Homestake Mine (South Dakota)

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The Homestake Mine pit in Lead, South Dakota
File:Auriferous greenschist, Homestake Mine SD.jpg
Typical auriferous greenschist gold ore from the Homestake Mine. Two small masses of native gold (Au) are visible near the bottom right.

The Homestake Mine was a deep underground gold mine located in Lead, South Dakota. Until it closed in 2002 it was the largest and deepest gold mine in North America. The mine produced more than 40 million troy ounces (approximately 1.25 million kilograms) of gold during its lifetime.[1] The Homestake Mine is famous in scientific circles for being the site at which the solar neutrino problem was first discovered. This became known as the Homestake Experiment. The deep underground laboratory was set up by Raymond Davis Jr. in the mid-1960s to become the first experiment to observe solar neutrinos.

On July 10, 2007, the mine was selected by the National Science Foundation as the location[2] for the Deep Underground Science and Engineering Laboratory (DUSEL), winning out over several candidates including the Henderson Mine near Empire, Colorado. It is now operated as the Sanford Underground Research Facility (SURF).

History

The Homestake Mine in 1889

The Homestake deposit was discovered by Fred and Moses Manuel, Alex Engh and Hank Harney in April 1876, during the Black Hills Gold Rush. A trio of mining entrepreneurs, George Hearst, Lloyd Tevis, and James Ben Ali Haggin, bought it from them for $70,000 the following year. George Hearst arrived at the mine in October 1877, and took active control of the property. Hearst had to haul in all the mining equipment by wagons from the nearest railhead in Sidney, Nebraska. Arthur De Wint Foote worked as an engineer.[3] Despite the remote location, an 80-stamp mill began crushing Homestake ore in July 1878.

The partners sold shares in the Homestake Mining Company, and listed it on the New York Stock Exchange in 1879. The Homestake would become one of the longest-listed stocks in the history of the NYSE (Con Edison's original name was New York Gas Light and was listed in 1824).

File:Homestake Mine, South Dakota, 1900.jpg
Homestake Mine in 1900

Hearst consolidated and enlarged the Homestake property by fair and foul means. He bought out some adjacent claims, and secured others in the courts. A Hearst employee killed a man who refused to sell his claim, but was acquitted in court after all the witnesses disappeared. Hearst purchased newspapers in Deadwood to influence public opinion, and an opposing newspaper editor was beaten up on a Deadwood street. Hearst himself realized that he might be on the receiving end of violence, and wrote a letter to his partners asking them to provide for his family should he be murdered. In the end, however, Hearst was the one who walked out alive, and very rich.[4]

By the time Hearst left the Black Hills in March 1879, he had added the claims of Giant, Golden Star, Netty, May Booth, Golden Star No. 2, Crown Point, Sunrise, and General Ellison to the original two claims of the Manuel Brothers, Golden Terra and Old Abe, totaling 30 acres. The ten-stamp mill had become 200, and 500 employees worked in the mine, mills, offices and shops. He owned the Boulder Ditch and water rights to Whitewood Creek, monopolizing the region. His railroad, Black Hills & Fort Pierre Railroad, gave him access to eastern Dakota territory. By 1900, the Homestake owned 300 claims, on 2000 acres, and was worked by more than 2000 employees.[5]:35,40,42

In 1901, the mine started using compressed air locomotives, replacing the mules and horses by the 1920s. Charles Washington Merrill introduced cyanidization to augment mercury-amalgamation for gold recovery. "Cyanide Charlie" finally achieved 94 per cent recovery. The gold was shipped to the Denver Mint.[5]:49–51

By 1906, the Ellison Shaft reached 1,550 feet, the B&M 1,250 feet, the Golden Star 1,100 feet, and the Golden Prospect 900 feet, producing 1,500,000 tons of ore. A disastrous fire struck on 25 March 1907, which took forty days to extinguish after the mine was flooded. Another disastrous fire struck in 1919.[5]:52–53,59

In 1927, company geologist Donald H. McLaughlin used a winze from the 2,000 level to demonstrate ore reached the 3,500 foot level. The Ross shaft was started in 1934, a second winze from the 3,500 foot level reached 4,100 feet, and a third winze from 4,100 feet was started in 1937. The Yates shaft was started in 1938. Production ceased from 1943 until 1945, due to Limitation Order L-208 from the War Production Board. By 1975, mining operations has reached the 6,800 foot level, and two winzes were planned to 8,000 feet.[5]:63–66,73–74

The gold ore mined at Homestake was considered low grade (less than one ounce per ton), but the body of ore was very large.[6] Through 2001, the mine produced 39.8 million ounces of gold and 9 million ounces of silver.[citation needed] In terms of total production, the Lead mining district, of which the Homestake mine is the only producer, was the second-largest gold producer in the United States, after the Carlin district in Nevada.

File:Homestake Mine gold ore, town of Lead, northern Black Hills, western South Dakota (3.6 cm acr.) (14736672692).jpg
Homestake high-grade gold ore, view is about 1.2 cm wide

The Homestake mine ceased production at the end of 2001. Reasons included low gold prices, poor ore quality, and high costs. The Barrick Gold Corporation (which had merged with the Homestake Mining Company in mid-2001) agreed in early 2002 to keep dewatering the mine as DUSEL negotiations proceeded, but as progress was slow and maintaining the pumps and ventilation was costing $250,000 per month,[7] switched them off on June 10, 2003 and closed the mine completely.[8]

In June 2009, researchers at Berkeley announced that Homestake would be reopened for scientific research on neutrinos and dark matter particles using DUSEL and Large Underground Xenon experiment.[9]

Geology

File:Homestake.jpg
Gold production and ore ledge discovery[10]:J4-J8

The gold at Homestake is almost exclusively confined to the Homestake Formation, an Early Proterozoic layer with iron carbonate and iron silicate. The original 20–30 m thick Homestake Formation, has been deformed and metamorphosed, resulting in upper greenschist facies of siderite-phyllite, and lower amphibolite facies of grunerite schists.[10]:J15

The iron may have been deposited by volcanic exhalation, perhaps in the presence of microorganisms.[10]:J17 Gold ore mineralization is most intense in the Main Ledge, at the surface, and the 9 Ledge, at the 3200 level (feet below the Incline Shaft, at 1594 m above sea level).[10]:J36

  • Homestake2.jpg

    Geologic map of the Black Hills[10]

  • Homestake3.jpg

    Geologic cross section. The Homestake Formation has been deformed into synclines, odd numbers, and anticlines, even numbers. Ore mineralization occurred mainly in the synclines, called Ledges.[10]:J36

  • Lead Geologic Map.jpg

    Lead Geologic Map. Note the locations of the Ellison, Old Abe, Highland, Deadwood Terra, and DeSmet shafts, south to north. The Caledonia Cut is labelled with a "1".[11]:14

  • Lead Geologic Map Legend.jpg

    Lead Geologic Map Legend[11]

See also

References

  1. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  2. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  3. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  4. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  5. ↑ 5.0 5.1 5.2 5.3 Bronson, W., and Watkins, T.H., 1977, Homestake, San Francisco: Homestake Mining Company
  6. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  7. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  8. ↑ Lua error in package.lua at line 80: module 'strict' not found. A history of the Homestake mine as it applies to DUSEL.
  9. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  10. ↑ 10.0 10.1 10.2 10.3 10.4 10.5 Caddey, S.W., Bachman, R.L., Campbell, T.J., Reid, R.R., and Otto, R.P., 1991, The Homestake Gold Mine, An Early Protozoroic Iron-Formation-Hosted Gold Deposit, Lawrence County, South Dakota, in Geology and Resources of Gold in the United States, USGS Bulletin 1857, Washington: United States Government Printing Office
  11. ↑ 11.0 11.1 Paige, S., 1924, Geology of the Region Around Lead South Dakota, USGS Bulletin 765, Washington:Government Printing Office

External links

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