Rock Identifier
Quartz vein rock with iron-oxide staining (Milky quartz (SiO₂), locally stained by hematite/goethite; possible feldspar or host-rock fragments) — mineral
mineral

Quartz vein rock with iron-oxide staining

Milky quartz (SiO₂), locally stained by hematite/goethite; possible feldspar or host-rock fragments

AI-generated identification · may be incorrect

Hardness about 7 Mohs; white to translucent, glassy-to-waxy luster, irregular fracture, and no obvious cleavage. Red-orange areas are likely iron oxides, while the coarse granular texture suggests a quartz-rich vein or breccia.

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Physical properties

Hardness about 7 Mohs; white to translucent, glassy-to-waxy luster, irregular fracture, and no obvious cleavage. Red-orange areas are likely iron oxides, while the coarse granular texture suggests a quartz-rich vein or breccia.

Formation & geological history

Formed when silica-rich hydrothermal fluids filled fractures and crystallized, later weathering to produce red hematite/goethite staining; exact age and host rock cannot be determined from the photograph.

Uses & applications

Common quartz specimens are collected decoratively and used in glass, abrasives, electronics, and engineered stone; iron-stained pieces are mainly ornamental or educational.

Geological facts

Quartz is one of Earth’s most abundant minerals and is piezoelectric. The red coloration generally reflects oxidized iron rather than red quartz itself.

Field identification & locations

Look for scratch resistance against glass, translucent gray-white quartz, and rusty red coatings; avoid confusing it with glass or resin. Common in hydrothermal veins worldwide, especially in granitic and metamorphic terrains.