
sedimentary
Tumbled quartz-rich pebble, possibly chert or jasper
Microcrystalline quartz (SiO₂), likely chert/jasper; exact identification requires testing
AI-generated identification · may be incorrectBrown-red, rounded, fine-grained, and dull to faintly waxy with small whitish patches; quartz hardness is about 7 Mohs, with no visible cleavage and a conchoidal fracture. Specific gravity is typically 2.6–2.7.
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Physical properties
Brown-red, rounded, fine-grained, and dull to faintly waxy with small whitish patches; quartz hardness is about 7 Mohs, with no visible cleavage and a conchoidal fracture. Specific gravity is typically 2.6–2.7.
Formation & geological history
Likely a naturally water-worn or human-tumbled silica-rich pebble formed from sedimentary microcrystalline quartz; age cannot be determined from the photograph. Chert and jasper form when silica precipitates or replaces sediment.
Uses & applications
Common pieces are used as lapidary material, beads, cabochons, and decorative tumbled stones; low-grade specimens have little industrial value compared with bulk silica.
Geological facts
The reddish-brown color commonly comes from iron oxides or hydroxides. A glass-scratch test can help confirm quartz, though it may damage the specimen.
Field identification & locations
Common in stream gravels and sedimentary regions worldwide; inspect for translucency, conchoidal fracture, and hardness, and distinguish it from softer iron-rich claystone by testing whether it scratches glass.
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