
sedimentary
Polished brown pebble, likely chert or jasper
Microcrystalline quartz (SiO₂), possibly iron-stained chert/jasper
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; brown to reddish-brown, opaque, fine-grained, with a waxy to dull luster and no visible cleavage. The smoothly tumbled shape and dark glossy edge indicate polishing or natural water wear.
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Physical properties
Hardness about 6.5–7 Mohs; brown to reddish-brown, opaque, fine-grained, with a waxy to dull luster and no visible cleavage. The smoothly tumbled shape and dark glossy edge indicate polishing or natural water wear.
Formation & geological history
Chert forms when silica-rich fluids replace or cement sediment, commonly in limestone or marine sediments; jasper is an iron-rich opaque variety. Formation ages vary widely, from Precambrian to recent, while the rounded specimen was later transported and polished.
Uses & applications
Used for decorative objects, cabochons, beads, carvings, and occasionally tools; its small size and plain color give it modest ornamental value.
Geological facts
Chert breaks with smooth conchoidal fracture and can resemble flint; jasper differs mainly by its stronger iron staining and opaque appearance.
Field identification & locations
Look for a glassy edge, conchoidal fracture, uniform fine texture, and ability to scratch ordinary glass; common sources include river gravels and sedimentary regions worldwide. Exact identification requires a fresh edge or hardness/streak testing.
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