The WW3 occurrence is located about 90 kilometres east-southeast of Dease Lake.

The area is underlain by upper Mississippian to Permian Cache Creek Complex rocks including volcanic, metavolcanics (greenstone), metasediments, gabbro and tectonically emplaced ultramafic rocks. The upper Mississippian to Permian Cache Creek Complex ultramafic rocks consist of peridotite, dunite and pyroxenite which are generally serpentinized.

At the WW3 showing, siliceous sericite-rich phyllites of the Mississippian to Triassic Kedahda Formation (Cache Creek Complex) contain 3 to 10 per cent disseminated pyrite, pyrrhotite and trace amounts of chalcopyrite.

On the PW claims in 1985, Getty Canadian Metals conducted a geological survey and took 234 rock and 134 soil samples. No other work is documented. See related occurrences PW3 (104I 112) and PW1 (104I 113) located 2.5 kilometres south.