The N110 showing consists of disseminated pyrite and chalcopyrite mineralization in Upper Triassic Stuhini Group volcanics and a syenite body. The most significant mineralization in the N110 canyon is hosted within Stuhini Group feldspar-phyric agglomerate and augite-feldspar-phyric crystal tuff, with up to 10 per cent pyrite and 2 per cent chalcopyrite. Potassium feldspar and epidote altered Stuhini Group volcanics mineralized with 4 per cent pyrite assayed 1.27 grams per tonne gold with 0.03 per cent parts per million copper (Assessment Report 21061). The best copper grades (0.24 per cent in sample 447127) appear to be found within the syenite.

Refer to Trophy (Ptarmigan) (104G 053) for related details and a common work history.