

Elsewhere there are irregular zones of stringer, up to 5 feet wide.

2
Head of Kleanza Creek—

At the head of Kleanza creek, 12 to 22 miles from the

2 Hanson, Ge: Geol. Surv., Canada, Sum. Rept., pt. A, p. 115.
Ann. Rept., Minister of Mines, B.C., 1917, p. 94.

en

railway, in and near stocks of granodiorite, there are a number of
copper deposits generally with low silver and no gold. They occur
in shattered or sheared zones or replace volcanics or limestone.
Some sparsely mineralized zones have considerable widths, and zones
or series of zones have been traced for considerable distances. The
properties include: North Star (Avon, Lowrie), Peerless, Wells,
Montana, and Lucky Jin.

Head of Chimdema sh Creek®.

At the head of Chimdemash creek mineral deposits occur

————<$—$—— $$ ————— —

2 Hanson, G.: Geol. Surv., Canada, Sum. Rept. 1925, pt.A, pelis.
Ann. Rept., Minister of Mines, B.C., 1924, p88.

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