| Lat / long: | 51.96687, -178.37033 |
| Primary: | Iron |
| Operation type: | Unknown |
| Development status: | Occurrence |
| Alteration processes: | The original flow rocks have been intensely altered to iron oxides, chlorite, magnetite, and quartz. The iron oxides may have resulted from the weathering of pyrite. |
| DEP | 10308194 |
| Reference | Nelson, S.W., Nokleberg, W.J., Miller-Hoare, M., and Mullen M.W., 1979, Siniktanneyak Mountain ophiolite, in Johnson, K.M. and Williams, J.R., The United States Geological Survey in Alaska, Accomplishments during 1978: U.S. Geological Survey Circular 804-B, p. B14-B16 |
| Reporter | S.H. Pilcher |