Quadrangle map, 1:250,000-scale | ID |
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Quadrangle map, 1:63,360-scale | C-4 |
Latitude | 62.52836 |
Longitude | -157.86091 |
Nearby scientific data | Find additional scientific data near this location |
Location and accuracy | This occurrence is on a small but prominent knob, hill 877, on an unnamed fork of Caribou Creek. The occurrences is at an elevation of about 700 feet, about 0.5 mile west to west-southwest of the center of section 8, T. 28 N., R. 46 W., of the Seward Meridian. The location is accurate. |
Geologic descriptionThis occurrence consists of altered, iron-oxide-stained hornfels near a biotite-bearing, fine grained intrusion. The intrusion has been radiometrically dated as 70.2 Ma (Miller and Bundtzen, 1994; Miller, Bundtzen, and Gray, 2005). The mineralized body is of uncertain size and orientation. One grab sample of mineralization rock contained 2,000 parts per billion (ppb) silver, 850 parts per million (ppm) arsenic, 200 ppm copper, 52 ppm bismuth, 30 ppm tin, and 50 ppb gold (McGimsey and others, 1988). | |
Geologic map unit | (-157.863307451315, 62.5276780437567) |
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Mineral deposit model | Sn-polymetallic deposit or Polymetallic vein (Cox and Singer, 1986; model 20b or 22c). |
Mineral deposit model number | 20b or 22c |
Age of mineralization | Undated; the nearby intrusion is 70.2 Ma (Miller and Bundtzen, 1994). |
Alteration of deposit | Iron oxide staining. |
Workings or exploration | The area was sampled by the Alaska Division of Geological and Geophysical Surveys and U.S. Geological Survey in 1986 (McGimsey and others, 1988). |
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Indication of production | None |
References | |
Reporters | T.K. Bundtzen (Pacific Rim Geological Consulting, Inc.), M.L. Miller (U.S. Geological Survey); and C.C. Hawley (Hawley Resource Group) |
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Last report date | 5/19/2003 |