Junior Mining Investment Pitch

Critical Ore Controls The secret ingredients for CRD's: A A Fluid source (Intrusive stock/porphyry) ☐ Currently undiscovered for the IC district Permissive carbonate host rocks for replacement >400 m of dolostone at IC • >600 m of dolostone at WPC Plumbing (faults) for the mineralized fluids WPC fault, Warm Springs fault (target), and IC fault Cap rock to concentrate the fluids 3 cap rocks in district: 2 schists (WPC) and greenstone (IC) How are CRD's formed? The mineralizing fluids coming from the intrusive stock (source/porphyry) are very hot and acidic. The metals are transported in this fluids along faults, following the path of least resistance. When the hot, acidic fluid interacts with the basic carbonate rocks, an acid neutralization reaction occurs (think baking soda and vinegar), which causes the metals to deposit as sulfides and causes the system to self-stope, creating km-scale mineralized bodies TSX-V: WAM WPC22-20 185.2-185.8 m 195 gpt Ag, 41.1% Zn, 5.0% Pb 2016 gpt (64.8 opt) AgEq WPC22-22 167.5-168.6 m 1355 gpt Ag, 22.3% Zn, 38.2% Pb 3449 gpt (110.9 opt) AgEq WPC22-20 193.4-194.7 m 392 gpt Ag, 3.4% Zn, 12.7% Pb 926 gpt (29.7 opt) AgEq WPC22-17 130.4-131.4 m 614 gpt Ag, 24.4% Zn, 31.5% Pb 2884 gpt (92.7 opt) AgEq WPC22-20 203.3-204.0 m 270 gpt Ag, 11.5% Zn, 9.6% Pb 1035 gpt (33.3 opt) AgEq

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