‘

Sige .

Black Havwhe safer

ie heme nee: Lae mene? B. C. Minister of Mines, 1928, pt..C,
Dp Owen Gives
-A-group-of-elaims: formerly-named the-Black. Hawk is

west of Blackjack Gulch on the northwestern slope of Lost Creek
‘‘Mouttain. The property is reported to be owned by J. Vlasak.

It is accessible by a wagon road that follows the flume from

--Lost Greek Placer: Gold, and then by trail up- Lost Creek Mountain

to an elevation of 4,125 feet. On this property at least eight
northerly and northeasterly striking quartz veins, ranging in

--width-from 15 -inehes to-5 feet, occur within a belt of: fractured

andesite 650 feet wide. A granodiorite batholith outcrops 1¢

‘miles south of the showing. The veins are mineralized with

galena, sphalerite, pyrrhotite, and pyrite, and the wall-rocks

~are- Silicified and pyritized. A selected sample from -one vein

fon. 0.015 ounce of gold a ton and 29.18 ounces, of silver a
on.

Bri ckson Property

This pnoperby. is owned by P. Sheila of Manson Creek,
alal, lies along Olson Creek, 2 miles above its mouth. The claims
straddle a granodiorite- argillite contact. The argillite is
also. cut by aplite dykes up to 30 feet wide. About 400 feet
north of the granodiorite-argillite contact two lenticular
quartz veins 8 and 16 inches wide respectively occur in sheared
argillite. +. They are sparsely mineralized with chalcopyrite and
pyrite and contain low values in gold and.silver.

Blackburn. Property.

six miles up Gaffney Creek from the Manson road is a

~~ ghowing owned by H.~ Blackburn of Fort St.-Jamess It consists of

a pyritized fracture zone, up to 13 feet wide, in grey, cherty
limestone of the Cache Creek group. It is reported to contain

several ounces of silver 2 ton.

-Kohse Copper Property

‘This amanoraal lies on Klawli River about 8 miles above
ra mouth. The claims are underlain by green Takla andesite,
in Deca altered to green, chloritic and talcose schists. A
large body of granodiorite outcrops about 1s miles south of the
mineral showing. The deposit comprises several mineralized
zones in sheared andesite, the widest being 55 feet. These zones
consist of quartz- carbonate veins up to 12 NONE S wide, but.
averaging about 4 inches, each separated by 3 to 4 feet’ of
altered andesite. ‘The veins are abundantly een eed with
chalcopyrite, pyrite, and minor azurite and malachite. The same
minerals are disseminated throughout the intervening altered
andesite. . Four grab samples assayed as follows;

SS |
Sample Gold Silver Copper
REN | OZ. per ton Oz. per ton Per cent
2-inch vein ) 0.41 35.54 ues GAL
12-inch vein )12-foot oer Gy VEN) 2.60
Wall-rock ) zone
between veins) 0.08. 1.95 as

Mineralized andesite
from 55-foot zone 0.06 Bad 0.10

rs | OC AT LC A Cn