
mineral
Clear Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: Colorless to white; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: Indistinct; Specific Gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Colorless to white
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 (Mohs scale); Color: Colorless to white; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: Indistinct; Specific Gravity: 2.65
Formation & geological history
Quartz forms through the cooling of silica-rich magma or from hydrothermal veins. It is found across all geological ages and in igneous, metamorphic, and sedimentary environments.
Uses & applications
Extensively used in electronics (piezoelectric properties), glassmaking, abrasive manufacturing, construction, and as a gemstone for jewelry and ornamental carving.
Geological facts
Quartz is the second most abundant mineral in the Earth's continental crust. It was historically believed by some ancient cultures to be 'permanent ice' frozen by the gods.
Field identification & locations
Identified in the field by its hardness (scratches glass/steel), lack of true cleavage, and characteristic conchoidal fracture. Extremely common in granite and sandstone.
More like this
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