Rock Identifier
Tumbled milky quartz (Quartz (silicon dioxide, SiO₂)) — mineral
mineral

Tumbled milky quartz

Quartz (silicon dioxide, SiO₂)

AI-generated identification · may be incorrect

Likely hardness 7 on the Mohs scale, translucent white to cream, with a vitreous-to-waxy luster and no visible cleavage. The smooth rounded shape indicates tumbling and polishing; exact identification is limited by the image.

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Physical properties

Likely hardness 7 on the Mohs scale, translucent white to cream, with a vitreous-to-waxy luster and no visible cleavage. The smooth rounded shape indicates tumbling and polishing; exact identification is limited by the image.

Formation & geological history

Quartz crystallizes from silica-rich igneous, metamorphic, and hydrothermal fluids; milky quartz commonly forms in veins due to microscopic fluid inclusions. Quartz ranges from ancient Precambrian rocks to geologically recent deposits.

Uses & applications

Used as an inexpensive ornamental stone, craft material, and collectible; quartz is also important in glass, ceramics, electronics, and engineered stone.

Geological facts

Quartz is one of Earth’s most abundant minerals and has a characteristic conchoidal fracture. Its white cloudiness commonly results from trapped microscopic fluids or fractures.

Field identification & locations

Test with a steel file or knife cautiously: quartz should resist scratching; it can scratch ordinary glass. Common sources include Brazil, Madagascar, the United States, and quartz veins worldwide.