
mineral
Ferruginous Quartz
Silicon Dioxide with Iron Oxide inclusions (SiO2 + Fe2O3)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: Oranges, reds, and browns due to iron staining; Luster: Vitreous to greasy; Crystal Structure: Trigonal; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Oranges, reds, and browns due to iron staining
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 (Mohs scale); Color: Oranges, reds, and browns due to iron staining; Luster: Vitreous to greasy; Crystal Structure: Trigonal; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65
Formation & geological history
Formed in hydrothermal veins or as a secondary mineral where iron-rich fluids interact with quartz crystals. The orange-red hue is caused by hematite or limonite inclusions during or after crystal growth.
Uses & applications
Used primarily by collectors and in metaphysical jewelry (often called 'Healer's Gold' or 'Hematoid Quartz').
Geological facts
The name 'ferruginous' comes from the Latin word 'ferrum', meaning iron. It is a common variety of quartz found globally where iron oxides are present in the soil or rock matrix.
Field identification & locations
Identify in the field by its hardness (will scratch glass) and its characteristic conchoidal fracture. Found frequently in gravel pits, riverbeds, and near iron-ore deposits.
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