The Douglas showing is located to the southeast of Douglas Peak, about 19 kilometres southeast of Port Alberni.

Basaltic flows and pillow basalt of the Upper Triassic Karmutsen Formation (Vancouver Group) are underlain by a complexly inter- layered succession of volcanics and sediments of the Paleozoic Sicker and Mississippian to Lower Permian Buttle Lake groups. In the area, the rocks comprise basaltic flows, agglomerates and bedded tuffs of the Upper Devonian McLaughlin Ridge Formation (Myra Formation), Sicker Group.

Gold-copper mineralization (likely pyrite and chalcopyrite) occurs in basalts. A sample assayed 28.1 grams per tonne gold and 0.9 per cent copper (George Cross News Letter #96, 1985).

In 2010, the area was staked by P. Saulnier as the Lime claims. The next year a program of prospecting and geochemical sampling was completed.