
mineral
Quartz with Iron Staining
Silicon Dioxide (SiO2) with Hematite/Limonite inclusions
AI-generated identification · may be incorrectHardness: 7 on Mohs scale. Color: Translucent white to milky quartz mixed with reddish-brown to orange iron oxide coatings. Luster: Vitreous to dull in weathered pockets. Fracture: Conchoidal to irregular.
- Hardness
- 7 on Mohs scale
- Luster
- Vitreous to dull in weathered pockets
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Physical properties
Hardness: 7 on Mohs scale. Color: Translucent white to milky quartz mixed with reddish-brown to orange iron oxide coatings. Luster: Vitreous to dull in weathered pockets. Fracture: Conchoidal to irregular.
Formation & geological history
Formed through hydrothermal or igneous processes where silica-rich fluids crystallized. The reddish coloration is caused by secondary oxidation of iron minerals (hematite or limonite) filling cracks and surface cavities.
Uses & applications
Used primarily as decorative specimens, in landscaping, lapidary tumbling, and as raw quartz material for industrial silica applications.
Geological facts
Iron oxide staining on quartz is often called 'iron rose' or 'red quartz' depending on the depth of coverage. The reddish skin can often be cleaned using oxalates or mild acids if clear quartz is preferred underneath.
Field identification & locations
Identify in the field by its hardness (scratches glass), glass-like fractured surfaces mixed with rusty orange-red iron staining. Highly common in riverbeds, gravel deposits, and pegmatite veins worldwide.
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