Quadrangle map, 1:250,000-scale | SO |
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Quadrangle map, 1:63,360-scale | C-5 |
Latitude | 64.652 |
Longitude | -164.261 |
Nearby scientific data | Find additional scientific data near this location |
Location and accuracy | This prospect is on the south side of Big Hurrah Creek (SO022) about 0.2 miles upstream of the mouth of Linda Vista Creek, a south tributary. This is locality 2 of Asher (1969, DGGS R33). |
Geologic descriptionTwo short adits explore quartz veins at this locality. The lower adit is reported to have exposed a 7- to 8-foot-wide, vertical but faulted, quartz vein (Smith, 1910, p. 147). The upper adit, a few hundred feet to the south of the lower one, is on a 1-foot-wide quartz vein with arsenopyrite, pyrite, and possibly marcasite (Asher, 1969, DGGS R33). A grab sample of this vein assayed 0.003 ounces Au per ton (Asher, 1969, DGGS R33). The country rock is part of a lower Paleozoic metasedimentary assemblage that includes a distinctive black, very fine-grained, graphitic schist (Sainsbury and others, 1972, OFR 511; Till and others, 1986). These quartz veins may be similar in age to some other gold-quartz veins of southern Seward Peninsula. The other southern Seward Peninsula lode gold deposits formed as a result of mid-Cretaceous metamorphism (Apodoca, 1994; Ford, 1993, Ford and Snee, 1996; Goldfarb and others, 1997) that accompanied regional extension (Miller and Hudson, 1991) and crustal melting (Hudson, 1994). This higher temperature metamorphism was superimposed on high pressure/low temperature metamorphic rocks of the region. | |
Geologic map unit | (-164.263605751659, 64.6512581735835) |
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Mineral deposit model | Gold-quartz vein in metamorphic rocks; low sulfide-Au quartz vein (Cox and Singer, 1986; model 36a). |
Mineral deposit model number | 36a |
Age of mineralization | Mid-Cretaceous?; possibly same age as some other gold-quartz veins of southern Seward Peninsula. |
Alteration of deposit | Quartz veining in metamorphic rocks. |
Workings or exploration | Two short adits explored quartz veins at this site. |
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Indication of production | None |
MRDS Number | A012594 |
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ReferencesApodoca, L.E., 1994, Genesis of lode gold deposits of the Rock Creek area, Nome mining district, Seward Peninsula, Alaska: Boulder, Colorado, University of Colorado, Ph.D. dissertation, 208 p.
Ford, R.C., 1993, Geology, geochemistry, and age of gold lodes at Bluff and Mt. Distin, Seward Peninsula, Alaska: Golden, Colorado School of Mines, Ph.D. dissertation, 302 p.
Ford, R.C., and Snee, L.W., 1996, 40Ar/39Ar thermochronology of white mica from the Nome district, Alaska--The first ages of lode sources to placer gold deposits in the Seward Peninsula: Economic Geology, v. 91, p. 213-220.
Goldfarb, R.J., Miller, L.D., Leach, D.L., and Snee, L.W, 1997, Gold deposits in metamorphic rocks in Alaska, in Goldfarb, R.J., and Miller, L.D., eds., Mineral Deposits of Alaska: Economic Geology Monograph 9, p. 151-190.
Hudson, T.L., 1994, Crustal melting events in Alaska, in Plafker, G., and Berg, H. C., eds., The Geology of Alaska: Geological Society of America, DNAG, The Geology of North America, Vol. G-1, p. 657-670.
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Reporters | Travis L. Hudson (Applied Geology) |
Last report date | 8/19/1999 |