Keweenawite

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Keweenawite is a discredited mineral species. It was described as an arsenide of copper, nickel, and cobalt containing 39% to 54% copper, 9.7% to 20% nickel, and 0.9% cobalt. [1] Keweenawite was discovered in July 1901, in the Mohawk Mine, Keweenaw County, Michigan. George A Koenig analyzed and named the copper ore. [2]

Contents

History

Keweenawite was first discovered, in July 1901, located on the fifth level of the Mohawk Mine between Shaft No. 1 and Shaft No. 2. Fred Smith, mine superintendent, sent specimens to George A Koenig for analysis. Koenig deemed it to be a new mineral species and named it keweenawite, after its discovery locality, Keweenaw County. [3]

However, a re-analysis of the material in 1971 found the keweenawite to be a mixture of the copper and nickel arsenates: α-domeykite, niccolite and rammelsbergite. [4]

See also

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Mohawkite is a rare rock consisting of mixtures of arsenic, silver, nickel, skutterudite and copper, with the formula Cu3As up to Cu6As, and the most desirable material was usually found in white quartz matrix. It has a hardness of 3–3.5 and a metallic luster. It is named after the Mohawk Mine, where it was originally found. Colors range from brassy-yellow to metallic gray, and sometimes will have a blue or greenish surface tarnish. These colors come from its two main ingredients, the arsenic-rich copper minerals algodonite and domeykite. Its color may resemble pyrrhotite, but unlike pyrrhotite, mohawkite is not magnetic.

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References

  1. World Mines Register, Volumes 4–5
  2. World Mines Register, Volume 2
  3. The American journal of science, Volume 164
  4. Moore, Paul B.; Copper-Nickel Arsenides of the Mohawk No. 2 Mine, Mohawk, Keweenaw Co., Michigan, American Mineralogist, V. 56, July–August, 1971 PDF