Hole SN-12-02 (152 metres) and SN-12-03 (122 metres) were each 30 metre easterly stepout holes from SH-11-007. Similar to the 2011 mineralization, drilling encountered a zone of silicification and sulphide bearing epithermal-type quartz stockwork veining in rhyolite tuffs from the surface to a depth of 60 metres. Hole SN-12-04 (236 metres) tested a possible extension of the Tower Zone mineralization 75 metres west of SN-12-07, extending across the Tower Creek valley fault. The hole intersected an extensive silicified zone from surface through the initial 120 metres, interpreted as a possible dilational fluid channelway for mineralization . Several quartz stockwork zones were encountered within the silicified zone and low levels of very fine sulphide mineralization was encountered throughout the hole.