
mineral
Ferruginous Quartz
Silicon Dioxide (SiO2) with Iron Oxide inclusions
Hardness: 7 (Mohs scale); Color: Yellow-orange to rusty brown due to iron staining; Luster: Vitreous to greasy; Crystal structure: Hexagonal/trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Yellow-orange to rusty brown due to iron staining
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 (Mohs scale); Color: Yellow-orange to rusty brown due to iron staining; Luster: Vitreous to greasy; Crystal structure: Hexagonal/trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed through hydrothermal processes in veins or within pegmatites. The yellow/orange coloring is a secondary staining or inclusion of hematite/limonite that occurs as groundwater rich in iron interacts with the quartz crystals over geological time.
Uses & applications
Used primarily as decorative garden stone, in landscaping, and architectural filler. High-quality specimens are popular among amateur mineral collectors and used in lapidary work for cabochons.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. This specific 'rusty' appearance is often called 'Iron Quartz' or 'Golden Healer' in metaphysical communities.
Field identification & locations
Identify by its ability to scratch glass, its waxy to glassy luster, and the presence of irregular internal fractures. Commonly found in riverbeds, beaches, and mountain runoff areas worldwide.
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mineral