The Blunt Mountain copper-molybdenum showings are located north of the saddle between Blunt Mountain and Mount Seaton at the headwaters of Luno and Blunt creeks.

The showings are hosted within the Blunt Mountain stock of the Late Cretaceous Bulkley Intrusions. A pyrite halo is strongly developed within the Middle Jurassic to Lower Cretaceous Bowser Lake Group hornfelsed sedimentary rocks. The mineralization occurs in a northeast-trending zone, approximately 2 kilometres in length, which probably extends as far as the Mount Seaton occurrence (093M 025). The chalcopyrite mineralization is associated with potassic alteration, with hornblende altered to biotite. Molybdenite is commonly associated with the copper mineralization.

In 1973, Cyprus Explorations Ltd. carried out geochemical sampling of the Gypsy claims. Copper concentrations were found to vary from 16 to 700 ppm and molybdenum concentrations varied from 5 to 380 ppm (EMPR PF Cyprus Anvil Read, D., 1973). During the same year, a magnetometer survey was conducted over a portion of the claims by Great Oaks Mining Corporation. The survey identified a magnetic low and heavily pyritized breccia boulders were found in the vicinity of the low (EMPR PF Cyprus Anvil Simpson, J.G., 1973).