
mineral
Tumbled jasper
Microcrystalline quartz (SiO₂), commonly iron-oxide-bearing chalcedony
AI-generated identification · may be incorrectOpaque, rounded and polished; mottled reddish-brown, tan, and cream colors with earthy to waxy luster. Mohs hardness 6.5–7; cryptocrystalline quartz, no cleavage, specific gravity about 2.6.
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Physical properties
Opaque, rounded and polished; mottled reddish-brown, tan, and cream colors with earthy to waxy luster. Mohs hardness 6.5–7; cryptocrystalline quartz, no cleavage, specific gravity about 2.6.
Formation & geological history
Forms when silica-rich groundwater fills cavities or fractures and becomes colored by iron oxides during diagenesis or volcanic alteration. The specimen is likely geologically ancient, but its exact age and locality cannot be determined from the image.
Uses & applications
Used for tumbled stones, cabochons, carvings, beads, and ornamental objects; durable varieties are also used decoratively. Common material generally has modest value.
Geological facts
Jasper is an opaque variety of chalcedony rather than a distinct single mineral species; color patterns reflect impurities and replacement textures.
Field identification & locations
Common in volcanic and sedimentary terrains worldwide, including the western United States, Madagascar, Brazil, India, and Australia. Identification is supported by opacity, hardness, quartz-like heft, and resistance to scratching by steel; this polished pebble could also be iron-stained agate or another chert.
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