Rock Identifier
Orbicular jasper (likely ocean jasper) (Silica-rich microcrystalline quartz/chalcedony with feldspar, clay minerals, and iron oxides) — mineral
mineral

Orbicular jasper (likely ocean jasper)

Silica-rich microcrystalline quartz/chalcedony with feldspar, clay minerals, and iron oxides

AI-generated identification · may be incorrect

Hardness about 6.5–7 Mohs; gray-green to brown matrix with cream-white rounded orbicules, mostly dull to subtly waxy luster, and no obvious cleavage. The specimen appears naturally rough and fine-grained, with orbicular texture visible throughout.

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Physical properties

Hardness about 6.5–7 Mohs; gray-green to brown matrix with cream-white rounded orbicules, mostly dull to subtly waxy luster, and no obvious cleavage. The specimen appears naturally rough and fine-grained, with orbicular texture visible throughout.

Formation & geological history

Formed by silica-rich volcanic or hydrothermal processes that produced concentric mineral growths and cemented them in a fine-grained matrix; exact age depends on locality, commonly Paleozoic to Mesozoic. Similar material is especially associated with Madagascar, though visual identification alone cannot confirm locality.

Uses & applications

Used as lapidary rough, cabochons, carvings, ornamental stone, and collectible specimens; it is generally not used as a structural construction stone.

Geological facts

The rounded “eyes” are orbicules, typically built from concentric layers of chalcedony, quartz, feldspar, and iron-bearing minerals. “Ocean jasper” is a trade name rather than a single strictly defined mineral species.

Field identification & locations

Look for hard, opaque, silica-rich material with rounded contrasting orbs; a steel file should barely scratch it, while quartz can scratch it. Commonly found in Madagascar, Mexico, Australia, and other volcanic terrains.