mineral

Tumbled white mineral fragment

Indeterminate; possibly milky quartz or calcite

AI-generated identification · may be incorrect

Small, smooth, opaque cream-white specimen with a dull to softly waxy luster; apparent hardness cannot be determined visually. Rounded edges suggest tumbling or natural abrasion, and the blurred image does not show cleavage or crystal form.

Identified August 25, 2026More mineral →

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Physical properties

Formation & geological history

Most plausibly quartz (SiO₂) or calcite (CaCO₃), formed in veins or sedimentary environments and later polished or weathered; geological age is undeterminable from the image.

Uses & applications

Tumbled pieces are used for decoration, crafts, teaching, and inexpensive collections; value is generally minimal.

Geological facts

Quartz has Mohs hardness 7 and no cleavage, while calcite has hardness 3 and prominent rhombohedral cleavage. A steel-knife scratch test and vinegar reaction can help distinguish them, though testing may damage the piece.

Field identification & locations

Common sources include quartz veins, gravel deposits, and limestone regions worldwide. Identify with a hardness test: quartz resists a knife, whereas calcite scratches readily and may fizz weakly in dilute acid.