|Quadrangle map, 1:250,000-scale||JU|
|Quadrangle map, 1:63,360-scale||B-3|
|Nearby scientific data||Find additional scientific data near this location|
|Location and accuracy||This mine is at an elevation of 800 feet, 1/4 mile east of Peterson Lake, 3 miles north of Auke Mountain, and 2 miles east of Lynn Canal. It is in the SW1/4SW1/4 section 32, T. 39 S., R. 65 E. of the Copper River Meridian, where the site is marked by a prospect symbol on the Juneau B-3 topographic map. The location is accurate.|
The Peterson Mine was discovered in 1897. Workings include 4 shafts, 11 adits, and numerous trenches (Redman and others, 1989). The deposit consists of quartz veins in northwest-striking phyllite and greenstone. A chloritized, 80- to 100-foot-thick diorite sill forms the footwall of the veins and the phyllite along this footwall contains finely disseminated pyrite and pyrrhotite. Augite lamprophyre also occurs in the footwall and augite melaphyre flows and breccias crop out east of the mine. The quartz veins form tabular bodies and lenses that trend north-northwest and dip shallowly to the northeast. They average 3 to 5 feet wide but locally are up to 30 feet thick (Knopf, 1912). The quartz contains arsenopyrite and native gold, and the ore averages 0.3 ounce of gold per ton. Between 1916 and 1982, at least 544 tons of ore were mined that yielded 211 ounces of gold and 8 ounces of silver. Some gold was also recovered between 1905 and 1915, but production records are not available (Redman and others, 1989). U.S. Bureau of Mines samples of quartz veins contained up to 15.3 ppm gold. The Bureau collected a 350 pound metallurgical sample in 1988 for cyanide amenability, flotation, and cyanide-leach-with-assay-screen-analysis tests. The deposit was drilled by FMC Corporation in 1988 (Redman and others, 1989).This prospect is in the Juneau Gold Belt, which consists of more than 200 gold-quartz-vein deposits that have produced nearly 7 million ounces of gold. These gold-bearing mesothermal quartz vein systems form a zone 160 km long by 5 to 8 km wide along the western margin of the Coast Mountains. The vein systems are in or near shear zones adjacent to west-verging, mid-Cretaceous thrust faults. The veins are hosted by diverse, variably metamorphosed, sedimentary, volcanic, and intrusive rocks. From the Coast Mountains batholith westward, the host rocks include mixed metasedimentary and metavolcanic sequences of Carboniferous and older, Permian and Triassic, and Jurassic-Cretaceous age. The sequences are juxtaposed along mid-Cretaceous thrust faults (Miller and others, 1994). The sequences are intruded by mid-Cretaceous to middle Eocene plutons, mainly diorite, tonalite, granodiorite, quartz monzonite, and granite. Sheetlike tonalite plutons emplaced just east of the Juneau Gold Belt and undeformed granite and granodiorite bodies that are emplaced farther to the east are between 55 and 48 Ma (Gehrels and others, 1991). The structural grain of the belt is defined by northwest-striking, moderately to steeply northeast-dipping, penetrative foliation that developed between Cretaceous and Eocene time (Miller and others, 1994). The majority of the veins in the Juneau Gold Belt strike northwest. Isotopic dates indicate that the auriferous veins in the Juneau Gold Belt formed between 56 and 55 Ma (Miller and others, 1994; Goldfarb and others, 1997).
|Geologic map unit||(-134.721989322424, 58.4402717000926)|
|Mineral deposit model||Low-sulfide Au-quartz vein (Cox and Singer, 1986; model 36a)|
|Mineral deposit model number||36a|
|Age of mineralization||Isotopic dates indicate that the auriferous veins in the Juneau Gold Belt formed between 56 and 55 Ma (Miller and others, 1994; Goldfarb and others, 1997).|
|Workings or exploration||The deposit at the Peterson Mine was discovered in 1897. Workings include 4 shafts, 11 adits, and numerous trenches (Redman and others, 1989). The deposit was drilled by FMC Corporation in 1988.|
|Indication of production||Yes; small|
|Production notes||Between 1916 and 1982, at least 544 tons of ore were mined that yielded 211 ounces of gold and 8 ounces of silver. Some gold was also recovered between 1905 and 1915 but production records are not available (Redman and others, 1989).|
Gehrels, G.E., McClelland, W.C., Samson, S.D., and Patchett, P.J., 1991, U-Pb geochronology of detrital zircons from a continental margin assemblage in the northern Coast Mountains, southeastern Alaska: Canadian Journal of Earth Sciences, v. 28, no. 8, p.1285-1300.
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.
Knopf, Adolph, 1912, The Eagle River region, southeastern Alaska: U.S. Geological Survey Bulletin 502, 61 p.
Miller, L.D., Goldfarb, R.J., Gehrels, G,E., and Snee, L.W., 1994, Genetic links among fluid cycling, vein formation, regional deformation, and plutonism in the Juneau gold belt, southeastern Alaska: Geology, v. 22, p. 203-206.
Redman, E.C., Maas, K.M., Kurtak, J.M., and Miller, L.D., 1991, Section D: Juneau Gold Belt subarea, in U.S. Bureau of Mines, Mineral investigations in the Juneau Mining District, Alaska, 1984-1988: Volume 2 - Detailed mine, prospect, and mineral occurrence descriptions: U.S. Bureau of Mines Special Publication VOL. 2D, 424 p., 19 sheets.
|Reporters||J.C. Barnett and L.D. Miller (Juneau, Alaska )|
|Last report date||12/15/2001|