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BH-12-02
BH-12-02 was collared slightly to the east of BH-12-01, again encountering mineralized quartz veining just within the bedrock, and also intersecting the Main #1 Vein further down the hole and the #2 Vein below it.
Assay highlights from this hole include;
----------------------------------------------------------------------------DDH From To Length Mo % Sn % W % Ag g/t Bi ppm Cu ppm Zn ppm----------------------------------------------------------------------------BH-12-02 31.4 32.2 0.8 0.102 0.019 1.32 2.8 3020 282 49 less thanBH-12-02 36.2 37 0.8 0.001 0.009 0.383 0.3 386 16 86BH-12-02 68.9 69.5 0.6 0.016 0.016 0.255 1.5 825 78 107BH-12-02 89 89.3 0.3 0.102 0.28 0.003 0.7 589 220 37BH-12-02 110.1 110.8 0.7 0.021 1.13 0.155 42.3 1540 57 61BH-12-02 176.2 177.2 1 0.002 0.08 0.415 0.6 69 136 97BH-12-02 218.8 219.4 0.6 0.239 0.027 0.952 0.5 50 73 109BH-12-02 235 236 1 1.14 0.088 0.026 0.6 50 77 1290 less thanBH-12-02 280 281 1 0.005 0.149 0.752 0.3 14 95 1920----------------------------------------------------------------------------
BH-12-03
This hole, collared to the NW of the mine area, also intersected the Main #1 Vein, in this instance around the start of the sediment/granitoid contact, after crossing through two clusters of mineralized veins in the sediments. The Main Vein zone, approximately 200-230m down the hole also contained notable copper and zinc mineralization, with one sample between 212-212.7 m encompassing sphalerite clots assaying 2.53% zinc.
Assay Highlights from this hole include;
---------------------------------------------------------------------------- CuDDH From To Length Mo % Sn % W % Ag g/t Bi ppm ppm Zn ppm---------------------------------------------------------------------------- less thanBH-12-03 46.3 47 0.7 0.277 0.008 0.039 0.3 35 47 128 less less less than than than lessBH-12-03 69.6 71.1 1.5 0.001 0.001 0.001 19.1 than 2 177 125BH-12-03 188.4 189.6 1.2 0.006 0.458 0.007 0.4 30 73 122BH-12-03 209 215.6 6.6 0.019 0.008 0.001 0.57 16.97 150.7 4047.73 less thanincluding 212 212.7 0.7 0.016 0.013 0.001 2.9 76 964 25300----------------------------------------------------------------------------
BH-12-04
This hole, collared furthest to the east to date as seen in the illustration above, extends the drill tested mineralization at Burnt Hill by approximately 1000 feet. This hole was selected in follow up to successful surface exploration which found visible cassiterite at the summit of Burnt Hill on a southern flank. This hole intersected the anticipated jointed sediment for its entire length, returning tin assays from surface down to approximately 80m on joint planes, below 150m the same joint planes return copper values with pyrrhotite-chalcopyrite flakes on the joints.
