The Ample-Goldmax Property is host to several known mineralized zones, primarily containing native gold with or without sulphides in mesothermal quartz vein stockworks, gold and traces of silver in sulphide zones, and possibly lower grade disseminated gold.  Most of the mineralized zones are associated with the Cayoosh Creek thrust fault, the dominant structural feature of the Property and a regional scale thrust fault that separates greenstones of the Bridge River Complex and the sedimentary rocks of the Cayoosh Assemblage.  Gold, generally with chalcopyrite, pyrrhotite and arsenopyrite, occurs in quartz veins, irregular silica flooded zones and silicified wall rock. 

Dilatant zones straddling the Cayoosh Creek fault and other sub-parallel low angle fault zones are favourable for gold mineralization.  Discontinuous quartz veins up to 2m in width and containing high-grade native gold occurs in areas of brittle faulting along the Cayoosh Creek fault, associate with diorite sills and dykes.  Less competent Cayoosh Assemblage phyllitic rocks adjacent to the fault are more likely to host lower grade gold mineralization in quartz stockworks and zones of disseminated arsenopyrite.  Mineralization can be traced for 3kms along the Cayoosh Creek fault from the Ample-Goldmax Zone westward through the Ample Mine and Wedge showing to the Omega Fraction and Golden Cache.  Similar style mineralization at the C Zone, east of the Ample-Goldmax Zone, indicates a probable strike extent of the favourable structural setting of at least 4kms.