[1] The main minerals found at Kanichee Mine include pyrite, pyrrhotite and chalcopyrite, occurring as semi-massive to massive veins.

[2] The Precambrian oval-shaped Kanichee layered intrusive complex is the largest of many sill-like mafic-ultramafic bodies in felsic and mafic metavolcanic rocks in the northern portion of the Temagami greenstone belt.

[3] A succession of cumulus phases comprising every magmatic series suggests that the Kanichee layered intrusive complex is south-facing, including the surrounding metavolcanic lava flows.

[3] This record indicates that magmatic rocks of the Kanichee layered intrusive complex originally formed in a level position and most likely very shallow beneath the Earth's crust.

[3] In the lower four magmatic series, masses of chromite, olivine and clinopyroxene develop rocks varying from dunite to clinopyroxenite.

[3] The fifth magmatic series comprise a similar suite of ultramafic rocks overlapped by olivine and quartz gabbros in which plagioclase, clinopyroxene and an iron–titanium oxide phase are the dominant minerals.

However, a geologic project is expected to be evaluated for potential sampling at new Kanichee deposits in 2009, sparking a possibility for renewed mining operations.