
mineral
Polished ocean jasper (orbicular jasper)
Microcrystalline quartz (SiO₂), commonly with chalcedony and iron-rich alteration minerals
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; pale blue-gray, cream, and brown concentric orbicular patterns; waxy to vitreous luster; cryptocrystalline quartz with no visible cleavage. The piece appears cut and polished.
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Physical properties
Hardness about 6.5–7 Mohs; pale blue-gray, cream, and brown concentric orbicular patterns; waxy to vitreous luster; cryptocrystalline quartz with no visible cleavage. The piece appears cut and polished.
Formation & geological history
A silica-rich volcanic rock, commonly rhyolitic, later replaced and filled by chalcedony and quartz in cavities and fractures; classic ocean jasper formed in Miocene volcanic rocks of Madagascar. Geological age is roughly 5–20 million years.
Uses & applications
Used for cabochons, beads, carvings, decorative slabs, and lapidary collections; not generally used as a construction stone.
Geological facts
Orbicular patterns result from repeated growth of quartz, feldspar, and iron-oxide-rich layers around nuclei. “Ocean jasper” is a trade name rather than a formally distinct mineral species.
Field identification & locations
Identify it by rounded orbicular or eye-like patterns, opaque-to-translucent chalcedony, and a polished waxy surface; classic material is associated with Madagascar’s northwest coast. Similar orbicular jasper occurs elsewhere, so locality confirmation matters.
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