
mineral
Ferruginous Quartz (Iron-stained Quartz)
Silicon Dioxide (SiO2) with Iron Oxide inclusions
Hardness: 7 (Mohs scale); Color: Rusty red, orange, and white; Luster: Vitreous to dull; Crystal structure: Hexagonal/Trigonal; Conchoidal fracture.
- Hardness
- 7 (Mohs scale)
- Color
- Rusty red, orange, and white
- Luster
- Vitreous to dull
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Physical properties
Hardness: 7 (Mohs scale); Color: Rusty red, orange, and white; Luster: Vitreous to dull; Crystal structure: Hexagonal/Trigonal; Conchoidal fracture.
Formation & geological history
Formed in hydrothermal veins or as a secondary deposit where iron-rich groundwater stains existing quartz over geological time. Often found as river-worn cobbles.
Uses & applications
Primarily collected as a lapidary material or specimen; also used in landscaping and as a source of high-purity silica in industrial glassmaking if cleaned.
Geological facts
The red coloration is caused by thin films or inclusions of hematite or limonite. In many cultures, these are referred to as 'Hematoïd Quartz' or 'Fire Quartz' when the inclusions are bright red.
Field identification & locations
Identify in the field by its superior hardness (cannot be scratched by steel) and various iron-staining patterns. Common in gravel pits and riverbeds globally.
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