Rock Identifier
White tumbled stone, likely quartz or milky chalcedony (Most likely microcrystalline quartz/chalcedony (SiO₂); exact identification requires hardness and specific-gravity testing) — mineral
mineral

White tumbled stone, likely quartz or milky chalcedony

Most likely microcrystalline quartz/chalcedony (SiO₂); exact identification requires hardness and specific-gravity testing

AI-generated identification · may be incorrect

Opaque white, smoothly tumbled, with a vitreous-to-waxy luster and no visible cleavage. Quartz has Mohs hardness 7 and specific gravity about 2.65; the rounded shape and uniform surface indicate human polishing.

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Physical properties

Opaque white, smoothly tumbled, with a vitreous-to-waxy luster and no visible cleavage. Quartz has Mohs hardness 7 and specific gravity about 2.65; the rounded shape and uniform surface indicate human polishing.

Formation & geological history

Quartz-rich material formed in silica-bearing veins, cavities, or sedimentary deposits; geological age cannot be determined from the photograph. It was later cut and mechanically tumbled for decoration or craft use.

Uses & applications

Commonly sold as a pocket stone, craft material, decorative aggregate, or inexpensive cabochon; not usually valuable as jewelry unless it has unusual translucency or patterning.

Geological facts

Milky quartz appears white because microscopic fluid inclusions and structural defects scatter light. Chalcedony is chemically quartz but consists of extremely fine interlocking quartz fibers.

Field identification & locations

Test with a steel file or glass: genuine quartz should scratch glass and resist a steel blade. Calcite, a possible alternative, is softer (Mohs 3) and would fizz in dilute hydrochloric acid; avoid acid unless appropriate.