Rock Identifier
Iron-stained quartz vein rock (Quartz-rich vein material with iron oxides/hydroxides (quartz, SiO₂, stained by hematite/goethite); likely hosted in a metamorphic rock) — metamorphic
metamorphic

Iron-stained quartz vein rock

Quartz-rich vein material with iron oxides/hydroxides (quartz, SiO₂, stained by hematite/goethite); likely hosted in a metamorphic rock

AI-generated identification · may be incorrect

White translucent-to-opaque quartz occurs with rusty red-brown iron staining and darker mineral grains. Quartz is Mohs 7, vitreous, and lacks cleavage; the stated lack of scratching in the white area is consistent with quartz, though a steel nail test is not definitive. Grainy, irregular texture;…

Identified More metamorphic →
Explore Iron-stained quartz vein rock in the encyclopedia →

Identify your own rocks.

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

Physical properties

White translucent-to-opaque quartz occurs with rusty red-brown iron staining and darker mineral grains. Quartz is Mohs 7, vitreous, and lacks cleavage; the stated lack of scratching in the white area is consistent with quartz, though a steel nail test is not definitive. Grainy, irregular texture; bulk hardness and density vary with the host rock.

Formation & geological history

Likely formed when silica-rich fluids filled fractures, then iron-bearing minerals oxidized to hematite/goethite; the host may have been altered or metamorphosed. The exact age and setting cannot be determined from the image alone.

Uses & applications

Mostly a collector or teaching specimen; quartz-rich material may have industrial uses if sufficiently pure and abundant, while this iron-stained piece is unlikely to be gem-grade.

Geological facts

Rusty colors commonly come from very small amounts of iron oxides coating or intergrown with quartz and other minerals.

Field identification & locations

Look for hard white patches that resist scratching, glassy or sugary fracture surfaces, and no regular cleavage; the red-brown staining suggests iron oxides. Quartz veins occur worldwide, including in metamorphic terrains, but precise locality needs field context.