
mineral
Milky Quartz with Mineral Inclusions
Quartz (Silicon Dioxide, SiO2)
Hardness: 7 on Mohs scale; Color: Opaque white to creamy tan with grey/dark inclusions; Luster: Vitreous to greasy; Crystal Structure: Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Opaque white to creamy tan with grey/dark inclusions
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Opaque white to creamy tan with grey/dark inclusions; Luster: Vitreous to greasy; Crystal Structure: Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed through the crystallization of magma or from hydrothermal veins. The milky appearance is caused by tiny fluid inclusions of gas or liquid trapped during crystal growth. These specimens can range in age from millions to billions of years.
Uses & applications
Used in the glass industry, as an abrasive, in electronics (due to piezoelectric properties), and widely in gemstone carving and landscaping gravel.
Geological facts
Milky quartz is the most common variety of crystalline quartz. Historically, it was used by many cultures for stone tools and ritual objects due to its durability and abundance.
Field identification & locations
Identify in the field by its inability to be scratched by a steel knife (hardness test) and its waxy or greasy luster. It is commonly found in riverbeds, glacial till, and mountainous outcrops worldwide.
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