
mineral
Quartz with Hematite
Silicon Dioxide (SiO2) with Ferric Oxide (Fe2O3)
Hardness: 7 (Mohs); Color: Milky/smoky white with reddish-brown stains; Luster: Vitreous; Crystal Structure: Hexagonal (Trigonal); Cleavage: Indistinct/Conchoidal fracture; Specific Gravity: 2.65.
- Hardness
- 7 (Mohs)
- Color
- Milky/smoky white with reddish-brown stains
- Luster
- Vitreous
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Physical properties
Hardness: 7 (Mohs); Color: Milky/smoky white with reddish-brown stains; Luster: Vitreous; Crystal Structure: Hexagonal (Trigonal); Cleavage: Indistinct/Conchoidal fracture; Specific Gravity: 2.65.
Formation & geological history
Formed through hydrothermal processes in veins or cavities where silica-rich fluids cooled and crystallized. The red coloration is due to the inclusion of Hematite (iron oxide) during or after the quartz formation.
Uses & applications
Used primarily as collector specimens, for metaphysical purposes, and sometimes as low-grade ore for silica in industrial glassmaking.
Geological facts
Quartz is the most abundant mineral in Earth's crust. When hematite is present as fine inclusions, it can create 'Strawberry Quartz' or 'Ferruginous Quartz'.
Field identification & locations
Identify in the field by its hardness (scratches glass), lack of cleavage, and the characteristic conchoidal fracture. Reddish staining often indicates iron influence from surrounding country rock.
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