Rock Identifier
Milky quartz (rough quartz crystal) (Quartz, silicon dioxide (SiO₂)) — mineral
mineral

Milky quartz (rough quartz crystal)

Quartz, silicon dioxide (SiO₂)

AI-generated identification · may be incorrect

Typically Mohs hardness 7, white to translucent, with a vitreous to waxy luster and hexagonal crystal structure; quartz has no true cleavage and shows conchoidal fracture. The specimen appears massive and fractured rather than sharply crystallized, with internal cloudiness likely from microscopic fluid inclusions or fr…

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Physical properties

Typically Mohs hardness 7, white to translucent, with a vitreous to waxy luster and hexagonal crystal structure; quartz has no true cleavage and shows conchoidal fracture. The specimen appears massive and fractured rather than sharply crystallized, with internal cloudiness likely from microscopic fluid inclusions or fractures.

Formation & geological history

Forms when silica-rich hydrothermal fluids cool in fractures and cavities, or crystallizes from igneous melts; quartz occurs from Precambrian rocks to modern veins. Exact age and locality cannot be determined from the photograph.

Uses & applications

Used in glass, ceramics, electronics, abrasives, engineered stone, and decorative objects; attractive translucent pieces are sold as inexpensive mineral specimens.

Geological facts

It can scratch ordinary steel or glass, while a steel blade will not scratch it. Milky quartz is common and is often confused with white calcite, which is softer and reacts with dilute acid.

Field identification & locations

Common in quartz veins, granite, pegmatites, metamorphic rocks, and stream gravels worldwide; test hardness and inspect for conchoidal fracture, but avoid destructive testing on valuable specimens. Likely a rough milky quartz fragment.