
mineral
Quartz Pebble
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Tan, beige, or off-white; Luster: Vitreous to waxy (smooth from water wear); Crystal Structure: Trigonal (not visible in pebble form); Cleavage: None; Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Tan, beige, or off-white
- Luster
- Vitreous to waxy (smooth from water wear)
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Physical properties
Hardness: 7 on Mohs scale; Color: Tan, beige, or off-white; Luster: Vitreous to waxy (smooth from water wear); Crystal Structure: Trigonal (not visible in pebble form); Cleavage: None; Specific Gravity: 2.65
Formation & geological history
Formed from igneous or metamorphic activity, then weathered and transported by water in rivers or coastal environments, rounding the edges through erosion.
Uses & applications
Commonly used in landscaping, as a component of concrete, or as a decorative 'worry stone' when naturally polished and rounded.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Rounded pebbles like this one are often found in fluvial (river) deposits and can be millions of years old.
Field identification & locations
Identify by its hardness (it will scratch glass) and lack of visible grains or pores. Found globally in riverbeds, beaches, and glacial till.
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