Rock Identifier
Ferruginous Quartz (Silicon Dioxide (SiO2) with Iron Oxide (Fe2O3) inclusions) — mineral
mineral

Ferruginous Quartz

Silicon Dioxide (SiO2) with Iron Oxide (Fe2O3) inclusions

Hardness: 7 on Mohs scale; Color: Brownish-orange to tan due to iron staining; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); SG: ~2.65

Hardness
7 on Mohs scale
Color
Brownish-orange to tan due to iron staining
Luster
Vitreous to greasy
Identified More mineral

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Physical properties

Hardness: 7 on Mohs scale; Color: Brownish-orange to tan due to iron staining; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); SG: ~2.65

Formation & geological history

Formed through the crystallization of silica-rich hydrothermal fluids. The brown/orange coloration is a result of secondary iron oxide infiltration (like limonite or hematite) into cracks and surfaces over geological time.

Uses & applications

Used primarily as low-grade lapidary material, decorative garden stone, and in metaphysical collecting. Industrial quartz is used in glassmaking and electronics.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust. Ferruginous quartz specifically is often called 'Iron Quartz' or 'Golden Healer' in the gem trade.

Field identification & locations

Identify in the field by its high hardness (it will scratch glass), lack of cleavage, and the presence of rust-colored staining on crystalline surfaces. Common globally in pegmatites and vein deposits.