
rock
Orbicular jasper (ocean jasper)
Silicified orbicular rhyolite; predominantly microcrystalline quartz/chalcedony (SiO₂) with iron-oxide-rich inclusions
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; opaque cream, red, and brown orbicules, with a waxy to vitreous luster and no obvious cleavage. The concentric spots are silica-rich spherulites and iron-oxide/mineral inclusions.
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Physical properties
Hardness about 6.5–7 Mohs; opaque cream, red, and brown orbicules, with a waxy to vitreous luster and no obvious cleavage. The concentric spots are silica-rich spherulites and iron-oxide/mineral inclusions.
Formation & geological history
A volcanic silica-rich rock formed when rhyolitic lava cooled and devitrified, producing orbicular textures later cemented or replaced by chalcedony. Classic ocean jasper formed in Madagascar, mainly in Miocene-age volcanic rocks (roughly 5–23 million years old).
Uses & applications
Used for cabochons, polished stones, carvings, beads, and decorative objects; valued primarily as a lapidary and collector material rather than construction stone.
Geological facts
Its “eye” patterns vary greatly from specimen to specimen, and many marketed examples are more accurately called orbicular jasper or orbicular rhyolite than true ocean jasper.
Field identification & locations
Identify it by the distinctive rounded, concentric red-and-cream orbs in a silica-rich matrix, high hardness, and inability to scratch with a steel knife easily. Common sources include Madagascar; similar orbicular jaspers occur in Oregon, Mexico, and Australia.
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