Geologic descriptionBanner Peak is underlain mainly by graphitic quartz schist (quartzite) faulted to the north against chlorite-rich metaturbidite schist and marble (Bundtzen and others, 1994). The Peterson and Lamoreaux quartz prospect is at an elevation of 650 feet in graphitic schist and within about 200 feet of the fault. Mertie (1918, p. 432) reported that the quartz body had a strike of N 45 E and a dip of 45 N, and was at least 8 feet thick, and irregularly bounded. The quartz is nearly white and not banded and contains sparsely disseminated galena. The Peterson and Lamoreaux antimony prospect is at an elevation of 550 feet, but its location is uncertain. It is in schist and reportedly produced 1,500 pounds of stibnite ore (Mertie, 1918, p. 439). |
Geologic map unit |
(-165.423399258616, 64.5727334847231) |
Mineral deposit model |
Low-sulfide Au-quartz vein (Cox and Singer, 1986, model 36a); simple Sb deposits? (Cox and Singer, 1986; model 27d). |
Mineral deposit model number |
36a, 27d? |
Age of mineralization |
Probably mid-Cretaceous; Mertie (1918 [B 662-I, p. 425-449]) thought the vein quartz could be old and possibly related to metamorphism; see NM207. |