This deposit was discovered prior to 1898 (Wells and others, 1986). It consists of multiple quartz veins in mica schist and chlorite schist near a granitic intrusive (Cobb, 1978 [OFR 78-374]). The veins strike N 20 W. and dip NE, parallel to the strike of the schistose host rocks. The veins can be traced discontinuously northwest to the Alaska Dano Mine (JU235). One vein is 15 to 25 feet thick and has been traced for 2,300 feet. It consists of quartz and calcite, with pyrite and pyrrhotite, and minor galena, specular hematite, and native gold. Another vein, 30 inches thick, consists of white quartz, pyrite, specular hematite, and minor chalcopyrite, galena, and copper oxides. It is crosscut by a calcite vein. The prospect is developed by 2 shafts, an unknown amount of drifts, and some open cuts (Wells and others, 1986). The prospect is included with the Alaska Dano and War Horse deposits in some reports (Cobb, 1978).