
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 incorrectCoarse, 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.
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