Rock Identifier
Quartz vein in iron-stained host rock (Quartz (SiO₂) with limonite/goethite staining, likely in altered basalt or another dark volcanic host) — mineral
mineral

Quartz vein in iron-stained host rock

Quartz (SiO₂) with limonite/goethite staining, likely in altered basalt or another dark volcanic host

AI-generated identification · may be incorrect

The specimen shows translucent to milky gray quartz with a glassy luster and irregular fracture, surrounded by rusty yellow-brown iron oxides and a dark fine-grained host. Quartz is Mohs hardness 7, lacks cleavage, and has specific gravity about 2.65;…

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Physical properties

The specimen shows translucent to milky gray quartz with a glassy luster and irregular fracture, surrounded by rusty yellow-brown iron oxides and a dark fine-grained host. Quartz is Mohs hardness 7, lacks cleavage, and has specific gravity about 2.65; the host is substantially softer or similar depending on composition.

Formation & geological history

Quartz precipitated from silica-rich hydrothermal fluids filling a fracture, while oxidation of iron-bearing minerals produced the limonite/goethite coating. The exact age and host rock cannot be determined from the image; such veins occur in many volcanic and metamorphic terrains.

Uses & applications

Primarily a collecting specimen; quartz-bearing rock may have minor industrial significance, but this piece is not gem grade or suitable for construction aggregate.

Geological facts

The orange-brown coloration is iron-oxide staining rather than the quartz’s intrinsic color. Quartz veins commonly record ancient fluid movement and can locally accompany sulfide ores or gold.

Field identification & locations

Identify it by testing for hardness: quartz scratches ordinary glass and resists a steel blade; acid produces no reaction. Common settings include hydrothermal veins in volcanic and metamorphic rocks worldwide.