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    Minerals A-E

Citrine

Name

Citrine

Chemistry

SiO2

Uses

As a gemstone and a mineral specimen

Color

Yellow to yellow/brown

Hardness

7

Specific gravity

2.6-2.7

Citrine is a quartz with a yellow included color.

Crystals are usually stubby. Can also be found as crystals in a geode. Most citrine are heat treated amethyst or sometimes smokey quartz that is heat treated. The difference is in the color. Heat treated amethyst is more reddish yellow. Natural citrine is more subdued. Naturally occuring citrine is relativaly scarce. We at the mineral gallery has some intersting natural clusters from Namibia.

It closely assembles topaz and is sometimes wrongly labelled as madeira topaz. Citrine is widely used as a gem, and is the most valuable Quartz gem.

Quartz crystallizes in the trigonal trapezohedral class of the rhombohedral subsystem of hexagonal symmetry. The quartz symmetry class lacks a center of symmetry or planes of symmetry. The (c) crystallographic axis is perpendicular to three polar axes (a) separated by 120 degrees in a plane. Because the polar axes differ on each end, the application of mechanical stress to such an axis produces electrical charges of opposite sign at each end (piezoelectricity); conversely, applied electrical fields produce mechanical stresses. The piezoelectric property makes quartz valuable in pressure gauges, electronic frequency-control devices, radios, and other applications. Most quartz crystals are twinned, although this may not be visible to the eye. The polar axes and enantiomorphism permit complex twinning.

When heated above 573¡ C (1,063¡ F) at 1 bar (14.50 lb/in6) of pressure, quartz assumes higher symmetry as the threefold c axis becomes sixfold. This hexagonal form is known as high quartz or Beta quartz. The transformation temperature is pressure-dependent, increasing by approximately 25 C degrees (45 F degrees) per kilobar. When high quartz is cooled below the inversion temperature, inversion to low quartz occurs rapidly. The first mild heating of quartz commonly will be accompanied by the emission of light (thermoluminescence), and irreversible color changes may occur in colored varieties. For example, amethyst may be transformed to citrine at 250¡ C (482¡ F) or higher. Vigorous rubbing of one quartz crystal by another may also produce visible light (triboluminescence).  

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