
mineral
Quartz Pebble (Tumbled / Beach Pebble)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale. Color: Milky white to pale pinkish-orange with iron staining. Luster: Vitreous to waxy. Crystal structure: Trigonal/Hexagonal. Specific gravity: 2.65. Cleavage: None (conchoidal fracture).
- Hardness
- 7 on Mohs scale
- Color
- Milky white to pale pinkish-orange with iron staining
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 on Mohs scale. Color: Milky white to pale pinkish-orange with iron staining. Luster: Vitreous to waxy. Crystal structure: Trigonal/Hexagonal. Specific gravity: 2.65. Cleavage: None (conchoidal fracture).
Formation & geological history
Formed in hydrothermal veins, pegmatites, and metamorphic environments. This specific specimen has been naturally or mechanically tumbled and smoothed, likely in a river, ocean beach, or rock tumbler.
Uses & applications
Commonly collected as pocket stones, decorative gravel, landscaping, tumbled gemstone collections, and used for craft projects.
Geological facts
Quartz is one of the most abundant minerals in Earth's continental crust. Pure quartz is transparent and colorless, but impurities like iron oxides give stones warm yellow, orange, or reddish hues.
Field identification & locations
Identified by its Mohs hardness of 7 (can scratch glass and steel easily), waxy to vitreous sheen, and lack of distinct cleavage. Commonly found along shorelines, gravel bars, and riverbeds globally.
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
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Epidote
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Igneous Pegmatite
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Granite
Granite (Phaneritic intrusive igneous rock)
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