
mineral
Milky Quartz Pebble
Silicon Dioxide (SiO2)
Hardness: 7 (Mohs scale); Color: White to tan with iron staining; Luster: Vitreous to waxy; Crystal structure: Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 (Mohs scale)
- Color
- White to tan with iron staining
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 (Mohs scale); Color: White to tan with iron staining; Luster: Vitreous to waxy; Crystal structure: Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed in hydrothermal veins or as a primary constituent of granitic pegmatites. This specific specimen is a water-worn or weathered pebble likely sourced from a fluvial or glacial deposit.
Uses & applications
Used in glass making, as an abrasive, in electronics (piezoelectric properties), and frequently as landscaping gravel or for lapidary tumbling.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Milky quartz gets its cloudy appearance from tiny fluid inclusions of gas or liquid trapped during crystal growth.
Field identification & locations
Identify in the field by its hardness (will scratch glass), lack of cleavage, and translucent to opaque white color. Found globally in almost all geological environments.
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