
mineral
Polished ocean jasper / orbicular jasper
Microcrystalline quartz (chalcedony), SiO₂, with iron-oxide and other mineral inclusions
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; opaque, glassy-to-waxy luster when polished, with reddish-brown, mustard-yellow, cream, and green mottling. It has no visible cleavage and a cryptocrystalline quartz structure; specific gravity is approximately 2.5–2.7.
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Physical properties
Hardness about 6.5–7 Mohs; opaque, glassy-to-waxy luster when polished, with reddish-brown, mustard-yellow, cream, and green mottling. It has no visible cleavage and a cryptocrystalline quartz structure; specific gravity is approximately 2.5–2.7.
Formation & geological history
Forms when silica-rich fluids fill cavities or replace volcanic rock, with iron and other impurities producing the colors and patterns. Most ocean jasper originates in Oligocene–Miocene volcanic rocks of Madagascar, roughly 5–30 million years old.
Uses & applications
Used for cabochons, beads, carvings, polished stones, and decorative objects; attractive patterned pieces are popular with collectors.
Geological facts
“Ocean jasper” is a trade name, not a single mineral species; orbicular patterns may resemble eyes or cellular growth rings.
Field identification & locations
Identify it by its very fine-grained, opaque chalcedony body, hardness, and natural multicolor orbicular or brecciated patterns; glass scratches more easily. Common sources include Madagascar, Mexico, Australia, and Indonesia.
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