
sedimentary
Chert (Red Jasper variant)
Silicon dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 Mohs; Color: Brick red to brownish-red; Luster: Dull to waxy; Structure: Microcrystalline/cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7
- Hardness
- 6
- Color
- Brick red to brownish-red
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5-7 Mohs; Color: Brick red to brownish-red; Luster: Dull to waxy; Structure: Microcrystalline/cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7
Formation & geological history
Formed through the accumulation of silica-rich microfossils or chemical precipitation in marine or volcanic environments, later lithified into dense rock. Often found in nodules within limestone or as bedded deposits.
Uses & applications
Historically used for stone tools (knapping); currently used for jewelry, lapidary cabochons, landscaping, and industrial abrasives.
Geological facts
Red chert is often called Jasper when it is opaque and colored by iron inclusions. It has been used by humans for hundreds of thousands of years to create sharp-edged tools due to its predictable conchoidal fracturing.
Field identification & locations
Identify in the field by its high hardness (scratches glass), smooth waxy feel, and characteristic shell-like (conchoidal) curved breakage patterns. Commonly found in river beds or eroded sedimentary outcrops.
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