
mineral
Tumbled Clear Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Colorless or transparent with minor inclusions; Luster: Vitreous; Crystal Structure: Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Colorless or transparent with minor inclusions
- Luster
- Vitreous
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Physical properties
Hardness: 7 on Mohs scale; Color: Colorless or transparent with minor inclusions; Luster: Vitreous; Crystal Structure: Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Forms in hydrothermal veins, pegmatites, and as a primary constituent of many igneous, metamorphic, and sedimentary rocks over a wide geological timeframe.
Uses & applications
Used in jewelry, decorative items, optical components, oscillators in electronics, and metaphysical healing practices.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Pure quartz, traditionally called rock crystal, has been used since antiquity for carvings and fire starters.
Field identification & locations
Identified by its high hardness (scratches glass easily), lack of cleavage, and conchoidal fracture. Commonly found worldwide in virtually all geological 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