
mineral
Ferruginous Quartz
Silicon Dioxide (SiO2) with Iron Oxide (Fe2O3) inclusions
Hardness: 7 on Mohs scale; Color: Brownish-orange to tan due to iron staining; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); SG: ~2.65
- Hardness
- 7 on Mohs scale
- Color
- Brownish-orange to tan due to iron staining
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Brownish-orange to tan due to iron staining; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); SG: ~2.65
Formation & geological history
Formed through the crystallization of silica-rich hydrothermal fluids. The brown/orange coloration is a result of secondary iron oxide infiltration (like limonite or hematite) into cracks and surfaces over geological time.
Uses & applications
Used primarily as low-grade lapidary material, decorative garden stone, and in metaphysical collecting. Industrial quartz is used in glassmaking and electronics.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Ferruginous quartz specifically is often called 'Iron Quartz' or 'Golden Healer' in the gem trade.
Field identification & locations
Identify in the field by its high hardness (it will scratch glass), lack of cleavage, and the presence of rust-colored staining on crystalline surfaces. Common globally in pegmatites and vein deposits.
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