
mineral
Ferruginous Quartz
Quartz (Silicon Dioxide) - SiO2 with Iron Oxide inclusions
Hardness: 7 on the Mohs scale. Color: White to milky with orange, brown, and reddish staining. Luster: Vitreous to greasy. Crystal Structure: Hexagonal (trigonal). Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
- Hardness
- 7 on the Mohs scale
- Color
- White to milky with orange, brown, and reddish staining
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on the Mohs scale. Color: White to milky with orange, brown, and reddish staining. Luster: Vitreous to greasy. Crystal Structure: Hexagonal (trigonal). Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
Formation & geological history
Formed through hydrothermal processes where silica-rich fluids crystallize in veins or pockets. The distinctive coloring comes from the infiltration of iron-bearing minerals like hematite or limonite into cracks or as inclusions during or after growth.
Uses & applications
Primarily used for landscape decoration, as garden stones, or as a collector's specimen for mineral hobbyists. High-purity quartz is used in glassmaking and electronics.
Geological facts
This type of quartz is often called 'Iron Quartz' or 'Golden Healer' in metaphysical circles. The rusty appearance is not surface dirt but is often trapped within the micro-cracks of the crystal structure.
Field identification & locations
Identify in the field by its ability to scratch glass and its lack of cleavage. Look for the characteristic glassy luster hidden beneath the iron-oxide staining. Common globally in igneous and metamorphic terrains.
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