Main commodities | Cu |
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Other commodities | Ag |
Ore minerals | chalcocite; chalcopyrite; malachite |
Gangue minerals | calcite; quartz |
Quadrangle map, 1:250,000-scale | MH |
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Quadrangle map, 1:63,360-scale | A-6 |
Latitude | 63.1492 |
Longitude | -146.8837 |
Nearby scientific data | Find additional scientific data near this location |
Location and accuracy | The Little Clearwater lode is at an elevation of about 4,850 feet about 0.7 mile southwest of peak 5315 at the south end of the Clearwater Mountains; it is in the SE1/4SE1/4 section 24, T. 20.S., R. 4 E., Fairbanks Meridian. The occurrence corresponds to locality A36 of Kurtak and others (1992), locality 3 in figure 4 of Cobb (1979 [OFR 79-238]), and locality 6 in table 2 of Nokleberg and others (1991). |
Geologic descriptionThe rock at the occurrence is propylitized basalt of the Nikolai Greenstone of Late Triassic age (Nokleberg and others, 1991). The deposit consists of copper-bearing quartz-calcite veins in the weakly altered basalt. Reported copper minerals are chalcopyrite, chalcocite, and malachite. Sample 1414 from metabasalt assayed 0.34 ounce of silver per ton and 1.08 percent copper; gold is present in a near-background amount (10 parts per billion) (Kurtak and others, 1992, table A32, p. 165). | |
Geologic map unit | (-146.885962897574, 63.1487580710163) |
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Mineral deposit model | Basaltic Cu (Cox and Singer, 1986; model 23). |
Mineral deposit model number | 23 |
Age of mineralization | The deposit is probably either Cretaceous or early Tertiary in age (see MH060, MH087, or MH100). |
Alteration of deposit | Propylitic alteration. |
Workings or exploration | U.S. Bureau of Mines sample 1414 contained 1.08 percent copper and 0.34 ounce of silver per ton (Kurtak and others, 1992, table A32). |
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Indication of production | None |
Additional commentsThe mineralized zones are small and mostly in rubble. |
References | |
Reporters | W.T. Ellis (Alaska Earth Science), C.C. Hawley (Hawley Resource Group), and W.J. Nokleberg (USGS) |
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Last report date | 8/5/2001 |