
mineral
Tumbled orbicular/patterned jasper (likely brecciated jasper)
Microcrystalline quartz (SiO₂) with iron-oxide and possibly calcite/chalcedony veining
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; dark gray to black with tan, cream, and rusty-brown branching veins; opaque, waxy to vitreous luster, cryptocrystalline quartz, and no obvious cleavage. The rounded surface indicates tumbling and polishing.
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Physical properties
Hardness about 6.5–7 Mohs; dark gray to black with tan, cream, and rusty-brown branching veins; opaque, waxy to vitreous luster, cryptocrystalline quartz, and no obvious cleavage. The rounded surface indicates tumbling and polishing.
Formation & geological history
Forms when silica-rich fluids cement and replace volcanic or sedimentary material, with iron oxides producing the brown veining; exact geological age and locality cannot be determined from the image. Common sources include Madagascar, India, Indonesia, Brazil, and the western United States.
Uses & applications
Used for cabochons, beads, carvings, decorative stones, and inexpensive polished specimens; it is generally ornamental rather than industrial.
Geological facts
Jasper is an opaque variety of chalcedony or microcrystalline quartz, and its patterns are produced by impurities, brecciation, and mineral-rich fluids. The specimen may also be sold under locality or trade names such as Picasso jasper, though visual identification alone is insufficient.
Field identification & locations
Identify by its opaque quartz-like body, very fine texture, glassy/waxy polish, and resistance to scratching by a steel knife; avoid acid and destructive tests. It is a polished tumbled geological specimen, not a crystal with visible crystal faces.
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