What’s not being talked about enough is the structural setting here. The continuity of high-grade mineralisation from surface, across many km's, isn't just a lucky strike, it's a textbook indicator of a large, potentially district-scale magmatic system. This isn't just about grades — it’s about the scale, and the cost effective extracting of shallow surface material. When you add in the strategic land expansion and how unexplored this reef actually is the upside is immense. People will catch on — just not before the smart money does.
Ann: High Grade and Wide Mineralised Zones from Surface at Dante, page-22
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