
mineral
Clear Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Colorless/Transparent; Luster: Vitreous (glassy); Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Colorless/Transparent
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Colorless/Transparent; Luster: Vitreous (glassy); Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Forms in a wide variety of environments including igneous, metamorphic, and sedimentary settings. Most commonly crystallizes from magma or hydrothermal vents. It is found in earth's crust dating back billions of years.
Uses & applications
Used in electronics for its piezoelectric properties, glass manufacturing, timekeeping (quartz watches), and widely used in jewelry and gemstone collecting.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. It was historically used to make stone tools and has been revered in various cultures for its supposed healing properties.
Field identification & locations
Identify by its hardness (can scratch glass), lack of cleavage, and transparent appearance. Commonly found globally in mountains, riverbeds, and as sand on beaches.
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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