
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 incorrectTypically 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.
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