
mineral
Clear Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: Colorless/transparent; Luster: Vitreous; Crystal structure: Trigonal (hexagonal prisms); Cleavage: None/Conchoidal fracture; Specific gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Colorless/transparent
- Luster
- Vitreous
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Physical properties
Hardness: 7 (Mohs scale); Color: Colorless/transparent; Luster: Vitreous; Crystal structure: Trigonal (hexagonal prisms); Cleavage: None/Conchoidal fracture; Specific gravity: 2.65
Formation & geological history
Formed from cooling magma (igneous) or precipitation from hydrothermal veins. Found globally in almost every geological environment.
Uses & applications
Used in jewelry, timekeeping (piezoelectric properties), glassmaking, electronics, and as a popular collector specimen.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Pure quartz is traditionally called rock crystal.
Field identification & locations
Identify by its hardness (will scratch glass), hexagonal crystal habit, and conchoidal (glass-like) fracture pattern. Found in Arkansas (USA), Brazil, and Madagascar.
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
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
Septarian Pebble
Septarian nodule / Concretion
sedimentary