Anvil Creek

The Anvil Creek 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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Site Name

Primary: Anvil Creek

Commodity

Primary: Gold
Secondary: Lead
Secondary: Silver
Secondary: Tungsten

Location

State: Alaska
District: Nome

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 Au-PGE

Orebody

Not available

Structure

Not available

Alterations

Not available

Rocks

Not available

Analytical Data

Not available

Materials

Ore: Galena
Ore: Gold
Ore: Magnetite
Ore: Scheelite
Gangue: Garnet

Comments

Comment (Exploration): Status = Active

Comment (Reference): Primary Reference = Collier and others, 1908

Comment (Geology): Geologic Description = increase of gold price in 1968, especially in the bowl between Nekula and Specimen Gulches. From 1993 until at least 1995, virgin bench deposits on the east side were mined by open-cut methods. These deposits and some of those in upper Anvil Creek could not be mined in earlier years because of conflicts with water supply, roads, and railroads. The shallow placers exploited early in the history of Anvil Creek probably averaged about 0.25 ounce of gold per cubic yard; some contained as much as 2.5 ounces of gold per cubic yard. Production in the first five years was about 1,000,000 dollars per year, or a total of about 250,000 ounces. The largest nugget reported was a gold-quartz nugget containing about 129 ounces of gold (Moffit, 1913, p. 79-83). Total production to date is probably about 500,000 ounces. The Anvil Creek fault zone transects the area more or less along Anvil Creek. This fault is a through-going, high-angle structure that juxtaposes different types of graphitic schist in this area (Hummel, 1962 [MF 247]). Bedrock is mostly graphitic schist that probably of early Paleozoic protolith age (Hummel, 1962 [MF-247]; Sainsbury, Hummel, and Hudson, 1972 [OFR 72-326]; Till and Dumoulin, 1994; Bundtzen and others, 1994).

Comment (Geology): Age = Quaternary; parts of Anvil Creek are at low enough elevations to have been influenced by Quaternary sea-level fluctuations.

Comment (Production): Production Notes = Anvil Creek is a major gold producer in the Nome mining district; the estimated total gold production is 500,000 ounces.

Comment (Workings): Workings / Exploration = Gold was discovered on Anvil Creek in September, 1898, and by the end of the year all of Anvil Creek between the coastal plain and Nekula Gulch was staked. From 1899 to 1902, rich and shallow alluvial deposits were mined, mostly by small-scale methods. Production from bench deposits began by 1903; they were mined partly by hydraulic elevators and partly by mechanical-hydraulic methods. Anvil Creek was dredged from about 1922 until 1932. In the 1930's, bench pay was mined, including the bench deposits near Specimen Gulch. In the 1990's, virgin ground was mined above Specimen Gulch and between Specimen Gulch and the coastal plain on the east side of Anvil Creek. These deposits could not be mined earlier because of land or water conflicts.

Comment (Geology): Geologic Description = Placer gold was discovered on lower Anvil Creek at an elevation of about 150 feet on September 22, 1898; by the end of 1898, the creek was staked between the coastal plain and Nekula Gulch (U.S. Mineral Survey plats, especially No. 722). The discoverers were the principals of the Pioneer Mining Company, Lindeberg, Lindblom, and Brynteson, and their associates. One claim, Nine Above, was initially proposed to be staked for Eskimos named Gabriel Adams and Constantine Uparazuck in recognition of their aid. The claim was otherwise staked and litigation over Nine Above lasted for decades. The operators recovered about 100 ounces of gold soon after their discovery, but it was to late in the season for intensive mining (Collier and others, 1908, p. 17-18). Intensive mining began in 1899; nuggets weighing between 20 and 25 ounces were found, and in 1900 about 1,750,000 dollars (85,000 ounces) worth of placer gold was produced on Anvil Creek. Cumulative production from discovery until the end of 1900 was estimated at 3,000,000 dollars or about 145,000 ounces of fine gold (Schrader and Brooks, 1900, p. 17; Brooks and others, 1901, p. 69, 71-74). The valley bottom placer was nearly exhausted by the end of 1902 (Collier and others, 1908, p. 31). The width of pay ranged from about 50 feet in the lower canyon to as much as 500 feet above Specimen Gulch. In the canyon, the pay gravel was 3 to 5 feet thick under a thin cover of muck and clay. Most of the gold was on bedrock, but it occurred throughout the gravel and in the top 1 to 2 feet of bedrock. By 1902, bench deposits were being mined (Brooks, 1903), especially on the east side of Anvil Creek (Collier and others, 1908, see figure 11, p. 189). The first hydraulic lifts were installed in about 1903, and a steam shovel was in use by 1904 (Brooks, 1905). Engineer C.W. Purington presented data on mining costs and methods and reported that gold from the bench gravels was very slightly purer than gold from the creeks; most of the gold was very close to 900 fine (Purington, 1905). Dredging of previously mined ground was introduced by 1922 (Brooks and Capps, 1924) and lasted until about 1929 (Smith, 1932). Two east-side benches were channels incised in bedrock. In places gold-bearing gravels spilled over the downhill bedrock rims of the channels, and bench placer pay mingled with the creek channel placers. In one cut, granitic boulders as well as a 40-pound galena nugget were found (Collier and others, 1908, p. 191). Placer gold in Anvil Creek had multiple sources. Some could have been derived from mineralized bedrock exposed on Banner Peak, Bonanza Hill, and the saddle between Anvil Creek and Snow Gulch. Much of the gold, however, apparently came from high-level placers near Nekula Gulch at the head of Anvil Creek. Mining of rich bench deposits on the east side of upper Anvil Creek took place until World War II (Smith, 1941, 1942). Mining commenced again on a moderate scale after the

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

References

Reference (Deposit): Schrader, F.C., and Brooks, A.H., 1900, Preliminary report on the Cape Nome gold region, Alaska: U.S. Geological Survey Special Publication, 56 p.

Reference (Deposit): Till, A.B., and Dumoulin, J.A, 1994, Geology of Seward Peninsula and St. Lawrence Island, in Plafker, G., and Berg, H.C., eds., The Geology of Alaska: Geological Society of America, The Geology of North America, DNAG, v. G-1, p. 141-152.

Reference (Deposit): Bundtzen, T.K., Reger, R.D., Laird, G.M., Pinney, D.S., Clautice, K.H., Liss, S.A., and Cruse, G.R., 1994, Progress report on the geology and mineral resources of the Nome mining district: Alaska Division of Geological and Geophysical Surveys, Public Data-File 94-39, 21 p., 2 sheets, scale 1:63,360.

Reference (Deposit): Sainsbury, C.L., Hummel, C.L., and Hudson, Travis, 1972, Reconnaissance geologic map of the Nome quadrangle, Seward Peninsula, Alaska: U.S. Geological Survey Open-File Report 72-326, 28 p., 1 sheet, scale 1:250,000.

Reference (Deposit): Cobb, E.H., 1972, Metallic mineral resources map of the Nome quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-463, 2 sheets, scale 1:250,000.

Reference (Deposit): Smith, P.S., 1932, Mineral industry of Alaska in 1929, in Smith, P.S., and others Mineral resources of Alaska, report on progress of investigations in 1929: U.S. Geological Survey Bulletin 824-A, p. 1-81.

Reference (Deposit): Hummel, C.L., 1962, Preliminary geologic map of the Nome C-1 quadrangle, Seward Peninsula, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-247, 1 sheet, scale 1:63,360.

Reference (Deposit): Cobb, E.H., 1978, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Nome quadrangle, Alaska: U.S. Geological Survey Open-File report 78-93, 213 p.

Reference (Deposit): Collier, A. J., Hess, F.L., Smith, P.S., and Brooks, A.H., 1908, The gold placers of parts of Seward Peninsula, Alaska, including the Nome, Council, Kougarok, Port Clarence, and Goodhope precincts: U.S. Geological Survey Bulletin 328, 343 p.

Reference (Deposit): Moffit, F.H., 1913, Geology of the Nome and Grand Central quadrangles, Alaska: U.S. Geological Survey Bulletin 533, 140 p.

Reference (Deposit): Brooks, A.H. and Capps, S.R., 1924, Mineral industry in Alaska, 1922: U.S. Geological Survey Bulletin 755, p. 1-56.

Reference (Deposit): Brooks, A.H., 1904, Placer mining in Alaska in 1903: U.S. Geological Survey Bulletin 225, p. 43-59.

Reference (Deposit): Brooks, A.H., 1905, Placer mining in Alaska in 1904: U.S. Geological Survey Bulletin 259, p. 18-31.

Reference (Deposit): Purington, C.W., 1905, Methods and costs of gravel and placer mining in Alaska: U.S. Geological Survey Bulletin 263, 273 p.

Reference (Deposit): Brooks, A.H., 1903, Placer gold mining in Alaska in 1902: U.S. Geological Survey Bulletin 213, p. 41-48.

Reference (Deposit): Brooks, A.H., Richardson, G. B., and Collier, A. J., 1901, Reconnaissance in the Cape Nome and Norton Bay regions, Alaska, in 1900: U.S. Geological Survey Special Publication, p. 1-180.

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