
mineral
Polished ocean jasper (orbicular jasper), probable
Microcrystalline quartz (SiO₂), chiefly chalcedony with iron-oxide and other mineral inclusions
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; multicolored red, green, gray, and yellow-brown patterns; vitreous to waxy luster; opaque, with no visible cleavage and conchoidal fracture. The smooth rounded surface indicates tumbling or natural water wear.
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Physical properties
Hardness about 6.5–7 Mohs; multicolored red, green, gray, and yellow-brown patterns; vitreous to waxy luster; opaque, with no visible cleavage and conchoidal fracture. The smooth rounded surface indicates tumbling or natural water wear.
Formation & geological history
Forms when silica-rich fluids replace or fill cavities in volcanic rock, with iron and other oxides producing the colors and patterns; most ocean jasper is Oligocene–Miocene age (roughly 5–30 million years) from Madagascar. Exact identification is uncertain from the photograph.
Uses & applications
Used as a lapidary stone for cabochons, beads, carvings, and polished display pieces; generally decorative rather than industrial.
Geological facts
Ocean jasper is valued for orbicular “eye” patterns, though this specimen appears more brecciated or mottled than strongly orbicular. Similar material may be sold simply as jasper or polychrome jasper.
Field identification & locations
Identify by its opaque multicolor silica body, glassy/waxy polish, and lack of cleavage; common sources include Madagascar, Brazil, India, and the western United States. A specific locality requires testing or provenance.
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