
mineral
Clear Quartz (Tumbled)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Clear/Colorless; Luster: Vitreous; Crystal Structure: Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Clear/Colorless
- Luster
- Vitreous
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Physical properties
Hardness: 7 on Mohs scale; Color: Clear/Colorless; Luster: Vitreous; Crystal Structure: Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed from silica-rich hydrothermal solutions or the cooling of magma in igneous rocks like granite. Found in environments spanning from metamorphic to sedimentary deposits over millions of years.
Uses & applications
Used in electronics (oscillators), optical instruments, jewelry, glassmaking, and metaphysical collections.
Geological facts
Quartz is the second most abundant mineral in Earth's crust. 'Rock crystal' was once believed by ancient Greeks to be ice that had frozen so hard it could never melt.
Field identification & locations
Identify by its hardness (scratches glass), lack of bubbles (unlike glass), and conchoidal fracture. Commonly found in riverbeds, mountains, and mines worldwide.
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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
Potassium Feldspar (Orthoclase)
Orthoclase (KAlSi3O8)
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Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral
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Mineral/Rock