
mineral
Hematoid Quartz (Fire Quartz)
Silicon Dioxide with Iron Oxide (SiO2 with Fe2O3)
Hardness: 7 on the Mohs scale. Color: Translucent to opaque white/translucent quartz with reddish-orange to brown hematite specks or inclusions. Luster: Vitreous to dull. Crystal structure: Trigonal (hexagonal system). Cleavage: None, exhibits conchoidal fracture.
- Hardness
- 7 on the Mohs scale
- Luster
- Vitreous to dull
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Physical properties
Hardness: 7 on the Mohs scale. Color: Translucent to opaque white/translucent quartz with reddish-orange to brown hematite specks or inclusions. Luster: Vitreous to dull. Crystal structure: Trigonal (hexagonal system). Cleavage: None, exhibits conchoidal fracture.
Formation & geological history
Formed when iron-rich water or minerals coat quartz crystals during or after growth, depositing hematite (iron oxide) inclusions inside or on the surface of the quartz matrix.
Uses & applications
Popular in lapidary work, jewelry, crystal healing practices, decorative displays, and mineral collection.
Geological facts
Also widely known as 'Fire Quartz' or 'Harlequin Quartz'. The distinctive red flecks and staining are caused by microscopic inclusions of hematite or goethite embedded within the quartz body.
Field identification & locations
Identified by its characteristic quartz hardness, vitreous body, and distinct reddish-pink to rust-colored spots or streaks. Commonly found worldwide in hydrothermal veins and pegmatites, notably in Brazil, Madagascar, and the USA.
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