
mineral
Quartz (specifically Clear Quartz or Rock Crystal)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Colorless to faint yellow/smoky; Luster: Vitreous (glassy); Crystal Structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Colorless to faint yellow/smoky
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Colorless to faint yellow/smoky; Luster: Vitreous (glassy); Crystal Structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed from cooling magma or hydrothermal veins. It is found in all types of geological environments and can be found in rocks from the Precambrian era to the present.
Uses & applications
Extensively used in electronics (oscillators), glass manufacturing, abrasives, construction sand, and as a gemstone in jewelry and metaphysical collecting.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. It is piezoelectric, meaning it generates an electric charge when mechanical pressure is applied.
Field identification & locations
Identify in the field by its glass-like appearance, inability to be scratched by a steel knife, and lacks cleavage (it breaks into curved, shell-like shards). Common in riverbeds and mountainous regions globally.
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