Rock Identifier
Tumbled white chalcedony (likely common opal or milky quartz) (Microcrystalline quartz, SiO₂; possibly hydrated silica opal, SiO₂·nH₂O) — mineral
mineral

Tumbled white chalcedony (likely common opal or milky quartz)

Microcrystalline quartz, SiO₂; possibly hydrated silica opal, SiO₂·nH₂O

AI-generated identification · may be incorrect

White to cream, translucent, waxy-to-glassy luster with rounded tumbled surfaces and small pits. Chalcedony has Mohs hardness 6.5–7; opal is softer at 5.5–6.5, lacks visible cleavage, and is cryptocrystalline or amorphous.

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Physical properties

White to cream, translucent, waxy-to-glassy luster with rounded tumbled surfaces and small pits. Chalcedony has Mohs hardness 6.5–7; opal is softer at 5.5–6.5, lacks visible cleavage, and is cryptocrystalline or amorphous.

Formation & geological history

Silica-rich groundwater deposited the material in cavities, veins, or volcanic vesicles; chalcedony commonly formed during the Cenozoic, while opal can form at many ages. The specimen has been cut or tumbled and polished by humans.

Uses & applications

Used as a decorative stone, cabochon, carving material, and lapidary rough; common pieces have modest jewelry and collecting value.

Geological facts

The porous-looking pits and creamy appearance are consistent with weathered or lightly polished chalcedony, though the photograph cannot distinguish it confidently from opal or even porous white quartz.

Field identification & locations

Field tests include hardness against steel or glass, conchoidal fracture, and specific gravity; opal may feel slightly lighter and show stronger translucency. Common sources include Brazil, Mexico, Australia, Turkey, and the western United States.