
mineral
Milky quartz pebble
Quartz (silicon dioxide, SiO₂)
AI-generated identification · may be incorrectWhite to translucent, glassy-to-waxy luster with irregular fracture and no obvious cleavage; Mohs hardness 7, specific gravity about 2.65, trigonal crystal structure. The rounded shape suggests natural water wear or tumbling.
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Physical properties
White to translucent, glassy-to-waxy luster with irregular fracture and no obvious cleavage; Mohs hardness 7, specific gravity about 2.65, trigonal crystal structure. The rounded shape suggests natural water wear or tumbling.
Formation & geological history
Forms when microscopic fluid inclusions, fractures, or impurities cloud otherwise clear quartz, commonly in igneous and metamorphic rocks and hydrothermal veins. Quartz is widespread from Precambrian to modern geological settings.
Uses & applications
Used as a durable aggregate, glass and ceramic raw material, abrasives, and ornamental or lapidary material; attractive pieces are collected but usually have modest value.
Geological facts
Quartz is one of Earth’s most abundant minerals and can scratch ordinary steel or glass. A steel nail should not scratch it, while quartz can scratch a knife blade or window glass.
Field identification & locations
Common in streambeds, quartz veins, granitic terrains, and beaches; identify by hardness, pale color, and lack of cleavage. The image alone cannot exclude white calcite, which is softer and reacts with dilute acid.
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