/ GEOLOGICAL REPORT on the ELM GROUP OF MINERAL CLAIMS KAMLOOPS, M.D. NTS 921/15W L a t . 50 Long. 120 58' JAY D. MURPHY, P. ENG. Owner and O p e r a t o r 1985 04 - 25 - 52' .. TABLE OF CONTENTS Page No. ........................ SUMMARY AND CONCLUSIONS. . . . . . . . . . . . . . . . . . . RECOMMENDATIONS. . . . . . . . . . . . . . . . . . . . . . . F I E L D PROCEDURES . . . . . . . . . . . . . . . . . . . . . . DISCUSSION OF RESULTS. . . . . . . . . . . . . . . . . . . . STATEMENT OF COSTS . . . . . . . . . . . . . . . . . . . . . STATEMENT OF QUALIFICATIONS. . . . . . . . . . . . . . . . . INTRODUCTION 1 2 2 2 2 4 5 L I S T OF ILLUSTRATIONS PLATE NO. 1 PLATE NO. 2 PLATE NO. 3 .............. ClaimMap. . . . . . . . . . . . . . . . Geology G o l d - S i l v e r Zone . . . . . . . . L o c a t i o n Map 2 3 Back Cover ADDENDA APPENDIX NO. 1 APPENDIX NO. 2 APPENDIX NO. 3 ...... C e r t i f i c a t e o f Assay K-6664. . . . . . . Geochemical Lab R e p o r t G-1188. . . . . . C e r t i f i c a t e o f Assay K-6313. 6 7 8 INTRODUCTION The ELM Group o f e i g h t c l a i m s , l o c a t e d under t h e 2-Post system, is c e n t r e d on t h e j u n c t i o n o f Criss and McGee Creeks, 25 km almost due n o r t h o f Savona on t h e Trans Canada Highway and 41.5 km by road. Access from Savona is v i a t h e Trans Canada Highway 9.3 km west t o Deadman Creek road. T h i s i s followed n o r t h f o r 12.4 km, t h e f i r s t 5 km being hard s u r f a c e d , t h e b a l a n c e well maintained g r a v e l . From Deadman Creek road an a c t i v e l o g g i n g road branches n o r t h e a s t f o r 10.8 km t o Criss Creek where a good camp s i t e is l o c a t e d j u s t n o r t h of t h e b r i d g e . From h e r e a l i t t l e used l o g g i n g road l e a d s n o r t h , then s o u t h e a s t t o t h e ELM claims, a d i s t a n c e of 9 km. The a r e a has been p a r t i a l l y logged, mainly on t h e west s i d e of Criss Creek, b u t a l s o on claim No. 7 e a s t of t h e creek. The r e s u l t i n g network of l o g g i n g t r a i l s p r o v i d e s good access w i t h i n t h e claims. The area is now e x t e n s i v e l y used f o r c a t t l e g r a z i n g d u r i n g t h e snow f r e e p e r i o d . E l e v a t i o n s w i t h i n t h e claims vary from 900 t o 1100 metres. R e l i e f is g e n e r a l l y moderate. One e x c e p t i o n is t h e north-west t r e n d i n g r i d g e along t h e southwest s i d e o f t h e c l a i m group which s l o p e s s t e e p l y s o u t h - e a s t t o Criss C r e e k , a drop o f over 200 meters. The area is w e l l d r a i n e d by Criss Creek, a f a s t flowing stream d r a i n i n g southwest t o Deadman River, which i n t u r n flows s o u t h t o t h e Thompson River. Bush is f a i r l y open and p a r k - l i k e , with n e g l i g i b l e underbrush even where t r e e growth is t h i c k e s t . Topography is subdued with r e l a t i v e l y g e n t l e s l o p e s e x c e p t immediately a d j a c e n t t o Criss C r e e k where near vertical r o c k s c a r p s up t o 30 metres, but u s u a l l y much less, are common. Rock e x p o s u r e s are confined mainly t o t h e c h a n n e l s and banks of Criss and McGee Creeks. Elsewhere, overburden predominates and rock exposures are r e s t r i c t e d t o r i d g e s and road cuts. Overburden varies from a t h i n mantle o f d e t r i t u s from t h e c u r r e n t e r o s i o n cycle t o remnants o f g l a c i a l outwash d e p o s i t s 5 t o 10m t h i c k as seen a t several l o c a t i o n s along Criss Creek. These remnants v a r y from silt grade t o b o u l d e r s and e x h i b i t d i s t i n c t c r o s s bedding. Government r e p o r t s i n d i c a t e t h a t m i n e r a l i z a t i o n on Criss Creek has s t i m u l a t e d e x p l o r a t i o n a c t i v i t y s i n c e a t l e a s t as e a r l y as 1893. I n i t i a l work was done f o r p l a c e r g o l d , l a t e r , mercury and l o d e gold. More r e e n t l y , molybdenum has been t h e metal o f i n t e r e s t . P r e v i o u s work on t h e claim group included d r i v i n g f i v e s h o r t a d i t s , d r i l l i n g a t l e a s t three diamond d r i l l h o l e s , e i g h t p e r c u s s i o n d r i l l h o l e s , and s e v e r a l geochemical s u r v e y s i n v o l v i n g both stream sediment and s o i l sampling 'programmes. The most r e c e n t work r e p o r t e d was done by Craigmont mines i n 1976 and i n c l u d e d e i g h t p e r c u s s i o n d r i l l h o l e s t o t a l l i n g 62511-1. M i n e r a l i z a t i o n is a s s o c i a t e d with a small g r a n i t e body o f L a t e Cretaceous or T e r t i a r y age i n t r u s i v e i n t o Cretaceous conglomerate. ...L i .. I I PLATE N0.I dj ELM G R O U P Kamloops M.D. 921/15W LOCATION MAP J.D.M. I1:500000 1 8 4 - 0 5 - 0 3 - 2 Previous sampling around t h e t h r e e o l d e d i t s on Criss Creek gave some It was decided t o do a d d i t i o n a l encouragement i n s i l v e r - l e a d values. sampling and d e t a i l e d mapping i n t h e general area surrounding t h e a d i t s t o more c l e a r l y d e f i n e t h e zone o f m i n e r a l i z a t i o n . Results o f t h i s work constitute the subject o f t h i s report. SUMMARY AND CONCLUSIONS A m i n e r a l i z e d shear zone has been t e n t a t i v e l y i d e n t i f i e d having an i n d i c a t e d w i d t h o f 50 t o 60m and a p o t e n t i a l s t r i k e l e n g t h o f 200m. Economic m i n e r a l s present i n c l u d e s i l v e r , gold, copper and lead. S i z e and grade o f m i n e r a l i z a t i o n must be more a c c u r a t e l y defined b e f o r e t h e economic prospects o f t h e zone can be estimated. Tonnage p o t e n t i a l i s l a r g e b u t i n d i c a t e d grade is low. RECOMMENDATIONS c) 1. Extend t h e proven s t r i k e l e n g t h o f t h e hanging w a l l v e i n by c a r e f u l A backhoe prospecting, hand t r e n c h i n g and/or mechanical trenching. i s considered t h e most a p p r o p r i a t e equipment f o r t h e l a t t e r phase. 2. Provided good grade v e i n m a t e r i a l can be proven for a s t r i k e l e n g t h i n t h e order o f loom, diamond d r i l l t e s t i n g would be warranted. At l e a s t two angle holes would be required, d r i l l i n g from t h e n o r t h e a s t s i d e C r i s s Creek t o t r a v e r s e t h e main shear zone from hanging w a l l t o A m i n i m u m d r i l l programme o f 160 t o 200m would be f o o t wall. required. FIELD PROCEDURES Rock outcrops i n and surrounding t h e a d i t area were mapped on a s c a l e o f 1:lOOO. Much o f t h i s work was concentrated along C r i s s Creek i t s e l f , which c o n t a i n s t h e b e s t rock exposures and t h e most s i g n i f i c a n t m i n e r a l i z a t i o n found t o date. Character samples were taken from t h e hanging w a l l v e i n and adjacent w a l l r o c k . One s e l e c t e d sample (151) was taken from a narrow, w e l l m i n e r a l i z e d shear within t h e main shear zone c l o s e t o A d i t No. 1. Survey c o n t r o l was mainly by compass and h i p chain but a p r e v i o u s l y e s t a b l i s h e d g r i d o f p i c k e t l i n e s was a l s o u t i l i z e d i n c o n j u n c t i o n with t h e topographic map used as a base f o r p l o t t i n g ' g e o l o g i c a l data. DISCUSSION OF RESULTS D e t a i l e d g e o l o g i c a l mapping revealed a s t r o n g quartz-carbonate v e i n t o 50cm wide c a r r y i n g good copper-silver-gold m i n e r a l i z a t i o n . This v e i n i s exposed f o r a s t r i k e l e n g t h o f 30m along t h e northeast s i d e o f C r i s s Creek and d i p s northeast a t 60 t o 65 degrees ( P l a t e No. 3 ) . M i n e r a l i z a t i o n i n c l u d e s heavy p y r i t e w i t h associated c h a l c o p y r i t e and t e t r a h e d r i t e , i n a d d i t i o n t o weak disseminations o f p y r i t e and t e t r a h e d r i t e more evenly d i s t r i b u t e d throughout t h e v e i n and a d j a c e n t ' w a l l rock. Sample r e s u l t s are t a b u l a t e d on P l a t e No. 3, showing values c f I ic, I ... PLATE N0.2 _ Meirro ELM MINERAL CLAIMS . 921/15w /000 sca/e : 1: 56000 7. 1. 1 CLAIM MAP J.D. M' I : 50000- 1 85-04-22 c i - > - i3 from t h e v e i n material exceeding 4 gm/t gold and 290 gm/t s i l v e r i n a d d i t i o n t o over 1%copper. Samples from a d j o i n i n g wallrock carry 8 . 9 qm/t silver i n t h e c a s e of p y r i t i c conglomerate and over 20 gm/t silver from m i n e r a l i z e d a p l i t e . A selected- sample from a mineralized s h e a r near Adit No. 1 assayed 620 gm/t s i l v e r i n a d d i t i o n t o low gold v a l u e s and n e a r l y 2% copper. The well d e f i n e d quartz-carbonate vein is i n t e r p r e t e d as t h e hanging wall o f a s t r o n g s h e a r zone 50 t o 60m wide t h a t p a r a l l e l s and p a r t l y u n d e r l i e s t h i s s e c t i o n of Criss Creek t r e n d i n g northwest f o r a d i s t a n c e of 200m. The f o o t w a l l is less well d e f i n e d but near Adit No. 3 t h e r e is a d e f i n i t e t r a n s i t i o n from sheared m a t e r i a l t o massive, normal appearing conglomerate. This s h e a r appears t o c a r r y low s i l v e r - l e a d v a l u e s throughout but i n c l u d e s well m i n e r a l i z e d v e i n s and s h e a r s c a r r y i n g copper-gold m i n e r a l s and much h i g h e r s i l v e r values. There is t h e p o s s i b i l i t y t h a t t h e s h e a r zone as a whole c o n t a i n s s u f f i c i e n t v a l u e s i n b a s e and p r e c i o u s m e t a l s t o s u p p o r t an open p i t o p e r a t i o n . Local geology c o n s i s t s of a small d i o r i t e plug i n t r u d i n g cobble conglomerate of probable Cretaceous age on t h e n o r t h s i d e of Criss Creek. Conglomerate c o n t a i n s t h e m i n e r a l i z e d s h e a r zone along Criss Creek as previously and elsewhere, i n a d d i t i o n t o f r e q u e n t s h e a r i n g , and d o l o m i t i c v a r i e t i e s . dj Conglomerate both s i d e s of t h e creek are c u t by numerous f i n e g r a i n e d , d a r k green t r a p d i k e s of v a r i a b l e s i z e and a t t i t u d e . A p l i t e a p p e a r s c l o s e l y a s s o c i a t e d with t h e s h e a r zone along Criss Creek and o c c u r s both as d i k e l i k e bodies w i t h i n and conformable t o t h e s h e a r zones and a s l e s s r e g u l a r masses along both s i d e s of t h e zone. No o u t c r o p s of t h e main g r a n i t e i n t r u s i v e (Unit 2 ) were seen i n t h e a r e a shown by P l a t e No. 3. -4STATEMENT OF COSTS . . The f o l l o w i n g c o s t s were i n c u r r e d on t h e ELM Group o f M i n e r a l Claims by J. D. Murphy, P. Eng. Fieldwork was c a r r i e d o u t on 1984-04-29 and 30 and Report p r e p a r a t i o n was completed between 1984-09-03 and 1984-09-21. between 1985-04-18 and 1985-04-25. LABOUR 12 days f i e l d w o r k , g e o l o g i c a l mapping & sampling @ $250 2 days r e p o r t p r e p a r a t i o n @ $250 T o t a l Labour $3,000.00 500.00 'm $ 3,500.00 TRANSPORTATION 12 days 4 X 4 r e n t a l @ $25 1127 k m @ $.20 Total Transportation $ 300.00 225.40 37-mx7 525.40 ASSAYING ij 2 2 6 2 4 2 1 - r o c k sample p r e p a r a t i o n s 0 $2.50 Ag geochem. a n a l y s i s @ $1.90 sample p r e p a r a t i o n s @ $3.75 Au-Ag assays @ $10.50 Ag assays @ $7.50 Cu assays @ $5.25 Pb assay @ $5.50 T o t a l Assaying $ $ 5.00 3.80 22.50 21.00 30.00 10.50 5.50 98.30 98.30 TYPING 30.00 1.5 h r s . @ $20 TOTAL COSTS $4,153.70 - 5 - STATEMENT OF QUALIFICATIONS I . Jay D. Murphy, hereby certify: 1. That I am a C o n s u l t i n g G e o l o g i c a l Engineer, r e s i d e n t at 1335 Todd Road, Kamloops, B.C. 2. That I am a g r a d u a t e from t h e U n i v e r s i t y o f Manitoba (1954) w i t h a B.Sc. i n G e o l o g i c a l Engineering. 3. That I have p r a c t i c e d my p r o f e s s i o n c o n t i n u o u s l y s i n c e g r a d u a t i o n . 4. That I am a member of t h e 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 of B r i t i s h Columbia and O n t a r i o . 5. That t h e i n f o r m a t i o n c o n t a i n e d i n t h i s r e p o r t is based on a p e r s o n a l examination of t h e s u b j e c t p r o p e r t y . c I I \ K A M L O ~ P S RFSEARCH & ASSAY LABORATORY LTD. 912 - I LAVAL CRESCENT- KAMLOOPS, D C c B.C. LICENSED ASSAYERS GEOCHEMICAL ANALYSTS METALLURGISTS v2c 5P5 PHONE: (604) 372-2784 TELEX: 048-8320 - CERTIFICATE OF ASSAY TO Mr. J a y M u r p h y Certificate No. 1335 Todd Rd., Date -~ Marked Au ozslton 1 May 9 , 1984. V2C 5B4 Kamloops, B.C. Kral No K 6313 151 ,016 ozslton 18.2 Pb cu ,e r c e n t iercent .2' 1.9 1 m I NOTE: c KAMLOOPS RESEARCH & A S A Y LABORATORY LTD. - 912 1 U V A L CRESCENT- KAMLOOPS. B.C. v2c 5P5 PHONE: (604) 372-2784 TELEX: 048-8320 B.C. LICENSED ASSAYERS GEOCHEMICAL ANALYSTS METALLURGISTS - CERTIFICATE OF ASSAY TO M r . Jay Murphy Certificate No. 1335 Todd Road Date Kamloops, B.C. 3 )PrPbp wtify Kral No Marked 181 182 185 186 187 September 25. 1984 V2C 584 that the following are the results of assays made by us upon the herein described Au )unces/ton 1 2 I 3 4 - 5 K-6664 Ag iunces/ton samples cu erc en t .52 .I7 .I5 8.7 6.5 I 4 1 D D -u m z 0 n X z 0 NOTE: Rewfs rclarned throe weeks. pulps relained lhree monlhs p e s s olhemise arranged Z&- Ilcgrslercd Assayer, Province ol Brrlrsh Coluntbu APPENDIX NO. 3 - 8 - KAMLOOPS RESARCH & A S M Y LABORATORY .’1 B.C.CERTIFIED ASSAYERS 912 LAVAL CRESCENT- KAMLOOPS, 6.C. M C 5P5 PHONE: (604) 372-2784 TELEX: 048-8320 - GEOCHEMICAL LAB REPORT M r . Jay Murphy 1335 Todd Road Kamloops, B.C. V2C 584 FILE NO. DATE September 2 1 , 1 9 8 4 ANALYST FIE NO. G- 1 188
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