
mineral
Quartz
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Clear to white; Luster: Vitreous/glassy; Crystal structure: Hexagonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Clear to white
- Luster
- Vitreous/glassy
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Physical properties
Hardness: 7 on Mohs scale; Color: Clear to white; Luster: Vitreous/glassy; Crystal structure: Hexagonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65.
Formation & geological history
Formed from cooling magma or precipitation from hydrothermal veins. It is found in almost all geological environments and ranges from Precambrian to recent ages.
Uses & applications
Used in glass manufacturing, electronics (oscillators), abrasives, jewelry (gemstones), and construction as an aggregate.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. It is piezoelectric, meaning it generates an electric charge when subjected to mechanical stress.
Field identification & locations
Identify by its inability to be scratched by steel, its glassy luster, and shell-like (conchoidal) fracture patterns. Commonly found in riverbeds, mountains, and desert sands.
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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