
mineral
Quartz with Iron Staining
Silicon Dioxide (SiO2) with Ferric Iron Oxides
AI-generated identification · may be incorrectHardness: 7 on Mohs scale. Color: Clear to white crystals with orange/brown staining. Luster: Vitreous (glassy). Crystal Structure: Hexagonal (trigonal system). Cleavage: None (conchoidal fracture).
- Hardness
- 7 on Mohs scale
- Color
- Clear to white crystals with orange/brown staining
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale. Color: Clear to white crystals with orange/brown staining. Luster: Vitreous (glassy). Crystal Structure: Hexagonal (trigonal system). Cleavage: None (conchoidal fracture).
Formation & geological history
Forms in hydrothermal veins or cavities within various rock types. The iron staining occurs when groundwater rich in iron oxide (limonite or hematite) coats the surfaces or penetrates micro-fractures in the quartz.
Uses & applications
Commonly used as decorative specimens, in jewelry as 'Sun-baked' or 'Tangerine' quartz, and in high volumes for the production of silicon, glass, and electronics.
Geological facts
Iron-stained quartz is colloquially known among some collectors as 'golden healer' or 'limonite quartz' depending on the depth and color of the coating. The staining is purely superficial and can often be removed with oxalic acid.
Field identification & locations
Identify in the field by its six-sided crystal faces and its ability to scratch glass easily. Look for these in rocky outcrops, dry creek beds, or around mine tailings. Found globally in almost all geological environments.
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