
sedimentary
Chert / Jasper
Microcrystalline Quartz (SiO2)
Hardness: 6.5-7 on Mohs scale; Color: Tan, brownish-gray, pinkish-orange, buff; Luster: Waxy to vitreous, dull weathered exterior; Cleavage: None (conchoidal fracture); Specific gravity: ~2.65
- Hardness
- 6
- Color
- Tan, brownish-gray, pinkish-orange, buff
- Luster
- Waxy to vitreous, dull weathered exterior
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Tan, brownish-gray, pinkish-orange, buff; Luster: Waxy to vitreous, dull weathered exterior; Cleavage: None (conchoidal fracture); Specific gravity: ~2.65
Formation & geological history
Formed via precipitation of silica-rich fluids in sedimentary layers or within cavities of volcanic/limestone formations. Fine microcrystalline structure grows as micro-fibrous chalcedony silica.
Uses & applications
Historically used for knapping sharp stone tools like arrowheads and scrapers. Modern uses include decorative rock garden specimens, lapidary cabochons, and landscape stone.
Geological facts
Chert and jasper are among the oldest materials used by early humans for tools due to their predictable conchoidal fracturing which yields razor-sharp edges.
Field identification & locations
Identified in the field by its distinct smooth conchoidal fracture surfaces alongside a dull, weathered chalky rind (cortex) and high hardness (scratches steel). Common in sedimentary basins worldwide.
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