Article

American Pacific Mining Corp. has reported significant geological findings from its Madison Copper-Gold Project in Montana. The exploration team applied a 'fugitive calcite' black-light technique, successfully identifying fluorescing calcite populations in newly exposed underground workings.

This technique revealed an additional 150 feet of access due to lower water levels. The findings suggest multiple mineral sources at Madison, supporting the hypothesis of a porphyry cluster and providing new data for exploration strategies. The use of ultraviolet scanning is noted as an effective tool for identifying mineralization indicators.