
mineral
Milky Quartz
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Milky white to light grey; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Milky white to light grey
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Milky white to light grey; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Forms in hydrothermal veins, pegmatites, and as a primary constituent in igneous rocks like granite. The milky opacity is caused by microscopic fluid inclusions of gas or liquid trapped during crystal growth.
Uses & applications
Used as a gemstone, in glassmaking, as a source of silicon for electronics, and widely as a decorative stone or landscaping material.
Geological facts
Milky quartz is the most common variety of crystalline quartz. It can often be found in large veins that are meters wide, sometimes containing traces of gold.
Field identification & locations
Identify by its hardness (will scratch glass), lack of cleavage, white color, and grainy or glassy texture. It is ubiquitous in riverbeds and mountainous regions globally.
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Schist
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Potassium Feldspar (Orthoclase)
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