
mineral
Clear Quartz (Rock Crystal)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Colorless/Transparent; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Colorless/Transparent
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Colorless/Transparent; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65
Formation & geological history
Forms in igneous, metamorphic, and sedimentary environments. It commonly crystallizes from magma or precipitates from hydrothermal veins. It is found in geological formations of all ages.
Uses & applications
Used in electronics (oscillators), optics, glassmaking, abrasives, jewelry, and as a popular metaphysical or collectible gemstone.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Its name comes from the Greek word 'krystallos,' meaning ice, as ancient Greeks believed quartz was permanently frozen ice.
Field identification & locations
Identify by its hardness (scratches glass), glass-like luster, and absence of cleavage. Found globally, especially in mountainous regions like the Alps, Brazil, and Arkansas, USA.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous