l ntroduct i on

tocat ion & Access

Topog rap hy

Genera 1 Geology

Local Geology

suwleys

Resu i t s

Conclrrsfons

Recommndat i ons

Certi f icate

Magnetic map

Geochemical map

Green Val ley Mines Ltd.

Vangorda Creek

Page I

Page I

Pagel - 2 Page 2

Page 2 - 3 Page 3

Page 3 - 4 Page 4

Page 4 - 5 Page 5 ( a f t e r )

I n binder a t back

i n binder a t back

the c le lu~s e r r tocsted I n tbte Vangorda Creek Area of Y w k m

Terr i tor ies cnd I la ~ ~ t r i d ~ ~ F P F e l l y ~ l v t r , 7 miles south-eelit of

the f n t e r r e c t f m of 8 l i n c Creek wi th the ~ e l l y ~ l v e r , end 24 m i l e a

fron, the Ross R iver . The 1 3 ~ ~ 0 0 M r i d l a n bisects the group.

ACC(HIS 16 by road to Ross Rlver, a d!!stsnce o f 210 road

r i l e s from mitcrhorse rnC thence by h e I 1 c o p t ~ r o r ~ 1 n t . r rood to the

COIICIW l on.

Thrse tirstriys are o v a i l r b l e st Vangord. Creek, Pam Creek

or Rosa ~ i v a r tor wheel equipped a i r c r a f t , or t n t h e 'tlty R h e r

for ski or f t m t equipped aircraft. me alr distance Is I10 miles.

Regular a i r sentce 1s available to Whttehoru fror, VsWouvU

end EQlontorr, and 0 branch fram the Al-a ~tghwey per to ~ l ~ f t . h o r w .

end f o o t h i l l areas. A g+arnd and n n d b d i s located a l m g the I r i v e r benkb and r i ses to the Anvtl kl.untrins, up to 7 W feet 1r1

height. I FEATWC S

The forests of the srea consist largely of whfte and b l u k

spruce, wl th belsun and Jackoirn. The t t a e r Iin 1s 8-t o t I 4,SOCi feet, but varies. *st p o d stends of t1llb.r are In the r i v e r I valley.' Recent brula b s mad+ the uWrbru8h very dtfftcutt for I

J

Ample wuter 18 avai lable as the Pel ly River Traverses the I property. Power, cdfflswnication end t r o n s w t sewices a n being 1 developed a t WQrby propert ies and rvould be eest ly available. duerbwden I 1, heavy on the property, w l th l i t t l e outcrop - a few pieces 8horing i n I t h e North corner. The property 1s almort en t i re ly conteined I n the I r i v e r ve l l ry .

The general geslogy *ill not be cover.d here, but reference

1s made to the Vurll f y in$ Rwrt of 28th Februery, 1966.

volcanic ash o f C.muo?c 8ilt.. I While I t 18 impossible t o ve r t f y due to toe& of wttr.p, i t I

sedfarnts and volctn!cs, lntluding graansto~o schist, i 1 ~ 8 1 0 m a end

ondesltes. The Tlntinr thrust fault posses just south o f the e l * In

A ~ e o c h m l c a l Survey was csndwcted over the c l e t n r cm 8 grld

of 300 x 100 feet, over eceswble areas. Three h s 8 liner were used.

Saqles m r e taken from the 8/C Ho&izo~ , s t en approximate depth of

Rerut t8 fcont*d 1

I n the a r m o f Base 11- I and ltnts QS end I23 of 81 3 z i n c

results were quite conkitsntly high Lead C-+ wrrcle 81- w e t i

above thres!mIa along ~ . 0 e I f r u $1, but leu for coppw and l e d along

t h a base t l n a 83. long the centre portion of the property results

are ge~ctrally lower by et Ies6t %3S.

sQ!uwm I t la f e l t that the commntm?fea ef zinc values along BL I and ,

flL 5 - w t h , i s lu* to the great- moblllty of zinc lams, causing a coneem-

trati- In the f l a t lytag gravel beds ad-g tbe wily ~ i v t r . Simr 1-4

I 8 constbrably less mobile tham w u l d k leu m t af Iemd on the

W werk could or r h w l l be &me at thfs point. The flat. ~ n r

alla able should be thoroq.bly wm1umt.d aad a ~ e l r r l n r t l o ~ of I n f w n t i m .

I .a a grrdurte of the ~nlvorslty ef Toronto. 1952,

017553Table of ContentsMaps