
mineral
White Quartz Pebble
Quartz (Silicon Dioxide, SiO2)
Hardness: 7 (Mohs scale); Color: White/milky; Luster: Vitreous to waxy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- White/milky
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 (Mohs scale); Color: White/milky; Luster: Vitreous to waxy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed through hydrothermal processes or igneous crystallization within veins. This specific specimen has been rounded and smoothed by water erosion (alluvial or beach action), likely over thousands of years.
Uses & applications
Used in glassmaking, electronics (piezoelectric properties), abrasives, and as decorative landscaping stone. Polished versions are used in costume jewelry and chakra/healing stone collections.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Milky white quartz gets its appearance from tiny fluid inclusions of gas or liquid trapped during crystal growth.
Field identification & locations
Identify in the field by its hardness (it will scratch glass) and lack of cleavage. It is commonly found in riverbeds, beaches, and mountain trails globally.
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