Commodities
PrimaryIron
SecondaryLead, Zinc, Copper
Geology
AlterationThe 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.
Economic & production
Development statusOccurrence
Identification
Deposit ID10308194
RegionNA
Data scoreD
Coordinates51.96687, -178.37033
References
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