Rock Identifier
Orbicular jasper (ocean jasper) (Silicified orbicular rhyolite; predominantly microcrystalline quartz/chalcedony (SiO₂) with iron-oxide-rich inclusions) — rock
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Orbicular jasper (ocean jasper)

Silicified orbicular rhyolite; predominantly microcrystalline quartz/chalcedony (SiO₂) with iron-oxide-rich inclusions

AI-generated identification · may be incorrect

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.

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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.