assessment on the

ASSESSMENT R E P O R T

ON THE

CAMSELL G R O U P

RICE G R O U P

BROWN G R O U P

HEDLEY, B . C .

SIMILKAMEEN AND OSOYOOS MINING 0 (0 ( 5 ( O # s

NTS 92€18e

Lat i tude 49 ' ps4 (8.7' f

Longitude 120'- b q 3

NTS LTD. A p r i l 3 r d , 1 9 8 7 G

W G. T. CONSULTANTS LTD. CONSUlTlNG GEOLOGISTS

T A B L E OF C O N T E N T S

P A G E

SUMMARY ......................................... 1 I N T R O D U C T I O N 2 .................................... L O C A T I O N AND A C C E S S ............................. 3 P R O P E R T Y ........................................ 3 P H Y S I O G R A P H Y .................................... 7 H I S T O R Y ......................................... 7 GEOLOGY ......................................... 9

G E O P H Y S I C S 1 6 D I S C U S S I O N ...................................... 1 7 S T A T E M E N T O F C O S T S 1 8 C E R T I F I C A T E S - W i l l i a m G . T i m m i n s 2 1

R . K r a u s e , F i e l d S u p e r v i s o r ...... 2 2

A P P E N D I X I - G e o c h e m i c a l R e s u l t s ................ 2 4

G E O C H E M I S T R Y 1 4 .................................... ...................................... .............................. ...............

R E F E R E N C E S ....................................... 2 3

L I S T OF F I G U R E S

1 ) L o c a t i o n Map ........................... 5 2 ) , C l a i . m Map 6

3 ) B r o w n G r o u p ............................ 4 ) R i c e , C a m s e l l G r o u p 11

.............................. G e o c h e m i s t r y Map - L o c a t i o n & R e s u l t s .. Map P o c k e t

I 1 I t

II .................... G e o p h y s i c s - B r o w n G r o u p

5 ) VLF-EM ( R a w D a t a ) ...................... Map P o c k e t 6 ) V L F - E M ( F i l t e r e d & C o n t o u r e d ) I t

7 ) M a g n e t o m e t e r S u r v e y .................... I t

I 1

.......... II

G e o p h y s i c s - C a m s e l l G r o u p

8 ) V L F - E M ( R a w D a t a ) ...................... Map P o c k e t 9 ) V1,F-EM ( F i l t e r e d & C o n t o u r e d ) 1 0 ) M a g n e t o m e t e r S u r v e y

II II

II I 1 .......... ....................

G e o p h y s i c s - R i c e G r o u p

1 1 ) VLF-EM ( R a w D a t a ) ...................... Map P o c k e t 1 2 ) V L F - E M ( F i l t e r e d &. C o n t o u r e d ) 1 3 ) M a g n e t o m e t e r Survey ....................

11 11

!I 11 ..........

W G. T. CONSULTANTS LTD. CONSUlTlNG GEOLOGISTS

- 1 -

SUMMARY

w The e x p l o r a t i o n p r o g r a m s c o n d u c t e d d u r i n g 1986 a n d J a n u a r y 1987

w e r e s u p e r v i s e d by W.G.T . C o n s u l t a n t s L t d . , of V a n c o u v e r , B . C .

A r e g i o n a l p r o g r a m c o n s i s t i n g o f s i l t s t r e a m s a m p l i n g ,

p r o s p e c t i n g a n d m a p p i n g w a s c o n d u c t e d d u r i n g t h e mon ths of May

and J u n e 1986 on t h e Hed1.ey R . C . p r o p e r t y o p e r a t e d by S e a d r i f t

I n t e r n a t i o n a l E x p l o r a t i o n s L t d .

A f o l l o w u p g e o p h y s i c a l p r o g r a m c o n s i s t i n g of EM-VLF a n d magne to -

m e t e r w a s c o n d u c t e d o v e r p o r t i o n s o f t h e p r o p e r t y d u r i n g December

1986 a n d J a n u a r y 1987 . T h e s e l o c a t i o n s w e r e d e l i n e a t e d d u r i n g

t h e p r e v i o u s summer s r e g i o n a l p r o g r a m . The m a g n e t o m e t e r u s e d

w a s a S c i n t r e x MF-I F l u x - g a t e m a g n e t o m e t e r , u s i n g t h e c l o s e d l o o p

me thod f o r d i u r n a l v a r i a t i o n c o r r e c t i o n s ( t h i s u n i t m e a s u r e s t h e

v e r t i c a l component of t h e e a r t h ’ s m a g n e t i c f i e l d ) ; t h e EM-VI,F w a s

a S a b e r Model 2 7 e l e c t r o m a g n e t o m e r i n c o r p o r a t i n g t h e S e a t t l e

c h a n n e l wh ich t r a n s m i t s a t 2 1 . 4 KHz. rlrrr

The c l a i m s a r e l o c a t e d t w o k i l o m e t e r s s o u t h a n d n i n e k i l o m e t e r s

t o t h e w e s t o f t h e town of H e d l e y i n s o u t h w e s t e r n B . C . The

t e r r a i n c o n s i s t s o f m a i n l y m o d e r a t e t o s t e e p s l o p e s F o r e s t e d w i t h

c o n i f e r o u s t r e e s and m o d e r a t e u n d e r g r o w t h .

The p u r p o s e o f t h e r e g i o n a l g e o c h e m i c a l p r o g r a m w a s t o t a r g e t

a r e a s of p o s s i b l e g o l d c o n c e n t r a t i o n b a s e d o n m o d e l s a p p l i c a b l e

t o t h e H e d l e y Go ld Camp.

The s o u t h e r n b l o c k is m a i n l y u n d e r l a i n by t h e N i c o l a Group.

O t h e r r o c k t y p e s o c c u r r i n g o n t h e p r o p e r t y a r e C o a s t T n t r t i s i v e s

a l o n g t h e n o r t h e r n b o u n d a r y , o n e o r more of t h e f o r m a t i o n s

Dradshaw, I n d e p e n d e n c e , Shoemaker a n d Old Tom a l o n g t h e e a s t e r n

b o u n d a r y . P l u g s a n d d y k e s o f g a b b r o o c c u r t h r o u g h o u t t h e Nicola

Group of r o c k s . Bands of me tamorphosed 1 i m e s t o n e , c a l c a r e o u s

a r g i l l i t e s a n d a r g i l l i t e s a r e s e e n on t h e p r o p e r t y . w

W G. T. CONSULTANTS LTD. CONSULTING GEOLOGISTS

- 2 -

INTRODUCTION

W . G . T . C o n s u l t a n t s L t d . , of V a n c o u v e r , R . C . h a v e b e e n r e t a i n e d by

I n t e r n a t i o n a l S e a d r i f t E x p l o r a t i o n s L t d . , t o o p e r a t e a n d

s u p e r v i s e t h e 1986 e x p l o r a t i o n p rogram on t h e Medley C l a i m Group ,

H e d l e y , R . C .

The i n i t i a l p r o g r a m a s c a r r i e d o u t p r o v i d e s g e o l o g i c a l

u n d e r s t a n d i n g of t h e u n d e r l y i n g r o c k s w i t h e m p h a s i s o n t a r g e t i n g

a r e a s of p o s s i b l e economic g o l d c o n c e n t r a t i o n s .

Thi.s r e p o r t i s b a s e d on t h e p r o g r a m s c o n d u c t e d d u r i n g I 9 8 6 a n d

J a n u a r y 1987 , p u b l i s h e d r e p o r t s , maps a n d government , r e p o r t s .

W. G. T. CONSULTANTS LTD. CONSULTING GEOLOGISTS

- 3 -

LOCATION AND ACCESS

W T h e c l a i m Block is 1.ocat;ed f rom 1 t o 10 k i l o m e t e r s s o u t h o f

Ilccll c y w i LIi a c c c s s p r o v i t l c t l by d r y w c a t , I i c r secont l i t i*y roat l s f r o m

t h e main W h i s t l e C r e e k r o a d f rom t h e P a u l C r e e k r o a d , 1 5 k i l o m e t e r s s o u t h of I Ied ley .

PROPERTY

The p r o p e r t y i s f o u n d on NTS map s h e e t 9 2 4 / 8 E ; t h e l a t i t u d e is 49 2 2 a n d l o n g i t u d e i s 120 0 7 ' . T h i s b l o c k c o n s i s t s o f 3 g r o u p i n g s

f r o m a t o t a l of 253 u n i t s .

SOUTH BLOCK: C a m s e l l Group

C L a i m Record Number of

N a m e Number U n i t s E x p i r y Date M . D .

Rice 1

R i c e 2 w 1801

1657 20

20

J a n . 10 /87 S i m i 1 kame e n

J a n . 28/87 osoyoos

C a m s e l l 1 165.5 12 J a n . 28 /87 @ s o y o o s

C a m s e l l 3 1654 1 5 J a n . 28 /87 o s o y o o s

C a m s e l l 4 1653 20 J a n . 28 /87 osoyoos

S n a f u 2 1813 - 6 J a n . 28 /87 S i m i l k a m e e n

9 3 t o t a l

Group I V Rice Group

C l a i m Record

Name Number

Rice #,? 1802

R i c e #4 1658 C a m s e l l #2 1656 S a n f u 2 1652

Number o f

U n i t s E x p i r y D a t e M . D .

20 J a n . 10 /87 S i m i. 1 kame e n

20 J a n . 28 /87 @soyoos

- 1 2 J a n . 28 /87 osoyoos

1 2 J a n . 28 /87 Os0 yoos

6 4 t o t a l


- 4 -

Group V Brown Group

w Claim Re c o r d

Name Number

Brown 1 16.51 Brown 2 1650

Brown 3 1649

Brown 4 1648

,Jessie 1 1647 Ann a t i re e 1646

Number of

U n i t s E x p i r y Date

1.5 J a n . 28 /87 20 . Jan . 28 /87 12 J a n . 28 /87 16 J a n . 28 /87 18 J a n . 28 /87 - 15 J a n . 28 /87 96 t o t a l

M . D .

osoyoos

osoyoos

o s o y o o s

osoyoos

osoyoos

osoyoos


-4

Islands

il

O c e o n

S E A O R I F T I N T E R N A T I O N A L EXPLORATION LTO. H E D L E Y PROPERTY

IO0 0 loo 200 300 4 0 0 Km.

MAP I BRAD‘S D R A F T I N G SFRVICE!

190 2 1 '

i C A L E :

I 100,000 .

I 120'13'

D A T E . F I G U R E : D R A W N B Y

M A R . 87 2 B D S

I 120°05'

' S N A F U 2 1652 (I)

I K m 0 2 K r n 4 Krn 1 J

I

SEADRIFT INTERNATIONAL EXPL. LTD. ,

HEDLEY AREA PROPERTY HEDLEY AREA, 6. C.

S I M I L K A M E E N , O S O Y O O S M. D.

C L A I M L O C A T I O N M A P

- 7 -

PHYSIOGRAPIIY

The t w o c l a i m b l o c k s l i e a t t h e s o u t h e r n e n d o f t h e p h y s i o g r a p h i - c

d i v i s i o n known a s t h e Thompson P l a t e a u S y s t e m w i - t h i n t h e W i l h e r t

Hills a r e a a n d m a i n l y w i t h i n t h e S m i t h , P e t t i g r e w a n d Pair1 C r e e k

d r a i n a g e a r e a s s o u t h and w e s t of H e d l e y . The t e r r a i n v a r i e s f rom

m o d e r a t e s l o p e s t h r o u g h o u t mos t o f t h e p r o p e r t i e s t o s t , e e p e r

s l o p e s o c c u r r i n g a l o n g t h e c r e e k s .

E l e v a t i o n s w i t h i n t h e N o r t h Block r a n g e tip t o 1 , 6 2 5 metcrs a l o n g

t h e W h i s t l e P e t t i g r e w C r e e k r i d g e i n t h e s o u t h w e s t a n d f r o m 550 meters i n t h e n o r t h e a s t w i t h i n t h e S i m i l k a m e e n R i v e r V a l l e y .

W i t h i n t h e S o u t h I3lock, e l e v a t i o n s r e a c h 1980 meters i n t h e

c e n t r a l s o u t h a t t h e h e a d w a t e r s o f t h e e a s t e r l y f l o w i n g P a u l

C r e e k a n d f rom 610 m e t e r s a l o n g t h e e a s t e r n b o u n d a r y a d j a c e n t t o

S i m i l a k m e e n R i v e r .

The ma in w a t e r s o u r c e s would b e t h e c r e e k s m e n t i o n e d a b o v e a n d

W t h e i r t r i b u t a r i e s w h i c h c r o s s t h e p r o p e r t i e s . O t h e r w i s e t h e

p r o p e r t i e s a r e f a i r l y d r y a n d w a t e r s u p p l y would d e p e n d o n

s e a s o n a l r u n o f f .

The f o r e s t c o v e r c o n s i s t s o f f i r , p i n e a n d s p r u c e and v a r i e s from

c l o s e l y g r o w i n g i-mmature s t a n d s t o m o r e w ide3y s p r e a d m a t u r e

s t a n d s .

H I S T O R Y

I n December of 1985 t h r o u g h mid J a n u a r y o f 1986 a d iamond d r i l l

p r o g r a m w a s c a r r i e d o u t on t h e H e d l e y C1ai.m Group f o r a s s e s s m e n t

p u r p o s e s . T h i s p rogram r e v e a l e d t h e c l a i m g r o u p t o b e p a r L i a l l y

unde r1a i .n by f e l s i c v o l c a n i c s w i t h p y r i t i c a l t e r a t i o n . I n

d i amond d r i l l h o l e # 4 a d a c i t i c a n d e s i t e was e n c o u n t e r e d w i t h

z o n e s of p o t a s s i c a l t e r a t i o n , s i . l i c i f i c a t i o n , h e m a t i z a t i o n a n d


- 8 -

z o n e s o f l e a c h i n g i n d i - c a t i n g a h i g h a c t i v i t y o f h y d r o t h e r m a l

w w a t e r s .

I n t h e s p r i n g of 1 9 8 3 a l o w - l e v e l a i r b o r n e magne t i - c a n d VI,F-Em

s u r v e y w a s c a r r i e d o v e r t h e p r o p e r t y w i t h i n t h e Fledley Gold Camp.

The s u r v e y s w e r e c a r r i e d o u t by E . A . Dodd, i n s t r u m e n t o p e r a t o r

a n d p r o j e c t manage r a n d L l o y d B r e w e r , n a v i g a t o r , b o t h o f whom a r e

of Co lumbia A i r b o r n e G e o p h y s i c a l S e r v i c e s L t d . I n t h e S p r i n g

programme a t o t a l o f 559.9 l i n e k i l o m e t e r s of a i r b o r n e s u r v e y s

w e r e d o n e o v e r t h e c l a i m s a n d s u r r o u n d i n g a r e a .

D u r i n g December o f 1984 and J a n u a r y o f 1 9 8 5 , s u r f a c e V L F - E M

s u r v e y s w e r e c a r r i e d o u t o v e r s e l e c t e d a r e a s of t h e H e d l e y c l a i m

g r o u p . The a r e a s were t a r g e t e d f rom t h e p r e v i o u s a i r b o r n e s u r v e y

c o m p l e t e d . The s u r v e y s w e r e c a r r i e d o u t by T r a n s - A r c t i c

E x p l o r a t i o n s L t d . , u n d e r t h e s u p e r v i s i o n of E . A . Dodd,

g e o p h y s i c a l t e c h n i c i a n . A t o t a l of 6 2 . 3 l i n e k i l o m e t e r s of VLF-

EM s u r v e y w e r e clone o v e r b o t h c l a i m g r o u p s .

w A d j a c e n t g r o u n d owned by Masco t Go ld Mines L t d . , r e c e n t l y

a n n o u n c e d t h a t i t h a s e n t e r e d i n t o a f o r m a l c o m m i t t m e n t w i t h t h e

C a n a d i a n I m p e r i a l Bank o f Commerce i n t h e amount o f $50 m i l l i o n

d o l l a r s . A p r o j e c t e d p r o d u c t i o n of 1 , 8 0 0 t o n s p e r d a y w i l l see

t h e p r o j e c t p r o d u c e a p p r o x i m a t e l y 1 0 0 , 0 0 0 t r o y o u n c e s o f g o l d p e r

annum For e a c h o f t h e f i r s t t w o y e a r s a t a n a v e r a g e o p e r a t i n g

c o s t of $120. U . S . p e r o u n c e , w h i c h w i l l r e s u l t i n a p a y b a c k

p e r i o d of u n d e r Lhree y e a r s b a s e d on $ 3 2 5 . U . S . p e r o u n c e .

As of J a n u a r y 1986 t h e p r e l i m i n a r y o r e r e s e r v e s a r e 7 , 1 0 0 , 0 0 0

t o n s g r a d i n g 0 . 1 5 t r o y o z . / t o n .

T h e s e r e s u l t s a r e b a s e d on t h e r e s u l t s of diamond d r i l l i n g wh ich

a l s o i n d i c a t e a downward c o n t i n u a t i o n o f t h e known mi .ne ra l i . zed

s t r u c t r i r e .


- 9 -

GEOLOGY 'cr

The f o l l o w i n g i s q u o t e d f rom S o o k o c h o f f ' s March 1983 r e p o r t :

" A c c o r d i n g t o Map 88A - P r i n c e t o n , t he g e n e r a l a r e a i s

u n d e r l a i n by t h e CJpper T r i a s s i c Nicola C r o u p o f v o l c a n i c s ,

s e d i m e n t s a n d s c h i s t s wh ich a r e i n t r u d e d by t h e J u r a s s i c

C o a s t I n t r u s i v e s a n d i n t r u s i v e s of p e r i d o t i t e , p y r o x e n i t e

a n d g a b b r o .

"The C o a s t I n t r u s i v e s a r e p r e d o m i n a n t i n e n v e l o p i n g t h e

Nicola Group which f o r m s a b a n d s t r e t c h i n g f r o m s o u t h o f

P r i n c e t o n t o beyond Kamloops Lake i n t h e n o r t h . The same

i n t r u s i v e s i n a d d i t i o n t o the more m a f i c r o c k i n t r u s i v e s a n d

p i n k a n d g r e y g r a n i t e a n d g r a n o d i o r i t e o f t h e [ Jpper

C r e t a c e o u s O t t e r I n t r i i s i o n s o c c u r a s s t o c k s a n d p l u g s w i t h i n

t h e N i c o l a b a n d . 'I

'IThe l a t e s t r o c k s of t h e r e g i o n , t h e K i n g s v a l e and P r i n c e t o n

Group o f v o l c a n i c s o c c u r a s v a r i s i z e d c a p p i n g s t h r o u g h o u t

t h e a r e a . "

"The N i c o l a g r o u p c o n s j s t s of a s u c c e s s i o n o f l a v a s o f

unknown t h i c k n e s s w i t h i r r e g u l a r i n t e r c a L a t i o n s o f

t u f f a c e o u s a n d a r g i l l a c e o u s l e n s e s a n d o c c a s s i o n a l b e d s o f

l i m e s t o n e . Dawson s t a t e s t h a t " t h e r e seems t o b e f u r t h e r in

s e v e r a l p l a c e s , a b l e n d i n g o f m a t e r i a l s o r i g i n a l l y v o l c a n i c

wiLh q i i a r t z o s e s e d i m e n t s , . . .

" F l o w b r e c c i a s a r e p r o b a b l y more common t h a n m a s s i v e l a v a

w i t h t h e d i f f e r e n t t y p e s a1 so mixed t o g e t h e r . An u n u s u a l

c a s e of a f l o w is a g r e e n i s h r o c k c o n t a i n i n g r o u n d e d

F r a g m e n t s of wha t a p p e a r s t o b e a red s y e n i t e b u t i s

a c t , u a l l y a f l o w b r e c c i a f e l d s p a r p o r h y r y . "

"The s e d i m e n t a r y r o c k s a r e m o r e r e s t r i c t e d w i t h s o m e

s e d i m e n t s o f c o n s i d e r a b l e e x t , e n t , however more commonly a s


- 1 0 -

s m a l l p a t c h e s of f i n e - g r a i n e d , w e l l -bedded t u f f o r

t u f f a c e o u s a r g i l l i t e a n d s m a l l l e n s e s o f b l u e - g r e y l i m e s t o n e

a l l t h r o u g h t h e v o l c a n i c r o c k s . 'I

" B r e c c i a s a r e common i n c e r t a i n a r e a s . The b r e c c i a s c o n s i s t

of a n g u l a r f r a g m e n t s ' h a l f a n i n c h t o o n e i n c h j.n s i z e ' , o f

p r e d o m i n a n a t l y v o l c a n i c r o c k s w i t h a r g i l l i t e wh ich a r e

f r e q u e n t l y a s s o c i a t e d w i t h t u f f o r g r e y w a c k e of ' a n e i g h t h

of o n e i n c h a c r o s s s u b a n g u l a r g r a i n s . It

" A t t h e I-ledley Camp g o l d d e p o s j . t s , t h e s t a t i f i e d N i c o l a

Rocks o f t h i n b e d d e d q u a r t z i - t e , a r g i l l i t e , t u f f a n d b r e c c i a ,

i n p a r t much s i l i c i f i e d , a r e f l o o r e d of a l a r g e body o f

g r a n o d i o r i t e arid i n t r u d e d by g a b b r o s t o c k s , d y k e s and s i l ls .

"The g r a n o d i o r i t e r a r e l y i s f o u n d i n the s e d i m e n t s , h o w e v e r ,

t h e b a s i c i n t r u s i o n s are a b u n d a n t l y r e p r e s e n t e d t h r o u g h the

ore z o n e . The ' C l i m a x s t o c k ' w a s o r i g i n a l l y b e l i e v e d t o b e

a s t o c k , h o w e v e r , t h e lower c o n t a c t i s c o n c o r d a n t w i t h t h e

i n t r u d e d s e d i m e n t s so t h a t t h e body c l o s e l y r e s e m b l e s a

l a r g e i r r e g u l a r s i l l . On t h e e a s t e r n p a r t of t h e C l i m a x

s t o c k , t h e ' s i l l s a n d d y k e s ' a r e p o r p h y r i e s . "

" E x t e n s i v e d e v e l o p m e n t of c o a r s e g a r n e t and p y r o x e n e s k a r n s

o c c u r s a s a h a l o o n t h e s u r f a c e o f t h e p o r p h y r y s i l l s which

a r e i n c o n t a c t ; w i t h l i m e s t o n e . The known o re s h o o t s o c c u r

i n t h e s k a r n n o t more t h a n ' 2 5 0 f e e t ' €rom the l i m e s t o n e

c o n t a c t . 'I

"The ma in N i c k e l P l a t e o r e b o d i e s v a r i e d f r o m ' I O Feet t o

more t h a n 100 F e e t ' i n t h i c k n e s s and w e r e u p t o ' 5 0 0 f e e t i n

l e n g t h a n d 350 f e e t i n w i d t h ' . The o r e b o d i e s o c c u r r e d

w i t h i n a z o n e p l u n g i n g N20W a t 30 d e g r e e s f o r a s l o p e

d i s t a n c e of ' 3 , 0 0 0 f e e t ' . W i t h i n t h e z o n e , t h e r e w e r e at

l e a s t s e v e n i r r e g u l a r s h e e t - l i k e d e p o s i t s o v e r l a p p i n g e n

e c h e l o n . I n a d d i t i o n t o o r e w i t h i n the s k a r n z o n e s , g o l d b v

W G. T. CONSULTANTS LTD. CONSUlTlNC GEOLOGISTS

- 1 1 -

m i n e r a l i z a t i o n a l s o o c c u r s i n c r o s s - c u t t i n g f r a c t u r e s of t h e

' d y k e s a n d s i l l s . '

"The N o r t h B l o c k H e d l e y p r o p e r t y o f S e a d r i f t I n t e r n a t i o n a l

p r e d o m i n a n a t l y c o v e r s t h e Ni-co la g r o u p of r o c k s i n c o n t a c t

w i t h i n t r u s i v e s i n t h e n o r t h e r n a n d s o u t h e a s t e r n p o r t i o n . A

g a b b r o i c p l u g i s i n d i c a t e d a l o n g t h e c e n t r a l e a s t e r n

b o r d e r .

" M i n e r a l s h o w i n g s w i t h i n o n e t o f o u r krn e a s t o f t h e N o r t h B l o c k

a r e d e s c r i b e d as:

IIa t h i c k s e r j e s of s t e e p l y d i p p i n g t i l t e d a r g i l l i t e s

i n t r u d e d by d y k e s a n d i r r e g u l a r masses o f d i o r i t e . Most o f

t h i s a r g i l l i t e is m a s s i v e a n d b l a c k . . . . . n o t l e s s t h a n

200 f e e t t h i c k or l i g h t c o l o u r e d r o c k s c o n s i s t i n g of

c a l c a r e o u s a r g i l l i t e , c h e r t , s o m e l i m e s t o n e a n d p o s s i b l e

s o m e t u f f s . . . The rocks h a v e b e e n f r a c t u r e d a n d s o m e o f

t h e s e f r a c t , u r e s h a v e b e e n f i l l e d by q u a r t z c a r r y i n g p y r i t e ,

a r s e n o p y r i t e , s p h a l e r i t e and a l i t t l c c h a l c o p y r i t e a n d

p y r r h o t i t e . The q u a r t z s t r i n g e r s a r e a l l s m a l l , t h e z o n e s

o f f r a c t u r i n g g e n e r a l l y weak , b u t s o m e o f t h e s e s m a l l

s t r i n g e r s c a r r y m o r e t h a n 2 o u n c e s of g o l d a t o n .

' I . . . . f i v e s h e a r - z o n e s wh ich t e n d t o f o l l o w t h e b e d d i n g

a r e l i g h t c o l o u r e d i n p a r t c a l c a r e o u s and c h e r t y s e d i m e n t s . . . The b e l t o f ( l i g h t c o l o u r e d ) s e d i m e n t s is i n t e r e s t i n g ,

b e c a u s e i n t h e s e a r s e n o p y r i t e , c o n t a i n i n g v a r i a b l e g o l d

v a l u e s , s e e m s t o o c c u r i n p r e f e r e n c e t o t h e d a r k e r

a r g i l l i t e s . . . It

"On t h e s h o w i n g e a s t o f W h i s t l e C r e e k :

"The d e p o s i t a p p e a r s t o h a v e f o r m e d by t h e r e p l a c e m e n t o f

g r e y , c h e r t y l i m e s t o n e , p r o b a b l y a l o n g some s o r t of a

f i s s u r e or f r a c t u r e z o n e , by a r s e n o p y r i t e a n d p y r i t e w i t h

W G. T. CONSULTANTS LTD. CONSULTING GEOlOGISTS

- 1 2 -

c a l c i t e a b o u t t h e o n l y i n t r o d u c e d g a n g u e m i n e r a l . . . t h e

m i n e r a l zone i s 6 t o 12 i n c h e s w i d e . . . a n o t h e r z o n e is 18

t o 24 i n c h e s w i d e . S a m p l e s of t h i s m a t e r i a l h a v e a s s a y e d

f rom 1 /4 t o 1 /2 o u n c e o f g o l d p e r t o n . "

"On a f o r m e r l y d i s c o v e r e d m i n e r a l s h o w i n g f o u r km t o t h e e a s t on

wh ich Banbury Gold i n c o n d u c t i n g e x p l o r a t i o n a n d d e v e l o p m e n t

work , t h e s h o w i n g i s d e s c r i b e d a s f o l l o w s : "

" F o u r s h e a r z o n e s a r e known on t h e p r o p e r t y , t h e p r i n c i p a l

o n e b e i n g o n t h e Maple L e a f c l a i m . T h i s is a n i r r e g u l a r ,

b r a n c h i n g z o n e s t r i k i n g n o r t h a n d d i p p i n g 60 d e g r e e s t o t h e

w e s t , w i t h o re s h o o t s d e v e l o p e d a t i n t e r v a l s a l o n g i t . The

z o n e i t s e l f i s a s much as 30 f e e t w i d e , b u t t h e g r e a t e s t

w i d t h o f q u a r t z is 1 2 f e e t . The o re m i n e r a l s o c c u r i n t h e

q u a r t z , b u t a r e n o t e v e n l y d i s s e m i n a t e d . The s h e a r m e e t s

t h e d i o r i t e a t a n a c u t e a n g l e , a n d i s b e s t m i n e r a l i z e d i n

t h e m e t a m o r p h i c r o c k s n e a r t h e c o n t a c t , b u t is b a r r e n i n t h e

d i o r i t e . . . Gold v a l u e s a r e e r r a t i c , v a r y i n g from 0 . 0 2

o u n c e s t o 0 . 8 0 o u n c e s a t o n . . .

t tThe S o u t h B l o c k i s a l s o p r e d o m i n a n t l y u n d e r 1 a i n b y Nico la

V o l c a n i c s i n c o n t a c t w i t h j n t r i i s j v e s a l o n g t h e n o r t h e r n a n d

e a s t e r n p e r i p h e r y . Gabbro p l i i g s a r e a l s o i n d i c a t e d w i t h i n

t h e g r a n i t e s i n t h e n o r t h e a s t e r n p o r t i o n o f t h e p r o p e r t y .

" T w o o l d m i n e r a l s h o w i n g s , o n e o f w h i c h i s n o t i n c l u d e d i n t h e

p r o p e r t y a n d t h e o t h e r i s f o u n d w i t h i n t h e s o u t h e a s t p o r t i o n of

t h e S o u t h B l o c k . The m i n e r a l s h o w i n g w i t i n t h e Crown g r a n t s is

d e s c r i b e d a s : I'

" s t e e p l y t i t l e d , b a n d e d s e d i m e n t s s t r i k e n o r t h - s o u t h and a r e

i n t r u d e d by d y k e s a n d s i l l s o f a u g i t e a n d / o r h o r n b l e n d e

a n d e s i t e s a n d d i o r i t e s . J u s t n o r t h w e s t o f t h e c l a i m s a r e

b a n d e d p u r p l e a n d g r e e n a n d e s i t e f l o w s a n d some breccias,

a n d t o t h e w e s t t o a t l e a s t a s f a r a s t h e 6 , 6 1 6 f o o t summit


- 1 3 -

( 1 m i l e t o t h e n o r t h w e s t ) is a l i g h t g r e y i n t r u s i v e d a c i t e .

C h e r t y ( p r o b a b l y s e d i m e n t a r y ) b r e c c i a s l i e b e t w e e n t h e

s e d i m e n t s and d a c i t e on t h e w e s t . The s e d i m e n t s a r e

a r g i l l a c e o u s t o q u a r t z i t e r o c k s , a l l me tamorphosed , and a r e

i n many r e s p e c t s s i m i l a r t o t h o s e e n c o u n t e r e d on N i c k e l

P l a t e Moun ta in . . . t h e d a c i t e i s a f r e s h , v a r i a b l e r o c k of

c o n s i d e r a b l e a r e a and c o n t a i n s p h e n o c r y s t s o f q u a r t z a n d

f e l d s p a r . . M i n e r a l i z a t i o n i n c l u d e s , a r e s e n o p y r i t e ,

p y r i t e and p y r r h o t i t e . I t is f o u n d a l m o s t e n t i r e l y i n t h e

s e d i m e n t s a n d a p p e a r s t o o c c u r s e l e c t i v e l y i n a f i n e d e n s e

b r o w n i s h r o c k wh ich i s p r o b a b l y a n a l t e r e d s h a l e . . . A l t e r a t i o n of b r o w n i s h f i n e s e d i m e n t s i n r e c t i c u l a t i n g

v e i n l e t s , i s a c c o m p a n i e d by s c a t t e r e d c r y s t a l s a n d i n s e a m s

a n d b l e b s of a r e s e n o p y r i t e . . .

"On t h e s h o w i n g i n d i c a t e d t o b e c o v e r e d by t h e N o r t h B l o c k a n d

bwo a n d o n e - h a l f km n o r t h e a s t o f t h e a b o v e d e s c r i b e d c rown g r a n t

s h o w i n g t h e d e p o s i t i s d e s c r i b e d a s f o l l o w s :

"The m i n e r a l d e p o s i t c o n s i s t s of p y r i t e , p y r r h o t j t e a n d

a r s e n o p y r i t e i n a s h e a r e d a n d a l t e r e d zone c r o s s i n g a 2 0

f o o t g r a n i t i c s i l l t h a t c u t s a r g i l l i t e a n d l i m e s t o n e a n d is

e s s e n t i a l l y c o n f i n e d t o t h e s i l l . The u n a l t e r e d h o s t r o c k

i s a n o r m a l a m p h i b o l i t e g r a n o d i o r i t e o r q u a r t z d i o r i t e

r e l a t e d t o t h e n e a r b y b a t h o l i t h . W h i l e a l t e r e d i t becomes

l i g h t c o l o u r e d and f i n e g r a i n e d a n d c o n s i s t s l a r g e l y o f

q u a r t z , e p i d o t e , c a l c i t e , p y r o x e n e ( p r o b a b l y d i o p s i d e ,

z i o s i t e a n d a p l i t e ) . A l t h o u g h r e s t r i c t e d i n e x t e n t , t h e

s u l p h i d e s a r e l o c a l l y m a s s i v e w i t h much a r e s e n o p y r i t e .

However, two s a m p l e s o f this m a t e r i a l t a k e n by I Ied ley o n l y

r e t u r n e d 0 . 0 2 and 0 . 0 1 o u n c e s o f g o l d p e r t o n r e s p e c t i v e l y . "


- 14 -

GEOCHEMISTRY

D u r i n g t h e mon ths o f May a n d J u n e , 1 9 8 6 , a r e g i o n a l s t r e a m

s e d i m e n t s ampl i -ng p rogram was c o n d u c t e d o v e r t h e J led ley c l a i m

g r o u p f o r S e a d r i f t I n t e r n a t i o n a l E x p l . o r a t i o n s L t d .

T h i s s i l t s t r e a m s a m p l i n g p rogram was c o n d u c t e d o v e r a l l s b r e a m s

o n t h e p r o p e r t y w i t h s a m p l e s t a k e n a t 100 meter i n t e r v a l s . Eacll

s a m p l e w a s a n a l - y s e d by T C P f o r Au, Ag, Cu, P b , Zn, As, W , C o , B i ,

S b , a n d F e by A c m e A n a l y t i c a l Labs of Vancouver , B . C . Also g r a b

s a m p l e s w e r e c o l l e c t e d d u r i n g t h e p r o s p e c t i n g p rogram a n d w e r e

a s s a y e d For Au and Ag.

With a l i m i t e d knowledge of t h e s t r a t i g r a p h y a n d g e o l o g y

u n d e r l y i n g t h e p r o p e r t y t h e si1.t s a m p l e s were gro i iped a s o n e

' p o p u l a t i o n . A f i r s t a p p r o x i m a t i o n was a p p l i e d u s i n g t h e G a u s i a n

C u r v e d i s t r i b u t i o n . S t a t s t i c a l a n a l y s i s was a p p l i e d t o Aug, Ag,

W , and Zn. 'crr

STATISTICS

C r e e k s : J o h n ' s , J o h n ' s 2 , J o h n ' s 3, J o h n ' s 4, L a r c a n , P e t t i g r e w

a n d P e t t i r g r e w 2

A u : N o . of S a m p l e s ( n )

n = 185 mean = 5.85 S D = 38.99

U s i n g pop n = 183 ( d e l e t e 120 pph; 4.55 p p b )

mean 1.88 S t a n d a r d Dev. 1 . 6 1


- 1s -

Ag:

W:

Zn:

No. of S a m p l e s ( n )

n = 1 8 5

No. of S a m p l e s ( n )

n = 1 8 5

N o . of S a m p l e s ( n )

mean = .16 s n = . t o

mean = 1 . 5 3 S D = 3.58

n = 1 8 5 mean = 6 6 . 7 8 S D = 6 7 . 6 3

E v i d e n c e d by t h e s t a t i s t i c a l m a n i p u l a t i o n a r e a n o m a l o u s s i l t

samples. T h e s e a n o m a l o u s v a l u e s a r e s p o r a d i c a n d a r e primarily

A u , A g , and A s , t h e r e w a s o n l y o n e c o b a l t anomaly r e t u r n e d a n d

, t h i s w a s f o u n d a l o n g t h e d r a i n a g e p a t t e r n of J o h n ' s 2 C r e e k . The

s a m p l e s t a k e n u p s t r e a m of t h i s c o b a l t anomaly show 3 a r s e n i c a n d

6 s i l v e r a n o m a l i e s of wh ich t h e r e is o n l y o n e c o i n c i d e n t anomaly .

J o h n ' s 2 c r e e k r e t u r n e d t h e h i g h e s t g o l d geochem f o u n d i n the

s i l t s , t h i s w a s 455 pph.

w

J o h n ' s 4 c r e e k r e t u r n e d t w o a n o m a l o u s gold, 1 2 0 ppb a n d 14 ppb a t

1 0 N a n d 9N r e s p e c t i v e l y

W G. T. CONSULTANTS LTD. CONSULTING CXOLOCISTS

- 16 -

GEO PHY S I C S

I n December of 1986 and J a n u a r y of 1 9 8 7 , a g e o p h y s i c a l s u r v e y

c o n s i s t i n g of m a g n e t o m e t e r a n d VLF-EM w a s c o n d u c t e d o v e r

d e s i g n a t e d p o r t i o n s of t h e p r o p e r t y .

' T h e e q u i p m e n t u s e d i n t h e s u r v e y was a S c i n t r e x MF-1 F l u x - g a t e

m a g n e t o m e t e r wh ich m e a s u r e s t h e v e r t i c a l component, o € t h e e a r t h ' s

m a g n e t i c f i e l d . The c l o s e d l o o p method w a s u s e d t o c o r r e c t f o r

d i u r n a l v a r i a t i o n s i n t h e e a r t h ' s m a g n e t i c f i e l d . A S a b e r Model

2 7 VLF-EM was u s e d a n d wh ich i n c o r p o r a t e d t h e S e a t t l e s t a t i o n

wh ich t r a n s m i t s a t 2 1 . 4 KHz. VLF-EM d a t a w a s f r a s e r f i l t e r e d

t h e n c o n t o u r e d .

The g e o p h y s i c a l s u r v e y c o n s i s t e d of t h r e e grids, a grid w a s

p l a c e d o v e r a p o r t i o n of e a c h o f t h e t h r e e c l a i m g r o u p i n g s a n d

t h e g r o u p i n g name d e s i g n a t e s t h e s u r v e y g r i d name; C a m s e l l , Rice

a n d Drown g r i d s . W

O v e r a l l , m a g n e t i c a l l y t h e p r o p e r t y i s r e l a t i v e l y f l a t ; t h i s

r e f l e c t s t h e u n d e r l y i n g g e o l o g y which c o n s i s t s p r i m a r i l y o f

t u f f a c e o u s r o c k s , a r g i l l i t e s , l i m e s t o n e s , a r g i l l a c e o u s l i m e s t o n e s

a n d i n t r u s i v e s . The i n t r u s i v e s h a v e b e e n r e g i o n a l mapped a n d a r e

a s s o c i a t e d w i t h t h e c o a s t p l u t o n i c complex .

The VLF-EM d a t a i n d i c a t e s l i n e a r s a r e p r e s e n t o n t h e p r o p e r t y ,

t h e s e l i n e a r s m o s t l i k e l y r e p r e s e n t f a u l t s a n d a r e f o u n d most

p r o m i n e n t on t h e C a m s e l l a n d R i c e G r o u p s w h i l e t h e Brown Group

a p p e a r s r e l a t i v e l y f l a t .

The l i n e a r s s e e n on b o t h g r i d s s t r i k e i.n a n o r t h e r l y a n d

n o r t h e a s t e r l y d i r e c t i o n .


- 1 7 -

DISCUSSION

The o r i g i n o f t h e s i l t s t r e a m a n o m a l i e s n e e d t o b e f o l l o w e d u p ,

t h e i r s o u r c e and o r i g i n l o c a t e d .

It a p p e a r s t h a t t h e t w o f a u l t s s e e n i n t h e VLF-EM d a t a on t h e

C a m s e l l Group c o u l d p o s s i b l y b e a s s o c i a t e d w i t h t h e a n o m a l o u s

s i l v e r a n d a r s e n i c v a l u e s s e e n i n t h e s i l t s t r e a m a n o m a l i e s .

T h i s a r e a is a h i g h p r i o r i t y a n d it i s recommended t h a t follow up

work b e i n i t i a t e d i n t h i s a r e a .

R e s p e c t P u l l y ,

W . G . Timmins , P . E n g . W.G.T. CONSULTANTS LTD. 902 - 837 West H a s t i n g s S t . , V a n c o u v e r , B . C .


- 18 -

STATEMENT OF COSTS

'rrr DROWN GROUP

S i i n c i * v i.s ion & Prosoectine

R. Krause 11 days 8 $250./day

Sample Collection

G. Auger 9 days @ $250./day

Silt Geochemistry (I.C.P.)

93 samples @ $1 2.25/sampIe

Support Costs

$60.00/man/day x 2 men x IO days

Truck Rental

$60.OO/day x 10 days

Fuel, Shipping, misc. (flagging, etc.)

w Ge o ph y s i c s

Grid Placement & VLF-EM & Magnetometer

20 line km's 8 $380.00/km

Report

PAC ACCT

Apply 1 year to:

Brown I (1651 Jan); Brown 2 (1650 Jan.) Brown 3 (1649 Jan); Brown 4 (1648 Jan.) Jesse S (1647 Jan); hnnahree (1646 Jan.)

$ 2,750.00

2,250.00

1,139.25

1,200.00

600.00

900.00

7,200.00

$169039.25 1.000.00

$17,039.25

2.200.00


CAMSELL GROUP

Supervision and Prospecting 'cr

4 d a y s 8 $250.OO/day

Sample Collection

4 days 8 $250.00/day

S i . L b GcocI~(.ttii.s(,t.y ( 1 .C.P.)

78 samples @ $12.25/sample

Support Costs

60/man/day x 2 men x 5 days

Fuel, Shipping Costs, Misc.

Geophysics: Grid Pl.acement & VLF-EM & Magnetometer

27.1 line km's 8 $380.00/km

Report

PAC

$ 1,000.00

1,000.00

955.50

600.00

4.50*00

10.298.00

$14,603.50

Apply 1 y e a r to:

Rice I (1801 Jan); Rice 2 (1657 Jan.) Camsell I (1655 Jan); Camsell 3 (1654 Jan.) Camsell 4 (1654 Jan); Snafu I (1813 Jan.)


- 20 -

R I C E GROUP

c S i l t G e o c h e m i s t r y ( I . C . P . )

14 s a m p l e s @ $ 1 2.2 .5 /sample

S u p e r v i s i o n & P r o s p e c t i n g

2 clays @ $ 2 5 0 . 0 0 / c i n y

Sample C o l l e c t i o n

1 d a y Q $250.OO/day

S u p p o r t C o s t s

$60 .00/man/day x 2 men x 2 days

T r u c k R e n t a l

$60.OO/day x 2 d a y s

F u e l , S h i p p i n g & Misc.

G e o p h y s i c s : G r i d P l a c e m e n t & VLF-EM & Magnetorneker

2 2 l i n e k m ' s Q $380.00/km

R e p o r t

PAC

Apply 1 y e a r t o :

R i c e 3 ( 1 8 0 2 J a n ) ; Rice 4 (16.58 Jan.) C a m s e l l 2 (1656 J a n ) ; SnaFu 2 ( 1 6 5 2 J a n . )

$ 171.50

500 .00

2.50.00

240 .00

1 2 0 . 0 0

1 0 0 . 0 0

8 , 3 6 0 . 0 0

$ 9 , 7 4 1 . 5 0

3 0 0 . 0 0

$ 1 0 , 0 4 1 . 5 0

3 , 8 4 0 . 0 0

____ $ 1 3 ,88 .-.____ 1 . 50

W G. T. CONSULTANTS LTD, CONSULTING GEOLOGISTS

- 2 1 -

CERTIFICATE

I, W T L L I A M G . T I M M T N S o f t h e C i - ty of V a n c o u v e r , i n t h e srr

P r o v i n c e of B r i t i s h C o l u m b i a , h e r e b y c e r t i f y t h a t , :

1 . T a m a g e o l o g i s t w i t h o € f i c e s a t 902 - 837 West [ l a s t i n g s

S t r e e t , V a n c o u v e r , B r i t i s h C o l u m b i a .

2 . I am a g r a d u a t e of t h e H a i l e y b u r y S c h o o l o f Mi-nes,

H a i l e y h u r y , O n t a r i o , a n d a t t e n d e d Mi-chigan T e c h n o l o g i c a l

I J n i - v e r s i t y .

3 . T am a member o f t h e P r o f e s s i o n a l E n g i n e e r s o F D r i t , i s h

Co lumbia and o f t he A s s o c i a t i o n O F P r o f e s s i o n a l E n g i - n e e r s ,

G e o l o g i s t s and G e o p h y s i c i s t s of A l b e r t a .

4 . T h a v e no d i r e c t o r i n d i r e c t i n t e r e s t i n e i t h e r t h e p r o p e r t y

o r s e c u r i t i e s o f I n t e r n a t i o n a l S e a d r i f t E x p l o r a t i o n s L t d . ,

or i t s a f f i l i a t e s , n o r d o I e x p e c t t o r e c e j v e a n y s u c h

i n t e r e s t .

5 . T h i s r e p o r t i s b a s e d on p u b l i s h e d r e p o r t s , r e c o r d s ,

g o v e r n m e n t r e p o r t s a n d s u p e r v i s i o n of a f i e l d p r o g r a m

c a r r i - e d o u t by M r . R . K r a u s e , B . S c . , e m p l o y e d by m e a n d

whose work i s w e l l known t o m e .

6 . I h e r e b y c o n s e n t t o t h e u s e of t h i s r e p o r t by t h e Company i n

c o n n e c t i o n w i t h a P r o s p e c t u s of a S t a t e m e n t of M a t e r i - a 1

F a c t s r e l a t e d t o t h e r a i s i n g of f u n d s f o r t h i s p r o j e c t .

D A T E D a t V a n c o u v e r , i n t h e P r o v i n c e of B r i t i s h C o l u m b i a , t h i s 3rd

d a y o f A p r i l , 1987.

W T L L T A M G . TTMMINS, P.Eng.


- 2 2 -

CERTIFICATE

T , ROBERT G . K R A U S E , of t h e C i t y of Vancouver , i n t h e

P r o v i n c e of B r i t i s h Co lumbia , h e r e b y c e r t i f y t h a t :

1 . I am a g e o l o g i s t w i t h o f f i c e s a t 902 - 837 West H a s t i n g s

S t r e e t , V a n c o u v e r , B r i t i s h Co lumbia .

2 . I am a g r a d u a t e of t h e U n i v e r s i t y of B r i t i s h C o l u m b i a ,

V a n c o u v e r , B r i t i s h Co lumbia .

3 . 1 h a v e worked i n t he m i n e r a l e x p l o r a t i o n f i e l d for 10 y e a r s

and h a v e p r a c t i s e d as a g e o l o g i s t f o r 2 y e a r s .

4. T p e r s o n a l 1 . y s u p e r v i s e d t h i s e x p l o r a t i o n p rogram o n s i t e .

DATED a t V a n c o u v e r , i.n t h e P r o v i n c e of B r i t i s h C o l u m b i a , this 3 r d

d a y o f A p r i l , 1987 .

R O O E R T G . KRAUSE, l 3 . S ~ . G e o l o g i s t


- 2 3 -

REFERENCES

D a v e Mark, G e o p h y s i c i s t s ; G E O P H Y S I C A L R E P O R T ON T H E A I R B O R N E

M A G N E T I C AND VLF-EM S U R V E Y S OVER T H E H E D L E Y P R O P E R T Y O S O Y O O S

AND S I M I L K A M E E N M I N I N G D I V I S I O N B R I T I S H C O L U M B I A : F e b r u a r y ,

1 9 8 4 -

D a v e Mark, G e o p h y s i c i s t : G E O P H Y S I C A L R E P O R T ON A VLF-EM S U R V E Y

OVER T H E BROWN C L A I M G R O U P . J O H N ' S C R E E K . HEDLEY AREA

O S O Y O O S M I N I N G D I V I S I O N B R I T I S H C O L U M B I A : A p r i l 2 5 t h , 1985.

D a v e Mark, G e o p h y s i c i s t s ; G E O P H Y S I C A L R E P O R T ON A VLF-EM S U R V E Y

ON TIIE C A M S E L L AND R I C E C L A I M G R O U P S , LARCAN C R E E K , H E D L E Y

A R E A O S O Y O O S AND S I M I L K A M E E N M I N I N G D I V I S I O N : April 9 t h , 1985.

W . G . T i m m i n s , R . K r a u s e : A S S E S S M E N T R E P O R T ON T H E H E D L E Y

P R O P E R T Y O S O Y O O S AND S I M I L K A M E E N M I N I N G D I V I S I O N . B R I T I S I I

C O L U M B I A : March. 1986.


- 24 -

A P P E N D I X


ACME CINALYTICfiL LABORATORIES LTD. DATE RECEIVEDz JUNE 28 1986 OS2 E.HASTINGS ST-VANCOUVER B.C. V 6 4 1R6

W O N € 253-3158 DATA LINE 251-1011 DATE REPORT MAILED:

GEOCHEMICCIL I C P R N F I L Y S X S

,500 6RAH SAHPLE IS Dl6ESTEO WITH 3HL 3-1-2 HCL-HNO3-HZO AT 95 DE6. C FOR ONE HOUR AND IS DILUTED T d 10 HL WITH WATER. THIS LEACH IS PARTIAL FOR HN.FE.CA.P.CR.H6.BA,Tl.B.AL.NA.K.W.Sl.ZR.CE,SN,V.N8 AND Tll. AU DETECTION LlHlT BY ICP IS 3 PPH. - SAHPLE TYPE! SILTS -35 HESH AU ANALYSIS BV AA FROH 10 6RAH SAHPLE.

ASSCSYCRr %&p. .DEAN TOYE. CERTIFIED B.C. ASSAYER.

SEADRIFT INT. FROJECT - HED FILE # 86-1204 PAGE 1

5AHPLEI Cu Pb Zn Ag Co Fe As Sb Bi W hut PPI! PPH PPH PPH PPH X PPH PPH PPH PPH PPB

JOHNS 19N 19 10 45 .1 7 3-06 9 2 2 2 1 JOHNS 18N 21 4 47 .l 7 2.71 14 2 2 3 2 JOHNS 1711 27 6 47 . I 7 2.89 11 2 2 1 10 JOHNS I6N 21 4 43 .1 6 2.51 11 3 2 1 2 JOHNS 15N 22 5 54 .l 6 2.27 10 2 2 1 1

JOHNS 14N 30 2 59 .1 7 2.07 11 2 3 1 3

JOHNS 12N 21 E 52 .1 5 1.77 12 2 3 2 2 JOHMS 11M 23 5 SO .1 S 1.70 14 3 2 2 3 JOHNS ION 21 2 51 .l 6 1.80 11 2 2 2 1

JOHNS 13N 26 4 5s .2 s 1.80 i o 2 2 1 3

JOHNS 9N 20 3 51 .2 5 1,72 13 2 2 I 1

JOHNS 7N 23 4 54 .I S 1.74 12 2 3 1 2 JOHNS 6N 23 2 47 .1 5 1.69 12 4 2 1 2 JOHNS SN 22 6 47 . t 5 1.76 14 . 2 2 2 2

JOHNS 8N 21 2 59 .2 5 1.89 15 2 4 i 1

JOHNS I N 20 5 50 .l 6 1.90 14 2 2 3 3 JOHNS 3N 21 5 47 . 1 6 1.70 9 2 3 1 2 JOHNS 2N 29 9 41 .2 6 1.78 14 2 2 2 4 JOHNS IN 68 4 54 .4 10 2.82 18 2 2 2 2 JOHNS O+OO 64 13 64 . 4 10 2.93 14 3 3 1 2

JOHNS 20E 22 2 61 , l 7 2.94 20 2 2 1 1 JOHNS 21E 26 4 72 . I 7 2.40 23 2 4 1 1 JOHNS 22E 17 3 60 . I 7 2.2s 18 2 2 1 1 JOHNS 23E 19 2 60 .I 7 2.45 17 2 2 1 1 JOHNS 24E 22 6 63 .1 7 2.29 IS 2 3 1 1

JOHNS 2% 17 5 57 .1 6 2.69 14 2 2 2 1 JOHNS 26E 19 3 63 .I 7 2.52 21 3 2 1 1 JOHNS 27E 16 8 52 .1 6 2.34 12 2 2 2 I JOHNS 28E 14 4 60 .I 7 2.32 16 2 2 1 1 JOHNS 29E 17 4 55 .1 7 2.37 18 3 2 1 1

JOHNS 30E 16 4 66 .2. 6 2.60 13 2 2 1 1 JOHNS 31E 19 2 65 .l B 2.61 16 2 4 1 1 JOHNS 32E 13 8 49 .l 7 2.49 13 2 2 2 1 JOHNS 33E 15 3 55 .1 6 2.22 13 2 2 1 1 JOHNS 2 76N 29 6 72 - 1 8 2.69 32 2 2 1 2

JOHNS 2 7SN 16 9 54 .1 7 2.38 25 2 2 1 2 STD C/AU 0.S 56 37 130 7.0 29 3.96 39 16 20 I 4 505

tr SEADRIFT INTERNATIONAL FROJECT

SAHPLE I Cu Pb Zn A9 Co Fe PPH PPH PPH PPH PPH Z

JOHNS 2 74N 20 9 54 .1 6 2.54 JOHNS 2 73N 23 7 eo .2 e 2.64 JOHNS 2 72N 34 7 e2 . i e 2.96 JOHNS 2 71N 26 2 75 .2 7 2.58 JOHNS 2 70N 24 9 63 .l 7 2.16

JOHNS 2 b9N 27 12 73 .1 7 2.46 JOHNS 2 60N 29 5 71 .1 6 2.31 JOHNS 2 6711 21 10 bb . l b 2.50 JOHNS 2 66N 17 6 59 .I 6 2.14 JOHNS 2 65N 22 10 65 , I 6 2.32

JOHNS 2 64N 26 5 77 .l 7 2.36 JOHNS 2 63N 23 12 03 . I 7 2.50 JOHNS 2 62N 17 5 67 .1 7 2.36 JOHNS 2 bQN 17 4 62 . l 5 2.18 JOHNS 2 59N 18 9 65 .l 6 2.20

JOHNS 2 56N ' 17 8 63 . I 4 2.06 JOHNS 2 57N 19 8 65 .1 6 2.11 JOHNS 2 56N 20 b 62 . I 6 2.07 JOHNS 2 55N 25 8 63 .I b 2.31 JOHMS 2 54M 24 b 61 ,2 7 2.25

JOHNS 2 52N 26 e 61, . i s 2.15 JOHNS 2 51N 26 10 60 .2 b 2.23 JOHNS 2 SON 29 8 64 .1 6 1.94 JOHNS 2 49N 25 7 b4 .1 b 2.04 JOHNS 2 48N 26 3 b3 .1 5 2.00

JOHNS 2 47N 24 9 59 . I 5 1.87 JOHNS 2 46N 23 s 52 . i 6 1.82 JOHNS 2 45N 27 b 60 .2 5 2.05 JOHNS 2 44N 27 7 65 .2 5 1.99 JOHNS 2 43N 31 5 76 . I b 2.08

JOHNS 2 43N ( A I 20 9 67 .1 6 2.24 JOHNS 2 421 21 9 51 .1 5 1.09 JOHNS 2 4lN 29 7 64 .2 6 2.02 JOHNS 2 ION 17 2 42 .1 5 1.70 JOHNS 2 39N 17 4 45 .1 5 1.92

JOHNS 2 SEN 23 io 49 .2 5 1.80 STD C/AU 0.5 61 43 131 7.1 2e 3.96

- HED FILE # 86-1204 FAGE 2

As Sb Bi Y Aut PPH PPI! PPH PPH eP8

2 4 3 3 1 1 3 9 2 2 1 1 4 4 2 3 1 1 2 4 2 4 1 3 1 6 2 3 1 2

1 9 2 2 2 1 1 3 2 4 1 1 1 1 2 2 1 1 9 2 3 1 1 9 2 2 1 1

1 1 2 2 1 1 1 2 2 2 1 2 1 0 2 2 2 3 9 2 2 1 1 1 0 2 2 1 1

9 2 3 1 1 13 2 2 1 455 1 0 2 3 1 2 1 1 2 2 2 4 8 2 2 1 1

. 9 2 2 1 5 1 0 2 2 2 2 0 2 2 1 2 7 3 2 1 2 9 2 2 1 2

7 2 2 1 1 9 2 2 1 2 e 2 2 1 1 e 2 4 1 2

1 0 2 2 1 1

1 3 2 3 1 1 1 1 2 2 1 1

8 2 3 1 2 1 1 2 3 1 2

e 2 2 1 3

1 1 2 2 1 1 39 15 22 13 SO0

SEADRIFT INT. PROJECT - HED FILE # 86-1204

SAHPLEI Cu Pb Zn l g Co Fe Is Sb Bi W Aut PPM PPH PPH ppn ppn x ppn ppn ppn ppn J~~~

JOHNS 2 37N 22 5 56 .2 6 1.93 7 2 2 1 2 JOHNS 2 3bN 20 3 59 .1 b 1.93 9 2 2 1 2 JOHNS 2 35N 27 3 67 .2 7 2.04 11 3 2 1 1 JOHNS 2 34N 20 12 56 .2 6 1.99 9 2 2 1 1 JOHNS 2 33N 22 6 57 .2 7 2.02 13 2 3 1 2

JOHNS 2 32N 22 6 46 .2 b 1.97 8 2 2 1 2 JOHNS 2 31N 21 7 50 ,I 6 1.08 6 2 2 1 3 JOHNS 2 30N 21 11 44 .2 6 1.99 9 2 2 1 2 JOHNS 2 29N 32 11 63 - 3 9 2.42 11 2 4 1 2 JOHNS 2 28N 27 7 56 .2 b 2.14 9 2 2 1 2

JOHNS 2 27N 20 7 52 . I 6 2.05 8 2 2 1 8 JOHNS 2 2bN 22 4 54 .2 6 1.90 I 1 2 2 1 3 JOHNS 2 25N 33 9 58 .3 7 1.96 12 2 2 1 4 JOHNS 2 24N 28 8 61 .5 5 1.84 14 2 2 1 2 JOWS 2 23N 23 2 47 .2 5 1.71 10 2 2 2 1

JOHNS 2 92N 15 2 50 .1 6 2.02 10 2 2 1 3 %

JOHNS 2 21N 24 S f 3 .2 5 1.87 11 2 2 1 2 JOHNS 2 20N 35 10 57 .S b 2.01 12 2 2 1 2 JOHNS 2 19N 7 7 40 . l 3 1 . 4 0 4 2 2 1 1 JOHNS 2 18N 35 S 60 ,3 7 2.20 14 2 2 1 1

JOHNS 2 16W 67 9 60 .7 8 1.E4 24 . 2 3 1 1 JOHNS 2 1% 55 8 53 ,4 7 1.80 23 2 2 1 1 JOHNS 2 14N 22 9 48 .l 6 2.27 29 2 2 2 2 JOHNS 2 13N 22 9 S5 .2 b 1.8b 17 2 2 1 2 JOHNS 2 12N 26 8 63 .3 7 2.16 15 3 2 1 2

JOHNS 2 1lN 8 10 33 .5 3 1.26 9 2 2 1 2 JOHNS 2 1OY 27 f 10 .2 5 1.86 14 2 2 1 3 JOHNS 2 9N 34 9 62 .3 b 1.85 15 3 2 1 2 JOHNS 2 ON 18 10 58 .2 4 1.63 7 2 3 1 1 JOHNS 2 7N 17 9 61 .1 5 2.18 12 2 2 1 1

JOHNS 2 6N 20 7 62 .2 7 3.32 29 2 4 1 1 JOMS 2 5N 24 10 58 .2 4 1.55 11 2 4 1 1 JOHNS 2 I N 19 9 70 .2 7 2.54 17 2 3 1 2 JOHNS 2 311 17 12 71 .1 b 2.39 14 2 2 1 1 JOHNS 2 211 17 11 79 .5 6 2.34 29 2 2 1 1

FAGE 3

JOHNS 2 1N 14 11 80 .3 b 2.42 3 2 2 1 1 JOHNS 2 O+OO 7 8 37 .1' 3 1.61 2 2 2 1 1 STD C/M 0.5 50 42 131 7.0 29 3.97 41 15 22 12 500

SEADRIFT INT. PROJECT - HED FILE # 86-1204 FAGE 4

SAMPLE1 Cu Pb In A9 Co Fe As Sb B i N Aut PPH PPH PPH PPH PPM X PPH PPI PPH PPH PPB

JOHNS 3 7N 22 9 61 .1 b 1.87 7 3 5 1 1 JOHNS 3 6N 30 12 103 .1 7 2.38 5 2 2 1 3 JOHNS 3 5N 30 8 106 .2 9 2.50 10 2 3 1 1 JOHNS 3 4N 24 9 78 .2 8 2.63 10 3 2 I 3 JOHNS 3 3N 32 2 104 .2 8 2.65 8 2 2 1 1

4

JOHNS 3 2N 33 9 115 .2 7 2.77 6 2 4 1 1 JOHNS 3 1N 22 2 119 .1 8 2.71 11 2 2 1 1 JOHNS 3 OtOO 27 5 853 .I 8 2.27 9 2 2 1 2 JOHNS 4 11N 10 3 60 .I 4 1.16 7 2 2 1 1 JOHNS 4 ION 11 b 49 .I 5 1.64 13 3 2 3 120

JOHNS 4 9N 9 5 se . I 6 2.15 15 2 2 1 14 JOHNS 4 EN 27 8 68 .I 7 2.07 24 2 2 1 1 JOHNS 4 7N 19 8 58 . l 7 2.07 30 2 5 1 1 JOHNS 4 6N 29 2 70 .2 7 2.47 14 2 b I 1 JOHNS 4 SN 28 10 137 .1 6 2.08 12 2 2 3 S

JOHNS 4 4N 30 13 73 . 3 7 2.44 14 3 2 2 3 JOHNS 4 3w 24 8 61 .2 5 2.24 10 2 2 10 2 JOHNS 4 2N 27 9 83 .I 7 2.31 14 3 2 1 4 JOHNS 4 IN 19 5 52 .1 5 1.95 10 2 3 43 4 JOHNS 4 O+OO 21 3 78 .1 8 2.07 14 2 2 1 1

LANCAR 8W 32 10 52 .1 8 2.50 6 . 2 2 1 1 CANCAR OtOO 25 7 65 , I 8 3.32 11 2 2 1 1 LMCAR 1E 28 4 63 .l b 3.38 9 2 2 1 1 LANCAR 2E 21 4 53 .1 7 4.50 10 2 3 1 1 LANCAR 3E 22 5 55 . i e 3.48 11 2 2 1 2

LANCAR 4E 23 2 50 .1 b 2.41 11 3 2 2 I LANCllR 5E 24 2 60 .I 7 2.59 1 1 2 2 1 1 LANCAR 6E 30 3 58 .1 8 2.72 9 2 2 1 1 LllNCIIR 7E 24 2 60 .l 7 2.77 11 2 3 1 1 LANCAR 9E 25 3 46 .1 6 2.58 7 3 3 1 2

LllNCAR 11E 25 5 47 .2 b 2.47 12 3 2 1 2 LANCAR 19E 30 b S5 .1 7 2.37 19 2 2 1 2 LMCAR 20E 27 2 53 .I b 2.12 13 2 2 1 I LMCAR 21E 36 5 75 .I 9 2.08 23 4 3 1 2 LANCAR 175OE 33 5 60 ,1 7 2.37 33 3 2 1 1

STD ClAU 0.5 57 39 132 7.1 29 3.94 40 15 20 12 510

SEADRIFT INT. PROJECT - HED F ILE # 86-1204

SAHPLEI Cu Pb Zn A9 Co Fe As Sb B i W Aut PPH PPH PPH PPI PPH x PPH PPH PPH PPH h e

-. - -

PET 27N 7 9 45 , I 4 1 . 3 7 5 2 2 1 1 PET 2LW e 4 41 . i 4 1 . 3 9 7 z 2 I i

PET 251 ' 7 15 13 .l 4 1.26 b 2 2 1 1 PET 24w 8 4 3 9 .2 4 1 . 2 4 4 2 3 2 1 PET 2% 9 7 36 .l 3 1 . 2 5 4 2 3 I 2

PET 21N 13 7 40 .2 4 1.51 5 2 3 1 3 PET 22N 9 4 39 . I 4 1 . 2 7 7 2 3 I 1

PET 2OW 9 7 39 .1 4 1 . 1 1 5 2 2 2 1 PET 19N b 5 37 . I 3 1 . 1 1 2 2 2 1 1 PET 18N 9 9 3 8 .1 4 1 . 1 1 4 2 4 1 1 PET 1711 8 b 42 .2 4 1 . 2 1 4 3 3 2 1 PET 1bN 9 7 42 . i 4 1 . 1 6 3 2 4 1 I

PET 1SN 9 14 42 . I 4 1.17 I 2 2 1 1 PET 11N 9 7 43 .1 4 1 . 2 3 3 3 2 1 1 PET 13N 9 b 41 .1 4 1 . 1 6 5 2 2 1 1 PET 12N 9 7 40 .2 4 1.14 4 2 3 1 1 PET 11N 0 b 41 .2 4 1 . 1 0 5 2 4 2 b

PET 10N 9 5 42 .1 3 1 . 1 6 7 2 4 I I PET 9N 10 7 51 .1 4 1.39 6 3 4 1 270 PET ON 10 7 44 .1 3 1.31 5 2 2 1 3 PET 7N 9 2 48 .I 4 1 . 4 4 b 2 2 1 1 PET bN , 9 2 53 .i 4 1.57 a 3 3 i i

PET 5N 12 5 I 0 . I ' 3 1 . 3 4 6 2 3 2 1 6TD C l A U 0.5 57 37 135 1.0 30 3.96 42 IS 22 13 500

SEADRIFT INTERNATIONAL PROJECT - HED FILE # 86-1204 PAGE 6 w SAHPLEt Cu Pb I n A9 CP Fe As Sb B i W Aut

PPI! PPH PPH PPI! PPH X PPH PPH PPH PPH r'PB

PET 3N 12 7 47 .I 4 1.54 9 2 2 3 1 PET 2N 13 3 54 .1 4 1.68 9 2 4 1 1 PET 1N 14 9 53 .1 4 1.67 10 2 2 1 2

PET 2 0 15 8 27 . I 4 1.41 2 2 4 1 1 PET 0 13 5 54 a 1 4 1.75 10 3 2 1 1

PET 2 1E 19 12 28 .I 3 1.24 4 2 2 1 3 PET 2 ZE 14 8 44 .l 4 1.69 2 2 3 4 1 PET 2 4E 15 10 36 .2 6 1.72 3 2 3 3 2 PET 2 5E 15 8 31 - 2 4 1.39 3 2 4 3 1 PET 2 6E 11 3 28 . I 4 1.12 4 2 4 2 1

PET 2 7E 11 3 25 .l 3 1.14 3 2 2 2 1 PET 2 BE 10 7 25 .1 4 1.19 3 2 2 2 2 PET 2 9E 15 6 21 .2 I 1.22 3 2 2 3 1 PET 2 10E 12 5 21 .2 3 1.18 2 2 2 2 1 PET 2 11E 10 5 20 .I 3 1.08 2 2 2 1 1

PET 2 12E' 10 6 17 .1 4 .97 4 2 3 2 1 PET 2 13E 16 13 20 - 2 4 1.13 2 2 2 2 1 PET 2 14E 18 9 19 .1 5 1.61 4 2 2 1 2 PET 2 1SE 20 11 15 - 3 6 1.72 4 2 2 4 1 PET 2 ME 21 17 15 .4 5 1.46 2 2 2 I 1

PET 2 17E 12 11 17 .2 I 1.35 3 3 2 3 2 PET 2 18E 13 12 17 .2 4 1.22 2 2 2 1 1 PET 2 19E 10 3 18 .1 3 1.19 3 2 2 1 1 PET 2 20E 10 - . - 2 22 .l 3 1.24 2 2 2 1 1

STD C/AU-O.S 56 39 130 7.3 28 3.94 39 16 21 14 480

V

assessment on the

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