Mineralization
The Graphite Creek deposit is characterized by coarse, crystalline (large-flake), graphite within graphite-bearing schist. Graphite mineralization is exposed at surface along the Kigluaik Mountain Range front. The large flake graphite occurs as disseminations and high grade segregations and lenses in distinct sillimanite-garnet-quartz-biotite schist and quartz-biotite schist. The host schist is continuous over 18 km of strike length, based on mapping, sampling and airborne geophysics.