
mineral
Quartz (River Pebble) and Chert/Jasper
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale. Color: Translucent white to tan (quartz) and brownish-red (chert). Luster: Vitreous to waxy. Crystal structure: Hexagonal/Trigonal. Cleavage: None (conchoidal fracture).
- Hardness
- 7 on Mohs scale
- Color
- Translucent white to tan (quartz) and brownish-red (chert)
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 on Mohs scale. Color: Translucent white to tan (quartz) and brownish-red (chert). Luster: Vitreous to waxy. Crystal structure: Hexagonal/Trigonal. Cleavage: None (conchoidal fracture).
Formation & geological history
Formed through hydrothermal or igneous processes (Quartz) and chemical sedimentary precipitation (Chert). These specific specimens are water-worn river pebbles likely millions of years old, rounded by fluvial erosion.
Uses & applications
Common quartz is used for abrasives and glassmaking; these specific pebbles are primarily collected for hobbyist tumbling, lapidary practice, or decorative landscaping.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Chert was historically used by indigenous peoples for stone tools and arrowheads due to its predictable conchoidal fracture leading to sharp edges.
Field identification & locations
Identify by its ability to scratch glass and lack of cleavage. These are common in river beds, beaches, and glacial till. Collectors look for unique banding or clarity in similar specimens.
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