Rock Identifier
Polished orbicular jasper (Silicified volcanic breccia or rhyolitic jasper; primarily microcrystalline quartz (SiO₂) with iron-oxide and other mineral inclusions) — rock
rock

Polished orbicular jasper

Silicified volcanic breccia or rhyolitic jasper; primarily microcrystalline quartz (SiO₂) with iron-oxide and other mineral inclusions

AI-generated identification · may be incorrect

Typically Mohs 6.5–7, opaque, orange-yellow with black, gray, and cream orbicular or brecciated patterns; waxy to vitreous luster when polished. Massive, noncleavable, and commonly has specific gravity around 2.5–2.7.

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Physical properties

Typically Mohs 6.5–7, opaque, orange-yellow with black, gray, and cream orbicular or brecciated patterns; waxy to vitreous luster when polished. Massive, noncleavable, and commonly has specific gravity around 2.5–2.7.

Formation & geological history

Forms when silica-rich volcanic fluids replace or cement volcanic ash, breccia, or spherulitic rhyolite; iron oxides create the orange coloration. Most examples are Cenozoic to older volcanic rocks, with exact age depending on locality.

Uses & applications

Used for cabochons, beads, carvings, polished stones, and lapidary collectibles; rarely used in construction because of its decorative value and small occurrence size.

Geological facts

The rounded shape and glossy surface indicate tumbling or polishing rather than natural weathering. Similar material is sold as ocean jasper, leopard jasper, or rainforest jasper, though trade names are not always scientifically precise.

Field identification & locations

Identify it by its fine-grained opaque quartz texture, hardness, and contrasting iron-rich patterns; it should resist scratching by a steel knife. Common sources include Madagascar, Mexico, Australia, and the western United States.