Rock Identifier
Polished Ocean Jasper cabochon (Ocean jasper: microcrystalline quartz (SiO₂), commonly mixed with chalcedony, feldspar, and iron/manganese oxides) — mineral
mineral

Polished Ocean Jasper cabochon

Ocean jasper: microcrystalline quartz (SiO₂), commonly mixed with chalcedony, feldspar, and iron/manganese oxides

AI-generated identification · may be incorrect

Hardness about 6.5–7 Mohs; opaque white, green, gray, and brown orbicular pattern with a waxy to vitreous polish. It is cryptocrystalline, lacks visible cleavage, and has specific gravity near 2.6.

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Physical properties

Hardness about 6.5–7 Mohs; opaque white, green, gray, and brown orbicular pattern with a waxy to vitreous polish. It is cryptocrystalline, lacks visible cleavage, and has specific gravity near 2.6.

Formation & geological history

Formed when silica-rich fluids filled cavities and replaced volcanic rock, producing orbicular chalcedony/jasper; most collectible material formed in Oligocene–Miocene volcanic rocks of Madagascar. The pictured piece is cut and polished.

Uses & applications

Used for cabochons, beads, carvings, and decorative specimens; generally unsuitable for major construction because it occurs as lapidary material.

Geological facts

Its distinctive concentric “orb” patterns arise from alternating chalcedony, quartz, and mineral-rich layers. Ocean jasper is also marketed as orbicular jasper, though patterns and composition vary substantially.

Field identification & locations

Identify it by testing for quartz-like hardness, opaque orbicular spots, and a smooth polish; avoid confusing it with painted or dyed jasper. Classic sources are the remote northwest coast of Madagascar, especially near Marovato.