FLOREX MINING CO.

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3489FLOREX MINING CO. LTD.Geological, Geochemical & Geophysical ReportJR CLAIMSLatitude 49O 19' North, Longitude 126' 07' WestAUTHOR:A. M. Homenuke, GeologistP. ENGINEER:W. G. StevensonDATE OF WORK:June 1-4, 1972D e p a r t m e n t ofMines and P e t r o l e u m Resources3.&?NO. . MAP . . .

C O N T E N T S.Conclusions .Location & Access .Property .Survey SpecificationsIntroduction .Geological Survey .Geochemical Survey .Data Presentation .SummaryDiscussion of .Instrument SpecificationsMagnetometer .RecommendationsBase Station Magnetometer CRecorder. .Certificate W . G . Stevenson. P . Engineer .Appendix Petrographic Study of 20 Hand Specimens .Statement of Operator’s Qualifications A M Homenuke111222-3334-555567891011-17I L L U S T R A T I O N S41 Figure 1g5Figure 2Location & Claims MapGeological MapGeochemical Map .CopperGeophysical Map .MagneticCompilation MapSoil Profile

LEGENDOutline ofCloimrnighroyShoreL XPLORATIONMAPSurveyodLTD.CLAIMSANDI " (10 M I L E SCO.f RiversAPPROXCLAIMSMAP- CLAIMSI" I 3 0 0 0YAPFEETLROX.*SURVEYSLTD'f

W36g.9NU. . .#I.-.,. J%L?. .,.I*.I.

SUMMARYDuring t h e p e r i o d June 1 t o June 4 , 1972, Tri-Con E x p l o r a t i o nSurveys L t d . , under t h e d i r e c t i o n of W. G. Stevenson, P. Engineer,c a r r i e d o u t a program of r e c o n n a i s s a n c e g e o l o g i c a l , geochemical andgeophysical s u r v e y i n g on t h e J R C l a i m Group, A l b e r n i Mining D i v i s i o n ,The i n f o r m a t i o n c o l l e c t e d i s shown on F i g u r e s 2-5B r i t i s h Columbia.i n t h e back of t h i s r e p o r t , F i g u r e 5 b e i n g a compilation of t h e s i g n i f i c a n t data.An area of i n t e r e s t d e s e r v i n g f u r t h e r i n v e s t i g a t i o nwas o u t l i n e d i n t h e c e n t e r of t h e claim group.CONCLUSIONSThe g e o l o g i c a l survey i n d i c a t e d t h e rocks on t h e claim group t ob e i n t r u s i v e , mainly q u a r t z monzonite, b u t w i t h s e c t i o n s of q u a r t zd i o r i t e , g r a n i t e , and a p l i t e .A broad geochemical anomaly ( g r e a t e r t h a n 20 p.p.m.)across thec e n t e r of t h e p r o p e r t y i n d i c a t e s a p o s s i b l e c o i n c i d e n t zone of mineralization.This comment is based on t h e f a c t t h a t known m i n e r a l i z a t i o nand m i n e r a l i z e d f l o a t occurrences are w i t h i n t h i s broad zone.Assay v a l u e s were t o o low (less t h a n 0.1% Copper) t o b e of economicimportance, b u t they do i n d i c a t e t h e presence of some porphyry coppermineralization.Due t o t h e s p a r s e o u t c r o p , t h e l a c k of any s t r o n g mag-n e t i c f e a t u r e s and t h e small number of a s s a y s t a k e n , i t appears t h a tt h i s zone m e r i t s some f u r t h e r a t t e n t i o n .LOCATION 6 ACCESSThe claims surveyed, J R 1-14,are l o c a t e d n e a r t h e c e n t e r of F l o r e sI s l a n d o f f t h e West Coast of Vancouver I s l a n d approximately 15 m i l e snorthwest of Tofino, B.C.The e x a c t l o c a t i o n i s l a t i t u d e 49019' N ,Longitude 126' 07' W.The p r o p e r t y may b e reached by t a k i n g a b o a t o r p l a n e t o F l o r e sI s l a n d and f o l l o w i n g a w e l l marked t r a i l on f o o t f o r 3 miles t o t h eca

Of the 20 specimens examined seven have been classified as quartz monzonite, five as quartz diorite, seven as granite and one as aplite. A thin section of one of the specimens of quartz monzonite showed 30% interstitial K-feldspar and 10% biotite which has replaced hornblende.

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