
mineral
Quartz Pebble
Silicon Dioxide (SiO2)
Hardness: 7 on the Mohs scale; Color: White to translucent; Luster: Vitreous to waxy (when water-worn); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 on the Mohs scale
- Color
- White to translucent
- Luster
- Vitreous to waxy (when water-worn)
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Physical properties
Hardness: 7 on the Mohs scale; Color: White to translucent; 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 solutions or cooling magma. This specific specimen is a 'river rock' or 'tumble' shaped by hydraulic erosion, where flowing water rounds the edges of broken quartz fragments over hundreds to thousands of years.
Uses & applications
Common quartz pebbles are used in landscaping, as drainage gravel, in glass manufacturing when crushed, and as simple decorative collectibles or worry stones.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. These rounded white pebbles are often called 'lucky stones' by children and are ubiquitous in riverbeds worldwide.
Field identification & locations
Identify by its ability to scratch glass, lack of cleavage, and white/milky appearance. They are found globally in riverbeds, beaches, and glacial till. Collectors look for high clarity or unique inclusions.
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Schist
Schist
Metamorphic
Epidote
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Gypsum (variety Selenite or Alabaster)
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