Quadrangle map, 1:250,000-scale | SH |
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Quadrangle map, 1:63,360-scale | A-1 |
Latitude | 66.11 |
Longitude | -156.02 |
Nearby scientific data | Find additional scientific data near this location |
Location and accuracy | This occurrence is at an elevation of about 2,000 feet, in the saddle of a ridge 3 miles northeast of Solsmunket Lake. The map site is in section 12, T. 8 N., R. 13E., of the Kateel River Meridian. Cobb (1972, MF-448), location 12. |
Geologic descriptionThis occurrence consists of a tungsten-bearing quartz vein, and of radioactive minerals, in monzonite (Miller and Ferrians, 1968). The quartz vein is 1 to 3 feet wide. It assayed 7,000 ppm W, but no tungsten mineral was noted. Samples of monzonite from the border facies of the Cretaceous Zane Hills pluton, which is mainly granodiorite, contained 14 to 33 ppm U and 75 to 199 ppm Th. The radioactivity apparently is mainly in uranothorianite, thorite, betafite, allanite, zircon and sphene. | |
Geologic map unit | (-156.022646040186, 66.1094343299285) |
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Mineral deposit model | Tungsten-bearing quartz vein and disseminated radioactive minerals in monzonite. |
Age of mineralization | Cretaceous. |
Workings or exploration | Site visited and sampled by U.S. Geological Survey (Miller and Ferrians, 1968). |
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Indication of production | None |
MRDS Number | A015600 |
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References | |
Reporters | Anita Williams (Anchorage, AK) |
Last report date | 12/16/1999 |