Chemical Formula |
SiO2 |
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Composition |
Silicon dioxide. Its purple coloring is usually caused by impurities of iron or manganese compounds. |
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Color |
Light to dark purple. Sometimes banded with purple and whitish lines. May also be mixed together with Citrine. |
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Streak |
White |
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Hardness |
7 |
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Crystal System |
Hexagonal |
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Crystal Forms |
Most often as protruding clusters of pyramids on a matrix base. These "pyramids" can be quite large. Also occurs as tall prismatic crystals, as short stubby crystals, in drusy aggregates, massive, in geodes, and as rounded waterworn stones. A very interesting habit is as crystalline crusts inside volcanic pipes. Crystals are usually striated horizontally, and occasionally have a scepter growth. |
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Transparency |
Transparent to translucent |
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Specific Gravity |
2.6 - 2.7 |
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Luster |
Vitreous |
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Cleavage |
Indiscernible |
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Fracture |
Conchoidal |
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Tenacity |
Brittle |
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Other ID Marks |
Occasionally fluorescent cream or white in shortwave ultraviolet light. |
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Complex Tests |
Dissolves in hydrofluoric acid. |
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In Group |
Silicates; Tectosilicates; Silica Group |
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Striking Features |
Color, crystal habits, and hardness. |
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Environment |
Occurs in all mineral environments, especially in igneous environments. |
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Rock Type |
Igneous, Sedimentary, Metamorphic |
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Popularity (1-4) |
1 |
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Prevalence (1-3) |
1 |
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Demand (1-3) |
1 |
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