A small quartz vein striking 057 degrees and dipping 35 to 40 degrees southeast is hosted by black argillites of the Lower and Middle Ordovician Active Formation. Mineralization consists of pyrite, pyrrhotite, galena, and sphalerite and has been exposed in a short adit and a number of surface trenches.
The vein produced 1,992 tonnes of ore in 1938, 1939 and 1940 with all but 52 tonnes being mined in 1940. From the total mined 511 grams of gold and 829 grams of silver were recovered.