
sedimentary
Chert (Jasper/Agate variety)
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 Mohs; Color: Brown, tan, and greenish-grey banding; Luster: Waxy to dull; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.6-2.65
- Hardness
- 6
- Color
- Brown, tan, and greenish-grey banding
- Luster
- Waxy to dull
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Physical properties
Hardness: 6.5-7 Mohs; Color: Brown, tan, and greenish-grey banding; Luster: Waxy to dull; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.6-2.65
Formation & geological history
Formed through the accumulation of silica-rich fluids in sedimentary environments or as nodules in limestone/chalk. Often involves the replacement of organic material or the deposition of silica from hydrothermal fluids.
Uses & applications
Commonly used in lapidary work for making cabochons, beads, and tumbled stones. Historically used for making sharp tools like arrowheads due to its conchoidal fracture.
Geological facts
Chert is so durable that it often survives as smooth pebbles in riverbeds and on beaches long after the surrounding rock has eroded away. Varieties with high iron content are typically called Jasper.
Field identification & locations
Identify in the field by its waxy texture, inability to be scratched by a steel knife, and smooth, shell-like (conchoidal) break patterns. Found globally in creek beds and gravel deposits.
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