Rock Identifier
Iron-stained quartz-rich rock, possibly quartz vein material (Quartz-rich vein rock with iron oxides/hydroxides (quartz, Fe₂O₃/FeO(OH)); exact identification requires testing) — metamorphic
metamorphic

Iron-stained quartz-rich rock, possibly quartz vein material

Quartz-rich vein rock with iron oxides/hydroxides (quartz, Fe₂O₃/FeO(OH)); exact identification requires testing

AI-generated identification · may be incorrect

Coarse, irregular quartz-rich mass with rusty red-brown, ochre, and pale gray areas. Quartz has Mohs hardness 7, vitreous luster, and hexagonal crystal structure; iron staining is earthy to dull. The specimen’s cleavage and density cannot be established from the image.

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Physical properties

Coarse, irregular quartz-rich mass with rusty red-brown, ochre, and pale gray areas. Quartz has Mohs hardness 7, vitreous luster, and hexagonal crystal structure; iron staining is earthy to dull. The specimen’s cleavage and density cannot be established from the image.

Formation & geological history

Likely formed when silica-rich fluids filled fractures and crystallized as quartz, followed or accompanied by iron-oxide alteration. The age and host-rock setting are not determinable from the photograph.

Uses & applications

Comparable material may be used as decorative stone, aggregate, or mineral-collection material; no obvious gem-quality crystals are visible.

Geological facts

Rust-colored staining commonly comes from hematite or goethite produced by oxidation of iron-bearing minerals.

Field identification & locations

Look for hard, glassy quartz patches that resist scratching by a steel nail, alongside softer rusty coatings. Quartz veins occur worldwide; the pictured outcrop context is insufficient to identify a locality or rock type confidently.