
mineral
Ferruginous Quartz
Silicon Dioxide (SiO2) with Hematite/Limonite impurities
Hardness: 7 (Mohs scale); Color: Yellowish-brown, orange, or rusty red due to iron oxide; Luster: Vitreous to dull; Crystal structure: Trigonal/Hexagonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65.
- Hardness
- 7 (Mohs scale)
- Color
- Yellowish-brown, orange, or rusty red due to iron oxide
- Luster
- Vitreous to dull
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Physical properties
Hardness: 7 (Mohs scale); Color: Yellowish-brown, orange, or rusty red due to iron oxide; Luster: Vitreous to dull; Crystal structure: Trigonal/Hexagonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65.
Formation & geological history
Formed through hydrothermal processes where silica-rich fluids crystallize in veins or cavities. The rusty coloration occurs when iron-rich groundwater (containing hematite or limonite) coats the surface or leaches into internal fractures over geological time.
Uses & applications
Primarily used as decorative stones, in landscaping, or as specimens for hobbyist mineral collectors. Larger industrial deposits of high-purity quartz are used in glass-making and electronics.
Geological facts
Also known as 'Iron Quartz' or 'Golden Healer' in metaphysical communities. The orange and brown staining is often just a thin 'skin' or coating that can sometimes be removed with oxalic acid to reveal clear quartz underneath.
Field identification & locations
Identify in the field by its ability to scratch glass and its characteristic rusty staining alongside a translucent to milky interior. It is commonly found in gravel pits, riverbeds, and mountainous regions worldwide.
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