
mineral
Quartz Pebble
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale. Color: Off-white to milky white with light yellowish/brownish iron stains. Luster: Vitreous to dull (weathered surface). Crystal Structure: Trigonal/Hexagonal. Cleavage: None (conchoidal fracture). Specific Gravity: ~2.65.
- Hardness
- 7 on Mohs scale
- Luster
- Vitreous to dull (weathered surface)
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Physical properties
Hardness: 7 on Mohs scale. Color: Off-white to milky white with light yellowish/brownish iron stains. Luster: Vitreous to dull (weathered surface). Crystal Structure: Trigonal/Hexagonal. Cleavage: None (conchoidal fracture). Specific Gravity: ~2.65.
Formation & geological history
Formed through crystallization in igneous veins or metamorphic environments. This rounded pebble shape was formed through aquatic or subaerial erosion, where water currents or waves naturally tumbled and smoothed the rock over time.
Uses & applications
Commonly used in landscaping, water filtration, construction aggregates, and as rock tumbling material for hobbyists.
Geological facts
Quartz is one of the most abundant and durable minerals on Earth's surface, highly resistant to both chemical and mechanical weathering, which allows quartz pebbles to survive long transport along rivers and beaches.
Field identification & locations
Look for a smooth, rounded surface with light coloration, high hardness that easily scratches glass, and a dull-to-waxy finish. Found abundantly in riverbeds, gravel pits, beaches, and glaciated terrains worldwide.
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