
Claim Geology
Geology of the Camp Project group of claims is similar to that of the Silver Summit (ConSil) portion of the Sunshine Mine. Prominent fault structures that have hosted millions of ounces of silver productions elsewhere, such as the Polaris fault, the Silver Summit vein fault and the Chester fault all trend through the Camp Project claims area. The north limb of the Big Creek anticline, which hosts some of the major silver deposits in the district also trends thorough the Camp Project area. Results of 13,200 feet of exploration geophysics performed during 2005 indicate a high chargeability/low-resistivity anomaly indicative of sulfide mineralization. This anomaly extended from near the surface to the maximum sensitivity of the test instrumentation in a generally east-west orientation and appears to increase in depth to the east. The Silver Summit, Chester, Wire Silver, "D", and Chester-Polaris "Hook" Veins all originate in or extend into the Camp Project claims at depth.