
mineral
Quartz (Milky/Clear variety)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Colorless to milky white; Luster: Vitreous (glassy); Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Colorless to milky white
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Colorless to milky white; Luster: Vitreous (glassy); Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed through the cooling of silica-rich magma or from hydrothermal veins. It is found in all three rock types (igneous, sedimentary, and metamorphic) across all geological ages.
Uses & applications
Widely used in glassmaking, electronics (piezoelectric properties), abrasives, jewelry (as semi-precious gemstones), and as a popular collector's specimen.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. While the social media tag in the image suggests 'diamond,' the visual features like the fracture pattern and luster are far more consistent with quartz.
Field identification & locations
Identify in the field by its hardness (it will scratch glass but cannot be scratched by a steel knife) and its lack of cleavage. Found globally in mountains, riverbeds, and mines.
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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