
metamorphic
Quartzite and Jasper Pebbles
Quartzite (re-crystallized Quartz) and Cryptocrystalline Quartz (SiO2)
Hardness: 6.5-7 (Mohs), Color: red, pink, brown, and grey, Luster: dull to vitreous, Crystal Structure: trigonal/hexagonal micro-textures, Specific Gravity: approx. 2.65
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 (Mohs), Color: red, pink, brown, and grey, Luster: dull to vitreous, Crystal Structure: trigonal/hexagonal micro-textures, Specific Gravity: approx. 2.65
Formation & geological history
Formed from the regional or contact metamorphism of quartz-rich sandstone. Most specimens in river gravels are aged between dozens to hundreds of millions of years old.
Uses & applications
Used for landscaping, decorative garden stones, tumbling, lapidary work, and as high-quality construction aggregate.
Geological facts
These pebbles are rounded due to fluvial erosion, meaning they were shaped by the movement of water over a long period. Many of the red hues come from trace inclusions of hematite.
Field identification & locations
Identify in the field by their extreme hardness (they will scratch glass) and lack of visible mineral grains. Commonly found in riverbeds, glacial tills, and shorelines worldwide.
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