Molybdenite mineralization occurs 1.5 kilometres northeast of Stave River, 13 kilometres north-northwest of the north end of Stave Lake.
A quartz vein, 4.6 to 23 metres wide, strikes northwest for at least 152 metres and dips steeply southwest. The vein cuts Late Cretaceous foliated quartz diorite of the Tertiary to Jurassic Coast Plutonic Complex.
Mineralization consists of irregularly scattered disseminations and blebs of molybdenite, up to 0.05 metres in diameter. A grab sample assayed 1.5 per cent molybdenite, 0.3 per cent copper, 13.7 grams per tonne silver and trace gold (Minister of Mines Annual Report 1918, p. 289).