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Ch. 21: Quartz

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has pyramidal terminations. Crystals are rhombohedral. They may be right-handed or left-handed forms due to tetrahedral symmetry. Two independent rhombohedra combine to give a hexagonal pyramid, but the faces differ in size, three smaller faces alternating with three larger faces; this is characteristic even in very small crystals. Twins are also found, as also irregular puzzling growths, which could be oriented and deciphered by the horizontal striations on the prism faces. The crystals vary enormously in size.
Quartz contains various inclusions: (a) solid inclusions of rutile, hematite, epidote, etc.; (6) liquids, e.g. water and liquid C02; and (c) gaseous inclusions, mostly C02. It has conchoidal fracture. Hardness = 7. Specific gravity = in pure quartz, varying from in other varieties.
Lustre: Vitreous. Transparent to translucent or opaque. Uniaxial. Optically positive. Mean index of refraction =, double refraction =and dispersion =
(low). It is optically active and rotates the plane of polarization to right or left according as it is a right- or left-handed crystal. Composition: Si02. Quartz may be very pure or contain mineral inclusions and other foreign matter. Also forms pseudomorphs, e.g. fossil wood. It is a fairly resistant mineral, but may be replaced by other minerals.
Uses
Crystalline and crypto-crystalline varieties of quartz are used for gem purposes. The crystalline quartz is cut in facetted forms or cabochon. Rock crystals are also cut into vases, crystal balls, idols, etc. When cut it resembles beryl and topaz. On account of its piezo­electric properties, properly oriented sections are used in radio apparatus as resonators and oscillators in radio-telephony and radiotelegraphy and for depth measurements in submarines.
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Ch. 21: Quartz Page of 187 Ch. 21: Quartz
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