Rock Identifier
Orbicular jasper (likely ocean jasper) (Silica-rich jasper/chalcedony, mainly microcrystalline quartz (SiO₂), with feldspar, zeolites, chlorite, and iron oxides) — mineral
mineral

Orbicular jasper (likely ocean jasper)

Silica-rich jasper/chalcedony, mainly microcrystalline quartz (SiO₂), with feldspar, zeolites, chlorite, and iron oxides

AI-generated identification · may be incorrect

Hardness about 6.5–7; opaque, green, cream, gray, and brown; dull to waxy luster; microcrystalline, massive structure with no cleavage. Rounded orbicular patterns and polished surface are visible.

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Physical properties

Hardness about 6.5–7; opaque, green, cream, gray, and brown; dull to waxy luster; microcrystalline, massive structure with no cleavage. Rounded orbicular patterns and polished surface are visible.

Formation & geological history

A volcanic or volcaniclastic silica-rich rock formed when mineral-rich fluids filled cavities and replaced material, producing orbicules. Ocean jasper is chiefly associated with Miocene volcanic rocks of Madagascar, though similar orbicular jasper occurs elsewhere.

Uses & applications

Used as a lapidary stone for cabochons, beads, carvings, and polished specimens; it has little industrial value compared with ordinary quartz.

Geological facts

The green coloration commonly reflects chlorite or other alteration minerals, while cream and brown zones may contain feldspar and iron oxides. “Ocean jasper” is a trade name rather than a single strict mineral species.

Field identification & locations

Identify it by its opaque multicolored orbicular texture, very fine grain, and glass-scratching hardness; it should not show the translucency typical of agate. Common sources include Madagascar, Mexico, Australia, and Oregon.