So.. back to the geology.
Similar to pegmatite swarm theory, these outcrops of pitchblende (Uraninite) usually arise at the surface as a result of an outer halo borne from and intrusive below (Pushing through) the UC.
The surface samples are off the chart. Previous exploration has failed to find the source at depth.
New data has been over-layed on older (but now digitised) data. DD coming up will likely look into new areas to hunt down the potential intrusion.
This is why I am happy to hold here. It’s analogous to the Cameco find and some others too.
The surface trench samples aren’t new, but the collation of old and new data is. New vectors increase the chance of a find substantially.
All about the first pass.
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