
mineral
Quartz Pebble
Quartz (Silicon Dioxide, SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale. Color: Translucent yellowish-white to honey-toned. Luster: Vitreous (glassy) to waxy when weathered. Crystal structure: Hexagonal. Cleavage: None (conchoidal fracture). Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Translucent yellowish-white to honey-toned
- Luster
- Vitreous (glassy) to waxy when weathered
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Physical properties
Hardness: 7 on Mohs scale. Color: Translucent yellowish-white to honey-toned. Luster: Vitreous (glassy) to waxy when weathered. Crystal structure: Hexagonal. Cleavage: None (conchoidal fracture). Specific gravity: 2.65.
Formation & geological history
Formed from hydrothermal veins or as a primary constituent in igneous rocks like granite. This specimen shows significant rounding and frosting due to alluvial or beach erosion (water transport).
Uses & applications
Used as an abrasive, in glass making, electronics, and as a common decorative pocket stone or garden pebble.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. These rounded pebbles are often called 'river glass' or 'sea quartz' depending on where they were found.
Field identification & locations
Identify in the field by its hardness (will scratch glass/steel) and the lack of cleavage planes. Found globally in riverbeds, beaches, and glacial till. Common everywhere but a staple for beginning collectors.
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