
mineral
Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale. Color: White, clear, or milky. Luster: Vitreous to greasy. Crystal Structure: Trigonal, hexagonal prism. Cleavage: None, exhibits conchoidal fracture. Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- White, clear, or milky
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale. Color: White, clear, or milky. Luster: Vitreous to greasy. Crystal Structure: Trigonal, hexagonal prism. Cleavage: None, exhibits conchoidal fracture. Specific Gravity: 2.65.
Formation & geological history
Forms in a wide variety of geological environments, most commonly as a primary component of igneous rocks like granite, in hydrothermal veins, and as detrital grains in sedimentary rocks. Can range in geological age from Precambrian to modern-day formations.
Uses & applications
Used in electronics (oscillators), glassmaking, abrasives, gemstones, and construction materials.
Geological facts
Quartz is one of the most abundant minerals in Earth's continental crust. It exhibits piezoelectric properties, meaning it can generate an electrical charge in response to mechanical stress.
Field identification & locations
Can be identified by its characteristic conchoidal fracture, lack of cleavage, and hardness of 7, which allows it to easily scratch glass. Found worldwide in almost every geological setting.
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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