Fox Gulch

The Fox Gulch is a 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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Site Name

Primary: Fox Gulch

Commodity

Secondary: Gold
Secondary: Chromium

Location

State: Alaska
District: Goodnews Bay

Land Status

Not available

Holdings

Not available

Workings

Not available

Ownership

Not available

Production

Not available

Deposit

Record Type: Site
Operation Category: Producer
Operation Type: Unknown
Years of Production:
Organization:
Significant:

Physiography

Not available

Mineral Deposit Model

Model Name: Placer PGE-Au

Orebody

Not available

Structure

Not available

Alterations

Not available

Rocks

Not available

Analytical Data

Not available

Materials

Ore: Chromite
Ore: Gold
Ore: Ilmenite
Ore: Magnetite

Comments

Comment (Production): Production Notes = If 0.02 ounce of PGM per cubic yard were recovered from 160,000 yards of pay, Fox Gulch produced 3,200 ounces of PGM.

Comment (Exploration): Status = Active?

Comment (Workings): Workings / Exploration = Placer tailings are present along about 1/2 mile of lower Fox Gulch. Small-scale mining took place as early as 1927 and continued intermittently until 1934, when the Goodnews Bay Mining Company started larger-scale dragline operations in the area (Mertie, 1940). The deposit was worked out by WWII. Mining was continuous from Fox Gulch downstream into Platinum Creek.

Comment (Geology): Geologic Description = Fox Gulch is where platinum was first discovered in the Salmon River area (1926). It has been placer mined for about 0.4 mile upstream from its junction with Platinum Creek. The headwaters of Fox Gulch are in dunite of the Red Mountain ultramafic pluton, and it also flows across border zone clinopyroxenite and hornblende-bearing rocks. In the area of mining, however, the bedrock is part of an assemblage that includes sheared argillite, graywacke, and mafic to intermediate, fine-grained igneous rocks that are difficult to identify because of their decomposed character where exposed in mining cuts (Mertie, 1940). These strata are included in a regional sedimentary and volcanic assemblage that ranges in age from Paleozoic to Mesozoic (Hoare and Coonrad, 1978). Gravels in lower Fox Gulch are up to 12 feet thick, but they thin upstream.The gravels are coarse, subangular, and locally derived and contain boulders averaging 8 to 12 inches in diameter. The average width of the paystreak was 75 feet and it extended at least 2,600 feet upstream from the mouth of Fox Gulch. Platinum was concentrated in the lower few feet of gravel, on bedrock, and in fractures in bedrock. Chromite is common in the heavy-mineral concentrates and some chromite grains are intergrown with PGM. The U. S. Bureau of Mines collected 4 samples from the present drainage. These samples contained 0.0009 to 0.0378 ounce of PGM per cubic yard (Fechner, 1988, p. 80) The highest grade sample was from unmined material in the upper part of the gulch. One sample of tailings in Fox Gulch contained 0.0121 ounce of PGM per cubic yard (Fechner, 1988). Microprobe analyses of PGM grains from these samples showed 1.3 to 1.9 percent Rh, 0.7 to 1.0 percent Ru, 37.7 to 48.6 percent Pt, 26.7 to 41.3 percent Ir, 9.8 to 13.4 percent Os, and 4.1 to 8.4 percent Fe. PGM-bearing phases that were identified in these samples included iron-platinum alloy containing 8 to 30 percent Fe; iron-platinum alloy with minor osmiridium inclusions; and hollingsworthite, irarsite, iridarsenite, iridium, sperrylite, and platarsite (Fechner, 1988, p. 80). The mean of 26 analyses of PGMs (recalculated to exclude impurities) recovered during mining from Fox Gulch and Platinum Creek above Squirrel Creek was 63.71% Pt, 28.01% Ir, 5.39% Os, 0.47% Ru, 1.82% Rh, 0.23% Pd, and 0.37% Au. Six samples from Fox Gulch, recalculated free of impurities, averaged 50.56 percent Pt, 39.14 percent Ir, 7.74 percent Os, 0.71 percent Ru, 1.62 percent Rh, 0.14 percent Pd, and 0.09 percent Au (Mertie, 1976). Fechner (1988) estimates that there are 160,000 cubic yards of tailings on Fox Gulch that contain 0.012 ounce of PGM per cubic yard and 20,000 cubic yards of unmined material that contain 0.02 ounce of PGM per cubic yard.

Comment (Reference): Primary Reference = Mertie, 1976

Comment (Reserve-Resource): Reserves = Fechner (1988) estimates that there are 160,000 cubic yards of tailings on Fox Gulch that contain 0.012 ounce of PGM per cubic yard and 20,000 cubic yards of unmined material that contain 0.02 ounce of PGM per cubic yard.

Comment (Geology): Age = Quaternary.

Comment (Deposit): Model Name = Placer PGE-Au (Cox and Singer, 1986; model 39b)

References

Reference (Deposit): Cobb, E.H., 1972, Metallic mineral resources map of the Hagemeister Island quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-362, 1 sheet, scale 1:250,000.

Reference (Deposit): Mertie, J.B., Jr., 1940, The Goodnews platinum deposits, Alaska: U.S. Geological Survey Bulletin 918, 97 p.

Reference (Deposit): Cobb, E.H., 1980, Summaries of data and lists of references to metallic and selected nonmetallic mineral deposits in fifteen quadrangles in southwestern and west-central Alaska: U.S. Geological Survey Open-File Report 80-909, 103 p.

Reference (Deposit): Alaska Earth Sciences, 2000, The Goodnews Bay ultramafic complexes: Unpublished data, http://aes.alaska.com/UMAF/FIGURES/page4.html
URL: http://aes.alaska.com/UMAF/FIGURES/page4.html

Reference (Deposit): Mertie, J.B., Jr., 1976, Platinum deposits in the Goodnews Bay district, Alaska: U.S. Geological Survey Professional Paper 938, 42 p.

Reference (Deposit): Hoare, J.M., and Coonrad, W.L., 1978, Geologic map of the Goodnews and Hagemeister Island quadrangles region, southwestern Alaska: U.S. Geological Survey Open-File Report 78-9-B, two sheets, scale 1:250,000.

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