The Garden Gully project area is characterised by a veneer of transported cover of variable thickness, underlain in places by a subsurface layer of duricrust. We believe that the combination of these factors has contributed to past soil geochemistry surveys failing to identify and locate accurately the underlying primary mineralised structures that our exploration has found. This was the rationale for the recent programme of air core. SAM surveys are currently undertaken over the Transylvania and Young prospects (see Figure 2 in link below) and other selected areas with complete cover will follow soon after.
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