Rocky Mountain Trench

West of the Wicheeda District, we have acquired a portfolio of small claims associated with unexplored regional stream geochemical results within a belt of Cambrian-Permian limestones and marbles in the western range of the Rockies. These Permian limestones represent a permissible setting for bulk-tonnage, low grade mineralization, as found elsewhere in the back range of the Rockies throughout the North American cordillera.

This area hosts the only indicated location of post-accretion cross faulting reported in B.C., where faults extend from Cordillerian terranes into the ancestral North American sedimentary rocks of the Rockies. This feature represents regional scale structural controls of economic scale and magnitude. The structure provides both the energy for mineralization and a suitable host horizon.

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Our jointly operated CADDIS LAKE property hosts a newly discovered coincident aeromag-MMI REE anomaly, demonstrating the viability of our hypothesis in our first year of prospecting

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The presence of carbonates implies potential for sediment hosted or Carlin style disseminated GOLD, SILVER, or ZINC mineralization; enrichment of these elements is indicated by regional geochemical surveying.

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While each of these prospects is a very early-stage target, they meet our mandate of (a) having top-tier geostatistics without a history of ground follow-up, while (b) representing a novel geological target for B.C.