
mineral
Polished orbicular jasper (likely ocean jasper)
Jasper, microcrystalline quartz (SiO₂), with iron-oxide and volcanic-mineral inclusions
AI-generated identification · may be incorrectHardness 6.5–7 Mohs; opaque brown, gray, cream, and reddish-orange colors; waxy to vitreous luster; cryptocrystalline quartz with no cleavage and conchoidal fracture. The rounded, polished form is a tumbled specimen.
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Physical properties
Hardness 6.5–7 Mohs; opaque brown, gray, cream, and reddish-orange colors; waxy to vitreous luster; cryptocrystalline quartz with no cleavage and conchoidal fracture. The rounded, polished form is a tumbled specimen.
Formation & geological history
Forms when silica-rich fluids replace or cement volcanic ash and rock, with iron oxides producing the colors and orbicular patterns. Ocean jasper formed mainly in Miocene volcanic environments of Madagascar, roughly 5–20 million years ago.
Uses & applications
Used for cabochons, beads, carvings, lapidary pieces, and decorative stone. Small tumbled pieces commonly sell for about $2–$10; unusually patterned specimens may reach $20–$50.
Geological facts
Jasper is a variety of opaque chalcedony and microcrystalline quartz rather than a separate mineral species. Orbicular jasper is prized for concentric or radiating inclusion patterns.
Field identification & locations
Identify it by its opaque, fine-grained body, glassy/waxy polish, hardness, and lack of visible cleavage; it should resist scratching by a steel blade. Common sources include Madagascar, Brazil, India, Mexico, and the western United States.
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