
mineral
Ferruginous Quartz
Silicon Dioxide with Iron Oxide (SiO2 + Fe2O3)
Hardness: 7 (Mohs scale); Color: Rusty orange, reddish-brown, or yellowish-tan; Luster: Vitreous to greasy; Crystal structure: Trigonal/Hexagonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65.
- Hardness
- 7 (Mohs scale)
- Color
- Rusty orange, reddish-brown, or yellowish-tan
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 (Mohs scale); Color: Rusty orange, reddish-brown, or yellowish-tan; Luster: Vitreous to greasy; Crystal structure: Trigonal/Hexagonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65.
Formation & geological history
Formed from silica-rich hydrothermal solutions or within metamorphic and igneous rocks. The distinct orange color is caused by hematite or limonite staining or inclusions, often occurring as groundwater percolates through cracks in the quartz over geological time.
Uses & applications
Commonly used in lapidary work for cabochons and tumbled stones, as decorative garden rocks, and occasionally in metaphysical collections.
Geological facts
Also known as iron quartz or 'Hematoid Quartz.' The iron oxide can be present as a thin coating on the outside or as internal inclusions that give the entire crystal a solid color.
Field identification & locations
Identify in the field by its high hardness (it will scratch glass), lack of cleavage, and the characteristic rusty staining. It is frequently found in riverbeds, gravel pits, and areas with high iron content in the soil.
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mineral