Unnamed (on northern Akun Island)

The Unnamed (on northern Akun Island) is a sulfur 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: Unnamed (on northern Akun Island)

Commodity

Primary: Sulfur
Secondary: Zinc
Secondary: Mercury
Secondary: Copper

Location

State: Alaska
District: Aleutian Islands

Land Status

Not available

Holdings

Not available

Workings

Not available

Ownership

Not available

Production

Not available

Deposit

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

Physiography

Not available

Mineral Deposit Model

Not available

Orebody

Not available

Structure

Not available

Alterations

Alteration Type: L
Alteration Text: Argillic.

Rocks

Name: Andesite
Role: Associated
Age Type: Associated Rock
Age Young: Pliocene

Analytical Data

Not available

Materials

Ore: Pyrite
Ore: Silver
Ore: Sulfur

Comments

Comment (Commodity): Ore Material = Sulfur (native)

Comment (Geology): Age = Tertiary or younger.

Comment (Exploration): Status = Inactive

Comment (Commodity): Ore Material = Silver (native)

Comment (Workings): Workings / Exploration = Attempts to mine the sulfur at this site continued off and on from 1917 to at least 1937, as described in various U.S. Geological Survey reports (see following). Maddren (1919) reported that numerous trenches, ranging in depth from 4 to 15 feet had been dug in 1917 and that 2 samples had assayed 55.5 and 22.8 percent sulfur. Martin (1920) reported a test shipment in 1918. Brooks (1921, 1922, and 1923) reported that a commercial deposit of sulfur was being opened up and that equipment for mining and reduction of sulfur was supposed to be in place at the end of 1920. Nothing of consequence was reported until it was announced that in 1930 Pacific Coast Sulfur Company was organized to mine the sulfur with a steam shovel and transport it to the beach using an aerial tram (Smith, 1933). The tram was actually built and the remains of it have been noted by recent workers in the area. In 1935 the prospect was acquired by Alaska Northwest Sulfur Company. No record of any production has been found.? Resource Associates of Alaska examined and sampled the prospect in 1979 and in 1984, looking for precious metals (Butherus and others, 1979; Butherus, 1984). All samples were anomalous in mercury, and a few were anomalous in copper and zinc. No gold was detected.

Comment (Reference): Primary Reference = Maddren, 1919

Comment (Reserve-Resource): Reserves = Estimates of the sulfur resource range from 1,200 tons (Maddren, 1919) to 20,000 tons (Bain, 1979).

Comment (Deposit): Model Name = Solfataric sulfur

Comment (Deposit): Other Comments = This site is on land selected by the Aleut Native Corporation.

Comment (Geology): Geologic Description = Rocks at this site consist of andesitic flows, agglomerates, and tuff breccias which exhibit extreme argillic alteration (Butherus and others, 1979). These rocks are thought to be Tertiary or younger in age (Simpson, 1985). Native sulfur occurs with the altered rock. Several small zones of altered material occur over a 15 to 20 acre area. The main zone of alteration and sulfur mineralization measures approximately 500 by 1200 feet. The altered material varies from dull yellowish earthy masses to to gray pyritic clay. Maddren (1919) describes the surface material as a highly decomposed earthy zone having a thickness of 1 to 4 feet. Below this zone is a 6 to 10 foot layer of seimleached decomposed rock which appears to be massive clay.? A small amount of sulfur commonly occurs as thin encrustations on walls of fractures and cavities. The encrustations are generally less than 1/8 inch thick, but may be up to 1 inch thick. Some sulfur is also present as disseminations in the altered rock. Most of the sulfur occurs within 1 to 4 feet of the surface. Two samples collected in 1917 contained 55.5 and 22.8 percent sulfur (Maddren, 1919). Using an average thickness of 2 feet and a sulfur content of 40 percent, he estimated a total resource of 1200 tons. Bain (1979), however, cites a U.S. Geological Survey estimate of 15,000 to 20,000 tons.? Resource Associates of Alaska examined this area in 1979 and again in 1984, looking primarily for precious metals (Butherus and others, 1979; Butherus, 1984). Three samples collected in 1979 contained up to 270 ppm copper, 7.6 ppm mercury, 16 ppm tungsten, and 260 ppm zinc. No gold was detected. In 1984, sixty-seven samples were collected and all but one were highly anomalous in mercury. A few samples were also anomalous in copper and zinc.

References

Reference (Deposit): Smith, P.S., 1933, Mineral industry of Alaska in 1931: U.S. Geological Survey Bulletin 844-A, p. 1-81.

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): Butherus, D.L, Gressitt, E.E., Pray, J., Corner, N.G., Lindberg, P.H., and Fankhauser, R.E., 1979, Exploration and evaluation of the Aleut Native Corporation lands; Volume III: Resource Associates of Alaska, 69 p. 90 sheets, various sacales. (Report held by the Aleut Native Corporation, Anchorage, Alaska.)

Reference (Deposit): Smith, P.S., 1933, Mineral industry of Alaska in 1930: U.S. Geological Survey Bulletin 836-A, p. 1-83.

Reference (Deposit): Butherus, D., 1984, Exploration and evaluation of northern Akun Island and Walrus Peak-Littlejohn areas, Aleut Native Corporation Lands: Resource Associates of Alaska, 14 p. (Report held by the Aleut Native Corporation, Anchorage, Alaska.)

Reference (Deposit): Smith, P.S., 1937, Mineral industry in Alaska in 1935: U.S. Geological Survey Bulletin 880-A, p. 1-95.

Reference (Deposit): Bain, E.H., 1979, Alaska minerals as a basis for industry: U.S. Bureau of Mines Information Circular 7379, 89 p.

Reference (Deposit): Martin, G.C., 1920, The Alaska mining industry in 1918: U.S. Geological Survey Bulletin 712-A, p. 1-52.

Reference (Deposit): Brooks, A.H., 1921, The future of Alaska mining, in Martin G.C. and others, Mineral resources of Alaska, 1917: U.S. Geological Survey Bulletin 714, p. 5-57.

Reference (Deposit): Brooks, A.H., 1922, The Alaska mining industry in 1920: U.S. Geological Survey Bulletin 722-A, p. 1-74.

Reference (Deposit): Brooks, A.H., 1923, The Alaska mining industry in 1921: U.S. Geological Survey Bulletin 739, p. 1-50.

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., and Martin, G. C. 1921, The Alaska mining industry in 1919: U.S. Geological Survey Bulletin 714, p. 59-95.

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.