
mineral
Milky Quartz with Pyrite and Iron Staining
Silicon Dioxide (SiO2) with Iron Disulfide (FeS2) inclusions
Hardness: 7 (Quartz) / 6-6.5 (Pyrite). Color: White to translucent with metallic gold flecks and reddish-orange staining. Luster: Vitreous to greasy. Crystal structure: Trigonal/Hexagonal. Cleavage: Indistinct/Conchoidal fracture.
- Hardness
- 7 (Quartz) / 6-6
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 (Quartz) / 6-6.5 (Pyrite). Color: White to translucent with metallic gold flecks and reddish-orange staining. Luster: Vitreous to greasy. Crystal structure: Trigonal/Hexagonal. Cleavage: Indistinct/Conchoidal fracture.
Formation & geological history
Formed in hydrothermal veins and pegmatites through the cooling of silica-rich hot fluids. The iron staining occurs from the oxidation of iron-bearing minerals (like pyrite) when exposed to water and air.
Uses & applications
Primarily used as decorative garden stone, landscape rock, or for mineral collecting. High-purity quartz is used in electronics and glass manufacturing.
Geological facts
The reddish-orange patches are often called 'Golden Healer' in metaphysical circles, though geologically it is simply hematite or limonite staining. The metallic inclusion is pyrite, famously known as 'fool\'s gold'.
Field identification & locations
Identify in the field by its hardness (it will scratch glass), its conchoidal (shell-like) fracture, and the presence of metallic inclusions. Commonly found in mountainous regions or creek beds near quartz veins.
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