Gold-bearing mineralization associated with iron formation on the MacLeod-Cockshutt and Hard Rock Properties in Canada is found in both quartz veins and as replacement of the sediment. The ore-bearing structures are controlled by lithological contacts and localized strain deformation. Structural analysis of vein, shear, and fold axis attitudes will permit confirmation of the field impression that all three are related to the three-tier structural hierarchy: 1. Hard Rock Synclinorium; 2. North Zone drag fold; and 3. minor drag folds.