
sedimentary
Polished orbicular jasper (likely ocean jasper)
Jasper: microcrystalline quartz (SiO₂), with iron oxides and other silicate inclusions
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; opaque, cream-to-golden brown with dark brown/black branching or orbicular patterns; vitreous to waxy luster after polishing; no visible cleavage; specific gravity roughly 2.5–2.9.
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Physical properties
Hardness about 6.5–7 Mohs; opaque, cream-to-golden brown with dark brown/black branching or orbicular patterns; vitreous to waxy luster after polishing; no visible cleavage; specific gravity roughly 2.5–2.9.
Formation & geological history
Formed when silica-rich fluids replaced or cemented volcanic ash and rock, with iron and manganese producing the dark patterns; most jasper is Precambrian to Phanerozoic, while classic ocean jasper formed in volcanic environments of Madagascar.
Uses & applications
Used for cabochons, carvings, spheres, ornaments, and lapidary objects; not generally used as a structural construction stone.
Geological facts
The pictured polished sphere strongly resembles orbicular jasper, though exact identification requires a close view of the pattern and an unpolished surface; “ocean jasper” is a trade name rather than a formal mineral species.
Field identification & locations
Identify by its opaque body, multicolored iron-rich patterning, glassy polish, and lack of obvious individual crystals; common sources include Madagascar, Brazil, India, Mexico, and the United States.
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