
mineral
Milky Quartz with Mica
Silicon Dioxide (SiO2) with Muscovite or Biotite inclusions
AI-generated identification · may be incorrectHardness: 7 on the Mohs scale. Color: White to milky translucent with silvery-green or gray mica flakes. Luster: Vitreous to greasy on quartz, pearly on mica. Crystal Structure: Trigonal (quartz) and monoclinic (mica). Cleavage: None for quartz, perfect basal cleavage for mica. Specific Gravity: 2.65.
- Hardness
- 7 on the Mohs scale
- Luster
- Vitreous to greasy on quartz, pearly on mica
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Physical properties
Hardness: 7 on the Mohs scale. Color: White to milky translucent with silvery-green or gray mica flakes. Luster: Vitreous to greasy on quartz, pearly on mica. Crystal Structure: Trigonal (quartz) and monoclinic (mica). Cleavage: None for quartz, perfect basal cleavage for mica. Specific Gravity: 2.65.
Formation & geological history
Formed in hydrothermal veins, pegmatites, and metamorphic environments through the cooling and crystallization of silica-rich fluids under high pressure and temperature over millions of years.
Uses & applications
Used in mineral collecting, ornamental displays, crystal lapidary work, and sometimes as a decorative landscape stone.
Geological facts
Milky quartz is the most common variety of crystalline quartz found on Earth. The milky appearance is caused by microscopic fluid inclusions trapped during crystal growth.
Field identification & locations
Easily identified by its high hardness (scratches glass), white milky color, conchoidal fracture, and the presence of flaky mica minerals embedded within the matrix. Found worldwide.
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