Geologic description
The regional geology consists of deformed and metamorphosed Silurian or Devonian carbonate, clastic and volcanic clastic rocks that have been intruded by Upper Jurassic and Lower Cretaceous granitic and dioritic rocks (Brew and others, 1992). Brew and Ford (1985) describe the rocks in the vicinity of this occurrence as predominantly Devonian and Silurian greenstone, greenschist, limestone and graywacke intruded by Cretaceous biotite-hornblende granodiorite. Jim Burnett, a prospector, reported that he sampled a 12-foot vein or zone of copper in the area that assayed 14% copper (Williams, 1953). Williams failed to locate the occurrence. Wells and others (1986) report a copper vein in this vicinity and assert that claims were active in 1900. |