
sedimentary
Tumbled brown chert or jasper pebble
Microcrystalline quartz (SiO₂), likely chert/jasper
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; opaque brown to honey-colored, with a waxy to dull luster and very fine-grained, cryptocrystalline structure. The rounded shape indicates natural water wear or tumbling; no visible cleavage, and a white weathered patch is present.
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Physical properties
Hardness about 6.5–7 Mohs; opaque brown to honey-colored, with a waxy to dull luster and very fine-grained, cryptocrystalline structure. The rounded shape indicates natural water wear or tumbling; no visible cleavage, and a white weathered patch is present.
Formation & geological history
Chert forms when silica-rich fluids replace or cement sediment, often from siliceous biological remains; jasper is an iron-rich opaque variety. It may range from Paleozoic to recent gravel deposits, depending on source rock.
Uses & applications
Commonly used for knapped tools, ornamental objects, cabochons, beads, and polished stones; this small specimen has modest decorative value.
Geological facts
Its quartz content makes it resistant to weathering and capable of producing a sharp conchoidal fracture. Brown coloration commonly reflects iron oxides or hydroxides.
Field identification & locations
Identify by hardness, lack of cleavage, waxy appearance, and conchoidal fracture; it should scratch glass but not be scratched by a steel knife. Common in river gravels and sedimentary terrains worldwide.
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