
mineral
Bull Quartz (Milky Quartz)
Quartz (Silicon Dioxide - SiO2)
Hardness: 7 on Mohs scale. Color: White to off-white with yellowish-brown iron staining. Luster: Vitreous to greasy. Crystal Structure: Hexagonal (often massive in this form). Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- White to off-white with yellowish-brown iron staining
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale. Color: White to off-white with yellowish-brown iron staining. Luster: Vitreous to greasy. Crystal Structure: Hexagonal (often massive in this form). Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
Formation & geological history
Formed from the cooling of silica-rich hydrothermal fluids in veins or as a primary mineral in igneous pegmatites. The milky appearance is caused by tiny inclusions of gas or liquid trapped during crystal growth. Can be found in rocks from almost any geological age.
Uses & applications
Used in glass making, as an abrasive, in the production of silicon for electronics, and as decorative stone in landscaping or rough rock collections. In historical mining, it was often used as an indicator for finding gold-bearing veins.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Milky quartz is the most common variety of crystalline quartz. Historically, it was sometimes referred to as 'low-grade quartz' when found without clear crystal terminations.
Field identification & locations
Identify in the field by its hardness (it will scratch glass and steel), lack of cleavage, and translucent white color. It is commonly found in mountainous regions, riverbeds as rounded pebbles, or protruding from eroded outcrops. Collectors look for iron staining (as seen here) which can sometimes indicate nearby mineralization.
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