
mineral
Quartz Crystal (Smoky Quartz)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Clear to grey-brown/smoky; Luster: Vitreous; Crystal System: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Clear to grey-brown/smoky
- Luster
- Vitreous
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Physical properties
Hardness: 7 on Mohs scale; Color: Clear to grey-brown/smoky; Luster: Vitreous; Crystal System: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed from silica-rich hydrothermal solutions or cooling magma within igneous rocks like granite. Smoky varieties often result from natural gamma radiation exposure during long geological periods.
Uses & applications
Used in electronics for its piezoelectric properties, glass manufacturing, jewelry, and widely collected as a metaphysical or display specimen.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. This specimen shows 'double termination' where points form at both ends, which is relatively rare compared to single-pointed crystals.
Field identification & locations
Look for six-sided prisms with pyramid-like terminations. It can scratch glass and does not react to acid. Common worldwide, with famous deposits in the Swiss Alps, Brazil, and Arkansas.
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sedimentary
Sandstone with Mineral Veining or Crust
Sedimentary Sandstone (mostly SiO2 with Fe2O3 tinting)
sedimentary
Schist
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Metamorphic
Epidote
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metamorphic
Gypsum (variety Selenite or Alabaster)
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