0 10 metres TECK EXPLORATION LTD. K A M L O O P S, B R I T I S H C O L U M B I A FIGURE DRAWN BY: S.A.SCALE: 1:200BY: J.Pautler Ten Mile Creek Property VAL CLAIM GROUP Trench 99-1, 00-05a START 0m 80 o 053 o 30 o 2 lim, sil, well fract 2 s-i sil vn’lets to 5 cm 2 s sil 10m 20m 30m 40m 2 m-s sil 60 o ? o 2 i sil v fract, lim folded 1 water qtz 80 o 30 o 80 o 20 o T5A-1 (<5,<0.2,<5) T5A-2 (200,<0.2,<5) T5A-3 (<5,<0.2,<5) T5A-4 (5,<0.2,<5) T5A-5 (<5,<0.2,<5) T5A-6 (5,<0.2,<5) T5A-7 (<5,<0.2,<5) T5A-8 (<5,<0.2,<5) T5A-9 (<5,<0.2,<5) T5A-10 (<5,<0.2,<5) T5A-11 (150,<0.2,<5) T5A-12 (<5,<0.2,<5) T5A-13 (2.48g/t,0.8,90) T5A-14 (45,<0.2,<5) T5A-15 (0.95g/t,<0.2,<5) T5A-16 (160,<0.2,<5) T5A-17 (<5,<0.2,<5) T5A-18 (60,<0.2,<5) T5A-19 (85,<0.2,<5) T5A-22 (65,<0.2,<5) T5A-20 (90,<0.2,<5) T5A-21 (70,<0.2,5) 1 gfic layers flat well fract gouge qtz str, lim white alteration minor white alteration lim, crumbly i sil to qtz vn, lim, mn on fract 1.2 g/t 6.0 m LEGEND Bleached and silicified. Contains ~5% evenly distributed Fe oxide pods. Usually contains quartz stringers, veinlets or veins to roughly 10%. Stockwork intrusive. Contains >30% quartz veins, randomly oriented. Intrusive component may appear similar to 2a but may also be pervasively limonitically altered. Silicified intrusion with rare veins or veinlets, in areas contains pervasive limonitic alteration Unit 2c brecciated as a crackle or in situ breccia Unaltered metasedimentary package. Quartzites with muscovitic partings, schist Highly fractured, silicified and stockworked unit 1 with rare chloritic alteration. Fractures often coated with limonite, manganese. * black partings, intense fracturing Chloritic with foliated siliceous-chloritic Gneiss (granitized 1), quartzite beds Sample no. Au ppb, Ag ppm, As ppm 2 1 2a... 2b... 2c... 2 cbx.. 1a... QUARTZ qtz py cp ga po mal quartz pyrite chalcopyrite galena pyrrhotite malachite MINERALS ser lim chl sil mn sericite limonite chlorite silicified manganese ALTERATION vn str stwk fract bx frags vein stringer stockwork fracture breccia fragments STRUCTURE wmsivwmsiv weak moderate strong intense very MODIFIERS INTRUSIONS 1d (40,0.4,35) L 56 N / 50+50E 120 o 2 T R E N C H T R A I L START: 0 m m m (15,<0.2,<5) m (15,<0.2,<5) m (55,<0.2,<5) (35,<0.2,<5) ( 5,<0.2,<5) (10,<0.2,<5) (10,<0.2,<5) ( 5,<0.2,<5) (<5,<0.2,<5) (10,<0.2,<5) (40,<0.2,<5) (<5,<0.2,<5) (<5,<0.2,<5) (<5,<0.2,<5) ( 5,<0.2,<5) ( 5,<0.2,<5) (<5,<0.2,<5) (<5,<0.2,<5) (<5,<0.2,<5) (<5,<0.2,<5) (30,<0.2,<5) (20,<0.2,<5) (15,<0.2,<5) ( 5,<0.2,<5) ( 5,<0.2,<5) ( 5,<0.2,<5) (15,<0.2,<5) (75,<0.2,<5) (25,<0.2,<5) (100,<0.2,<5) sil’d 2 2 dominant fracture set 60 o sil’d 055 o 50 o 090 o 64 o fractures 2 2a 337 o 67 o limonitic alteration sil’d 2 2 stwk 1-1a 1 Grades from highly fractured limonitic / manganese altered 2 to silcified stockwork 2 to 2a 1-1a L 56 N / 50+25E 002 o 35 o