
mineral
Polished orbicular jasper (likely ocean jasper)
Jasper, a microcrystalline quartz variety; mainly SiO₂ with iron-oxide and other mineral inclusions
AI-generated identification · may be incorrectOpaque, black-gray, mustard-yellow, and rusty-orange orbicular pattern with a glassy polish; Mohs hardness about 6.5–7, no visible cleavage, cryptocrystalline quartz structure, and specific gravity around 2.6. The rounded specimen is human-polished.
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Physical properties
Opaque, black-gray, mustard-yellow, and rusty-orange orbicular pattern with a glassy polish; Mohs hardness about 6.5–7, no visible cleavage, cryptocrystalline quartz structure, and specific gravity around 2.6. The rounded specimen is human-polished.
Formation & geological history
Forms when silica-rich fluids cement volcanic ash or replace volcanic rock, with iron oxides producing yellow-orange coloration and orbicular textures. Classic ocean jasper formed in Oligocene–Miocene volcanic rocks of Madagascar, though similar jasper occurs worldwide.
Uses & applications
Used for cabochons, carvings, palm stones, beads, and decorative objects; attractive polished pieces are valued by collectors rather than for industrial use.
Geological facts
“Ocean jasper” is a trade name, not a single formally defined mineral species. Orbicular patterns may consist of radiating quartz, feldspar, chalcedony, and iron-oxide-rich zones.
Field identification & locations
Identify by its opaque hardness, waxy-to-glassy luster, multicolored concentric or orb-like patches, and resistance to scratching by steel; it should not fizz in dilute acid. Common sources include Madagascar, Mexico, Oregon, and Australia.
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