
mineral
Milky Quartz Pebble
Quartz (Silicon Dioxide - SiO2)
Hardness: 7 on Mohs scale; Color: Milky white to light grey; Luster: Vitreous (glassy) to waxy when wet; Crystal structure: Trigonal/Hexagonal (cryptocrystalline in this form); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Milky white to light grey
- Luster
- Vitreous (glassy) to waxy when wet
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Physical properties
Hardness: 7 on Mohs scale; Color: Milky white to light grey; Luster: Vitreous (glassy) to waxy when wet; Crystal structure: Trigonal/Hexagonal (cryptocrystalline in this form); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed from silica-rich hydrothermal fluids cooling in veins or from the crystallization of magma. This specific specimen is a 'river rock' or 'tumble stones' pebble, shaped and smoothed by water erosion over thousands of years.
Uses & applications
Used in glassmaking, electronics (piezoelectric properties), abrasives, and as decorative gravel or landscaping stones. Polished versions are common in beginner rock collections and metaphysical use.
Geological facts
Milky quartz gets its cloudy appearance from tiny fluid inclusions of gas or liquid trapped during the crystal's growth. It is the most common variety of crystalline quartz found on Earth's crust.
Field identification & locations
Identify in the field by its inability to be scratched by a steel knife, its white 'milky' opacity, and its smooth, rounded texture if found near water. It is ubiquitous in gravel beds, beaches, and mountain streams worldwide.
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