Nugget Creek

The Nugget 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

Satelite View

MRDS mine locations are often very general, and in some cases are incorrect. Some mine remains have been covered or removed by modern industrial activity or by development of things like housing. The satellite view offers a quick glimpse as to whether the MRDS location corresponds to visible mine remains.

Site Name

Primary: Nugget Creek

Commodity

Primary: Gold
Secondary: Tungsten

Location

State: Alaska
District: Juneau (Skagway subdistrict)

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

Name: Gravel
Role: Host
Age Type: Host Rock
Age Young: Holocene

Analytical Data

Not available

Materials

Ore: Gold

Comments

Comment (Workings): Workings / Exploration = Placer gold was discovered in 1899 but there was no development until 1902 (Wright, 1904 [B 236]). Sporadic mining occurred in 1902 to 1913, 1929, and since 1980 (Hoekzema and others, 1986). Remains of a small hydraulic plant exist on east side of creek 1.5 miles above junction with Tsirku River. A flume was used to divert the creek between 1902 and 1909 for hydraulic methods (Hoekzema and others, 1986). Gravels in the lower section of the Nugget Creek canyon were tested with suction dredges between 1980 and 1985 with encouraging results. The alluvial fan at the mouth of Nugget Creek was patented in 1934 (Hoekzema and others, 1986).

Comment (Production): Production Notes = Approximately 350 ounces of gold was produced by small hydraulic operations between 1902 and 1909 (Eakin, 1919).

Comment (Reference): Primary Reference = Hoekzema and others, 1986

Comment (Reserve-Resource): Reserves = A significant but untested, identified resource exists in the alluvial fan at the mouth of the creek which coalesces with the fan at the mouth of Cottonwood Creek to the west. Abandoned channels that may host placer gold have been identified in the fan between Cottonwood and Nugget Creeks (Hoekzema and others, 1986).

Comment (Geology): Age = Quaternary placer.

Comment (Exploration): Status = Probably inactive

Comment (Geology): Geologic Description = Some gold was mined on Nugget Creek beginning in 1899 and there has been sporadic mining since. Production has probably been small (Hoekzema and others, 1986). Wright (1904 [B 225 and B 236]) describes the deposit as primarily creek-bed gravels and low side-bench gravels. Deposits in the creek occur as rich pockets in potholes. The low- bench deposits are usually very narrow and from the bottom upward, typically consist of a 2-foot layer of glacial mud, a foot or more of cemented slate wash, a 10-foot bed of pay dirt, and a few feet of colluvium. Many large blocks of diorite occur in the pay gravels and substantially add to the cost of mining. However, Hoekzema and others (1986) also cite the presence of abandoned channels at higher elevations on the east side of the creek and an alluvial fan at the mouth of the creek. They report that alluvium in the lower canyon is 12 to 20 feet deep and that gold is found on or near bedrock,; little gold is found in the overlying gravels. the best value obtained by the U.S. Bureau of Mines contained 0.0138 ounces of gold per cubic yard in a sample collected from an abandoned channel adjacent to the Tsirku River. Gravel resources in the existing stream channel are small but have been shown to contain coarse gold by recent suction dredge operations. The average stream gradient is over 900 feet per mile.? the Nugget Creek placer mineralization lies within a northwest-trending zone of quartz-sulfide veining in sediments and slates in the Skagway B-4 quadrangle described by Wright (1904 [B 225 and B 236], Eakin (1918 and 1919), and MacKevett and others (1974) and considered to be the source of placer gold in this area.

Comment (Deposit): Model Name = Alluvial fan and paleo-channel placer deposits (Cox and Singer, 1986; model 39a).

References

Reference (Deposit): Still, J.C., Hoekzema, R.B., Bundtzen, T.K., Gilbert, W.G., Wier, K.R., Burns, L.E., and Fechner, S.A., 1991, Economic geology of Haines-Klukwan-Porcupine area, southeastern Alaska: Alaska Division of Geological and Geophysical Surveys Report of Investigations 91-4, 156 p., 5 sheets, scale 1:63,360.

Reference (Deposit): Still, J.C., 1991, Bureau of Mines mineral investigations in the Juneau mining district, Alaska, 1984 - 1988, v. 2, Detailed mine, prospect, and mineral occurrence descriptions, section A, Haines-Klukwan-Porcupine subarea: U.S. Bureau of Mines of Mines Special Publication, 214 p.

Reference (Deposit): Hoekzema, R.B., Fechner, S.A., and Bundtzen, T.K., 1986, Distribution, analysis, and recovery of placer gold from the Porcupine mining area, southeast Alaska: U.S. Bureau of Mines Open-File Report 89-86, 49 p., 4 sheets.

Reference (Deposit): Redman, E.C., Gilbert, W.G., Jones, B.K., Rosenkrans, D.S., and Hickok, B.D., 1985, Preliminary bedrock-geologic map of the Skagway B-4 Quadrangle: Alaska Division of Geological and Geophysical Surveys Report of Investigations 85-6, 1 sheet, scale 1:40,000.

Reference (Deposit): Berg, H.C., 1984, Regional geologic summary, metallogenesis, and mineral resources of southeastern Alaska: U.S. Geological Survey Open-file Report 84-572, 298 p., 1 plate, scale approx. 1:600,000.

Reference (Deposit): Wright, C.W., 1904, The Porcupine district, Alaska: U.S. Geological Survey Bulletin 236, 35 p.

Reference (Deposit): Eakin, H.M., 1919, The Porcupine gold placer district, Alaska: U.S. Geological Survey Bulletin 699, 29 p.

Reference (Deposit): Still, J.C., Weir, K.R., Gilbert, W.G., and Redman, E.C., 1984, Stream-sediment, float, and bedrock sampling in the Porcupine mining area, southeast Alaska: U.S. Bureau of Mines Open-File Report 173-84, 19 p.

Reference (Deposit): Eakin, H.M., 1918, Gold placer mining in the Porcupine district: U.S. Geological Survey Bulletin 662-B, p. 93-100.

Reference (Deposit): Wright, C.W., 1904, The Porcupine placer mining district, Alaska in Emmons, S.F., and Hayes, C.W., eds., Contributions to economic geology 1903: U.S. Geological Survey Bulletin 225, p. 60-63.

Reference (Deposit): Cobb, E.H., 1972, Metallic mineral resources map of the Skagway quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-424, 1 sheet, scale 1:250,000.

Reference (Deposit): Cobb, E.H., 1978, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Mt. Fairweather and Skagway quadrangles, Alaska: U.S. Geological Survey Open-File Report 78-316, 123 p.

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.