Geological folding and faulting of the mineralisation over time...

Geological folding and faulting of the mineralisation over time can also create different lenses or sections of a resource.

What starts out as a planar body, as seen in VMS formation, can end up having a completely different orientation and morphology with the movement of geological structures over many years.

I like the fact they don’t understand the genesis of Rupice yet because we aren’t locked into a corresponding typical size of resource. Lots to learn here about the resource, it’s formtion and overall size. Rupice may surprise to the upside in both grade and size?