
mineral
Ferruginous Quartz
Silicon Dioxide (SiO2) with Iron Oxide inclusions
Hardness: 7 on the Mohs scale. Color: Translucent white to opaque tan, orange, or rusty brown due to iron. Luster: Vitreous to dull. Crystal Structure: Hexagonal (trigonal) crystal system. Cleavage: Indistinct/Conchoidal fracture.
- Hardness
- 7 on the Mohs scale
- Luster
- Vitreous to dull
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Physical properties
Hardness: 7 on the Mohs scale. Color: Translucent white to opaque tan, orange, or rusty brown due to iron. Luster: Vitreous to dull. Crystal Structure: Hexagonal (trigonal) crystal system. Cleavage: Indistinct/Conchoidal fracture.
Formation & geological history
Formed in hydrothermal veins or as mass precipitates. The iron staining occurs when groundwater rich in iron oxide (limonite or hematite) coats or infiltrates the quartz crystals during or after formation.
Uses & applications
Used primarily as decorative garden stones, in rough jewelry (cabs), and as pocket stones for collectors. High-quality clear quartz is used in electronics, but ferruginous varieties are mostly ornamental.
Geological facts
Also known as 'Iron Quartz' or 'Golden Healer' in metaphysical circles. This specific specimen appears to be a water-worn or weathered chunk of vein quartz, which has acquired a characteristic 'rusty' patina through oxidation.
Field identification & locations
Identify by its ability to scratch glass (hardness 7) and its lack of reaction to acid. It is commonly found in gravel pits, riverbeds, and mountainous regions worldwide. Collectors look for unique banding or internal iron dendrites.
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