Tenderfoot Creek

Site Name

Primary: Tenderfoot Creek

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Commodity

Primary: Gold
Secondary: Lead
Secondary: Silver

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Location

State: Alaska
District: Fairbanks

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Land Status

Not available

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Holdings

Not available

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Workings

Not available

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Ownership

Not available

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Production

Not available

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Deposit

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

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Physiography

Not available

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Mineral Deposit Model

Model Name: Placer Au-PGE

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Orebody

Not available

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Structure

Not available

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Alterations

Not available

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Rocks

Not available

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Analytical Data

Not available

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Materials

Ore: Galena
Ore: Gold

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Comments

Comment (Geology): Geologic Description = The Richardson area is characterized by gentle slopes and broad, alluvium-filled valleys (Prindle and Katz, 1913, p. 140). The area is unglaciated and largely overlain by windblown silt, sand, and loess, locally up to 50 meters thick (Foster and others, 1979). The bedrock in the region comprises greenschist to amphibolite facies schist, marble, and gneiss that have been intruded by various igneous bodies (Bundtzen and Reger, 1977, p. 29). The schist and marble are probably Paleozoic, and the gneiss has a probable protolith of Precambrian and Paleozoic sedimentary and igneous rocks (Weber and others, 1978). The intrusive bodies in the area range in composition from rhyolite to andesite. Fine-grained rhyolite containing quartz and feldspar phenocrysts is common throughout the area (Olson and others, 1985). At the nearby Democrat Lode (BD014), the rhyolite contains arsenopyrite, gold, and pyrite, and is albitic, clay, and sericite altered (R.J. Newberry, oral communication, 1998). Structurally, the Richardson region is cut by a northwest-trending fracture system termed the Richardson Lineament. The lineament appears to correspond with the distribution of the rhyolite and other intrusive bodies and placer gold deposits (Bundtzen and Reger, 1977, p. 29). Also, the lineament tends to separate gneissic rocks to the northeast from schistose rocks to the southwest (Swainbank and others, 1984). ? Tenderfoot Creek has been the largest gold producer in the Richardson district. However, the gold from Tenderfoot Creek is the lowest grade of any in the Yukon region (Chapin, 1914). Bundtzen and Reger (1977) reported a gold fineness of 670 for Tenderfoot Creek. Metz and Hawkins (1981) reported the average gold fineness to be 901. Glover (1920?) reported a range in gold fineness of 622 to 735 for Tenderfoot Creek. Mining operations occurred in the lower 4 miles of the creek. The alluvium ranges from 30 feet in thickness at the head of the creek to 155 feet near the mouth (Chapin, 1914). Pan concentrates contain amphibole, clinopyroxene, feldspar, garnet, gold, ilmenite, magnetite, quartz, sphene, and zircon (Bundtzen and Reger, 1977). Chapin (1914) reports that a piece of gold-bearing galena float was recovered during mining operations. However, the bedrock source was not found.? Placer gold was first discovered in the Richardson district in 1905. Mining initially occurred on Tenderfoot Creek and expanded to nearby Banner Creek (BD001) and associated tributaries. Because the depth to bedrock in the drainage is 30 to 155 feet, early mining on Tenderfoot Creek was largely by drifting methods (Ellsworth and Parker, 1911). In recent years, surface mining, utilizing earth moving equipment, has taken place in the upper portions of Tenderfoot Creek. After peak gold production in 1908, mining in the area declined (Olson and others, 1985). From 1905 through 1921, production for the Richardson district was approximately 95,000 ounces of gold and 24,000 ounces of silver (Bundtzen and Reger, 1977). Since 1980, the district has produced approximately 10,000 additional ounces of gold from intermittent mining (Olson and others, 1985). Production figures specifically for Tenderfoot Creek are not available, but it has been one of the major producers in the district.

Comment (Reference): Primary Reference = Cobb and Eberlein, 1980

Comment (Workings): Workings / Exploration = Placer gold was first discovered in the Richardson district in 1905. Mining initially occurred on Tenderfoot Creek and expanded to nearby Banner Creek (BD001) and associated tributaries. Because the depth to bedrock in the drainage is 30 to 155 feet, early mining on Tenderfoot Creek was largely by drifting methods (Ellsworth and Parker, 1911). In recent years, surface mining, utilizing earth moving equipment, has taken place in the upper portions of Tenderfoot Creek.

Comment (Exploration): Status = Inactive

Comment (Geology): Age = Quaternary

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

Comment (Production): Production Notes = After peak gold production in 1908, mining in the area declined (Olson and others, 1985). From 1905 through 1921, production for the Richardson district was approximately 95,000 ounces of gold and 24,000 ounces of silver (Bundtzen and Reger, 1977). Since 1980, the district has produced approximately 10,000 additional ounces of gold from intermittent mining (Olson and others, 1985). Production figures specifically for Tenderfoot Creek are not available, but it has been one of the major producers in the district.

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References

Reference (Deposit): Glover, A.E., 1950, Placer gold fineness: Alaska Territorial Department of Mines Miscellaneous Report 195-1, 38 p.

Reference (Deposit): Bundtzen, T.K., and Reger, R.D., 1977, The Richardson lineament-a structural control for gold deposits in the Richardson mining district, Alaska: Alaska Division of Geological and Geophysical Surveys Geologic Report 55, 46 p.

Reference (Deposit): Ellsworth, C.E., and Parker, G.L., 1911, Placer mining in the Yukon-Tanana region: U.S. Geological Survey Bulletin 480, 325 p.

Reference (Deposit): Saunders, R.H., 1965, A geochemical investigation in the Richardson area, Big Delta quadrangle, Alaska: Alaska Division of Mines and Minerals Geochemical Report 3, 11 p.

Reference (Deposit): Chapin, Theodore, 1914, Placer mining in the Yukon-Tanana region: U.S. Geological Survey Bulletin 592-J, p. 357-362.

Reference (Deposit): Prindle, L.M., and Katz, F.J., 1913, Detailed description of the Fairbanks district, in Prindle, L. M., A geologic reconnaissance of the Fairbanks quadrangle, Alaska: U.S. Geological Survey Bulletin 525, p. 59-152.

Reference (Deposit): Olson, B.G., Burton, J., Wolff, E.N., and Swainbank, R.D., 1985, Mining and minerals in the golden heart of Alaska: Fairbanks North Star Borough Publication, 80 p.

Reference (Deposit): Swainbank, R.C., Burton, J.P., and Metz, P.A., 1984, Bedrock geology of the Richardson mining district, Alaska: University of Alaska, Mineral Industry Research Laboratory Open-File Report 84-2, 60 p., 8 maps, scale 1:40,000.

Reference (Deposit): Metz, P.A., and Hawkins, D.B., 1981, A summary of gold fineness values from Alaska placer deposits: University of Alaska, Fairbanks, Mineral Industry Research Laboratory Report No. 45, 63 p.

Reference (Deposit): Eberlein, G.D., Chapman, R.M., Foster, H.L., and Gassaway, J.S., 1977, Map and table describing known metalliferous and selected nonmetalliferous mineral deposits in central Alaska: U.S. Geological Survey Open-File Report 77-168-D, 132 p., 1 map, scale 1:1,000,000.

Reference (Deposit): Weber, F.R., Foster, H.L., Keith, T.E.C., Dusel-Bacon, C., 1978, Preliminary geologic map of the Big Delta quadrangle, Alaska: U.S. Geological Survey Open-File Report 78-529A, 1 sheet, scale 1:250,000.

Reference (Deposit): Menzie, W.D., and Foster, H.L., 1979, Metalliferous and selected nonmetalliferous mineral resource potential in the Big Delta quadrangle, Alaska: U.S. Geological Survey Open-File Report 78-529D, 61 p., 1 sheet, scale 1:250,000.

Reference (Deposit): Cobb, E.H., and Eberlein, G.D., 1980, Summaries of data on and lists of references to metallic and selected nonmetallic mineral deposits in the Big Delta and Tanacross quadrangles, Alaska: U.S. Geological Survey Open-File Report 80-1086, 77 p.

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