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MALACHITE.<br />
Malachite is green carbonite of copper, formed in copper ore<br />
deposits in the Urals, Australia and United States. Its hardness is<br />
3.5 to 4; specific gravity 3.7 to 4; lustre adamantine to vitreous.<br />
The bright green of its color is lined by darker shades, the structure<br />
concentric, evidence of deposition from a solution in water of successive<br />
layers.<br />
In this country it is seldom used for personal adornment, except<br />
in connection with azurite, with which it is sometimes found.<br />
Cut en cabochon across the alternate layers, a fine mottled effect<br />
is produced. But little of this combined form is to be found now,<br />
as most of it was melted for copper before it came into vogue for<br />
jewelry.<br />
Malachite and to a lesser extent azurite are infinitely<br />
more beautiful in the natural state, with the subdued coloring of the<br />
mineral, and its soft, fuzzy, velvety texture. Polishing simply makes<br />
these lovely greens and blues bold and hard.<br />
AZURITE.<br />
Azurite is a form of chessylite, which is very similar to malachite.<br />
It has a fine dark-blue color, like that of lapis-lazuli. In<br />
hardness it is 3.7, in specific gravity it is 3.8, so it is both softer<br />
and denser than lapis. Its lustre is vitreous and the mineral takes<br />
a good polish.<br />
BENETOITE.<br />
New minerals or substances have lately been found, but play<br />
little part in personal adornment. Benetoite is one of these, discovered<br />
in 1907 in the Mt. Diablo range near the San Benito, Fresno<br />
County line, California, by Messrs. Hawkins and Sanders. Chemically<br />
it is a very acid titano-silicate of barium, hexagonal, hardness<br />
6 to 6.5, highly refractive. It was said at first that if cut right it<br />
would rival the blue sapphire in color and brilliance, but one glance<br />
at it shows this to be a wild exaggeration.