The Mac property is located on the west slopes of Snow Peak about 22 kilometres west of the community of Dease Lake. Access is south on a 4 by 4 road up Dease Creek from Laketon to an ATV trail going south to Snow Peak.

The showing area is underlain by Lower Jurassic Laberge Group (Takwahoni Formation) phyllitic slates and Late Cretaceous Snow Peak pluton granitic rocks. Several areas of quartz veining, some sheeted, were observed cutting the slates. Pyritic mafic dikes crosscut the granitic rocks and are up to two metres wide and have been traced for 1000 metres.

Five quartz veins were bulk sampled and using gravity concentration and a microscope to view the concentrates, pyrite, sphalerite, galena, chalcopyrite and tetrahedrite, in order of abundance, were observed. Native gold and silver were also evident (Assessment Report 28972).

In 2006, owner M. Swenson conducted prospecting and collected 20 kilogram bulk samples of vein material from five areas; forty samples were viewed under a microscope.