The Krieghoff property is geographically situated in an area well suited for the concentration of mineral deposits. To date, some five zinc showing have been mapped within the property limits and two additional showings have been documented immediately south of the claim group. From case histories described under "Local Geology", it is indicated that there is direct association between mineral occurences and the Proterozoic intrusive sills within the Blondeau formation. The presence of this sills within the part of the property may have played a role in the mobilization of sulfide-bearing hydrothermal fluids. Several airborne (in-put) anomalies (II, VII, VII), as well as ground VLF and electromagnetic conductor remain unexplored or unexplained to date.