
mineral
Quartz Pebble
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale. Color: Milky white to translucent. Luster: Vitreous (glassy) to greasy. Crystal system: Trigonal. Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Milky white to translucent
- Luster
- Vitreous (glassy) to greasy
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Physical properties
Hardness: 7 on Mohs scale. Color: Milky white to translucent. Luster: Vitreous (glassy) to greasy. Crystal system: Trigonal. Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
Formation & geological history
Formed in igneous pegmatites, hydrothermal veins, and metamorphic rocks. Over time, weathering and water erosion break down the host rock, smoothing the durable quartz into river or beach pebbles.
Uses & applications
Used in glassmaking, electronics (piezoelectric applications), abrasive products, landscaping, and lapidary tumbling for hobbyists.
Geological facts
Quartz is one of the most abundant and durable minerals in Earth's continental crust. Its high resistance to mechanical weathering allows it to survive long river transport.
Field identification & locations
Identified by its extreme hardness (scratches glass, cannot be scratched by steel), lack of cleavage, and smooth water-worn surface. Found globally along riverbeds, beaches, and gravel deposits.
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