Rock Identifier
Milky quartz with dark mineral veins (Quartz, silicon dioxide (SiO₂), likely massive vein quartz; dark veins may be chlorite, mica, iron/manganese oxides, or a sulfide mineral) — mineral
mineral

Milky quartz with dark mineral veins

Quartz, silicon dioxide (SiO₂), likely massive vein quartz; dark veins may be chlorite, mica, iron/manganese oxides, or a sulfide mineral

AI-generated identification · may be incorrect

Typically white to cream, translucent to opaque, with a vitreous-to-waxy luster and irregular fracture; Mohs hardness 7, no cleavage, hexagonal crystal structure, and specific gravity about 2.65. The specimen appears massive and weathered rather than distinctly crystalline.

Identified More mineral
Explore Milky quartz with dark mineral veins in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Typically white to cream, translucent to opaque, with a vitreous-to-waxy luster and irregular fracture; Mohs hardness 7, no cleavage, hexagonal crystal structure, and specific gravity about 2.65. The specimen appears massive and weathered rather than distinctly crystalline.

Formation & geological history

Likely formed when silica-rich hydrothermal fluids filled fractures in surrounding rock, later exposed by uplift and weathering; precise age and locality cannot be determined from the image. Associated dark material may represent altered host rock or secondary minerals.

Uses & applications

Quartz is used in glass, ceramics, electronics, abrasives, and engineered stone; attractive pieces are sold as cabinet specimens or lapidary material. The irregular, fractured appearance limits gemstone value.

Geological facts

Milky color results from microscopic fluid inclusions, fractures, or defects scattering light. Dark vein material should be tested separately because it may significantly change the identification.

Field identification & locations

Identify with a steel file or glass-scratch test: quartz should scratch glass and resist a steel knife; it should not fizz in dilute acid. Common in hydrothermal veins, pegmatites, and quartz-rich metamorphic rocks worldwide.