Ann: Investor Presentation at Fremantle, page-40

That GG rig must be close now.

We'll be largely defining the Lydia and CP lodes, but will that allow further exploration of the predicted broad, deep mineralised zone?

How extensive is that deep mineralised zone?

How rich?

It appears alteration beneath CP increases with depth, can we infer that grades likely increase too?

With every new mineralised structure we discover I'm torn between hoping for rich surface expression of that system, or following it deeper. A new, rich near-surface zone would be a quick win, but THX are seeking a broader, deeper system. A system connecting the mineralised vertical faults we are finding. It's a breathtaking thought...

Aside from exploring deep alteration zones, discovering new surface-reaching mineralised faults there's the DHTEM at Granite Well.

Yep. I'm looking forward to drilling again.