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(1) Reported widths are "drilled widths" not true widths and may not be indicative of the true grade, width and style of mineralization on the property. (2) Values from hole CSK24-02 are previously released, see news release September 24, 2024
Table 2: Drill Hole Locations for this News Release
Exploration Target
The "White River Intrusive Complex" ("WRIC") is a favourable setting for magmatic nickel-copper sulphide mineralization and is considered a "feeder system" with a high volume of magma flow. Due to the abundance of magmatic Ni-Cu-PGE showings at the base of the WRIC and the discovery of the nickel-rich Canalask footwall deposit, the project hosts strong potential for both "magmatic feeder-type" basal deposits and "epigenetic footwall-type" footwall deposits. The geological setting draws comparison to the world-class Norilsk Ni-Cu-PGE camp.
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