Main commodities | Cu |
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Ore minerals | chalcocite; native copper |
Quadrangle map, 1:250,000-scale | MC |
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Quadrangle map, 1:63,360-scale | C-3 |
Latitude | 61.7278 |
Longitude | -141.9079 |
Nearby scientific data | Find additional scientific data near this location |
Location and accuracy | This prospect is high on the south valley wall of the Middle Fork of the White River. It is at an elevation of about 6,000 feet, 4,400 feet north-northeast of elevation 8233 in the NE1/4 of section 2, T. 2 S., R. 19 E. of the Copper River Meridian. This is locality 156 of MacKevett (1976); the location may be accurate to within a thousand feet. |
Geologic descriptionThis old copper prospect is in Triassic Nikolai Greenstone, but no other information about it is available (Capps, 1916, p. 122; MacKevett, 1976). Copper mineralization is common in Nikolai Greenstone and is thought to have accompanied regional deformation and low-grade metamorphism in the Late Jurassic to Early Cretaceous (MacKevett and others, 1997). | |
Geologic map unit | (-141.910004908746, 61.72741794078) |
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Mineral deposit model | Basaltic Cu (Cox and Singer, 1986; model 23) |
Mineral deposit model number | 23 |
Age of mineralization | Cretaceous? Copper mineralization is common in Nikolai Greenstone and is thought to have accompanied regional deformation and low-grade metamorphism in the Late Jurassic to Early Cretaceous (MacKevett and others, 1997). |
Workings or exploration | Possibly some minor work. |
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Indication of production | None |
Additional commentsThe locality is in the Wrangell-Saint Elias National Park and Preserve. |
ReferencesMacKevett, E.M., Jr., Cox, D.P., Potter, R.W., III, and Silberman, M.L., 1997, Kennecott-type deposits in the Wrangell Mountains, Alaska--High-grade copper ores near a basalt-limestone contact, in Goldfarb, R.J., and Miller, L.D., eds., Mineral deposits of Alaska: Economic Geology Monograph 9, p. 66-89.
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Reporters | Travis L. Hudson (Applied Geology, Inc.) |
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Last report date | 1/12/2003 |