The Coronation Zone, as outlined by historical drilling, contains significant massive and semi-massive sulphide grades and tonnes as well as over mineable widths (>2 m). It is the most significant VMS deposit outside of the Mt. Sicker deposits in the area and occurs at shallow depths of <150 m below surface. Previous metallurgical testing and pre-feasibility studies (Roberts, 2007; Broughton, 1987) although not current, demonstrate the possibility that the deposit can be economic and deserves further investigation.  Furthermore, there is abundant exploration potential to depth and on strike along the Coronation Trend to warrant additional exploration as VMS deposits such of these tend to occur as clusters including the most immediate analogues (Mt. Sicker and Buttle Lake Myra Falls deposits).