Field book of common rocks and minerals : $b for identifying the rocks and minerals of the United States and interpreting their origins and meaningsLoomis, Frederic Brewster
Science
Field book of common rocks and minerals : $b for identifying the rocks and minerals of the United States and interpreting their origins and meanings
Loomis, Frederic Brewster
Minerals -- United States; Rocks -- United States
Cobalt is another of the metals, of which the United States does not
have an adequate supply. Sweden, Norway and India were the chief sources
of supply until cobalt was found near the town of Cobalt in Ontario,
Canada, and now this district furnishes 90% of the world’s supply.
Cobaltite
CoAsS
Pl. 26
_cobalt glance_
Usually crystalline in cubes, pyritohedrons or octahedrons; hardness
5.5; specific gravity 6.1; color reddish silver-white; streak
grayish-black; luster metallic; opaque on thin edges.
In color cobaltite may appear very like arsenopyrite, especially if the
reddish tinge is not strong, in which case the mineral can be definitely
determined by putting a piece in nitric acid. If it is cobaltite the
solution will be colored rose-red, if arsenopyrite there will be no
change of color. The forms of the crystals are the same as those of
pyrite, but the color will easily distinguish cobaltite from pyrite.
This pink color is characteristically present either in or about cobalt
minerals, being sometimes called “cobalt bloom.” It is a
cobalt-arsenic-oxide with water of crystallization (Co₃As₂O₈·8H₂O),
which results from the exposure of cobalt and arsenic minerals to air
and moisture. It is the pink color on the figures of both cobaltite and
smaltite. In Sweden, Norway and India, this is the chief ore for cobalt,
but in the United States it is rather rare, but is found in Oregon, and
at Cobalt, Canada.
Smaltite
(CoNi)As₂
Pl. 26
_gray cobalt ore_
Usually occurs in masses; hardness 5.5; specific gravity 6.2; color
tin-white to steel-gray; streak grayish-black; luster metallic; opaque
on thin edges.
While very like cobaltite, smaltite is almost never found in crystals,
but when crystals are found, they are cubes. The color is tin-white but
there is usually a pink tinge visible due to the presence of small
amounts of “cobalt bloom.” If in any doubt about the determination of
this mineral, put a piece in nitric acid. If it colors the acid
rose-pink, and is non-crystalline it is pretty surely smaltite; if the
acid is not affected it is arsenopyrite.
Smaltite is found in Kentucky, Missouri, Colorado, Idaho, California,
and at Cobalt in Canada.
Chromium
Public-domain text, read in full here on John Shaqi.
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