
mineral
Tumbled jasper (likely brecciated or leopard jasper)
Microcrystalline quartz/chalcedony, SiO₂, with iron-oxide inclusions
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; opaque reddish-brown, cream, and mauve coloration; typically dull to waxy luster; cryptocrystalline quartz with no visible cleavage and conchoidal fracture. The rounded shape indicates tumbling or natural water wear.
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Physical properties
Hardness about 6.5–7 Mohs; opaque reddish-brown, cream, and mauve coloration; typically dull to waxy luster; cryptocrystalline quartz with no visible cleavage and conchoidal fracture. The rounded shape indicates tumbling or natural water wear.
Formation & geological history
Jasper forms when silica-rich fluids replace or cement volcanic ash, sediments, or brecciated rock, with iron oxides producing red-brown tones. It may form across many geological ages, commonly in volcanic and sedimentary environments.
Uses & applications
Used for cabochons, beads, carvings, polished stones, lapidary décor, and inexpensive jewelry; rarely used as a minor ornamental building stone.
Geological facts
Brecciated jasper contains angular fragments cemented by chalcedony, while leopard jasper shows orbicular or spotted patterns; the image’s pattern is not diagnostic enough for a precise variety.
Field identification & locations
Identify it by its opaque patterned body, glassy-to-waxy silica texture, lack of cleavage, and inability to scratch it with a steel knife easily. Common sources include India, Madagascar, Brazil, Mexico, and the western United States.
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