
sedimentary
Chert (often called Jasper or Flint)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale. Color: Highly variable, featuring reds, yellows, and browns due to iron inclusions. Luster: Waxy to dull. Structure: Microcrystalline quartz. Fracture: Conchoidal (shell-like curves).
- Hardness
- 6
- Luster
- Waxy to dull
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Physical properties
Hardness: 6.5-7 on Mohs scale. Color: Highly variable, featuring reds, yellows, and browns due to iron inclusions. Luster: Waxy to dull. Structure: Microcrystalline quartz. Fracture: Conchoidal (shell-like curves).
Formation & geological history
Formed by the precipitation of silica from aqueous fluids, often replacing organic material or occupying voids in limestone. It can form as nodules or bedded deposits and dates from various geological eras, including the Paleozoic.
Uses & applications
Historically used for stone tools (knapping) due to its sharp edges. Modernly used in lapidary work for jewelry, cabochons, and as decorative gravel.
Geological facts
Chert was one of the first materials utilized by early humans for tools because of its predictable fracture pattern. When it is red or yellow, it is commonly referred to in the lapidary trade as Jasper.
Field identification & locations
Identify in the field by its hardness (will scratch glass), waxy luster, and curved, glass-like fracture surfaces. Frequently found in stream beds, gravel pits, and eroding out of limestone outcrops.
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