Main commodities | Cu |
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Ore minerals | chalcocite; malachite |
Quadrangle map, 1:250,000-scale | MC |
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Quadrangle map, 1:63,360-scale | C-6 |
Latitude | 61.5446 |
Longitude | -143.0815 |
Nearby scientific data | Find additional scientific data near this location |
Location and accuracy | This occurrence is on the west valley wall of lower Kennicott Glacier. It is at an elevation of about 4,600 feet, 3,000 feet southeast of the center of section 5, T. 4 S., R 13 E. of the Copper River Meridian. This is locality 95 of MacKevett (1976); the location is accurate to within about 1,000 feet. |
Geologic descriptionThis occurrence consists of a small malachite-coated pod of chalcocite in Triassic Nikolai Greenstone (MacKevett, 1976). The widespread deposition of copper in Triassic greenstone and limestone of the area is thought to have accompanied regional deformation and low-grade metamorphism in the Late Jurassic or Early Cretaceous (MacKevett and others, 1997). Copper-bearing minerals were deposited in the underlying Nikolai Greenstone at about 112 Ma (Silberman and others, 1980). | |
Geologic map unit | (-143.083582127752, 61.5441605677565) |
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Mineral deposit model | Basaltic Cu (Cox and Singer, 1986; model 23) |
Mineral deposit model number | 23 |
Age of mineralization | Cretaceous? The widespread deposition of copper in Triassic greenstone and limestone of the area is thought to have accompanied regional deformation and low-grade metamorphism in the Late Jurassic or Early Cretaceous (MacKevett and others, 1997). Copper-bearing minerals were deposited in the underlying Nikolai Greenstone at about 112 Ma (Silberman and others, 1980). |
Alteration of deposit | Oxidation. |
Workings or exploration | Limited surface examination. |
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Indication of production | None |
Additional commentsThe locality is in the Wrangell-Saint Elias National Park and Preserve. |
References | |
Reporters | Travis L. Hudson (Applied Geology, Inc.) |
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Last report date | 1/12/2003 |