
mineral
Milky Quartz (or Iron-Stained Quartz)
Quartz (Silicon Dioxide, SiO2)
Hardness: 7 on Mohs scale; Color: Milky white with yellowish-brown iron oxidation staining; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Milky white with yellowish-brown iron oxidation staining
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Milky white with yellowish-brown iron oxidation staining; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed through hydrothermal processes where silica-rich fluids cool in veins, or as a primary mineral in igneous and metamorphic rocks. This specimen likely formed in a hydrothermal vein and has been weathered at the surface, leading to the iron-oxide staining (rust colors).
Uses & applications
Used in glass manufacturing, as an abrasive, in electronics (piezoelectric properties), in construction as aggregate, and as a semi-precious gemstone or metaphysical specimen.
Geological facts
Quartz is the second most abundant mineral in the Earth's continental crust. Milky quartz gets its opaque white color from microscopic fluid inclusions of gas or liquid trapped during crystal growth.
Field identification & locations
Identify in the field by its hardness (it will scratch glass and steel), lack of cleavage, and waxy/vitreous luster. Common in mountainous regions, riverbeds, and as veins in surrounding rock. Tips for collectors: check for crystal faces in cavities (vugs).
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