
mineral
Clear quartz tumbled stone
Quartz (silicon dioxide, SiO₂)
AI-generated identification · may be incorrectTransparent to translucent, colorless, and vitreous with rounded, polished surfaces. Mohs hardness 7; trigonal crystal structure, no cleavage, conchoidal fracture, and specific gravity about 2.65.
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Physical properties
Transparent to translucent, colorless, and vitreous with rounded, polished surfaces. Mohs hardness 7; trigonal crystal structure, no cleavage, conchoidal fracture, and specific gravity about 2.65.
Formation & geological history
Likely natural quartz that was mechanically tumbled and polished; quartz formed in igneous, hydrothermal, and metamorphic environments over geologic time. The photograph cannot establish a precise age or locality.
Uses & applications
Used as a decorative and collectible stone, in jewelry, and industrially for glass, abrasives, electronics, and optical components.
Geological facts
Clear quartz is commonly called rock crystal. Internal fractures, bubbles, or surface reflections can resemble inclusions; a true quartz specimen scratches ordinary glass but should not be confused with man-made glass.
Field identification & locations
Identify by its glassy luster, rounded conchoidal surfaces, hardness, and lack of cleavage. Common sources include Brazil, Madagascar, the United States, and many hydrothermal vein districts.
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