IL .J :, Prospectors Report 1987-1988 Geochemical .

i - . ? I iL 1:",.JP r o s p e c t o r s Report o n 1987-1988Geochemical ReconnaisanceGeochemical SurveyJ GroixpCathy-Cethy-J #&l2 Eineral C l a i m sPar Mtn/Rain?\ow Lake AreaC a r i b 0 0 hlining D i v i s i o nNTS93C14 W-Dates Worked:July 3 r d13thLongitude 125* 26'W L z t - t u d e 52* 49"

Table o f ContentspageP r o p e r t y Location MzpiiiTo po g r a p h i cal MzpC l a i m MapiiiIntroductionLocation & Access11-2Physio grapliyRegional Geology22 -3Geochemistry4C o n clu.s i o n s4Qualifications5Statement of C o s t s6Addeilduni-Sample Analysis Reports and Geochem Kap

.dVN NOl.LV3ffl U W d O t J d

AIntroduction:I n t e r e s t i n t h e r e g i o n a l geology of t h e Rainbow Lake/Far Mountain area w a s first brought t o my a t t e n t i o n i n 1965by a n a s s i s t a n t guide o u t f i t t e r from Anahim Lake, B.C.Havingguided a g e o l o g i s t from t h e United States, t h i s i n d i v i d u a li n d i c a t e d t h e p o s s i b l e presence o f Cu/Au v l a u e s on t h e NWf l a n k o f Far Mountain.With t h e s t a k i n g o f t h e Ilga Mineralclaims by Kerr-Addison i n May 1963, a t t e n t i o n w a s againfocused on t h i s area.After p r e l i m i n a r y reconnaisance i n1984 and 1985, t h e Cathy-J U 2 claims were s t a k e d on J u l y 23and 24, 1986.Location and Access:The Cathy-J#1&2 mineral claims, c o n s i s t i n g o f 20u n i t s each, are l o c a t e d on t h e northwest flank o f Far Mountainapproximately 40 miles n o r t h o f Anahim Lake, B.C.198 miles west o f W i l l i a m s Lake, B.C.which isLocation on NTS Map93C14W is 52*49'N l a t i t u d e , 125*26'W l o n g i t u d e .Access t o t h e Cathy-J p r o p e r t i e s is by f l o a t p l a n et o Rainbow Lake which l i e s approximately 1500 metres n o r t hwest o f the NW c o r n e r of t h e C a t h y 4 #2 claim.Alternately,a c c e s s is by 4-wheel drive approximately 40 miles on t h e DeanRiver Road t o t h e w e s t s h o r e o f Rainbow Lake; t h e n by b o a tacross the lake.Swamp t e r r a i n around t h e l a k e s h o r e makesv e h i c l e a c c e s s t o t h e p r o p e r t y p r e s e n t l y impossible.1

The nearest helicopter service is from Burns Lake(Alpine Helicopters), Prince George (Northern Mountain, andOkanagon) and/or Quesnel, B.C.Physiography :The claims area is situated on the northwestern slopeof Far Mountain approximately 1,500 metres s o u t h e a s t o fRainbow Lake.Elevation o f claims i s between 1,250 metresand 1,650 metres.The area is generally covered by wetconiferous f o r e s t s ; mature spruce and balsam a t the lowerelevations, narrow wet meadows a t mid elevations and subalpine f o r e s t s a t the higher elevations.the d r i e r exposed ridges.Pine s t a n d s coverGround cover c o n s i s t s of heavysphagum moss i n wet areas, reindeer lichen i n the d r i e r areas.Glacial till coverst h e e n t i r e a r e a , b u t i s generally shallow.Outcrop i s very extensive, especially along watercourses.Regional G e o l o a :Far Mountain a t %he northern extremity of the IlgatchuzRange i s a l a t e Tertiary shield volcano o f t h e e a s t trendingAnahim Volcanic Belt.As a r e s u l t o f primary magmatic a c t i v i t y ,the lower elevations a r e composed o f v i s i c u l a r and amygdalordalandesite and basalt.Secondary eruptions produced a largecap of d a c i t e , basalt, andesite, obsidian and rhyolite-p a r t i c u l a r l y along the north flowing Rich Creek drainage.2

PUnfortunately these upper e l e v a t i o n s seem devoid ofany commercial mineralization.No anomolous regions havebeen discovered.On t h e northwest flank of Far Mountain, a t e l e v a t i o n sbelow 1,500 metres, t h e T e r t i a r y volcanic a c t i v i t y d i dn o t cover t h e exposed J u r a s s i c geology.Thus t h e claimsarea is predominantly d i o r i t e , c h l o r i t e s c h i s t , g r a n d i o r i t eand p o r p h y r i t i c q u a r t z monzonite,Quartz i n t r u s i v e s througho u t t h e s c h i s t vary from 0.5 cm t o 1.0 c m i n width, g e n e r a l l yl y i n g along t h e s c h i s t ' s cleavage planes.In the northernone h a l f of t h e claims a r e a , large white q u a r t z blocks,upt o one metre cubed are s c a t t e r e d along the major watercourse;b u t no quartz outcrops have been found i n t h i s a r e a largeenough t o p a r e n t these quartz p i e c e s ,In t h e southern oneh a l f of t h e claims a r e a , q u a r t z comprises 30 t ogroundmass.35 of t h eMuch f o l d i n g and p y r i t i c degeneration (weather-ing) i s e v i d e n t i n t h i s area.3

Geochemical :Eleven days were s p e n t i n 1988 reochem samnling.S o i l s were t a k e n a t t h e B horizon v:hich v a r i e d from 12-24i n c h e s deeg.Rock s a m d e s were grab samples i n t h e n o r t h e r nclaims a r e a , exce7t a l o n g n o r t h e r n boundry where e x p l o s i v e swere used t o g e t t o ledrock.Approximately 50% f l o a t and50 ?jedrock sampling were taken i n t h e s o u t h e r n claims area.I n r o c k s Cu v a l u e s ranged from 2 ppm t o 17,000 ppm;Zn v a l u e s from 50 ppm t o 1,360ppm; Pb f r o m 4 ppm t o 2,700 ppmA g V:ESfrom 0.2 t o 42ppm; Au from 5 ppF t o 1 , 7 7 5 pp5.v a l u e s were g e n e r a l l y much lower.SoilIt appears a l l mineraliza-t i o n i s a s s o c i a t e d with t h e q u a r t z i n t r u s i v e s .Conclusions :F u r t h e r s o i l and rock geochemical sampling shouldbe c a r r i e d o u t t o i d e n t i f y t h e s o u r c e o f m i n e r a l i z a t i o n .Pre1i:i:inary r e s u l t s i n d i c a t e c o n c e n t r a t i n g i n an a r e a a tapproximately 1250 hl s o u t h along t h e C a t h y 4 1 & 2 houndryi n common.F u r t h e r i n v e s t i g a t i o n should also c e n t e r a l o n gt h e s o u t h e r n h u n d r i e s alo-ig the h o r s e t r a i l where exposedquartz is visalle.4

Qua ' i f i c a t i o n s :1.One y e a r c o l l e g e g e n e r a l geology course a t Potsdam,N.Y.,2.USA.Two y e a r s f i e l d work under t h e d i r e c t i o n o f M r . MichaelSmith, g e o l o g i s t f o r BOP.-Selco, a s s i s t a n t t o D r . S t a nHoffman on t h e G r a n 5,6,7 and Laid claims i n t h e "Capoose'Fawnee Mountain area.3.P r e s e n t p r o s p e c t i n g and f i e l d work done under s e l fd i r e c t i o n w i t h sample a n a l y s i s and a d v i c e from M r .RonaldG. McArthur, D i s t r i c t G e o l o g i s t , Noranda E x p l o r a t i o n ,1750 Quinn S t . , P r i n c e George, B.C.David H. Rozek

,-STATEIGSYT OF COSTSWages :11 d a y s ( J u l y 3 r d-13th) @ 125 /day 1375.00T r a n s p o r t a t ion:T o y o t a 4 x 4 P r i n c e George t o TGP LakeAirflightTop Lake t o Rainhow LFkeReturn t r i p-65.00250.00200.00Food:-1 5 .CO/day X 11 d a y sExplosives:Uisc:-(Flagging, Topofil, e t c . )165.00200.0025.00Anal ys i s :138 samples X 12.00Assessment Report P r e p a r a t i o n1656.00200 00

P L A C E RD O M EI N CGEOCHEMICAL DATA LISTING:( V A N C O U V E RL A B O R A T O R Y )BC GEN EXPL CATHY JPDL l a b d a t a f i l e :P8231CATHY JAREA :MAPSHEET NO:93C14WVENTURE :BC GEN EXPLGEOLOGIST:E KIMURALAB PROJECT NO:8231*PLEASE DISTRIBUTE RESULTS TO:EK DR LR MG RH LABREMARKS :"AU1 RESULTS REPORTED IN PPB""COPY OF RESULTS TO D ROZEK; 9392 N KELLY ROAD; PRINCE GEORGE BCV2K 2x3'STANDARD ANALYSIS METHODS USED BY PDL GEOCHEM LAB ARE LISTED BELOW:ALL RESULTS EXPRESSED AS INDICATED IN UNITS COLUMN BELOWANY EXCEPTIONS FOR THIS PROJECT ARE NOTED ABOVEREMARKS:UNITSMO PPMCU PPMZN PPMPB PPMCD PPMNI PPMCO PPMAG PPMAU PPMAU1 PPBU PPMV PPMW PPMF PPMAS PPMSB PPMBI PPMMN PPMFE %HG PPBBA %NA %K %CA %SR PPMMG %SN PPMPT PPBPD PPBLO1 %INTERNAL LAB STANDARDS HAVE BEEN INCLUDED FOR REFERENCE.SAMPLE NUMBERS FOLLOWED BY * ARE DUPLICATE 25.025.01.0ATTACK HN03HCL04/HN03HCL04/HN03HCL04/HN03AQUA REGIAAQUA REGIADIL HN03HF/HCL04/HN03/HCLHCL04/H3P04NA2C03/KN03 FUSIONAQUA DIL 3/HCLNH4I FUSIONFIRE ASSAYFIRE ASSAYASH 600 DEG .02-20%5-2000PPB0.02-20%0.2 -20%0.2 -20%0.02-20%10-20000.2-20%5-500DL lOPPBDL SPPB0.02-99%METHODATOMIC ABSORPTIONATOMIC ABSORPTIONATOMIC ABSORPTIONA.A. BACKGROUND COR.A.A. BACKGROUND COR.ATOMIC ABSORPTIONATOMIC ABSORPTIONA.A. BACKGROUND CORA.A. SOLVENT EXTRACT.A.A. SOLVENT EXTRACT.FLOURIMETRY SOLV. EX.ATOMIC ABSORPTIONDC PLASMASPECIFIC ION ELECTRODEDC PLASMADC PLASMAA.A. BACKGROUND COR.ATOMIC ABSORPTIONDC PLASMAA.A. COLD VAPOR GEN.ATOMIC ABSORPTIONDC PLASMADC PLASMADC PLASMADC PLASMADC PLASMAA.A. SOLVENT EXTRACT.DC PLASMADC PLASMAWEIGH RESIDUE

PLACER GEOCHEM ASSAY SYSTEM: DATA FROM BC GEN EXPL CATHY JGRID’- ‘3C14WISTD P8813188132ci 4R 88305R 8830612 14A88114B881158811988120R 18231823182318231823182318231823182316721173494 0I 0 0.2CO.2 0.2 0.2 0.2 0.2CO.2 0.2 0.2 55106111152471671035811810840211089740 126045’0’1360 0.27%19019951000.40%END OF LISTING 41 RECORDS PRINTEDGCLIST RUN AT: 15:32:440.88% 0.2 0.2 0.2 0.26.0 0.2261.3 0.24212 0.2CO.2CO.2AU1 5 55 5 5 5 5 5 5 5 5 5 5 590)50M.L* 0.2 0.2 0.2 0.210KO.2 56.05401.257514- 1775) 0.2351.32 5051q-:-lr3c” TZw? s-lHAu?cf-,irT; u f i n ?

PLACER DEVELOPMENT LIMITED:GEOCHEM ASSAY SYSTEMm3 IF o l l o w i n g e l e m e n t s needed some v a l u e s a d j u s t e d :ELEMENTcuPBAGAU 1NSSLOWHI%BLNK0000100003024210000100NVAL33.3333338 r e c o r d s skipped: t e s t s , d u p l i c a t e a n a l y s e sSUMMARY O F GEOCHEM DATA:ITEM# 0000END O F GCHSCAN:DATE :cu0330BC GEN EXPL CATHY JMINIMUM93C14W88:09:14MAXIMUMAVERAGESTD. 17000.002700.001360.00t i m e : .49508.55256.6433 RECORDS PROCESSED

PLACER GEOCHEM ASSAY SYSTEM: DATA FROM BC GEN EXPL CATHY 4W93C14W93C14W93C14W9 3C14W9 3C14W93C14W9 272. 650N82727700N7700N* 728850N8850N* C14W93C14W93C14WtestZNSAMPLESTD 0W9500W9500W9500W9500W9500W9500W9500W9500WSTD P9500W9500W9500W9500W9500W9500W9500W9500W9500WSTD P9500W9500W9500W10600W10650W10 7 5 OW107 5 OW107 5 OW10750W10 7 5 4665612566534, 097881359490PBAG0.5540.62020 C0.29 CO.213 0.2500.20.73411 0.213 0.212 CO.210 0.213 0.212 0.214 0.210 CO.211 0.28 0.218 0.213 0.21.210015 CO.22 o--L!22.-.13 CO.210 0.213 0.210 0.211 0.212 CO.210 CO.29 CO.29 KO.211 C0.213 CO.213 0.210 CO.217 CO.216 C0.210 0.212 0.21041.811 CO.210 KO.29 CO.28 CO.211 0.210 0.29 CO.28 CO.213 CO.21101.314 0.216 C0.2170.27652.1130.2110.2220.3130.2120.2, 5 o.z---- 5-130105 5 5 5

ii; PLACER GEOCHEM ASSAY SYSTEM: DATA FROM BC GEN EXPL CATHY W10750W10750WSTD lO0OWllO0OWllO0OWllO0OWllO0OWllO0OWSTD PllO0OWllO0OWllO0OWllO0OWllO0OWllO0OWSTD PSTD AUSTD AUSTD AUBa 7 600N82729650N827282729700N9700N* 300N827282728600N82728615N82728650N8650N* 2729000N82729050N82729100N82729150N9150N* 0687298124931211 o 01211104C0.20.2 o .2 o .20.30.20.60.21.60.20.50.70.60.30.30.60.30.30.3 o .20.50.40.30.20.30.3 0.2 0.2 0.2C0.2 0.2CO.2CO.2 0.20.2 0.2 0.20.20.2 0.2 0.2CO.20.2 0.2 0.2CO.2 0.20.21.2 0.2c0.2 0.2 0.2 0.20.21.45 5.

PLACER DEVELOPMENT LIMITED:GEOCHEM ASSAY SYSTEM8a72Following elements needed some values adjusted:ELEMENTAGAU 1NSSLOWHI%BLNKNVAL00699300000010510515 records skipped: tests, duplicate analysesSUMMARY O F GEOCHEM DATA:ITEMGRIDSAMPPROJAGAU1cuPBZN# VALUESMISSING10501901051051051051050000010586END OF GCHSCAN:DATE :BC GEN EXPL CATHY UMtime: 11:42:05AVERAGE0.205.0227.3413.70107.64STD. DEV.0.2513.6133.008.36100.10105 RECORDS PROCESSED

were used to get to ledrock. Approximately 50% float and 50 ?jedrock sampling were taken in the southern claims area. In rocks Cu values ranged from 2 ppm to 17,000 ppm; Zn values from 50 ppm to 1,360ppm; Pb from 4 ppm 2,700 ppm- Ag V:ES from 0.2 to 42ppm; Au from 5 ppF to 1,775 pp5. Soil values were generally much lower.