
mineral
Milky Quartz Pebble
Quartz (Silicon Dioxide, SiO2)
Hardness: 7 on Mohs scale. Color: Milky white to translucent off-white. Luster: Vitreous to greasy. Crystal System: Trigonal. Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Milky white to translucent off-white
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale. Color: Milky white to translucent off-white. Luster: Vitreous to greasy. Crystal System: Trigonal. Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
Formation & geological history
Forms in igneous, metamorphic, and hydrothermally altered rock environments. White opacity is caused by microscopic fluid inclusions trapped during crystal growth. This rounded specimen was shaped and smoothed by natural water erosion in a stream, river, or beach environment.
Uses & applications
Used in glassmaking, abrasives, quartz gravel for landscaping, and as a common specimen for rock tumbling and entry-level mineral collections.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Milky quartz gets its cloudy appearance from millions of microscopic bubbles of gas and liquid trapped as the mineral crystallized.
Field identification & locations
Identified by its harness (can scratch glass easily and cannot be scratched by a steel knife), smooth water-worn surface, lack of cleavage, and characteristic waxy or vitreous white appearance. Found worldwide in riverbeds, gravel deposits, and beaches.
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