When are the drill results due ?, page-16

Mt Berghaus
The Mt Berghaus deposit is hosted in a sequence of deformed Archaean siliciclastic rocks. Later quartz
-feldspar porphyries intrude the siliciclastic rock sequence. The trend of the gold mineralisation has a
known cumulative strike of ~2km in length and locally 25m wide, with potential for growth along strike
of the known gold mineralisation. Mineralised zones are typically east-northeast-west-southwest
striking and occur as sub-vertical, steeply dipping structures to the south-southeast.
Mineralisation is largely constrained to strongly weathered bedrock. Where drilling has intersected
unweathered mineralisation, it comprises quartz veining and pyrite. The unweathered gold
mineralisation is considered free milling.
The weathering profile comprises a veneer of calcrete or transported sands. Mineralisation and bedrock
are weathered up to a depth of 60m.