Rock Identifier
Tumbled milky chalcedony (likely common opal or quartz-rich chalcedony) (Chalcedony, microcrystalline SiO₂; identification is uncertain from the photo) — mineral
mineral

Tumbled milky chalcedony (likely common opal or quartz-rich chalcedony)

Chalcedony, microcrystalline SiO₂; identification is uncertain from the photo

AI-generated identification · may be incorrect

Pale gray-white, opaque to slightly translucent, with a smooth tumbled surface and waxy luster; quartz hardness about 6.5–7 Mohs, trigonal crystal structure at the microscopic level, no obvious cleavage. Brown patches may be iron-oxide staining or inclusions.

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Physical properties

Pale gray-white, opaque to slightly translucent, with a smooth tumbled surface and waxy luster; quartz hardness about 6.5–7 Mohs, trigonal crystal structure at the microscopic level, no obvious cleavage. Brown patches may be iron-oxide staining or inclusions.

Formation & geological history

Silica-rich fluids deposited the material in rock cavities or fractures; its exact geological age and source cannot be determined from the image.

Uses & applications

Commonly tumbled for collecting, craft, and jewelry; chalcedony is also used for beads and ornamental objects.

Geological facts

Chalcedony is made of extremely fine quartz crystals, so individual crystals are generally not visible without magnification.

Field identification & locations

Look for waxy luster, hardness near 7, and conchoidal fracture; a scratch or acid test is not advisable on a collectible. Chalcedony occurs worldwide in volcanic cavities and sedimentary deposits; the photo does not establish a locality.