
mineral
Tumbled white stone, likely milky quartz
Quartz (SiO₂), probable; identification is uncertain from the photo alone
AI-generated identification · may be incorrectOpaque to translucent white, smooth and rounded; quartz has Mohs hardness 7, a vitreous luster when freshly broken, and no cleavage. The polished surface appears matte or softly glossy.
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Physical properties
Opaque to translucent white, smooth and rounded; quartz has Mohs hardness 7, a vitreous luster when freshly broken, and no cleavage. The polished surface appears matte or softly glossy.
Formation & geological history
If quartz, it formed as silica crystallized in veins or cavities and was later naturally rounded or mechanically tumbled. Quartz occurs in rocks of many geological ages.
Uses & applications
Common as a decorative or collectible tumbled stone; quartz is also used in glassmaking, electronics, and construction materials.
Geological facts
Quartz is one of Earth’s most abundant minerals; milky appearance usually comes from microscopic inclusions or fluid-filled defects.
Field identification & locations
A hardness or streak test, or inspection for conchoidal fracture, can help distinguish quartz from softer white stones such as calcite. Quartz is widespread worldwide; the photo does not establish the exact material or locality.
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