here is what is important about the Headway As predicted by our geological model, at approximately 2684, an srsenopyrite enriched replacement
sulphiditic mineralized zone was encountered. The zone is approximately 12 m in length and had
anomalous gold mineralization associated with the sulphide mineralization. The current geological model
has been tested and proven to a depth of 2,751 metres. Both drill holes have penetrated the lower balmer
mafic volcanics that currently host the sulphiditic mineralization ore type at the Red Lake Mine (see
Headway Stratigraphy posted on our website).
In my opinion It is highly important that this was encountered as this is a marker of the possible HGZ mineralization.
The fact that they have resumed drilling at the Headway is only part of the major issue here.