
mineral
Quartz Pebble
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale. Color: Translucent white to milky tan. Luster: Vitreous to waxy (when water-worn). Crystal Structure: Hexagonal (trigonal). Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Translucent white to milky tan
- Luster
- Vitreous to waxy (when water-worn)
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Physical properties
Hardness: 7 on Mohs scale. Color: Translucent white to milky tan. Luster: Vitreous to waxy (when water-worn). Crystal Structure: Hexagonal (trigonal). Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
Formation & geological history
Formed from silica-rich hydrothermal fluids or within igneous and metamorphic rocks. This specific specimen has been weather-worn and rounded by water transport in a river or coastal environment, likely over thousands of years.
Uses & applications
Used in glassmaking, abrasives, and as decorative landscaping gravel. High-purity quartz is essential in electronics and silicon chip manufacturing.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. This pebble shape is the result of 'abrasion' which happens as the rock hits others in moving water.
Field identification & locations
Identify by its hardness (cannot be scratched by a steel knife) and lack of cleavage. Often found in riverbeds, beaches, and glacial till globally.
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Epidote
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Granite (Phaneritic intrusive igneous rock)
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