
mineral
Clear Quartz
Silicon Dioxide (SiO2)
Hardness: 7 (Mohs scale), Color: Colorless/Transparent, Luster: Vitreous (glassy), Crystal System: Hexagonal/Trigonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65
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Physical properties
Hardness: 7 (Mohs scale), Color: Colorless/Transparent, Luster: Vitreous (glassy), Crystal System: Hexagonal/Trigonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65
Formation & geological history
Formed through the crystallization of magma or from hydrothermal veins. It is found in many geological environments ranging from igneous to metamorphic rocks and can be of almost any geological age.
Uses & applications
Used widely in electronics (oscillators), optics, glassmaking, clocks, gemstones, and metaphysical healing practices.
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 stress is applied.
Field identification & locations
Identify by its hardness (will scratch glass), lack of cleavage, and transparent appearance. Commonly found in riverbeds, mountains, and sand. Look for glassy luster and curved fracture surfaces.
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Arenite (SiO2 based)
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Epidote
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Nephrite Jade
Nephrite
Mineral/Rock
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
Metamorphic Rock
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mineral