kfc, Looking at the scale on map, the north cluster of Magnetite/Chalcopyrite boulder outcrops on the Serpentine dike is 3km wide and 12 km long. So very big surface outcrop area. Every occurrence is on the edge of the Serpentine dikes and these are not float boulders, they are in place (bedrock outcrops). A very big scentific report on Cyrus VMS deposits shows that VMSs can develop over Serpentine (ultramafics), image above. In other places there the serpentine will be subsurface. And it is possible/likley that as boulders on the edge of serpendine that indeed lower down is serpentine.
The fact there are so many surface outcrops of Magnetite/Chalcopyrite over such a large area indicates it is not isolated. It indicates that conditions for high-grade VMS formation on Beacon's land are widespread. Here is the full report. https://www.sciencedirect.com/science/article/pii/S0009254119304322
Multiple types of geophysics can find things worth drilling easily as the boulder minerlogy is very magnetic, conductive, and high gravity. Serpentine is a very lightweight rock, so big contrast gravity-wise. Subsurface geologic mapping should be extra easy here with geophysics. The climate, foliage, and terrain are super easy. Bet that they are very excited to start drilling after geophysics.
Cheers
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