Frontispiece. View from central part of Trapper Gold property main soil anomaly, looking northwest along kmscale gold-in-soil anomaly to east-facing

Transcription

1 Frntispiece. View frm central part f Trapper Gld prperty main sil anmaly, lking nrthwest alng kmscale gld-in-sil anmaly t east-facing slpes acrss ; nte range-brwn weathering Fe carbnate altered rcks marking margins f zne near ridgeline, t either side f break in slpe.

2 Explratin Prgram, Trapper Gld Prperty, Nrthern Bundary Ranges, Tulsequah Map Area (NTS 4K/07 & ) Atlin Mining Divisin, Nrthwestern British Clumbia, Latitude 8 28'N, Lngitude 2 44'W fr Cnstantine Metal Resurces Ltd., by C.J. Greig (M.Sc. P.Ge.) and S.T. Flasha (M.Sc.) January 28,

3 TABLE OF CONTENTS 1.0 Summary ntrductin Lcatin, Access, and Physigraphy Climate and Vegetatin Claims Gelgic Setting & Mineral Occurrences Reginal Gelgic and Gechemical Wrk Lcal Gelgy Previus Explratin Cnstantine Metal Resurces Ltd. Explratin Prgram Sil & Stream Sediment Gechemical Sampling Sil Gechemical Sampling Prcedure & Analytical Techniques Rck Gechemical Sampling Rck Gechemical Sampling Prcedure & Analytical Techniques Satellite magery and nterpretatin Cnclusins and Recmmendatins References i-

4 LST OF FGURES & TABLES Frntispiece. View frm central part f Trapper Gld prperty main sil anmaly, lking nrthwest alng km-scale gld-in-sil anmaly t east-facing slpes acrss ; nte range-brwn weathering Fe carbnate altered rcks marking margins f zne near ridgeline, t either side f break in slpe. Figure 1. Lcatin f the Trapper Gld prperty, nrthwestern British Clumbia Figure 2. Lcatin f the Trapper Gld prperty, nrthwestern British Clumbia, shwing lcatin f the Glden Bear Mine access rad Figure 3. Trapper Gld prperty tenures, Atlin Mining Divisin, nrthwestern British Clumbia Table 1. Trapper Gld prperty tenure infrmatin Figure 4. Reginal gelgic map, shwing lcatin f the Trapper Gld prperty, surrunding mineral tenures, and selected mineral ccurrences Figure. Prperty gelgy, Trapper Gld prperty, after Waltn (4) Figure 6. Cnstantine gelgist, Darwin Je P Green, examining Fe carbnate altered mafic tuffaceus rcks, western slpes f nlaw creek, Trapper Gld prperty Figure 7. Detail shwing pervasively Fe carbnate altered matrix t mafic fine- t mediumgrained lithic lapilli tuff, prbably f Upper Triassic Stuhini Grup; area Figure 8. Stained (left) and etched (right) slabs f hrnblende(?)-pyrxene feldspar bearing finet medium-grained mnznite r mnzdirite; bars at base are 1 cm Figure 9. Trapper Gld prperty, verview map shwing lcatin f sil gechemical sampling recnnaissance traverses, relative t Chevrn Minerals 4 sil gechemical grid.. -- Figure. Previus rck sample gechemistry, Trapper Gld prperty, shwing the lcatin f the tw shrt trenches excavated by Chevrn Minerals and Slmn Resurces Figure. Sil and stream sediment sample lcatins, Cnstantine Metals prgram, Trapper Gld prperty Figure 12. View nrthwest alng the Fe carbnate alteratin zne which hsts the apprximately 2 km lng gld-in-sil anmaly n the Trapper Gld prperty Figure. Gld gechemistry in sil and stream sediment samples, Cnstantine Metals prgram, Trapper Gld prperty ii-

5 Figure 14. dealized trend f gld mineralizatin n the Trapper Gld prperty, based n sil sample results frm Chevrn Minerals 3 prgram, Richfield Ventures 08 prgram, and thse frm Cnstantine Metals prgram Figure 1. Rck sample lcatins, Cnstantine Metals prgram, Trapper Gld prperty Figure. Gld gechemistry f rck samples frm Cnstantine Metals prgram, shwing gld-in-sils data frm Richfield 08 sampling, Trapper Gld prperty Figure. Old man (Charles Tw-Pdy Greig) attempting t sample Fe carbnate-quartz vein west f ; grab sample H48414, see detail in fig Figure. Detail f chalcpyrite-rich grab sample H48414, frm vein shwn in fig. cntaining g/t Au,.1 g/t Ag, and 3.23% Cu Figure 19. Well expsed Fe carbnate alteratin zne cntinuus t the sutheast with main Trapper Gld mineralizing system and truncated by uncnfrmity with verlying rewrked(?) Tertiary(?) vlcanic rcks; near eastern limit f prperty, n Tw Pdy and Weenus Sup tenures LST OF APPENDCES Appendix. Appendix. Sil & Stream Sediment Sample Lcatins Sil & Stream Sediment Sample Gechemical Data Appendix. Rck Gechemical Sample Descriptins and Lcatins Appendix V. Rck Gechemical Sample Data Appendix V. Satellite magery nterpretatin; Reprt by Ming-H Du Appendix V. Cst Statement Appendix V. Statement f Qualificatins -iii-

6 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha 1.0 Summary n late August,, a fur persn crew mbilized by helicpter frm Juneau, Alaska, spent a day n the Trapper Gld prperty prspecting and sil sampling. The purpse f the wrk was t examine and pssibly extend the nrthwest-trending Au-in-sil gechemical anmaly n the eastern side f which was riginally utlined in the early 0's by Chevrn Minerals. The pssible nrthwestward cntinuatin f the sil anmaly alng-strike and acrss was accmplished by means f sil gechemical cntur sample lines and a brief gelgical examinatin. n additin, the central part f the main sil anmaly n the eastern side f the creek was examined and prspected. n ttal, rck, 9 sil, and 2 stream sediment samples were cllected and sent fr analysis t ALS-Chemex Labratries in Vancuver, B.C. The mst significant results frm the prgram were frm the sil gechem lines, where fifteen samples in tw lines returned greater than 0 ppb Au acrss distances f between and 0 metres. The results strngly suggest that the Trapper prperty gld mineralized zne n the west side f lies at, and perhaps t the nrth f, the nrthern ends f the sil cntur lines. There the best results are cincident with range-brwn weathering, strngly Fe carbnate altered mafic vlcanic rcks, much as they are t the east f creek. Thus the sil sampling prvides gd evidence that the Au-bearing mineralizing system n the prperty is cntinuus ver at least 2 km alng a nrthwest trend. On the basis f the psitive results f the field prgram, Cnstantine cmmissined a study f satellite imagery fr the Trapper Gld prperty area. The study utilized Landsat TM, ASTER, and GeEye images that were used t identify znes in the regin f irn xides, clay alteratin, and silicificatin, all f which are knwn t be assciated with gld mineralizatin n the prperty. The resultant interpretive images als include structural interpretatins and create excellent targets fr the next phase f explratin n the prperty and in the immediate vicinity. Further wrk n the prperty is recmmended. t shuld be based ut f a camp n the prperty and shuld begin with the establishment f a cut-and-chained grid ver the main gechemical anmaly. Systematic wrk acrss the grid shuld include prspecting, gelgic mapping, and in-fill sil gechemical sampling. The grid shuld als serve as cntrl fr an nduced -1-

7 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha Plarizatin (P) and magnetmeter/vlf-em survey. At the same time, the camp might serve as a base fr helicpter-supprted wrk n the mre distant parts f the prperty, as well as farther afield, fllwing up targets generated by the satellite imagery study. Shuld the early stage wrk n the grid prvide encuragement, a drill prgram utilizing a lightweight fly-drill shuld be cnsidered. 2.0 ntrductin The Trapper Gld prperty, als knwn previusly as the Trapper Lake, Check-Mate r Ech prperty, and riginally as the nlaw prperty, cnsists f nine tenures ttalling 376 hectares. t was staked fr its precius metals ptential. Previus sil sampling prgrams in the early 0's by Chevrn Minerals f Canada utlined a large-scale, high-tenr gld-in-sil gechemical anmaly. Hwever, a prgram run in 0 by Slmn Resurces Ltd., which attempted t test the Chevrn wrk, shed sme dubt n the existence f the anmaly and its assciated mineralizatin. Prir t staking the riginal claim f the Trapper Gld prperty grup in 07, the lead authr came t the cnclusin that Slmn s wrk did nt adequately test the anmaly, and in fact, the nly sil samples cllected clse t the main part f it actually returned highly anmalus results. n 08, a sil sampling prgram was designed fr Richfield Ventures Crp. t better test the Chevrn anmaly. Over 0 samples were cllected, as well as rck samples and stream sediment samples. The prgram prved fruitful as anmalus Au-in-sil values, typically between 0 ppb and +00 ppb Au, extended ver a kilmetre in length and averaged 0-0 metres in width (Greig 08). Assciated Fe carbnate-silica alteratin als suggested the presence f a large-scale hydrthermal system. Further wrk was recmmended. n spite f the psitive results, the adverse ecnmic climate f the latter half f 08 led Richfield Ventures Crp. t drp the ptin n the Trapper Lake prperty and return it t Greig. n 09, he came t an agreement with Cnstantine Metal Resurces Ltd. and after expanding the prperty smewhat, explratin n what is nw named the Trapper Gld prperty recmmenced in. -2-

8 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha 3.0 Lcatin, Access, and Physigraphy The Trapper Gld prperty, lcated in nrthwest British Clumbia s Atlin Mining Divisin, lies within the nrthern Bundary Ranges f the Cast Muntains (Chechilda Range), immediately west f the Tahltan Highlands and Stikine Plateau (figs. 1 and 2). The prperty is centred n a nrthsuth trending ridge system, and the suthern and eastern slpes f the ridge drain int Tunjny Lake and the west-nrthwest shres f Trapper Lake (fig. 3). The western claims straddle the headwaters f a shrt tributary f what is knwn lcally as La Jaune Creek (Baker and Simmns 06). This tributary, infrmally named by Tupper (0), flws nrtherly int La Jaune Creek, which in turn flws nrtherly int the Sutlahine River, a majr tributary f the nklin and Taku rivers. Elevatins n the Trapper Gld prperty reach mre than 00 metres, and relief is greater than 00 metres, with terrain generally relatively gently-slping in the immediate vicinity f, with steeper rcky r grassy slpes, particularly in the central part f the claim grup (Frntispiece). The prperty is mst readily accessible by helicpter, frm either Atlin (2 km t the nrthwest), Dease Lake (19 km t the east), r Juneau, Alaska (apprx. 0 km t the west). The clsest cmmunities are Telegraph Creek (4 km t the sutheast) and Juneau, which f curse lies acrss the U.S. brder. The Glden Bear mine rad, 4 km suth f the prperty, culd prvide ready access but is currently washed-ut, and s practical rad access is 1 km distant. As a cnsequence, the mst suitable access is by air, specifically by helicpter, althugh Trapper and Tunjny lakes can be serviced by flatplane, and there are flatplane bases at Telegraph Creek, Dease Lake, Atlin, and Juneau. -3-

9 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha YUK ON TER RT ORY Atlin N Trapper Lake Gld Prperty Stikine R Dease Lake L ia rd R BRTSH COLUMBA Frt Nelsn NWT CANADA LEGEND / LÉGENDE Prvincial capital Other ppulated places ALASKA USA Stewart Willistn L Frt St Jhn Trans-Canada Highway Majr rad Ferry rute Prince Gerge Fras Fl e r nternatinal bundary Prvincial bundary Bella Cla Williams Lake PACFC OCEAN F r ase r R Glden Kamlps AL BE R TA Kelwna Scale 0 km km Nanaim Vancuver Trail Victria UNTED STATES OF AMERCA Cranbrk Figure 1. Lcatin f the Trapper Gld prperty, nrthwestern British Clumbia. -4-

10 0000 me mn Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy Hwy mn Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Cassiar Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart Stewart me me me me me 0000 me mn mn Dease Lake Dease Lake Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla Tanzilla River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha Trapper Lake Chechilda Peak Tatsamenie Lake skut nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin nklin River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River Sheslay River Trapper Gld Prperty t t t t t t t t t t t t t t t t t t t t t t t t t t t t t t t t t t t t t t t t t t t t t t t t t Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Juneau Hwy Sheslay Creek Glden Bear Mine Telegraph Tahltan River Telegraph Creek River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River River RCHFELD VENTURES CORP. Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Stikine Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Schaft Date:27//08 Authr: Trapper Gld Prperty Dease Lake - Telegraph Creek Area, Nrthwest BC Creek Office: me Drawing: R. Greig Scale: 1: Prjectin: UTM Zne 8 (NAD 83) kilmetres Figure 2. Lcatin f the Trapper Gld prperty, nrthwestern British Clumbia, shwing lcatin f the Glden Bear Mine access rad. --

11 -6-6,488,000 mn 6,486,000 mn 6,484,000 mn 6,482,000 mn Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek La La La La La La La La La La La La La La La La La La La La La La La La La La La La La La La La La La La La La La La La La La La La La La La La La Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune Jaune 00 6,000 me Rimfire Minerals Crp. 6,000 me nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek 673 TWOON ECHO JALER HX 632,000 me 6,000 me 636,000 me 632,000 me WHEELNUS WEENUS SOUP KNEER Tunjny Lake 64 TWO-POODY JOE-PO 6,000 me 636,000 me Date:6/1/ Authr: Office: C Greig Drawing: SFlasha Scale: 1: _Z 638,000 me 638,000 me 6,488,000 mn Prjectin: UTM Zne 8 (NAD 83) Cntur nterval: 40m 0. 1 Trapper Gld Prperty Claim Lcatin kilmetres 6,486,000 mn 6,484,000 mn Trapper Lake 2 6,482,000 mn Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha Figure 3. Trapper Gld prperty tenures, Atlin Mining Divisin, nrthwestern British Clumbia.

12 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha 4.0 Climate and Vegetatin The Trapper Gld prperty experiences mderate summers and cld winters. Temperatures typically range between /C and 1/C in summer and -/C and - /C in winter. Precipitatin is lwest in the spring mnths and snw accumulatins in winter can be expected t exceed 1. metres. ts lcatin n the lee side f the Cast Muntains results in a smewhat drier climate than areas nearer the Pacific cast. Belw treeline, which lies between 10 and 0 metres, vegetatin n the prperty cnsists primarily f thick dwarf balsam fir (alpine fir) with lcal willw and juniper, while at higher elevatins, grasses and high alpine flra prevail. Outcrp is generally gd, althugh uncnslidated fluvial depsits are cmmn alng the curses f nlaw creek and its tributaries, and talus r scree mantles parts f the steeper slpes..0 Claims The prperty cnsists f nine mineral titles (fig. 3) encmpassing an area f apprximately 6.0 km (E-W) by 6. km (N-S), fr a ttal f 3,76 hectares (Table 1). The riginal Trapper Gld prperty claim was staked in 07, and was centred n nlaw creek and the anmalus Au-in-sil values utlined by Chevrn Minerals in the early 0's. Additinal claims were added t the surrunding Table 1. Trapper Gld prperty tenure infrmatin. Tenure Number Claim Name ssue Date Gd T Date Area (ha) 61 ECHO 07/JUL/01 12/OCT/ TWOON 09/OCT/ 12/OCT/ JALER 09/OCT/ 12/OCT/ HX 09/OCT/ 12/OCT/ WHEELNUS 09/OCT/ 12/OCT/ KNEER 09/OCT/ 12/OCT/ TWO-POODY 09/OCT/ 12/OCT/ JOE-PO 09/OCT/ 12/OCT/ WEENUS SOUP 09/OCT/ 12/OCT/ TOTAL

13 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha area in 09 after that grund came pen. The claims are held by Charles Greig but they are currently 0% wned by Cnstantine Metal Resurces Ltd., as per an agreement signed in May,. The prperty is in gd standing until Octber, 12, pending acceptance f this reprt. Rimfire Minerals Crp. hlds the titles adjacent t the western and nrthern parts f the prperty, and these titles are cntiguus with a large blck f Rimfire claims that cver the well-knwn Thrn prperty (fig. 4). 6.0 Gelgic Setting & Mineral Occurrences 6.1 Reginal Gelgic and Gechemical Wrk The nly dcumented reginal mapping undertaken in the immediate area f the Trapper Gld prperty was that by Suther (Map 12A, 1971), wh mapped the Tulsequah mapsheet (NTS 4K) at 1:,000 scale. Mre recent and mre detailed 1:0,000 scale mapping, in large part supprted by the B.C. Gelgical Survey Branch (BCGSB), has been undertaken t the sutheast f the prperty in the Tatsamenie Lake (e.g., Oliver and Hdgsn 9, Bradfrd and Brwn 1993, Oliver and Gabites 1993, and Oliver 199). Part f this mre detailed wrk was fcussed n Devnian and Permian lithlgies assciated with gld mineralizatin discvered near Muddy Lake by Chevrn Minerals in the early 0's. Similarly, t the nrthwest, the BCGSB has undertaken 1:0,000 scale mapping in the vicinity f the Tulsequah depsit in recent years (e.g., Mihalnyuk et al. 1994, Sherlck et al. 1994, Sebert et al. 199). A 1:,000 scale reginal gechemical survey (RGS) was als undertaken by the GSC and BCGSB thrughut the Tulsequah mapsheet in 7. The reginal gelgy, largely after Suther (1971), is shwn in Figure 4, while Tupper (0) has nicely summarized the ecnmic significance f mineral depsits in the regin. This -8-

14 -9- TULSEQUAH CHEF MNE 6,00,000 mn 6,490,000 mn 6,4,000 mn 6,470,000 mn Authr: RCHFELD VENTURES CORP. Date:2/12/08 Office: CGreig Drawing: SFlasha 90,000 me Scale: 1:000 Prjectin: UTM Zne 8 (NAD 83) 0 ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA ALASKA Trapper Gld Prperty Reginal Gelgy 2. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. B.C. kilmetres 600,000 me 600,000 me 6,000 me 6,000 me 6,000 me 6,000 me 6,000 me 640,000 me Rimfire Mineral Crp. Thrn Prperty Thrn Trapper Gld Prperty 6,000 me 640,000 me 60,000 me Stratified Rcks 60,000 me Early Ecene - Slk Grup Lwer Jurassic - Laberge Grup 660,000 me cnglmerate, carse clastic sedimentary rcks undivided sedimentary rcks andesitic vlcanic rcks Upper Triassic - Stuhini Grup undivided sedimentary rcks undivided vlcanic rcks Carbnifierus - Stikine Assemblage vlcaniclastic rcks carse clastic sedimentary rcks Devnian t Mississippian - Whitewater Metamrphic Cmplex 6,,000 mn 6,,000 mn 6,00,000 mn greenstne t greenschist metamrphic rcks ntrusive Rcks 6,490,000 mn Palecene t Ecene - Slk-Hyder Plutnic Suite granite, alkali feldspar granite intrusive rcks Late Cretaceus - Windy Table Cmplex quartz diritic intrusive rcks Middle Triassic t Late Triassic quartz diritic intrusive rcks 6,4,000 mn 6,470,000 mn 6,460,000 mn GOLDEN BEAR MNE Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha Figure 4. Reginal gelgic map, shwing lcatin f the Trapper Gld prperty, surrunding mineral tenures, and selected mineral ccurrences.,000 me

15 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha part f British Clumbia is underlain by rcks f the Stikine terrane, r Stikinia, a mid-palezic t Middle Jurassic vlcanic island arc terrane with a prbable rigin in the eastern Pacific. Stikinian rcks include bth vlcan-sedimentary successins and cmmn ceval plutns. n the immediate area f the Trapper Gld prperty, there are few, if any, age-cnstraints n the vlcanic r vlcansedimentary rcks r n the intrusive rcks emplaced int them, althugh mst f the stratified rcks have been assigned t the Upper Triassic Stuhini Grup. Rcks f the Stuhini Grup were largely depsited in a submarine arc-type envirnment and cmprise basalt and basaltic-andesite flws and pillw lavas, carse fragmental rcks, and lapilli tuff. Many f these rcks may be augite-phyric, but feldspar-phyric varieties are als cmmn. Subrdinate limestne, argillite, and siltstne have als been bserved lcally (Bradfrd and Brwn 1993, Mihalynuk 1994, Suther 1971). Large bdies f quartz dirite, strngly fliated dirite, and minr grandirite, which Suther (1971) believed t be Lwer r Middle Triassic in age, are fund t the east and west f Tatsarnenie Lake. T the nrthwest f Trapper Lake, Suther (1971) mapped a belt f Laberge Grup rcks cnsisting f well bedded Lwer t Middle Jurassic greywacke, siltstne, silty sandstne, mudstne, and limey pebble cnglmerate f the nklin Frmatin, and granite-bulder and chert-pebble cnglmerate, greywacke, quartz sandstne, siltstne, and shale assigned t the Takwahni Frmatin. ntruded int and verlying the early t middle Meszic Stuhini and Laberge sequences are Late Cretaceus and Early Tertiary intrusive and extrusive rcks f the Windy Table cmplex and the Slk Grup, respectively (Mihalynuk 1994). Rcks f the Windy Table Cmplex cmprise feldspar prphyritic rcks and quartz dirite, while Slk Grup rcks include rhylite, dacite and trachyte flws, pyrclastic rcks, and vlcanic-derived sedimentary rcks, as well as felsic dykes. --

16 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha 6.2 Lcal Gelgy A schematic map shwing the gelgy f the Trapper Gld prperty is shwn in Figure. As riginally depicted by Suther (1971), mst f the prperty was believed t be underlain by rcks f the Upper Triassic Stuhini Grup. Waltn (4), wrking fr Chevrn Minerals, utlined a brad nrthwest-trending zne f Fe carbnate-altered mafic vlcanic rcks, apprximately 600 t 00 metres acrss, which hsts the gld-in-sil gechemical anmaly that was als first identified by Chevrn, in 3, and which has largely been the fcus fr subsequent explratin. The map in Figure als shws tw dirite stcks immediately t the suth and east f the sil anmaly. They are smewhat elngate alng nrthwest trends, with the western stck having a mre irregular utline, a length f up t 600 metres, and a width f apprximately 0 r 0 metres acrss. Waltn (4) als mapped a nrtheast-trending fault cutting the eastern stck, as well as a number f lcal nrth-, nrtheast-, and nrthwest-trending rhylite prphyry dykes f prbable Tertiary age. As described by Waltn (4), Stuhini Grup rcks n the prperty cnsist largely f dark green massive and lcally augite-phyric flws and tuffaceus rcks. Flws lcally display pillw structures and very lcal flw-banding, while tuffaceus rcks are typically lithic lapilli tuff, and lcal crystal-rich ash tuff. Bedding in the tuffaceus rcks suggested t Waltn (4) that the sequence dipped steeply t the east. He als bserved the diritic stcks, which he described as cnsisting f medium-grained, equigranular pale weathering dirite lacking significant sulphides, and exhibiting nly lcal chlrite alteratin f mafic minerals. Aspinall (1998) als prduced a schematic gelgic map f the prperty. Althugh it differs in sme respects frm the map f Waltn (4), particularly with regard t the extent f Fe carbnate alteratin, it lacks detail, as well as bvius pints fr registratin, and therefre --

17 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha 63,000 me prphyritic feldspar 6,48,000 andesite mn 6,484,000 mn Trapper Gld Prperty 6,483,000 mn Gelgy frm Chevrn 4 631,000 me 632,000 me 633,000 me 6,000 me 6,000 me 63,000 me 632,000 me 633,000 me ,486,000 mn 6,48,000 mn 6,484,000 mn ,483,000 mn Tertiary-Cretaceus - Slk Grup dacitic feldspar prphyry rhylitic feldspar prphyry Jurassic-Cretaceus dirite Triassic - Stuhini Grup basalt flws agglmeritic basalt undivided vlcanic rcks cntact cntact fault _Z Date:6/1/ Authr: Office: C Greig Drawing: SFlasha Scale: 1:000 0 Prjectin: UTM Zne 8 (NAD 83) Cntur nterval: 40m 00 1,000 metres cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact cntact limit limit limit limit limit limit limit limit limit limit limit limit f f f f mapping mapping mapping mapping mapping mapping mapping mapping mapping mapping mapping 631,000 me Figure. Prperty gelgy, Trapper Gld prperty, after Waltn (4). -12-

18 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha integratin f the tw is prblematic. Slmn s crew als made sme gelgic bservatins during their wrk n the prperty (Tupper 0), but n significant changes were made t Waltn s (4) map. Althugh n systematic gelgic mapping was undertaken during Richfield s wrk n the Trapper Gld prperty in 08, a number f gelgic bservatins were made during the limited time spent prspecting and sil sampling the suthwestern margin f Chevrn s gld gechemical anmaly. Fr example, the well expsed range-brwn weathering rcks in the lwer reaches f the tributaries t, which hst the gld-in-sil anmaly, were described by Greig (08) t largely represent strngly Fe carbnate altered and variably silicifed mafic tuffaceus rcks (figs. 6 and 7). Greig (08) als bserved that the mafic stratified rcks were intruded lcally by alkalic intrusive rcks, and that the dirites mapped by Chevrn and thers may well be alkalic, because K-feldspar staining f the single sample cllected frm the diritic intrusive rcks indeed Figure 6. Cnstantine gelgist, Darwin Je P Green, examining Fe carbnate altered mafic tuffaceus rcks, western slpes f nlaw creek, Trapper Gld prperty. suggests that the rcks are alkalic (fig. 8). Greig (08) explained that --

19 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha Figure 7. Detail shwing pervasively Fe carbnate altered matrix t mafic fine- t medium-grained lithic lapilli tuff, prbably f Upper Triassic Stuhini Grup; nlaw Creek area. Figure 8. Stained (left) and etched (right) slabs f hrnblende(?)- pyrxene feldspar bearing fine- t medium-grained mnznite r mnzdirite; bars at base are 1 cm. -14-

20 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha this may be taken t suggest that the intrusive rcks n the prperty may be as ld as latest Triassic r earliest Jurassic, rather than Cretaceus r Tertiary, as had been suggested by previus wrkers, because alkalic intrusive rcks are cmmn early t mid Meszic f this part f nrthern Stikinia (e.g., Brwn et al.1996). f that is the case, this shuld be cnsidered favurable, as alkalic intrusive rcks emplaced int Upper Triassic mafic vlcanic rcks elsewhere within Stikinia (and Quesnellia) bear a cmmn assciatin with mineral depsits, and mre significantly, thse mineral depsits are cmmnly precius metals-rich (e.g., Galre Creek, Snippaker Creek, Silbak-Premier). 6.3 Previus Explratin The Trapper Gld prperty was first staked as the nlaw claim by Chevrn Minerals Ltd. in 2, when anmalus gld values were returned in sil gechemical samples cllected alng recnnaissance traverse lines (Waltn 4). Chevrn gelgists nted that bth the recnnaissance-style sil gechemical sampling and subsequent grid-cntrlled sil sampling (700 samples; fig. 9) indicated that there was a large area f anmalus gld present n the prperty, and that within the anmaly there were a number f very high values. Fr example, in the grid gechemical wrk, between ten and fifteen individual sil samples yielded gld values greater than 00 ppb, and tw sites yielded >00 ppb Au alng the >1 km strike length f the anmaly. The anmaly als encmpassed many supprtive +0 ppb Au values, and it als appeared t be pen t the west, near the valley bttm f nlaw creek (fig. 9). As fllw-up t the grid sil gechemical wrk, bulk sampling and heavy mineral separatin f sil cllected at grid sample sites yielding the highest gld values (up t 860 ppb) cnfirmed their lcatin and high gld cntent, and shwed that visible gld grains were likely -1-

21 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha 63,000 me 6,487,000 mn Richfield 08 >0 ppb 6,486,000 Au mn 6,48,000 mn 6,484,000 mn 6,000 me 631,000 me 632,000 me 633,000 me 6,000 me 631,000 me 632,000 me 633,000 me 6,000 me 6,487,000 mn Date:19/1/ Authr: Office: C Greig Drawing: S Flasha Scale: 1:000 _Z 0 Trapper Gld Prperty Sil Sample Lcatins 3, 04, 08 & Prjectin: UTM Zne 8 (NAD 83) Cntur nterval: 40m 00 metres 1,000 samples Richfield 08 sil samples 6,486,000 mn Slmn (04) sil lines Slmn (04) >40 ppb Au Chevrn (3) sil grid Chevrn (3) sil >0 and 0 ppb Au 6,48,000 mn 6,484,000 mn Figure 9. Trapper Gld prperty, verview map shwing lcatin f sil gechemical sampling recnnaissance traverses (Slmn Resurces Ltd. 04, Richfield Ventures 08, and Cnstantine Metal Resurces ), relative t Chevrn Minerals 4 sil gechemical grid. --

22 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha present n the prperty (Waltn 4). Waltn (4) als nted that there was a crrelatin between gld and As and Sb, and nted that the extensive As-Sb hal arund the cre f the Au anmaly suggested that the mineralizing system culd be quite large. The 4 Chevrn fllw-up prgram als included preliminary mapping and prspecting, with ver grab samples and channel samples cllected. Grab samples included ne sample which returned mre than.0 g/t Au, and the channel samples, all cllected frm a single trench, returned up t 6.2 g/t Au. The trench excavated by Chevrn measured apprximately 3 x 8 metres, with the lng dimensin riented perpendicular t the verall trend f the gld-in-sil anmaly. The trench was excavated in bth altered tuffaceus rcks and in a silicified felsic dyke(?), and the eleven 1.0 metre chip samples all returned values greater than 0.3 g/t Au and 3.8 g/t Ag. As mentined abve, the sample returning the highest value was 6.2 g/t Au, alng with.4 g/t Ag, and verall, the samples averaged 1.9 g/t Au and 9.0 g/t Ag, which suggests that altered wallrck n the prperty may prvide gd supprt fr any higher-grade material encuntered. Accrding t Waltn (4), previus sampling in the area had returned grades in grab samples ranging up t 33 g/t Au. The trench sampling als apparently cnfirmed that the better grades were btained frm sulphide veins, as ppsed t the silica flding cmmn in the trenched area. Furthermre, Waltn (4) nted that prspecting n the prperty cntinued t result in the discvery f mre veins, in spite f the rather sparse utcrp. Chevrn gelgists and prspectrs als cllected a cnsiderable number f samples elsewhere n the nlaw prperty. Althugh the samples were analyzed nly fr Au, Ag, Sb, and As, it is ntable that As values up t and lcally exceeding 1.0% were btained. The high-arsenic samples als cmmnly returned elevated gld values. Several samples returning gld values were als apparently cllected frm within the bunds f ne f the diritic stcks (Waltn 4). --

23 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha Althugh Chevrn gelgists recmmended further wrk be dne n the nlaw prperty (Waltn 4), n further wrk appears t have been dcumented (e.g., Waltn 7), perhaps because Chevrn was devting mst f its cnsiderable energies t its gld discvery at nearby Muddy (Bearskin) Lake, which ultimately became the Glden Bear depsit (fig. 4). n 1994 the nlaw claim was allwed t lapse, but in 1998 it was restaked by Clive Aspinall as the Check-Mate 2 claims, and in the same year Aspinall cllected a ttal f 1 rck, sil, and stream sediment samples, with the highest gld values returned being 2.04 g/t in a sil sample, 0.09 g/t frm a stream sediment sample, and g/t in a rck sample frm flat (Aspinall 1998). Aspinall als suggested that the Fe-carbnate alteratin utlined by Chevrn was much mre extensive than indicated by the previus wrk, that alteratin was clsely assciated with what he interpreted t be an uncnfrmity, and that a high-sulphidatin depsit mdel, such as had been applied t the nearby Thrn prperty, might be applicable t the Trapper Gld prperty. n 04, Aspinall ptined the prperty t Slmn Resurces Ltd., and three additinal claims were added t the nrth and east f Aspinall s riginal Check-Mate 2 tenure. Slmn s 04 wrk prgram, ttaling abut man-days, was designed t cnfirm the sil gechemical anmalies and bedrck sample results btained by Chevrn, as well as t evaluate the adjacent newly-staked claims using stream sediment gechemistry, recnnaissance sil sampling, prspecting, and gelgy. Slmn s crews cllected a ttal f 8 rck samples, 3 sil samples, and stream sediment samples (Tupper 0). The stream sediment samples cllected by Slmn were cllected primarily frm westflwing tributaries f. The results, tgether with thse frm ther nearby streams, cnfirmed that the area was highly anmalus in Au, As, Sb, Hg, and Cu, as had been determined in the gvernment Reginal Gechemical Survey (RGS; BCGS 9). n particular, the Slmn --

24 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha survey shwed that the upper headwaters f were anmalus in Au, as were the tributaries draining westward int the creek frm the anmaly utlined by Chevrn (e.g., 141 ppb Au; ppb Au; 67 ppb Au). These streams were als highly anmalus in As, Sb, Pb, Zn, and Cu. The results suggested t Tupper (0) that there may be metal znatin within the hydrthermal system n the prperty, frm Au+As+Pb in the suth t As+Sb+Zn in the nrth, with Cu being mst highly anmalus in between. Accrding t Tupper (0), the 04 sil gechemical wrk was designed t incrprate and augment the wrk by Chevrn. Slmn cmpleted a ttal f eight cntur sil lines, including fur detailed lines with clse sample spacings, sme f which were apparently intended t test the significant results frm Chevrn s 4 sil gechemistry grid (fig. 9). The ther detailed lines were intended t test fr ptential bedrck mineralizatin, and fur lnger cntur lines, with wider sample spacings, were intended t help fill gaps in Chevrn s sil gechemical cverage, and t help evaluate the ptential f the prperty verall (fig. 9). Eight additinal islated sil gechemical samples were cllected during the curse f prspecting traverses. As nted by Tupper (0), relatively few sil samples cllected by Slmn yielded gld results abve the detectin limit. The exceptins included a shrt line f eleven samples marginal t the anmaly defined by Chevrn, which yielded strngly anmalus gld and base metals gechemistry (averaging ppb Au; fig. 9), and a string f samples frm the nrthernmst limit f a shrt sil line farther t the west, near, which als verlapped the edge f the Chevrn anmaly (fig. 9). One islated sil gechemical sample cllected n a prspecting traverse, suth f the main Chevrn anmaly, was als highly anmalus in base and precius metals, returning.36 g/t Au,.1 g/t Ag, 3,0 ppm As, 0.71% Pb, 0.% ppm Zn, and 1 ppm Cu. -19-

25 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha Accrding t Tupper (0), rck sampling by bth Slmn in 04 and Aspinall in 1998 failed t duplicate the results fr gld frm Chevrn s trench. Tupper (0) reprted a high f nly ppb Au (with 32.7 ppm Ag). There is sme dubt, hwever, as t whether r nt Slmn s crews, r Aspinall fr that matter, actually tested the Chevrn trench. Fr ne, Slmn s samples, althugh cllected near t r alng the creek frm which Chevrn s samples were cllected (near the nrtheastern margin f the gechemistry anmaly), may well have been cllected a significant distance uphill frm the trench, as its lcatin in Figure suggests. n late July, 08, Richfield Ventures Crp. sent a fur persn crew, cnsisting f ne gelgist and three sil samplers, t spend a day prspecting and cllecting sil samples acrss the central part f the Chevrn sil grid (Greig 08). Over 0 sil samples were cllected, alng with rck samples, and stream sediment samples (figs. 9 and ). The results were very encuraging, and they clearly supprted Chevrn s previus results. Tw pieces f flat cllected frm the main target area returned greater than 1 g/t Au. When the results fr gld f the 08 sil sampling were cmbined with thse frm Chevrn s wrk, the high tenr sil anmaly, with cmmn Au results >00 ppb, and many supprtive +0 ppb values, was fund t be upwards f a kilmetre in length, and it appeared t Greig (08) t average as much as 0-0 metres in width. n additin, the assciated Fe carbnate-silica alteratin system suggested t Greig (08) that it represented an hydrthermal system f significant extent. 7.0 Cnstantine Metal Resurces Ltd. Explratin Prgram 7.1 Sil & Stream Sediment Gechemical Sampling Wrk in was limited t a single day in August, with a fcus n testing the cntinuity f the Chevrn-Richfield gld-in-sil gechemical anmaly westward acrss, where rusty- --

26 6,000 me 63,000 me 6,487,000 mn 633,000 me 633,000 me 6,486,000 mn 6,484,000 mn 6,48,000 mn 6,486,000 mn 631,000 me 631,000 me 632,000 me 632,000 me 6,48,000 mn 6,484,000 mn 6,000 me 6,000 me 7 < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < ,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19,0 19, ,000 Prjectin: UTM Zne 8 (NAD 83) Cntur nterval: 40m metres 00 Trapper Gld Prperty Rck Gechemistry Slmn 04 Au (ppb) Date:19/1/ Scale: 1:000 0 Drawing: S Flasha _Z Authr: Office: C Greig trench (Chevrn 4) grab sample (Slmn 04) flat sample (Slmn 04) grab sample (Chevrn 4) Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha Figure. Previus rck sample gechemistry, Trapper Gld prperty, shwing the lcatin f the tw shrt trenches excavated by Chevrn Minerals and Slmn Resurces. Chevrn Trench Sampling Slmn Trench Sampling flat & grab samples (Richfield 08) --

27 631,0 me 631,000 me 6,484,600 mn 6,0 me 631,000 me 631,0 me 6,48,600 mn ,48,400 mn 6,48,0 mn 6,484,0 mn 6,48,000 mn 6,0 me 6,400 me 6,600 me 6,48,0 mn 6,400 me 6,600 me 6,48,600 mn 6,484,400 mn 6,484,600 mn 6,484,0 mn 6,000 me 6,0 me 6,48,000 mn SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS093 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS086 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS089 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS090 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS091 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS092 SFTLS094 SFTLS094 SFTLS094 SFTLS094 SFTLS094 SFTLS094 SFTLS094 SFTLS094 SFTLS094 SFTLS094 SFTLS094 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SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS007 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS008 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS009 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS0 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS012 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS001 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS002 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS003 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS004 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS00 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 SFTLS006 Prjectin: UTM Zne 8 (NAD 83) Cntur nterval: 40m metres 0 Trapper Gld Prperty Sil & Stream Sediment Sample Lcatins Drawing: SFlasha _Z Authr: Office: C Greig Date:6/1/ Scale: 1: sil sample silt sample Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha Figure. Sil and stream sediment sample lcatins, Cnstantine Metal Resurces' prgram, Trapper Gld prperty. --

28 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha weathering range-brwn and lcally gssanus rck expsures suggested that the mineralized and altered zne was present (figs. 9,, 12, and Frntispiece). This was accmplished by sampling nrthward dwn alng the ridgeline west f creek and alng the western claim bundary, and then dubling back suthward and cnturing alng the east-facing slpe abve the creek, at a lwer elevatin than the ridgeline (an elevatin f between 1 and 00 metres; fig. ). A ttal f 9 sil samples were cllected at spacings f 2 metres alng the sil cntur lines (Appendix ). n additin, tw stream sediment samples were cllected where small drainages were encuntered (fig. ; Appendix ). Neither f the silt samples yielded highly anmalus results fr gld, althugh ne did return an anmalus value f ppb Au, and that sample is anmalus in a number f the ther Figure 12. View nrthwest alng the Fe carbnate alteratin zne which hsts the apprximately 2 km lng gld-insil anmaly n the Trapper Gld prperty. -23-

29 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha pathfinder elements, including cpper, arsenic, and antimny. On the cntrary, hwever, fifteen f the sil samples n the traverse returned Au values greater than 0 ppb, with five f thse ver 0 ppb Au and Au values ranging as high as 79 ppb Au (fig. ; Appendix ). The higher Au-insil values cncentrate near the nrthern end f the sil cntur lines, where the Fe carbnate altered rcks and rusty-weathering utcrps are mst ntable and, it is imprtant t nte, where the traverse dubled back tward the suth. This is imprtant, f curse, because the sil gechemical data indicates that the gld anmaly nt nly remains pen t the west, but als t the nrth. As is clear in Figure, the sil cntur traverses did nt cmpletely crss the trend f the main sil anmaly inferred by prjecting the Chevrn-Richfield main anmaly nrthwestward acrss nlaw Creek. Assuming that the gld-in-sil anmaly west f nlaw creek is indeed cntinuus with the main sil anmaly east f the creek, as bth the sil gechemical data and the altered and mineralized rcks lgically suggest, then the nrthwest-trending mineralizing system has a strike extent which is clearly greater than 1. r 2 km in length (fig. 14). Unlike the 08 data set, the anmalus samples in the data set d nt shw as strng a crrelatin between gld and the base metals, silver, and a number f pathfinder elements, such as As and Sb (Appendix ). That being said, hwever, the psitive crrelatin des still generally exist and remains fairly strng, s at wrst the mineralizing system appears simply t be weakening smewhat, r its cre lies at a greater depth alng this part f the mineralized trend. t is interesting t nte that sme samples, such as a grup marginal t thse which yield the highest gld values n the lwer elevatin line (samples SFTL ), yield very strngly anmalus values in pathfinder elements arsenic and antimny, as well as in cpper. t is als interesting t remind neself that the data set remains incmplete, since the gld gechemistry indicates that the -24-

30 631,0 me 631,000 me 6,484,600 mn 6,0 me 631,000 me 631,0 me 6,48,600 mn ,48,400 mn 6,48,0 mn 6,484,0 mn 6,48,000 mn 6,0 me 6,400 me 6,600 me 6,48,0 mn 6,400 me 6,600 me 6,48,600 mn 6,484,400 mn 6,484,600 mn 6,484,0 mn 6,000 me 6,0 me 6,48,000 mn < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < 6 8 < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < 7 < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < 8 7 < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < 7 < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < 8 < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < 6 < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < < 0 metres Scale: 1: Trapper Lake Prperty Sil & Stream Sediment Gechemistry Au (ppb) Drawing: SFlasha _Z Date:6/1/ Authr: Office: C Greig Prjectin: UTM Zne 8 (NAD 83) Cntur nterval: 40m sil sample silt sample Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha Figure. Gld gechemistry in sil and stream sediment samples, Cnstantine Metal Resurces' prgram, Trapper Gld prperty. -2-

31 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha 6,00 me 631,000 me 631,00 me Au (ppb) Sil 0 t 79 () 632,000 me 6,486,000 mn nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw nlaw Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek 0 t 0 () 6,486,000 mn 2 t 0 (2) t 2 () 2 t (64) all thers (4) Au (ppb) Sil t 3,70 (48) 6,48,00 mn Au mineralizatin trend 0 t 0 (6) 2 t 0 (4) t 2 (46) 2 t (23) 6,48,00 mn cntured Au sil gechemistry Chevrn 3; 0, 0, & 00 ppb Au 6,48,000 mn 6,48,000 mn RMFRE 6,484,00 mn 6,484,00 mn _Z 6,484,000 mn Date:6/1/ Authr: Office: C Greig Drawing: SFlasha Trapper Gld Prperty Sil Gechemistry 3, 08 & Au (ppb) 6,484,000 mn Scale: 1: Prjectin: UTM Zne 8 (NAD 83) metres Cntur nterval: 40m 6,00 me ,000 me Figure 14. dealized trend f gld mineralizatin n the Trapper Gld prperty, based n sil sample results frm Chevrn Minerals 3 prgram, Richfield Ventures 08 prgram, and thse frm Cnstantine Metals prgram ,00 me 632,000 me

32 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha entire width f the anmaly may nt have been traversed by the sample lines. Clearly, mre data is necessary t fully utline the zne and t evaluate the metals zning in and surrunding the cre f the Trapper Gld hydrthermal system Sil Gechemical Sampling Prcedure & Analytical Techniques Sil samples were cllected by digging a hle dwn t the B hrizn using a mattck, where sil was cllected at an average depth f apprximately t 1 centimetres. The sil was placed in standard Kraft paper sil sample bags that were labelled with sample numbers. Similarly, stream sediment samples, cnsisting f fresh silt, silty sand, r lcally silty mud, cllected by hand, were als placed in labelled Kraft paper sample bags. Cntrl n all lcatins was prvided by hand-held GPS, and sample sites were marked with flagging tape labelled with sample numbers. The sil and stream sediment samples were dried, split, and crushed at ALS Chemex Labratries in Whitehrse, Yukn, and analyzed at ALS Chemex Labratries in Vancuver, B.C. The preparatry wrk utilized a -0 micrn screen, while chemical disslutin was accmplished using a fur acid digestin. Analytical wrk utilized an CP-MS system yielding results fr a 33 element explratin package, while gld analyses utilized a gram fire assay with an atmic absrptin spectrphtmetry finish. 7.2 Rck Gechemical Sampling A ttal f rck samples were cllected n the Trapper Gld prperty in, including 7 grab samples, samples f flat, and 8 samples making up a cntinuus chip acrss an utcrp f 24 metres (fig. 1; Appendices & V). The bulk f the samples were cllected frm within the large gld-in-sil anmaly utlined by Richfield Ventures and Chevrn Minerals. Seven samples -27-

33 631,0 me 6,484,600 mn 6,484,700 mn 631,700 me 631,0 me 6,484,0 mn 6,483,900 mn 6,484,000 mn 6,484,0 mn 6,484,0 mn 6,484,400 mn 6,484,00 mn ,00 me 631,700 me 631,400 me 631,00 me 631,600 me 631,0 me 631,0 me 631,0 me 631,400 me 6,484,00 mn 6,484,0 mn 6,484,400 mn ,0 me 631,0 me 631,0 me 6,484,000 mn 6,484,0 mn 6,484,0 mn 6,484,600 mn 6,484,700 mn H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4849 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4847 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4846 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H48419 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4840 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4842 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4843 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H4844 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H48412 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H48414 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H4841 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 H484 Prjectin: UTM Zne 8 (NAD 83) Cntur nterval: 40m Scale: 1: metres Trapper Gld Prperty Rck Sample Lcatins Drawing: S Flasha _Z Date:14/1/ Authr: Office: C Greig Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha Figure 1. Rck sample lcatins, Cnstantine Metal Resurces prgram, Trapper Gld prperty. -28-

34 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha were frm veins and Fe carbnate-altered and silicified rcks encuntered in an area suthwest f the main anmaly, where there had been little previus sampling. Three samples cllected frm angular flat blcks, and clearly nt far frm surce, were cllected nly 7 metres upslpe frm Richfield s sample frm flat that yielded.0 g/t Au in 08, returned gld values greater than 1 g/t (fig. ). Of thse samples, the tw yielding the highest gld grades were cllected clse t ne anther and yielded 6.03 g/t Au and 4. g/t Au, and bth yielded.1 g/t Ag in additin t the gld. Like the higher-grade samples cllected by Richfield, these rcks were mafic vlcanic rcks cut by quartz Fe carbnate veinlets cntaining pyrite alng with minr galena, and pssible sphalerite and chalcpyrite. The mafic rcks were als pyrite- and chlrite-altered. The third higher-grade sample, which returned 1. g/t Au and 96.4 g/t Ag, and lcated nly metres frm the ther tw, was a thrughly xidized and silicified rck cntaining abundant bxwrk and limnite, much like the sample cllected by Richfield which yielded.0 g/t Au. A number f ther samples cllected in this prgram are wrthy f nte. n particular, tw samples cllected frm very angular dcm-scale blcks which were darker brwn in clur than the typical Fe carbnate altered rcks, and which were very siliceus, and which cntained up t % sulphides as veinlets and disseminated pyrite and arsenpyrite, may be significant. This is because the samples, H4846 and H4847, nt nly returned appreciable precius metals (0.76 g/t Au and 7.2 g/t Ag fr 6, and g/t Au and.1 g/t Ag fr 7), but als because they exhibit near-cmplete replacement f mafic vlcanic rck matrices and phencrysts by silica and sulphides. While the precius metals values in these samples were nt as high as expected, the precius metals results, their assciatin with elevated base metals and pathfinder elements such as -29-

35 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha 631,0 me 631,0 me 631,0 me 631,400 me 631,00 me 631,700 me 631,0 me ,484,700 mn <0.00 < < < ,484,700 mn 6,484,600 mn 24m chip sample 6,484,600 mn 6,484,00 mn 6,484,00 mn 6,484,400 mn 6,484,400 mn ,484,0 mn 6,484,0 mn 6,484,0 mn 6,484,0 mn Au (ppb) Sil 08 0 t 3,70 (48) 6,484,0 mn 0 t 0 (6) 6,484,0 mn 2 t 0 (4) t 2 (46) 0 t (23) 6,484,000 mn 631,0 me 631,0 me < < ,0 me 631,400 me 631,00 me 631,600 me 631,700 me 6,484,000 mn Date:14/1/ Authr: Trapper Gld Prperty Rck Gechemistry Office: C Greig Au (g/t) Drawing: S Flasha Scale: 1:4000 _Z Prjectin: UTM Zne 8 (NAD 83) metres 6,483,900 mn Cntur nterval: 40m Figure. Gld gechemistry f rck samples frm Cnstantine Metal Resurces prgram, shwing gld-in-sils data frm Richfield 08 sampling, Trapper Gld prperty ,0 me 0

36 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha arsenic and antimny, and the whlesale replacement by silica des attest t the strength f the hydrthermal system, and t its depth ptential. The eight 3 metre cntinuus chip samples (ttal 24 m; H484 t H484), cllected frm a small spur-ridge f utcrp within the Au-in-sil anmaly, are als f nte. They yielded smewhat disappinting results, as the pyrite-bearing, quartz and calcite veined, Fe carbnate altered mafic rcks returned n gld values greater than ppb Au (fig. ). Tw grab samples frm an area suthwest f the main sil anmaly acrss als yielded intriguing results, as ne, cllected frm a 0. t 1.0 metre thick discntinuus Fe carbnate-quartz vein-breccia zne, returned 0.83 g/t Au, and anther, cllected frm the chalcpyrite-rich part f an Fe carbnate-quartz vein, returned g/t Au as well as.1 g/t Ag and 3.23% Cu (figs. and ). These results, which were returned frm samples cllected ver 0 metres frm the main sil anmaly, indicate that further recnnaissance explratin wrk is warranted n the prperty well beynd the limits f the main target area. Limited helicpter recnnaissance elsewhere n the claims, such as sutheastward alng the trend f the main sil gechemical anmaly, strngly supprts such recmmendatins (e.g., fig. 19) Rck Gechemical Sampling Prcedure & Analytical Techniques Rck gechemical samples cllected in the field were placed in strng, well-labelled plastic bags, which were sealed with flagging tape. As with the sil samples, sample sites were marked with flagging tape labelled with sample numbers. The samples were dried, crushed, pulverized, and split at ALS Chemex Labratries in Whitehrse, Yukn, and analyzed at ALS Chemex Labratries in Vancuver, B.C. The analysis cnsisted f a fur acid digestin with a 33 element explratin -31-

37 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha Figure. Old man (Charles Tw-Pdy Greig) attempting t sample Fe carbnate-quartz vein west f ; grab sample H48414, see detail in fig.. Figure. Detail f chalcpyrite-rich grab sample H48414, frm vein shwn in fig. cntaining g/t Au,.1 g/t Ag, and 3.23% Cu. -32-

38 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha Figure 19. Well expsed Fe carbnate alteratin zne cntinuus t the sutheast with main Trapper Gld mineralizing system and truncated by uncnfrmity with verlying rewrked(?) Tertiary(?) vlcanic rcks; near eastern limit f prperty, n Tw Pdy and Weenus Sup tenures. package CP-MS finish, plus fire assay fr gld f a gram split, with an atmic absrptin spectrphtmetry finish (Appendix V). 8.0 Satellite magery and nterpretatin Based n the encuraging gld ptential manifest in the attractive gld gechemical anmaly n the Trapper Gld prperty, and the relative lack f available alteratin-related gelgical infrmatin n it and the surrunding area, Cnstantine Metal Resurces made the decisin t use satellite imagery t aid in the explratin prcess. n the fall f, mage2map Services f Clrad, -33-

39 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha USA, were hired t acquire and interpret Landsat TM (Thematic Mapper), ASTER (Advanced Spacebrne Thermal Emissin and Reflectin Radimeter), and GeEye images f the prperty. An interpretive reprt was prepared and submitted by Ming-H Du in January,, and is included as Appendix V. The images utline the intensity f lcal irn xide develpment and clay alteratin, and als identify areas f silicificatin. The interpreted presence f eight separate hydrthermal alteratin minerals (e.g., alunite, chlrite + calcite, sericite + illite) were distinguished as well. n additin, ineaments and ther structural features were identified. 9.0 Cnclusins and Recmmendatins The explratin prgram has demnstrated that significant ptential remains fr the discvery f a large gld depsit n the Trapper Gld prperty. The new sil gechemical data strngly suggests the pssibility that the nrthwest trending gld mineralizing system is as much as 2.0 kms r mre in strike extent; it als remains pen t the nrthwest and sutheast. While n systematic gelgic r alteratin mapping was undertaken, ur preliminary bservatins, alng with thse frm previus wrk, indicate that the hydrthermal system is characterized by Fe carbnate alteratin f mafic cuntry rcks, and that the gld-bearing cre t the zne is characterized by the presence f carbnate-quartz veining and silicificatin accmpanied by sulphides (chiefly pyrite), with the highest gld values clsely assciated with the presence f the base metals sulphides galena, sphalerite, and chalcpyrite. As the prgram was limited in bth time and area cvered, the recmmendatins made in 08 by Greig remain valid. He suggested that a systematic prgram f sil sampling, prspecting, and recnnaissance mapping be undertaken acrss the prperty, and that a gridcntrlled gechemical and gephysical survey be cmpleted alng the length f the main sil --

40 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha anmaly. Such a grid shuld have a baseline which parallels the length f the nrthwest-sutheast trending mineralized system, and crsslines, spaced every fifty metres, running perpendicular. The grid wuld prvide cntrl and access fr in-fill sil gechemical sampling, gelgic mapping, and grund gephysical surveys (Magnetmeter, nduced Plarizatin (P), and pssibly VLF-EM). While the magnetmeter wrk wuld aid greatly in mapping, and the VLF-EM may help t detect structures, the P survey wuld be particularly useful, since there is a knwn assciatin n the prperty f gld with sulphide veins and there is a prbable assciatin f gld with silica-pyrite flded rhylitic intrusins (Greig 08) and silicificatin f mafic rcks. This strngly suggests that P wuld be a very useful tl fr targeting larger znes, whether they be stckwrk znes, clsely-spaced sheeted veins, r mineralizatin assciated with disseminated and/r fracturecntrlled sulphides (Greig 08). The P wrk shuld be particularly helpful n the mre prlyexpsed lwer parts f the prperty, in the vicinity f. Given that the Trapper Gld prperty is nw almst ten times larger than when Greig (08) made these recmmendatins, and given that a number f znes f alteratin have been utlined in the satellite imagery, careful cnsideratin shuld als be given t cnducting mre reginal-scale wrk in the next phase f explratin. The interpretatins given in the appendix t this reprt, which describe the satellite imagery, prvide a first-rder tl fr fcussing these effrts, and further stream sediment sampling f the many drainages in the area surrunding the Trapper prperty may be an effective way f supplementing the satellite imagery data. n supprt f bth the prperty- and mre reginal-scale prgrams, a camp shuld be established n the prperty, with mbilizatin by flatplane t either Trapper r Tunjny lakes, and subsequently by helicpter t the prperty. Frm there, the grid culd be cut and the subsequent gelgical, gechemical, and gephysical wrk culd be largely undertaken by ft traverses. -3-

41 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha Fllwing establishment f the camp, supplies culd be replenished using chpper flights ut f Dease Lake, Atlin, r perhaps Juneau. The mre reginal-scale wrk wuld f curse necessitate daily helicpter supprt. -36-

42 Cnstantine Metal Resurces Ltd., Explratin Prgram, Trapper Gld Prperty, by Greig & Flasha.0 References Aspinall, C., 1998, Gelgical-Gechemical Assessment Reprt, Checkmate 2 Claim, Atlin Mining Divisin; B.C. Ministry f Mines, 44p. (including appendices and maps). Baker, D. and Simmns, A., 06, Gelgical, Gechemical, Gephysical and Diamnd Drilling Assessment Reprt, Thrn Prperty, Atlin Mining Divisin; fr Cangld Limited and Rimfire Minerals Crpratin; B.C. Ministry f Mines, 290p. (including appendices and maps). Brwn, D.A., Gunning, M.H., and Greig, C.J The Stikine Prject: Gelgy f Western Telegraph Creek Map Area, Nrthwestern British Clumbia (NTS 4G/, 6, W, 12, and ); Bulletin 9, B.C. Ministry f Emplyment and nvestment, p. Greig, C. J., 08, 08 Gechemical Prgram, Trapper Lake/nlaw Prperty, Atlin Mining Divisin; fr Richfield Ventures Crp.; B.C. Ministry f Mines, 2p. (including appendices and maps). Suther, J. G., 1971, Gelgy and Mineral Depsits f Tulsequah map-area, British Clumbia, Gelgical Survey f Canada, Memir 362, 84p. Tupper, D.W., 0, Gelgical and Gechemical Assessment Reprt, Checkmate Prperty, Atlin Mining Divisin; fr Slmn Resurces Limited; B.C. Ministry f Mines, 81p. (including appendices and maps). Waltn, G., 4, Gelgical-Gechemical Assessment Reprt, nlaw 1 Claim, Atlin Mining Divisin; fr Chevrn Minerals Limited; B.C. Ministry f Mines, 24p. (including appendices and maps). Waltn, G., 7, Summary Assessment Reprt, Tats Prject, Atlin Mining Divisin; fr Chevrn Minerals Limited, Diamet Minerals Limited, and Lightning Creek Mines Limited; B.C. Ministry f Mines, 3p. (including appendices and maps). -37-

43 Appendix Sil & Stream Sediment Sample Lcatins

44 Sample Easting Nrthing Sample Easting Nrthing Number NAD 83 Zne 8 Number NAD 83 Zne 8 Sil Data SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS SFTLS Silt Data SFTLS SFTLT SFTLS SFTLT

45 Appendix Sil & Stream Sediment Sample Gechemical Data

46 91 Lt 9a' ; '- >=' E- -At OF 6 ; + i. - : 6q =fr -q qrld!, u: (D,< Q =. 0, r3 Q D- JO OE O bf Ea?a - - 3: q io O- 3= F, (D (! :r v = A, E A, 3 lds, 2 tct = Eg sd =-\ F,f lf,+\\ ;d\ ;l ql B : e 1\ \ g 6l -{ <plr) )sf9 C1?Zttt Y?s> s=== qaz.n tl{= <trm 32H; NrEZr <m V s8 1 F m FG trr F!n V -lm tt) - { P 0 v =z c) F m z c) v =m-tl n r c) - {t + = =. r J 0, (D gl.l n - pi F, 9, t n 6' (D q =. J J,a' n(d +. :1? r'l A, fp ts+'1, -t' rl:: H-':'X' ia = 2 NE:-" " -{ F; rg *;.p ='.AL, );e. F) 3g.D c 6 3 = c 6- =' t -.D -q JD J nt, =q, - 9) = J ' D rt g n s.zn > dq'- f 3u n '' -O? glc $ ;PA ^a NNE H< N a- PO tu- ( ad el <Fn > z9z! OY PP; m <62. v== --l (){z Fuft (=i r m n-z> -.1 N(J- <rni Ollum s8 VC arlv r?lr.) -tm ltl t-{ f! g (D il CL g >E Ri{ - =! :th ^m x.e.1, \Jr A, <Nq moll vta mh

47 (D.D E t! : - t' '9!, (.D n 3 3 ld f r 0., f rtl T $n A' taa-n r-{-{{ ----r tshfhts (f, rtllr q6qqq BUUW@ 6\Os$ 9999P NNNON d6a6 PP999 $@@ sn Ap:eA ar{-{q q {s@{ {aq q6q6q ATTA -{ r--rtsptshf + -{ -l --l <) trrll WNFO@ $$N@.- *i'6'dij Y:r vrann@.-paaa q@irlrin F9r:{r{9 + -{ -{ --{ -l -rr-r tsfhtsf rttr q@vqq NON@N AOO 99 OJ {!rb {@N AppAA an i!' :{ P P:{:{ rs@ {@6 60N 6666q ittti iil-l+ -r--r HHPHF ttlr qa6@q NNNNts UNHO@ ON@NN s@ 9P99P rq Ae-pA brbr qqqqa nania -{l{j-{ ---rr tsptstsh ttttl 6666q NNN$@ pppaa SHEAg AeAAp ir ir' { q6q66 aniaa -rrrr PtsHtsP tttll 66qq6 tshpts<j ents( +-J-t-{-l <) Y 9biibb ): 9199P qqq 0N@{ dra rs{ qq666 TNAT- aqqqq l{{-{l -TTT- rrr-- FHHHF c) ltttr 6WAAq <) <) 6!6q 99P9P - bbb9b ): sr9p9p Sqq '@bbin- N{rO@ NJ{J iannr -t{{j+ r--rr c) qqql4 9P999 ON O}NAO - -tt'cb ry - lnbinarit {@ i:\-{ NO@Nr N@NO!rq g 3 E a- t' n t= af tr8 s XA'Fil t 9-e,i tb r - =! - E 33=l _r = ets.p q3* * ai f = ba>6 -e f,6 rl J 3 ru rt g l/l!7n > it i, ;H -s9 f = il d- ;94 h etx Fx H<! rr DO x> \ ( a iu OJNNq NOOSS {qr@ a ${Oq 00{ {AOO a 3HSg si N@H: as = EE Fn ō r E 0r_ h 3 { NN-NN brb\\' N{0 4Orr NO@OO a irin\b'b! NNNNN ra ih'{enbt a td'br\b, NNNNN 999PP { s!@ - en ' - it NNNNN j tbb'-id{ N@O@O!- 'qin' papaa d ih ' it NNNNN 9:'P:'9 {N@ 60{ paeaa qini^ a {{ NNNNN AAOOA L is ir id td q6r fr9p99 ug AOJOq eagee!b!{ OOJN@ inbr\i$br {6@ A60d OOJAJ 'brbbl NNNNN an ihi{si r{d@ P9P9P 600q 6SO@O -3 " q et 3-S -f bxl'6 3 ^T -3 g e ^f -E b,e 6 { 9 'n <Frf) a >!! E 6FG i g=> E' fra= 3 F== g 3 Est <Trm x- CDm{ ' r)z> N(,l- (E- CD/m VC fnf rr! _1 m vt - { 0qqs {@N@ 6r@60 OJON@ *s 6J-OO {@@ d';gge a tse n= JT {r@a q 0@{ \60 NJJJJ Nj@r@!nil!r TNNJ 00 J{@ l!er{f} A@@ ONN {@rq a B{8ds {@@ qqa 9PPOP9D 6{O!N N$ r;iu q;; &00 ihj'a{\ a *s t'6 -f! brf6 _,r' = s! 6'a = =gtr -.1 rdo E! ql "g; 3 H>3" S lre - 1n4.;e i-{!x^(! i-f>i' rrr Otb r -F.Dn- FrOh.Li>

48 (D E :ft' t A, ( n 33 l} : r A, : ( 6' =. =n A, (D Ttatt {-t{-{ trrtt 6qq6a 6\Oqs 6N@6 TNAAT c UNFOG P -;'9 {@N@ sas@ a -{S$a i< 6Yj {@6 s\b!\b {NOO@ \ br b'@ ir a@{ ispee 3S P 6{@OO d6& a66q6 NNAT -{{-{-l-t ----r rf a b'@is'at NOJ@O -a@i deb;b {{-l-l-t tnarrrr-- '--A- 9PPPP {{!u@ NjN { -{ --t --t r---r -l rtttt (> NNNNF UNtsO(O 9 :'P jnr inbiriqit SrOOO E@N qnsa@ AAAT {@N a :' t-j r^ ;' ;" drdiq 3s33{ 999P9 N@{ J@N}A -t-t-l-{- (>c tlttt ttaa- r--r lttlt \b'b.iii! 0{@@!r$!r:l!, SON{N a{n Edd:l \ b' L ir' N@OO TAATT {{l{--{ r---- c) OOOJA NO@@@ -@N 6@6 NJOO@ d }JNO {{ -{-lrll rrttt aqs1l c) -T!T rr--- OOJJN 'bd''*b OOJNO ipieb,l\ NOONN ql"es* P9;':'9 {@ru{ $s{@ A, : s_ n a tt c f -gf XFFil r b:r^6.t b: b.) b,*;.6-f -E <* 3=U = *E;E = -f bx6- rl rl J ' r! -l g r/t t7n > gi8; -_ g ; f b' r f = t3 ii NN: H< \ T p > { tu_ r q ri@ 90 bbbbb NsOO{ {@N@ ^-r s@@ NNJJ {NN!O 600! 900 ONOSG NOO{6 'bbbb :ir {{{a 0NA s rlp rr6; NN6@N 6 r6n NO{rO c bi@ - a ;ir$r NNOAO ijq s{r - -:6@ P9999 J ONOON s ;!;i 'aib-b NA@OO NOS v -i6s 9a bbbbrt) {sn $$r T FE =6 -s -!_? NE -r 36 t bx66.t ue!1 ^- -1 t <r-o A >E 29t i?e : E=t E' s,a= e Fe-- i Bq! b (-f, c1 zb N(,l- - Olm-l Ffi 28 vc' mf 4 _tmr') A t-{ s diilp sj@_ NNNNN :'li =@{= NNNNN aaa N$NdO J6{@ { ss=19 60 a NNNNN a NNNNN 999Srp Jr=0 NNNNN 99PP9 NONdO 6NNNO QBE;g NNNNN 9P999 j@@ OJJO{ XJ ea@ NNNNN 999P9 ONN@J r{@46 0{0 AO@@ a@{ NNNNN aa 9PPP9 606{O rt = -E ga Or sf a g ( erf tr -.1 "E; il 3 rqlj E the =l=::e i; (r^ - n Fr *(b XEx^rD -- i-s>; Fl ()rb Vts/F_A' m (f a i-.i ED

49 * lt1 E (! : i- T 0, rcl 6 33 f ( 0, g J ro t a' n a. =: nq, 664q6 A-trN l-.{{{-l ---rr FtststsH c) aa aa {a N6J a -1{{{-r rr--- HtststsH (f ttttt a N q{ q a --{--{++-l ttrrl 666Aq NNNNN 6\Oq+ 6A6qq itna! tsfhhf ttllt 66@66 NNNNF WNHO@ --t+{l-t e aa a e ATT-N --{ -l --{ -{.l ----r tttrr 6\Crq aa e 66qqq intn- q@a6q TTTTA --rr- HtsFHF 66q6q Tntna {{{{-l r-rr- PtsHHH a rtlll HtsHHO UNFO(O aa NJJN aa 6 6qq6q TTNA J-lJl-l ----r PHtsFts qqqqq () Jq@!@ a TTTT- r-rrr -1+-r-{-{ FFtsHH ttrr 666 (> cici PNFNH D 3g ṉ tl a = rqj n A= O - ;frfh Ef ': =6 gt = E crr ō 3 *E <6 r = tse 6 J rl j t! rl g l,l!zn > Xb f O =b ;f8 [ -= 0 sa8 r Hd 6. F?Y a6- ^ar NNE H< \ nr > \ 6 s N 6 NS0 N{ r6 AON@O NONO- NO@N= *s$ee li!tsq tsi -fi Na; lli {@: pf = NE ry6 E { i, r 6- CT EL 3 { <Fr) >!! r)y(, 8R; <62. m,{ F== Hql (rfi CDrn{ nz> Ngl- (!!p CDrm?8 -C lflv r(-) -lm tt t-{ =J!l- N-{.DO.s S "E;!?>S" -:( re s i - n x!x^(d -a;,9 -S>i' lrrc)(b t r f;89

50 6 /D {D lc tt (! =i' -v A, ( 33.} r s,a' rl a' n=r 0i TANA -{ -t -{ -l -l -rrrr tsffhh ht,\tt ANNN\ 6!0 e99ae! = {abi in br in ir +brititbr AJ{6@ qq6 uu;i!= 6O qq66q TT-A -rrrr FHtsHH qqw6a TTATT --r-r FPtsHF -r --{ --{ { -l --{+++-l qa@@q ttllt qq@6q ttrtl \\!\6 6\Or a btrbfpie S@ Apppz HHHSA sr9999 6@ s@s {rsq PA99A SeHSg AAApp iiinirq@ 9!rP!nd AA@6:. N@ u:i {: aae qq6qa at-an ----r HPPtsts --'l++--{ ctct tttlt wqqaq ir ie ir ir ir a@n bbbbb a is i! br br t OJOJ@ q6{rs q{nrn -tana -{-{i+-l f---f c)<) ttltt 6\OqS S'9PPP 9PSr99 a qqq tr in i.r ir ir 6{OOO b'- l b's JOq@@ _.t i@n 6000 qqaqq nraaa -l-t{-l-{ tsfhhts -f--- tttll 66qqq 6NON$ 9bbbb!:? f 9P999 qqq q {@@ r*s3h OSNON {AA a nnnta + --{ r-rrr-{ -t -{ tshfph ttllt sss 6!OSA id i,r ir ar is sns@ P99AA gsghh sqq bbrinbid 66{OO ilsps* N@q a6664 ann-a -lj-l{l --r-- HHtstsF qq6qv ttlr P9P99 ANNON sn AAppp HH3*: AAptr.' irrirr@{r inb'@ls q-.${r D 3g 0 n tt c J tr3 c XFFil 6< 9-QF 06 0 * F! - E e3 - i P; >+ -3@g 3 f bx>,6 *T -i )a T E F6 J =' J D rl _ t'l!zn > 4H n 'j <9 ; 83= F Pi h. 6 X ^r:r NNE H< \ p!r > \ { t_ rcl q F' d 3 P9tr9i qqa@! SA-A' JJAOO ''F in i'q r '{bbb, u$u$s r \ b, b' br as 9999P NNNNN aaaa \{\ida' ro@@s 999P9 qq JJNNJ NO{GO -- ir in' NNNNN :. in b, i '* {00@ PC9S:S) 6q NN;ON r@n$ Apps'A br' NNNNN raqn 6000 ir in''q tt NNO}N {@qa NNNNN r@ qq6q -f {@-; 999PS) q@{ -ANSA raa OO{JN 9P9P9 NOOOq r brin'bb' 9PP:'r' O{@NJ r@jo AAsj- '6'6-q O@NNN {{}sn -r ;=6e ct = 3-U = E*Sta pe i -3 as _r *el'6 + T' <Fr) fr n?e d. leg - E=t r' E =6= ;=) g qur" ; D, 'j-{< <Eil - CDm{ r)z> (!!p \8 N(,- O)^.m VC fn- 4r) _tm t1 r -{ (7.*Hsa; srfnfrll {J OONOA sa6 AOOO@ ioor-- { qqsa trirbb'@ {N@O isids N{EiEi{ N@NS@ 0J@r ipe NNJJN s\$qs isss $@{ a@q r@@@ ^r-i-i d600s OOSNA {0{ NP PPPP :-@ ti@@ digas 3E;@@ i ixjs P3f'9i. d!@{ bins{ -f -:Qd tse Lr ^T X! f bxj6 = ae 'a g N-t rno E!AT \JC.- >P 6 +F 3 fr>s E -:lcl rh g =l=::! i:h^^o 6 +(!t ^ -.* X'sX^.D -S>i" rnotb m6.l-r> -Ptt ^-'

51 (D E i'! q, (,D 3 3 (D f { A' 4 t ( 6' f. n=r, n-nt! -J -{ --{ { -{ ---rr tlttl 9 P!:'i frna a j{q sltl 4.1 t, 1 a qq@q6 \N\\O ANHO@ S1 r':'9 a!n :' :'a 9 -i-:! E8H3E A P;'9 P {{r{! TNNAT --{-l{-{{ --rr trrlt qqqa6 T-TNA -rrr- HPFHH trrtt 6qvq6 -l+-{-l bb:-'@in {@rq {{{@- -66 r6000 b'@b{it {6A@{ -r-rl{-l cd6u UNtsO(O 1., ls 9:. a6 P:':'19 AO q@q 6NP6@ {xn@ vq a ir{l:-{ 0@ qa66@ NTTii ---r- PFFtsH q6qqq tttll qq66@ ntnta ---r- HFtsHH rtttl 6@qqa -r+l{-l NrdOO s@ ;l $3{ A-A-1 rra bttarbr' N t-rtt -l-'.lll{ r-rrr PtstsHts ct ttltl 666@6 uqqqs r a J, NNJNN r $r 9a P9999 nta-i + -.{ --l -{ J ----r (f, ttttt !Ou jn rja{o 6 :' :. 1.9 l.u :. N{S! ONOON a p AANT {{++-{ r---r qq6q6 ltttt rr ' b, '@ :. a OONNJ qaa@ {s{q gr$mb P 9 9:'P NfOO{ sl@@!, 3g : t =J Fgt XfrFil Ar b:r^6 T = 6E r0 bxf6-f!-t '3t q 3fu bxf-f TJ ' 0 rl g t'l t7n > es- fi f au a) -_ P ii NNE H< \ SO n- x> \ N ;" ro 6- d er h 3 H$ua pdlsj ir6! rndh 999P9 AA*4.!{l xnn{ 6rNO a0s 9P {q aq Nlr N\O N@OJ}{ s dis-b @6 ri=fii *Nr "igges NS--d --AAi {dn@{ a bbbbb 6-AA- ssn0 NO{O@ an@{ OASJN dq 'd@s JJSNS 'N-A\ =r@ s Ssa-a a irbbbb GSs@ djy' r!u{n $:$gs N@{$ i< rt = f -'s E: - 6 -ta -! 36 f bx 6 = -P Sd -l.l, <H(.) d >!! E 1 =AA Pr; ;' 36= ;1= J< Q EUrf' ::= F O)m-l OZD pqr (mi F;yr i8 vc' fnv _tm tl t1'! r) r{ lw NNNN aa irarlir'$ NOj@O N N NONN r${a NNNNN PPP99 NNOOO {N JJNJJ N6N i;;;'h NNNNN aa 6{{d {NSO ;ts {S@i NNNNN 9000a 9PP99 NN@{O NNNJ ar *FsEs NNNNN irlididl q@{ NNNNN 999PP {{N0 {{{ 0{@s NNNNN a P99P9 NOO{O NOOO@ R3*\d NNNNN Qa 9PP9P SNOOO f *E Kd T *P9n.T BE f 6 T T = brld f! :r F"' *.tt 9) "E; r P-}; -lll re 3 - -rj.rv ;Hgst H!x^(! E-S>; mtb FH.! n' mou.l-.icg

52 * 6 tarna {J-l{-1 r--rr \\n\\ NT-AT --{ --{ -l t-- trrll Nts!\\\ -AAT l{+j{ -f--- <) qqqq6 rltll AT-TN.{+-l{-l ---r ttrrl 666qq Tnnna --{ --{ i -{ (> ttrtl 66AW6 qququ 61ctl q S NTTTN -{-{l-{l -r--r {{ll{ r---r tllrr ATTTl -{-{-l+{ --rrr D 3g! a a rl J 3 D rl 1 E f * x! A, (.D n 3 (D 3 l ro $, 4 ( T 6 d. =r!, (D a 6a 6drSl A 4 a {{{ N a!sn a@ s@ N{N$ s NJ@@O {@Nrq -i<< -{@ 6000 eaa NNJNN N NN@N SdeSi a a NNNl\' OJN6 N{qa a N N J@NO {60N q@ e sssag -Gf ;FFil c f E l EE N 3 +l <6 = =* fr!t. ō n E7N > aqe t =u n ;s8 [ Or= ^-T Nn: ts< \ at g trcl d 0, 3 -{ <rrf) >!l z.?z ny(^ gp; <61 m v --l H$= = (=m CD rrt.z> -l N(Jr- (mi F;n 38 vc. fn;l, rlr) '-1 ltl r { T 3 g ii{ r! *t D, "E; *!?>J E f;e = l = ::'tt : H g+e X'X^ 's>i" rflotb fi3 9n

53 f a i' 'lt D ( n 33 a r D, s f ( J-.D t. 6=r p, N --{ r- -t <) t r( 9P Ap Hg 99 q@ $ {?TTTN {{-ll.l rr--r Q rtttr i! ir b ir'n NS$OO 9S'AAA Hggi;H 99Sr99 qqq q :- b i b, {s{ N@@ qn:s TNTT- -{ { -{ --t -{ r--rr 6{Oq} i, tr i i, it NNO AAppp Hg g qqq {@{ \irbisi rqs N@N}O a NTTTT -{-{l+{ r---- P9999 NO@@ PPPPA! NJOJ: -@H P99PS) { birq\i r@ {NONN 6{6S ONO@N N{@J@ D 3 E 6- =tt c = -qt Af ;FFil - a= 9=Q E d d r - F! - b >i, 93-3 _4 3E e E r = b:r1.6 -E ra rf EE gn r J ' 0rl g U!7N > eq3 6 Jeb -_ P ;sh d r= F h NgE F< \ -x p x> - N 6 b_ r 6- (t q, 3 99 {@ NN L- 9St 60 JN { a in i.n in i! q ra ar \b,\aie ON@N J bihiritb, N@SJ P9999 q NN@O rno@@ $u 9 :' :.!e l.t $s@{ ir tr ir ih i! NNNOS J{@@ = -= "'J E 3 -'U = b :R Ltd = t ^E - ;E -E e^f = *Et'E 6 -{ 9! <tsr) E lsg fl n? - EH' ;' s6= E ;=i i H$l N, <Efr F Ctlm{ OZD Nt2l- (!!p O)^'m 38 vc' anid 4r] -t rn vt - { E@ NO {ONA 0q {rn irbinsb, ON@@J NNNNJ q{@ 4@N easde Sqa ilbirb JNNNN SNANO aa = _r *e t'6 = b>sja = ae g a T er N-l rdo erd "E; * 3 P.>S S lre - -rjr.v x!x^(! :HE+E i-s>; mtb f,s;

54 (D E (Di'! OJ n 33 /D 3 r 0, *t ( = n.d a. =! st * TT {-l -- tl NO {a NN OJ brb AO 098 6B nnaa- -{-{{+l rr-rtstsphts tltt 666q6 c) :'99Pi' r@@{r N{@{O iidbra, {sa is-i -<EE9= Tnt-a JJ-l{-{ r-rrr <) ttlll aqqq@ 9:':^;":' 00 q{ :^ ;'9 sngaj -A3s aaaat -.t -J -l J -{ r---- J ro@o AOJOd i, - ij :. ^_-i gnts3b!, 3g n t f c -Lf 6 ;rfil r = bx^6 T e i-6 -T b x-= - 6 = 3:!J g -f *E EE J 3' 0 i g, ul!7n > Xb 6 f Cu al -_ ry ;sb'd 0= O }P N8 H< \ n- OO x> \ s tu* r tt qt_ P9999 {ONN@ {0{ blsfn 3 NO N! NJ {q JN ON P @@jj rr$ N@@O@ NJNAO ;l a s@ vs dd'sh* NJX 6v :@s bbbbb {s6n $$ - ' z* 3 -'g _r = HE! 7i -r -E #E T 6x qe!2= = -{ <F 249 f.)?ln Es* S=l Hq! (rf, Ct't m { r)z> N (fl- <m7 CDfrrr 28 vc. rnf r!r.) -1m tt t-{ N@ NO { NN 6{@ s@@ JJAJAF NNNNN 9P99P AOONA fn@@n {@40 iperi Fv- NNNNN NS N@@ r@r@ NNNNN P99P9 JNOqO f *EK6 d st *P?ō f 3 bnl6 f! t lr F+ t!o *.t' DJ "E.!c23 T E f;e = i: (ra =::El - n+r:h mo(b =-J> -HrD A' m0.l-itd

55 * td E lj (D f sx tg, tc) a, 6 33 f (!, a =' r = =. =.r g, trt +-t r- -{ -{ + -l --{ rr--- <) tt ttttt (@ ((@ ds {ONJO { 6{OOO N-TTi {-lll-l r--rr ttttl 6@@60 6\U aaa NNN r6060 at-r- -{+-{l{ r---r HHFtsF c) tttlr 6q66q a OAA{{ s@qa{ a i-ir YO:i@A D 3g na tt c J -qt xa;il = ee rc E'e E -: <- JE = =E =a?.t Nq ry= -J j' 0 rl g tf!7n >?ts t f ;H n " -O = - K f = 6:4 ^i Nn: H< \ PO n- x> \ C t i', ro 6- q P 3 { <r(1 >!! z=z r.)y(/r PBi <1 *==- Hqi (,rm Orm-t r)z> l\j \., Sfi 38 VC fnf rr) -1rn alt t- + 3 =!, ill q9 E!!r "E; il 3 HS -li r re 3 i - n X!X^.D -a;a E's> morb r f,3 9

56 Appendix Rck Gechemical Sample Descriptins and Lcatins

57 Sample Easting Nrthing Number NAD 83 Zne 8 DESCRPTON H Fe-carb breccia - structural zne in creek - within dense FP prphyry basalt - chpstick prphyry H m bulder f siliceus breccia with Fe-carb matrix 1% py H hematite-limnite-silica-fe cb alng fracture (frc/vein=88/087(dip directin)) H cpy-rich part f Fe cb (subrdinate)-qz vein (phts), 0. t 1.0 m thick (lcally) and expsed discntinuusly ver - m; cuts acicular fs prphyry; vein=/44 (dip directin); hand specimen cllected (HS 14) H silica-pyrite rich part f same vein as sampled in H48414, apprx m t NE; sme dark grey quartz (py-rich) and sme well-develped quartzlimnite bxwrk (HS 1) H cm thick grab frm py-silica-bearing vein-breccia zne (4/37=Vbx; dip directin) H vuggy quartz with thin streaks f sulphide at east edge f m wide quartz vein H start f hrizntal chip line (east edge) alng tp f small spine abve strng gld in sils - chips all 3 m in length - this sample md green and lesser fe-carb altered w/ pyx phens - wk-md perv fe-carb altd carse baslatic fragmental H m chip - pervasive fe-carb alt'd basalt fragmental w/ mm scale carb +/- qtz veinlets, 0.-2% py H m chip - pervasive fe-carb alt'd basalt fragmental w/ mm scale carb +/- qtz veinlets, 0.-2% py H m chip - pervasive fe-carb alt'd basalt fragmental w/ mm scale carb +/- qtz veinlets, 0.-2% py H m chip - less pervasive fe-carb than H , and mre friablwe alt'd basalt fragmental w/ mm scale carb +/- qtz veinlets, 0.-2% py H m chip - less pervasive fe-carb than H , and mre friablwe alt'd basalt fragmental w/ mm scale carb +/- qtz veinlets, 0.-2% py H m chip - stubby FP in an aphanitic matrix. wk t negligible and n bvius veining H end f hrizntal chip line - 3m chip - stubby FP in an aphanitic matrix. wk t negligible and n bvius veining H flat f thrughly xidized siliceus rck, frm lse rubble near base f spine f utcrp paralleling part f gld-in-sil anmaly; abundant bxwrk and yellwish t brwnish limnite H flat frm lse rubble near base f spine f utcrp paralleling part f gld-in-sil anmaly; pssibly siliceus high-level prphyritic intrusive rck r perhaps silicified mafic (pyrxene-phyric) fragmental (actually almst certainly the latter); cntains mderately abundant "replacement" disseminated pyrite and arsenpyrite and lcal veinlet-hsted sulphides in amunts f up t apprximately %; very siliceus; darker-brwn weathering than typical Fe cb altered rcks; LKE THS ROCK VERY MUCH! H flat frm lse rubble near base f spine f utcrp paralleling part f gld-in-sil anmaly; mre r less the same as H4846: pssibly siliceus high-level prphyritic intrusive rck r perhaps silicified mafic (pyrxene-phyric) fragmental (actually almst certainly the latter); pssibly siliceus high-level prphyritic intrusive rck r perhaps silicified mafic (pyrxene-phyric) fragmental (actually almst certainly the latter); cntains mderately abundant "replacement" disseminated pyrite and arsenpyrite and lcal veinlet-hsted sulphides in amunts f up t apprximately %; very siliceus; darker-brwn weathering than typical Fe cb altered rcks; LKE THS ROCK VERY MUCH! H flat frm lse rubble near base f spine f utcrp paralleling part f gld-in-sil anmaly; dead-lking white cm-scale cc vein with Fe cb altered wall rcks and lcal (islated?!) Cu-stained (malachite r chrysclla?) subrund "pebble" (?!) f unusual appearance H flat frm lse rubble near base f spine f utcrp paralleling part f gld-in-sil anmaly; weakly silicified (siliceus) mderately pyritized (up t 2%; sme aspy?) rcks; mderately limnitic (less silicified equivalent f 6 and 7?) H flat frm lse rubble near base f spine f utcrp paralleling part f gld-in-sil anmaly; <1% pyrite in variably qz-py veined and altered mafic(?) rcks (HS 0) H flat frm lse rubble near base f spine f utcrp paralleling part f gld-in-sil anmaly; even less pyrite than H4849 (nne?), plus lcal silica in variably Fe cb altered mafic(?) rck

58 Sample Easting Nrthing Number NAD 83 Zne 8 DESCRPTON H flat frm lse rubble near base f spine f utcrp paralleling part f gld-in-sil anmaly; qz Fe cb alteratin and veining (typically <0. cm) cutting mafic(?) rcks, with sparse but cmmn assciated pyrite (HS 2) H flat frm lse rubble near base f spine f utcrp paralleling part f gld-in-sil anmaly; mafic rcks, still green and relatively unaltered, with nly lcal qz-cc-py-gl veining H flat frm lse rubble near base f spine f utcrp paralleling part f gld-in-sil anmaly; qz vein with very minr pyrite; up t -7 cm thick and cut by mm-scale Fe cb veinlets which are mre r less perpendicular t the qz vein SFTLR Grab; sample taken frm cm wide gassanus zne in rusty area; mm-scale veinlets and seams f aspy? and py; Fe-carbnate alteratin? Finegrained vlcanic rck?

59 Appendix V Rck Gechemical Sample Data

60 4 L' -4 g6' -1 d+ 6-6 '- >=' _A' 6- (b EV.DE O * + :. - 6= pts ^ TO_ sr <a!, cr: -< Qr e+ t n=. -JOD' q-? Nrgzl- 0r- J6 OE O b;l E= P+ a- - a1 q -n ao Oa E= 0, (D 3 q v c A, g A, 3 lt 6- p, 2 ( E c,''t; g" =-\ ail Ftt\ ;l ql B ;l D 8l { <r-dcl 2479 O? Z.tt g*si *=== qu=e 'l{< FEfi"T <m V Al 4 m s8 vc m2 tnr) -tm Vl t- { ><< gemm lllr $EE >@ C-a@ s33* l;;= riaiae!.d : PE'F3 lrac a =-6 A, = sias ^'f, FsF r> Rs *iff ;>> Fss r n (, m g (^,'ij -J z. za{f c =m z -.1 z { r) 't, v r) rtg vfl tt U v =z ct v rmz c) v =r r(] n rf) T { (D = (a =. = J gr (D 9, at n.d 0 q d g p.t p 9, A 9.!, 6 - =..6' n D 3(1 0, J? O+-93 -=. Hu. ;' rrel :r' " A 'i,d T = " + -Jq Nd -.1 0j A' iv E ea; e -ao_ H+ -*' ' *.0. EN J 9 c tt3 ; ld c il 6 =' ;r.d -6 JD J (-) FT 3 9J 0, see996= *AAE$ UEE(1 a6v E c c \'='0J FAAi:aE q ^i'ii'='e Q J { ;-g Fg:sFE ='l q '-f.l+ tij a6+9tpf. f$e-h?e E r. A,;; 6,; '= =S 3A JO - cl m g m 2 E-{ z ltr! m.9 vtrl! v { z rl ) ', r!.t n t7n > eq c J Cu fl '. 3qg'$ 'n = +P r Pd 6. m?x 0- ^- NNE H< \ ar g x> O { i, rc) a(t A, h 3 { 9 <Hr) >82 Y ^rje3> <a4 *ej 8q3 (rf; Cnm{ r)z> N('- SH 28 VC f'dv rq -tm tl t-{ =J g F',D ct (f >E i'{ 0- :6 nth l-j!! (Jr O) <Nq mo!? F? mf

61 ..,1 r v $$ 6@@ $@NtsO T $$$ --- $$ 66@@G &$+ -- as$ (e! --T- $S t, 3g n tt dj rqj XAFil b P N P i L, i, ir 9s99 NrhEE :"66sA s:rrq'6 JJJ@] j 6JNSJ r b' b ir'q N@{O N$ P9!rr{E s-nb, tt tr 1" :.!e &@{{N N@@@S AAeAp bbqbq 8363= 9999P qq!n!tl:' Asppp 000 =r@@ Eia@- - ' in "'l in bl :r!, :r :r :' rd)n@ {N@AJ PgAPA FAAA y@!iniri! P-Q; 06 - F i! - r ge EE -r = 3i E its t eh n ;f8 il r= il -Pi b. :: 0- ^-a ts<! s: rr PO x> \!s { a { N JNNO@ ir ir b in'@ 00 rp*- AJJ--N a@x " $ 6{J Y:{N - -{d@@ rv 6 sgbbh 9Jf!'!' a N!$N9!' 6{@d@ {rnn -rsg$ SBesS rons b$:-irb 600 f = blr>n- -E r a.t N & b. ro 6- cr OJ f q AA ^ y irinirir PSr999 qqa 9PP99 q6q AApAp irin'q = 3E FE -l 9 <Pr. >! NNNNN ieql:.\ as{ LSti'; SESd*f NNNWN NJNJO 9 te;' A NNNNN Sq b :. ir:. s {{@ b'ininain 6@SET ''NNNN {600 A'-s"AA innirir 60r-.b@u' N*NNN 99!'PP rn@ {NOO - inlnqit J@NJJ 90@ 3 f b;rl'6 3i RE!-r = -: t'e =aa PBi <a1 S=l r) Puft (rf, { z O) m r)z> -{ Ngt- (mi F;rr i8 vc. ttr qf -tfi tt r J :{ q! *-f RN3= eshaa N{{O@ J{ ieid- 338 r{:r } NrOOO N${O@ - - -:SSi F i\3!i sr!r!n :{ N9@JJ a E$Sta 9!r {s; 9!n9r.1.) OOJJN JONO@ 36- ON@NS ONqN ierds sr!d,(r!n N@N@O NOO{@ u sf *E t O s ^T = f bxjn- = b'6 ō f! : P. il'-{.do -6 >E+ 8N; O -rct rb 1ffi;i - eiss mo # ;

62 n -{ ō v(f A] N] N $ N N N s { N e 9 q -:f, l ir b b L'-l 6N!@! 33-3-l *-.-*l --rranl y-r66!rl H3a63l A A ANA {@@} NOO{ JlYN 0{@! 60$r Erg e,{q NNNNN c PPSTP 66N ""=l :::::l ;_l "^"""1 P9PP9 NJNNN rr@ a 83qHs jrno b:.b'nt! { N.S3* NJNN.- NNNNN aaa Q NNN rnoso ---:rr 6@@@6 $$ tshfhf cr qa@nf 1$i{!rN a@@ NN a {NO@ eddd PdNO P qn $$ 6@6@ SAA$ ss ilt -l -t -] a r6{r ajnorn r$@ {a Ns00 rsll NJJJO {u {NOq AA AN NNNNN ac NNNN {{ =""-l ::::ll 0 a{j{@l { rl NO{tq a)" BS$.; PP99' a3--id \a\--!d NOOO= {@ NNNNN JJJON r{ --- $$ 6@6@@ ss$ l l qa@nf rr irb'n\b 6!{N AAAl.A OAJJJ '-tr'{l rq@@ 3E$$s da-a 99.P9 AOJAJ A{@N@ Nj{OO 6NOqr b'i,rblb NJ@N 3B-66 ;ii NNNNN a = tt rt 0 n f tt 43 ->3 ht- X*-Fil t b;r^6 = EE T 3 E"'H -E =$ -E;E -f E = -f bxf- E!t tt b: En 6 L- l< t-t l-e3fi l l= lbx-6 l= l: l-s*e t: lt t: l-s - E l-e s t: l*e=e "= t* rl J 3', D -l g U + ql E r9' F.D t n aq c -7N > r!!u n!? i- 3 ;d'l r= s -Pi L ezy ^rr Nns H<! _T p >,\ \ N 6 { tu_ ( 6- cr t- 6 3 { 9 <r-o 2Q2!/ur PBi <a4 m F2= --l HT! (rrf, dz> CDm-{ Ngr (m-h 38 VC?fl v rr! n tr 3!r il-{ l!o -tm v, d >E+ i?; O c;^rd -ro 1T!'l = ;S*E gisl m Fea' rrr O ii (t,

63 ! -1 r O v QOOOO ,qA s -:ls -Na q --r-- diidq {{@ a q. 2a- R 6e; AJ - EP' il' s.= T- $$ &@@@@ $$S tsfhtsf 66@66 $antso S HHtsHF 6 U@Nts aa s8s;d --:ET 4S 66@@@ $+$ aa \i3d3 a eudid D 3g g a tt 3f FLf 6 A= D + -f:6 cl!! -l ō -q si.a6 =!l -E <6 E n J ' D rl g n lzn > d9 l4u t" n '' -O a 39c F Pi 6- NE ts< \ nt $ > \ ( & {$daq N6@ry d{{n- ssddd a\sil$ N - r.*! F 9:R!-'9 F!,1 N h, ro 6- tt 8r 3 -{ 9 3 <tsr.) ci >! P '-1; { xff; - 'lj-r< s, F <!m CDm-{ OZ}. 3 Ngr.ci (trp -;' CD'M n38 :',C, fn7 _tm rr!r) J1 t- -{ P 3!l tr{. a-fr >Eru 8't? ; -lcr rb - ;-H-E!isl m f;9

64 Appendix V Satellite magery nterpretatin; Reprt by Ming-H Du

65 Memrandum Ming-H Du President/Cnsulting Gelgist mage2map Services, nc. 704 Newhall Drive Highlands Ranch, Clrad 0 - USA Tel: (3) Fax: (3) ming@image2map.cm T: Frm: Subject: Darwin Green, VP Explratin, Cnstantine Metal Resurces Ltd. Ming-H Du, mage2map Services, nc. Satellite imagery interpretatin f the Trapper Gld Prject Area, Nrthern B.C., Canada Date: January, ntrductin On behalf f Cnstantine Metal Resurces Ltd., three types f satellite imagery data were acquired and interpreted ver the Trapper Gld Prject Area, Nrthern British Clumbia, during the interim September t Octber 19,. The satellite imagery data included Landsat TM (Thematic Mapper), ASTER (Advanced Spacebrne Thermal Emissin and Reflectin Radimeter), and GeEye. The Landsat TM data was interpreted fr ptential ccurrences f clay and irn xide alteratin. Lineament and circular features were als interpreted t delineate pssible reginal structures. The ASTER data was interpreted fr ptential ccurrences f seven alteratin minerals, irn xide and silicificatin. n additin, lineaments and circulars bserved frm the ASTER data but nt in the Landsat TM were mapped. The GeEye data was rthrectified and gereferenced t prvide a detailed base image map at 0-centimeter reslutin. Table f Cntents ntrductin.. 1 Table f Cntents.1 Landsat TM Data.2 ASTER Data 2 GeEye Data 3 Figure 1 - Landsat TM False-Clr mage..4 Figure 2 - Landsat TM-nterpreted Clay Alteratin Occurrences... Figure 3 - Landsat TM-nterpreted rn Oxide Alteratin Occurrences.6 1

66 Figure 4 - Landsat TM-nterpreted Lineaments and Circulars...7 Figure - ASTER False-Clr mage.8 Figure 6 - ASTER-nterpreted Alteratin Minerals Occurrences 9 Figure 7 - ASTER-nterpreted rn Oxide Alteratin Occurrences... Figure 8 - ASTER-nterpreted Silicificatin Occurrences. Figure 9 - ASTER-nterpreted Lineaments and Circulars...12 Figure - GeEye False-Clr mage. Raw Data Landsat Thematic Mapper (TM) Data The raw Landsat TM data utilized was part f the Landsat Path 7 Rw 19 captured n September, 199. The data was dwnladed free f charge frm the USGS EarthExplrer site at Data Prcessing and nterpretatin 1) The raw data was reprjected t UTM Zne 8N, NAD83 datum fr all TM bands except band 6 (thermal) which was nt utilized. 2) A false-clr 742 image was generated t prvide a backgrund imagery fr the entire prject regin. The image is cmpsed f TM band 7, 4 and 2 in red, green and blue clrs, respectively. Clr and cntrast enhancement were perfrmed t highlight features in the image. The false-clr image is attached as Figure 1. 3) Ptential irn xide alteratin was interpreted frm the TM data. Three levels f intensity were delineated: weak FeOx, medium FeOx and strng FeOx. The FeOx alteratin was verlaid n a gray-scale image as shwn in the Figure 2. 4) Ptential clay alteratin was interpreted frm the TM data. Three levels f intensity were delineated: weak clay, medium clay and strng clay. The clay alteratin was verlaid n a gray-scale image as shwn in the Figure 3. ) Structural interpretatin was carried ut by delineatin f linear and circulars features utilizing the false-clr 742 image as the base. Manual interpretatin was carried ut fr structural features ptential related t gelgic faults and cntracts. The lineaments and circulars were verlaid n the false-clr image as shwn in the Figure 4. Raw Data ASTER Data The raw ASTER data utilized was part f the ASTER scene captured n September 14, 06. A full ASTER scene cvers an area f 60 by 60 km. The data was purchased frm the ERSDAC (Earth Remte Sensing Data Analysis Center) ASTER site in Japan at Data Prcessing and nterpretatin 2

67 1) A false-clr 3 image was generated t prvide backgrund imagery fr the entire prject area. The image is cmpsed f the ASTER band 3, 2 and 1 in red, green and blue clrs, respectively. Clr and cntrast enhancement were perfrmed t highlight features in the image. The false-clr image is attached as Figure. 2) Ptential clay alteratin was interpreted frm the SWR (ShrtWave nfrared) prtin f the ASTER data. The interpretatin includes delineatin f eight ptential hydrthermal alteratin minerals: alunite, chlrite+calcite, sericite+illite, jarsite, kalinite+alunite, mntmrillnite, kalinite and smectite. The clay alteratin minerals were verlaid n a gray-scale image as shwn in the Figure 6. 3) Ptential irn xide alteratin was interpreted frm the VNR (Visible Near nfrared) prtin f the ASTER data. Three levels f intensity were delineated: weak FeOx, medium FeOx and strng FeOx. The FeOx alteratin was verlaid n a gray-scale image as shwn in the Figure 7. 4) Ptential silicificatin alteratin was interpreted frm the TR (Thermal nfrared) prtin f the ASTER data. Three levels f intensity were delineated: weak SiO2, medium SiO2 and strng SiO2. The SiO2 alteratin was verlaid n a gray-scale image as shwn in the Figure 8. ) Structural interpretatin was carried ut by delineatin f linear and circulars features utilizing the false-clr 3 image as the base. Manual interpretatin was carried ut fr structural features ptential related t gelgic faults and cntracts. The lineaments and circulars were verlaid n a gray-scale image as shwn in the Figure 9. 6) The interpreted data was reprjected t UTM Zne 8N, NAD83 datum. Raw Data GeEye Data The raw GeEye data utilized was part f the GeEye-1 scene captured n July, 09. The data was purchased frm the emap nternatinal, a reseller f the GeEye Crpratin based in Thrntn, Clrad. The GeEye-1 data purchased cntains by km cverage. The purchased data is a pan-sharpened, 0-cm, 4-band, rth ready standard prduct. Mre infrmatin abut the GeEye-1 data can be fund n the cmpany website at Data Prcessing and nterpretatin 1) The raw GeEye data was rthrectified using the ratinal plynmial cefficient (RPC) prvided in the data and the digital elevatin mdel (DEM) raster data derived frm gridding the tpgraphic cntur data prvided by the client. 2) The rthrectified image was then gereferenced t imprve accuracy using grund cntrls pints (GCP) frm the drainage and rad vectrs als prvided by the client. 3) A false-clr 432 image was generated t prvide detailed backgrund imagery fr the entire prject area. The image is cmpsed f the GeEye band 4, 3 and 2 in red, green 3

68 and blue clrs, respectively. Clr and cntrast enhancement were perfrmed t highlight features in the image. The false-clr image is shwn as the Figure. 4

69

70 6

71 7

72 8

73 9