
mineral
White Quartz Pebble
Quartz (Silicon Dioxide, SiO2)
Hardness: 7 on Mohs scale. Color: Milky white to translucent. Luster: Vitreous (glassy) to waxy. Crystal structure: Trigonal/Hexagonal. Cleavage: Indistinct/None. Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Milky white to translucent
- Luster
- Vitreous (glassy) to waxy
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Physical properties
Hardness: 7 on Mohs scale. Color: Milky white to translucent. Luster: Vitreous (glassy) to waxy. Crystal structure: Trigonal/Hexagonal. Cleavage: Indistinct/None. Specific gravity: 2.65.
Formation & geological history
Formed from silica-rich hydrothermal fluids cooling in veins or from the crystallization of igneous magma. This specific specimen is a water-worn river pebble, likely millions of years old, smoothed by erosion.
Uses & applications
Commonly used as decorative landscaping stone (river rock), in glassmaking, as an abrasive, and in electronics for its piezoelectric properties. This specimen has ornamental/garden value.
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 conchoidal fracture. Found globally in riverbeds, beaches, and mountains.
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