
sedimentary
Polished brown quartz-rich rock, possibly chert or jasper
Microcrystalline quartz (SiO₂), likely chert/jasper; exact identification is uncertain from the image
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; brown, gray, and cream mottling with a dull to waxy luster and irregular conchoidal-looking fracture. It appears fine-grained and partly polished, with no clearly visible crystal cleavage.
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Physical properties
Hardness about 6.5–7 Mohs; brown, gray, and cream mottling with a dull to waxy luster and irregular conchoidal-looking fracture. It appears fine-grained and partly polished, with no clearly visible crystal cleavage.
Formation & geological history
Chert forms when silica precipitates from groundwater or replaces sediments, commonly during diagenesis; jasper is an opaque iron-rich variety. Formation ages range widely from Precambrian to recent sedimentary environments.
Uses & applications
Used for carving, cabochons, beads, tumbled stones, and occasionally ornamental stone; historically, chert was important for sharp tools and fire-starting.
Geological facts
The specimen may also be a brecciated or iron-stained jasper/chert, but the photograph does not show diagnostic banding or mineral grains clearly enough for a precise variety.
Field identification & locations
Look for a glassy or waxy surface, very fine texture, conchoidal fracture, and inability to scratch it with a steel knife; quartz-rich material can scratch glass. Common sources include sedimentary basins worldwide, especially flint and jasper localities.
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