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HYPERSTHENE AND BRONZITE
These minerals, belonging to the pyroxene group, are employed in jewelry when, on account of a fibrous structure or a regular arrangement of inclusions, they exhibit a chatoyant effect. They do not afford trans­parent stones, but are cut en cabochon to make cat's-eyes and give other schillerizing effects.
The color of hypersthene is usually a dark bronze, so opaque as to approach a metal in luster. The light which plays over it is copper-red in color, and very brilliant in a good stone. The cause of the chatoyancy is supposed to be countless crystals of the oxide of titanium, known as brookite, which are arranged in regular order in the stone. The stone must be cut with reference to the direction of these in order to give the chatoyant effect.
The hypersthene used for this purpose comes almost exclusively from the Island of Paul on the coast of Labrador. Here it occurs together with labradorite as shore pebbles, and it may also be quarried from neigh­boring cliffs. For cutting, a sound piece without flaws must be used, and it is often necessary to break a number of fragments before a suit­able one can be found. Yet the supply of material is so abundant and the demand comparatively so limited that the stones do not command a high price.
The hardness of hypersthene is 5-6; its specific gravity 3.4-3.5. It fuses before the blowpipe to a black enamel, and is partially decomposed by hydrochloric acid. Its name comes from two Greek words meaning very tough. It is a common constituent of eruptive rocks, usually in small crystals. Its system of crystallization is orthorhombic. In com­position it is a silicate chiefly of iron and magnesium.
Enstatite resembles hypersthene in composition and properties, and its limited use in jewelry is to furnish " cat's-eyes " of a green color. The chatoyant effect is due usually to a fibrous structure. The principal locality for this variety is near Harzburg in the Harz. Schillerizing bronzite is found in a few localities in this country.
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