Gray Lead

The Gray Lead 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: Gray Lead

Commodity

Primary: Gold
Secondary: Antimony
Secondary: Silver
Secondary: Copper
Secondary: Lead

Location

State: Alaska
District: Goodpaster

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

Not available

Orebody

Not available

Structure

Not available

Alterations

Not available

Rocks

Name: Granite
Role: Associated
Age Type: Associated Rock
Age Young: Late Cretaceous

Analytical Data

Not available

Materials

Ore: Stibnite
Ore: Pyrite
Ore: Jamesonite
Ore: Gold
Ore: Digenite
Ore: Covellite
Ore: Arsenopyrite
Gangue: Quartz

Comments

Comment (Geology): Age = Postdates Cretaceous granodiorite intrusion

Comment (Deposit): Model Name = Shear hosted, magmatic-hydrothermal vein

Comment (Geology): Geologic Description = The area is characterized by rounded hills and flat-topped ridges (Thomas, 1970). The most prominent ridge is Black Mountain, which trends about 12 miles in a northerly direction and is underlain by a Cretaceous granodiorite (Weber and others, 1978). Several creeks flow westward off Black Mountain in steep, parallel, v-shaped valleys to form the Headwaters of Tibbs Creek. Bordering Black Mountain to the west is a combination of augen gneiss, gneissic schist, and schist. There is intense shearing and faulting in the contact between the metamorphic and intrusive rocks. This shearing is observed in the underground workings and at the surface as pronounced saddle-like depressions across the spurs separating the westward-flowing tributaries of Tibbs Creek. This shear zone trends roughly N15E and dips 65 degrees NW. The lode deposits in the area are gold-bearing quartz veins in the shear zone. Most of the veins are in the shear zone, although some are found in intrusive rocks. The veins contain gold and a variable combination of sulfides, including arsenopyrite, covellite, digenite, jamesonite, pyrite, and stibnite. Typically, gold content decreases as sulfides increase. Veins are commonly 2 to 3 feet in width, with some as wide as 8 feet (Thomas, 1970). When gold is present, it is usually extremely fine grained. However, several nearby veins such as the Blue Lead mine (BD003) and Grizzly Bear mine (BD018) contain relatively coarse gold, which is easily visible in hand specimen. ? the Gray Lead mine is centered on a quartz vein 2 feet in width. Based on underground workings, the vein dips steeply to the west (Joesting, 1938). Foster and others (1978) performed two emission spectroscopy analyses on rock samples from the Gray Lead mine: sample 74WR-181c contained greater than 10,000ppm As, 15 ppm Ba, 150 ppm Bi, 5 ppm Co, 1 ppm Cr, 7 ppm Cu, 50 ppm Pb, 500 ppm Se, and 4.0 ppm Au; and sample 74WR-181d contained 10,000ppm As, 30 ppm B, 300 ppm Ba, 10 ppm Bi, 2 ppm Cr, 50 ppm Cu, 50 ppm La, 5 ppm Nb, 7 ppm Pb, 7 ppm Sc, 20 ppm Sn, 7 ppm Sr, 30 ppm V, 15 ppm Y, 70 ppm Zr, and 1.5 ppm Au.? the Goodpaster region was first explored for placer gold in 1915. In the early 1930's, gold-bearing quartz veins were discovered in the upper Tibbs Creek area. By the winter of 1936, the first underground workings were being installed. The original base camp was on Summit Creek. A 450 foot tunnel was driven along a small vein, termed the Blue Lead Extension. After disappointing results, the work was stopped. In the summer of 1936, five men drove a 300-foot tunnel at the outcrop of the Blue Lead vein (Reed, 1937). During the winter of 1937, a 300-foot tunnel was driven at the Grizzly Bear mine (BD018) and a 50-ton mill was constructed. In the summer of 1938, the mill was moved to the Blue Lead mine and operated for a year and a half until the fall of 1939 (Joesting, 1938). Subsequently, from 1939 to 1941, approximately 1,300 feet of surface and subsurface workings were completed at the Gray Lead mine (Thomas, 1970). Over 300 feet of the vein was traced at the surface(Joesting, 1938). There was limited exploration reported in the 1970's. The mine shaft opening was accessible, but blocked by ice (Thomas, 1970). It is reported that 350 tons of ore was produced from the nearby Grizzly Bear mine and processed at the mill at the Blue Lead mine. Another 150 tons was produced from the Blue Lead mine (Reed, 1937). Thomas (1970) reports that no ore from the Gray Lead mine was taken to the mill. It is unknown how much, if any, ore was processed elsewhere.

Comment (Workings): Workings / Exploration = The Goodpaster region was first explored for placer gold in 1915. In the early 1930's, gold-bearing quartz veins were discovered in the upper Tibbs Creek area. By the winter of 1936, the first underground workings were being installed. The original base camp was on Summit Creek. A 450-foot tunnel was driven along a small vein, termed the Blue Lead Extension (BD003). After disappointing results, the work stopped. In the summer of 1936, five men drove a 300-foot tunnel at the outcrop of the Blue Lead vein (Reed, 1937). During the winter of 1937, a 300 foot tunnel was driven at the Grizzly Bear mine along with the construction of a 50-ton amalgamation recovery mill. In the summer of 1938, the mill was moved to the Blue Lead mine and operated for 1.5 years until the fall of 1939 (Joesting, 1938). Subsequently, from 1939 to 1941, approximately 1,300 feet of surface and subsurface workings were completed at the Grey Lead mine (Thomas, 1970). Over 300 feet of the surface expression of the vein was traced (Joesting, 1938). There has been limited exploration reported in the 1970's. The mine shaft opening is accessible, but blocked by ice (Thomas, 1970).

Comment (Exploration): Status = Inactive

Comment (Reference): Primary Reference = Thomas, 1970

Comment (Production): Production Notes = It is reported that 350 tons of ore was produced from the Grizzly Bear mine and processed at the mill at the Blue Lead mine. Another 150 tons was produced from the Blue Lead mine (Reed, 1937). Thomas (1970) reports that no ore from the Gray Lead mine was taken to the mill. It is unknown how much, if any, ore was processed elsewhere.

References

Reference (Deposit): Thomas, B.I., 1970, Reconnaissance of the gold-bearing quartz veins in the Tibbs Creek area, Goodpaster River, Big Delta quadrangle, central Alaska: U.S. Bureau of Mines Open-File Report 14-70, 12 p.

Reference (Deposit): Joesting, H.R., 1938, Mining and prospecting in the Goodpaster region: Alaska Territorial Department of Mines , 2 p.

Reference (Deposit): Smith, P.S., 1938, Mineral industry of Alaska in 1936: U.S. Geological Survey Bulletin 897-A, p. 1-107.

Reference (Deposit): Smith, P.S., 1939, Mineral industry of Alaska in 1938: U.S. Geological Survey Bulletin 917-A, p. 1-113.

Reference (Deposit): Saunders, R.H., 1967, Mineral occurences in the Yukon-Tanana region, Alaska: Alaska Division of Mines and Minerals Special Report 2, 58 p.

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.

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): Foster, H.L., Albert, N.R.D., Griscom, Andrew, Hessin, T.D., Menzie, W.D., Turner, D.L, and Wilson, F.H., 1979, The Alaskan Mineral Resource Assessment Program: Background information to accompany folio of geologic and mineral resource maps of the Big Delta quadrangle, Alaska: U.S. Geological Survey Circular 783, 19 p.

Reference (Deposit): Reed, I.M., 1937, Brief report on Goodpaster quartz lode mining at the head of Johnson and Boulder Creeks: Alaska Territorial Department of Mines , 1 p.

Reference (Deposit): Cobb, E.H., 1972, Metallic mineral resources map of the Big Delta quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-388, 1 sheet, scale 1:250,000.

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.

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.