The Strike Point property is underlain by Archean volcanic rocks that are identical to or similar to the hanging wall volcanic rocks that host San Gold's Hinge and Cohiba zones. As well, an embayment of volcanic rocks extends northward across the regional Wanipigow Shear where it contains mafic volcanics and interbedded iron formations that remain largely unexplored. More importantly, the hanging wall volcanics of the southern part of the Strike Point property contain structural elements that are identical or similar to the structures that host San Gold's Hinge and Cohiba zones. Significantly, the Strike Point property contains the western 5 kms of a 10 km long faulted fold axis that extends eastward from Horseshoe Lake to the San Gold No. 1 mine. This important 10 km long structure is considered to be a possible mineralization conduit for the multiple parallel Hinge Structures on the San Gold mining lease.