
sedimentary
Quartz Pebble
Crystalline Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: white to light gray, translucent; Luster: waxy to vitreous; Crystal structure: Trigonal (though rounded by water); Specific gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- white to light gray, translucent
- Luster
- waxy to vitreous
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Physical properties
Hardness: 7 on Mohs scale; Color: white to light gray, translucent; Luster: waxy to vitreous; Crystal structure: Trigonal (though rounded by water); Specific gravity: 2.65
Formation & geological history
Formed via crystallization from silica-rich fluids (hydrothermal or igneous) and later eroded into a stream or beach pebble through water action, likely during the Holocene or Pleistocene era.
Uses & applications
Used in construction aggregates, landscaping, and occasionally as a source of silica for glassmaking or in jewelry lapidary for tumbling.
Geological facts
Quartz is one of the most abundant minerals on Earth's crust. Most beach and river pebbles in temperate zones are composed of quartz because of its extreme physical and chemical durability compared to other minerals.
Field identification & locations
Identify by its inability to be scratched by steel, its smooth water-worn surface, and its resistance to acid. Commonly found in riverbeds, glacial deposits, and along coastlines.
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