Rock Identifier
Tumbled milky quartz (Quartz, SiO₂; trigonal crystal system) — mineral
mineral

Tumbled milky quartz

Quartz, SiO₂; trigonal crystal system

AI-generated identification · may be incorrect

Hardness 7 Mohs; white to gray, translucent, with a vitreous-to-greasy luster. The rounded surface obscures natural crystal faces; quartz has no cleavage and uneven fracture.

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Physical properties

Hardness 7 Mohs; white to gray, translucent, with a vitreous-to-greasy luster. The rounded surface obscures natural crystal faces; quartz has no cleavage and uneven fracture.

Formation & geological history

Quartz crystallizes from silica-rich fluids and melts in many rock types; milky appearance comes from microscopic fluid or gas inclusions. Quartz formed throughout geological time, and this piece has been mechanically tumbled and polished.

Uses & applications

Commonly used in jewelry, ornaments, and collections; quartz also has major industrial uses in glassmaking and electronics.

Geological facts

Quartz is one of Earth’s most abundant minerals and occurs in igneous, sedimentary, and metamorphic rocks.

Field identification & locations

Look for hardness near 7, glass-scratching ability, and absence of cleavage; milky quartz is widespread in veins and many regions worldwide. Its smooth oval shape indicates processing rather than natural crystal growth.