Grant

The Grant 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: Grant

Commodity

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

Location

State: Alaska
District: Fairbanks

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

Alteration Text: The O'Dea vein-fault zone is heavily oxidized; it consists of gold-bearing quartz breccia cemented by iron, arsenic and antimony oxides, broken schist fragments, mylonite, and minor sulfides (Bundtzen and Kline, 1981).

Rocks

Role: Host
Age Type: Host Rock
Age Young: Proterozoic

Analytical Data

Not available

Materials

Ore: Arsenic
Ore: Arsenopyrite
Ore: Galena
Ore: Gold
Ore: Scheelite
Gangue: Goethite
Gangue: Muscovite

Comments

Comment (Exploration): Status = Inactive

Comment (Commodity): Ore Material = antimony oxides

Comment (Reserve-Resource): Reserves = The results of the 1990 ACNC drilling on a portion of the O'Dea vein system show a resource of 212,000 tons of material that contains 0.36 ounce of gold per ton (Swainbank and others, 1991, p. 11).

Comment (Reference): Primary Reference = Bundtzen and Kline, 1981

Comment (Deposit): Model Name = Structurally controlled, auriferous vein-fault deposit hosted in polymetamorphic schist and quartzite.

Comment (Geology): Geologic Description = The Grant mine consists of two, structurally controlled, gold-bearing vein-fault deposits, hosted in polymetamorphic schist and quartzite: the Irishman zone (FB057) and the O'Dea zone. From December 1980 to June 1981, Bundtzen and Kline (1981) spent 25 days mapping the underground workings at the Grant mine, and the following is a summary of their work. At the Irishman vein-fault system, late-stage silica injection was accompanied by free gold, arsenopyrite, lead-antimony sulfosalts and rare scheelite. Ore fluids were emplaced along a fault zone trending sinuously N. 20-40 E. and dipping steeply to the southeast. On the 150-foot and 200-foot levels, the vein-fault dips from 58 to 72 degrees, but it flattens out to 15 to 35 degrees in raises above the 100-foot level, where it intersects incompetent graphite-muscovite schist. Vein widths vary from 3 to more than 22 inches and average about 13 inches wide on the 100-foot and 150-foot levels. By 1982, underground exploration and development had shown that the Irishman vein was more than 400 feet long and had not bottomed out in the lowest workings. The deposit probably continues beyond the southwest end of the ore body that has been explored, but the northeast end is cut by a north-northwest-striking joint-fault system. The O'Dea breccia zone consists of auriferous quartz breccia cemented by iron, arsenic, and antimony oxides, broken schist fragments, mylonite, and minor sulfides. The width of the vein-fault system varies from 6 inches to more than 6 feet. Multiple injections of silica also occurred along the O'Dea breccia zone, but unlike the Irishman system, recurrent movement along the vein-fault zone resulted in heavily oxidized, broken, and brecciated zones. The first recorded exploration at this site occurred in 1929, when lode gold mineralization was found at the bottom of an old shaft that was sunk for placer prospecting. The shaft was sunk through muck and gravel to bedrock which dipped east at a steep angle (Hill, 1933, p. 150). This original shaft was continued in bedrock to a depth of 240 feet and had 280 feet of drifts on the 200-foot and 240-foot levels. The 5- to 6-foot-wide quartz vein was said to strike N. 40 E. and dip 65 E. (Hill, 1933). Before 1931, approximately 500 to 600 tons of ore was milled from this vein. Exploration and development at the mine has been intermittent since the 1920's. Prior to 1950, about 6,000 tons of ore were mined from the Irishman vein (Eakins and others, 1985, p. 16). From 1979 to 1981, Tri-Con Mining, operator for Silverado Gold Mines, Ltd., at the Grant gold mine, engaged in an aggressive exploration and development program on the Irishman, O'Dea, and other gold-bearing shear zones on the Grant property (Eakins and others, 1985, p. 16). Underground workings consisted of 3,600 feet of drifts, crosscuts, and raises on and above the 200-foot level of the O'Dea zone (Bundtzen and Kline, 1981). During 1984, a $1.9 million exploration program was completed at the Grant mine (Eakins and others, 1985, p. 16). The drilling program defined an ore system on the O'Dea zone that extends 4,000 feet on strike and is as much as 1,000 feet deep. In 1985, the Grant mine recovered 1,563 ounces of gold and 1,178 ounces of silver from 5,036 tons of ore (Bundtzen and others, 1986, p. 26). During the seven weeks of mine production in 1989, the mill processed 8,000 tons which yielded 732 ounces of gold and 138 ounces of silver. From December 1987 to February 1989 when the mine closed, the Grant mine produced a total of 9,454 ounces of gold and 3,658 ounces of silver from 96,555 tons of ore at an average grade of 0.098 ounce of gold per ton (Bundtzen and others, 1990, p. 36-37).

Comment (Production): Production Notes = Prior to 1950, about 6,000 tons of ore were mined from the Irishman vein (Eakins and others, 1985, p. 16). In 1985, the Grant mine recovered 1,563 ounces of gold and 1,178 ounces of silver from 5,036 tons of ore (Bundtzen and others, 1986, p. 26). During the seven weeks of mine production in 1989, the mill processed 8,000 tons, which yielded 732 ounces of gold and 138 ounces of silver. From December 1987 to February 1989 when the mine closed, the Grant mine produced a total of 9,454 ounces of gold and 3,658 ounces of silver from 96,555 tons of ore at an average grade of 0.098 ounce of gold per ton (Bundtzen and others, 1990, p. 36-37). In early 1989, after the 100,000-ton tailings pond filled up at the Grant mine, the company decided that the costs for construction and permitting of a new tailings facility was prohibitive, and mining was shut down (Bundtzen and others, 1990, p. 37).

Comment (Geology): Age = Gold-bearing quartz veins cut Fairbanks Schist host rocks that are considered to be pre-Devonian and probably Proterozoic in age (Newberry and others, 1996).

Comment (Workings): Workings / Exploration = The first recorded exploration at this site occurred in 1929, when lode gold mineralization was found at the bottom of an old shaft that was sunk for placer prospecting. The shaft was sunk through muck and gravel to bedrock, which dipped east at a steep angle (Hill, 1933, p. 150). This original shaft was continued in bedrock to a depth of 240 feet and had 280 feet of drifts on the 200-foot and 240-foot levels. Exploration and development at the mine has been intermittent since the 1920's. From 1979 to 1981, Tri-Con Mining, operator for Silverado Gold Mines, Ltd., at the Grant gold mine, engaged in an aggressive exploration and development program on the Irishman, O'Dea, and other gold-bearing shear zones on the Grant property (Eakins and others, 1985, p. 16). Underground workings consisted of 3,600 feet of drifts and crosscuts and raises on and above the 200-foot level of the O'Dea zone (Bundtzen and Kline, 1981). The principal levels at the Irishman vein were at the 100-foot, 150-foot and 200-foot levels (Bundtzen and Kline, 1981). During 1984, a $1.9 million dollar exploration program was completed at the Grant mine (Eakins and others, 1985, p. 16). The drilling program defined an ore system on the O'Dea zone that extends 4,000 feet along strike and is as much as 1,000 feet deep. Late in 1989, Silverado Gold Mines, Ltd., signed an option agreement with American Copper and Nickel (ACNC) to explore and develop Silverado mining properties on Ester Dome, including the Grant mine property (Bundtzen and others, 1990, p. 37). In 1990, ACNC drilled 17,434 feet of core in the O'Dea vein system and on the Ethel vein system 2,000 feet to the north (Swainbank and others, 1991). ACNC also conducted an aerial geophysical survey of the area that same year (Bundtzen and others, 1991).

References

Reference (Deposit): Cobb, E.H., 1972, Metallic mineral resources map of the Fairbanks quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-410, 1 sheet, scale 1:250,000.

Reference (Deposit): Cobb, E.H., 1976, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Fairbanks quadrangle, Alaska: U.S. Geological Survey Open-File Report 76-662, 174 p.

Reference (Deposit): Bundtzen, T. K. and Kline, J. T., 1981, Geologic mine map, Grant gold mine: Alaska Division of Geological and Geophysical Surveys Open-File Report 141, 2 p., 1 sheet, scale 1:120.

Reference (Deposit): Hill, J.M., 1933, Lode deposits of the Fairbanks District, Alaska: U.S. Geological Survey Bulletin 849-B, p. 29-163.

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

Reference (Deposit): Smith, P.S. 1939, Mineral industry in Alaska in 1937: U.S. Geological Survey Bulletin 910-A, p. 1-113.

Reference (Deposit): Killeen, P.L., and Mertie, J.B., 1951, Antimony ore in the Fairbanks District, Alaska: U.S. Geological Survey Open-File Report 51-46, 43 p.

Reference (Deposit): Chapman, R.M., and Foster, R.L., 1969, Lode mines and prospects in the Fairbanks district, Alaska: U.S. Geological Survey Professional Paper 625-D, 25 p., 1 plate.

Reference (Deposit): Smith, P.S., 1939, Mineral industry of Alaska in 1937: U.S. Geological Survey Bulletin 910-A, p. 1-113.

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): Newberry, R.J., Bundtzen, T.K., Clautice, K.C., Combellick, R.A., Douglas, T., Laird, G.M., Liss, S.A., Pinney, D.S., Reifenstuhl, R.R., and Solie, D.N., 1996, Preliminary geologic map of the Fairbanks mining district, Alaska: Alaska Division of Geological and Geophysical Surveys Public Data File 96-16, 17 p., 2 sheets, scale 1:63,360.

Reference (Deposit): Bundtzen, T. K., Swainbank, R. C., Wood, J. E., and Clough, A. H., 1991, Alaska's mineral industry 1991: Alaska Division of Geological and Geophysical Surveys Special Report 46, 89 p.

Reference (Deposit): Swainbank, R.C., Bundtzen, T.K., and Wood, J.E., 1991, Alaska's Mineral Industry 1990: Alaska Division of Geological and Geophysical Surveys Special Report 45, 78 p.

Reference (Deposit): Conwell, C.N., 1982, Mineral preparation, Grant gold mine, Alaska: Alaska Division of Geological and Geophysical Surveys Geologic Report 74, 15 p.

Reference (Deposit): Eakins, G.R., Bundtzen, T.K., Lueck, L.L. Green, C.B., Gallagher, J.L., and Robinson, M.S., 1985, Alaska mineral industry, 1984: Alaska Division of Geological and Geophysical Surveys Special Report 38, 57p.

Reference (Deposit): Bundtzen, T.K., Swainbank, R.C., Deagen, J.R. and Moore, J.L., 1990, Alaska's mineral industry 1989: Alaska Division of Geological and Geophysical Surveys Special Report 44, 100 p.

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