Rock Identifier
Quartz-rich breccia or vein quartz specimen (Microcrystalline and crystalline quartz (SiO₂), possibly with iron-oxide staining and minor sulfides) — mineral
mineral

Quartz-rich breccia or vein quartz specimen

Microcrystalline and crystalline quartz (SiO₂), possibly with iron-oxide staining and minor sulfides

AI-generated identification · may be incorrect

Hardness about 7 Mohs; white, gray, translucent, and brown-gold areas with vitreous to waxy luster. Irregular fractured/brecciated texture, no obvious cleavage, and specific gravity near 2.65; the metallic dark patches may be iron oxides or sulfides.

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Physical properties

Hardness about 7 Mohs; white, gray, translucent, and brown-gold areas with vitreous to waxy luster. Irregular fractured/brecciated texture, no obvious cleavage, and specific gravity near 2.65; the metallic dark patches may be iron oxides or sulfides.

Formation & geological history

Likely formed when silica-rich hydrothermal fluids filled and cemented fractures, with later oxidation producing brown and black staining. Exact geological age and locality cannot be determined from the photograph.

Uses & applications

Common quartz-rich material is used for aggregate, silica, glass, and decorative stone; attractive pieces are sold as cabinet specimens. Value is usually modest unless the metallic inclusions or locality are distinctive.

Geological facts

The angular internal fragments and vein-like pale quartz are characteristic of brecciation followed by mineral deposition. A streak test, hardness test, and close inspection for metallic sulfides would improve identification.

Field identification & locations

Look for glassy fracture surfaces, inability to scratch quartz with a steel knife, and possible iron-rich yellow-brown coatings; vinegar will not fizz. Common in hydrothermal veins and mineralized fault zones worldwide.