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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.
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However, a re-analysis of the material in 1971 found the keweenawite to be a mixture of the copper and nickel arsenates:
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containing 39% to 54% copper, 9.7% to 20% nickel, and 0.9% cobalt. Keweenawite was discovered in July 1901, in the
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Keweenawite was first discovered, in July 1901, located on the fifth level of the
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Copper-Nickel
Arsenides of the Mohawk No. 2 Mine, Mohawk, Keweenaw Co., Michigan,
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is a discredited mineral species. It was described as an
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141:American Mineralogist, V. 56, July–August, 1971
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127:The American journal of science, Volume 164
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175:. You can help Knowledge (XXG) by
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105:World Mines Register, Volumes 4–5
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163:This article about a specific
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237:Keweenaw County, Michigan
232:Geology of Michigan
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137:Moore, Paul B.;
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177:expanding it
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57:Mohawk Mine
37:Mohawk Mine
17:Keweenawite
216:Categories
169:mineraloid
92:References
85:Mohawkite
69:niccolite
222:Minerals
79:See also
45:Michigan
21:arsenide
165:mineral
51:History
33:cobalt
31:, and
29:nickel
25:copper
227:Rocks
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143:PDF
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