
mineral
White Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: White to milky; Luster: Vitreous (glassy); Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- White to milky
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: White to milky; Luster: Vitreous (glassy); Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed from molten magma as it cools or by hydrothermal activity. Quartz is found in all three rock types (igneous, metamorphic, and sedimentary) across most geological eras.
Uses & applications
Used in glass manufacturing, electronics (due to piezoelectric properties), construction, abrasives, and as semi-precious gemstones in jewelry.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Its name comes from the German word 'quarz' and it has been used since ancient times for carving and tools.
Field identification & locations
Identify by its hardness (it scratches glass easily) and lack of cleavage. Commonly found in riverbeds, mountains, and beaches. Collectors look for clear hexagonal crystal points.
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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