The Gold Run is a gold mine located in Alaska.
About the MRDS Data:
All mine locations were obtained from the USGS Mineral Resources Data System. The locations and other information in this database have not been verified for accuracy. It should be assumed that all mines are on private property.
Mine Info
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Gold Run MRDS details
Site Name
Primary: Gold Run
Commodity
Primary: Gold
Secondary: Tungsten
Location
State: Alaska
District: Fairhaven
Land Status
Not available
Holdings
Not available
Workings
Not available
Ownership
Not available
Production
Not available
Deposit
Record Type: Site
Operation Category: Past Producer
Operation Type: Unknown
Years of Production:
Organization:
Significant:
Physiography
Not available
Mineral Deposit Model
Model Name: Placer Au-PGE
Orebody
Not available
Structure
Not available
Alterations
Not available
Rocks
Not available
Analytical Data
Not available
Materials
Ore: Gold
Ore: Scheelite
Ore: Wolframite
Gangue: Kyanite
Comments
Comment (Exploration): Status = Inactive
Comment (Geology): Age = Quaternary
Comment (Deposit): Model Name = Placer Au-PGE (Cox and Singer, 1986; model 39a)
Comment (Reference): Primary Reference = Cobb, 1975 (OFR 75-429)
Comment (Geology): Geologic Description = Placer gold was discovered on Gold Run Creek in 1908 and mining or exploration activities were reported for many years up to WW II (Cobb, 1975, OFR 75-429). Early mining was in ground 6 to 12 feet deep in the upper creek (Henshaw, 1910). Scheelite, wolframite, and kyanite were reported to be present in placer concentrates and kyanite was exposed in a placer cut (Anderson, 1947). Bedrock along the north and east side of Kiwalik Mountain is part of Lower Paleozoic metasedimentary assemblage that includes metamophosed felsic dikes or sills thought to be related to the Devonian Kiwalik Mountain gneiss (Till and others, 1986). The metasedimentary assemblage includes marble, metapelitic rocks, and in some areas quartz-mica rocks that may be metatuffs or exhalites. Felsic metavolcanic rocks are present in this assemblage at the HOM (BN077) and Big Bar (BN083) prospects. Some skarn-like rocks are also present locally on this side of Kiwalik Mountain. The Lower Paleozoic assemblage is inferred to lay unconformably on polydeformed metapelitic schist of Monument Mountain that may be Precambrian in age.
Comment (Workings): Workings / Exploration = Surface open-cut placer workings are present locally on this creek.
References
Reference (Deposit): Cobb, E.H., 1972, Metallic mineral resources map of the Bendeleben quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-417, 1 sheet, scale 1:250,000.
Reference (Deposit): Cobb, E.H., 1975, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Bendeleben quadrangle, Alaska: U.S. Geological Survey Open-File Report 75-429, 123 p.
Reference (Deposit): Till, A.B., Dumoulin, J.A., Gamble, B. ., Kaufman, D.S., and Carroll, P.I., 1986, Preliminary geologic map and fossil data, Soloman, Bendeleben, and southern Kotzebue quadrangles, Seward Peninsula, Alaska: U.S. Geological Survey Open-File Report 86-276, 10 p., 3 plates, scale 1:250,000.
Reference (Deposit): Anderson, Eskil, 1947, Mineral occurrences other than gold deposits in northwestern Alaska: Alaska Territorial Division of Mines Pamphlet 5-R, 48 p.
Reference (Deposit): Henshaw, F.F., 1910, Mining in Seward Peninsula: U.S. Geological Survey Bulletin 442, p. 353-371.
The Top Ten Gold Producing States
These ten states contributed the most to the gold production that built the West from 1848 through the 1930s. The Top Ten Gold Producing States.
