
mineral
Quartz
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: White to colorless; Luster: Vitreous/glassy; Crystal Structure: Trigonal/hexagonal; Cleavage: None/conchoidal fracture; Specific gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- White to colorless
- Luster
- Vitreous/glassy
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Physical properties
Hardness: 7 on Mohs scale; Color: White to colorless; Luster: Vitreous/glassy; Crystal Structure: Trigonal/hexagonal; Cleavage: None/conchoidal fracture; Specific gravity: 2.65
Formation & geological history
Formed in various environments including cooling igneous magma, hydrothermal veins, and metamorphic rocks. It is one of the most common minerals in the Earth's crust.
Uses & applications
Used in glassmaking, abrasives, electronic oscillators (piezoelectric properties), jewelry, and as a component in concrete and mortar.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. It is highly resistant to chemical and physical weathering, which is why it often ends up as beach sand.
Field identification & locations
Identify by its hardness (scratches glass), lack of cleavage, and glassy appearance. Common in granite and found globally in mountainous or sandy areas.
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Schist
Schist
Metamorphic
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Nephrite Jade
Nephrite
Mineral/Rock
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
Metamorphic Rock
Biotite Schist
Biotite-rich Schist [K(Mg,Fe)3AlSi3O10(F,OH)2]
metamorphic