820444 FORMERL Y: U N I O N M I N I E R E E X P L O R A T I O N S

"~ A A N D M I N I N G C O R P O R A T I O N L I M I T E D

_ . : l : i _ „ i n J i : o q i j / 3 £ Suite 200 - 4299 C a n a d a Way. Burnaby . B.C. V 5 G 1H4 Te l ephone (604) 437-9491 Telex 04-356532

YEAR END REPORT

1981

WHISTLER PROJECT

by

F r e d e r i c k F e l d e r , M.Sc.

J a n u a r y 1982

T A B L E O F C O N T E N T ^ page

SUMMARY 1

LOCATION AND ACCESS . . 2

CONCESSION 2

REGIONAL GEOLOGY 2

DETAILED GEOLOGY 3

GEOCHEMICAL SURVEYS 3 S o i l G e o c h e m i c a l S u r v e y s 3

Rock G e o c h e m i c a l S u r v e y s 3

GEOPHYSICAL SURVEYS 4

DIAMOND DRILLING 4

DISCUSSION OF RESULTS . 5

CONCLUSION 6

A N N E X E S ;

ANNEX I - DRILL HOLE RECORDS

T A B L E S ^

TABLE 1 - C L A M S DATA

TABLE 2 - ROCK SAMPLES FROM THE WHISTLER PROJECT

F I G U R E S f o l l o w i n g page

1. LOCATION OF WHISTLER PROJECT AND CALLAGHAN CREEK ROOF PENDANTS 2

SOUTHWESTERN BRITISH COLUMBIA

2. INDEX MAP SHOWING LOCATION OF WHISTLER PROJECT CLAIMS 2

3. GENERAL GEOLOGY OF PART OF THE CALLAGHAN CREEK ROOF PENDANT 2

4. WHISTLER PROJECT 1981 - GEOLOGY i n p o c k e t

5. WHISTLER PROJECT 1981 - ROCK GEOCHEMICAL SURVEY i n p o c k e t

FIGURES ( c o n t . ) f o l l o w i n g pa=

6. WHISTLER PROJECT 1981 - SOIL GEOCHEMISTRY - COPPER i n po c k e t

7. WHISTLER PROJECT 1981 » SOIL GEOCHEMISTRY - LEAD i n p o c k e t

8. WHISTLER PROJECT 1981 - SOIL GEOCHEMISTRY - ZINC i n p o c k e t

9. WHISTLER PROJECT 1981 - SOIL GEOCHEMISTRY - SILVER i n p o c k e t

10. WHISTLER PROJECT 1981 - COMPOSITE OF SOIL GEOCHEMICAL SURVEYS i n po c k e t FOR Cu, Pb, Zn, Ag

11. WHISTLER PROJECT 1981 - ROCK GEOCHEMICAL SURVEY - COMPOSITE i n p o c k e t ANOMALIES

12. WHISTLER PROJECT 1981 - EM-16 PHASE ( H j e l t F i l t e r e d ) I n p o c k e t

13. WHISTLER PROJECT 1981 - CONDUCTOR C - l , ELECTROMAGNETICS (Ground) .. i n p o c k e t MAX-MIN & CRONE SHOOTBACK

13a. WHISTLER PROJECT 1981 - CONDUCTOR C - l , ELECTROMAGNETICS, MAX-MIN, . i n p o c k e t LINE 50N

14. WHISTLER PROJECT 1981 - MAX-MIN, ELECTROMAGNETICS, LINE 1000N, i n p o c k e t W GRID

15. WHISTLER PROJECT 1981 - MAX-MIN, ELECTROMAGNETICS, LINE 3800N, i n p o c k e t W GRID

16. WHISTLER PROJECT 1981 - COMPOSITE MAP, DIAMOND DRILL HOLE NO. 1 ... i n p o c k e t AREA, W GRID

17. WHISTLER PROJECT 1981 - DIAMOND DRILL HOLE NO. 1 SECTION i n p o c k e t

18. WHISTLER PROJECT 1981 - COMPOSITE MAP, DIAMOND DRILL HOLES 2&3 i n p o c k e t

AREA

19. WHISTLER PROJECT 1981 - DIAMOND DRILL HOLE NO. 2 SECTION i n p o c k e t

20. WHISTLER PROJECT 1981 - DIAMOND DRILL HOLE NO. 3 SECTION i n p o c k e t

SUMMARY

The 1981 W h i s t l e r Program c o m p r i s e d d e t a i l e d g r ound f o l l o w up i n v o l v i n g r o c k s a m p l i n g , EM 16, R e s i s t i v i t y , Max-Min s u r v e y s as w e l l as a d d i t i o n a l s o i l s a m p l i n g . D u r i n g t h e months o f O c t o b e r and November t h r e e t a r g e t s were t e s t e d by diamond d r i l l i n g .

The d r i l l i n g e n c o u n t e r e d p y r i t i z e d r h y o l i t i c h o r i z o n s i n t e r c a l a t e d w i t h b l a c k s h a l e s t h a t l o c a l l y a r e g r a p h i t i c i n two o f t h e h o l e s . The p y r i t i c bands were w e a k l y anomalous i n base m e t a l s . A t h i r d d r i l l h o l e , on t h e n o r t h end o f t h e p r o p e r t y , c u t t h e c o n t a c t zone between i n t r u s i v e d i o r i t e s and b a s i c v o l c a n i c s , w e a k l y anomalous c o p p e r v a l u e s were found i n t h e c o n t a c t zone.

The work c a r r i e d o u t by UMEX on t h e UMEX-SAMIM gro u n d f a i l e d t o g i v e any p o s i t i v e encouragement f o r e i t h e r v e i n o r s t r a t i f o r m m a s s i v e s u l f i d e m i n e r a l i -z a t i o n . No f u r t h e r work i s recommended f o r 1982.

- 2 -

LOCATION AND ACCESS

The W h i s t l e r p r o j e c t i s l o c a t e d w i t h i n the P a c i f i c Ranges o f t h e C o a s t M o u n t a i n s , a p p r o x i m a t e l y 10 k i l o m e t e r s west o f the m u n i c i p a l i t y o f W h i s t l e r and 42 and 90 k i l o m e t e r s n o r t h o f Squamish and Vancouver r e s p e c t i v e l y . The c l a i m s are w i t h i n t h e V a n c o u v e r M i n i n g D i v i s i o n i n N.T.S. 92J/3E w i t h a p p r o x i m a t e l a t i t u d e ar_d l o n g i t u d e c o o r d i n a t e s b e i n g 50°06 TN and 123°08 !W ( F i g u r e 1 ) .

The s o u t h e r n b o u n d a r y o f t h e c l a i m s l i e t h r e e and one h a l f k i l o m e t e r s n o r t h : f Highway 99. D u r i n g 1981 e x t e n s i v e u p g r a d i n g work on the Cheakamus P a s s p o r t i o n c f the Highway was done by Dawson C o n s t r u c t i o n o f V a n c ouver. G r a v e l r o a d s g i v e a c c e s s to c l a i m s on b o t h t h e e a s t and west s i d e o f C a l l a g h a n Creek ( F i g u r e 2 ) .

The r e g i o n has s t r o n g r e l i e f w i t h peaks e x c e e d i n g 2,000 m e t e r s and v a l l e y s h a v i n g an e l e v a t i o n o f a p p r o x i m a t e l y 500 m e t e r s . On t h e W h i s t l e r p r o j e c t a r e a , the l o w e s t p o i n t i s t h e C a l l a g h a n Creek a t a p p r o x i m a t e l y 600 m e t e r s and t h e h i g h e s t p r i n t b e i n g about 1,400 m e t e r s above sea l e v e l .

The B r i t i s h C o l u m b i a R a i l w a y p a s s e s s e v e r a l k i l o m e t e r s s o u t h o f t h e p r o p e r t y . A l s o , h i g h t e n s i o n power l i n e s p a r a l l e l Highway 99. The a d j o i n i n g N o r t h A i r Mines houses i t s p e r s o n n e l a t e i t h e r t h e mine i n t r a i l e r s o r buses them t o Squamish.

CONCESSION

The ground h e l d by t h e UMEX-SAMIM W h i s t l e r j o i n t v e n t u r e program i s g i v e n i n F i g u r e 2. I n T a b l e 1 b e l o w a r e g i v e n the d e t a i l s o f t h e c l a i m s :

Name o f R e c o r d Month o f No. o f E x p i r y C l a i m No. R e c o r d U n i t s Date

Dasher 271 4 12 1983 C u p i d 277 5 5 1983 A n g e l 311 8 8 1983 P r a n c e r 272 4 20 1984 Hans 171 5 10 1983 Pet 172 5 4 1983 Hans 2 721 7 8 1982 Hans 3 722 7 12 1982 Hans 4 723 7 4 1982 Hans 5 801 11 4 1982

A l l o f t h e above c l a i m s w i t h the e x c e p t i o n of Hans 5 have been put i n t o one group (Dasher Group) on t h e 17th o f March 1981. The t o t a l s u r f a c e a r e a c o n t r o l l e d by UMEX on b e h a l f o f t h e j o i n t v e n t u r e i s 1,640 HA.

REGIONAL GEOLOGY

The a r e a i s u n d e r l a i n by t h e C a l l a g h a n C reek r o o f pendent ( F i g u r e 3 ) . T h i s i s one o f the numerous v o l c a n i c - s e d i m e n t a r y r o o f pendents t h a t t r e n d n o r t h w e s t e r l y t h r o u g h o u t t h e C o a s t P l u t o n i c Complex. The v o l c a n i c - s e d i m e n t a r y r o o f pendent i s p o s s i b l y of E a r l y C r e t a c e o u s age, s u g g e s t i n g t h a t t h i s maybe c o e v a l w i t h t h e Gambler Group w i t h w h i c h i t s h a r e s many s i m i l a r i t i e s . A c c o r d i n g t o M i l l e r and S i n c l a i r ^ the

M i l l e r , J.M.L. and S i n c l a i r , A . J . (1978) Geology o f p a r t o f t h e C a l l a g h a n Creek Roof Pendent, i n G e o l o g i c a l F i e l d w o r k 1977, B.C. M i n i s t r y o f M i n e s and P e t r o l e u m R e s o u r c e s pp. 96-102.

3

BRITISH C O L U M B I A

U M E X C O R P O R A T I O N LTD.

F I G U R E N O . 1

L O C A T I O N OF W H I S T L E R P R O J E C " .

A N D C A L L A G H A N C R E E K ROOF P E N D A N T S

S O U T H W E S T E R N B R I T I S H C O L U M B I A

LEGEND

Terliory

(7] Volcanics o) Basalt b] Acidic Tuff c] Rhyolite

Cretaceous (or earlier) [6] Coast Plutonic Complex

.[5] Agglomerate a) Volcanic Breccia [4j Acidic Volcanic Rocks H Crystal Tuff K j Aaglomeratt ('j Greenstone

Conlacf (opproxEfnate, assumed)

Fault (opprciimate.ossumed)

A Mine Adit

O Mi.neral Occurrence

Limit of Mopping

Figure No. 3

WHISTLER PROJECT 1931 Genera ! Geo logy of Fart

( i f 4 t\j» Colloghan Creek Roof Pend ant

Scale:

U M E X C O R P O R A T I O N 4 L T D . Drown by: H.Holm Det«: Msy , 1981

êypd by;Mfiler, Sincbi 3 DWG. No. •MHIHIHW HI"ii" ii'ini

- 3 -

C o a s t P l u t o n i c complex i n t r u s i v e s range i n c o m p o s i t i o n f r o m q u a r t z d i o r i t e t o q u a r t z m o n z o n i t e . A w e s t e r n zone o f i n t r u s i o n s i s p r e d o m i n a n t l y C r e t a c e o u s , whereas an e a s t e r n zone i s e a r l y T e r t i a r y .

DETAILED GEOLOGY

I n 1980 t h e c l a i m a r e a was mapped on a 1:10,000 s c a l e , and i n 1981 the v o l c a n i c s e d i m e n t a r y p a c k a g e on t h e w e s t e r n h a l f o f t h e c l a i m s was p r o s p e c t e d c a r e f u l l y ( F i g u r e s 4 and 5 ) .

C o n s i d e r i n g t h e r e l a t i v e abundance o f o u t c r o p p i n g on most o f t h e p r o p e r t y , emphasis was p l a c e d on e x a m i n i n g t h e a r e a s o f known s o i l g e o c h e m i c a l a n o m a l i e s , as w e l l as c o n d u c t o r s .

Some o f t h e l o n g e r c o n d u c t o r s were f o u n d t o be u n d e r l a i n by a h o r i z o n c o n t a i n i n g p y r i t i f e r o u s s e r i c i t e s c h i s t . T h i s s c h i s t h o r i z o n c a n be t r a c e d f o r s e v e r a l hundred m e t e r s , and was f o u n d t o c o n t a i n q u a r t z eyes i n some p l a c e s . C l o s e t o , and s p a t i a l l y above, t h e p y r i t i c s c h i s t h o r i z o n t h e r e o c c u r r e d a b l a c k s h a l e band, w h i c h i n p l a c e s was q u i t e g r a p h i t i c . S m a l l l e n s e s o f l i m e s t o n e a l s o o c c u r r e d w i t h i n the s h a l e . These a c i d - v o l c a n i c and p r e d o m i n a n t l y c l a s t i c s e d i m e n t a r y h o r i z o n s were l e s s t han one hun-d r e d m e t e r s t h i c k , and were bound by more b a s i c v o l c a n i c u n i t s p r o b a b l y o f d a c i t i c t o a n d e s i t i c c o m p o s i t i o n on b o t h s i d e s . I n p l a c e s t h e b a s i c v o l c a n i c r o c k s were s t r o n g l y s i l i c i f i e d g i v i n g r i s e t o much l i g h t e r c o l o u r e d r o c k s . Where s i l i c i f i c a t i o n was v e r y i n t e n s e t h e s e w o u l d r e s e m b l e r h y o l i t e s . The p r e s e n c e o f t h e s e " r h y o l i t i z e d a n d e s i t e s 1 1 , adds t o t h e d i f f i c u l t y o f mapping i n t h i s a r e a . The few whole r o c k a n a l y s e s p e r f o r m e d on some o f the a c i d l o o k i n g r o c k s as w e l l as t h i n s e c t i o n examina-t i o n seem t o c o n f i r m t h a t a t l e a s t some o f them a r e h i g h l y s i l i c i f i e d and c a l c i f i e d r o c k s whose o r i g i n a l c o m p o s i t i o n i t i s no l o n g e r p o s s i b l e t o a s c e r t a i n .

GEOCHEMICAL SURVEYS S o i l G e o c h e m i c a l S u r v e y s

I n 1981 a d d i t i o n a l s o i l g e o c h e m i c a l s u r v e y s were c a r r i e d o u t i n the a r e a s where the s a m p l i n g d e n s i t i e s o f p r e v i o u s s u r v e y s was i n s u f f i c i e n t , o r i n a r e a s where no p r e v i o u s s a m p l i n g had been done. F i g u r e s 6-9 c o n t a i n t h e r e s u l t s o f a l l the geo-c h e m i c a l s u r v e y s i n c l u d i n g t h e 1981 d a t a . F i g u r e 10 i s a c o m p o s i t e d i a g r a m showing the anomalous m e t a l c o n t e n t s o f the w e s t e r n p a r t o f t h e c l a i m a r e a on a 1:5,000 s c a l e A t o t a l o f 152 s o i l samples were c o l l e c t e d i n 1981.

Rock G e o c h e m i c a l S u r v e y s

I n o r d e r t o g i v e a b e t t e r d e f i n i t i o n o f the f o l l o w up t a r g e t s a r o c k s a m p l i n g program was done o v e r t h e w e s t e r n p o r t i o n o f t h a t c l a i m a r e a . N i n e t y f i v e r o c k samples were c o l l e c t e d . The g r e a t e s t d e n s i t y o f r o c k s a m p l i n g was c o n c e n t r a t e d on the a r e a u n d e r l a i n by t h e f a i r l y c o n t i n u o u s m u l t i - e l e m e n t s o i l g e o c h e m i c a l a n o m a l i e s and c o i n c i d e n t VLF-Em c o n d u c t o r s . The m a j o r i t y o f t h e s e r o c k s were a n a l y z e d f o r t h e i r Cu, Pb, Zn, Ag and Au c o n t e n t s , w i t h some o f t h e r o c k s a l s o b e i n g a n a l y z e d f o r t h e i r Hg and Ba c o n t e n t s ( F i g u r e 5 ) . Samples t a k e n on t h e w e a k l y m i n e r a l i z e d s h o v i n g had anomalous v a l u e s i n a l l o f t h e s e e l e m e n t s . A l s o i n a r e a s o f weak m i n e r a l i z a t i o n , weak mer c u r y a n o m a l i e s were found t o o c c u r (up t o 1,460 p p b ) . The b a r i u m v a l u e s were q u i t e low, i n d i c a t i n g t h a t t h e m i n e r a l i z a t i o n o c c u r r i n g i n t h i s a r e a i s n o t b a r i t i c , a l s o no c o r r e l a t i o n was f o u n d t o e x i s t between t h e b a r i u m and t h e base m e t a l c o n t e n t s .

There i s a f a i r l y good o v e r a l l c o r r e l a t i o n between t h e d i s t r i b u t i o n o f the s o i l and r o c k g e o c h e m i c a l a n o m a l i e s . The i n t e n s i t i e s o f t h e m u l t i e lement a n o m a l i e s i n

- 4 -

the r o c k s were o f t h e same o r d e r o f magnitude as were f o u n d i n t h e s o i l s ( F i g u r e 11).

The r e s u l t s o f t h e r o c k sample s u r v e y a r e g i v e n i n T a b l e 2.

GEOPHYSICAL SURVEYS

The a i r b o r n e s u r v e y done i n 1980 i n d i c a t e d t h e p r e s e n c e o f e i g h t VLF-EM c o n d u c t o r s . The f o l l o w up o f t h e s e c o n d u c t o r s was done t o a l a r g e degree i n t h e f a l l o f 1980 (See Y e a r End R e p o r t f o r 1980).

I n 1981 t h e ground VLF-EM 16 s u r v e y was e x t e n d e d o v e r t h e w e s t e r n h a l f o f the c l a i m group u n d e r l a i n by t h e a l t e r n a t i n g a c i d and b a s i c v o l c a n o c l a s t i c and s e d i -mentary r o c k s . T h i s was a l s o t h e a r e a o f t h e most abundant s o i l g e o c h e m i c a l a n o m a l i e s . A t o t a l o f 17.29 k i l o m e t e r s o f l i n e s were s u r v e y e d u s i n g a G e o n i c s EM 16 u n i t ; a t o t a l o f 1700 r e a d i n g s were t a k e n . The r e s u l t s o f t h i s s u r v e y g i v e n i n F i g u r e 12, i n d i c a t e t h a t t h e m a j o r i t y o f t h e c o n d u c t o r s f e l l a l o n g f a i r l y c o n -t i n u o u s c o n d u c t i v e t r e n d s . One can d e c i p h e r a p p r o x i m a t e l y one dozen such c o n -d u c t i v e t r e n d s h a v i n g l e n g t h s e x c e e d i n g 300 m e t e r s (1000 f e e t ) , w i t h a few o f the c o n d u c t o r s b e i n g t r a c e a b l e o v e r a d i s t a n c e o f o v e r two k i l o m e t e r s . Some o f t h e s h o r t e r c o n d u c t o r s i n d i c a t e d may a c t u a l l y be p a r t o f l o n g e r s t r u c t u r e s , b u t f o r l a c k o f i n f o r m a t i o n c a n n o t be t i e d t o g e t h e r . On t h e f i l t e r e d d a t a ( H j e l t f i l t e r ) t h e s e c o n d u c t i v e zones had i n t e n s i t i e s t h a t v a r i e d f r o m 5% t o o v e r 50%, t h e r e b y i n d i c a t i n g t h a t o v e r a l l t h e s e were f a i r l y poor c o n d u c t o r s w i t h a v e r y h i g h v a r i a t i o n o f con-d u c t i v i t y .

I n a d d i t i o n t o t h e ground VLF-EM s u r v e y a l i m i t e d amount o f MAX-MIN s u r v e y s were done on s p e c i f i c p o r t i o n s o f t he VLF c o n d u c t o r s as w e l l as on one o f t h e a i r b o r n e c o n d u c t o r s . A t o t a l o f 1,425 m e t e r s o f MAX-MIN s u r v e y s u s i n g an APEX MAX-MIN I I was c a r r i e d o u t u s i n g 3 f r e q u e n c i e s (222 Hz, 888 Hz and 3555 H z ) .

On a i r b o r n e c o n d u c t o r C - l a d d i t i o n a l MAX-MIN s u r v e y s u s i n g 200 meter c a b l e s e p a r a t i o n was done i n 1981 ( F i g u r e s 13 and 13A). Mr. McKantz o f SAMIM examined t h e MAX-MIN d a t a i n c o n j u n c t i o n w i t h t h e SHOOT BACK r e s u l t s and c o n c l u d e d t h a t t h i s c o n d u c t o r was e i t h e r a n a r r o w s h e a r o r c l a y zone, o r p o t e n t i a l l y o v e r b u r d e n s o u r c e . The d a t a s u g g e s t s t h a t the c o n d u c t o r was s h a l l o w , and s i n c e t h e c o n d u c t o r o c c u r s i n a g r a v e l l y l o w l y i n g a r e a , i t was a s s i g n e d a low p r i o r i t y f o r f o l l o w up.

On t h e l o n g c o n d u c t o r t h a t c o i n c i d e s w i t h t h e showing on the r o a d as w e l l as th e s o i l and r o c k g e o c h e m i c a l a n o m a l i e s , one t e s t l i n e was r u n w i t h t h e MAX-MIN to see i f t h e VLF-EM 16 c o n d u c t o r s can be p i c k e d up. The MAX-MIN s u r v e y was done w i t h 50 m e t e r s s p r e a d on t h r e e f r e q u e n c i e s . O n l y a v e r y weak (

- 5 -

e i t h e r a Hughes 500D o r a B e l l 206 J e t r a n g e r on c a s u a l c h a r t e r from e i t h e r Pemberton o r Okanagan H e l i c o p t e r s r e s p e c t i v e l y . The d r i l l i n g commenced on t h e 22nd o f O c t o b e r , and was t e r m i n a t e d on t h e 2 4 t h o f November.

Between s e c t i o n s 3800 & 3900N, d r i l l h o l e DDH-W-1 was d r i l l e d on t h e P r a n c e r c l a i m ( F i g u r e 16) on a c o i n c i d e n t s o i l g e o c h e m i c a l anomaly and a r e l a t i v e l y s h o r t and weak VLF c o n d u c t o r . MAX-MIN s u r v e y s on t h e c o n d u c t o r d i d n o t g i v e any r e s p o n s e on t h e two c a b l e s e p a r a t i o n s used (50 & 100 m t s ) . The s o i l g e o c h e m i c a l anomaly c o n t a i n e d v a l u e s o f up t o 1700 ppm Cu and 2700 ppm Zn. The c o n d u c t o r was weak w i t h f i l t e r e d v a l u e s o f +14.6%. The d r i l l h o l e e n c o u n t e r e d d i o r i t e from 0 t o 20.12 mts. From 20.12 t o 72.24 mts a n d e s i t i c t o r h y o l i t i c t u f f s , s i l i c i f i e d b a s i c v o l c a n i c s , as w e l l as s i l i c i f i e d t u f f s were e n c o u n t e r e d ( F i g u r e 1 7 ) . M i n o r d i s s e m i n a t e d p y r i t e was e n c o u n t e r e d i n t h e h o l e . A d e t a i l e d d e s c r i p t i o n o f t h e c o r e i s f o u n d i n Annex 1.

Weakly anomalous c o p p e r and z i n c v a l u e s were f o u n d w i t h i n t h e d i o r i t e and the v o l c a n i c r o c k s . I t i s p o s s i b l e t h a t t h e VLF-EM c o n d u c t o r was caused by t h e c o n t a c t between t h e d i o r i t e and t h e v o l c a n i c and v o l c a n o c l a s t i c r o c k s . The weak m i n e r a l i -z a t i o n may have been s u f f i c i e n t t o e x p l a i n t h e s o i l g e o c h e m i c a l a n o m a l i e s .

D r i l l h o l e DDH-W-2 was d r i l l e d n e a r s e c t i o n 900N on t h e Dasher c l a i m ( F i g u r e 1 8 ) . The d r i l l h o l e was p o s i t i o n e d t o t e s t c o i n c i d e n t s o i l , r o c k and a VLF-EM c o n d u c t o r . The s o i l g e o c h e m i c a l anomaly c o n t a i n e d up t o 240 ppm Cu, 740 ppm Zn and 181 ppm Pb. A l s o a c o i n c i d e n t r o c k g e o c h e m i c a l t r e n d i s f o u n d . The VLF-EM c o n d u c t o r s were found t o be r e l a t i v e l y s t r o n g , w i t h v a l u e s o f up t o +65.5% b e i n g r e c o r d e d . C o i n c i d i n g w i t h t h e EM-16 c o n d u c t o r s t h e r e a r e marked r e s i s t i v i t y l o w s .

D r i l l h o l e DDH-W-2 i n t e r s e c t e d a n d e s i t i c and g r e e n c h l o r i t i c s c h i s t f r o m 0 t o 34.14 m e t e r s ( F i g u r e 19). T h i s was f o l l o w e d by a s e r i e s o f a l t e r n a t i n g b l a c k s h a l e and r h y o l i t i c a s h f l o w s . A t i n c r e a s i n g d e p t h t h e r e was a marked i n c r e a s e o f s e r i c i t e s c h i s t . A t h i n band o f b r e c c i a t e d r h y o l i t e was e n c o u n t e r e d from 48.92 t o 49.22 m e t e r s . D i s s e m i n a t e d p y r i t e and p y r i t e v e i n l e t s o c c u r r e d t h r o u g h o u t most o f t h e h o l e . The d r i l l l o g s a r e a t t a c h e d i n t h e Annex o f t h i s r e p o r t .

D r i l l h o l e DDH-W-3 was d r i l l e d t o t e s t t h e same h o r i z o n as was i n t e r s e c t e d by d r i l l h o l e DDH-W-2, o n l y 170 m e t e r s t o t h e s o u t h ( F i g u r e 18). A l s o d r i l l h o l e DDH-W-3 i n t e r s e c t e d t h e h o r i z o n o f i n t e r e s t 35 m e t e r s s o u t h o f the r o a d s howing.

To t h e d e p t h o f 41.15 m e t e r s h o l e DDH-W-3 i n t e r s e c t e d p r e d o m i n a n t l y a n d e s i t e f l o w s and t u f f s . From 41.15 t o t h e end o f t h e h o l e , t h e r e o c c u r r e d a s u c c e s s i o n o f s h a l e s and r h y o l i t e s , w i t h t h e r e l a t i v e p r o p o r t i o n o f t h e fo r m e r i n c r e a s i n g w i t h d e p t h . From 66.45 t o 67.36 met e r s t h e r e o c c u r r e d c o n t o r t e d s i l i c i f i e d r h y o l i t e w i t h p y r i t e o f a p p r o x i m a t e l y 5% o v e r t h e w i d t h o f t h e i n t e r s e c t i o n ( F i g u r e 2 0 ) . A n a l y s e s o f t h i s i n t e r s e c t i o n gave 147 ppm Cu, 141 ppm Zn and 1.3 ppm Ag. S i m i l a r l y w e a k l y anomalous c o n c e n t r a t i o n s o f base m e t a l s were e n c o u n t e r e d i n a number o f p l a c e s w i t h i n t h e d r i l l h o l e b o t h w i t h s h a l e and r h y o l i t e .

DISCUSSION OF RESULTS

The 1981 diamond d r i l l program t e s t e d t h r e e o f t h e g e o c h e m i c a l - g e o p h y s i c a l -g e o l o g i c a l t a r g e t s on t h e W h i s t l e r p r o j e c t .

The r e l a t i v e weakness o f t h e anomalous r e s p o n s e s made i t more d i f f i c u l t t o d e c i d e t h e l o c a t i o n o f t h e diamond d r i l l h o l e s . The t a r g e t s had c o i n c i d e n t s o i l and r o c k g e o c h e m i c a l r e s p o n s e s t o g e t h e r w i t h t h e p r e s e n c e o f weak t o s t r o n g VLF-EM

6

- 6 -

c o n d u c t o r s . The MAX-MIN s u r v e y s f a i l e d t o g i v e a r e s p o n s e on t h e s t r o n g e r o f t h e s e c o n d u c t o r s s u g g e s t i n g t h a t t h e VLF-EM c o n d u c t o r s were p r o b a b l y weak ones.

The f i r s t d r i l l h o l e w h i c h was d r i l l e d on a m o d e r a t e l y good s o i l g e o c h e m i c a l anomaly, w i t h a c o i n c i d e n t weak VLF-EM c o n d u c t o r i n t e r s e c t e d a c o n t a c t zone between a d i o r i t e and a n d e s i t e . The c o n t a c t c o u l d p o s s i b l y e x p l a i n t h e weak c o n d u c t o r . Weakly anomalous b a s e m e t a l c o n c e n t r a t i o n s o c c u r r e d , p o s s i b l y r e l a t e d t o some m e t a l r e m o b i l i z a t i o n r e l a t i n g t o t h e d i o r i t e i n t r u s i o n , may have been s u f f i c i e n t t o e x p l a i n t h e s o i l g e o c h e m i c a l anomaly.

D r i l l h o l e s 2 and 3 were p r o b a b l y d r i l l e d on t h e same s t r u c t u r e a t two d i f f e r e n t l o c a t i o n s . A sequence o f a l t e r n a t i n g s h a l e s and r h y o l i t e and r h y o l i t e t u f f s c o i n -c i d e d w i t h t h e zone o f c o n d u c t i v i t y and s o i l g e o c h e m i c a l a n o m a l i e s . The r h y o l i t e and r h y o l i t e t u f f s c o n t a i n e d from s e v e r a l t o o v e r f i v e p e r c e n t p y r i t e . The b l a c k s h a l e a l s o c o n t a i n e d p y r i t e v e i n l e t s as w e l l as d i s s e m i n a t i o n s o f p y r i t e . Weakly anomalous b a s e m e t a l v a l u e s were found t o o c c u r w i t h b o t h t h e s e r o c k t y p e s , e x p l a i n i n g t h e s o i l g e o c h e m i c a l anomaly. The VLF c o n d u c t o r s were p r o b a b l y caused by t h e b l a c k s h a l e w h i c h i n p l a c e s was g r a p h i t i c , as w e l l as t h e p y r i t e r i c h s e d i m e n t s o r v o l c a n i c s .

The s h e a r zone f o u n d on the e a s t e r n boundary o f t h e c l a i m s , o c c u r s w i t h i n a g g l o m e r a t e . A l t h o u g h t h i s s h e a r zone i s w i t h i n t h e f a v o r a b l e a g g l o m e r a t e , t h e poor g e o c h e m i c a l s o i l and r o c k r e s p o n s e s o b t a i n e d f r o m i t have d i s c o u r a g e d us froze t e s t i n g i t by diamond d r i l l i n g .

CONCLUSION

The 1981 e x p l o r a t i o n program on t h e W h i s t l e r p r o j e c t had f o r i t s o b j e c t i v e the e x p l o r i n g f o r b a s e and p r e c i o u s m e t a l m i n e r a l i z a t i o n o f v o l c a n o g e n e t i c a f f i n i t y . I t was f u r t h e r m o r e c o n s i d e r e d t h a t o n l y n e a r s u r f a c e t a r g e t s s h o u l d be e x p l o r e d f o r .

The g e o l o g i c a l and d r i l l i n g r e s u l t s i n d i c a t e d t h a t t h e v o l c a n o g e n i c base m e t a l e v e n t s t h a t o c c u r r e d on t h i s p r o p e r t y were o f a v e r y weak n a t u r e , n o t g i v i n g r i s e t o any h o r i z o n s o f i n t e n s e s u l f i d e d e p o s i t i o n . The e v i d e n c e f o r p r e c i o u s m e t a l v e i n development i s v e r y s p a r s e . On the e a s t e r n edge a n a r r o w s h e a r zone has been t r a c e d f o r a d i s t a n c e o f 800 m e t e r s . On s t r i k e w i t h t h i s s h e a r a weak VLF c o n d u c t o r o c c u r s , a l s o a v e r y weak MAX-MIN c o n d u c t o r i s found a t t h i s l o c a l e . The s o i l g e o c h e m i c a l r e s p o n s e on t h i s v e i n i s v e r y weak.

The f i e l d work c a r r i e d o u t on t h e W h i s t l e r p r o j e c t has n o t r e s u l t e d i n any e v i d e n c e o f economic m i n e r a l i z a t i o n . Some weak m a n i f e s t a t i o n s o f v o l c a n o g e n e t i c m i n e r a l i z a t i o n as w e l l as v e i n i n g o c c u r s , however d r i l l i n g o f a few o f t h e t a r g e t s has shown t h a t t h e m i n e r a l i z i n g e v e n t s gave r i s e t o o n l y uneconomic m e t a l c o n c e n -t r a t i o n s .

No a t t e m p t has been made t o t e s t t h e a r e a f o r d e e p e r t a r g e t s , and t h e r e f o r e p o s s i b i l i t i e s f o r m i n e r a l i z a t i o n a t d e p t h s t i l l e x i s t .

W i t h i n t h e framework o f t h e o b j e c t i v e s s e t o u t f o r t h e W h i s t l e r Program by the J o i n t V e n t u r e p a r t n e r s , we do n o t recommend any f u r t h e r work on the p r o p e r t y .

TABLE 2 _ t

ROCK SAMPLES FROM THE WHISTLER PROJECT

Sample Sample Cu Pb Zn Ag Au Hg Ba No. Loc a t i o n ppm ppm ppm ppm ppjn ppm

30201 W925N-120E 32 80 105 0.4 .005 15 30202 W925N+120E 85 95 120 0.3 .005 30 30203 W925N+120E 45 30 50 0.4 .005 10 30204 W925N+120E 130 50 120 0.3 .005 270 30205 W925N+120E 230 32 115 0.3 .005 180 30206 WBL+2600N 32 18 60 0.1 .005 20 30207 50m S of WBL+2750N 60 21 75 0.1 .005 140 30208 5m SW of 3800N+900E 39 25 40 0.1 .005 70 30209 X1000N+500W 60 26 55 0.1 .005 1300 30210 On road up to X2200N 15 19 17 0.1 .005 80 013171 BL+235N 330 7 160 0.2 .005 .010 013172 BL+240N 43 4 60 0.1 .010 .040 013173 BL+230N 165 6 148 0.2 .010 .010 013174 67 6 145 0.2 .020 .010 013175 18 2 42 0.1 .005 .010 013176 78 24 82 0.2 .015 .010 013177 58 38 205 0.4 .010 .010 013178 W1800N+50E 76 2 145 0.4 .005 .020 013179 W1070N+170W 13 10 70 0. 1 .005 .010 013180 W300N+50W 15 2 64 0.1 .005 .005 013181 W300N+190E 9 3 60 0.1 .005 .010 013182 W2350N+100W 20 5 42 0.5 .020 .005 013183 W1000W+150E 52 8 100 0.4 .010 .010 013184 W2400N+70W 10 3 43 0.1 .005 .005 013185 W2400N+71W 67 4 60 0.1 .005 .010 013186 W2800N+80W 1 2 6 0.1 .005 .010 013187 W2800N+80W 5 2 100 0.1 .005 .005 013188 W2800N+145W 250 4 130 0.4 .005 .015 013189 W330N+950E 1 2 14 0. 1 .005 .005 013190 X1050N+500W 17 8 375 0. 1 .005 .080 013151 W3700N+1160W 45 4 65 0.1 .005 013152 15m SW of 9N+4.5W 70 6 118 0.5 .005 013153 W3200N+1290W 290 3 60 0.7 .005 013154 W3400N+790W 14 2 54 0.1 .005 013155 W3300N+775W 56 3 40 0.1 .005 013156 W1600N+280W 61 11 118 0.2 .005 013157 W3000N+825W 41 3 60 0.1 .005 013158 W3840N+875W 290 6 118 0.5 .005 013159 X1400N+800W 118 5 110 0.2 .005 013160 X1400N+780W 22 6 80 0.1 .005 013161 X1400N+760W 69 7 105 0.3 .005 013162 X1310N+700W 25 6 102 0.1 .005 013163 W1410N+500W 3 5 90 0.1 .005 013164 W1000N+130E 58 8 39 0.5 .025 013165 W3700N+800W 73 5 34 0.3 .005 013166 W3125N+270W 54 6 128 0.2 .005 013167 W3125N+350W 42 6 118 0.1 .005 013168 W1200N+120W 146 8 92 0.5 .015

TABLE 2 ( c o n t . )

Sample Sample Cu Pb Zn Ag Au Hg Ba No. Location ppm £pjm £P_m ppm ppm ppm

013169 W1800N+100W 29 7 82 0.2 .005 013170 W2200N+50W 78 6 80 0.2 .005 013191 WBL+200N 16 8 142 0.1 .010 .005 130 013192 WBL+200N 220 45 172 0.4 .015 .005 710 013193 WHX2300N+1328W 62 10 51 0.1 .005 .005 100 013194 W2600N+160W 20 4 70 0.1 .005 .005 90 013195 W2600N+170W 2 2 5 0.1 .005 .005 10 013196 W2600N+200W 74 6 100 0.1 .005 .010 130 013197 W2480N+150W 44 6 120 0.1 .005 .010 390 013198 W2000N+100W 20 2 72 0.1 .005 .010 90 013199 W2000N+70W 54 6 83 0.1 .005 .010 830 013200 W1950N+40W 42 11 116 0.1 .005 .010 1600 030901 W1830N+15W 2 2 23 0.1 .005 .010 810 030902 W1740N+25W 68 4 50 0.2 .005 .010 70 030903 W3400N+290W 10 24 120 0.1 .010 .040 30 030904 W550W+4010N 46 9 98 0.1 .005 .020 170 030905 W4000N+620W 290 6 95 0.1 .005 .010 90 030906 W3885N+915W 30 6 57 0.1 .005 .015 10 030907 W3800N+975W 16 5 62 0.1 .005 .005 10 030908 W3850N+915W 14 5 69 0.1 .005 .010 20 030909 W3855N+910W 2 4 90 0. 1 .005 .010 50 030910 W3100N+245W 34 3 39 0.1 .005 .005 840 030911 W3100N+120W 140 6 72 0.1 .005 .010 70 030912 W2900N+100W 42 5 78 0.1 .005 .010 80 030913 W2900N+50W 54 3 61 0.1 .005 .005 50 030914 W2900N+125W 110 5 60 0.1 .005 .015 60 030915 WBL+2900N 2 2 16 0.1 .005 .010 110 030916 W2900N+75E 6 3 42 0.1 .005 .005 60 030917 WBL+2825E 63 4 54 0.1 .005 .010 130 030918 X2550N+1470W 40 6 35 0.1 .005 .005 70 W81T1 Main conductive zone 5 7 54 W81T2 Main conductive zone 23 13 64 W81T3 Main conductive zone 27 9 80 W81T4 Main conductive zone 11 15 52 W81T5 Main conductive zone 36 11 78 W81T6 Main conductive zone 17 10 108 W81T7 Main conductive zone 13 14 44 W81T8 Main conductive zone 410 415 4750 W81T9 Main conductive zone 58 31 144 W81T10 Main conductive zone 4 15 230 W81T12 Main conductive zone 50 6 98 W81T13 Main conductive zone 35 8 84

A N N E X I

P R n . l F P T : ' S t l e r UMEX Inc. Described by: • Cheval ier Property: 3asher DRILL HOLE RECORD Page ] of 2 Drill Hnifi No DDH #1 Beorina = n 6 o ° e Drilled by; D r i l c o r

Location W Grid 3860N + 910W Dip = -50° Machine: Hydracore 28 Date Started: Oct. 22, 198l

1 Depth= 72.24 meters Core Size: BQ Date Finished: Oct. 25. 1981 1

Depth % Core Description & Lithology

Depth i

Sample No.

Assay Results

From To

% Core Description & Lithology

From To

i

Sample No. Mo Cu

ppm Pb ppm

Zn ppm

Ag ppm

Au ppm

0 4 .57 0 Overburden. 15.85 17-37 30261 3 62 7 224 .3 .005 4.57 7 .62 95 D io r i t e which contains vest iges of ep idot ized bas ic 20.88 22.71 30262 4 576 2 70 .6 .005

vo1 can i c s . — „ 27.43 28.04 30258 3 37 8 66 .4 .005

7.62 10.67 95 D i o r i t e with f ine grained ep idot ized zones. d i s s . Py 36.27 37.80 30260 1 2 7 38 .1 .005 10.67 15 .24 95 Same as above. d i s s . Py 48.46 51.21 30264 3 87 5 299 .3 .005 15.24 17 .98 100 Basic vo l can ics with epidote and c a l c i t e veins and d i s s . Py £

48.46 51.21 30264 3 87 5 299 .3 .005 15.24 17 .98 100 Basic vo l can ics with epidote and c a l c i t e veins and d i s s . Py £

^ . 4 7 S6.69 30263 2 206 6 300 .3 .005 1 elements of d i o r i t e . ve i ns. ^ . 4 7 S6.69 30263 2 206 6 300 .3 .005 elements of d i o r i t e . ve i ns.

63.09 63.70 30259 1 11 5 44 .1 .005 17.98 20 11 S i l i c i f i e d d i o r i t i c brecc ia with narrow beds of Py veins 63.09 63.70 30259 1 11 5 44 .1 .005 17.98 20 S i l i c i f i e d d i o r i t i c brecc ia with narrow beds of Py veins 66.14 69.19 30257 1 10 ' 3 50 . 1 .005 ep ido t ized bas ic vo l c an i c s . 66.14 69.19 30257 1 10 ' 3 50 . 1 .005

1 ep ido t ized bas ic vo l c an i c s .

70-71 72.24 30256 1 10 3 57 . 1 .00^ 20. 12 22 .56 95 S i l i c i f i e d bas ic vo l c an i c s . 70-71 72.24 30256 1 10 3 57 . 1 .00^

22.56 29 87 95 Basic vo lcan ic dykes. mag

29.87 32 61 95 intensely s i l i c i f i e d bas ic vo l c an i c s . d i s s . Py 32.61 35 66 95 Same as above. d i s s . Py

35.66 38.71 95 Same as above. d i s s . Py 38.71 41 • 76 95 Same as above. d i s s . Py 41 .76 44 .81 95 Same as above. d i s s . Py 44.81 46 • 33 95 Same as above. d i s s . Py 46.33 48 • 77 95 S i l i c i f i e d tu f f s ( andes i t i c to rhyo1 i t i c ) . d i s s . Py ^8.77 52 .43 95 Epidote, c a l c i t e veins in bas ic v o l c a n i c s . d i s s . Py ^8.77 52 .43 95 Epidote, c a l c i t e veins in bas ic v o l c a n i c s . d i s s . Py 52.43 55 47 95 Same as above. d i s s . Py 52.43 55 47 95 Same as above. d i s s . Py 55.47 58 52 95 Same as above. d i s s . Py 55.47 58 52 95 Same as above. d i s s . Py 58.52 60 66 95 Same as above. d i ss ^ Py 60.66 63-09 95 S i l i c i f i e d basic vo l can i c s . 63-09 66.14 95 Intensely s i l i c i f i e d basic vo l c an i c s . d i s s . Py i { T T !

I

PROJECT^ Whist ler UMEX iHC. Described by= A. Cheval ier Pmnertv: Dasher DRILL HOLE RECORD Page J__ of 2

Driii Hole No. DDH //1

Page J__ of 2

Depth % Core Description ft Lithology Mineralization Sample

No.

Assay Results

From To

% Core Description ft Lithology Mineralization Sample

No.

66.1 k 6 9 . 1 9 95 Same as above. d i s s , py

6 9 . 1 9 71 -63 95 Same as above. d i s s , py

71 -63 7 2 . 2k 95 T u f f s , s i l i c i f i e d , p y r i t i c , poss i bly andes i t i c to py veins

dac i t i c in o r i g i n .

.. . .

1 •

!

~~——

•—

• ;

PROJECT' * n i s t l e r UMEX InC. Described by: A - Cheva l ie r 1 Property: p a s h e r DRILL HOLE RECORD P a g e l _ o f _ L .

Drill Hole No. D D H n Beorlnq = n 6 q ° e Drilled by: D r i l c o r

LocGtioniW Grid 91 ON + 100E Dip = -60° Machine: hydracore 28 Dote Storied: Nov. 6, 1981 Depth = 73-76 meters Core Size = BQ- Dote F in i shed^ o v • ] 5, 1981

Depth % Core Description & Lithology Minerolizotioo

Depth Sample

No.

Assay Results

From To

% Core Description & Lithology Minerolizotioo

From

8.53

To Sample

No. Mo ppm

Cu PPm

Pb ppm

Zn ppm

Ag ppm

Au ppm

0 5. 79 Overburden.

From

8.53 9-25 j 31134 2 54 7 106 .2 .001

, 5.79 9. 75 70 Green c h l o r i t i c s ch i s t with c a l c i t i c and quartz veins • cpy & py 10.97 11 .58 31135 3 82 8 81 .2 .00:

9.75 12. 30 95 Same as above. py v e i n l e t ! 17.37 18.29 i

31133 2 77 5 79 .2 .00: 12.80 15. 35

— 100 Same as above but less ve in ing . " 35.05 35.36 31129 1 1 119 6 100 .4 .00:

15.85 18. 90 95 Same as above but h ighly s i l i c i f i e d . •11

- 36.27 36.88 ! 31130 19 78 11 109 .3 .001 18.90 21. 95 95 Green c h l o r i t i c andes i t i c s c h i s t . 11

- 36.27 36.88 ! 31130 19 78 11 109 .3 .001 18.90 21. 95 95 Green c h l o r i t i c andes i t i c s c h i s t . 11

39.32 l 31131 22 47 8 118 .3 .00: 21 .95 24. 99 95 Green c h l o r i t i c andes i te . 3o. HQ

39.32 l 31131 22 47 8 118 .3 .00: 21 .95 24. 99 95 Green c h l o r i t i c andes i te .

39.62 31132 11 47 10 150 .3 .001 24.99 28. nil 1 nn Same_ as above. 39.32 39.62 31132 11 47 10 150 .3 .001 24.99 28. Same_ as above.

42.37 31127 6 108 6 120 .1 .00; 28.04 31 • 09 100 Same as above but more massive sect ions in s c h i s t . " 42.06 42.37 31127 6 108 6 120 .1 .00; 28.04 31 • 09 100 Same as above but more massive sect ions in s c h i s t . " 46.02 31128 5 41 7 105 .1 .00: 31 .09 34. 14 95 Progressive t r ans i t i on from c h l o r i t i c andesite to d i ss py ' 45.42 46.02 31128 5 41 7 105 .1 .00:

r h y o l i t i c ashf lows. 48.77 49.38 1 31125 19 93 14 81 .3 .00! 34.14 35. 05 95 Clay a l t e red r h y o l i t i c ashf lows. py 53-04 53.64 | 31126 3 57 7 85 .2 .00!

35.05 39- 32 95 Interbedded r h y o l i t i c ashflows with l i g h t l y g r a p h i t i c 57.91 58.52 | 31124 5 59 9 80 .5 .00!

black shales (10% ashflow) 66.45 67.06 1 31123 4 83 10 111 .3 .001 39.32 39. 62 ,100 Brecc iated rhyo l i t e in black shale matr ix . py veins 70.41 71 .0Z 30265 4 111 2 85 .2 .005 39.62 42. 37 95 Black shales with p y r i t i c veins p a r a l l e l to the py veins

bedd i ng. 41.75 m - 30 cm r h y o l i t i c flow ( s i l l ? ) py veins

i . . . 42.37 m - Clay a l t e red contact . Black shales and py veins vol can i c s .

^2.37 46. 94 95 Rhyoli t i c ashf 1 ow. d i s s , py

ii6.94 47. 55 100 Black shales with p y r i t i c veins pa r a l l e l to the py ve in l e t s

bedd i ng.

L . . ..

PROJECT 1 Whist ler U M E X iQC. Described by: A. Cheval ier Property: Dasher DRILL HOLE RECORD Page ] _ of _ Drill Mole No. D D H # 2

Page ] _ of _

Depth % Core Description ft Lithology Minerol ization Sample

No.

Assay Results

From To

% Core Description ft Lithology Minerol ization Sample

No.

1

47-55 48.16 95 Rhyoli t i c ashf1ow. d i 5 s . py

48 .16 49.68 95 Black sha1es.

48-92 m - 30 cm s i l i c i f i e d , brecciated rhyo l i t e and .. black sha le , r ich in c rosscut t ing p y r i t i c v e i n l e t s .

49 .68 55-17 95 1nterbedded rhyol i te (may be t r a ch i t i c ) ashflow and black shale (proport ion of black shale 5-10%)

py r i t e veins pa ra l l e l to the bedding.

55-17 60 .35 95 Same as above with proport ion of black shales 15 -20%,

l i g h t l y metamorphosed to s e r i c i t i c s c h i s t s .

57-91 - 58.52 m - Same as above, c lay a l te red

broken zone.

6 0 . 3 5 69 .19 95 S e r i c i t i c sch i s t ( r h y o l i t i c ashf low).

69 .19 73 .76 85 Several quartz veins (10-15 cm wide) in l i g h t l y

s i l i c i f i e d s e r i c i t e sch i s t ( r h y o l i t i c ashf low).

1

•

P R O J E C T = W h i s t l e r UMEX InC. Described by- A• Cheva l i e r W M V . D a s h e r DRILL HOLE RECORD Page 1 of 2 Dri l l Hole No. DDH //3 Bearinq = S ? 0 W Dr i l l ed by: D r i l c o r

L o c a M o n : W G r i d 7 6 0 N " 1 7 5 E Dip= " 4 6 ° Machine: H y d r a c o r e 28 Dote S tar ted : Nov. 16 . 1981 Depth = 94.49 me t e r s Core Size = BO Date F in ished: Nov. 2 4 , 1981

Depth % Core Description & Lithology

Depth Sample

No.

Assay Results

From To

% Core Description & Lithology Minerolization From To

Sample No. Mo ppm

Cu • ppm

Pb ppm

Zn ppm

Ag ppm

Au ppm

0 1 .22 O v e r b u r d e n . 13.72 14*. 33 30255 3 5M 6 56 .2 ,005 1 .22 38 .10 85 Andes i t e . 25.91 26 .52 30254 2 1 10 64 .1 .005

13 .72 - 14 .33 m - C l a y a l t e r e d zone i n a n d e s i t e . 3 7 . 1 9 38.10 30251 2 41 4 66 .2 .005 25.91 - 26.52 m - S i l i c i f i e d s c h i s t o s e zone 40 .23 4 0 . 8 4 30252 4 6 2 64 .2 .005 ( a s h f l o w t u f f ? ) 41 .76 42 .37 30253 2 34 5 66 .2 .005

38 .10 41 -15 95 B l e a c h e d and c l a y a l t e r e d s i l i c i f i e d a n d e s i t e . 45.72 46 .63 31150 27 14 13 73 -3 .005

4 1 . 1 5 47.85 100 M a s s i v e r h y o l i t e c o n t a i n i n g d i s s . Py . py 45.72 46 .63 31150 27 14 13 73 -3 .005

4 1 . 1 5 47.85 100 M a s s i v e r h y o l i t e c o n t a i n i n g d i s s . Py . py 4 9 . 3 8 4 9 . 6 8 31149 2& 70 ? 93 •7 .025 4 7 . 8 5 49 .68 95 B l e a c h e d and c l a y a l t e r e d r h y o l i t e . 4 9 . 3 8 4 9 . 6 8 31149 2& 70 ? 93 •7 .025 4 7 . 8 5 49 .68 95 B l e a c h e d and c l a y a l t e r e d r h y o l i t e . 49 .68 50 .90 31148 28 72 13 82 .4 .005 4 9 . 6 8 50 .90 95 C o n t a c t zone between r h y o l i t e and s h a l e , b r e c c l a t e d . 49 .68 50 .90 31148 28 72 13

82 .4 .005 4 9 . 6 8 50 .90 95 C o n t a c t zone between r h y o l i t e and s h a l e , b r e c c l a t e d .

55-78 56 .39 31147 54 75 5 305 .8 .005 50.90 57.30 100 I n t e r b e d d e d , l i g h t l y g r a p h i t i c , b roken s h a l e s w i t h py v e i n s 55-78 56 .39 31147 54 75 5 305 .8 .005 50.90 57.30 100 I n t e r b e d d e d , l i g h t l y g r a p h i t i c , b roken s h a l e s w i t h py v e i n s

56 .69 35 146 2 151 .6 .005 s i l i c i f i e d r h y o l i t i c a s h f l o w s . 56 .69 57-30 31144 35 146 2 151 .6 .005

57-30 6 0 . 3 5 85 S i l i c i f i e d r h y o l i t i c t u f f , p y r i t i c c o n t a c t z o n e s . 58.22 58 .83 31145 3 153 2 94 .6 -005

60 .35 66.45 75 B l a c k g r a p h i t i c s h a l e s w i t h a g g l o m e r a t i c s e c t i o n s py v e i n s 60 .05 60 .66 31146 13 81 2 100 .3 .005

and c a l c i t e v e i n s . Some s m a l l s e c t i o n s a r e c l a y 64 .92 66 .14 31142 50 64 10 274 -5 .005

a l t e r e d and p y r i t i c v e i n s o c c u r p a r a l l e l t o the 66 .14 67 .36 31143 38 147 14 141 1-3 .010

bedd i n g . ; 73-55 77.72 31141 21 59 10 141 .8 .005 6 6 . 4 5 67-36 95 P y r i t i c s i l i c i f i e d c o n t o r t e d r h y o l i t e . 5% d i ' s s py 77-72 79-86 ! 31140 25 42 17 157 .8 .005 67.36 71 .02 95 M a s s i v e b l e a c h e d s h a l e s . 79 .86 81.08

1

31139 7 80 8 167 .5 .005 71 -02 80.16 95 I n t e r b e d d e d b l a c k s h a l e s and r h y o l i t e w i t h s e c t i o n s d i s s py

79 .86 81.08 1

31139 7 80 8 167 .5 .005 71 -02 80.16 95 I n t e r b e d d e d b l a c k s h a l e s and r h y o l i t e w i t h s e c t i o n s d i s s py

81 .08 82 .60 31138 19 49 35 122 .7 .005 o f s i l i c i f i e d b r e c c i a w h i c h c o n t a i n some d i s s e m i n . 0-2%) 81 .08 82 .60 31138 19 49 35 122 .7 .005 o f s i l i c i f i e d b r e c c i a w h i c h c o n t a i n some d i s s e m i n . 0-2%) 85.95 86 .26 31137 5 64 17 56 .4 . 005 p y r i te ( o ve r 1Z). 85.95 86 .26 31137 5 64 17 56 .4 . 005

80.16 81 .08 100 P y r i t i c r h v o l i t e . py v e i n s & 92.96 94 .49 ! 3H36 12 127 6 100 .4 .005

d i s s . I

PROJECT-- whistler UMEX- Inc. Property D a s h e r DRILL HOLE RECORD Drill Hole No. DDH //3

Depth % Core Description 8 Lithology Mineralization Sample

No.

Assay Results

From To

% Core Description 8 Lithology Mineralization Sample

No.

81 .08 8 2 . 6 0 95 Interbedded black shale and r h y o l i t e , 85% sha le . Black

shale contains up to \% Py. Rhyol i te is f r ac tu red .

8 2 . 4 5 m - quartz veins conta in ing 5 cm wide massive p y r i t i c

veIns.

8 2 . 6 0 92 .66 100 L ight l y s i l i c i f i e d interbedded g r aph i t i c black shales with 30 cm sect ion of r h yo l i t e .

8 5 . 6 5 - 87 .17 m - p y r i t i c zone 1% Py ve in le t s 9 2 . 6 6 9 4 . 4 9 L ight l y s i l i c i f i e d t r ans i t i on zone from rhyo l i t e to

andes i te .

-

—^——

^age 2_of 2_

Described by: A " Chevalier^