
sedimentary
Chert (Flint)
Microcrystalline silica (SiO2)
Hardness 7 (Mohs), tan to gray color, waxy to dull luster, cryptocrystalline structure, conchoidal fracture, specific gravity 2.6
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Physical properties
Hardness 7 (Mohs), tan to gray color, waxy to dull luster, cryptocrystalline structure, conchoidal fracture, specific gravity 2.6
Formation & geological history
Formed as nodules or layers in limestone or chalk through the precipitation of silica from groundwater or biological sources (diatoms/sponges).
Uses & applications
Historically used for stone tools and fire-starting; currently used as construction aggregate or decorative landscape stone.
Geological facts
Chert breaks with a conchoidal (shell-like) fracture, producing very sharp edges which is why it was the primary material for arrowheads and scrapers in prehistoric times.
Field identification & locations
Identify by its extreme hardness (cannot be scratched by steel) and smooth, curved break patterns. Commonly found in stream beds or eroding out of limestone cliffs.
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Cone-in-cone structure (Secondary Sedimentary Structure)
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Clastic Sedimentary Rock Grain (SiO2 dominated)
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Chert Breccia
Brecciated Chert (Microcrystalline Silica)
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Sandstone
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