Lower Gold Standard

The Lower Gold Standard 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: Lower Gold Standard
Secondary: Lone Jack (Helm Bay)
Secondary: Alaska
Secondary: Free Gold

Commodity

Primary: Gold
Secondary: Bismuth
Secondary: Lead

Location

State: Alaska
District: Ketchikan

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: Low-sulfide Au-quartz vein

Orebody

Not available

Structure

Not available

Alterations

Alteration Type: L
Alteration Text: Locally, the wallrock next to the veins is bleached and impregnated with pyrite.

Rocks

Not available

Analytical Data

Not available

Materials

Ore: Tetradymite
Ore: Pyrite
Ore: Gold
Ore: Galena
Gangue: Quartz
Gangue: Chlorite
Gangue: Calcite

Comments

Comment (Deposit): Model Name = Low-sulfide gold-quartz vein (Cox and Singer, 1986; model 36a)

Comment (Reference): Primary Reference = Brooks, 1902; Maas and others, 1995

Comment (Geology): Age = Late Cretaceous.

Comment (Deposit): Other Comments = the Gold Standard was the largest producer of gold and silver in the Helm Bay area. In early reports, it was also referred to as the Alaska and Free Gold claims (Cobb and Elliott, 1980, p. 46).

Comment (Workings): Workings / Exploration = The deposit was discovered in 1897 and mined intermittently from 1898 to 1941. It was developed by a 150-foot shaft and 700 feet of drifts and tunnels on two levels. A ten-stamp mill on the site was installed in 1899 and was still operating at 20 tons per day in 1938. An average grade of $6.00 Au/ton was reported in 1922 (Brooks, 1922, p. 35). ? Maas and others (1995, p. 192) report a 1300-foot adit and two glory holes at the lower Gold Standard mine, and a nine-foot adit on the Lone Jack claim. They also report (p. 191) that the entire lower Gold Standard adit was sampled by private interests as recently as 1993, but the gold values were subeconomic.

Comment (Geology): Geologic Description = The country rocks near this site are marine, andesitic and basaltic metavolcanic rocks that are gradationally interbedded with flyschlike metasedimentary rocks (Berg and others, 1988, p. 18). The strata were regionally metamorphosed to greenschist-grade phyllite and semischist in Late Cretaceous time (Brew, 1996, p. 27). The depositional age of the strata is uncertain. Berg and others (1998, p. 17) report that they closely resemble Upper Jurassic to mid-Cretaceous strata nearby on Gravina Island. ? the deposit consists of auriferous, pyritic quartz fissure veins in schistose metavolcanic (greenstone) and subordinate metapelitic rocks (Brooks, 1902, p. 59-60; Wright and Wright, 1908, p. 153-155; Cobb and Elliott, 1980, p. 46). There are two sets of veins: both sets strike N25W, parallel to the foliation of the schistose hostrocks, but dip in opposite directions. The older set dips 60-85 NE, parallel to the foliation, and contains the best ore, especially at the intersection of the two vein systems (Brooks, 1902, p. 59). The principal vein is 6 inches to 6 feet thick and has been traced along strike for more than 1000 feet. It consists of quartz, calcite, and chlorite, and, in addition to free gold, contains pyrite and minor tetrahedrite and galena. The walls of the vein are well defined by slickensides with gouge on the footwall side, and by a seam filled with calcite carrying free gold along the hanging wall. Locally, the wallrock next to the veins is bleached and impregnated with pyrite (Maas and others, 1995, p. 183). ? Maas and others (1995, table 25) report the following average metal contents in their samples from the lower Gold Standard mine: 10.4 ppm Au, 99 ppm Cu, 7.4 ppm Pb, 48 ppm Zn, 2.3 ppm Te, and 9.6 ppm Sn. They also report (table 24) that the average gold content in quartz at two places on this property is 8.12 and 8.71 ppm, and that the average gold content in pyritic schist is 17.0 and 35.9 ppm. The sampling by Maas and others (1995, p. 184) shows a distinct northward plunge to the ore zone, which is cut off by a fault that strikes NE and dips 45SE. The continuation of the ore zone past this fault has not yet been determined.? Fluid inclusion studies of quartz vein material from several of the Helm Bay lodes suggest that the veins formed at temperatures and pressures consistent with conditions during the Late Cretaceous greenschist-grade regional metamorphism (Maas and others, 1995, p. 184).

Comment (Production): Production Notes = Maas and others (1995, p. 192) report that the combined production from the lower and upper Gold Standard mines from about 1898 to 1941 was 310 kg or more of gold, and 33 kg or more of silver. They do not report the amount produced only from the lower Gold Standard. Judging from the assay values and the extent of the workings, production from each mine may have been about equal. In addition to the lode production, a little placer gold was mined in 1913 from near the main outcrop of the vein (Cobb and Elliott, 1980, p. 46).

References

Reference (Deposit): Brew, D.A., 1996, Geologic map of the Craig, Dixon Entrance, and parts of the Ketchikan and Prince Rupert quadrangles, southeastern Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-2319, 53 p., 1 sheet, scale 1:250,000.

Reference (Deposit): Maas, K.M., Bittenbender, P E., and Still, J.C., 1995, Mineral investigations in the Ketchikan mining district, southeastern Alaska: U.S. Bureau of Mines Open-File Report 11-95, 606 p.

Reference (Deposit): Cobb, E.H., and Elliott, R.L., 1980, Summaries of data on and lists of references to metallic and selected nonmetallic mineral deposits in the Ketchikan and Prince Rupert quadrangles, Alaska: U.S. Geological Survey Open-File Report 80-1053, 154 p.

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

Reference (Deposit): Elliott, R.L., Berg, H.C., and Karl, Susan, 1978, map and table describing metalliferous and selected nonmetalliferous mineral deposits, Ketchikan and Prince Rupert quadrangles, Alaska: U.S. Geological Survey Open-file Report, 78-73-B,17 p., scale 1:250,000.

Reference (Deposit): Berg, H.C., Elliott, R.L., and Koch, R.D., 1988, Geologic map of the Ketchikan and Prince Rupert quadrangles, southeastern Alaska: U.S. Geological Survey Mineral Investigations Series Map MF-1807,27 p., scale 1:250,000.

Reference (Deposit): Brooks, A.H., 1902, Preliminary report on the Ketchikan mining district, Alaska, with an introductory sketch of the geology of southeastern Alaska: U.S. Geological Survey Professional Paper 1, 120 p.

Reference (Deposit): Wright, F.E., and Wright, C.W., 1908, The Ketchikan and Wrangell mining districts, Alaska: U.S. Geological Survey Bulletin 347, 210 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.