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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.

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