
sedimentary
Polished brown chert or jasper pebble
Microcrystalline quartz (SiO₂), likely iron-stained chert/jasper
AI-generated identification · may be incorrectTypically hardness 6.5–7 Mohs, opaque brown to reddish-brown color, waxy to glassy luster, very fine-grained cryptocrystalline structure, and no visible cleavage. The rounded, glossy surface indicates natural water wear or tumbling/polishing.
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Physical properties
Typically hardness 6.5–7 Mohs, opaque brown to reddish-brown color, waxy to glassy luster, very fine-grained cryptocrystalline structure, and no visible cleavage. The rounded, glossy surface indicates natural water wear or tumbling/polishing.
Formation & geological history
Chert forms when silica-rich fluids replace or precipitate from sediment, commonly in limestone or marine sediments; iron oxides create the brown coloration. Its exact geological age cannot be determined from the photograph.
Uses & applications
Used as decorative stone, lapidary material, cabochons, beads, and occasionally as a durable aggregate or toolstone. This specimen appears primarily ornamental or collectible.
Geological facts
Chert fractures conchoidally and can produce extremely sharp edges when broken. Jasper is an opaque, impure variety of chert containing iron oxides and other minerals.
Field identification & locations
Identify with a steel scratch test (it should resist scratching), absence of cleavage, and conchoidal fracture; a streak test is usually white to pale brown. Common sources include river gravels and sedimentary regions worldwide.
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