
mineral
Quartz (Iron-stained)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale), Color: Clear to translucent with orange/brown surface staining (Iron Oxide/Limonite), Luster: Vitreous, Crystal Structure: Hexagonal/Trigonal, Cleavage: None (Conchoidal fracture), Specific Gravity: 2.65
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Physical properties
Hardness: 7 (Mohs scale), Color: Clear to translucent with orange/brown surface staining (Iron Oxide/Limonite), Luster: Vitreous, Crystal Structure: Hexagonal/Trigonal, Cleavage: None (Conchoidal fracture), Specific Gravity: 2.65
Formation & geological history
Formed from cooling silica-rich magma or from hydrothermal veins. The iron staining occurs when the specimen is exposed to groundwater containing dissolved iron minerals which precipitate onto the surface or into micro-fractures.
Uses & applications
Used extensively in the glass industry, electronics (piezoelectric properties), and as decorative specimens or metaphysical stones. Natural crystals are popular for amateur collectors.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Iron-stained quartz is often mistakenly called 'Tangerine Quartz' or 'Golden Healer' in metaphysical communities.
Field identification & locations
Identify by its hardness (scratches glass), conchoidal fracture (curved glass-like breaks), and lack of cleavage. Common worldwide in nearly all geological environments. This specific piece shows a typical rough, naturally weathered appearance.
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