
mineral
Clear Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Clear to translucent; Luster: Vitreous; Crystal system: Trigonal/Hexagonal; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Clear to translucent
- Luster
- Vitreous
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Physical properties
Hardness: 7 on Mohs scale; Color: Clear to translucent; Luster: Vitreous; Crystal system: Trigonal/Hexagonal; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65
Formation & geological history
Quartz forms in a wide variety of geological environments, most notably from the cooling of magma or precipitation from hydrothermal veins. It is a major constituent of igneous rocks like granite and metamorphic rocks like quartzite.
Uses & applications
Extensively used in electronics for its piezoelectric properties, glass manufacturing, abrasives, timekeeping (quartz watches), and as a gemstone for jewelry and metaphysical collecting.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. It is highly resistant to both mechanical and chemical weathering.
Field identification & locations
Identify by its 7 hardness (scratches glass and steel), hexagonal crystal shape (if present), and conchoidal (shell-like) fracture patterns. It is found globally in almost all rock-forming environments.
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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
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